Irkutsk region.
Ekhirit-Bulagatsky district: general information
Educated in 1918.
The population is 31.6 thousand people.
Area - 5.2 thousand km 2.
The average per capita income of the population is 5628 thousand rubles.
Telephone code: +7-39541.
The postal code is 669001.
The head of the district is Igor Petrovich Usov.
Administrative division
Social sphere
Education
The education system of the municipality Ekhirit-Bulagat district includes:
40 educational institutions,
20 preschool educational institutions,
1 educational institution NGO/SPO,
2 institutions of additional education,
2 regional state educational institutions.
The situation with preschool institutions. The queue today is about 800 people. In 2013 this problem filmed in Aluzhino, where a kindergarten for 49 children was opened, in 2014 the picture will change dramatically in Ust-Ordynsky. Of course, for the better. It is planned to commission three kindergartens in the regional center at once: two for 98 children and one large one for 220 children. In a year, the construction of another one, designed for 147 children, will be completed. Thus, they will try very hard to comply with the decree of the President of the Russian Federation and ensure by 2016 preschool education all local residents aged 3 to 7 years.
While the construction of new kindergartens is underway, Ust-Orda is trying to solve the problem by expanding existing ones. And in a rather unexpected way. The know-how of the Yolochka kindergarten is that new group opened in a private house.
There are 4,500 students and over 500 teachers in the district. In 2010, according to Rospotrebnadzor, three educational institutions- in Novonikolaevsk, Khabarovsk and Kharazargay - were recognized as not meeting the requirements of SanPiN. They had to be hastily reconstructed seriously - each took about 15 million rubles. And now here is the Ust-Ordynskaya middle comprehensive school No. 1 im. V. Borsoeva, where the speaker of the Legislative Assembly of the Irkutsk region Lyudmila Berlina once studied, is celebrating her half-century anniversary in a modern guise.
In 2013, a modern sports and recreation complex was opened, which was named after Konstantin Baimeev. Football players, wrestlers, archers, representatives of other sports are engaged here literally from morning to night.
In 2013, 37 million was spent on the overhaul of the Ekhirit-Bulagat inter-settlement leisure center. The building, which turns 75 in 2014, was last renovated in the 1990s. In total, more than 2 thousand people work at the Center, there are three dozen teams of various directions, and eight of them bear the title of people's.
Economy
One of the most successfully developing on the territory of the Ekhirit-Bulagatsky district is the Tugutuysky agricultural enterprise. They started in 2009 with the cultivation of 1,500 hectares of land, the director of the enterprise Vladimir Monkhoev recalls, the yield was 16 centners per hectare. Now about three thousand hectares are used for sowing, and up to 24 centners are harvested.
Up to 70 percent of sour cream and other dairy products sold by private traders at the Central Market and other markets are brought from the Ekhirit-Bulagat district.
Natives and residents of the Ekhirit-Bulagat district
- Khaidurov Efim Leontyevich - designer of sports weapons, winner of the world and European championships.
- Boronoev Asalkhan Olzonovich - Professor of Philosophy and Psychology, St. Petersburg State University.
- Manzhuev Gennady Nikolaevich - master of sports of the USSR and international class in freestyle wrestling, head of the representative office of the Republic of Buryatia in Mongolia.
- Badinnikov Viktor Yakovlevich - academician, rector of the State Technical (St.
Physical and geographical characteristics of the Ekhirit-Bulagat district 1.1 Geographical position, borders, the size of the territory.Ekhirit-Bulagatsky district is a municipal formation in the southeast of the Irkutsk region. The administrative center is the settlement of Ust-Ordynsky. (Figure 1) The Ekhirit-Bulagat district includes the territories of 13 rural settlements, in total 51 settlements.
Municipalities ( rural settlements):
Aluzhinskoye
Akhinsky
Gakhan
Zahalskoe
Kapsalskoye
Korsuk
Kulunkui
Novo-Nikolaevskoe
Oloiskoye
Tugutuyskoe
Ust-Orda
Kharazargai
Kharatai
Fig.1 Administrative-territorial division of the Irkutsk region
Areas are marked with numbers:
1 - Alarsky (UOBO), 2 - Angarsky, 3 - Balagansky, 4 - Bayandaevsky (UOBO), 5 - Bodaibinsky, 6 - Bokhansky (UOBO), 7 - Bratsky, 8 - Zhigalovsky, 9 - Zalarinsky, 10 - Ziminsky, 11 - Irkutsky, 12 - Kazachinsko-Lensky, 13 - Katangsky, 14 - Kachugsky, 15 Kirensky, 16 - Kuitunsky, 17 - Mamsko-Chuysky, 18 - Nizhneilimsky, 19 - Nizhneudinsky, 20 - Nukutsky (UOBO), 21 - Olkhonsky, 22 - Osinsky (UOBO), 23 - Slyudyansky, 24 - Taishetsky, 25 - Tulunsky, 26 - Usolsky, 27 - Ust-Ilimsky, 28 - Ust-Kutsky, 29 - Ust-Udinsky, 30 - Cheremkhovsky, 31 - Chunsky, 32 - Shelekhovsky, 33 - Ekhirit-Bulagatsky (UOBO)
Rice. 2 map of the Ust-Orda Buryat district of the Irkutsk region
The name of the district is due to the residence of large tribal groups of the Buryats - Ekhirits and Bulagats - who formed on this territory and settled throughout the Baikal region.
Ekhirit-Bulagatsky district is located in the south of the Irkutsk region, occupies the southeastern part of the Ust-Ordynsky Buryat district, borders Bayandaevsky in the northeast, Olkhonsky in the east, Irkutsk in the south and southwest, and Bokhansky in the west and in the north - with the Kachug regions. The administrative center is the village of Ust-Ordynsky. Until January 1, 2008, it was the administrative center of the Ust-Orda Buryat Autonomous Okrug. It was the only center of a constituent entity of the Russian Federation with the status of a rural settlement (Fig. 2)
The area of the district is 5.2 thousand square kilometers, the population is 29.4 thousand people (as of 01.01.2010). The area is multinational. Buryats are the indigenous population. Of the other nationalities, Russians predominate, less Ukrainians, Belarusians, Tatars, etc.
The Okrug is located in Cisbaikalia, occupies the southern part of the Leno-Angara plateau. Altitude above sea level is over 1000 meters. The landscape of the district is determined by the Irkutsk-Balaganskaya forest-steppe, within which it is located. The landscape of the district is very picturesque: spacious meadows and pastures interspersed with coniferous forests. The surface is heavily dissected by river valleys.
Most of the district is located within the Angara river basin and only a small, easternmost section lies in the Lena river basin. The territory of the district is irrigated by the tributaries of the Angara river: Unga, Osa, Ida and Kuda. On the territory of the district there are small lakes in the river valleys: Alyaty, Altarik, Orda, Angol.
Main Natural resources districts: oil, combustible gas and condensate, coal, non-metallic building materials (clay, gypsum).
1.2. Geological structure and relief
1. 2.1. Tectonics
Geotectonically, the area is located in the southern part of an ancient platform or ancient continent that formed over a billion years ago and has since been covered only occasionally by continental shallow seas. But before becoming a continent, this section earth's crust has undergone a complex evolution.
During the first three billion years, the processes of formation and synthesis of almost all igneous, metamorphic, sedimentary rocks and minerals, ore formations took place on Earth, and organic life appeared, modern atmosphere, hydrosphere, foundations were formed, the foundations of modern continents, which in the future were no longer experienced significant temperature effects and deformations. One of these continents was the Siberian Precambrian continental ancient platform, which was covered by the sea only at the very beginning of its existence.
The last sea left the territory of the district in the middle of the Paleozoic era, leaving numerous sedimentary rocks of the Vendian with an age of 650 - 570 million years), Cambrian (with an age of 570 - 505 million years) periods geological history Earth. During all this time, the territory of the district in tectonic terms represented two regions different in morphology.
Most of the territory of the district (Osinsky, Bokhansky, Nukutsky)
leveled by a section of the Siberian platform submerged under sea level.
The smaller southeastern part of the okrug (Ekhirit-Bulagatsky, Bayandaevsky) was a site that was more intensively submerged under the sea level - a foredeep gravitating towards the edge of the platform and laid on a stable solid platform foundation. The subsidence of the earth's crust in it was compensated by the accumulation of sedimentary rocks of the Late Proterozoic, Early Paleozoic, Mesozoic and Cenozoic ages. Thus, during the Late Proterozoic - Early Paleozoic (in the interval 650 - 400 million years ago), the marginal trough was filled with sediments, at the very bottom represented by sandstones, siltstones and mudstones. The thickness of these deposits, determined from deep drilling data (Fig. 3), is more than 300 m. These rocks lie directly on the solid crystalline formation of the platform, which in turn is composed of metamorphosed and highly deformed rocks formed at high temperatures and pressures. Consequently, before the arrival of the sea, the basement rocks had to cool down and turn into a fairly vast plain capable of accommodating the whole sea. Geologists called this sea the Angara-Lena trough.
Sediments of a higher stratigraphic level, and, consequently, of a younger age, include sandy layers interspersed with siltstones, mudstones, and carbonate rocks interbedded with marls and anhydrites (Fig. 3). Approximately at the turn of the Precambrian and Phanerozoic tectonic movements slowed down significantly - the mountains stopped growing, the bowing stopped. The so-called period of stable standing of the platform in a hot climate began, i.e., the Siberian continent at that time was somewhere in hot latitudes. Sea water was supplied from the ocean to the platform. Here it evaporated, leaving layers of rock salt, limestone, dolomite, gypsum and anhydrite with a total thickness of 1300-1800 m.
Further, in the Middle Cambrian era, in all likelihood, the connection between the Cambrian seas and the ocean is broken. The seas often begin to dry up, the carbonates remaining on the surface begin to weather, turn into flour, i.e., desert conditions are established in the district.
All this is evidenced by the rocks of the Middle Cambrian deposits of the Verkholenskaya Formation, whose outcrops occupy vast expanses in the northern part of the district (Fig. 3). The sole, the lowest, part of these deposits is composed of clay-marl breccias with fragments of the underlying dolomites of the Angara suite, which are replaced by dolomite flour.
Rice. 2. Geological section along the line of the city of Tolban - Kudinsky ridge.
Platform cover species:
1 - Quaternary system;
2 - Neogene;
3 - Jurassic rocks;
4 - terrigenous rocks of the Late and Middle Cambrian;
5 – carbonate-halogen rocks of the Early Cambrian;
6 – rocks of the Vendian system.
Archean-Proterozoic platform basement rocks:
7 - metamorphic, crumpled into folds;
8 - igneous (a - granites, b - diorites);
9 - faults and thrusts.
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Above are variegated gypsum mudstones, marly dolomites with interlayers of siltstones and sandstones, followed by quartz and carbonate sandstones with interlayers of marls and siltstones, and at the very top lie mainly sandstones. The color of the rocks is predominantly reddish, spotty. The thickness of the Middle Cambrian suite of rocks is from 350 to 550 m.
The time interval between the Cambrian and the Jurassic did not leave any geological traces in the form of rocks. It was during this period that the entire complex of previously formed rocks was deformed into folded structures of various sizes and morphology.
Rice. 3. Geological structure[
5
]
The largest of them extend for many tens of kilometers (Fig. 4). Folding in the sedimentary cover of the platform is most intensively observed near its edge along the eastern margin within the Angara-Lena foredeep. Complex linear narrow ridge-like swells and troughs are widely developed here. With distance from the edge of the platform to its center, the intensity of the folds weakens, they become wider, flatter, the angles on the wings decrease from 20-10°. The folds turn into box-shaped forms, but do not lose their great length and asymmetry. Their northwestern wings are steeper, while the southeastern ones are more gentle. The ratio of the height of the folds to their width is 0.1-0.09
The folds of the Angara-Lena trough can be traced for hundreds of kilometers parallel to the edge of the platform.
From the beginning of the Middle Jurassic, the process of lowering the territory began to prevail and sedimentation processes resumed, thanks to which we have material evidence of the geological history of this period - the rocks of the Jurassic system, which lie on the eroded and highly dissected relief of the Lower Cambrian rocks. In general, on the entire Siberian platform, they are filled with an asymmetric piedmont trough, elongated along the edge of the platform along the Sayan-Baikal domed uplift, which rises in the Jurassic. Its northwestern branch is called the Pre-Sayan foothill trough, and the northeastern branch is called the Pre-Baikal. The latter is superimposed on the Angara-Lena Paleozoic foredeep.
In the Jurassic, the Cis-Baikal trough extended from the Irkutsk Pre-Sayan region to longitude c. Bayanday at a distance of no more than 150 km.
The Pre-Baikal trough of the Mesozoic time is filled with coal-bearing deposits 500-600 m thick in the area of Irkutsk and no more than 300 m in the area of the upper reaches of the river. Where. On the territory of the Okrug, Jurassic formations are known in a significant part and are represented by continental, mainly clastic deposits of the lake-river type.
Rice. 4. Scheme of tectonic structures
The rocks of the Jurassic system indicate that during their formation, paleographic conditions of warm, humid landscapes existed on the territory of the district. Thus, coarse clastic deposits tell about the existence of wide river valleys with winding river channels, and sandy-siltstone and clayey rocks tell about the setting of wide river floodplains with numerous oxbow lakes, swamps, and lakes. The second half of the Mesozoic and almost the entire Paleogene were again an epoch of prolonged regional leveling of the relief of the Siberian Platform under conditions of relative tectonic quiescence and a climate favorable for chemical weathering.
The most ancient Cenozoic rock complexes of the district are represented by unique Paleogene-Neogene deposits that were formed along narrow partial depressions of the Meso-Canozoic age. These sediments are represented by various clays, often high alumina, sandy loams, loams, sands, and brown coals. Occasionally, shell limestones and calcareous fine-grained tuffites are noted. Huge reserves of brick, refractory, drill clay and brown coal are concentrated in these deposits. The thickness of the sediments reaches 250-300 m. They almost everywhere overlie the Cretaceous-Paleogene leveling surface, which is the result of a long uplift or tectonic quiescence of the territory of the district. The distribution area of individual depressions with Paleogene-Neogene deposits borders the Cis-Baikal Cenozoic piedmont trough, which in the district is mostly superimposed on the Angara-Lena Early Paleozoic marginal trough, and less on the Early Middle Jurassic eponymous piedmont trough described above. In the southwest, it goes beyond the territory of the district and in the valley of the river. Angara smoothly merges with the Pre-Sayan Cenozoic foothill foredeep. From the river valley Angara, it extends to the city of Kirensk for a distance of almost 600 km and is one of the most noticeable neotectonic structures of the Siberian Platform.
The Cenozoic Cis-Baikal piedmont trough, like its earlier predecessors, is located on the edge of the Siberian platform and is compensatory in relation to the Baikal arch uplift. To the west, the trough is joined by the comparable Upper Lena uplift, which separates it from the Siberian platform. The latter in the Cenozoic probably experienced a slower uplift, and a plateau was formed on it. The absolute marks of the relief of the territory of the uplift in the basin of the river. Where they fluctuate within 900-1000 m.
The width on the territory of the district reaches 90 km, its axis extends subparallel to the foothills of the Baikal mountain region, its summit surface lies along the axis of the trough at elevations of 400-900 m, and the hinge is inclined in the area of the village. Bayandai to the northeast.
Modern sediments on the geochronological scale belong to the Quaternary or anthropogenic period and are represented by river boulder-pebbles, pebbles, sands and clays up to 60-80 m thick, distributed along modern large river valleys. Loose rocks are widespread on slopes and watersheds. Their thickness on the slopes reaches 10-15 m, and on the watersheds - 1.5-2 m.
1.2.2. Relief
Orthographically, the district is located within the Leno-Angara flat upland, the absolute heights and dissection of which increase from south to north, and the relative elevation changes are 250-350 m. The lowest point of the district's relief is the level of the river. Hangars - 440 m, and the most high mountain located in the north of the Bayandaevsky district - 1048 m.
The relief of the area was formed under the influence of the latest tectonics, erosion-denudation processes and structural and lithological features of bedrocks. Neotectonic movements determined the magnitude of the absolute marks of the territory. They, according to scientists, determined the intensity of the formation of landforms.
The main orographic structure of the Okrug's territory is determined by the following elements of the mega-relief: the Leno-Angara Plateau, slightly inclined to the south; northwestern spurs of the poorly dissected Onot Upland with absolute heights up to 1000 m; the plains of the Pre-Sayan and Pre-Baikal regions with absolute elevations of 500-700 m; Irkutsk-Cheremkhovskaya Plain with a depth of dissection of 30-100 m; The central part in the relief of the Ekhirit-Bulagatsky region is occupied by the Kuda depression, which is a plain 60-80 km wide with a structural ridge-hollow relief. Rather narrow ridges have relative heights of 120-180 m.
The southwestern part of the same area falls within the Irkutsk depression; in the northwest, the Kudinsky depression is bordered by the Kudinsky ridge, and in the southeast, by the Onot upland (Fig. 5).
The ridges are characterized by deep vertical dissection with absolute marks of watersheds of 923 to 1000 m. The depth of incision of river and stream valleys reaches 270-360 m, and the maximum width is 10 km. Within the Kuda and Irkutsk depressions, a structural-erosion relief is developed, consisting of linearly elongated rather narrow ridges and intermountain depressions. The absolute marks of the ridges range from 630 to 909 m, the depth of the erosion incision of the valleys is 120-190 m.
Microforms of cryogenic relief are associated with the wide development within the permafrost region. On the floodplain and above-floodplain terrace deposits, gentle slopes of northern exposure, fissure-polygonal forms are formed, in the wide bottoms of the valleys - bulgunnyakhs up to 5-20 m high, seasonal heaving mounds, reaching in diameter from 8 to 20 m and 0.5-3.0 m height.
On the valley slopes and terraces with a thick cover of loose deposits, there are ravines reaching several hundred meters in length, 10-30 m wide and 2-7 m deep. Here you can also find numerous ruts and gullies - future ravines.
Rice. 5. Orographic scheme
1.3. Climate
The climate of the region, located in the south of the Irkutsk region, is sharply continental with long cold winters, low precipitation throughout the year, and relatively hot short summers.
One of the main climate-forming factors is solar radiation entering the earth, which, in turn, significantly depends on the circulation of air masses (which manifests itself through the cloudiness and transparency of the atmosphere) and the characteristics of the underlying surface.
The main feature of the region's climate - sharp continentality - is due to atmospheric circulation. In winter, a powerful anticyclone is formed on the territory of Eastern Siberia, in which clear calm weather prevails, contributing to the loss of heat from the earth's surface as a result of radiation. characteristic feature summer circulation is an increase in cyclonic activity, frequent repetition of cloudy weather types with precipitation.
The arrival of solar radiation varies across the territory and is determined primarily by astronomical factors - the length of the day (Table 1) and the height of the sun above the horizon. In turn, the value of these parameters depends on the latitude of the place.
The length of the day within the county varies at the southern border of the territory from 7 hours 48 minutes; on the northern one - from 07:26 to 17:06 on December 15 and June 15, respectively. From March to September, the length of the day increases with advancement to the north, and from September to March it decreases.
The height of the sun at noon and the intensity of direct solar radiation on a horizontal surface in a clear sky are shown in Table. 2.
Table 1
Sunrise (at), sunset (w), length of day (p) on the 15th day of each month
Latitudehail
Mean solar time, h min by month
III
VII
VIII
XII
52 p. sh.
8 .02
7.17
6.16
5.05
4.07
3.39
3.57
4.43
5.53
6.23
7.17
8.01
16.16
17.11
18.02
18.55
19.45
20.21
20.15
19.27
18.17
17.09
16.09
15.49
8.14
10.00
11.46
13.50
15.38
16.42
16.18
14.44
12.44
10.50
8.50
7.48
54 p. sh.
8.12
7.42
6.17
5.01
3.58
3.27
3.47
4.36
5.32
6.27
7.27
8.12
16.06
17.06
18.01
18.59
19.54
20.33
20.25
19.34
18.18
17.05
16.01
15.38
7.54
9.44
11.44
13.58
15.56
17.06
16.38
14.58
12.46
10.38
8.34
7.26
table 2
Height of the sun at noon, in degrees
latitude,hail
III
VII
VIII
XII
52 p. sh.
16.8
24.9
35.8
47.7
56.8
61.3
59.6
52.2
41.1
29.6
19.6
14.7
54 p. sh.
14.8
22.9
33.8
45.7
54.8
59.3
57.6
50.2
39.1
27.6
17.6
12.7
Table 3
Intensity of direct solar radiation, cal/cm²
latitude,hail
III
VII
VIII
XII
52 p. sh.
0.57
0.83
1.16
1.47
1.66
1.74
1.71
1.56
1.30
0.98
0.66
0.50
54 p. sh.
0.51
0.38
1.10
1.42
1.62
1.70
1.67
1.52
1.25
0.92
0.60
0.44
The highest height of the sun is observed in June and is 61° 18' on the southern border and 59° 18' on the northern one. The lowest - in December - 14° 42' on the southern border and 12° 42' on the northern. Accordingly, the value of solar radiation reaches 1.71 and 1.67 kcal/cm² months in July, and 0.50 and 0.44 kcal/cm² months in December. (Table 3).
The radiation balance, which determines the residual heat at the earth's surface, is about 3 kcal / cm² in July, and in December - only -0.5 - -0.8 kcal / cm². The period with a long radiation balance, the time of heat accumulation by the underlying surface lasts about 8 months. The sign of the radiation balance changes in spring at the beginning of March, and in autumn in November. In the daily course of solar radiation and radiation balance, the maximum is observed at noon, since at this time the highest height of the sun above the horizon is observed during the day.
atmospheric circulation. For temperate latitudes of the northern hemisphere, the west-east transfer of air masses is characteristic. In general, during the year, the movement of air masses from west to east prevails, which has a high percentage of repetition for many stations of the district, including Ust-Ordynskaya. In certain periods of the year, this mechanism is disturbed by the formation of a baric maximum and minimum over most of the Asian continent, or by the passage of surface cyclones and anticyclones through the territory of the district. The south of the Irkutsk region, which includes the district, is characterized by the fact that almost no Pacific air masses enter here. But very often this territory, in the rear of the cyclones, is invaded by arctic air, which, passing over the continent, transforms into the air of temperate latitudes.
In winter, the weather is determined mainly by the influence of the Asian anticyclone, which reaches its maximum development in January. Clear frosty weather prevails with a significant number of windless days.
Rice. 6. Air temperature and prevailing wind direction in January
Rice. 7. Air temperature and prevailing wind direction in July
Rice. 8. Annual total precipitation
Often at the beginning of winter there are warmings associated with the passage of cyclones from the southern and central regions of Western Siberia.
In spring, when the air temperature rises, the Asian anticyclone weakens, the number of cyclones coming from the southwest and west increases, bringing warm air from the regions of Central Asia and Kazakhstan. This causes sharp short-term warming, which are replaced by strong winds and cooling.
In summer, in contrast to winter, there is a general decrease atmospheric pressure and establishing a cyclonic type of weather. The first half of summer is usually hot, dry, with a lot of clear days. The second half of summer is rich in precipitation. This is due to the arrival of cycles from Mongolia.
In the first half of autumn, cloudy, dry weather with weak winds prevails, which is formed by anticyclones passing through the territory or cyclones coming from the Aral-Caspian basin. In the second half, the invasion of Arctic air masses, cooling and precipitation are increasingly taking place. At the end of autumn, the formation of the Asian anticyclone begins.
Atmospheric pressure and prevailing winds. The most important condition, which determines the direction of the transfer of air masses, is the distribution of atmospheric pressure near the earth's surface and relief. Throughout the year in central and western parts The district is dominated by winds of the northwestern and southeastern directions, in the eastern part there is a high frequency of winds of the northern, northwestern and northeastern directions. The average monthly and annual wind speed for the Ust-Orda station of the Ekhirit-Bulagatsky district is shown in Table 4.
Air temperature. The air weakly absorbs radiation, so the rays of the sun almost do not heat up. It receives the main heat from the surface of the earth heated by the sun's rays.
Table 4
Average monthly and annual wind speed, m/s
Therefore, the onset of the maximum values of air temperature is always delayed in relation to the moment of the greatest arrival of solar radiation.
For the Ust-Orda station, the average annual temperature is negative and amounts to -0.3º C. The change in the average monthly temperatures in January and July is shown in fig. 6-7.
The coldest month is January. In most parts of the district, the average air temperature in January is approximately -24º C and varies from -22º C to -26º C. The lowest temperatures are observed in lower relief forms, mainly in river valleys and small basins with absolute meters.
Heavy cold air “flows down” here in winter during anticyclonic weather, forming “lakes of cold” and surface inversions.
From three to five days in winter are observed with an average daily air temperature of -30º С to -35º С. and duration of sunshine. But the presence of snow cover in February-March delays the rapid rise in temperature. March throughout the district remains a cold month with significant negative air temperatures. A rapid rise in temperature begins in April with the melting of the snow cover. Despite the fact that, except for the southern part of the district, in its central and northern regions, the average daily air temperatures remain negative, they have small values. For Ust-Orda, the average daily temperatures are -0.4º C. The transition of the average daily temperature through 0º C towards positive values takes place from 12 to 18 April. In May-June, its rapid growth begins. The warmest month is July. The average monthly temperatures in July vary from 14º C to 18º C, and the average daily temperatures reach 25º C. Almost every year in summer, you can expect several days with average daily air temperatures above 30º C, less often they occur at the end of May. The onset of intense heat in summer is associated with the arrival of tropical air. Such periods are fire hazardous and harmful to crops.
Since August, the air temperature begins to slowly drop, and at the end of the month, night frosts are already possible. A sharp drop in temperature occurs in September, and it reaches 7-8º C. However, this month there are many hot days with daily temperatures above 20º C in some years. Until December, the temperature drops intensively by 8-12º C from month to month. The transition of the average daily temperature through 0º C downwards is carried out on October 12-16.
Precipitation. On average, from 250 to 400 mm of precipitation falls annually, of which 78% is liquid precipitation, 16% is solid and 6% is mixed. A noticeable decrease in precipitation occurs from west to east (Fig. 8). This is due to the flow of air masses from the west, northwest and north. And since the East Sayan is stretched from the southeast to the northwest, and the Leno-Angara plateau stretches mainly from the southwest to the northeast, then, passing through the ridges and uplands, successively leaving moisture on each windward slope , in the eastern part of the district comes withered. The huge mass of water Baikal has almost no effect on the moistening of the district due to high ridges. Thus, the eastern part of the territory, which belongs to the Baikal depression within the district, is the most arid. This area of insufficient moisture and belongs to the zone of risky farming.
Snow cover has a significant impact on climate. It delays the increase in air temperature in spring, as a large number of heat is spent on melting it, and not on heating the air. At the same time, it protects the soil from severe cooling and deep freezing, which is very important for a good wintering of plants. In spring, when snow melts, a lot of water is formed, which determines the spring regime of rivers.
The first snow cover appears on October 14. As a rule, it does not stay for the winter and melts under the influence of the warming typical for this month. A stable snow cover appears on November 1-10 and disappears on April 8-11, the date of its complete disappearance is April 27 - May 4. The duration of the snow cover period is 154 days. In mountainous areas and on hills, snow melts much later - at the end of May.
The height of snow cover in the steppe and forest-steppe regions varies between 10-25 cm and in forested areas - 40-60 cm. Deforested open areas very often they are bare, the snow is completely blown off from them, or an insignificant layer remains, which leads to deep freezing of these areas and makes farming difficult.
1.4. Water
The waters of the district are represented by surface waters - rivers, lakes, swamps, a reservoir - groundwater. Their regime and dynamics are determined by a complex combination of natural-climatic and anthropogenic factors.
1.4.1. surface water
Most of the district is characterized by insufficient supply of surface water. In addition, the water of a number of surface sources is characterized by high mineralization and is suitable only for technical purposes.
The average module of surface runoff in the whole district does not exceed 1 l/s s km/² and varies from 0.3-0.7 l/s s km² in the left-bank part of the okrug to 2.9-3.5 l/s s km² . Areas with the highest runoff modulus are in Osinsky and most of the Bayandaevsky districts, with the lowest runoff modulus - in Alar and Nukut.
The annual total runoff, formed within the administrative boundaries of the district, is 1.1 km² per year, i.e. a little more than 0.1% of the transit flow of the river. Hangars (Table 5).
Table 5
Surface runoff volume
AreaArea, thousand square meters km
Average drain module, l / s with sq. km
The volume of surface runoff, cub. km/year
Angarsk
2,7
0,3
0,03
bokhansky
3,7
1,3
0,15
Bayandaevsky
3,8
2,1
0,25
Nukut
2,4
0,5
0,04
Osinsky
4,4
2,9
0,40
Ekhirit-Bulagatsky
5,1
1,5
0,24
District total:
22,1
1,6
1,11
One of the features of the district is the development of karst, which is highly developed in the coastal zone of the Bratsk reservoir, in the basin of the river. Kuda, in the vicinity of the villages of Gakhany, Khara-Nur-Khuta and Nuhe-Nur. The presence of karst is associated with the leakage of part of surface water into karst massifs, which is especially noticeable in the basin of the river. Ides. Due to karst, some areas are deprived of surface watercourses.
Even fairly large permanent streams are lost when crossing karst massifs.
Along with the zones of absorption of surface waters, there are also zones of discharge. The outlets of springs in the basin of the river are connected with the discharge of karst waters. Wasps.
The rivers of the district belong to the basins - the Yenisei and Lena. Watershed along the northeastern tip of the air. Most of the district's surface belongs to the river basin. Yenisei (R. Angara and its tributaries), smaller - to the river basin. Lena.
The river network is poorly developed and uneven (Table 6). It is represented by sections of the river. Angara with its right tributaries Kuda, Ida, Osa and left rivers. Zalari and Ungoy. The Angara carries its waters through the territory of the district for 40 km and about 80 km along its border with the Usolsky and Irkutsk regions.
One of the main rivers of the district, the Kuda, has a fairly extensive network of tributaries (Table 5). Its largest tributary is the Murin.
The density of the river network in the district varies from 0.1 to 1.0 km/km². The maximum is observed in the eastern part of the district - in the interfluve of the river. Murin and Bulga. Minimum - in the left bank of the river. Angara and the Ido-Osinsky interfluve. In the central part of the district, the density of the river network is 0.2-0.3 km/km².
According to the type of water regime and the nature of feeding, the rivers of the district belong to the Sredne-Angara hydrological region of the Irkutsk region. The rivers are fed by mixed water, snow, rain and, to a lesser extent, groundwater. The regime of the rivers of this region is characterized by: spring flood with a rise in the water level from 1 to 4 m; summer rain floods, in some years exceeding the maximum flood; intermittent low water, with a low standing water level up to the drying up of individual rivers in summer and autumn; stable winter low water, sometimes accompanied by complete freezing of rivers.
Table 6
Characteristics of the rivers of the Ekhirit-Bulagat region
Ust-Orda Buryat Okrug
RiverAnnual volume of runoff, million cubic meters m
(observation point)
Angara (pr. tributary of the Yenisei)
763100 (v. Buret)
Zalari (left tributary of the Angara)
15, 5 (n. Novonukutsky)
Unga (left tributary of the Angara)
15.5 (village Semenovsky)
Ida (pr. tributary of the Angara)
103 (v. Morozova)
Where (pr. tributary of the Angara)
56.9 (n. Bozoy)
443 (v. Granoshchina outside the district)
Murin (left tributary of the Kuda)
15.0 (v. Zagatuy)
Obusa (pr. tributary of the Wasp)
101 (village Gorkhon)
Osa (pr. tributary of the Angara)
143 (v. Osa)
Kulenga (left tributary of the Lena)
271 (village of Belousovo outside the district)
Manzurka (left tributary of the Lena)
303 (v. Zueva outside the district)
The high water passes in April-May and lasts 35-40 days. During this period, in areas with an intensive distribution of karst, the runoff is 35-50%, and in the rest - 55-60% of the annual. After the spring rise, the water level drops to the minimum values, until the drying up of small rivers, and is held for 15-20 days before the onset of summer floods associated with rainfall in the second half of summer. 2-3 rain floods come along the rivers with a high water rise of up to 1 m, in rainy years - from 1.5 to 2 m. Summer runoff in rivers is 30-35% of the annual. In autumn, the water level in the rivers steadily and gradually decreases to the minimum values before freezing.
At the end of October the rivers freeze. The ice cover lasts from 160 to 170 days. Its thickness is 0.8-1.5 m. In places where rivers freeze to the bottom, icing forms, which increase the ice thickness to 2 m.
The runoff of suspended sediments is determined by the erosive activity of rivers and anthropogenic factors. Depending on the erosion activity, it varies from the turbidity of the water in the rivers. The average erosion coefficient for the territory of the district is 7.0 t/km² per year, turbidity is from 25 to 50 g/m³. The rivers within the Manzur and Onot uplands, as well as in the upper reaches of the Osa and Obusa, are characterized by low turbidity. Turbidity increases in the middle and lower reaches. The main share of sediments falls on the period of spring floods and rain floods (80-90% of the annual). Turbidity and sediment runoff in low water decreases from the source to the mouth due to the weakening of the erosive activity of the flows and the increase in water flow. During the flood period, an inverse relationship is observed.
Hydrochemical characteristics of rivers. The mineralization of river waters is determined by the climatic conditions of the region, the geological structure of the territory, the type of soil and the characteristics of the vegetation cover. The rivers of the district form the chemical composition in the southern part of the Irkutsk amphitheater among heavily gypsum sedimentary rocks of the Cambrian age under conditions of insufficient moisture. Here, waters of hydrocarbonate and sulfate types are formed, with increased and high mineralization. The sulfate type includes the waters of the river. Ida, Ungi, Kudy, the rest - to hydrocarbonate.
Mineralization of surface waters varies throughout the year. It is lowest during the spring flood and is 100-200 mg/l for most rivers, and 250-300 mg/l for Ida, Osa, Unga, but during the period of floods it can decrease by 1.5-2.0 times. The highest mineralization is observed in the winter low water before the snowmelt, when the rivers are fed mainly by groundwater. During this period, it reaches 1000 mg / l. And it varies within 500-1000 mg/l.
Thus, the waters of the district's rivers can be classified as fresh water with a low degree of mineralization in spring, with an average degree of mineralization in spring. summer period and high in winter.
1.4.2. lakes
In terms of size, most of the lakes of the district have an area of \u200b\u200bless than 1 km². The largest, located in the western part, is Lake. Alyaty. Its length is 4 km, and the maximum width is 0.5 km. Lake Alyaty is flowing. The river flows into it and flows out of it. Alar. The flow of the lake contributes to the rapid exchange of water in it. In total, there are more than 100 lakes within the district. The largest reservoirs are located in the left-bank part of the river basin. Hangars. In the right-bank half of the district, the lakes are much smaller in area, from one to several tens of hectares. For example, in the river basin There are 71 lakes in Kuda, but their total area is only about 2 km².
The lakes of the district belong to three genetic groups: karst, thermokarst and floodplain.
Karst lakes are found in the northwestern part of the district, in the Ekhirit-Bulagatsky and Bayandaevsky districts. The largest karst lake is the lake. Khara-Nur, located on the right bank of the river. Kamenki. The length of the lake is 300 m, the width is 200 m. It has a runoff in the river. Duduy. The water in the lake is low-mineralized, hydrocarbonate class, calcium.
Thermokarst lakes are common in the eastern and northeastern parts of the district. On the bottoms of valleys and ravines, in river valleys. Karst and thermokarst lakes often occur in the same area.
The largest thermokarst lake Nuhe-Nur, located in the middle part of the Zadai-Tologoy valley, fills a depression on the surface of a high terrace. Its length is 60 m, width is 10 m, the prevailing depth is 4-5 m. The total mineralization in the lake is high - 6500 mg / l, the water has a bitter taste, the concentration of sulfates prevails - 4365 mg / l. A group of lakes of thermokarst origin of smaller sizes is concentrated one and a half to two kilometers north of Lake Nukhe-Nur. There are similar lakes in the Kurlunkun Pad, in the region of dd. Idyga, Bahai and Bayandai. They are shallow, 1.0-1.5 meters deep, their length, as a rule, does not exceed 200 m, and their width is 100 m. The banks are heavily swamped, overgrown with sedge and reeds.
There are not many floodplain lakes. They have an elongated shape and are not large in size. A large floodplain lake is Lake. Horde. The area of its water surface is 36.5 hectares. The lake has an elongated pear shape. Two well-defined capes protrude into its middle part. The length of the lake is more than 900 m, the maximum width of the western section is 350 m, the eastern section is 500 m, the maximum depth is 16 m. The coastline is slightly indented, has a length of about 3 km. At the western end, a small bay passes into the bed of the river. Ordushki.
The floodplain lakes should also include oxbow reservoirs formed as a result of meandering of the riverbed.
According to the chemical composition of the rivers, most of the lakes are hydrocarbonate-calcium. According to the level of mineralization, they are fresh, with the amount of salts in the range of 500-800 mg/l. Lakes of karst origin have high mineralization. They have a high content of sulfates and magnesium.
Within the district, there are several dozen ponds. Many of the previously existing ponds have now been eliminated. Only in the river basin Where there were about a hundred of them.
Considering that water resources for economic and domestic water supply are very limited, an increase in the degree of their use can be ensured only by regulating the flow by restoring destroyed ponds. Being the main regulators of runoff, they gain enough water near their water areas. high level groundwater.
1.4.3. The groundwater
According to the hydrogeological feature, the territory of the district belongs to the East Siberian artesian region, which occupies a huge space from the Taimyr Peninsula in the north to Baikal in the south, and is completely located within the even larger Angara-Lena artesian basin.
In a vertical section, groundwater can be subdivided into two hydrogeochemical zones or two floors. The upper floor occupies the uppermost part of geological formations and is distinguished by the fact that its waters have close water exchange with atmospheric precipitation and surface waters of rivers and lakes. Here, mainly oxygen-nitrogen and nitrogen waters of atmospheric nutrition are developed. In the areas of permafrost development, suprapermafrost hydrocarbonate waters belong to this stage. The thickness, thickness or depth of the waters of this floor is 200 m within the district.
The waters of the lower floor have no connection with the day surface and do not participate in the modern circulation of natural waters. They have a sedimentogenic, less often ancient infiltration origin. In this regard, the mineralization and chemical composition of these waters largely reflect the composition and mineralization of the waters of the ancient seas, in which the accumulation of water-bearing rocks took place.
The suprapermafrost hydrocarbonate waters of the upper floor have a mineralization of up to 0.5-1.0 g/kg, and in areas with a shallow occurrence of halogen formations up to 3-10 and even 50-100 g/kg. fresh water here bicarbonate calcium or slightly salty with a mineralization of up to 10 g / kg, sulfate calcium, chloride-sulfate sodium-calcium, sulfate-chloride calcium-sodium. There are also strongly saline waters with a salinity of more than 35 g/kg.
The waters of the lower level are mainly methane, nitrogen-methane, less often nitrogen thermal and cold reservoir waters. According to the degree of mineralization, among these waters there are very strong (up to 350 g / kg) and even super-hard (up to 410-420 g / kg) brines with oil-type methane gases, hydrogen sulfide, potassium, strontium.
The temperature of the district's groundwater near the surface of the platform foundation will change from 10 to 40ºС, i.e. it falls into the zone of cold, warm and slightly hot waters.
The waters of the upper level have rather significant dynamic resources and provide the flow of rivers in winter time. So, for example, the consumption of r. Hangars due to underground power in the winter low water is 550-600 m³ / s.
At the first drilling works (slightly to the north of Novonukutsky village) up to 200 m, underground waters of the upper hydrogeochemical stage are encountered, represented initially by fresh hydrocarbonate waters with a mineralization of up to 0.5 g/kg. Then, closer to the mark of 200 m, they are replaced by salty (1-3 g/kg) sulfate-calcium and sulfate-chloride calcium-sodium. We can assume such mineralization due to the widely developed Middle Cambrian variegated sulfate rocks.
At the interval of 200-680 m of this hypothetical drilling, one can find groundwater of the second or lower hydrogeochemical level, represented first by saline sodium chloride (1-35 g/kg) waters, and then by brines (35-140 g/kg). Such mineralization and composition of the waters are most probable, since at the beginning of the interval the host rocks will be limestones, dolomites, anhydrites and gypsum, and towards the end of the interval there will be layers of Early Cambrian rock salt.
Under the pressure of the overlying layers, groundwater can rise quite high from the places of formation, not only in wells, but also in zones weakened by faults. In this way, for example, daytime deep brines are reached in the form of open or hidden discharge centers emerging at the bottom of rivers and lakes. But most often they do not rise to the surface of the earth, but form underground lakes and hidden sources of unloading. The latter greatly complicate the extraction of fresh groundwater for domestic and drinking water supply and significantly worsen the geoecological situation.
Subaerial and especially hidden centers of brine discharge on the territory of the district are widespread in the Alar, Nukut, Osinsky and Bokhan regions, in the valleys of the river. Ungi, Osa and on the coast of the Bratsk reservoir (near the village of Khadakhan).
In the river valley Kamenki, 18 km northwest of Bayandai sinkholes 18 m deep and up to 200 m wide, there is a lake in which brines are unloaded, which is why the mineralization of water at a depth of 2-3 meters reaches 190 g/l.
At the interval of 680-1940 meters, a well will have to be drilled in completely saline and carbonate rocks, in connection with this, one will certainly have to deal with calcium chloride brines with a mineralization of 140-350 g / kg, and closer to the end of the interval with brines with a mineralization of 270 meters even more 350 g/kg. In the drilling interval 1940-2660 meters, i.e. Before the foundation of the platform, there will be some decrease in the salinity of brines to 270-350 g/kg and a change in the chemical composition of waters to calcium-sodium chloride.
Then there will be very strong metamorphic crystalline rocks of the basement of the platform, containing only fissure and fissure-vein waters in fault zones, which in composition and mineralization value correspond to the more common brines, possibly of juvenile origin.
1.5. Soils
The soil cover of the region is well studied. Soddy-forest brown soils are widespread along the slopes and watersheds. They lie under pine forests on the destruction products of Jurassic rocks and make up about 15% of the district. The humus horizon with a thickness of 20 cm contains 3-8% humus, the pH is slightly acidic, and the mechanical composition is sandy loam.
Let us present the profile and chemical composition of humus-calcareous soils of the Ekhirit-Bulagatsky region (Table 7).
Table 7
Chemical composition humus-calcareous soils
Power,cm
Humus,
Nitrogen
Movement
phosphorus
pH
Calcium
Sodium
Ekhirit-
Bulagat-
sky
0-18
6,0
0,404
7,0
36,31
1,93
20-32
4,06
0,234
7,0
28,81
40-60
1,93
7,2
24,28
Humus-calcareous gray and brown soils have the following morphological structure:Ekhirit-Bulagatsky district, Kuda river, slope with birch forest .
A0 - absent.
A 0-18 cm. Dark brown, up to 3 cm dusty, and below a clearly expressed granular structure. Medium loamy, with a significant content of the skeleton. The transition to the next horizon is gradual.
At 18-35 cm Brown, silty-granular structure with a significant content of the skeleton.
C 35-78 cm. Light brown with a whitish tint due to the high content of lime. Almost structureless, very loose, strongly skeletal. From 78 cm, crushed stone from lime-clay rock follows. The soil boils up from a depth of 15 cm.
Soddy-calcareous soils occupy about 30% of the territory of the district, located on different elements of the relief under forest and meadow-steppe vegetation. There are subtypes brown (on red-colored loams) and gray (on weathering products of limestones and dolomites). Soil profile up to 80-100. Humus horizon 15-20 cm, humus in the layer 0-5 cm up to 14%. Carbonates in leached soils occur at a depth of 50 cm, in typical soils they occur close to the surface, pH is neutral or slightly alkaline. The mechanical composition is heavy loams.
Gray forest soils with signs of podzolization formed on the deluvium of Jurassic sandstones. Distributed on the left bank of the river. Angara in the Ida-Kudinsky interfluve, makes up 10% of the district. These are loamy and sandy loamy soils with a humus horizon of 5 to 30 cm and a humus content of 2 to 5%, and in dark gray up to 10%. On carbonate-free deposits, the pH is acidic; on carbonates in the lower part of the profile, it is alkaline. Phytocenosis of gray forest soils.
Podzolic soils (1% of the territory of the district) are found in separate patches on watersheds and ancient terraces under light coniferous and moss forests. The thickness of the podzolic horizon is 7-15 cm, the humus horizon is 5-15 cm, humus content is 1-4%, and the pH is acidic.
IN soil cover In the okrug, a significant role (up to 10%) is played by medium-thick and thin medium-humus chernozems. They develop on a carbonate basis and have a lumpy-silty structure. They are located on the surface of terraces and in valleys gently sloping under steppe and meadow-steppe vegetation. Soil-forming rocks are loess-like and heavy loams. On steeper slopes, they are replaced by low-humus and thin washed-out gravelly chernozems. In the river valley Kuda on elevated areas there are chernozem-like solonetsous low-humus soils.
In the lower parts of the valleys, the soils are chernozem-like, slightly solonetzic. Among the chernozems, solonetsous make up 75%, leached - 20% and carbonate - 5%. In accordance with the subtypes, the thickness of the humus horizon changes - 40-30-20 cm, the depth of carbonates - 70-10-0 cm. %; The pH of carbonate-free horizons is slightly acidic, while that of carbonate horizons is slightly alkaline. The mechanical composition is medium and heavy loams. Profile of the chernozem soil located on the meadow terrace of the river. Murin on an iron meadow, given in the book of I. V. Nikolaev "Soils of the Irkutsk region", is as follows:
A0 0-5 cm. Dark brown. The granular-silty structure is weakly expressed.
A2 5-35 cm. Dark in color, loamy, lumpy-powdery. The transition is gradual.
В1 39-69 cm. Brown, with dark spots, lumpy-powdery, medium loam. The transition is gradual.
B2 72 cm and below. Reddish brown with dark streaks. Light loam. Grey. Boils up from 35 cm.
Within the Lena-Angara steppe, leached and solonetsous chernozems are located. They are strictly confined to the middle and partly to the lower parts of the watersheds. The soil-forming rocks of chernozems are loess-like loams and sandy loams.
Carbonate chernozems have a humus horizon thickness of 20-35 cm. The color of horizon A is brownish-gray or grayish-brown. The structure is finely lumpy, the addition is loose. Carbonates rise to the surface. At a depth of 5-10 cm from the surface, pseudomycelium appears. Under horizons A there is a thin layer of loess-like loam ranging in size from 20-40 cm.
Alkaline chernozems for the described territory are a fairly common subtype. The thickness of their humus horizon, as a rule, does not exceed 30 cm. The color of the rocks of the horizon is brownish-gray or grayish-brown. The structure is lumpy, turning into a columnar. The uppermost layer of horizon A, 3–5 cm thick, is pulverized and structureless, while the rest of it is compacted; carbonates in the humus horizon are most often found at a depth of about 10 cm from the surface. This type of chernozem belongs to alkaline, deep effervescent.
On the territory of the district, about 12% of the total area falls on meadow-chernozem soils. They are located along the bottoms of dry hollows, low parts of slopes and microrelief depressions on ancient terraces. On these soils, an increased amount of moisture accumulates due to its inflow from higher surfaces and due to the presence of long-term seasonal permafrost, which persists much longer than on positive relief elements.
Meadow-chernozem soils are formed under grass-forb steppe meadows and sparse birch forests with a lush grass cover. A large mass of herbaceous vegetation in harsh climatic conditions does not have time to completely decompose. Therefore, meadow-chernozem soils are characterized by a large thickness of the humus horizon - on average up to 0.6-1.0 meters or more. The humus content is 9-15%, often 20% or more, the pH of the upper horizons is slightly acidic and neutral.
Below is a description of the meadow-chernozem soils on the river. Kuluta Ekhirit-Bulagatsky district.
A0 0-60 cm. Intensely dark in color, friable, completely structureless to a depth of 35 cm, finely lumpy fragile particles are mixed with it below. The transition of horizons is gradual.
At 60-120 cm. The color is variegated. Humus patches alternate with those of the parent rock. Fragile lumpy structure.
C from 120 cm and below, carbonate loam. Boils from 75-80 cm.
The negative relief elements are characterized by swampy silt-gley, humus-peaty soils. Peat thickness up to 30 cm.
The most valuable in agriculture are chernozems, sulfuric forest and sod-calcareous brown soils. Their natural fertility is reduced as a result of long-term economic use, violation of agrotechnical methods of tillage, light mechanical composition of chernozems and gray forest soils, lack of moisture, which can be compensated by reclamation methods. Soddy-calcareous loamy soils are subject to water erosion.
The plowing of forests in some areas, where up to 60% of the area has been developed, has led to a change in the potential fertility of soils and deterioration in land quality.
1.6. Vegetation
The vegetation of the region is rich and varied. At present, it has been quite fully studied thanks to the work of many Siberian botanists (Novokonov, 1984; Popov, 1957, 1957,1959; Frolova, 1960,1979; Peshkova, 1972.1985; Malyshev, Peshkova, 1984)
The flora of the region is rich and varied and includes about 800 plant species, 366 genera, 84 families from divisions: angiosperms, gymnosperms, ferns, lycopsids and horsetails. In addition to them, there are many dozens of species from the moss and lichen divisions. In the vegetation cover of the district, plants of different divisions play a different role. For example, the species diversity of gymnosperms is small, only 7 species, but their family representatives form coniferous taiga in the vast territories of the district. The vast majority of species, about 770, are flowering plants. They dominate almost all phytocenoses. The most floristically rich among them are the well-known families: aster (composite) - 98 species, bluegrass (cereal) - 75, sedge - 56, ranunculus - 40, cabbage (cruciferous) - 35, clove - 29, lily - 22, buckwheat and umbrella - 21 species. Of the other families, a significant role is played by burrows - 20, lambaceae - 18, haze (swan) - 17, willow and orchids - 16 species each, borage - 14, violets - 13, primroses - 11, saxifrage - 10 species. The listed 20 families of flowering plants account for 79% of the flora of the district, excluding mosses and lichens. (Fig. 10).
Rice. 10. Vegetation cover[ 5 ]
Plants that prefer to live in dry places - xerophytes, there are 384 species in the district. There are 240 species in the forests, mostly mesophytes. In meadows and swamps, under conditions of sufficient or excessive moisture, 295 species grow, belonging to mesophytes and hygromesophytes. There are only 32 species of water-coastal hydrophytes and hygrophytes, 90 weed-ruderal and roadside species.
The flora of the district includes many useful plants: food, fodder, medicinal, technical, melliferous, etc..
Food wild plants are quite common. Over 100 species of edible plants can be named in the flora of the district. In terms of their nutritional value and taste, they are not inferior to cultural ones. Unfortunately, in Siberia, not all of them are used for food. For a long time, berry plants have been of the greatest interest: currants, raspberries, lingonberries, blueberries, blueberries, honeysuckle, strawberries and wild strawberries, as well as bird cherry. Their tasty and healthy fruits are consumed fresh or they are used to make jams, jams, fruit drinks, vitamin drinks and juices.
Of great nutritional importance are species from the families of buckwheat, lily, cereals, umbrella, cruciferous, Asteraceae, etc. You can cook various dishes from wild plants: soups, cereals, salads, drinks, and even bake bread. The most protein-rich nettle, sorrel, quinoa; the rhizomes of many aquatic and coastal plants are distinguished by a high content of starch, and the rhizomes of bracken fern contain up to 40-46% starch, birch sap is rich in sugars. Enough in the district and high-vitamin salad greens: these are wild onions and garlic, dandelion, shepherd's purse, large plantain, medium chickweed and midges, etc.
When collecting food plants, remember that they will benefit if they are collected in environmentally friendly places, away from major highways and factories.
Certain conditions must be observed when collecting medicinal plants, which are also rich in the flora of the district. About 300 plant species can be used to treat various ailments.
Medicines grow in the forest, in the field and even on the roads. With colds and coughs, diaphoretic syrups from raspberries, lingonberries, as well as flowering heads of red clover, licorice roots or infusions of thyme, cumin, and pine buds help well.
Forage wild plants are bread for animals. There are more than 200 species of them in the hayfields and pastures of the district. Cereals and legumes have the highest lumpy qualities as a source of valuable proteins and carbohydrates. Among legumes, these are clover, alfalfa, sweet clover, chin, peas - vetch, sainfoin; among the cereals - bluegrass, couch grass, rump, barley, foxtail, timothy grass, feather grass, vostrets, fescue, thin-legged, etc. Animals love to feast on odorous and bitter, as well as salty and sour herbs, which improve appetite, help to cure the disease. Of these herbs, dandelion, wormwood, yarrow, sorrel, quinoa, saltwort are known.
Almost all insect-pollinated plants are melliferous. The sources of honey are nectar and pollen. In beekeeping, legumes are most valued (cleves, alfalfa, sweet clover, sainfoin), many rosaceae (rose hips, cinquefoil, meadowsweet), various umbellate, buckwheat, labiate, boletus plants and, of course, Ivan tea, which grows in abundance along forest clearings and along roads.
There are many other useful plants in the flora of the district, for example, technical plants that provide construction (coniferous plants) and ornamental material (baskets are woven from willow branches, brushes for whitewashing walls are knitted from feather grass and sedge leaves). There are also essential oil plants - sources of aromatic substances for perfumery and medicine. These are calamus, or calamus root, thyme, mint, valerian, wild rosemary, etc. Tannins necessary for special processing of animal skins, giving them elasticity and water resistance, can be obtained from the bark of spruce, larch, and various types of willow.
Of the plants that bring harm to humans, weeds and poisonous herbs should be noted. Three groups are distinguished among them: weedy, ruderal and roadside. Weeds in fields and gardens significantly reduce the yield of cultivated plants. They successfully compete with them, carry away a lot of nutrients, moisture, and intercept light. The greatest harm is caused by rhizomatous and rhizomatous weeds, which intensively reproduce vegetatively. Most often among them there are: creeping couch grass, field horsetail, field sow thistle, etc.
Ruderal, or wasteland plants grow in wastelands near fences, on garbage and manure heaps, that is, on soils enriched with organic matter. They usually have tall, erect stems and large, often spiny leaves. These are gray motherwort, descuria, rezuha, thistle, wormwood and paniculata.
Roadside plants have their adaptations. Their stems are not tall, recumbent, the leaves are small, and the large ones form basal rosettes. The veins in the leaves are very strong. Most often among them there are plantain, dandelion, creeping clover, knotweed or bird buckwheat, discoid chamomile.
The vegetation cover of the Ekhirit-Bulagatsky district is represented by a complex combination of steppes, meadows, swamps and bushes.
Steppe tin of vegetation. Steppe vegetation, as a rule, does not stretch in wide strips (2-10 km) along the river. Angara, Wasp, Ida, Ungi, Kuda and their tributaries. Steppes occupy an insignificant area compared to forests. Distributed in elevated areas of floodplain and above-floodplain terraces and adjacent mountain slopes. The latter have different steepness and carry the most diverse steppe vegetation, and the highly dissected relief allows the existence of a number of steppe groups with different ecologies. According to G. A. Peshkova (1969), 5 subtypes of steppes can be distinguished in the Angara region: meadow, real, saz, desert and mountain.
Meadow steppes are located on gentle slopes and lower floodplain terraces on the most fertile, powerful humus horizons of chernozems. Of these, vostrets steppes from vostrets or branched lemus are most often found. Grasses form the basis of the herbage of the meadow steppes: branched yoster, bluegrass drawn, thin-legged comb, wheatgrass comb. Of the legumes, there is quite a lot of sickle-shaped alfalfa, and of other herbs - goat-leaved volodushka, substituting wormwood, fragrant onions, stemless cinquefoil and strawberries. Here, but along the higher crests of the terraces above the floodplains and along the slopes with light sandy soils, thin-legged-fescue steppes spread. Dominant in them are fescue, or Valisian fescue, or fine-legged comb. The herbage is rich in hardish sedge, Siberian thyme (thyme), white-tomented speedwell, stemless cinquefoil. The set of these herbs indicates a state of severe disruption of vegetation under the influence of grazing.
Cirrus-feather grass meadow steppes are also characterized by a variety of species composition and lush herbage. Of the cereals, besides the feather grass, bluegrass drawn, awnless rump, fluffy sheep, steppe timothy are common here. In the forbs, along with steppe grasses (tuberous sage, real bedstraw, sandy sainfoin, small red-headed lily, dwarf lily), meadow-forest and forest cannon species are often found (lupine clover, Siberian adonis, bearded wrestler, fragrant kupena, long-haired anemone). Strawberry clumps and clearings are also characteristic, sometimes separated into independent associations.
Of the real ones, there are often tyrsovye with hair-like feather grass, wheatgrass and serpentine steppes. They are distributed along the southern slopes of ridges and high terraces with leached sandy loamy chernozems. Tyrs steppes form a large number of associations, which is explained by the ability of feather grass to grow on soils that are diverse in chemical and mechanical composition. The bulk of the herbage is formed by a large number of associations, which is explained by the ability of feather grass to grow on soils that are diverse in chemical and mechanical composition. The bulk of the herbage is formed by grasses: hairy feather grass, Lena fescue, combed fescue, combed wheatgrass. The forbs are also rich in floristic terms. Here are cold wormwood, alpine aster, pale yellow scabiosa, forked cinquefoil, Angarsk astragalus, common edelweiss and other species. The species composition varies depending on the microrelief. In the depressions, the herbage is distinguished by great density and lush development, an abundance of meadow species.
Both meadow and real steppes have been plowed up due to the fact that they are confined to more or less leveled flat areas with relatively fertile soils.
Saz steppes are common in meadow solonchaks on the first floodplain terraces of many rivers, and especially the rivers. Zalari, Ungi, Kudy. The highest parts of these terraces are occupied by Chinese oyster mushroom, on slight depressions - by Pabo oyster mushroom, and closer to the terraces they give way to thickets of brilliant chia. Depending on the predominance of one or another cereal, formations of vostrets and chiev steppes are distinguished. These grasses are usually accompanied by halophytic herbs: thin-colored sagebrush, lanceolate thermopsis, Siberian mountaineer, creeping cochia, Russian and solonchak slider, Kornut's plantain, Gmelin's kermek, cold wormwood, nitrate wormwood.
The subtype of desert steppes includes the wormwood nitrate formation, which also occurs in the same way as the saz steppes on the first floodplain terraces of the river. Unga, Kuda and other tributaries of the Angara. The edificator of these steppes, wormwood nitrate, is accompanied by the same plants as in the saz steppes, but much more often here in microdepressions there are associations of saltwort, soleros european, hornbearing swede, tripolium vulgaris, tellungiella solonets, seaside milkweed.
From the mountain steppes, fescue from the Lena fescue are noted, and along flat terraces on soils with a thin humus horizon and a light mechanical composition, bluegrass steppes from bluegrass racemose and attenuated. Very often, sometimes on large areas, there are three formations similar in floristic composition: cold wormwood, stemless lapchak and thyme. These steppes develop along steep southern slopes, as well as on stony-gravelly soils in flat places. These plants tend to endure strong trampling. On overgrazed pastures, around watering places, they begin to dominate in place of feather grass, raptor or fine-legged steppes.
Steppes in combination with aspen and birch, less often pine mixed-grass-steppe forests, create a peculiar appearance of the Angara forest-steppe.
Meadow and swamp type of vegetation. Meadows develop along the bottoms of river valleys. Depending on the moisture conditions, real, steppe, swampy and peaty meadows are distinguished.
Real meadows in the treeless part of the district grow on meadow-chernozem and soddy-meadow soils along elevated sections of river valleys. Their herbage is heterogeneous. The cereal base is created by creeping couch grass, meadow bluegrass, meadow fescue, awnless brome, giant bent grass, meadow foxtail. The herbage is dominated by cumin, common and Buryat, medicinal burnet, red clover, meadow rank, yarrow, meadow geranium, and many types of buttercup. Downstream in the river valleys, the salinity of soddy-meadow soils increases. The first witnesses to the appearance of easily soluble salts in the soil are usually two cereals: short-awned barley and cane foxtail. These meadows represent a halophytic variant of true large-grass plants. They are used as grasslands. Their herbage is magnificently developed, the projective cover is 100%, the height is 50-60 cm. In addition to grasses, various herbs are constantly found. In areas used for grazing, goose cinquefoil, saline slider, sow thistle stemless, veinless sedge, furrowed astragalus, bitter Saussurea, Siberian mountaineer, sea sorrel, seaside triostrennik appear. The herbage becomes sparse, and the exposed soil areas are covered with field crusts.
Steppe meadows are developed on less humid slopes and terraces. They have a smaller projective cover, up to 70-80%, and other dominants appear in the herbage. Of the cereals, these are bluegrass narrow-leaved and steppe timothy; from legumes - alfalfa, sweet clover, pleasant peas. Excessively moist marshy meadows on meadow-marsh soils are formed by sedge, reed, beckmania formations. On peaty meadows on pre-purulent-peaty-gley soils on permafrost, purple reed grass, soddy pike, soddy sedge, and cottongrass dominate. These are, as a rule, tussocked unproductive meadows.
All meadows are fodder lands. With agronomically correct use, they can be highly efficient hayfields and pastures.
Wetlands occupy a small part of the county. Together with meadows, they form complexes in extended river valleys and belong to the lowland type. Bogs are more often fed by supra-permafrost perched waters, less often by groundwater. The soils are meadow-boggy, saline to varying degrees, as well as soddy-meadow permafrost soils with well-pronounced gleying in the lower supra-permafrost part. These are grass and moss-grass, shrub and tree-shrub swamps. In forested areas, moss swamps overgrown with birch, spruce and larch are common. Hypnum mosses grow on the hummocks of such swamps, and cuckoo flax and sphagnum grow in depressions between hummocks. Marsh wild rosemary, blueberries, cloudberries, as well as marsh horsetail, various types of sedges grow singly. Among other plants, there are bog hamedafne, narrow-leaved cotton grass. In steppe areas, saline lowland bogs are common, in which herbs play a significant role: marigold marigold, three-leafed watch, marsh cinquefoil, marsh triostrennik, solonchak mustard. This type of vegetation is partly used for haymaking, after reclamation it is involved in agricultural production. Bogs in the upper reaches of the rivers are of exceptionally important water protection and water regulation importance.
7. Animal world
The fauna of the Ekhirit-Bulagat region is rich. Of the 100 species of mammals living in the south of Eastern Siberia, more than 50 are represented here. Of the 274 species of birds living in the Irkutsk region, up to 70% of the total species composition is found in the district.
The taiga complex of the district belongs to the southern taiga faunistic complex of the Irkutsk region. It occupies a fairly large area. Of the birds here, the most characteristic are representatives of the order Galliformes, which remain to winter in the taiga, and therefore are well adapted to the harsh conditions of the cold season. Chickens lead a terrestrial lifestyle, food - earrings, buds, shoots, needles - is obtained mainly from trees.
The largest representative of this order is the common capercaillie. Male weight 3-5, 6 kg. In late March - early April, capercaillie begin to visit traditional places of mating. They walk in the snow and pick each other up. The males sing in the evening, at first in the trees, and after the morning dawn they descend to the ground, where capercaillie fly up to them. Capercaillie chicks are born after 26 days and grow rapidly. After 10 days, they can fly up into trees. The composition of the food of these birds changes with age and season. Chicks feed on insects, then they eat flowers, and at the end of summer - berries, seeds, green parts of plants. In winter, capercaillie feed on pine nuts and pine needles. Quite numerous from the order of chicken - hazel grouse, less common black grouse. Chickens are hunted mainly by shooting from a gun, in the fall they hunt with a husky, and in the spring they get it on a current. Summer brood hunting is prohibited.
Of the other birds of the taiga zone, the black woodpecker is widespread, and a large number of passerines: waxwing, bluetail, flycatcher, nightingale, as well as remaining for the winter siskin, tap dance, bullfinch, schur, crossbill, nutcracker, jay, kuksha, pika, tits; from the detachment of owls - a bearded owl. Some birds stock up for the winter.
The black stork is found in dense high-stemmed forests. This rare species is listed in the Red Book of the Irkutsk region and Russia.
Mammals in the process of evolution have developed a number of adaptations for existence in the taiga zone - these are wider paws for moving through the snow, a more fluffy tail, and sometimes a change in color to match the color of the snow. From the detachment of animals, a bear lives here, which is an omnivore and hibernates for the winter, a Siberian weasel characterized by reddish snow. The lynx is a typical inhabitant of the taiga; it feeds on forest birds, rodents, and hares. Hunts at dusk. In size, it reaches 1 m in length with a small weight of 8 - 15 kg. Usually in the taiga, the weasel is the smallest predator, the ermine, the wolverine, which is called the hyena of the north, is less common, since it eats carrion but can hunt rodents and birds.
From the detachment of rodents in the taiga, usually: squirrel, flying squirrel, chipmunk and voles.
Of the artiodactyls, the elk is the most adapted to life in the taiga. He easily walks through the swamps, can swim. The elk feeds on various plants, in winter it eats the shoots of young pine, aspen, willow, with a light frost it gnaws at the bark of trees. Often this has a negative effect on forest vegetation, often the trees dry up and die. Moose can be attacked by wolves sometimes by bears, young animals and calves are especially affected. Snowy winters have a detrimental effect on the number of elks. The meat of the animal has a good taste, its skin is very tasty. Of the other ungulates on the territory of the district, there is a deer - a subspecies of the red deer.
This complex is the most favorable for animals, as it includes a multi-tiered deciduous forest, shrubs and grasses are not uncommon. The most characteristic birds of this complex are the Greater and Lesser Spotted Woodpeckers, the White-tailed Woodpecker; goshawk, sparrowhawk, black kite, buzzard; hawk and long-eared owls; forest pipit, shrike, several species of thrushes, warblers, crickets, tits, buntings - common, red, dubrovnik, etc. Some birds of deciduous forests remain wintering, for example, goldfinch, crow, magpie, etc. Rare, listed in the Red Book of the Irkutsk region , are the blue magpie (recorded on the Kude River near the village of Kapsal; currently, its range is expanding; it settles in floodplain forests, along river banks, leads a nomadic lifestyle. Nests on willow, bird cherry at a height of 1.5 m); mistletoe - a large thrush. Recorded in Nukut and Ekhirit-Bulagat regions (Bakhtai and Kudareyka villages).
A viviparous lizard lives in this zone, preferring wet places.
Of the amphibians on the territory of this complex, there are moored frog, which is less demanding on humidity than the Siberian frog and winters on land.
Mammals of the taiga zone can also be observed in the forest-steppe zone. Of the order of artiodactyls, the roe deer is the most typical, which prefers mixed forests with well-developed undergrowth and grass cover. In winter, roe deer feed throughout the day. In summer it feeds on grass, leaves, thin shoots of trees and shrubs, in winter - on twigs, digs grass and lichens from under the snow. Many animals die from starvation and epizootics. In many places, the roe deer is under protection. To increase its numbers, it is necessary to organize winter feeding and fight against predators.
Animals and birds intensively affect the forest litter and soil. Many of them vigorously rummage through the litter, looking for food. The forest litter is permeated with whole labyrinths of surface passages of moles, voles, shrews, which also contributes to its aeration and decomposition.
A significant part of animals and birds feed on other animals, exterminating a large number of forest pests. Insectivorous birds are the orderlies of the forest. The most useful birds that live all year round are tits, pikas, nuthatches and woodpeckers, which destroy insects at all stages of development. Along with birds, insects and mammals are destroyed: shrew, mole, bats, mouse-like rodents and badger. They eat the larvae of May beetles and leafworms.
Many forest birds and animals forage not only in the forest, but also outside it: in the fields and meadows.
These are the enemies of such dangerous pests of cultivated plants as wireworm, beet weevil, etc.
Forest birds of prey, owls and corvids systematically prey on field rodents. Pigeons, buntings and other granivorous birds destroy weed seeds, and by collecting grains of cultivated plants in the fields, they reduce the food supply of harmful mouse-like rodents. At the same time, some forest birds and animals become agricultural pests.
Some species of forest birds and animals spread various diseases, including those dangerous to humans and domestic animals. The encephalitis virus is transmitted to people by ticks, whose owners at certain stages of development are chipmunks, hares, squirrels, wolves, hazel grouses, forest horses, etc. Predatory animals, partly rats and mice, can be carriers of the rabies virus.
The forest-steppe complex is represented by predatory animals - the wolf and the fox, the light-colored polecat and the badger; from the order of ungulates - roe deer; from the order of insectivores - Siberian mole and shrew. Of these, the light polecat, listed in the Red Book of the Irkutsk region, is rare. It is marked along the river valley. Where. The ferret feeds on mouse-like rodents and ground squirrels.
Rare birds of the forest-steppe complex, listed in the Red Book of the Irkutsk region, are the small sparrowhawk; saker falcon - a large falcon with relatively wide wings; Asian snipe godwit.
There are few shelters in this zone, so the birds here, some of the birds of prey are confined to the steppes: red-footed falcon, field harrier, imperial eagle, steppe eagle. There are much more species from the order of passerines: skylark, steppe pipit, black-headed coinage, field sparrow, etc. Almost all steppe birds run well and have a protective color. In winter, most of them leave the steppe due to lack of food. Very rare, listed in the Red Book of the Irkutsk region and the USSR, is the demoiselle crane - the smallest of the cranes, living in fescue-feather grass and wormwood-cereal steppes with sparse herbage. IN last years demoiselle crane nesting on farmland was noted. It feeds on seeds and sprouts of plants, insects, lizards and small rodents. Recorded on migration in Ekhirit-Bulagatsky region, in the vicinity of the village. Kudareyka, Ust-Ordynsky, Elovka, Krasny Yar. In the summer it was seen in the Bayandaevsky district.
In the steppe and forest-steppe zones, there is an ordinary or nimble lizard listed in the Red Book of the Irkutsk region. The viper lives in the steppe, sometimes in the forest-steppe zone. It is a slow and phlegmatic snake. Its main food is voles, less often small birds.
The mammals of the steppe zone mostly belong to the order of rodents. This is a long-tailed ground squirrel, marmot tarbagan and field mouse, which has become rare and is listed in the Red Book of the Irkutsk region.
A rare species listed in the Red Book of the Irkutsk region is the shelduck, a red duck that nests in hilly steppes in the presence of open water bodies. Once upon a time bustards were found in the Ekhirit-Bulagat steppes. Now this species from the Red Book of the Irkutsk region and the RSFSR is extremely rare.
The fauna of the natural complexes of bolts and reservoirs is relatively diverse. For the marsh, the coot, the shepherd, and the lapwing are more characteristic. The common crane is rare. It is noted in the swampy areas of the river basin. Where. Of the birds of prey, it is found here: the marsh harrier, from the detachment of owls - the marsh owl, etc.
Mammals settle near the reservoir: water shrew, water rat.
Reservoirs and river floodplains can be foci of tularemia. In the transmission of infection, near-aquatic animals, as well as the pasyuk rat, living near humans, play a paramount role.
- The essence of the dispute: Other lawsuits
Claims Khabituyeva E.P. partially satisfy. recover in favor of Habitueva E.P. from the Ministry of Finance of the Russian Federation at the expense of the Treasury of the Russian Federation, the lost old-age pension in the amount of<данные изъяты>rub. The lawsuit against the Office of the Pension Fund of the Russian Federation in the Ust-Orda Buryat District, FKU OIK-1 of the GUFSIN of Russia for the Irkutsk region, the GUFSIN of Russia for the Irkutsk region is denied. Refuse to satisfy the claim Khabituyeva E.P. claiming compensation for moral damages...
- The essence of the dispute: Disputes related to the inheritance of property
Satisfy the claim of Kondratyev Boris Nikolaevich. Establish the fact of belonging to M, DD.MM.YYYY of the year of birth, certificate of ownership of land series No. issued by DD.MM.YYYY Komzem of the Ekhirit-Bulagat district in which the person in whose name the certificate was issued is indicated M, DD.MM .YYYY year of birth, No. (passport data). Establish the fact that Kondratiev Boris Nikolaevich accepted the inheritance that opened after the death of mother M, DD.MM.YYYY.b., who died DD.MM ...
151.
Decision of September 5, 2013 in case No. 12-50/2013
Decision of the justice of the peace of the court district No. 134 of the Ekhirit-Bulagatsky district dated *** on the recognition of R. M. Sabirov guilty of committing an administrative offense under Art. 12.8 part 1 of the Code of Administrative Offenses and sentencing in the form of deprivation of the right to drive vehicles for a period of 1 year 6 months - leave unchanged, the complaint of Sabirov R. M. - without satisfaction. This decision takes effect immediately. Judge Asaeva L. A....
152.
Judgment dated September 4, 2013
Satisfy the claims of the acting prosecutor of the Ekhirit-Bulagat district. To oblige the individual entrepreneur Alexander Dmitrievich Berdanosov to carry out certification of workplaces in terms of working conditions, followed by certification of the organization of work on labor protection, to provide conditions for employees to undergo medical examinations. The court decision can be appealed to the Irkutsk Regional Court within a month from the date of the final decision. .
153.
Judgment dated September 4, 2013
The essence of the dispute: Disputes related to transactions with private houses and privatized apartments
To satisfy the claims of Andreeva Victoria Viktorovna and Andreev Alexander Viktorovich. Contract for the sale of an apartment and a land plot located at<адрес>from DD.MM.YYYY, concluded between Andreeva Victoria Viktorovna, Andreev Alexander Viktorovich on the one hand and Chebotnyagina Olga Petrovna, acting for herself and in the interests of minor children A, G, M and R on the other hand, terminate ...
154.
Judgment dated September 4, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
Satisfy the claim of Mikhailova Lidia Abokshinovna. Establish the fact of acceptance by Mikhailova Lidia Abokshinovna, born DD.MM.YYYY, born<адрес>, an inheritance opened after the death of her father O, who died DD.MM.YYYY, in the form of a land share with an area<данные изъяты>ha. To recognize Mikhailova Lidia Abokshinovna, DD.MM.YYYY, the right of ownership to the land share with an area of<данные изъяты>ha...
155.
Judgment dated September 3, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Disputes related to the inheritance of property
Satisfy the claims of Mazko Vladimir Stepanovich for the restoration of the term for accepting the inheritance, establishing the fact of accepting the inheritance. To restore Mazko Vladimir Stepanovich the deadline for accepting the inheritance in the form of an apartment with a total area<данные изъяты>sq.m, located at<адрес>, the lost pension for December 2012, left after the death of M, who died DD.MM.YYYY ...
156.
Judgment dated September 2, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Complaints about wrong. actual (no.) - from violations of the electoral law
In satisfying the application of Yevgeny Trofimovich Bardakhanov on recognizing the decision of the Ekhirit-Bulagat territorial election commission dated DD.MM.YYYY No. illegal and canceling it, the obligation of the Ekhirit-Bulagat territorial election commission to eliminate the violations committed, to refuse in full. Reasoned decision of the court will be made DD.MM.YYYY. The decision of the court can be appealed to the Irkutsk Regional Court within 5 days from the date of the decision in the final form ...
157.
Judgment dated September 2, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Other from public law relations
DD.MM.YYYY Ekhirit-Bulagatskaya TEC adopted decision No., which appointed elections for the position of the head of the municipality "Ust-Ordynskoye" on September 08, 2013. DD.MM.YYYY by the decision of the election commission, Borkhodoev Eduard Borisovich, nominated by self-nomination, was registered as a candidate for the post of head of the municipality ...
158.
Judgment of September 2, 2013 in case No. 5-39/2013
Ekhirit-Bulagatsky District Court (Irkutsk region) - Administrative
...*** at 18.15 h. Zabanov A.K., driving a car of the brand "<данные изъяты>» state number number, moving along the country road from the side<адрес>to the side<адрес>and crossing the highway 1P-418 for 64 km. when entering the main road from a secondary one, did not provide an advantage in traffic and collided with a car of the brand "<данные изъяты>» license plate<данные изъяты>under the control of B2, which moved from the side<адрес>towards<адрес>along the main road...
159.
Decision of September 2, 2013 in case No. 2-679/2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
Acting statement Satisfy the head of the FKU OIK-1 of the GUFSIN of Russia for the Irkutsk Region. Establish in relation to Mikhailova O.V., born *** in<адрес>, administrative supervision in the form of administrative restrictions: -prohibit travel outside<адрес>EAO without the permission of the police authority - to appear at the police department at the place of residence or stay for registration 2 times a month, for a period of one year for each restriction ...
160.
Judgment dated August 30, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
161.
Judgment dated August 30, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
Satisfy the claims of Alfa-Bank OJSC. collect from Boroldoeva H.C. in favor of Alfa-Bank OJSC debt under the loan agreement from *** in the amount of<данные изъяты>rub., as well as the cost of paying the state fee in the amount of<данные изъяты>rub. The decision can be appealed to the Irkutsk Regional Court within one month from the date of its adoption. Judge Asaeva L. A....
162.
Judgment dated August 30, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
163.
Judgment dated August 30, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
Subject of the dispute: Other disputes related to land use
The statement of claim of Kokourov Vladimir Vasilievich is partially satisfied. Recognize as invalid the descriptions of the location of the boundaries and turning points of the land plot with the cadastral number, the permitted use - for conducting personal subsidiary plots located on the lands settlements, by the address:<адрес>...
164.
Judgment dated August 29, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
Claims Elaeva T.C. to satisfy. Restore Elaeva T.S. term for acceptance of the inheritance opened after the death of *** husband E. The decision can be appealed to the Irkutsk Regional Court within one month from the date of its issuance. Judge Asaeva L. A....
165.
Definition of August 29, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
AND ABOUT. Head of the Ministry of Defense of the Ministry of Internal Affairs of Russia "Ekhirit-Bulagatsky" And he applied to the court with this application, in which he asks to establish administrative supervision in relation to Rezenkov V.A. for a period of one year with the establishment of administrative restrictions. In support of the stated, he indicates that Rezenkov V.A. has an unexpunged (unspent) conviction for committing, with dangerous recidivism, crimes under Art. 111 part 1 of the Criminal Code Russian Federation(hereinafter - UK)...
166.
Judgment dated August 29, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Other lawsuits
Claims and.about. Satisfy the prosecutor of the Ekhirit-Bulagat district. To oblige the individual entrepreneur Popova Tatyana Valeryevna to carry out certification of workplaces in terms of working conditions with subsequent certification of the organization of work on labor protection, to provide conditions for employees to undergo medical examinations. The court decision can be appealed to the Irkutsk Regional Court within a month from the date of the decision in the final form .
167.
Judgment dated August 29, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Labor disputes - others arising from labor
Claims and.about. Satisfy the prosecutor of the Ekhirit-Bulagat district. To oblige the individual entrepreneur Gubin Valery Filippovich to carry out certification of workplaces in terms of working conditions with subsequent certification of the organization of work on labor protection, to provide conditions for employees to undergo medical examinations. The court decision can be appealed to the Irkutsk Regional Court within a month from the date of the decision in the final form .
168.
Judgment dated August 29, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Disputes related to the inheritance of property
In satisfaction of the claims of Halimova Marina Viktorovna to Eremina E.M., the legal representative of the minor Halimova M.R., Khalimov A.R. on the inclusion of an apartment and a land plot in the estate and the recognition of the right of ownership of an apartment and a land plot to refuse due to the omission of acceptance of the inheritance. A reasoned court decision will be made by DD.MM.YYYY...
169.
Judgment dated August 28, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The claims of Daglaeva G.K., ***, partially satisfy. Recognize for Daglaeva G.K. ownership of a residential building with a total area of 60.29 sq.m., incl. residential 38, 2 sq.m., and a land plot of 1885 sq.m., located in<адрес>. Reject the rest of the claims. The decision can be appealed to the Irkutsk Regional Court within one month from the date of its adoption. Judge Asaeva L. A....
170.
Judgment dated August 28, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
Statement of the prosecutor of the Ekhirit-Bulagatsky district Khulkhanova L.M. in the interests of an indefinite circle of persons to satisfy. Recognize the inaction of the Duma of the municipality "Aluzhinskoye", expressed in the failure to bring the Charter of the municipality "Aluzhinskoye" in accordance with the current legislation, illegal. Oblige the Duma of the municipality "Aluzhinskoye" to make changes to the Charter of the municipality "Aluzhinskoye" in accordance with the requirements federal law from 28.11...
171.
Judgment dated August 27, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
172.
Judgment dated August 27, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
173.
Judgment dated August 27, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Disputes related to the inheritance of property
Satisfy the claim of Viktor Grigoryevich Myasnikov. Establish the fact of belonging to B, DD.MM.YYYY.r., a certificate of ownership of land of series No. issued by DD.MM.YYYY Komzem of the Ekhirit-Bulagatsky district in which the person in whose name the certificate was issued is indicated B, No. (passport data ). Include in the composition of the estate left after the death of B, DD.MM.YYYY, born DD.MM ...
174.
Judgment dated August 27, 2013
Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil
The essence of the dispute: Complaints about wrong. actual (no.) - public authorities, local governments
Statement of the prosecutor of the Ekhirit-Bulagatsky district Khulkhanova L.M. in the interests of an indefinite circle of persons to satisfy. Recognize the inaction of the Duma of the municipality "Akhinsky", expressed in the failure to bring the Charter of the municipality "Akhinsky" into line with the current legislation, illegal. To oblige the Duma of the municipality "Akhinsky" to make changes to the Charter of the municipality "Akhinsky" in accordance with the requirements of the Federal Law of November 28 ...
175.
Decree of August 27, 2013
The bodies of the preliminary investigation Fedotov D.A. accused of committing theft, that is, the secret theft of another's property, committed with causing significant damage to a citizen. The crime was committed under the following circumstances: DD.MM...
178.
Judgment dated August 22, 2013 in case No. 1-81/2013
Ekhirit-Bulagatsky District Court (Irkutsk region) - Criminal
DD.MM.YYYY around 23.00 Kolosov A.Yu. was near the house of E at the address<адрес>, where he decided to steal the Stihl 180 chainsaw from the summer kitchen located in the courtyard of the said house, and from under the barn, also located in the courtyard of the said house, to steal meat and beef belonging to c. E Realizing his criminal intent aimed at the secret theft of property E, Kolosov A.Yu...
