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Soil Salt Content and Its Relationship with Crops and Groundwater Depth in the Yinchuan Plain (China) Using Remote Sensing

机译:银川平原(中国)土壤盐分含量及其与作物和地下水深度的关系

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摘要

Soil salt content and its relationships with crops and water table depth were investigated in this study by using remote sensing techniques and field measurements in the Yinchuan plain of China. Moderate Resolution Imaging Spectroradiometer-Normalized Difference Vegetation Index (MODIS NDVI) was used as an indicator of crop development, field samples were analyzed fa: soil salt content, and observation wells provided water table data. Comparison of crop development defined from NDVI to soil salt values indicated that crop may develop well when the surface soil salt content is lower than 0.5 g/kg. Its growth is restricted when the soil salt content is between 0.5 and 4 g/kg, and little crop growth occurs when the soil salt content is greater than 4 g/kg. Comparison of soil salinity and water table depth in the beginning of the growing season showed, that areas with water table depth between 0.9 m and 3 m are the most affected by soil salinization. This information is crucial for the optimal control of drainage and irrigation in this important cropping region of China.
机译:本研究利用遥感技术和田间测量技术,研究了中国银川平原土壤盐分含量及其与作物和地下水位的关系。中分辨率成像光谱仪-归一化植被指数(MODIS NDVI)被用作作物生长的指标,对田间样品进行了分析:土壤盐分含量,并且观察井提供了地下水位数据。从NDVI定义的作物生长与土壤盐分值的比较表明,当表层土壤盐分含量低于0.5 g / kg时,作物可能生长良好。当土壤盐含量在0.5至4 g / kg之间时,其生长受到限制,而当土壤盐含量大于4 g / kg时,几乎没有作物生长。生长季节开始时土壤盐分和地下水位深度的比较表明,地下水位在0.9 m至3 m之间的区域受土壤盐碱化影响最大。这些信息对于在这个重要的农作物地区优化控制排水和灌溉至关重要。

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