Результаты исследований: Научные публикации в периодических изданиях › статья по материалам конференции › Рецензирование
Dynamics of peat accumulation processes in the areas of the periglacial zone of the basin watershed of Tugur-Nimelen rivers. / Chakov, V. V.; Parkhomchuk, E. V.; Zakharchenko, E. N.
в: IOP Conference Series: Earth and Environmental Science, Том 895, № 1, 012010, 09.11.2021.Результаты исследований: Научные публикации в периодических изданиях › статья по материалам конференции › Рецензирование
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TY - JOUR
T1 - Dynamics of peat accumulation processes in the areas of the periglacial zone of the basin watershed of Tugur-Nimelen rivers
AU - Chakov, V. V.
AU - Parkhomchuk, E. V.
AU - Zakharchenko, E. N.
N1 - Funding Information: This work was supported by the Center for International Forestry Research (CIFOR) in close collaboration with the Ministry of Agriculture, Forestry and Fisheries, Japan (MAFF) and the CGIAR (LoA dated July 10, 2020; LoA dated June 9, 2021), and also by the Ministry of Science and Higher Education of the Russian Federation (state assignment theme No. 0294-2019-0001). Publisher Copyright: © Published under licence by IOP Publishing Ltd.
PY - 2021/11/9
Y1 - 2021/11/9
N2 - The paper considers the features of waterlogging of a flat watershed, unique in its structure and evolution, between the valley complexes of the two largest watercourses of Khabarovsk Territory. The Tugur and Nimelen rivers had rather powerful debit of water flows during the Pleistocene and were repeatedly redirected from the northern azimuth (the Sea of Okhotsk) to the southern one (the Amur catchment). This process continued partly at the early stages of the Holocene, as the stratigraphy of the peat deposits of the bogs formed indicates here.
AB - The paper considers the features of waterlogging of a flat watershed, unique in its structure and evolution, between the valley complexes of the two largest watercourses of Khabarovsk Territory. The Tugur and Nimelen rivers had rather powerful debit of water flows during the Pleistocene and were repeatedly redirected from the northern azimuth (the Sea of Okhotsk) to the southern one (the Amur catchment). This process continued partly at the early stages of the Holocene, as the stratigraphy of the peat deposits of the bogs formed indicates here.
UR - http://www.scopus.com/inward/record.url?scp=85120482601&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/895/1/012010
DO - 10.1088/1755-1315/895/1/012010
M3 - Conference article
AN - SCOPUS:85120482601
VL - 895
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012010
T2 - 2021 International Scientific Conference on Regions of New Development: The Current State of Natural Complexes and Their Protection, RND 2021
Y2 - 5 October 2021 through 7 October 2021
ER -
ID: 34909522