Zobrazeno 1 - 7
of 7
pro vyhledávání: '"M. O. Tarkhov"'
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 87, Pp 39-54 (2017)
The results of the four-year study of the temperature regime of soils of three common landscapes of northern taiga in Western Siberia, located in the area of discontinuous permafrost, are presented. The soils of lumpy peatlands are characterized by m
Externí odkaz:
https://doaj.org/article/b1615b4278f543f693a1495de38bb7de
Autor:
G. V. Matyshak, S. V. Chuvanov, O. Yu. Goncharova, V. A. Trifonova, M. V. Timofeeva, A. V. Isaeva, M. O. Tarkhov
Publikováno v:
Eurasian Soil Science. 56:434-446
Autor:
M. O. Tarkhov, G. V. Matyshak, S. V. Chuvanov, A. R. Sefiliyan, I. M. Ryzhova, O. Yu. Goncharova, D. G. Petrov
Publikováno v:
Eurasian Soil Science. 54:1028-1037
Peatland soils in permafrost area are among the major components of global carbon cycle. In the case of predicted climate change, they may act as a significant source of greenhouse gases efflux. A four-year transplantation experiment (transplantation
Autor:
A. R. Sefilian, M. O. Tarkhov, G. V. Matyshak, O. Yu. Goncharova, A. A. Bobrik, Maria Timofeeva
Publikováno v:
Contemporary Problems of Ecology. 12:534-543
In the course of research performed in the continuous and discontinuous permafrost zone of the north of Western Siberia, the values of autotrophic (root) and heterotrophic (microbial) soil respiration and their ratio were estimated for typical ecosys
Autor:
Aleksey V. Kachalkin, A. V. Yakushev, M. O. Tarkhov, D. G. Petrov, G. V. Matyshak, A. R. Sefilyan
Publikováno v:
Eurasian Soil Science. 52:1081-1090
A destructive peat horizon Tmd of bare peat circles on flat-topped peat mounds in the north of Western Siberia differs from peat horizons (T) of typical peat soils in its higher density, water content, and comminution of peat residues; lower microbia
Autor:
I. M. Ryzhova, O. Yu. Goncharova, D. G. Petrov, G. V. Matyshak, M. O. Tarkhov, N. Petrzhik, A. A. Bobrik
Publikováno v:
Eurasian Soil Science. 52:945-953
Palsa peatland soils are known as significant terrestrial storage of the Earth’s soil carbon. The response of these soils to changing climate may result in a strong feedback to global carbon balance. In laboratory, we investigated the effect of ris
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 87, Pp 39-54 (2017)
The results of the four-year study of the temperature regime of soils of three common landscapes of northern taiga in Western Siberia, located in the area of discontinuous permafrost, are presented. The soils of lumpy peatlands are characterized by m