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晋中盆地典型耕地厚度、土壤养分空间变异
引用本文:乔磊,黄明镜,张吴平,王国芳,任健.晋中盆地典型耕地厚度、土壤养分空间变异[J].中国农学通报,2020,36(1):89-97.
作者姓名:乔磊  黄明镜  张吴平  王国芳  任健
作者单位:1. 山西农业大学资源环境学院,山西太谷 030800;2. 山西省农业科学院旱地农业研究中心,太原 030031
基金项目:山西省重点研发计划重点项目“旱作农田降水资源高效利用技术研究”(201703D211002-2);山西省科技攻关项目“水肥高效利用——山西 省作物种植系统的生命周期水肥评价及其应用”(20130311008-5)。
摘    要:旨在探究旱作区耕地土壤耕层厚度及土壤养分空间格局与变异规律。以晋中盆地典型耕地土壤为研究对象,运用地统计学方法对耕地耕层厚度及土壤养分的空间变异进行分析,土壤养分选取有机质、pH、有效磷、缓效钾4个指标。结果表明:(1)各个指标的空间自相关性都是随着距离的增加而减小;(2)有效磷的半变异函数最优模型为高斯模型,其他指标的最优模型均为指数模型。各指标的块金系数由大到小依次为:有机质>有效磷>pH>耕层厚度>缓效钾;(3)耕层厚度、有效磷均为西北高东南低的空间格局,缓效钾为东北高西南低,有机质为西南高东北低,pH除北洸乡偏低外均偏高。地统计方法能良好地描述土壤性质的空间分布和变异特征,各土壤性质的空间变异过程中随机性与结构性并存,并且随机性均小于50%。

关 键 词:农田土壤  地统计学  莫兰指数  耕层厚度  土壤养分  
收稿时间:2019/8/27 0:00:00
修稿时间:2019/10/21 0:00:00

Thickness and Soil Nutrients of Typical Cultivated Land in Jinzhong Basin: Spatial Variation
Qiao Lei,Huang Mingjing,Zhang Wuping,Wang Guofang,Ren Jian.Thickness and Soil Nutrients of Typical Cultivated Land in Jinzhong Basin: Spatial Variation[J].Chinese Agricultural Science Bulletin,2020,36(1):89-97.
Authors:Qiao Lei  Huang Mingjing  Zhang Wuping  Wang Guofang  Ren Jian
Institution:1. College of Resources and Environment, Shanxi Agricultural University, Taigu Shanxi 030800;2. Dryland Agriculture Research Center, Shanxi Academy of Agricultural Sciences, Taiyuan 030031
Abstract:The paper aims to explore the spatial pattern and spatial variation rule of cultivated land thickness and soil nutrients in drying farming region. Taking typical cultivated soil in Jinzhong basin as the research object, we analyzed the spatial variation of thickness of cultivated layer (TCL) and soil nutrients by geostatistics method, with soil organic matter (SOM), pH, available phosphorus (AP) and slow-effect potassium (SK) as the soil nutrients indexes. The results showed that: (1) the spatial autocorrelation of each index decreased with the increase of distance; (2) the optimum semivariance model of AP was Gaussian model, and the optimum semivariance model of other indexes was exponential model; the ratio of Nugget to Sill of each index was in order from large to small: SOM>AP>pH>TCL>SK; (3) the spatial pattern of TCL and AP had the tendency with higher in southeast and lower in northwest, SK had spatial pattern with higher in northeast and lower in southwest, SOM had spatial pattern with higher in southwest and lower in northeast, pH was high in whole study area except Beiguang. In conclusion, geostatistical method can describe the spatial pattern and variation characteristics of soil properties well; in the process of spatial variation of soil properties, the randomness and structure coexist, and the randomness is less than 50%.
Keywords:cultivated soil  geostatistics  Moran's I  thickness of cultivated layer  soil nutrients  
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