SOME FEATURES OF THE DYNAMICS OF QUALITATIVE COMPOSITION OF THE ORGANIC MATTER IN SOD-PODZOLIC SOILS DURING REFORESTATION

Section

Physical geography and biogeography, soil geography and landscape geochemistry

Title

SOME FEATURES OF THE DYNAMICS OF QUALITATIVE COMPOSITION OF THE ORGANIC MATTER IN SOD-PODZOLIC SOILS DURING REFORESTATION

Сontributors

Z.S. Artemyeva, Leading researcher of the Department of Biology and Biochemistry of Soils, V. V. Dokuchaev Soil Institute, This email address is being protected from spambots. You need JavaScript enabled to view it.

Abstract

The processes of the overgrowing of abandoned soils by native vegetation have been studied. It has been shown that in arable soils after their removal from agricultural use and the development of secondary forest in their place, with an increase of forest renewal period, starting from 20 years from the moment of reforestation, positive trends in their humus state take place. It is revealed that it is possible to completely restore their humus state within 80—100 years, which is reflected in the full compliance of the OM parame ters with those of automorphic Sodpodzolic soils of the Center of the Russian Plain, i.e., the level of accumulation and the share of carbon in organic and mineral-mineral fractions in the total accumulation of carbon in the soil and in the value of the ratio (CLF/CClay).

Keywords

soil organic matter, reforestation, granulo- dencymetric fractionation, light fractions.

References

1.  Efimov V. N., Ivanov A. I. Skrytaya degradatsiya khorosho okulturennykh derno¬vo-podzolistykh pochv Rossii [The hid- den degradation of well-cultivated Sodpodzolic soils of Russia]. Agrokhimiya [Agrochemistry]. 2001. No. 6. P. 5—10. (in Russian)

2.  Makarov I. B. Evolyutsiya pakhotnykh dernovo-podzolistykh pochv pri vyvode ikh iz selskokhozyaystvennogo ispozovaniya [Evolution of arable Sodpodzolic soils during their withdrawal from agricultural use]. Istoriya razvitiya pochv SSSR v golotsene [History of the development of the USSR soils in the Holocene]. Pushchino. 1984. P. 191—192.        (in Russian)

3.  Litvinovich A. V., Pavlova O. Yu., Chernov D. V. Izmeneniye gumusovogo sostoyaniya dernovo-podzolistoy peschanoy pochvy pri prekrashchenii antropogennogo vozdeystviya[Changes in the humus content of Sod-podzolic sandy soil with the cessation of anthropogenous impact] Dokl. Ros. akademii s/kh nauk [Report for the Rus. Academy of Agricul tural Sciences]. 2002. No. 6. P. 26—28. (in Russian)

4.  Baranova O. Yu. Antropogennye izmeneniya dernovo-podzolistykh pochv i ikh evolyutsiya pri lesovozobnovlenii. [An- thropogenic changes in Sodpodzolic soils and their evolution during reforestation]. Dissertatsiya. … MGU [PhD Thesis. … Moscow State University]. 1987. 122 p. (in Russian)

5.  Artemyeva Z. S., Fedotov G. N. Sostav funktsionalnykh pulov legkorazlagaye-mogo organicheskogo veshchestva avto- morfnykh zonalnogo ryada pochv tsentra russkoy ravniny [Composition of functional pools of the readily decomposable organic matter of automorphic zonal series of soils of the Cental Russian Plain]. Vestnik MGU [Bulletin of Moscow University. Ser. 17. Soil Science]. 2013. No. 4. P. 3—10. (in Russian)

6.  Jens Leifeld, Ingrid Kogel-Knabner. Soil organic matter fractions as early indicators for carbon stock changes under different land-use. Geoderma. Vol. 124. Issues 1—2. January 2005. P. 143—155.

7.  Christensen B. T. Physical fractionation of soil and organic matter in primary particle size and density separates. Ad vances in Soil Sci. 1992. Vol. 20. P. 1—90.