AN STUDY ON MINERALOGY OF SOILS FORMED ON AGHAJARI FORMATION IN MASJED SOLEIMAN AND GHALE KHAJE AREA

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MEHDIZADEH H.; MOOSAVI M.H.; GHORBANI H.

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Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2010 | Volume:20 | Issue:77 (GEOLOGY ISSUE) Page(s): 151-172

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Title

AN STUDY ON MINERALOGY OF SOILS FORMED ON AGHAJARI FORMATION IN MASJED SOLEIMAN AND GHALE KHAJE AREA

Author(s)

MEHDIZADEH H. | MOOSAVI M.H. | GHORBANI H. | Issue Writer Certificate

Keywords

MINERALOGYQ3

CLAY MINERALSQ3

X – RAY DIFFRACTIONQ3

TOPOGRAPHYQ3

MASJED SOLEIMANQ3

GHALE KHAJEQ3

AGHAJARI FORMATIONQ3

Abstract

Introduction: To investigate the MINERALOGY of soils formed on AGHAJARI FORMATION and its relationship to TOPOGRAPHY, two soil profiles were selected, Masjed-Suleiman and Ghale-Khaje. Soil profiles as well as soil samples were selected in a way to show the effects of TOPOGRAPHY in a toposequence. The soils had the same parent materials while TOPOGRAPHY as well as climate was their most important diffraction factors Aim: The aims of this research are to identify MINERALOGY, TOPOGRAPHY effects on the CLAY MINERALS conversions and soils evolution on a toposequence, with same parent materials in Masjed-Suleiman and Ghale-Khaje Area.Material and Methods: After surveying the area, based on TOPOGRAPHY and site properties, five profiles were dig in a toposequence. All profiles were described based on USDA Standard Soil Description Manual and soil samples were taken from all horizons.MINERALOGY of the soils was thoroughly studied by X-ray Diffraction (XRD) method.Result: X-ray differactograms showed Illite, Kaolinite, Quartz and Feldespares in parent materials and Illite, Chlorite, Kaolonite, Vermiculite, Smectite as well as Paligorskite in soils body.Conclusion: The results also showed that as move from the top to the downhill, the amount of primary minerals such as Illite was decreased while Smectite was increased. This could be described as soil development criteria. Also, with decrease in slope, cation exchange capacity (CEC) of the soils were increased which is due to increase in Smectite as well as Vermiculite minerals in the soil body.

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APA: Copy

MEHDIZADEH, H., MOOSAVI, M.H., & GHORBANI, H.. (2010). AN STUDY ON MINERALOGY OF SOILS FORMED ON AGHAJARI FORMATION IN MASJED SOLEIMAN AND GHALE KHAJE AREA. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 20(77 (GEOLOGY ISSUE)), 151-172. SID. https://sid.ir/paper/70609/en

Vancouver: Copy

MEHDIZADEH H., MOOSAVI M.H., GHORBANI H.. AN STUDY ON MINERALOGY OF SOILS FORMED ON AGHAJARI FORMATION IN MASJED SOLEIMAN AND GHALE KHAJE AREA. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2010;20(77 (GEOLOGY ISSUE)):151-172. Available from: https://sid.ir/paper/70609/en

IEEE: Copy

H. MEHDIZADEH, M.H. MOOSAVI, and H. GHORBANI, “AN STUDY ON MINERALOGY OF SOILS FORMED ON AGHAJARI FORMATION IN MASJED SOLEIMAN AND GHALE KHAJE AREA,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 20, no. 77 (GEOLOGY ISSUE), pp. 151–172, 2010, [Online]. Available: https://sid.ir/paper/70609/en

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