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Astrakhantsev G. P. Minina T. R. Petrova N. A. Poloskov V. N. Rukhovets L. A. 《Water Resources》2003,30(2):209-220
A zoobenthos submodel is included in an ecosystem model. The new model is used to assess the role of zoobenthos in the phosphorus exchange at the water–bed interface, in particular, the phosphorus cycle in the water body ecosystem is described more accurately. The calculated zoobenthos distribution over the bed of a lake can be used in modeling the lake ichthyocenoses. 相似文献
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A. M. Nikanorov L. I. Minina V. A. Bruzgalo L. S. Kosmenko M. Yu. Kondakova O. S. Reshetnyak A. O. Danilenko 《Water Resources》2016,43(5):791-802
Many-year variations of water pollution and the state of more than two hundred of rivers (or their segments) in different latitudinal zones in European Russia are estimated. In accordance with latitudinal zonality, space and time trends in variations of water quality and the state of rivers are identified. By the level of water pollution, most river ecosystems (or their segments) were classified as polluted and very polluted, very polluted and dirty, dirty and very dirty. A tendency toward water quality improvement could be seen in the recent decade. More than 50% of the examined river ecosystems are at the transitional state of passing from natural (and/or equilibrium) to crisis state. 相似文献
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Maksimochkin V. I. Trukhin V. I. Minina Yu. A. Garanin V. K. Bovkun A. V. Anashkin S. M. 《Izvestiya Physics of the Solid Earth》2013,49(2):289-305
Izvestiya, Physics of the Solid Earth - The magnetic properties and mineralogy of kimberlites from four pipes (BK53, BK56, AK08, and AK06) in Botswana are studied. It is shown that magnetic... 相似文献
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A. M. Nikanorov O. B. Bartsev D. N. Gar’kusha E. A. Zubkov L. I. Minina 《Water Resources》2017,44(7):952-962
Underflooding of different extent was recorded in 133 populated localities in southern Rostov oblast, among which 4 such localities are always partly underflooded, and 77 localities suffer underflooding during spring floods and freshets. Minimal estimates show that the area of the territories underflooded every year and only in wet years is 282 km2 or 19% of the total built-up area in the southern Rostov oblast. Technogenic factors were found to dominate as the causes of underflooding in the majority of the populated localities. However, natural or slightly disturbed subsoil water regime is typical of the built-up territories in the southern Rostov oblast, where it implies annual periodicity of level variations with a peak in spring and a minimum in autumn. 相似文献
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L. A. Rukhovets G. P. Astrakhantsev T. R. Minina N. A. Petrova V. N. Poloskov 《Water Resources》2006,33(3):338-352
The effect of potential climate changes on the ecosystem of Lake Ladoga at different levels of anthropogenic load is studied using mathematical models. The Lake Ladoga year-round circulation corresponding to potential climate changes in the lake catchment area is reproduced. The year-round regime of functioning of the lake ecosystem is reproduced using ecosystem models. The potential changes in the lake ecosystem due to changes in the phosphorus load within the limits observed in 1961–1983 are found to be more essential than those due to prognostic changes in climate. 相似文献
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O. R. Minina N. A. Doronina G. E. Nekrasov L. I. Vetluzhskikh V. S. Lantseva V. A. Aristov S. V. Naugol’nykh A. V. Kurilenko E. V. Khodyreva 《Geotectonics》2016,50(3):276-294
New data on the composition, age, structure, and geodynamic settings of the Upper Silurian–lower Middle Carboniferous rocks in the Baikal–Vitim Fold System (BVFS) are reported. These rocks make up the Early Hercynian structural stage of the BVFS, within which the Uda–Vitim, Vitimkan–Tsipa, and Turka–Kurba lithotectonic zones are recognized. The Early Hercynian stage combines rocks of two stratigraphic levels: Upper Silurian–Upper Devonian (S2–D3) and Upper–Devonian–Middle Carboniferous (D3–C21). On the basis of lithostratigraphic and spatiotemporal relationships between sedimentary and volcanic–sedimentary complexes of the Early Hercynian stage three formations are identified, which characterize the main tectonic regimes of the early half of the Late Paleozoic. It has been established that a common paleobasin that evolved through consecutively changing geodynamic settings at the passive and active continental margins existed in the Silurian (?)–early Middle Carboniferous in the northeastern part (in present-day coordinates) of the western Transbaikal region. 相似文献
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L. A. Rukhovets N. A. Petrova V. V. Menshutkin G. P. Astrakhantsev T. R. Minina V. N. Poloskov T. N. Petrova O. M. Susareva 《Water Resources》2011,38(6):806-817
A study of the transformation of Lake Ladoga ecosystem in 1996–2005 shows that a decrease in the phosphorus load after 1995
has not cause a decrease in lake ecosystem productivity. Mathematical modeling provided an explanation of the observed phenomenon,
thus justifying limnologists’ hypothesis that phosphorus turnover within a water body accelerates with increasing abundance
of bacterioplankton and aquatic fungi. Computational experiments have shown that the additional amount of phosphorus that
is required for maintaining phytoplankton productivity is additionally released by destructors (bacterioplankton and aquatic
fungi) from detritus and organic matter dissolved in water. 相似文献