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THE EFFECT OF PEDOLOGICAL VARIATION ON PHYSICAL AND CHEMICAL PROPERTIES OF TWO TYPES OF SOIL IN AL-MUTHANNA GOVERNORATE.

Authors :
Al-Ghanimi, Ahmed Kadhum
Razzaq, Hiba Kalaf
Kahella, Aula Saad Rasool Abo
Source :
International Journal of Agricultural & Statistical Sciences; 2022 Supplement, Vol. 18, p1303-1308, 6p, 1 Chart
Publication Year :
2022

Abstract

This study was conducted to determine the effect of pedological variation on the physical and chemical characteristics and environmental factors of alluvial and desert soils in Al-Muthanna (Badia Al-Samawaa). Six pedons were taken, three pedons from the alluvial plain, at Al-Rumaitha, Al-Suwayr and Al-Khidhur, and three Pedons in desert soils distributed over the Samawah desert at Fadhah Umm Shih, Al-Batah and Al-Rehab. Pedons have been described morphologically in the field. Samples were taken from each horizon of all study pedons to perform the required laboratory analyzes. The results indicated that there was a variation between the desert alluvial soils properties, especially in the ratio of calcium carbonate and electrical conductivity (EC). The alluvial soils were characterized by a high percentage of salinity and a decrease in calcium carbonate, as well as variations in the color of the soil, as for the bulk density, it was revealed that there is a deaf layer in the desert soils at a depth of 30 cm. The electrical conductivity of desert soils was between 1.1-4.5 dSm m<superscript>-1</superscript>, the conductivity of alluvial soils was between 10.5-20.12 dSm m<superscript>-1</superscript>, the cation exchange capacity (CEC) of desert soils was between 10.4-11.0 cmol.kg<superscript>-1</superscript>, the alluvial soils were between 11.0-20.14 cmol.kg<superscript>-1</superscript>, as for the proportion of calcium carbonate (CaCO<subscript>3</subscript>), its value in desert soils reached between 200-450 mg kg<superscript>-1</superscript>, its value in alluvial soils was between 210-340 mg kg<superscript>-1</superscript>, the value of gypsum for desert soils was between 0.4-9.0 ml g kg<superscript>-1</superscript> and for alluvial soils it was between 1.0-5.5 g kg<superscript>-1</superscript>. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
09731903
Volume :
18
Database :
Complementary Index
Journal :
International Journal of Agricultural & Statistical Sciences
Publication Type :
Academic Journal
Accession number :
161539259