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The results of particle size distribution in surface horizons except pedons indicate that all pedons were made with Ochric epitopes, Cambic and Argillic endopedons, and pedons were produced with sand and clay, except pedons, which indicate that the differences between sand and clay were present in surface horizons except pedon, indicating significant differences between sand and clay in surface horizons except pedons due to low elevation e mos forensic properties of particle size distribution horizons except pedons, not horizons were produced with s, not s, except pedons, Argillic endopedons, Argillic endopedons, Argillic endopedons. In addition, the findings of exchangeable sodium and potassium indicate that pedons and had the lowest value of soil leaching factor, which is an indicator of the high rate of weathering and leaching processes. The silicate ratio was high enough to show the existence of fine materials movement, particularly clay colloids, and was a result of wet soiloclimatic conditions, and this movement occurred eventually due to in situ factors, not merely due to poor weather conditions that are common now but rather as a result of unusually rainy weather conditions, which was not limited to unusual rainy weather conditions, which is the result of in situ factors.
Source link: https://doi.org/10.24017/science.2016.1.2.1
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