Structure of the arable layer of chernozem formed from loess affected with compaction by tractor wheels.
1988
Slowinska Jurkiewicz A. | Domzal H.
Cracks in regular, vertical arrangement, mostly 30-150 microns wide, were found to occur in the surface layer of soil subjected to direct compaction. Below the surface zone soil compaction increases so strongly that pores larger than 20 microns do not appear at all.
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Información bibliográfica
Otras materias
Porosite du sol; Compactacion del suelo
Idioma
Inglés
Nota
8 ref. Summaries (En, Pl).
Tipo
Journal Article; Journal Part; Summary
Fuente
Polish-Journal-of-Soil-Science (Poland). (1988). v. 21(2) p. 145-151. Distributed 1989.
Autores corporativos
Academy of Agriculture, Lublin (Poland)
NWFP Agricultural Univ., Peshawar (Pakistan). Dept. of Soil Science.
2012-11-15
AGRIS AP
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