Pedogenetic evolution of clay minerals and agricultural implications in three paddy soil chronosequences of south China derived from different parent materials

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• 作者：Guang-Zhong Han (1) (2) (3)
  Gan-Lin Zhang (1) (2)
  De-Cheng Li (1)
  Jin-Ling Yang (1)
  
  1. State Key Laboratory of Soil and Sustainable Agriculture ; Institute of Soil Science ; Chinese Academy of Sciences ; Nanjing ; 210008 ; People鈥檚 Republic of China
  2. University of the Chinese Academy of Sciences ; Beijing ; 100049 ; People鈥檚 Republic of China
  3. College of Resources and Environmental Science ; Neijiang Normal University ; Neijiang ; 641112 ; People鈥檚 Republic of China
  
• 关键词：Clay minerals ; Depotassication ; K ; bearing minerals ; Paddy soil chronosequences ; Parent materials
• 刊名：Journal of Soils and Sediments
• 出版年：2015
• 出版时间：February 2015
• 年：2015
• 卷：15
• 期：2
• 页码：423-435
• 全文大小：2,140 KB
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• 刊物类别：Earth and Environmental Science
• 刊物主题：Environment
  Soil Science and Conservation
  Environment
  Environmental Physics
  
• 出版者：Springer Berlin / Heidelberg
• ISSN：1614-7480

文摘

Purpose This study aims to understand how clay minerals change sequentially with paddy cultivation age and how parent materials (or original soils) affect the clay mineral behavior of paddy soils. Materials and methods Three paddy soil chronosequences in the hilly regions of South China, derived from purple sandy shale (PS), Quaternary red clays (RC), and red sandstone (RS), were selected to explore the dynamic changes in clay mineralogy, by comparing physical, chemical, and mineralogical properties of soil sequences. Results and discussion For RC and RS soils, both of which have a low K content, there was little change in the clay minerals. Long-term paddy cultivation can promote formation of illite-like minerals; however, this form of K storage was limited under present farming conditions. In PS soils, which are abundant in K-bearing minerals, the depotassication was strong, accompanied by marked transformation of clay minerals. Kaolinite-like minerals gradually decreased with paddy cultivation age; by contrast, derivative clay minerals such as secondary chlorite and halloysite gradually increased. Strong depotassication mainly occurred in the nonclay fractions. The rate of depotassication and the generation of clay fractions were much faster than in natural soils. Conclusions The clay minerals of paddy soils mainly followed the feature of their original soils. Their evolutions could be distinguished based on their constituents, which are greatly affected by their parent materials. Moreover, paddy cultivation is able to modify clay mineralogy, according to the original mineralogy and paddy soil management.