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    松嫩平原土壤盐碱化地表基质成因研究

    Origin of surface substrate for soil salinization and alkalization in the Songnen Plain

    • 摘要: 为查明松嫩平原土壤盐碱化地表基质成因,文章以松嫩平原松原市为例,使用Sentinel-2多光谱影像,遍历各类常用土壤盐分指数(soil salinity index, SSI)、土壤水分指数(soil water index, SWI)、植被指数(vegetation index, VI),构建最优三维光谱特征模型计算土壤盐碱化指数(soil salinization-alkalization index, SSAI),反演土壤盐碱化状况。通过对盐碱化区域地表水、地下水取样测试盐分离子含量,结合地下水位状况分析盐分离子来源。通过平面格网布点、垂向分层取样的方式开展地表基质调查,取得深部5 m以内不同层位共计2 362个土壤样品pH值和质地测试结果,构建三维地表基质模型。结果显示,遥感反演结果与表层土壤盐分含量拟合呈正相关线性关系(决定系数R2=0.74),研究区表现为小苏打型碱化特征,土壤盐分离子主要来源于地下水,深部多层黏质土壤起到隔水层的作用阻碍了盐分离子随水分的向下渗透运移和稀释,这一地表基质状况是研究区土壤盐碱化的客观成因。

       

      Abstract: To determine the origin of surface substrate for soil salinization and alkalization in the Songnen Plain, this study investigated Songyuan City based on Sentinel-2 multispectral images. Considering various commonly used indices like the soil salinity index (SSI), soil water index (SWI), and vegetation index (VI), this study constructed the optimal 3D spectral feature model to calculate the soil salinization-alkalization index (SSAI) for inversion of the soil salinization-alkalization status. Surface water and groundwater in areas subjected to soil salinization and alkalization were sampled to test their salt ion concentrations, followed by the analysis of salt ion sources according to the groundwater levels. The surface substrate was explored through planar grid layout and vertical stratified sampling. A total of 2 362 soil samples were collected in various layers within a depth of 5 m to test their pH and texture for the construction of a 3D surface substrate model. The results of this study reveal a positive linear correlation between the inversion result of remote sensing data and the topsoil salt content (coefficient of determination: R2=0.74). The study area was characterized by alkalization of sodium bicarbonate, with soil salt ions originating primarily from groundwater. The deep multilayer argillaceous soils acted as an aquiclude to prevent the downward infiltration, migration, and dilution of salt ions along with water. This surface substrate condition serves as the objective cause of soil salinization and alkalization in the study area.

       

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