Abstract
Agricultural use may change soil. These changes may be observed by examining certain soil properties. In numerous cases of agricultural use, soil compaction may be observed at the depth of 25–35 cm. After many years of use, this may lead to the creation of a plough sole. On arable grounds, which are generally fertilized by minerals, a decrease in organic matter content and soil acidification are frequently observed.
Language: English
Page range: 153 - 162
Published on: Nov 25, 2018
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year
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© 2018 Barbara Braun, published by Faculty of Geography and Regional Studies, University of Warsaw
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.