Owliaie, H., Adhami, E., Jafari, S., Rajaie, M., Ghasemi Fasaei, R. (2010). Distribution of Magnetic Susceptibility in Relation to Iron Compounds in Some Selected Soils of Fars Province. , 23(2), 191-204. doi: 10.22092/ijsr.2010.126950
H. R. Owliaie; E. Adhami; Siroos Jafari; M. Rajaie; R. Ghasemi Fasaei. "Distribution of Magnetic Susceptibility in Relation to Iron Compounds in Some Selected Soils of Fars Province". , 23, 2, 2010, 191-204. doi: 10.22092/ijsr.2010.126950
Owliaie, H., Adhami, E., Jafari, S., Rajaie, M., Ghasemi Fasaei, R. (2010). 'Distribution of Magnetic Susceptibility in Relation to Iron Compounds in Some Selected Soils of Fars Province', , 23(2), pp. 191-204. doi: 10.22092/ijsr.2010.126950
Owliaie, H., Adhami, E., Jafari, S., Rajaie, M., Ghasemi Fasaei, R. Distribution of Magnetic Susceptibility in Relation to Iron Compounds in Some Selected Soils of Fars Province. , 2010; 23(2): 191-204. doi: 10.22092/ijsr.2010.126950

Distribution of Magnetic Susceptibility in Relation to Iron Compounds in Some Selected Soils of Fars Province

پژوهش های خاک
Volume 23, Issue 2, March 2009, Pages 191-204    PDF (471.45 K)
Document Type: Research Paper
DOI: 10.22092/ijsr.2010.126950
Authors
H. R. Owliaie* 1; E. Adhami1; Siroos Jafari2; M. Rajaie3; R. Ghasemi Fasaei4
1Assistant Professor, College of Agriculture, Yasouj University
2Assistant Professor, University of Agriculture & Natural Resources of Ramin, Khuzestan
3Scientific Member of Fars Research Center of Agriculture & Natural Resources
4Assistant Professor of Shiraz University, College of Agriculture & Natural Resources, Darab
Abstract
Distribution of soil magnetic susceptibility (χ) and Fe compounds were studied in 14 soil profiles, reflecting key climatic conditions, land use, and drainage classes in Fars Province. Magnetic susceptibility was measured both on oven-dry basis (χod) and minerogenic basis (compensating for mobile diamagnetic materials such as carbonates and gypsum, χm). Magnetic susceptibility of eluvial horizons was greater than that of the illuvial horizons in most of the soils. This is probably a result of eluviation of diamagnetic materials as well as pedogenic formation of ferrimagnetic minerals in soil surface. Poorly and somewhat poorly drained soils had distinctly lower χm than well-drained soils. There was a positive significant correlation (P<0.01) between crystalline pedogenic Fe (Fed-Feo) and χm. Similar relationship was noticed between mean annual rainfall and χm.
Keywords
Magnetic susceptibility; iron compounds; calcareous soils; drainage class; rainfall
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