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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书目信息
其它主题
Porosite du sol; Compactacion del suelo
语言
英语
注释
8 ref. Summaries (En, Pl).
类型
Journal Article; Journal Part; Summary
来源
Polish-Journal-of-Soil-Science (Poland). (1988). v. 21(2) p. 145-151. Distributed 1989.
团体作者
Academy of Agriculture, Lublin (Poland)
NWFP Agricultural Univ., Peshawar (Pakistan). Dept. of Soil Science.
2012-11-15
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