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THE SPATIAL PATTERN CHARACTERISTICS OF SOIL NUTRIENTS AT THE FIELD SCALE

机译:田间土壤养分的空间分布特征。

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This paper took the wheat field of typical alluvial soil area as the research site,aimed to explore the spatial pattern of the soil nutrients, such as soil available potassium, soil available phosphorus, soil organic matter (SOM) and soil alkali hydrolysable nitrogen. With the help of DGPS, a total of 104 topsoil(0-20cm) samples were collected. Based on classical statistics, research results indicated the average content of soil available potassium was 287.476g/kg, the high value was 483.433g/kg, the low value was 119.435g/kg. The average content of soil available phosphorus was 54.228g/kg, the high value was 293.13g/kg, the low value was 18.77g/kg. The average content of SOM was 36.901g/kg, the high value was 47.420g/kg, the low value was 21.110g/kg. The average content of soil alkali hydrolysable nitrogen was 66.444g/kg, the high value was 166.474g/kg, the low value was 29.846g/kg. Geostatistical analysis, combined with geographical information system(GIS), the range, nugget and sill of soil nutrients characteristics were calculated, semivariogram model was established, ordinary kriging was applied, and the spatial distributing map of soil nutrients was drawn. It is shown that the semivariogram structures of the soil nutrients was spherical, the ratio of nugget/sill of soil available potassium, SOM, soil alkali hydrolysable nitrogen was 0.399, 0.746 and 0.696, respectively, which belonged to the middle intensity, the ratio of nugget/sill of soil available phosphorus was 0.759, which belonged to the low intensity. Spatial variation of soil available potassium was mainly caused by structural factors(parent material, terrain, climate, water table etc.), the structure variability of it took 60.1% of the total variability, the spatial variation of soil available phosphorus, SOM and soil alkaline hydrolysis nitrogen were mainly caused by random factors(fertilization, environmental pollution, cultivation measures, management etc.), the random variability of them took 75.9%, 74.6%, 69.6% of the total variability, respectively, the spatial correlation distance of SOM, soil alkaline hydrolysis nitrogen, soil available potassium and soil available phosphorus was 44.898 m, 45.191 m, 57.691 m and 23.328 m, respectively.
机译:本文以典型冲积土壤区的麦田为研究对象, 目的在于探索土壤养分的空间格局,例如土壤速效钾,土壤速效磷,土壤有机质(SOM)和土壤碱解性氮。在DGPS的帮助下,总共收集了104个表土(0-20厘米)样品。根据经典统计,研究结果表明土壤有效钾平均含量为287.476g / kg,最高值为483.433g / kg,最低值为119.435g / kg。土壤有效磷平均含量为54.228g / kg,最高值为293.13g / kg,最低值为18.77g / kg。 SOM的平均含量为36.901g / kg,最高值为47.420g / kg,最低值为21.110g / kg。土壤碱解氮的平均含量为66.444g / kg,最高值为166.474g / kg,最低值为29.846g / kg。地统计学分析,结合地理信息系统(GIS),计算了土壤养分特征的范围,金块和基石,建立了半变异函数模型,应用普通克里金法,绘制了土壤养分的空间分布图。结果表明,土壤养分的半变异函数结构为球形,土壤速效钾,SOM,碱金属可水解氮的块金/基石比分别为0.399、0.746和0.696,属于中等强度。土壤有效磷的金块/基岩为0.759,属于低强度。土壤有效钾的空间变异主要是由结构因素(母体,地形,气候,地下水位等)引起的,其结构变异性占总变异性的60.1%,土壤有效磷,SOM和土壤的空间变异性碱性水解氮主要由随机因素(施肥,环境污染,栽培措施,管理等)引起,它们的随机变异性分别占总变异性的75.9%,74.6%,69.6%,SOM的空间相关距离土壤碱性水解氮,土壤有效钾和土壤有效磷分别为44.898 m,45.191 m,57.691 m和23.328 m。

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