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Information Journal Paper

Title

VARIATION IN SOIL CLAY MINERALS OF SEMIARID REGIONS OF FARS PROVINCE, IRAN

Pages

  165-180

Abstract

 Transformation and NEOFORMATION of CLAY MINERALS as affected by various physiographic positions were studied in soils from semi-arid regions of Fars province in southern Iran. Soil samples were taken from control sections of soil profiles at various PHYSIOGRAPHIC UNITS. Clay specimens were prepared from soil samples. The clay mineralogy of specimens was analyzed by X-ray diffraction. Mica (illite), chlorite, smectite (montmorillonite), vermiculite, palygorskite, and interstratified illite-smectite and chlorite-smectite were recognized. The higher PHYSIOGRAPHIC UNITS contained more illite and chlorite, whereas the lower ones had a higher montmorillonite and palygorskite. This was further confirmed by changes in cation exchange capacity of soils. Inherited illite and chlorite were transformed to montmorillonite and vermiculite. It is possible that NEOFORMATION of montmorillonite and palygorskite from soil solutions has also occurred.

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    APA: Copy

    BAGHERNEZHAD, MAJID. (2000). VARIATION IN SOIL CLAY MINERALS OF SEMIARID REGIONS OF FARS PROVINCE, IRAN. IRAN AGRICULTURAL RESEARCH, 19(2), 165-180. SID. https://sid.ir/paper/16152/en

    Vancouver: Copy

    BAGHERNEZHAD MAJID. VARIATION IN SOIL CLAY MINERALS OF SEMIARID REGIONS OF FARS PROVINCE, IRAN. IRAN AGRICULTURAL RESEARCH[Internet]. 2000;19(2):165-180. Available from: https://sid.ir/paper/16152/en

    IEEE: Copy

    MAJID BAGHERNEZHAD, “VARIATION IN SOIL CLAY MINERALS OF SEMIARID REGIONS OF FARS PROVINCE, IRAN,” IRAN AGRICULTURAL RESEARCH, vol. 19, no. 2, pp. 165–180, 2000, [Online]. Available: https://sid.ir/paper/16152/en

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