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Predicting water content using linear spectral mixture model on soil spectra

机译:在土壤光谱上使用线性光谱混合模型预测含水量

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摘要

Remote sensing has been widely applied for soil moisture estimation. However, such estimates become difficult to obtain and can be inaccurate when applied to complex earth surfaces with more than one soil type because of the interference of spectral signals from different soil components. This study aims to develop a moisture prediction method that is insensitive to soil types;;this is based on in situ samples collected from an intertidal zone in Jiangsu Province in China and on laboratory measurements of soil spectra. The results demonstrate that for a reflectance-based method, moisture content is closely related to reflectance on the three wavebands centered at 2143, 1760, and 742 nm for four types of soil (sand, silty sand, sandy silt, and silt) considered separately;;the relationship is not close if all soil types are mixed together (R~2 = 0.77). To develop the desired model, a linear spectral mixture model (LSMM) was employed to extract parameter water abundance (Wa: information on soil water content) in advance, while eliminating redundant information from other soil components. Wa has a relatively higher correlation (R~2 = 0.82) than reflectance with moisture content for a mixed soil type. Thus, employing the LSMM helps realize a practical water content estimation model for predicting moisture over complex earth surfaces, because it has the potential of eliminating spectral effects from soil components.
机译:遥感已广泛应用于土壤水分的估算。然而,由于来自不同土壤成分的光谱信号的干扰,这样的估计变得难以获得并且当应用于具有一种以上土壤类型的复杂地球表面时可能是不准确的。这项研究的目的是开发一种对土壤类型不敏感的水分预测方法;该方法基于从中国江苏省潮间带采集的原位样品和土壤光谱的实验室测量结果。结果表明,对于基于反射率的方法,对于分别考虑的四种类型的土壤(砂,粉砂,粉沙和粉沙),水分含量与以2143、1760和742 nm为中心的三个波段的反射率密切相关。 ;;如果将所有土壤类型混合在一起,则关系不紧密(R〜2 = 0.77)。为了建立所需的模型,采用线性光谱混合模型(LSMM)预先提取参数水丰度(Wa:有关土壤水分的信息),同时从其他土壤成分中消除多余的信息。与混合土壤类型的水分含量相比,Wa具有相对较高的相关性(R〜2 = 0.82)。因此,采用LSMM有助于实现一种实用的含水量估算模型,以预测复杂地球表面的水分,因为它具有消除土壤成分光谱影响的潜力。

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