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长期施肥对棕壤矿物吸附点位钾有效性及其剖面分布的影响
引用本文:李娜,韩晓日,杨劲峰,刘宁,李巧宁,房大伟.长期施肥对棕壤矿物吸附点位钾有效性及其剖面分布的影响[J].植物营养与肥料学报,2012,18(6):1413-1418.
作者姓名:李娜  韩晓日  杨劲峰  刘宁  李巧宁  房大伟
作者单位:1.沈阳农业大学土地与环境学院,土壤肥料资源高效利用国家工程实验室,农业部东北玉米营养与施肥科学观测试验站,辽宁沈阳 110866
基金项目:国家自然科学基金,国家科技支撑计划
摘    要:运用连续提取法结合常规方法,研究玉米玉米大豆轮作条件下,经过31年不同施肥后棕壤矿物吸附的p位钾、 e位钾和i位钾的有效性及其剖面分布情况。结果表明: 耕层土壤各位点钾含量及占全钾比例均表现为i位>e位>p位; 长期单施化学钾肥或不施钾各位点钾含量降低,有机肥配施化肥可以维持土壤中各位点钾含量。相关分析表明,交换性钾与p位和e位钾相关性显著,相关系数分别为0.926*和0.886*; 植株地上部吸钾量与p和e位钾呈显著正相关关系,与i位钾呈极显著正相关关系(r=0.963**); 不同位点间钾含量呈极显著正相关关系。在剖面分布中,p、 e和i位钾含量均表现为020 cm>2040 cm。

关 键 词:长期施肥    棕壤    吸附位点钾    表观平衡    有效性    剖面分布
收稿时间:2012-03-16

Effects of long-term fertilization on the availability of K adsorbed by clay minerals and profile distribution in brown soil
LI Na HAN Xiao-ri YANG Jin-feng liu ning LI Qiao-ning FANG Da-wei.Effects of long-term fertilization on the availability of K adsorbed by clay minerals and profile distribution in brown soil[J].Plant Nutrition and Fertilizer Science,2012,18(6):1413-1418.
Authors:LI Na HAN Xiao-ri YANG Jin-feng liu ning LI Qiao-ning FANG Da-wei
Institution:1.College of Land and Environment,Shenyang Agricultural University/National Engineering Laboratory of High Efficient Use on Soil and Fertilizer Resources/Experiment Station of Northeast Maize Nutrition and Fertilization,Ministry of Agriculture,Shenyang 110866,China
Abstract:The sequential extractions combined with conventional methods were used to study the availability of K adsorbed by clay minerals and the profile distribution under long term fertilization of brown soil, with a maize maize soybean rotation. Results showed that the contents of K and the proportion in total K on arable layer presented as follows:  i>e>p. Contents of p, e and i sites K with chemical K fertilizer application and no K fertilizer application decreased. And organic manure with K fertilizer application could remain the amount of K at a higher level. Correlation analysis indicated positive correlation between p site K,  e site K and exchangable K, and the correlation coefficient were 0.926*and 0.886*, respectively. A positive significant correlation was observed between p site K, e site K and the uptake of K by crops. And there was a highly significant correlation between i sites and the uptake of K by crops (r=0.963**). There was an extremely significant positive correlation among p site K, e site K and i site K. The tendency of contents of potassium were all changed with depth as follows:  0-20 cm>20-40 cm.
Keywords:long-term fertilization  brown soil  K adsorbed by clay minerals  apparent balance  availability  profile distribution
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