DSpace

King Saud University Repository >
King Saud University >
COLLEGES >
Science Colleges >
College of Foods And Agricultural Science >
College of Foods And Agricultural Science >

Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/10097

Title: Distribution of Palygorskite in Sediments and Soils of Eastern Saudi Arabia.
Authors: H. Shadfan
A. S. Al-Mashhady
Issue Date: 1985
Abstract: Rock samples representing different soil parent materials from the Jurassic, Cretaceous and Tertiary periods in eastern Saudi Arabia were investigated for their mineralogical and chemical properties. Samples from five soil profiles found on these rocks also were studied. Palygorskite was found to be the dominant mineral in the clay fraction of the Tertiary and upper Cretaceous sediments. Some shales of Tertiary origin contained mainly palygorskite with minor amounts of gypsum and soluble salts. Palygorskite was not found in any sediments of the early lower Cretaceous and Jurassic periods, and kaolinite was the dominant mineral in the clay fraction of those sediments. Soils associated with Jurassic limestone near the Riyadh area also showed a predominance of kaolinite in their clay fractions. However, the clay fractions of the soils found on Tertiary sediments in the eastern part of the country were dominated by palygorskite. The presence of palygorskite in the soils paralleled its presence in the parent materials or the rocks exposed in the area. Eolian transport of palygorskite was found to be a factor for the occurrence of palygorskite in the soil. Thus, the major portion of the soil palygorskite probably originated from the Tertiary sediments in eastern Saudi Arabia.
URI: http://hdl.handle.net/123456789/10097
Appears in Collections:College of Foods And Agricultural Science

Files in This Item:

File Description SizeFormat
243.docx11.41 kBMicrosoft Word XMLView/Open

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

 

DSpace Software Copyright © 2002-2007 MIT and Hewlett-Packard - Feedback