Biocrust as a surface protection of erodible nebkhas
Since the timescale of a nebkha from the initial formation to the eventual destruction might be 1 to 200 years, little is known about the whole evolutionary path. In the phase of erosion and deflation, nebkhas are usually one source of aeolian sand and dust. Biocrust, a common living cover in arid a...
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Published in | Earth surface processes and landforms Vol. 49; no. 13; pp. 4523 - 4531 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Bognor Regis
Wiley Subscription Services, Inc
01.10.2024
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Subjects | |
Online Access | Get full text |
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