Wet–dry cycles on sandy and loessial Negev soils: Implications for biocrust establishment and growth?

Author:

Kidron Giora J.1ORCID,Kronenfeld Rafael2,Xiao Bo3,Starinsky Abraham1

Affiliation:

1. Institute of Earth Sciences The Hebrew University Jerusalem Israel

2. Meteorological Unit Israel Meteorological Service Kibbutz Sede Boqer Israel

3. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Chinese Academy of Sciences and Ministry of Water Resources Yangling China

Publisher

Wiley

Subject

Earth-Surface Processes,Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics

Reference75 articles.

1. EFFECTS OF SOIL TEXTURE ON EVAPORATIVE LOSS AND AVAILABLE WATER IN SEMI-ARID CLIMATES

2. Effects of soil characteristics on moisture evaporation

3. Empirical models of rain-spells characteristics – A case study of a Mediterranean-arid climatic transect

4. The formation of dew

5. An initial study of pedogenic features along a transect across longitudinal dunes and interdune areas, Nizzana region, Negev, Israel;Blume H. P.;Advance in Geoecology,1995

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