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קהילה:
אסיף מאגר המחקר החקלאי
פותח על ידי קלירמאש פתרונות בע"מ -
Effect of soil erosion on the biodiversity of soil crust within the Ziporim basin of Israel
Year:
2004
Authors :
צעדי, אלי
;
.
Volume :
5
Co-Authors:
  • T Akuja - Blaustein Institute for Desert Research Ben Gurion University of the Negev, Sede Boker, 84990, Israel; Department of Agronomy Egerton University, PO Box 536, Njoro, Kenya
  • E Zaady - Blaustein Institute for Desert Research, Ben Gurion University of the Negev, Sede Boker, 84990, Israel
Facilitators :
From page:
0
To page:
0
(
Total pages:
1
)
Abstract:

The biological soil crust is composed of living microorganisms. In deserts it is mainly the non-vascular plants that constitute the soil crust. Protein, polysaccharide, NDVI and Organic carbon showed significant differences (P<0.05) at all sites. Areas above waterfalls and non- agricultural contained more crust than those below and agricultural areas, respectively. The vegetative cover in the former sites reduced both wind and water erosion. However, areas below waterfalls had the highest protein due to the proximity of microorganisms to water that might have accumulated here during winter. The water facilitated accelerated metabolic activities of all microphytes

Note:
Related Files :
NDVI
Negev
organic carbon
protein polysaccharide
Soil crust
עוד תגיות
תוכן קשור
More details
DOI :
10.4314/ijard.v5i1.2556
Article number:
0
Affiliations:
Database:
Publication Type:
מאמר
;
.
Language:
אנגלית
Editors' remarks:
ID:
50586
Last updated date:
02/03/2022 17:27
Creation date:
29/09/2020 20:06
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Scientific Publication
Effect of soil erosion on the biodiversity of soil crust within the Ziporim basin of Israel
5
  • T Akuja - Blaustein Institute for Desert Research Ben Gurion University of the Negev, Sede Boker, 84990, Israel; Department of Agronomy Egerton University, PO Box 536, Njoro, Kenya
  • E Zaady - Blaustein Institute for Desert Research, Ben Gurion University of the Negev, Sede Boker, 84990, Israel
Effect of soil erosion on the biodiversity of soil crust within the Ziporim basin of Israel

The biological soil crust is composed of living microorganisms. In deserts it is mainly the non-vascular plants that constitute the soil crust. Protein, polysaccharide, NDVI and Organic carbon showed significant differences (P<0.05) at all sites. Areas above waterfalls and non- agricultural contained more crust than those below and agricultural areas, respectively. The vegetative cover in the former sites reduced both wind and water erosion. However, areas below waterfalls had the highest protein due to the proximity of microorganisms to water that might have accumulated here during winter. The water facilitated accelerated metabolic activities of all microphytes

Scientific Publication
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