STUDIES ON DEPOSITION MODE OF SOME SOILS IN THE WESTERN NILE DELTA, EGYPT

,. M. A. Zayed, ,. H. M. A. El-Tape, ,. A. A. Al-Toukhy
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Abstract

: This study aims to discrimination between the nature of the depositional media and different mechanisms or processes, deposition environments as well as hydrodynamic conditions for some soils of the western Nile Delta, Egypt. Soils of western Nile Delta have two main physiographic units namely, the river terraces that differ in their ages and the complex unit of Wadi El-Natrun. Results of the average median size (Md) for the studied soils showed that, these soils have generally coarse and very coarse sand. Results of their mean size (Mz)indicated that, the coarse sand > medium sand > fine sand. Their sorting values (σ 1 ) are between poorly and very poorly sorted except soils belong to windblown sand that have moderately well and moderately sorted. Values of skewness (SK I ) tend to be positive to very positive skewed, which have a tail of fine grains. The predominant kurtosis (KG) classes recorded are the lepto and very leptokurtic. Depositional regime tends to be fluvial (deltaic) environments, while hydrodynamic conditions showed mechanism of rolling and suspension transportation.
埃及西尼罗河三角洲部分土壤沉积模式研究
本研究旨在区分埃及尼罗河三角洲西部一些土壤的沉积介质性质、不同的沉积机制或过程、沉积环境以及水动力条件。尼罗河三角洲西部的土壤有两个主要的地理单元,即年龄不同的河流阶地和纳特伦河的复杂单元。研究土壤的平均中位粒径(Md)结果表明,这些土壤普遍具有粗砂和极粗砂。其平均粒径(Mz)表现为粗砂>中砂>细砂。除风沙类土壤分选较好和中等外,其余土壤分选值(σ 1)均介于差分选和极差分选之间。偏度值(SK I)倾向于正到非常正的偏度,其尾部有细颗粒。主要的峰度(KG)类别记录是瘦和非常瘦峰度。沉积环境倾向于河流(三角洲)环境,水动力条件表现为滚动和悬浮搬运机制。
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