Article ID Journal Published Year Pages File Type
6408344 Geoderma 2016 9 Pages PDF
Abstract
In this sloping area, the litter generated by shrubs did not provide greater SOM at the site where it occurred, but few meters below, where it was deposited by water erosion. Comparisons between downslope and upper slope soils yielded significant differences An increase in SOM (from 1.99 to 2.75%); N (from 0.133% to 0.196%); CND (counting number drop) (from 16 to 34) and a decrease of bulk density (from 1.32 to 1.27 g cm− 3) respectively.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
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