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פותח על ידי קלירמאש פתרונות בע"מ -
Factors affecting the stability of soil crusts in subsequent storms.
Year:
1986
Authors :
לוי, גיא
;
.
מורין, יוסף
;
.
שיינברג, יצחק
;
.
Volume :
50
Co-Authors:
Levy, G., ARO, Volcani Center, Bet Dagan 50250, Israel.
Shainberg, I., ARO, Volcani Center, Bet Dagan 50250, Israel.
Morin, J., ARO, Volcani Center, Bet Dagan 50250, Israel.
Facilitators :
From page:
196
To page:
201
(
Total pages:
6
)
Abstract:
The stability of the crust was found to depend on the mechanisms of its formation. The crusts of soils with low exchangeable sodium percentages (ESP) exposed to distilled water (DW) and saline water (SW) rain and the crust of a soil with high ESP exposed to SW rain were found to be unstable and to be affected strongly by 1) the salinity of the rainwater in subsequent storms, 2) the impact energy of the raindrops, and 3) the length of the drying period between consecutive storms. Conversely, a crust in which chemical dispersion supplemented physical dispersion (a soil with high ESP exposed to DW rain) was found to be stable and to be less affected by the water salinity of the subsequent storm, by its impact energy, or by the extent of drying between storms. -after Authors
Note:
Related Files :
Aggregate stability
Clay dispersion
drying
METEOROLOGY - Storms
raindrop energy
salinity
Sodicity
Soils
SURFACES - Stability
עוד תגיות
תוכן קשור
More details
DOI :
Article number:
0
Affiliations:
Database:
סקופוס
Publication Type:
Language:
אנגלית
Editors' remarks:
ID:
29110
Last updated date:
02/03/2022 17:27
Creation date:
17/04/2018 00:44
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Scientific Publication
Factors affecting the stability of soil crusts in subsequent storms.
50
Levy, G., ARO, Volcani Center, Bet Dagan 50250, Israel.
Shainberg, I., ARO, Volcani Center, Bet Dagan 50250, Israel.
Morin, J., ARO, Volcani Center, Bet Dagan 50250, Israel.
Factors affecting the stability of soil crusts in subsequent storms.
The stability of the crust was found to depend on the mechanisms of its formation. The crusts of soils with low exchangeable sodium percentages (ESP) exposed to distilled water (DW) and saline water (SW) rain and the crust of a soil with high ESP exposed to SW rain were found to be unstable and to be affected strongly by 1) the salinity of the rainwater in subsequent storms, 2) the impact energy of the raindrops, and 3) the length of the drying period between consecutive storms. Conversely, a crust in which chemical dispersion supplemented physical dispersion (a soil with high ESP exposed to DW rain) was found to be stable and to be less affected by the water salinity of the subsequent storm, by its impact energy, or by the extent of drying between storms. -after Authors
Scientific Publication
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