| 我国东南部地区红壤表土养分的淋溶及再分布 |
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| 作者姓名： | SUN Bo ZHANG Tao-Lin ZHAO Qi-Guo |
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| 作者单位： | Institute of Soil Science, the Chinese Academy of Sciences, P.O. Box 821, Nanjing 210008 China
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| 基金项目： | 国家重点基础研究发展计划(973计划)，中国科学院资助项目 |
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| 摘 要： | The leaching and redistribution of nutrients in the surface layer of 4 types of red soils in Southeast China were studied with a lysimeter experiment under field conditions. Results showed that the leaching concentrated in the rainy season (from April to June). Generally, the leaching of soil nutrients from the surface layer of red soils was in the order of Ca > Mg > K > NO3-N. In fertilization treatment, the total amount of soil nutrients leached out of the surface layer in a red soil derived from granite was the highest in all soils. The uptake by grass decreased the leaching of fertilizer ions in surface layer, particularly for NO3-N. Soil total N and exchangeable K, Ca and Mg in the surface layer decreased with leaching and grass uptake during the 2 years without new fertilization of urea, Ca(H2PO4)2, KCl, CaCO3 and MgCO3. Ca moved from the application layer (0~5 cm) of fertilizer and accumulated in the 10~30 cm depth in the soils studied except that derived from Quaternary red clay. The deficiency of soil exchangeable K will become a serious degradation process facing the Southeast China.
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| 关 键 词： | 红壤 营养成分 淋溶作用 分布规律 中国 云贵高原 长江流域 |
Leaching and redistribution of nutrients in surface layer of red soils in Southeast China |
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| SUN Bo,ZHANG Tao-Lin,ZHAO Qi-Guo.Leaching and redistribution of nutrients in surface layer of red soils in Southeast China[J].Pedosphere,2000,10(2):135-142. |
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| Authors: | SUN Bo ZHANG Tao-Lin and ZHAO Qi-Guo |
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| Institution: | Institute of Soil Science, the Chinese Academy of Sciences, P.O. Box 821, Nanjing 210008 (China);Institute of Soil Science, the Chinese Academy of Sciences, P.O. Box 821, Nanjing 210008 (China);Institute of Soil Science, the Chinese Academy of Sciences, P.O. Box 821, Nanjing 210008 (China) |
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| Abstract: | The leaching and redistribution of nutrients in the surface layer of 4 types of red soils in Southeast China were studied with a lysimeter experiment under field conditions. Results showed that the leaching concentrated in the rainy season (from April to June). Generally, the leaching of soil nutrients from the surface layer of red soils was in the order of Ca ＞ Mg ＞ K ＞ NO3-N. In fertilization treatment, the total amount of soil nutrients leached out of the surface layer in a red soil derived from granite was the highest in all soils. The uptake by grass decreased the leaching of fertilizer ions in surface layer, particularly for NO3-N. Soil total N and exchangeable K, Ca and Mg in the surface layer decreased with leaching and grass uptake during the 2 years without new fertilization of urea, Ca(H2PO4)2, KCl, CaCO3 and MgCO3. Ca moved from the application layer (0～5 cm) of fertilizer and accumulated in the 10～30 cm depth in the soils studied except that derived from Quaternary red clay. The deficiency of soil exchangeable K will become a serious degradation process facing the Southeast China. |
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| Keywords: | leaching nutrients red soils redistribution Southeast China |
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