Specific surface area of eroded soils formed from loess.
1988
Glinski J. | Stawinski J. | Borowiec J.
The specific surface area (S) of eroded soils formed from loess was determined. This property of the tested soils ranged from 17 to 81 (sq. m)/g. S is a sensitive index of genetic soil-forming processes and surface erosion in loess soils.
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Bibliographic information
Other Subjects
Genesis del suelo; Suelo erosionado; Roche mere; Sol erode; Propiedades fisico quimicas suelo; Propriete physicochimique du sol
Language
English
Note
4 tables; 8 ref. Summaries (En, Pl).
Type
Journal Article; Journal Part; Summary
Source
Polish-Journal-of-Soil-Science (Poland). (1988). v. 21(1) p. 15-22. Distributed 1989.
Corporate Author
Instytut Agrofizyki, Lublin (Poland) Akademia Rolnicza, Lublin (Poland)
NWFP Agricultural Univ., Peshawar (Pakistan). Dept. of Soil Science.
2012-11-15
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