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典型毛乌素沙漠-黄土高原过渡带土壤盐渍化空间异质性及其影响因素

赵宣 郝起礼 孙婴婴

应用生态学报2017,Vol.28Issue(6):1761-1768,8.
应用生态学报2017,Vol.28Issue(6):1761-1768,8.DOI:10.13287/j.1001-9332.201706.034

典型毛乌素沙漠-黄土高原过渡带土壤盐渍化空间异质性及其影响因素

Spatial heterogeneity of soil salinization and its influencing factors in the typical region of the Mu Us Desert-Loess Plateau transitional zone, Northwest China

赵宣 1郝起礼 2孙婴婴3

作者信息

  • 1. 陕西省土地工程建设集团有限责任公司,西安710075
  • 2. 陕西地建土地工程技术研究院有限责任公司,西安710075
  • 3. 国土资源部退化及未利用土地整治工程重点实验室,西安710075
  • 折叠

摘要

Abstract

Studies on the spatial heterogeneity of saline soil in the Mu Us Desert-Loess Plateau transition zone are meaningful for understanding the mechanisms of land desertification.Taking the Mu Us Desert-Loess Plateau transition zone as the study subject,its spatial heterogeneity of pH,electrical conductivity (EC) and total salt content were analyzed by using on-site sampling followed with indoor analysis,classical statistical and geostatistical analysis.The results indicated that:1)The average values of pH,EC and total salt content were 8.44,5.13 mS · em-1 and 21.66 g · kg-1,respectively,and the coefficient of variation ranged from 6.9% to 73.3%.The pH was weakly variable,while EC and total salt content were moderately variable.2) Results of semivariogram analysis showed that the most fitting model for spatial variability of all three indexes was spherical model.The C0/(C0+C) ratios of three indexes ranged from 8.6% to 14.3%,which suggested the spatial variability of all indexes had a strong spatial autocorrelation,and the structural factors played a more important role.The variation range decreased in order of pH <total salt < EC.The Kriging interpolation showed that pH,EC and total salt content distributed in a striped pattern with good continuity.The pH value increased with increasing terrain slope,while EC and total salt content decreased.3) In terms of vertical distribution,the salt aggregated on surface in the area with severe salinization.In the area with light salinization,the vertical distribution of salinity was firstly decreased and then increased.In general,the heterogeneity of soil salinization in the Mu Us DesertLoess Plateau transition zone was influenced by climate,landscape,plant distribution,especially affected by geological conditions,topography and hydrogeological conditions.This study provided a theoretical basis for future land engineering and ecosystem restoration programs.

关键词

毛乌素沙漠-黄土高原过渡带/土壤盐渍化/空间异质性/影响因素

Key words

Mu Us desert-loess plateau transition zone/soil salinization/spatial heterogeneity/influencing factors

引用本文复制引用

赵宣,郝起礼,孙婴婴..典型毛乌素沙漠-黄土高原过渡带土壤盐渍化空间异质性及其影响因素[J].应用生态学报,2017,28(6):1761-1768,8.

基金项目

本文由陕西省重点科技创新团队计划项目(2016KCT-23)资助 This work was supported by the Science and Technology Innovation Team Program of Shaanxi Province (2016KCT-23). (2016KCT-23)

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