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Prediction of Soil Moisture Content and Soil Salt Concentration from Hyperspectral Laboratory and Field Data

机译:利用高光谱实验室和野外数据预测土壤水分和盐分含量

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This research examines the simultaneous retrieval of surface soil moisture and salt concentrations using hyperspectral reflectance data in an arid environment. We conducted laboratory and outdoor field experiments in which we examined three key soil variables: soil moisture, salt and texture (silty loam, clay and silty clay). The soil moisture content models for multiple textures (M_SMC models) were based on selected hyperspectral reflectance data located around 1460, 1900 and 2010 nm and resulted in R2 values higher than 0.933. Meanwhile, the soil salt concentrations were also accurately (R2 0.748) modeled (M_SSC models) based on wavebands located at 540, 1740, 2010 and 2350 nm. When the different texture samples were mixed (SL + C + SC models), soil moisture was still accurately retrieved (R2 = 0.937) but the soil salt not as well (R2 = 0.47). After stratifying the samples by retrieved soil moisture levels, the R2 of calibrated M_SSCSMC models for soil salt concentrations improved to 0.951. This two-step method also showed applicability for analyzing soil-salt samples in the field. The M_SSCSMC models resulted in R2 values equal to 0.912 when moisture is lower than 0.15, and R2 values equal to 0.481 when soil moisture is between 0.15 and 0.2.
机译:这项研究研究了在干旱环境中使用高光谱反射率数据同时检索地表土壤水分和盐分的浓度。我们进行了实验室和室外田间试验,在其中我们研究了三个关键的土壤变量:土壤湿度,盐分和质地(粉质壤土,黏土和粉质黏土)。基于多种纹理的土壤水分含量模型(M_SMC模型)基于选定的位于1460、1900和2010 nm附近的高光谱反射率数据,得出的R 2 值高于0.933。同时,基于位于540、1740、2010和2350 nm的波段,还准确地(R_sup> 2 = 0.937),但土壤盐分却不那么理想(R 2 = 0.47)。通过取回的土壤水分含量对样品进行分层后,校正后的M_SSC SMC 模型的土壤盐分浓度的R 2 提高至0.951。这种分两步的方法还显示了在现场分析土壤盐样品的适用性。 M_SSC SMC 模型在水分低于0.15时得出R 2 值等于0.912,而土壤水分时R 2 值等于0.481介于0.15和0.2之间。

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