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长期施用钾肥对草甸土钾素形态的影响
引用本文:谭德水,金继运,黄绍文,汪仁,孙文涛. 长期施用钾肥对草甸土钾素形态的影响[J]. 中国土壤与肥料, 2007, 0(3): 52-54
作者姓名:谭德水  金继运  黄绍文  汪仁  孙文涛
作者单位:1. 中国农业科学院农业资源与农业区划研究所/农业部植物营养与养分循环重点实验室,北京,100081
2. 辽宁省农业科学院环境资源与农村能源研究所,辽宁,沈阳,110161
基金项目:中国-加拿大钾磷研究所合作项目
摘    要:通过连续13年的钾肥定位试验,研究了施钾对草甸土耕层土壤钾素各形态含量和比例的影响。结果表明,长期施用钾肥较不施钾处理可以增加耕层土中水溶性钾、非特殊吸附钾、特殊吸附钾、非交换性钾的含量和在全钾中的比例,施钾量增加促进了这种状况,同时降低了矿物钾在全钾中的比例。随土层加深,大部分处理的水溶性钾、非特殊吸附钾、特殊吸附钾和非交换性钾含量和比例随之降低,而矿物钾和全钾含量相应处理却随之升高,其中施钾处理的效果明显。

关 键 词:长期施钾  草甸土  钾素形态
文章编号:1673-6257(2007)03-0052-03
修稿时间:2006-03-28

Effect of long-term K application on potassium forms in meadow soil
TAN De-shui,JIN Ji-yun,HUANG Shao-wen,WANG Ren,SUN Wen-tao. Effect of long-term K application on potassium forms in meadow soil[J]. Soil and Fertilizer Sciences, 2007, 0(3): 52-54
Authors:TAN De-shui  JIN Ji-yun  HUANG Shao-wen  WANG Ren  SUN Wen-tao
Affiliation:1.Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences/Key Laboratory of Plant Nutrition Cychng, Ministry of Agriculture, Beijing 100081 ; 2. Researth Institute of Environmental Resource and Rural Energy Resource, Liaoning Academy of Agricultural Science, Shenyang 110161
Abstract:Based on the long - term field experiment of K application on meadow soil, the effect of K fertilizer apphcation on the content and proportion of K was discussed. The result showed that long - term K application could increase the content and proportion of water - soluble K, non - specially adsorbed K, specially adsorbed K, non - exchangeable K in the plough layer, and decrease the proportion of mineral K in the same time. Along with the layer going to deeper, the content and proportion of water- soluble K, non - specially adsorbed K, specially adsorbed K, non - exchangeable K in most treatments decreased, and the effect was more distinct in the treatments of K application, but mineral K and total K behaved the opposite result. K fertilizer application could increase corn grain yield remarkably.
Keywords:long- term K application   meadow soil   potassium form
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