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Loss of K-Bearing Clay Minerals in Flood-Irrigated, Rice-Growing Soils in Jiangxi Province, China

Published online by Cambridge University Press:  01 January 2024

Zhongpei Li ,
B. Velde  and
Decheng Li
Zhongpei Li
Affiliation:
Institute of Soil Science, Chinese Academy of Sciences, 71 Beijing East Road, 210008, Nanjing, China
B. Velde*
Affiliation:
Laboratoire de Géologie, CNRS 2113 Ecole Normale Supérieure, 24 rue Lhomond, 75231 Paris, France
Decheng Li
Affiliation:
Institute of Soil Science, Chinese Academy of Sciences, 71 Beijing East Road, 210008, Nanjing, China Laboratoire de Géologie, CNRS 2113 Ecole Normale Supérieure, 24 rue Lhomond, 75231 Paris, France
*
*E-mail address of corresponding author: [email protected]
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Abstract

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The loss of K-bearing clay minerals has been observed over an 80 y cultivation period in Chinese rice paddies despite the use of NKP fertilizers. Clay mineral determinations were made in flood-irrigated paddies cultivated for 3, 10, 15, 30 and 80 y in clayey (45 wt.%), red soils derived from red Quaternary sediments. Three clay minerals are initially present in these soils: illite-mica, magnesian chlorite and an interstratified mica-aluminous chlorite mineral. This last phase was identified using computer simulations. The K-bearing phases (discrete mica and illite as well as interstratified mica layers) are to a large extent lost while the Fe content decreases in the soil as a whole and increases in the chlorite. The mica component in the mixed-layer mineral decreases also. These changes in clay mineralogy and relative abundance suggest a loss of potassic minerals and an increase in the formation of less siliceous, more ferro-magnesian chlorite. These changes occur over 30 y or less, a rather rapid, irreversible transformation of soil clay minerals. Such loss of potassic minerals renders the cultivation more dependent on fertilizer amendment.

Keywords

Clay MineralIrrigationMica-chlorite InterlayerPotassium
Type
Research Article
Information
Clays and Clay Minerals , Volume 51 , Issue 1 , February 2003 , pp. 75 - 82
Copyright
Copyright © 2003, The Clay Minerals Society

References

Bertsch, P.M. Bloom, P.R. and Klute, A., (1996) Aluminum Methods of Soil Analysis Madison Wisconsin Soil Science Society America 516 550.Google Scholar
Chen, M. and Liu, G.L., (1994) Clay mineral compositions, soil fertility and surface chemistry characteristics of Quaternary red soils of southern Hunan province Scientia Agricultura Sinica 27 24 30.Google Scholar
Dassonville, F. and Renault, P., (2002) Interactions between microbial processes and geochemical transformations under anaerobic conditions: a review Agronomie 22 1–18 10.1051/agro:2001001.Google Scholar
Deng, S.Q. and Xu, M.X., (1990) Studies on soil particles in China. III Physical and chemical properties of different particle size fractions of red earth in hilly lands of central Jiangxi Province Acta Pedologica Sinica 27 368 376.Google Scholar
Gharrabi, M. Velde, B. and Sagon, J.-P., (1998) The transformation of illite to muscovite in pelitic rocks: Constraints from X-ray diffraction Clays and Clay Minerals 46 79–88 10.1346/CCMN.1998.0460109.CrossRefGoogle Scholar
Ionue, K. Yoshida, M. Kaneko, K. and Nakano, K., (1977) Chloritization of paddy soils caused by acidic irrigation-water Journal of Science of Soil Manure Japan 48 193 200.Google Scholar
Jiang, M.Y. Yang, D.Y. and Hseung, Y., (1982) Soil colloid researches, VIII. Mineralogical composition of the colloids of five important soils of China Acta Pedologica Sinica 19 62 70.Google Scholar
Lanson, B., (1997) Decomposition of experimental X-ray diffraction patterns (profile fitting); A convenient way to study clay minerals Clays and Clay Minerals 40 40–52 10.1346/CCMN.1992.0400106.Google Scholar
Loeppert, R.L. Inskeep, W.P. and Klute, A., (1996) Iron Methods of Soil Analysis Madison Wisconsin Soil Science Society of America 639 664.Google Scholar
Moore, D.E. and Reynolds, R.C., (1997) X-ray Diffraction and the Identification of Clay Minerals 2nd New York Oxford University Press 378 pp.Google Scholar
Pharande, A., Hillier, S., Cotter-Howells, J. and Roe, M. (2000) Possible effects of irrigation on the clay mineralogy of Vertisols from Maharashtra, India. Abstracts of the 37 th Annual Meeting of the Clay Minerals Society, Loyola University, Chicago.Google Scholar
Prikhod’ko, V.E. Dronova, T.Y. and Sokolova, T.A., (2000) Clay minerals in soils of the Solonetzic complex and their alteration upon irrigation in the northern part of the Caspian Lowland Eurasian Soil Science 33 1295 1302.Google Scholar
Reynolds, R.C. Jr., (1985) NEWMOD a computer program for the calculation of one dimensional diffraction patterns of mixed layer clays Hanover, New Hampshire, USA R.C. Reynolds, 8 Brook Rd.Google Scholar
Shanmei, W. Shuaui, Y. and Ruicai, H., (1988) Clay minerals of Vertisols and vertic Fluvents in relation to soil classification in China Journal of Nanjing Agricultural University 11 60 66.Google Scholar
Velde, B., (2001) Clay minerals in the agricultural surface soils in the Central United States Clay Minerals 39 277–294 10.1180/000985501750539391.Google Scholar
Velde, B., (1985) Clay minerals: A Physico-chemical Explanation of their Occurrence Amsterdam Elsevier 427 pp.Google Scholar
Zhang-Ming, K. and He-Zhen, X., (1998) Clay mineralogy of major soils in mountain and hilly areas in Zhejiang Province, China Acta Agriculturae Zhejingensis 10 201 205.Google Scholar