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An Empirical Method for Soil Salinity and Moisture Inversion in West of Jilin

机译:吉林西部土壤盐度和水分反演的实证方法

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Soil salinization has been known as a world wide problem. It is a chemical process that causes soil degradation particularly in arid and semi-arid agriculture region. There both advantages and disadvantages of optical and microwave remote sensing in the recognition of salinization soil. In order to retrieve both soil salinity and moisture, an empirical method is presented in this paper which is combined optical, microwave remote sensing and ground-based data. Based on the analysis of the relationship between SAR backscatter, NDVI and soil salinity and moisture, a multiple linear regression is used. The RMSE of soil salinity and moisture are 3.175 g/Kg and 3.169% respectively. The results demonstrate that combing microwave and optical remote sensing are suitable for inversion salinity and moisture content in salinization soil, however, methods based on theory knowledge need to be proposed in further research.
机译:土壤盐渍化被称为世界各地的问题。它是一种尤其导致土壤退化,特别是在干旱和半干旱农业区的化学过程。盐化土识别中的光学和微波遥感的优缺点。为了检索土壤盐度和水分,本文提出了一种经验方法,其是光学,微波遥感和基于地面数据的组合。基于分析SAR后散射,NDVI和土壤盐度与水分的关系,使用多元线性回归。土壤盐度和水分的RMSE分别为3.175克/千克和3.169%。结果表明,梳理微波和光学遥感是适用于盐渍化土壤中的反转盐度和水分含量,但是需要在进一步研究中提出基于理论知识的方法。

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