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The effect of mineral weathering and soil solution concentration on ESR—SAR relationships of arid and semi‐arid zone soils from Israel
Year:
1984
Source of publication :
Journal of Soil Science
Authors :
Alperovitch, Nachman. I.
;
.
Frenkel, Haim
;
.
Volume :
35
Co-Authors:

FRENKEL, H., Division of Soil Physical Chemistry, Institute of Soils and Water, Volcani Centre, Bet Dagan, Israel
ALPEROVITCH, N., Division of Soil Physical Chemistry, Institute of Soils and Water, Volcani Centre, Bet Dagan, Israel

Facilitators :
From page:
367
To page:
372
(
Total pages:
6
)
Abstract:
ESR—SAR relationships of 623 soil samples from arid and semi‐arid zones in Israel were found to depend on soil salinity and cation exchange capacity as reflected crudely by the saturation percentage. The Gapon constant decreased as salinity increased and, for a given salinity level, it also decreased as the soil saturation percentage (SP) increased. There was no relationship between ESR and SAR for soils with low SP values (20–40) or low salinity levels (0.2–2 dSm−1). Regression equations are presented for different salinity and saturation percentage levels. Copyright © 1984, Wiley Blackwell. All rights reserved
Note:
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More details
DOI :
10.1111/j.1365-2389.1984.tb00292.x
Article number:
0
Affiliations:
Database:
Scopus
Publication Type:
article
;
.
Language:
English
Editors' remarks:
ID:
27153
Last updated date:
02/03/2022 17:27
Creation date:
17/04/2018 00:28
Scientific Publication
The effect of mineral weathering and soil solution concentration on ESR—SAR relationships of arid and semi‐arid zone soils from Israel
35

FRENKEL, H., Division of Soil Physical Chemistry, Institute of Soils and Water, Volcani Centre, Bet Dagan, Israel
ALPEROVITCH, N., Division of Soil Physical Chemistry, Institute of Soils and Water, Volcani Centre, Bet Dagan, Israel

The effect of mineral weathering and soil solution concentration on ESR—SAR relationships of arid and semi‐arid zone soils from Israel
ESR—SAR relationships of 623 soil samples from arid and semi‐arid zones in Israel were found to depend on soil salinity and cation exchange capacity as reflected crudely by the saturation percentage. The Gapon constant decreased as salinity increased and, for a given salinity level, it also decreased as the soil saturation percentage (SP) increased. There was no relationship between ESR and SAR for soils with low SP values (20–40) or low salinity levels (0.2–2 dSm−1). Regression equations are presented for different salinity and saturation percentage levels. Copyright © 1984, Wiley Blackwell. All rights reserved
Scientific Publication
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