Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

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Найдено документов в текущей БД: 14

    Space-time impact of fire events on swamp-forest ecosystems of the west Siberian Plain
/ V. V. Furyaev [et al.] // Contemp. Probl. Ecol. - 2013. - Vol. 6, Is. 2. - P156-161, DOI 10.1134/S1995425513020042. - Cited References: 10 . - 6. - ISSN 1995-4255
РУБ Ecology

Аннотация: An analysis of information on the groundwater dynamics, frequency of fire events, and postfire progressive-age stages of vegetation in the swamp-forest ecosystems of the southern taiga and forest-steppe zone of the West Siberian Plain has shown that fire events are a permanent factor that controls the scales and dynamics of the forest and swamp formation processes under these specific conditions in the modern era. The greatest influence on the dynamics of ecosystems is exerted by the frequency of fires. The scope and depth of the transformation of swamp ecosystems affected by the pyrogenic factor are due to their environmental regimes and have their own properties in different landscapes.

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Держатели документа:
[Furyaev, V. V.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Krasnoyarsk 660036, Russia
[Zabolotskiy, V. I.] Adm Fed Serv Supervis Nat Resource Usage Altai Kr, Krasnoyarsk, Russia

Доп.точки доступа:
Furyaev, V.V.; Zabolotskiy, V.I.; Samsonenko, S.D.; Chernykh, V.A.

    Seasonal variability of element fluxes in two Central Siberian rivers draining high latitude permafrost dominated areas
[Text] / M. L. Bagard [et al.] // Geochim. Cosmochim. Acta. - 2011. - Vol. 75, Is. 12. - P3335-3357, DOI 10.1016/j.gca.2011.03.024. - Cited References: 80. - This work benefited from fruitful discussions with S. Derenne, J. Templier, and T. Weber and from thorough reviews by S. Gislason, Ed Tipper and an anonymous reviewer. We also thank the associate Editor S. Hemming. B. Kieffel, Th. Perronne and E. Pelt are acknowledged for their help in measuring U and Sr isotope ratios. This work was financially supported by the French INSU-CNRS program "EC2CO-Cytrix", and CNRS program "GDRI Car-Wet-Sib". It was also supported by the funding from the Region Alsace, France, and the CPER 2003-2013 "REALISE". MLB benefited the funding of a Ph.D. scholarship from the French Ministry of National Education and Research. This is an EOST-LHyGeS contribution. . - 23. - ISSN 0016-7037
РУБ Geochemistry & Geophysics

Аннотация: In order to constrain the origin and fluxes of elements carried by rivers of high latitude permafrost-dominated areas, major and trace element concentrations as well as Sr and U isotopic ratios were analyzed in the dissolved load of two Siberian rivers (Kochechum and Nizhnyaya Tunguska) regularly sampled over two hydrological cycles (2005-2007). Large water volumes of both rivers were also collected in spring 2008 in order to perform size separation through dialysis experiments. This study was completed by spatial sampling of the Kochechum watershed carried out during summer and by a detailed analysis of the main hydrological compartments of a small watershed. From element concentration variations along the hydrological cycle, different periods can be marked out, matching hydrological periods. During winter baseflow period (October to May) there is a concentration increase for major soluble cations and anions by an order of magnitude. The spring flood period (end of May-beginning of June) is marked by a sharp concentration decrease for soluble elements whereas dissolved organic carbon and insoluble element concentrations strongly increase. When the spring flood discharge occurs, the significant increase of aluminum and iron concentrations is related to the presence of organo-mineral colloids that mobilize insoluble elements. The study of colloidal REE reveals the occurrence of two colloid sources successively involved over time: spring colloids mainly originate from the uppermost organic-rich part of soils whereas summer colloids rather come from the deep mineral horizons. Furthermore, U and Sr isotopic ratios together with soluble cation budgets in the Kochechum river impose for soluble elements the existence of three distinct fluxes over the year: (a) at the spring flood a surface flux coming from the leaching of shallow organic soil levels and containing a significant colloidal component (b) a subsurface flux predominant during summer and fall mainly controlled by water-rock interactions within mineral soils and (c) a deep groundwater flux predominant during winter which enters large rivers through unfrozen permafrost-paths. Detailed study of the Kochechum watershed suggests that the contribution of this deep flux strongly depends on the depth and continuous nature of the permafrost. (C) 2011 Elsevier Ltd. All rights reserved.

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Держатели документа:
[Bagard, Marie-Laure
Chabaux, Francois
Stille, Peter
Rihs, Sophie] Univ Strasbourg, F-67084 Strasbourg, France
[Bagard, Marie-Laure
Chabaux, Francois
Stille, Peter
Rihs, Sophie] CNRS, EOST, LHyGeS, F-67084 Strasbourg, France
[Pokrovsky, Oleg S.
Viers, Jerome
Dupre, Bernard] Observ Midi Pyrenees, UMR 5563, CNRS, LMTG, Paris, France
[Prokushkin, Anatoly S.] SB RAS, VN Sukachev Inst Forest, Krasnoyarsk, Russia
[Schmitt, Anne-Desiree] Univ Franche Comte, CNRS, UMR 6249, F-25030 Besancon, France

Доп.точки доступа:
Bagard, M.L.; Chabaux, F...; Pokrovsky, O.S.; Viers, J...; Prokushkin, A.S.; Stille, P...; Rihs, S...; Schmitt, A.D.; Dupre, B...

    Multiparametric analysis of soil properties in the drained forest bogs of Western Siberia
[Text] / T. T. Efremova, T. M. Ovchinnikova, V. G. Sukhovol'skii // Eurasian Soil Sci. - 2006. - Vol. 39, Is. 6. - P588-596, DOI 10.1134/S1064229306060020. - Cited References: 26 . - 9. - ISSN 1064-2293
РУБ Soil Science

Аннотация: The application of multiparametric statistical methods has confirmed that peat soils are different in the degree of their drainage and properties because of their modification during a 20 - 25 year period of artificial drainage operation. The following sequence represents the relative significance of the contribution to the soil changes of the parameters studied: groundwater table air capacity pH T-0 Eh water-soluble: C Fe3+ and the activity of soil oxidoreductases in the following sequence: peroxidase catalase dehydrogenase. The necessity to supplement the substantive - genetic principle of the classification of drained peat soils with characterization of their water regime is substantiated.

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Держатели документа:
Russian Acad Sci, Siberian Div, Sukachev Inst Forestry, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Efremova, T.T.; Ovchinnikova, T.M.; Sukhovol'skii, V.G.

    Dissolved organic matter sources in large Arctic rivers
/ R. M.W. Amon [et al.] // Geochimica et Cosmochimica Acta. - 2012. - Vol. 94. - P217-237, DOI 10.1016/j.gca.2012.07.015 . - ISSN 0016-7037
Аннотация: The biomarker composition of dissolved organic carbon (DOC) of the six largest Arctic rivers was studied between 2003 and 2007 as part of the PARTNERS Project. Samples were collected over seasonal cycles relatively close to the river mouths. Here we report the lignin phenol and p-hydroxybenzene composition of Arctic river DOC in order to identify major sources of carbon. Arctic river DOC represents an important carbon conduit linking the large pools of organic carbon in the Arctic/Subarctic watersheds to the Arctic Ocean. Most of the annual lignin discharge (>75%) occurs during the two month of spring freshet with extremely high lignin concentrations and a lignin phenol composition indicative of fresh vegetation from boreal forests. The three large Siberian rivers, Lena, Yenisei, and Ob, which also have the highest proportion of forests within their watersheds, contribute about 90% of the total lignin discharge to the Arctic Ocean. The composition of river DOC is also characterized by elevated levels of p-hydroxybenzenes, particularly during the low flow season, which indicates a larger contribution from mosses and peat bogs. The lignin composition was strongly related to the average 14C-age of DOC supporting the abundance of young, boreal-vegetation-derived leachates during spring flood, and older, soil-, peat-, and wetland-derived DOC during groundwater dominated low flow conditions, particularly in the Ob and Yukon Rivers. We observed significant differences in DOC concentration and composition between the rivers over the seasonal cycles with the Mackenzie River being the most unique, the Lena River being similar to the Yenisei, and the Yukon being most similar to the Ob. The observed relationship between the lignin phenol composition and watershed characteristics suggests that DOC discharge from these rivers could increase in a warmer climate under otherwise undisturbed conditions. В© 2012 Elsevier Ltd.

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Держатели документа:
Department of Marine Sciences, Texas A and M University at Galveston, Galveston, United States
Department of Oceanography, Texas A and M University, College Station, United States
V.N. Sukachev Institute of Forest SB RAS, Akademgorodok, Krasnoyarsk, Russian Federation
Institut fur Bodenkunde, Leibniz-Universitat Hannover, Hannover, Germany
Leibniz Institute of Marine Sciences, University of Kiel (IFM-GEOMAR), Kiel, Germany
Department of Marine Ecology, National Environmental Research Institute, University of Aarhus, Roskilde, Denmark
Yale School of Forestry and Environmental Studies, Yale University, CT, United States
The Woods Hole Research Center, Woods Hole, MA, United States
Marine Science Institute, University of Texas at Austin, Port Aransas, TX, United States
Marine Biological Laboratory, Woods Hole, MA, United States
South Russia Centre for Preparation and Implementation of International Projects, Rostov-on-Don, Russian Federation

Доп.точки доступа:
Amon, R.M.W.; Rinehart, A.J.; Duan, S.; Louchouarn, P.; Prokushkin, A.; Guggenberger, G.; Bauch, D.; Stedmon, C.; Raymond, P.A.; Holmes, R.M.; McClelland, J.W.; Peterson, B.J.; Walker, S.A.; Zhulidov, A.V.

    Land use impacts on river hydrological regimes in Northern Asia
/ A. Onuchin [et al.] // IAHS-AISH Publication. - 2009. - Vol. 331: Symposium JS.4 at the Joint Convention of the International Association of Hydrological Sciences, IAHS and the International Association of Hydrogeologists, IAH (6 September 2009 through 12 September 2009, Hyderabad) Conference code: 83573. - P163-170 . -

Кл.слова (ненормированные):
Afforestation -- Clear cuts -- Forest logging -- Hydrological regime -- Precipitation -- River catchments -- River flow -- Afforestation -- Clear cuts -- Forest logging -- Hydrological regime -- Precipitation -- River catchments -- River flow -- Catchments -- Decision making -- Groundwater -- Hydrogeology -- Land use -- Landforms -- Reforestation -- Runoff -- Stream flow -- Water resources -- Watersheds -- Rivers -- afforestation -- assessment method -- catchment -- clearcutting -- decision making -- environmental indicator -- human activity -- hydrological regime -- hydrology -- land cover -- land use change -- logging (geophysics) -- regional climate -- river flow -- runoff -- sustainability -- water quality -- watershed -- Siberia

Аннотация: River flow is vitally important to many human activities. River flow is influenced by climatic and land-cover changes. Land-use practices have a significant effect on water flow and quality. Land use can change surface runoff, which in turn can be used as an environmental indicator of a land use level of sustamability. Along with the regional climate, hydrological processes occurring in river basins in Siberia and mountainous Kyrgyzia are controlled by forest logging and afforestation. The method used to analyse annual river flow genesis to date allowed the onset of, and assessment of, the level of human activities in the watersheds. Moreover, river flow genesis can be used in land use decision-making. River flow reflects all watershed changes, which can have opposite effects, thus compensating for each other. This study confirmed that river flow changes in time, thus reflecting land cover changes in watersheds. Copyright В© 2009 IAHS Press.

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Держатели документа:
V. N. Sukachev Institute of Forest Siberian Branch, Russian Academy of Sciences, 660036, Academgorodok, Krasnoyarsk, Russian Federation
P. A. Gan Institute of Forest and Nut Plantation, Kyrgyzian Academy of Sciences, Kargachevaya rosha, 15, 720015, Bishkek, Kyrgyzstan

Доп.точки доступа:
Onuchin, A.; Burenina, T.; Gaparov, K.; Ziryukina, N.

    GIS-based tool to determine streamside forest shelterbelt width
/ M. Korets, A. Onuchin // IAHS-AISH Publication. - 2009. - Vol. 331: Symposium JS.4 at the Joint Convention of the International Association of Hydrological Sciences, IAHS and the International Association of Hydrogeologists, IAH (6 September 2009 through 12 September 2009, Hyderabad) Conference code: 83573. - P510-513 . -

Кл.слова (ненормированные):
Central Siberia -- DEM -- GIS -- Streamside forest shelterbelt -- Surface runoff -- DEM -- GIS -- SIBERIA -- Streamside forest shelterbelt -- Surface runoff -- Algorithms -- Groundwater -- Hydrogeology -- Reservoirs (water) -- Runoff -- Surface structure -- Water pollution -- Water quality -- Water resources -- Rivers -- algorithm -- assessment method -- basin management -- empirical analysis -- forest ecosystem -- GIS -- hydrology -- infiltration -- integrated approach -- landscape -- pollution -- runoff -- shelterbelt -- slope -- software -- spatial analysis -- stream -- three-dimensional modeling -- water quality -- water resource -- Yenisei Basin -- Sandfly fever sicilian virus

Аннотация: Forest areas can intercept surface runoff from upslope bare areas and transfer it to interflow. Therefore, planting protective forests along the banks of rivers, reservoirs, and lakes preserves natural water sources from pollution. Depending on the particular landscape conditions, the streamside forest shelterbelt (SFS) width is often either wider or narrower than the ecologically substantiated width. As a result, either water quality worsens or the ecologically unjustified prohibition of forest use leads to economic losses. The assessment of SFS width using GIS technologies allows considerable simplification of evaluation procedures and their application in practice. DEM processing is integrated into most modern GIS software packages. For example, the popular ESRI ArcGIS package with its Spatial Analyst module provides extra options for calculating a series of relief-based hydrological features, which include calculation procedures for surface flow direction, length of flow-producing slopes and surface flow accumulations. Two algorithms for GIS-based SFS construction were tested for several rivers of the Yenisei basin and Krasnoyarsk Reservoir, Siberia. The first algorithm is technically simple and based on empirical equations of runoff slope length, slope steepness and soil infiltration. The second one includes a three-dimensional flow accumulation procedure and thus it is more sensitive to real surface structure. Both algorithms are ready to be used in practice. The results obtained indicate that, on average, the SFS width along banks of large rivers might be reduced, while in some cases it should be widened along the banks of small streams. Copyright В© 2009 IAHS Press.

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Держатели документа:
V. N. Sukachev Institute of Forest, Siberian Branch, Russian Academy of Sciences, 50/28, Akademgorodok, 660036, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Korets, M.; Onuchin, A.

    Variation of the hydrological regime of Bele-Shira closed basin in Southern Siberia and its reflection in the radial growth of Larix sibirica
/ E. A. Babushkina [et al.] // Reg. Envir. Chang. - 2017. - Vol. 17, Is. 6. - P1725-1737, DOI 10.1007/s10113-017-1137-1. - Cited References:41. - This study was funded by the Russian Foundation for Basic Research and the Republic of Khakassia according to the research Projects No. 14-44-04043 and No. 15-05-01666. We also thank anonymous reviewers and editor Wolfgang Cramer for their helpful comments. . - ISSN 1436-3798. - ISSN 1436-378X
РУБ Environmental Sciences + Environmental Studies

Аннотация: This study analyses dynamics of the hydrological regime of Bele-Shira closed basin and evaluates the potential for using radial growth of Siberian larch (Larix sibirica) for its assessment. We investigated the relationships between different characteristics of the water level variation of Lake Shira, precipitation amount and long-term regional chronologies developed from 56 living trees and 32 dead trees on three sites across this basin. Graphical and correlation analysis indicate that the interannual change (June minus previous June) of the water level of Lake Shira is strongly positively related to the annual sum of precipitation from July to June and the radial growth of larch. It was shown that this hydrological characteristic integrates the current dynamics of the regional precipitation and moisture regime as a whole of the Bele-Shira closed basin on interannual and decadal scales. The water level of Lake Shira fluctuates on a multi-year timescale in synchrony with the cumulative sum of the tree-ring chronology and also has strong positive long-term trend, probably driven by the continual groundwater inflow from neighboring Lake Itkul. Delayed relationships of precipitation and radial growth with the Lake Shira level change are interpreted with reference to a water balance model of the closed basin. Results offer the possibility of reconstructing interannual and decadal variation of the hydrological regime during the last few centuries through regression models using tree-ring chronologies or the dynamics of climatic variables recovered from them.

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Держатели документа:
Siberian Fed Univ, Khakass Tech Inst, 27 Shchetinkina St, Abakan 655017, Russia.
Russian Acad Sci, Inst Geog, 29 Staromonetniy Pereulok, Moscow 119017, Russia.
Univ Arizona, Tree Ring Res Lab, 1215 E Lowell St,Box 210045, Tucson, AZ 85721 USA.
Siberian Fed Univ, 79 Pr Svobodniy, Krasnoyarsk 660041, Russia.
Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, 50-28 Akademgorodok, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Babushkina, Elena A.; Belokopytova, Liliana V.; Grachev, Alexi M.; Meko, David M.; Vaganov, Eugene A.; Russian Foundation for Basic Research; Republic of Khakassia [14-44-04043, 15-05-01666]

    Water and energy transfer modeling in a permafrost-dominated, forested catchment of Central Siberia: The key role of rooting depth
/ L. Orgogozo [et al.] // Permafrost Periglacial Process. - 2019. - Vol. 30, Is. 2. - P75-89, DOI 10.1002/ppp.1995. - Cited References:89. - CALMIP supercomputing center, Grant/Award Number: p12166; Campus France, Grant/Award Number: Kolmogorov No 14.587.21.0036; Russian Science Foundation, Grant/Award Number: 18-17-00237 . - ISSN 1045-6740. - ISSN 1099-1530
РУБ Geography, Physical + Geology

Аннотация: To quantify the impact of evapotranspiration phenomena on active layer dynamics in a permafrost-dominated forested watershed in Central Siberia, we performed a numerical cryohydrological study of water and energy transfer using a new open source cryohydrogeology simulator, with two innovative features: spatially distributed, mechanistic handling of evapotranspiration and inclusion of a numerical tool in a high- performance computing toolbox for numerical simulation of fluid dynamics, OpenFOAM. In this region, the heterogeneity of solar exposure leads to strong contrasts in vegetation cover, which constitutes the main source of variability in hydrological conditions at the landscape scale. The uncalibrated numerical results reproduce reasonably well the measured soil temperature profiles and the dynamics of infiltrated waters revealed by previous biogeochemical studies. The impacts of thermo-hydrological processes on water fluxes from the soils to the stream are discussed through a comparison between numerical results and field data. The impact of evapotranspiration on water fluxes is studied numerically, and highlights a strong sensitivity to variability in rooting depth and corresponding evapotranspiration at slopes of different aspect in the catchment.

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Держатели документа:
Univ Toulouse, Observ Midi Pyrenees, GET, UMR CNRS UR IRD UPS 5563 234, 14 Ave Edouard Belin, F-31400 Toulouse, France.
Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk, Russia.
Tomsk State Univ, BIO GEO CLIM Lab, Tomsk, Russia.
Univ Paris Saclay, Lab Sci Climat & Environm, IPSL LSCE, UMR CNRS CEA UVSQ 8212, Gif Sur Yvette, France.
Univ Toulouse, INPT, UPS, IMFT, Toulouse, France.
CNRS, IMFT, Toulouse, France.

Доп.точки доступа:
Orgogozo, Laurent; Prokushkin, Anatoly S.; Pokrovsky, Oleg S.; Grenier, Christophe; Quintard, Michel; Viers, Jerome; Audry, Stephane; CALMIP supercomputing center [p12166]; Campus France [14.587.21.0036]; Russian Science Foundation [18-17-00237]

    The Estimation of Solid Precipitation Distribution in the Taiga Zone of the Yenisei River Basin Using Satellite Data
/ I. V. Danilova, A. A. Onuchin // Russ. Meteorol. Hydrol. - 2019. - Vol. 44, Is. 1. - P71-77, DOI 10.3103/S1068373919010084. - Cited References:17. - The research was supported by the Russian Foundation for Basic Research (grant 18-05-00781). . - ISSN 1068-3739. - ISSN 1934-8096
РУБ Meteorology & Atmospheric Sciences

Аннотация: A methodology is presented for the estimation of the annual spatial distribution of solid precipitation using GRACE (Gravity Recovery and Climate Experiment) satellite data. The data are provided in the grid cells of 1 degrees (latitude and longitude) and allow calculating the water thickness changes near the Earth's surface including the snow cover water. The GRACE-based difference in water equivalent between the beginning and end of winter was found to be caused by both snow water and land surface characteristics which control the groundwater movement. The regularities revealed for the analyzed region and spatial detailing enable the construction of annual raster low- and mediumresolution (1 degrees and 90 m, respectively) images of solid precipitation.

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Держатели документа:
Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Akademgorodok 50,Str 28, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Danilova, I. V.; Onuchin, A. A.; Russian Foundation for Basic Research [18-05-00781]

    Weak impact of landscape parameters and rock lithology on Mg isotope composition of the Yenisey River and its tributaries
/ V. Mavromatis, A. S. Prokushkin, M. A. Korets [et al.] // Chem. Geol. - 2020. - Vol. 540. - Ст. 119547, DOI 10.1016/j.chemgeo.2020.119547 . - ISSN 0009-2541
Аннотация: Constraining the mechanisms controlling the riverine flux of major cations and their isotopes including that of Mg to the World Ocean is one of the challenges in Earth surface isotope geochemistry. In an attempt to identify the main factors affecting the Mg isotopic composition of large rivers including vegetation, climate and lithology of the watershed, we studied the largest, in terms of discharge, Siberian river, Yenisey, and 20 of its main tributaries, during spring flood, summer flow and winter. The working hypothesis was that the influence of bedrock composition is most pronounced in winter, when the soils are frozen and the rivers are fed by deep underground waters. Thus, we anticipated that the presence of permafrost will help to distinguish the impact of surface processes, linked to biological uptake and release, and deep soil/underground transport of Mg from mineral sources. In contrast to these expectations, no sizable differences in the Mg isotope composition of the river water (±0.1‰) for both the Yenisey tributaries and its main channel has been observed between the spring flood (May) and the winter (March) period. Those two periods are characterized by the differences of discharge and degree of lithological impact on element source in the river water. Regardless of the season, there was no straightforward control of lithology (relative abundance of carbonates, basalts, granites and sedimentary rocks) on ?26Mg in the main tributaries of the Yenisey river. Our findings suggest that the use of riverine Mg isotope signature for tracing weathering mechanisms and dominant lithological impact is not straightforward at the scale of large rivers whose watersheds present multiple lithologies, variable climatic conditions and vegetation types. © 2020 Elsevier B.V.

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Держатели документа:
Geosciences Environnement Toulouse (GET), CNRS, UMR 5563, Observatoire Midi-Pyrenees, 14 Av. E. Belin, Toulouse, 31400, France
V.N. Sukachev Institute of Forest, SB RAS, Akademgorodok 50/28, Krasnoyarsk, 660036, Russian Federation
BIO-GEO-CLIM Laboratory, Tomsk State University, Tomsk, Russian Federation
N. Laverov Federal Center for Arctic Research, IEPN, Russian Academy of Science, 23 Naber. Sev. Dviny, Arkhangelsk, Russian Federation

Доп.точки доступа:
Mavromatis, V.; Prokushkin, A. S.; Korets, M. A.; Chmeleff, J.; Mounic, S.; Pokrovsky, O. S.

    Testing landscape, climate and lithology impact on carbon, major and trace elements of the lena river and its tributaries during a spring flood period
/ S. N. Vorobyev, Y. Kolesnichenko, M. A. Korets, O. S. Pokrovsky // Water. - 2021. - Vol. 13, Is. 15. - Ст. 2093, DOI 10.3390/w13152093 . - ISSN 2073-4441
Аннотация: Transport of carbon, major and trace elements by rivers in permafrost-affected regions is one of the key factors in circumpolar aquatic ecosystem response to climate warming and permafrost thaw. A snap-shot study of major and trace element concentration in the Lena River basin during the peak of spring flood revealed a specific group of solutes according to their spatial pattern across the river main stem and tributaries and allowed the establishment of a link to certain landscape parameters. We demonstrate a systematic decrease of labile major and trace anion, alkali and alkaline-earth metal concentration downstream of the main stem of the Lena River, linked to change in dominant rocks from carbonate to silicate, and a northward decreasing influence of the groundwater. In contrast, dissolved organic carbon (DOC) and a number of low-soluble elements exhibited an increase in concentration from the SW to the NE part of the river. We tentatively link this to an increase in soil organic carbon stock and silicate rocks in the Lena River watershed in this direction. Among all the landscape parameters, the proportion of sporadic permafrost on the watershed strongly influenced concentrations of soluble highly mobile elements (Cl, B, DIC, Li, Na, K, Mg, Ca, Sr, Mo, As and U). Another important factor of element concentration control in the Lena River tributaries was the coverage of the watershed by light (for B, Cl, Na, K, U) and deciduous (for Fe, Ni, Zn, Ge, Rb, Zr, La, Th) needle-leaf forest (pine and larch). Our results also suggest a DOC-enhanced transport of low-soluble trace elements in the NW part of the basin. This part of the basin is dominated by silicate rocks and continuous permafrost, as compared to the carbonate rock-dominated and groundwater-affected SW part of the Lena River basin. Overall, the impact of rock lithology and permafrost on major and trace solutes of the Lena River basin during the peak of spring flood was mostly detected at the scale of the main stem. Such an impact for tributaries was much less pronounced, because of the dominance of surface flow and lower hydrological connectivity with deep groundwater in the latter. Future changes in the river water chemistry linked to climate warming and permafrost thaw at the scale of the whole river basin are likely to stem from changes in the spatial pattern of dominant vegetation as well as the permafrost regime. We argue that comparable studies of large, permafrost-affected rivers during contrasting seasons, including winter baseflow, should allow efficient prediction of future changes in riverine ‘inorganic’ hydrochemistry induced by permafrost thaw. © 2021 by the authorsLicensee MDPI, Basel, Switzerland.

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Держатели документа:
BIO-GEO-CLIM Laboratory, Tomsk State University, 35 Lenina, Tomsk, 634050, Russian Federation
V.N. Sukachev Institute of Forest of the Siberian Branch of Russian Academy of Sciences—Separated Department of the KSC SB RAS, Krasnoyarsk, 660036, Russian Federation
Geosciences and Environment Toulouse, UMR 5563 CNRS, University of Toulouse, 14 Avenue Edouard Belin, Toulouse, 31400, France
N. Laverov Federal Center for Integrated Arctic Research, Russian Academy of Sciences, 23 Nab. Northern Dvina, Arkhangelsk, 163002, Russian Federation

Доп.точки доступа:
Vorobyev, S. N.; Kolesnichenko, Y.; Korets, M. A.; Pokrovsky, O. S.

    Testing Landscape, Climate and Lithology Impact on Carbon, Major and Trace Elements of the Lena River and Its Tributaries during a Spring Flood Period
/ S. N. Vorobyev, Y. Kolesnichenko, M. A. Korets, O. S. Pokrovsky // Water. - 2021. - Vol. 13, Is. 15. - Ст. 2093, DOI 10.3390/w13152093. - Cited References:75. - This research was funded by RSF, grant number 18-17-00238-P and by RFBR, grants No 19-55-15002, 20-05-00729_a. . - ISSN 2073-4441
РУБ Environmental Sciences + Water Resources
Рубрики:
WESTERN SIBERIAN RIVERS
   IRON-RICH NANOCOLLOIDS

   FLUVIAL GEOCHEMISTRY

Кл.слова (ненормированные):
river -- hydrochemistry -- permafrost -- forest -- landscape -- lithology -- carbonate rocks -- trace element -- major element

Аннотация: Transport of carbon, major and trace elements by rivers in permafrost-affected regions is one of the key factors in circumpolar aquatic ecosystem response to climate warming and permafrost thaw. A snap-shot study of major and trace element concentration in the Lena River basin during the peak of spring flood revealed a specific group of solutes according to their spatial pattern across the river main stem and tributaries and allowed the establishment of a link to certain landscape parameters. We demonstrate a systematic decrease of labile major and trace anion, alkali and alkaline-earth metal concentration downstream of the main stem of the Lena River, linked to change in dominant rocks from carbonate to silicate, and a northward decreasing influence of the groundwater. In contrast, dissolved organic carbon (DOC) and a number of low-soluble elements exhibited an increase in concentration from the SW to the NE part of the river. We tentatively link this to an increase in soil organic carbon stock and silicate rocks in the Lena River watershed in this direction. Among all the landscape parameters, the proportion of sporadic permafrost on the watershed strongly influenced concentrations of soluble highly mobile elements (Cl, B, DIC, Li, Na, K, Mg, Ca, Sr, Mo, As and U). Another important factor of element concentration control in the Lena River tributaries was the coverage of the watershed by light (for B, Cl, Na, K, U) and deciduous (for Fe, Ni, Zn, Ge, Rb, Zr, La, Th) needle-leaf forest (pine and larch). Our results also suggest a DOC-enhanced transport of low-soluble trace elements in the NW part of the basin. This part of the basin is dominated by silicate rocks and continuous permafrost, as compared to the carbonate rock-dominated and groundwater-affected SW part of the Lena River basin. Overall, the impact of rock lithology and permafrost on major and trace solutes of the Lena River basin during the peak of spring flood was mostly detected at the scale of the main stem. Such an impact for tributaries was much less pronounced, because of the dominance of surface flow and lower hydrological connectivity with deep groundwater in the latter. Future changes in the river water chemistry linked to climate warming and permafrost thaw at the scale of the whole river basin are likely to stem from changes in the spatial pattern of dominant vegetation as well as the permafrost regime. We argue that comparable studies of large, permafrost-affected rivers during contrasting seasons, including winter baseflow, should allow efficient prediction of future changes in riverine 'inorganic' hydrochemistry induced by permafrost thaw.

WOS

Держатели документа:
Tomsk State Univ, BIO GEO CLIM Lab, 35 Lenina, Tomsk 634050, Russia.
Russian Acad Sci, Dept KSC, SB RAS, VN Sukachev Inst Forest,Siberian Branch, Krasnoyarsk 660036, Russia.
Univ Toulouse, Geosci & Environm Toulouse, UMR 5563, CNRS, 14 Ave Edouard Belin, F-31400 Toulouse, France.
Russian Acad Sci, N Laverov Fed Ctr Integrated Arctic Res, 23 Nab Northern Dvina, Arkhangelsk 163002, Russia.

Доп.точки доступа:
Vorobyev, Sergey N.; Kolesnichenko, Yuri; Korets, Mikhail A.; Pokrovsky, Oleg S.; Pokrovsky, Oleg; RSFRussian Science Foundation (RSF) [18-17-00238-P]; RFBRRussian Foundation for Basic Research (RFBR) [19-55-15002, 20-05-00729_a]

    SEASONAL DYNAMICS OF CO2 EMISSION FROM THE SURFACE OF THE RAISED BOG IN CENTRAL SIBERIA
/ A. V. Makhnykina, D. A. Polosukhina, R. A. Kolosov, A. S. Prokushkin // Geosfernye Issledov. - 2021. - Is. 4. - С. 85-93, DOI 10.17223/25421379/21/7. - Cited References:25 . - ISSN 2542-1379. - ISSN 2541-9943
РУБ Geosciences, Multidisciplinary
Рубрики:
CARBON
   RESPIRATION

   PEATLANDS

Кл.слова (ненормированные):
CO2 emission -- vegetation period -- groundwater level -- boreal zone -- carbon -- cycle

Аннотация: The bog ecosystems of the northern regions, with low productivity, can accumulate large amounts of carbon due to the low rate of decomposition and respiration. However, it is expected that climate change will lead to an intensification of assimilation and respiratory activity. In this work we considered the emission activity of a raised bog during the growing season. We also analyzed the main environmental factors that could have a significant impact on the CO2 emission rates from the bog surface. In our study, we examined the seasonal dynamics of CO2 emission from the surface of a raised bog (ryam). The study of soil emission was carried out for three seasons (2018-2020) on sections of the bog area of different heights - ridges and hollows. Soil emission measurements were performed using an LI-8100A infrared gas analyzer (Li-cor Inc., Lincoln, USA). Temperature measurements measured at three depths - 5, 10, and 15 cm from the surface using a Soil Temperature Probe Type E (Omega, USA). A Theta Probe Model ML moisture meter (Delta T Devices Ltd., UK) was used to measure the volumetric moisture (5 cm from the surface). The bog water level was measured during the entire frost-free period using the HOBO Water level logger U20L-04 (Onset, USA). In terms of the temperature regime of soils, the studied areas also differ significantly from each other, demonstrating the big discrepancies in the more humid seasons of 2019 and 2020. The difference in temperature in these seasons was about 1.0 degrees C, while in the 2018 season with insufficient moisture, the difference was two times less 0.5 degrees C. The maximum emission fluxes of CO2 in the studied bog massif were recorded in the first half of August, and the lowest - from the middle of September. The highest emission rates were recorded in the 2019 season: CO2 fluxes from the bog surface averaged 4.17 +/- 4.55 mu mol CO2/m(2)/s per season. For all observation seasons, CO2 fluxes on ridges exceeded hollows by more than 60 % (p <= 0.05). The strongest dependence was observed between the CO2 emission rate and soil temperature, moreover, in the season with the amount of precipitation below the mean annual norm (http://www.meteo.ru) - 2018, the correlation is higher and the rcoefficient was 0.6 and 0.8 for the ridge and hollow sites, respectively (p <= 0.05). The dependence of CO2 emission on moisture conditions, on the contrary, is rather weak for two sites, and is often negative. Thus, based on the results obtained, it can be concluded that the emission flux from the surface of a raised bog during the snow-free period depends not only on the moisture conditions of a particular season, but also on the section of the bog area: the emission of CO2 from local elevations of the microrelief - ridges is much higher than from more watered areas - hollows. A significant response to moisture conditions was found only for the season with insufficient moisture and in an elevated section of the bog area - ridge site. The CO2 emission rate during the growing season is mainly determined by the temperature regime.

WOS

Держатели документа:
Siberian Fed Univ, Krasnoyarsk, Russia.
SB RAS, VN Sukachev Inst Forest, Krasnoyarsk, Russia.

Доп.точки доступа:
Makhnykina, A., V; Polosukhina, D. A.; Kolosov, R. A.; Prokushkin, A. S.

    Эколого-геохимическая оценка торфяных почв болотных ельников Кузнецкого Алатау
[Текст] / Т. Т. Ефремова, О. А. Шапченкова, С. П. Ефремов, А. Ф. Аврова, М. В. Седельников // Сибирский лесной журнал. - 2022. - № 4. - С. 14-25, DOI 10.15372/SJFS20220402 . - ISSN 2311-1410
ГРНТИ

Аннотация: Исследованы лесные торфяные почвы заболоченных речных долин восточного макросклона Кузнецкого Алатау. Выявлено сильное варьирование ( С v 42-88 %) содержания макро- и микроэлементов в слое современных почв (0-30 см). Средневзвешенное количество (с учетом мощности горизонтов почв и площадей торфяных массивов) в пределах орографического профиля 1087-573 м н. у. м. составляет (мг/кг): Fe8623 > Al7295 > Mn335 > Sr230 > Zn37.8 > Cr15.4 > Cu13.2 > Ni9.9 > Pb4.6 > Co3.4 > Cd0.21. Методами многомерного статистического анализа выполнено структурирование торфяных почв по содержанию зольных элементов в три кластера, соответствующие высотным отметкам 1087, 832-622, 573 м н. у. м. Наибольшими дискриминирующими возможностями обладают Zn и Fe (82.6 %). Меньшую долю различия обеспечивают Cu, Ni (17.4 %). Топографические ряды долинных торфяных почв определяются гидрогеохимической зональностью подземных вод, а также выносом элементов латеральными миграционными потоками. Впервые статистически обоснованы границы высотных поясов торфяных почв по содержанию минеральных элементов и охарактеризован геохимический состав выделенных экотопических рядов (кластеров) почв. В почвах автономного ландшафта (высокогорья) аккумулируется только Pb и Cd. По сравнению с ним в кластере почв среднегорья количество большинства зольных элементов увеличивается в среднем в 2 раза. В низкогорье интенсивность аккумуляции несколько ослабевает. В почвенном профиле радиальная геохимическая миграция Fe как характерного элемента болот с большей силой положительно связана с зольностью торфяного субстрата, Sr - с реакцией среды, Cu и Mn - с фульвокислотами. В текущий период не выявлено техногенной деградации торфяных почв восточных отрогов Кузнецкого Алатау. Эколого-геохимические особенности горных торфяных почв согласуются с характеристикой естественных биогеохимических провинций юга Центральной Сибири, в пределах которых они развиваются.
The studies were carried out in forest peat soils of swampy river valleys of the eastern macroslope of the Kuznetsk Alatau. The content of macro- and microelements in the layer of modern soils (0-30 cm) varies greatly (Cv 42-88 %). The weighted average amount (taking into account the thickness of soil horizons and peat areas) within the orographic profile of 1087-573 m a. s. l. is: Fe8623 > Al7295 > Mn335 > Sr230 > Zn37.8 > Cr15.4 > Cu13.2 > Ni9.9 > Pb4.6 > Co3.4 > Cd0.21, mg/kg. The methods of multidimensional statistical analysis have been used to structure peat soils according to the content of ash elements into three clusters corresponding to altitudinal gradient - 1087, 832-622, 573 m a. s. l. Zn and Fe have the greatest discriminating ability (82.6 %). A smaller share of the difference is provided by Cu, Ni (17.4 %). The topographic series of river valley peat soils are determined by the hydrogeochemical zonality of groundwater, as well as the removal of elements by lateral migration flows. For the first time, the boundaries of the vertical altitudinal zonality of peat soils are statistically were proved by the content of mineral elements and the geochemical composition of the selected ecotopic series (clusters) of soils is characterized. Only Pb and Cd accumulate in the soils of the autonomous landscape (highlands). In comparison with it, in the cluster of soils of the middle highlands, the amount of most ash elements increases by an average of 2 times. In the low mountains, the intensity of accumulation weakens somewhat. In the soil profile, the radial geochemical migration of iron as a characteristic element of swamps is more strongly positively correlated with the ash content of the peat substrate, strontium - with the soil pH, Cu and Mn - with fulvic acids. In the current period, no technogenic degradation of peat soils of the eastern macroslope of the Kuznetsk Alatau has been detected. The ecological and geochemical features of mountain peat soils are consistent with the characteristics of the natural biogeochemical provinces on the south of Central Siberia, within which they develop.

РИНЦ

Держатели документа:
ИЛ СО РАН : 660036, Красноярск, Академгородок, 50, стр. 28

Доп.точки доступа:
Шапченкова, Ольга Александровна; Shapchenkova Ol'ga Alexandrovna; Ефремов, Станислав Петрович; Efremov S.P.; Аврова, Ада Федоровна; Avrova Ada Fyedorovna; Седельников, М.В.; Efremova T.T.