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Estimation of Soil Moisture Percentage Using LANDSAT-based Moisture Stress Index

机译:基于LANDSAT的水分胁迫指数估算土壤水分百分比。

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The global agronomy community needs quick and frequent information on soil moisture variability and spatial trends in order to maximize crop production to meet growing food demands in a changing climate. However, in situ soil moisture measurement is expensive and labor intensive. Remote sensing based biophysical and predictive regression modeling approach have the potential for efficiently estimating soil moisture content over large areas. The study investigates the use of Moisture Stress Index (MSI) to estimate soil moisture variability in Alabama. In situ data were obtained from Soil Climate Analysis Network (SCAN) sites in Alabama and MSI developed from LANDSAT 8 OLI and LANDSAT 5 TM data. Pearson product moment correlation analysis showed that MSI strongly correlates with 16-day average growing season soil moisture measurements, with negative correlations of -0.519, -0.482 and -0.895 at 5, 10, and 20 cm soil depths respectively. The correlations of MSI and growing season moisture were low at sites where soil moisture was extremely low (<-0.3 at all depths). Simple linear regression model constructed for soil moisture at 20 cm depth (R2=0.79, p<0.05) correlated well with MSI values and was successfully used to estimate soil moisture percentage within a standard error of ± 3. Resulting MSI products were used to successfully produce the spatial distribution of soil moisture percentage at 20 cm depth. The study concludes that MSI is a good indicator of soil moisture conditions, and could be efficiently utilized in areas where in situ soil moisture data are unavailable.
机译:全球农艺学界需要有关土壤水分变异性和空间趋势的快速而频繁的信息,以使作物产量最大化,以满足气候变化带来的不断增长的粮食需求。然而,原位土壤水分测量是昂贵且劳动密集的。基于遥感的生物物理和预测性回归建模方法具有有效估算大面积土壤水分含量的潜力。该研究调查了利用水分胁迫指数(MSI)估算阿拉巴马州土壤湿度的变化。从阿拉巴马州的土壤气候分析网络(SCAN)站点获得原位数据,并从LANDSAT 8 OLI和LANDSAT 5 TM数据开发出MSI。皮尔逊积矩相关分析表明,MSI与16天平均生长季土壤湿度测量值密切相关,在5、10和20 cm土层深度分别为-0.519,-0.482和-0.895负相关。在土壤水分极低的地区(所有深度均<-0.3),MSI与生长季节水分的相关性较低。为20厘米深度(R2 = 0.79,p <0.05)的土壤水分构建的简单线性回归模型与MSI值具有很好的相关性,并成功地用于在±3的标准误差内估算土壤水分百分比。产生20 cm深度土壤水分百分比的空间分布。该研究得出的结论是,MSI是土壤水分状况的良好指标,可以在没有原位土壤水分数据的地区有效利用。

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