首页|黄河下游冲积平原土壤水带土体质地空间变异特征研究

黄河下游冲积平原土壤水带土体质地空间变异特征研究

Spatial Variability of Soil Water Zone Texture in the Alluvial Plain of the Lower Reaches of the Yellow River

扫码查看
选择河南省开封市兰考县中部闫楼乡作为研究区,运用经典统计学、地统计学与Voxler相结合的方法,研究土壤水带土体质地的空间变异性和分布规律.结果表明:研究区土壤水带不同土体颗粒的空间变异性具有显著差异,变异性强度为砂粒>黏粒>粉粒,且土体质地的空间变异性强度随土壤水带深度增加而增大.土壤水带砂、粉、黏粒的空间相关程度不同,空间相关性强度黏粒>砂粒>粉粒.土壤水带中,砂粒在浅层的空间分布最优模型为高斯模型,在中层和深层为球状模型;粉粒在浅层和中层的空间分布最优模型均为高斯模型;黏粒的空间分布最优模型在浅层和深层的为球状模型,中层为高斯模型.
This study elucidated the spatial variability of heterogeneous soil texture in the soil water zone combining the classical statistics,geostatistics and Voxler method for a real-world field in the Yan-lou Township of the middle of Lankao County,Kaifeng City,Henan Province.The results showed that the spatial variability of different soil particles in the soil water zone in the study area was significantly different,and the variability intensity was sand>clay>silt,and the spatial variability intensity of soil tex-ture increased with depth of soil water zone increasing.The spatial correlation degree of sand,silt and clay in soil water zone was different,and the spatial correlation strength was clay>sand>silt.In the soil water zone,the optimal distribution model of sand in the shallow layer is Gaussian model,and the optimal distribution model in the middle and deep layer is spherical model.The optimal models of particle spatial distribution in shallow and middle layers are Gaussian models.The optimal distribution model of clay par-ticles is the spherical model in the shallow layer and deep layer,Gaussian model in the middle layer.

alluvial plain of Yellow Riversoil water zonegeostatisticsspatial variation

王琳、潘登、关健、刘丽丽

展开 >

河南省自然资源监测和国土整治院,河南 郑州 450046

河南省自然资源科技创新中心(地下水资源调查监测研究),河南 郑州 450046

华北水利水电大学,河南 郑州 450046

黄河冲积平原 土壤水带 地统计学 空间变异

国家自然科学基金资助项目河南省自然资源厅2019年度省自然资源科研项目

42202266201937913

2024

河北工程大学学报(自然科学版)
河北工程大学

河北工程大学学报(自然科学版)

CSTPCD
影响因子:0.543
ISSN:1673-9469
年,卷(期):2024.41(4)