Zobrazeno 1 - 10
of 61
pro vyhledávání: '"A F, Krasnov"'
Autor:
Panos Panagos, Pasquale Borrelli, Katrin Meusburger, Bofu Yu, Andreas Klik, Kyoung Jae Lim, Jae E. Yang, Jinren Ni, Chiyuan Miao, Nabansu Chattopadhyay, Seyed Hamidreza Sadeghi, Zeinab Hazbavi, Mohsen Zabihi, Gennady A. Larionov, Sergey F. Krasnov, Andrey V. Gorobets, Yoav Levi, Gunay Erpul, Christian Birkel, Natalia Hoyos, Victoria Naipal, Paulo Tarso S. Oliveira, Carlos A. Bonilla, Mohamed Meddi, Werner Nel, Hassan Al Dashti, Martino Boni, Nazzareno Diodato, Kristof Van Oost, Mark Nearing, Cristiano Ballabio
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-12 (2017)
Abstract The exposure of the Earth’s surface to the energetic input of rainfall is one of the key factors controlling water erosion. While water erosion is identified as the most serious cause of soil degradation globally, global patterns of rainfa
Externí odkaz:
https://doaj.org/article/07f598e8e6e94108b92a17641e260430
Autor:
O. G. Bushueva, A. V. Gorobets, N. G. Dobrovol’Skaya, Z. P. Kiryukhina, S. F. Krasnov, G. A. Larionov, L. F. Litvin
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 78, Pp 20-30 (2015)
It is known that tensile strength of soil samples is by three orders of magnitude greater than the shear stresses on the bottom of slope streams responsible for the detachment and transport of soil particles by water current. C.E. Mirtskhulava believ
Externí odkaz:
https://doaj.org/article/b20d820c065948ef8b3b94daaaec3b91
Publikováno v:
Eurasian Soil Science. 54:648-652
The erosive capacity of slope water flows, a key parameter in the quantitative assessment of soil erosion, is defined as the difference between the transporting capacity of the flow and the total content of its suspended load and bedload. Therefore,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96b2322f8497f509d7751cd8aa190cc2
https://doi.org/10.1134/s1064229321040062
https://doi.org/10.1134/s1064229321040062
Publikováno v:
Eurasian Soil Science. 54:150-160
Socioeconomic reforms in agrarian sector together with climate changes induce spatial changes in the anthropogenic factors of agricultural soil erosion and soil erosion patterns in the Asian part of Russia. Comparison of pre- and post-reform quantita
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55bf8a192ec0af272e86ccc87cebc7b1
https://doi.org/10.1134/s1064229321010075
https://doi.org/10.1134/s1064229321010075
Autor:
L. F. Litvin, S. F. Krasnov, N. G. Dobrovol’skaya, G. A. Larionov, A. V. Gorobets, Z. P. Kiryukhina
Publikováno v:
Eurasian Soil Science. 52:1306-1309
It has been experimentally shown that there are two ranges of water flow velocities, at which the erodibility of a monofractional soil (of aggregates 1–2 mm) sharply differs. In the low-velocity range, the erodibility varies from 171.53 to 3.17 m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc01b08b21f982e7464f2d98dafadcf4
https://doi.org/10.1134/s1064229319090047
https://doi.org/10.1134/s1064229319090047
Autor:
G. A. Larionov, I. A. Maksimova, N. G. Dobrovol’skaya, Z. P. Kiryukhina, O. G. Bushueva, A. V. Gorobets, L. F. Litvin, S. F. Krasnov, I. I. Sudnitsyn
Publikováno v:
Eurasian Soil Science. 51:336-344
The effect of different factors and preparation conditions of monofraction samples from the arable horizon of leached chernozem on soil erodibility and its relationship with soil tensile strength (STS) has been studied. The exposure of samples at 38
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f29ed9034d70614cce35990ece46b142
https://doi.org/10.1134/s1064229318030067
https://doi.org/10.1134/s1064229318030067
Autor:
N. G. Dobrovol’skaya, A. V. Gorobets, I. I. Sudnitsyn, L. F. Litvin, G. A. Larionov, S. F. Krasnov, L. V. Kobylchenko Kuksina, Z. P. Kiryukhina, O. G. Bushueva
Publikováno v:
Eurasian Soil Science. 51:251-254
It has been shown in experiments in a hydraulic flume with a knee-shaped bend that the rate of soil erosion more than doubles at the flow impact angles to the channel side from 0° to 50°. At higher channel bends, the experiment could not be perform
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5518cf3449b327eb6b19d8639ffc5c0c
https://doi.org/10.1134/s1064229318020072
https://doi.org/10.1134/s1064229318020072
Publikováno v:
Eurasian Soil Science. 50:1344-1353
Socioeconomic transformation together with climate change in recent decades significantly affected the geography of agricultural erosion in European Russia. Calculations of erosion rate and soil loss from slopes using logical-mathematical erosion mod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5712fe3f758a4f79fc91e8b3394e86a5
https://doi.org/10.1134/s1064229317110084
https://doi.org/10.1134/s1064229317110084
Autor:
L. F. Litvin, S. F. Krasnov, I. I. Sudnitsyn, Z. P. Kiryukhina, G. A. Larionov, N. G. Dobrovol’skaya, A. V. Gorobets
Publikováno v:
Eurasian Soil Science. 50:335-340
The effect of density of monofraction samples from the plow horizon of leached chernozem on the rupture rate of interaggregate bonds in water has been studied. The rupture rate of bonds has been determined in a hydraulic flume by alternating passive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f39a7d921b48a27d878dc64d057abab
https://doi.org/10.1134/s1064229317010094
https://doi.org/10.1134/s1064229317010094
Autor:
G. A. Larionov, Z. P. Kiryukhina, O. G. Bushueva, N. G. Dobrovol’skaya, L. F. Litvin, S. F. Krasnov
Publikováno v:
Eurasian Soil Science. 49:546-550
It has been experimentally shown with monoaggregate model samples of chernozemic soil as an example that the weakening of cohesion between soil particles is due to the molecular interaction of soil particles with water as a dipole substance rather th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a07bb21ac72af3cf3fc5e20ce4ae6b8
https://doi.org/10.1134/s1064229316050100
https://doi.org/10.1134/s1064229316050100