辽宁农田土壤全量养分空间分布(摘要)(英文)

目的]揭示土壤全量养分空间分布的异质性,为农田的科学管理及提高作物产量提供理论依据。方法]秋收后、土壤封冻前,在辽宁省59个农业气象站选择典型农业生态类型,分别于0～20cm和20～40cm进行混合取样,并进行相应的GPS定位。分别分析不同深度土壤全量养分,有机碳和全氮:元素分析仪测定(ElementarⅢ,德国);全磷:Na2CO3熔融-钼锑钪比色;全钾:NaOH熔融-火焰光度计法。利用SPSS13.0对土壤全量养分进行正态分布检验,不满足正态分布的进行对数转换,直至满足正态分布为止。利用SPSS13.0软件将Excel中的经度、纬度、海拔和属性数据转换为dbf格式。利用GIS9.2中的Kriging插值绘图,在ArcMap中将土壤属性的插值图与辽宁省行政区域图叠加,得到全量养分的空间分布图。结果]不同土壤深度全碳、全氮和全磷呈现出东高西低的分布趋势,但全钾在辽西分布较高。土壤表层(0～20cm)全碳、全氮、全磷和全钾含量均高于下层(20～40cm),表现为土壤表层富集的现象。全钾随土壤深度变化量较小,其表层和下层平均含量分别为17.64和17.08g/kg。结论]不同土壤深度全量养分的分布特征为农田管理提供了理论依据。

Spatial Distribution of Soil Total Nutrients of Farmland in Liaoning Province

Objective]The aim was to reveal the spatial distribution characteristics of total nutrients in soil and provide a theoretical basis for farmland management and improvement of crop yield. Method]GIS technique was used to analyze the spatial distribution characteristics of total C,total N,total P and total K for different soil layers in Liaoning Province. Result]The results showed that the content of total C,total N,total P decrease from east to west,but the content of total K was high in north district of Liaoning Province. The content of total C,total N,total P and total K was higher in soil surface （0-20 cm） than the lower （20-40 cm）. Total K varied less with soil depth,and its mean content was respectively 17.64 g/kg and 17.08 g/kg for soil surface and soil lower layer. Conclusion]The results of the distribution of soil total nutrients in different soil layers supplied a theory basis for farmland management.