Have a personal or library account? Click to login
Biological soil crusts cause subcritical water repellency in a sand dune ecosystem located along a rainfall gradient in the NW Negev desert, Israel Cover

Biological soil crusts cause subcritical water repellency in a sand dune ecosystem located along a rainfall gradient in the NW Negev desert, Israel

Open Access
|May 2016

Abstract

The biological soil crusts (BSCs) in the NW Negev cause local water redistribution by increasing surface runoff. The effects of pore clogging and swelling of organic and inorganic crust components were intensively investigated in earlier studies. However, the effect of water repellency (WR) was not addressed systematically yet. This study investigates subcritical WR of BSCs in three different study sites in the NW Negev. For this purpose, three common methods to determine soil WR were used: (i) the repellency index (RI) method (ii) the water drop penetration time (WDPT) test and (iii) the Wilhelmy plate method (WPM). Furthermore, the potential influence of WR on local water redistribution is discussed and the applied methods are compared. We found the BSC to be subcritically water repellent. The degree of WR may only affect water redistribution on a microscale and has little influence on the ecosystem as a whole. The RI method was clearly the most appropriate to use, whereas the WDPT and the WPM failed to detect subcritical WR.

DOI: https://doi.org/10.1515/johh-2016-0001 | Journal eISSN: 1338-4333 | Journal ISSN: 0042-790X
Language: English
Page range: 133 - 140
Submitted on: Apr 28, 2015
|
Accepted on: Sep 28, 2015
|
Published on: May 12, 2016
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year

© 2016 Hannes Keck, Vincent John Martin Noah Linus Felde, Sylvie Laureen Drahorad, Peter Felix-Henningsen, published by Slovak Academy of Sciences, Institute of Hydrology
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.