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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Библиографическая информация
Другие темы
Porosite du sol; Compactacion del suelo
Язык
Английский
Примечание
8 ref. Summaries (En, Pl).
Тип
Journal Article; Journal Part; Summary
Источник
Polish-Journal-of-Soil-Science (Poland). (1988). v. 21(2) p. 145-151. Distributed 1989.
Корпоративный автор/ Групповой автор
Academy of Agriculture, Lublin (Poland)
NWFP Agricultural Univ., Peshawar (Pakistan). Dept. of Soil Science.
2012-11-15
AGRIS AP
Поставщик данных
Эту запись предоставил Wolters Kluwer
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