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[中国西北毛乌素沙漠-黄土高原过渡带典型区域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].

作者信息

Zhao Xuan, Hao Qi Li, Sun Ying Ying

机构信息

Shaanxi Provincial Land Engineering Construction Group Co, Ltd, Xi'an 710075, China.

Institute of Shaanxi Land Engineering and Technology Co, Ltd, Xi'an 710075, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2017 Jun 18;28(6):1761-1768. doi: 10.13287/j.1001-9332.201706.034.

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·cm and 21.66 g·kg, 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 C/(C+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 Desert-Loess 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.

摘要

对毛乌素沙漠-黄土高原过渡区盐碱土空间异质性的研究,对于理解土地沙漠化机制具有重要意义。以毛乌素沙漠-黄土高原过渡区为研究对象,采用现场采样并结合室内分析、经典统计分析和地统计分析的方法,对其pH值、电导率(EC)和总盐含量的空间异质性进行了分析。结果表明:1)pH值、EC值和总盐含量的平均值分别为8.44、5.13 mS·cm和21.66 g·kg,变异系数在6.9%至73.3%之间。pH值变异较弱,而EC值和总盐含量变异中等。2)半变异函数分析结果表明,三个指标空间变异性的最优拟合模型均为球状模型。三个指标的C/(C+C)比值在8.6%至14.3%之间,表明各指标的空间变异性具有较强的空间自相关性,且结构因素起更重要作用。变异范围按pH<总盐<EC的顺序减小。克里金插值显示,pH值、EC值和总盐含量呈条带状分布,连续性较好。pH值随地形坡度增加而升高,而EC值和总盐含量则降低。3)在垂直分布方面,重度盐碱化区域盐分在地表聚集。轻度盐碱化区域,盐分垂直分布先降低后升高。总体而言,毛乌素沙漠-黄土高原过渡区土壤盐碱化的异质性受气候、地貌、植物分布影响,尤其受地质条件、地形和水文地质条件影响。本研究为未来土地工程和生态系统恢复项目提供了理论依据。

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