Role of cryogenic processes in the organization of soils at macro-, mesoand micro-levels
Аннотация
Cryogenic processes that occur in permafrost-affected and perennially frozen soils are analyzed and systematized. Their influences are observed at the three levels of soil organization. Thin sections are prepared from thawed and frozen soil samples.
Об авторе
S. Gubin
Institute of Physico-Chemical and Biological Problems in Soil Science, Russian Academy of Sciences
Россия
Россия
Список литературы
1. Geocryological Dictionary (GEOS, Moscow, 2003) [in Russian].
2. M. I. Gerasimova, S. V. Gubin and S.A. Shoba, Micromorphology of Soils of the USSR Zonal Soils (Pushchino, 1992) [in Russian].
3. Glaciological Dictionary (Gidrometizdat, Leningrad, 1984) [in Russian].
4. S. V. Gubin, “Structure formation dynamics in Tundra Cryogenic Non-Gleyed Soils (Tundra Cryozems),” Pochvovedenie, 10, 62-70 (1993) [in Russian].
5. N. A. Karavaeva and V. O. Targulian, “Humus distribution features in tundra soils of the Northern Yakutia,” Pochvovedenie, 12, 36-45 (1960) [in Russian].
6. N. A. Karavaeva, V. O. Targulian, A.S. Cherkinsky et al., Elementary Soil-Forming Processes (Nauka, Moscow, 1992) [in Russian].
7. T. D. Morozova, “Micromorphological characteristics of Pale Yellow Permafrost soils of central Yakutia in relation to cryogenesis,” Pochvovedenie, 11, 79-89 (1965) [in Russian].
8. V. V. Rogov, Fundamentals of Cryogenesis (GEO, Novosibirsk, 2009) [in Russian].
9. G. V. Rusanova, Micromorphology of Taiga Soils (Nauka, Moscow, 1987) [in Russian].
Для цитирования:
. . Бюллетень Почвенного института имени В.В. Докучаева. 2016;(86):53-63. https://doi.org/10.19047/0136-1694-2016-86-53-63
For citation:
Gubin S.V. Role of cryogenic processes in the organization of soils at macro-, mesoand micro-levels. Dokuchaev Soil Bulletin. 2016;(86):53-63. https://doi.org/10.19047/0136-1694-2016-86-53-63
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