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Forms of K as a function of clay mineralogy and soil development

Published online by Cambridge University Press:  09 July 2018

K. Nabiollahy ,
F. Khormali ,
K. Bazargan  and
SH. Ayoubi
K. Nabiollahy
Affiliation:
Department of Soil Science, College of Agriculture, Gorgon University of Agricultural Sciences and Natural Resources, Gorgan, Iran
F. Khormali*
Affiliation:
Department of Soil Science, College of Agriculture, Gorgon University of Agricultural Sciences and Natural Resources, Gorgan, Iran
K. Bazargan
Affiliation:
Soil and Water Research Institute of Iran, Tehran
SH. Ayoubi
Affiliation:
Department of Soil Science, College of Agriculture, Gorgon University of Agricultural Sciences and Natural Resources, Gorgan, Iran
*
*E-mail: Khormali@yahoo.com
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Abstract

The relationships between different pools of K, i.e. exchangeable, HN03-extractable, mineral and total, were investigated as a function of clay mineralogy and soil development in soils of Kharkeh Research Station, Kurdestan Province, western Iran. Samples from different horizons often pedons were selected and analysed for clay mineralogy and K fractionation. X-ray diffraction patterns revealed that clay minerals in the soils studied were similar in type, while their abundances were different. The smectite content was significantly greater in Vertisols than in the other soils. The results of K fractionation showed that mineral K and HN03-extractable K (exchangeable and nonexchangeable, respectively) and the clay content of the soils containing lesser illite (10–30%) were significantly different from those with more illite (30–50%). Moreover, the regression slopes between water-soluble and NE4OAc-extractable K were lower in soils with more smectite due mainly to the presence of larger specific surface areas for K sorption in smectitic soils. Based on soil evolution and different forms of K, the soils studied were grouped in two major categories: (1) Vertisols and (2) Entisols, Inceptisols and Mollisols. There were greater contents of all forms of K in Vertisols than in the other soil orders. This was mainly related to the greater clay content and the dominance of smectite in the clay fraction of Vertisols.

Keywords

clay mineralspotassiumsoil developmentIran
Type
Research papers
Information
Clay Minerals , Volume 41 , Issue 3 , September 2006 , pp. 739 - 749
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2006

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References

Addiscott, T.M. & Johnson, A.E. (1975) Potassium in soils under different cropping systems. III. Nonexchangeable potassium in soils from long-term experiments at Rothamsted and Woburn. Journal of Agricultural Science (Cambridge). 84, 513–524.Google Scholar
Al Kanani, T., Mackenzie, A.F. & Ross, G.J. (1984) Potassium status of some Quebec soils: K released by nitric acid and sodium tetraphenyl boron as related to particle size and mineralogy. Canadian Journal of Soil Science. 64, 99–106.Google Scholar
Arnold, P.W. & Close, B.M. (1961) Potasium-releasing power of soils from the Agdell rotation experiment assessed by glass house cropping. Soil Science Society of America Proceedings. 33, 226–230.Google Scholar
Bhonsle, N.S., Pal, S.K. & Sekhon, G.S. (1992) Relationship of forms and release characteristics with clay mineralogy. Geoderma. 54, 258–293.CrossRefGoogle Scholar
Brar, M.S., Subbarao, A. & Sekhon, G.S. (1986) Solution exchangeable, and nonexchangeable potassium in five soil series from the alluvial soils region of Northern India. Soil Science. 142, 229–234.CrossRefGoogle Scholar
Chapman, H.D. (1965) Cation exchange capacity. Pp. 891–901 in: Methods of Soil Analysis, Part. (Black, C.A., editor). American Society of Agronomy, Madison, Wisconsin.Google Scholar
Cimrin, K.M., Akca, E., Senol, M.B. & Kapur, S. (2004) Potassium potential of the soils of the Gaves Region in Eastern Anatolia. Turk Journal of Agriculture. 28, 259–266.Google Scholar
Conyers, E.S. & Mclean, E.O. (1969) Plant uptake and chemical extractions for evaluating potassium release characteristics of soils. Soil Science Society of America Proceedings. 33, 226–230.CrossRefGoogle Scholar
Day, P.R. (1965) Particle fractionation and particle-size analysis. Pp. 545–567 in: Methods of Soil Analysis, Part. (Black, C.A., editor). American Society of Agronomy, Madison, Wisconsin.Google Scholar
Gosh, B.N. & Singh, R.D. (2002) Potassium release characteristics of some soils of Uttar Pradesh hills varying in altitude and their relationship with forms of soil K and clay mineralogy. Geoderma. 104, 135–141.CrossRefGoogle Scholar
Hosseinpour, A., Kalbasi, M. & Khademi, H. (2001) Kinetics of non-exchangeable K release in soil and soil components of Gilan Province. Iran Soil and Water Journal. 14, 112–119.Google Scholar
Huang, P.M. (1977) Feldspars, olivines, pyroxenes and amphiboles. Pp. 553–602 in: Minerals in Soil Environment. (Nixon, J.B. & Weed, S., editors). Soil Science Society of America, Madison, Wisconsin.Google Scholar
Hutcheon, I., Bloch, J. & Modus, S. (2000) Potassium enrichment in shale fluid transport or provenance. Journal of Geochemical Exploraction. 69, 17–22.CrossRefGoogle Scholar
Jackson, M.L. (1975) Soil Chemical Analysis: Advanced Course. Department of Soils, College of Agriculture, University of Wisconsin, Madison, Wisconsin.Google Scholar
Jalali, M. (2006) Kinetics of non-exchangeable potassium release and availability in some calcareous soils of western Iran. Geoderm. (in press).Google Scholar
Johns, W.D., Grim, R.E. & Bradley, F. (1954) Quantitative estimation of clay minerals by diffraction methods. Journal of Sedimentary Petrology. 24, 242–251.Google Scholar
Khormali, F. & Abtahi, A. (2003) Origin and distribution of clay minerals in calcareous arid and semiarid soils of Fars Province, southern Iran. Clay Minerals. 38, 511–527.CrossRefGoogle Scholar
Khormali, F., Abtahi, A. & Owliaie, H.R. (2005) Late Mesozic-Cenozoic clay mineral succession of southern Iran and their palaeoclimatic implications. Clay Minerals. 40, 191–203.CrossRefGoogle Scholar
Kilmer, V.J., Younts, S.E. & Brady, N.C. (1968) The Role of Potassium in Agriculture. American Society of Agronomy, Madison, Wisconsin.Google Scholar
Kittrick, J.A. & Hope, E.W. (1963) A procedure for the particle size separation of soils for X-ray diffraction Analysis. Soil Science. 96, 312–325.CrossRefGoogle Scholar
Knudsen, D., Peterson, G.A. & Part, P.E. (1996) Lithium, sodium and potassium. Pp. 403–429 in: Methods of Soil Analysis. Part. (Page, A.L. et al.. editors). American Society of Agronomy, Madison, Wisconsin.Google Scholar
Majumdar, K.S., Sandy, K. & Datta, S.H. (2002) Potassium release and fixation behavior of mineralogically different soils of India. 11th World Congress of Soil Science. pp. 14–21.Google Scholar
Martin, H.W. & Sparks, D.L. (1985) On the behavior of non-exchangeable potassium in soils. Communications in Soil Science and Plant Analysis. 16, 133–162.CrossRefGoogle Scholar
Mclean, A.J. (1961) Potassium-supplying power of some Canadian soils. Canadian Journal of Soil Science. 41, 196–206.CrossRefGoogle Scholar
Mclean, E.O. & Watson, M.E. (1985) Soil measurements of plant-available potassium. Pp. 277–303 in: Potassium in Agricultur. (Munson, R.D., editor). American Society of Agronomy, Madison, Wisconsin.Google Scholar
Mehra, O.P. & Jackson, M.L. (1960) Iron oxide removal from soils and clays by a dithionate citrate system with sodium bicarbonate. Clay Minerals. 7, 317–327.Google Scholar
Nelson, D.W. & Sommers, L.E. (1982) Total carbon, organic carbon, and organic matter. Pp. 539–579 in: Methods of Soil Analysis, Part. (Page, A.L., editor). American Society of Agronomy, Madison, Wisconsin.Google Scholar
Nemeth, K., Mengel, K. & Grimme, H. (1970) The concentration of K, Ca, and Mg in the saturation extract in relation to exchangeable K, Ca and Mg. Soil Science. 109, 179–185.CrossRefGoogle Scholar
Salinity Laboratory Staff (1954) Diagnosis and Improvement of Saline and Alkali Soils. Handbook No. 60, United States Department of Agriculture, Washington, D.C. Google Scholar
Samuel, N. & Delvaux, B. (2004) Selective sorption of potassium in a weathering sequence of volcanic ash soils from Guadeloupe, French West Indies. Catena. 56, 185–198.Google Scholar
Scott, A.D. (1968) Effect of particle size on interlayer potassium exchange in mica. 9th International Congress on Soil Science, Transactions. pp. 649–660.Google Scholar
Sharply, A.N. (1989) Relationship between forms of potassium with mineralogy. Soil Science Society of America Journal. 53, 1023–1027.CrossRefGoogle Scholar
Sparks, D.L. & Huang, P.M. (1985) Physical chemistry of soil potassium. Pp. 201–276 in: Potassium in Agriculture of Temperate Region Soil. (Munson, R.E., editor). Soil Science Society of America, Madison, Wisconsin.Google Scholar
Surapaneni, A., Palmer, A.S., Tillman, R.W., Kirkman, J.H. & Gregg, P.E.H. (2002) The mineralogy and potassium supplying power of some loessial and related soils of New Zealand. Geoderma. 110, 191–204.CrossRefGoogle Scholar