苏干湖湿地土壤全盐含量特征及其与地下水的关联
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国家自然科学基金项目(41461013,41861009)


Characteristics of soil total salt content and its correlation with groundwater in Sugan Lake wetland
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    摘要:

    地下水是内陆盐沼湿地生态水文过程及演变的关键因素,地下水位埋深和水质特征交互作用影响水盐运移过程和表层土壤盐渍化程度。根据2018年8月土壤盐分与地下水特征的监测数据,运用经典统计学、皮尔逊相关性和主成分分析等方法对苏干湖湿地(93°47'53″-94°04'26″E,38°50'07″-38°56'27″N)不同水位下表层0-10 cm土壤全盐含量、地下水水质特征及其间的关系进行定量分析。结果表明:(1)研究区0-10 cm土壤全盐含量的均值为204.41 g/kg,随地下水埋深的增加,土壤全盐含量的均值、变化幅度和变异系数呈先增加后降低的趋势。(2)地下水埋深介于0.17-6 m,pH在7.06-9.56范围,阳离子以Na+为主,阴离子以SO42-和Cl-为主,离子浓度变异系数从强到弱依次为Na+ > Mg2+ > Ca2+ > Cl- > SO42- > HCO3- > K+ > CO32-。(3)关联分析表明,在水埋深<1 m、1-2 m的区域表层全盐含量与地下水埋深呈正相关,地下水埋深介于2-3 m和>3 m的区域两者间呈负相关;土壤全盐含量与地下水水质离子Na+、Mg2+、SO42-、Cl-间呈极显著正相关,与K+、CO32-、HCO3-间的相关系数较低且不显著。内陆盐沼湿地表层土壤全盐含量与地下水埋深、地下水水质特征的关联分析,体现了内陆盐沼湿地土壤水盐运移过程的复杂性。

    Abstract:

    Groundwater is a key factor in the ecological and hydrological process and evolution of inland salt marsh wetlands. The interaction between the depth of groundwater level and the characteristics of water quality affects the process of water and salt migration and the degree of surface soil salinization. Based on the monitoring data of soil salinity and groundwater characteristics in August 2018, classical statistics, Pearson correlation and principal component analysis were used to analyze the total soil salt content of 0-10 cm soil, groundwater quality characteristics of surface soil at different water levels in Sugan Lake wetland (93°47'53″-94°04'26″E, 38°50'07″-38°56'27″N) and they are interrelationships between the total salt content of surface soil 0-10 cm and groundwater quality were quantified and analyzed. The results showed that:(1) The mean value of soil total salt content in 0-10 cm surface layer of Sugan Lake wetland was 204.41 g/kg, and its variation range and variation coefficient were large, and the variation coefficient ≥ 100% belonged to strong variability. The mean value, magnitude of change and coefficient of variation of the total salt content of soil showed a trend of increasing and then decreasing with the increase of groundwater burial depth. (2) The depth of groundwater was between 0.17-6 m, the pH was in the range of 7.06-9.56, the cations were mainly Na+, while the anions were mainly SO42- and Cl-, and the variation of ion concentration from strong to weak was Na+ > Mg2+ > Ca2+ > Cl- > SO42- > HCO3- > K+ > CO32-. (3) Correlation analysis showed that the surface total salt content was positively correlated with groundwater depth in areas with water depth <1 m and 1-2 m, and negatively correlated with water depth between 2-3 m and >3 m. The variation of groundwater depth increases the spatial heterogeneity of topsoil total salt content. Under the action of their physical and chemical properties, evaporation and concentration, leaching and cation adsorption, the correlation between ions and soil salt content were different, The total salt content was significantly positively correlated with Na+, Mg2+, SO42- and Cl-, while the correlation coefficient with K+, CO32- and HCO3- were low and not significant. The correlation analysis of surface soil salt content with groundwater depth and groundwater quality characteristics reflects the complexity of soil water and salt transport process in inland salt marsh wetlands.

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康满萍,赵成章,李群.苏干湖湿地土壤全盐含量特征及其与地下水的关联.生态学报,2022,42(22):9026~9034

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