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פותח על ידי קלירמאש פתרונות בע"מ -
Weathering and mobility sequence of minor elements on a basaltic pedomorphic surface, Galilee, Israel
Year:
1974
Source of publication :
Geoderma
Authors :
קויומדז'יסקי, חנה
;
.
Volume :
12
Co-Authors:
Yaalon, D.H., Department of Geology, The Hebrew University, Jerusalem, Israel
Brenner, I., Geochemistry Division, Geological Survey of Israel, Jerusalem, Israel
Koyumdjisky, H., Institute of Soil and Water, The Volcani Center, Bet Dagan, Israel
Facilitators :
From page:
233
To page:
244
(
Total pages:
12
)
Abstract:
A number of minor elements was determined in 21 samples of several soil profiles of a young pedomorphic surface on basalt, Upper Galilee, Israel, ranging from red basaltic Lithosols to lithic Red Mediterranean soils and montmorillonitic Grumusols (Xerorthents, Lithic Xerochrepts, and Chromoxererts). Strontium and to a lesser extent barium are lost during the weathering of the feldspars; Sr continues to be leached out on the slope. Titanium concentrates in the non-clay residue and follows iron during its redistribution on the slope. Manganese is more mobile than iron. Cobalt is partially correlated with manganese, but like Ni, Cr, Cu and V, these elements do not show any definite trend and appear to be rather immobile under the moderate weathering conditions of the Mediterranean environment where montmorillonite is the major clay mineral. © 1974.
Note:
Related Files :
Galilee (site)
soil
עוד תגיות
תוכן קשור
More details
DOI :
10.1016/0016-7061(74)90071-8
Article number:
0
Affiliations:
Database:
סקופוס
Publication Type:
מאמר
;
.
Language:
אנגלית
Editors' remarks:
ID:
20505
Last updated date:
02/03/2022 17:27
Creation date:
16/04/2018 23:37
Scientific Publication
Weathering and mobility sequence of minor elements on a basaltic pedomorphic surface, Galilee, Israel
12
Yaalon, D.H., Department of Geology, The Hebrew University, Jerusalem, Israel
Brenner, I., Geochemistry Division, Geological Survey of Israel, Jerusalem, Israel
Koyumdjisky, H., Institute of Soil and Water, The Volcani Center, Bet Dagan, Israel
Weathering and mobility sequence of minor elements on a basaltic pedomorphic surface, Galilee, Israel
A number of minor elements was determined in 21 samples of several soil profiles of a young pedomorphic surface on basalt, Upper Galilee, Israel, ranging from red basaltic Lithosols to lithic Red Mediterranean soils and montmorillonitic Grumusols (Xerorthents, Lithic Xerochrepts, and Chromoxererts). Strontium and to a lesser extent barium are lost during the weathering of the feldspars; Sr continues to be leached out on the slope. Titanium concentrates in the non-clay residue and follows iron during its redistribution on the slope. Manganese is more mobile than iron. Cobalt is partially correlated with manganese, but like Ni, Cr, Cu and V, these elements do not show any definite trend and appear to be rather immobile under the moderate weathering conditions of the Mediterranean environment where montmorillonite is the major clay mineral. © 1974.
Scientific Publication
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