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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Soil organic carbon assessment by field and airborne spectrometry in bare croplands: accounting for soil surface roughness.
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Soil organic carbon assessment by field and airborne spectrometry in bare croplands: accounting for soil surface roughness.

机译:通过田间和空气传播光谱法对裸露农田的土壤有机碳进行评估:考虑到土壤表面粗糙度。

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Visible, Near and Short Wave Infrared (VNSWIR) diffuse reflectance spectroscopy (350 nm to 2500 nm) has been proven to be an efficient tool to determine the Soil Organic Carbon (SOC) content. SOC assessment (SOCa) is usually done by using calibration samples and multivariate models. However one of the major constraints of this technique, when used in field conditions is the spatial variation in surface soil properties (soil water content, roughness, vegetation residue) which induces a spectral variability not directly related to SOC and hence reduces the SOCa accuracy. This study focuses on the impact of soil roughness on SOCa by outdoor VIS-NIR-SWIR spectroscopy and is based on the assumption that soil roughness effect can be approximated by its related shadowing effect. A new method for identifying and correcting the effect of soil shadow on reflectance spectra measured with an Analytical Spectral Devices (ASD) spectroradiometer and an Airborne Hyperspectral Sensor (AHS-160) on freshly tilled fields in the Grand Duchy of Luxembourg was elaborated and tested. This method is based on the shooting of soil vertical photographs in the visible spectrum and the derivation of a shadow correction factor resulting from the comparison of "reflectance" of shadowed and illuminated soil areas. Moreover, the study of laboratory ASD reflectance of shadowed soil samples showed that the influence of shadow on reflectance varies according to wavelength. Consequently a correction factor in the entire [350-2500 nm] spectral range was computed to translate this differential influence. Our results showed that SOCa was improved by 27% for field spectral data and by 25% for airborne spectral data by correcting the effect of soil relative shadow. However, compared to simple mathematical treatment of the spectra (first derivative, etc.) able to remove variation in soil albedo due to roughness, the proposed method, leads only to slightly more accurate SOCa.
机译:可见,近红外和短波红外(VNSWIR)漫反射光谱(350 nm至2500 nm)已被证明是确定土壤有机碳(SOC)含量的有效工具。 SOC评估(SOCa)通常是通过使用校准样本和多元模型来完成的。但是,在田间条件下使用时,此技术的主要限制之一是表层土壤特性(土壤含水量,粗糙度,植被残留)的空间变化,这会导致与SOC不直接相关的光谱变化,从而降低SOCa精度。这项研究的重点是室外VIS-NIR-SWIR光谱法对土壤粗糙度对SOCa的影响,并基于这样的假设,即土壤粗糙度效应可以通过其相关的阴影效应来近似。阐述并测试了一种新方法,该方法用于识别和校正土壤阴影对反射光谱的影响,该反射光谱是使用分析光谱仪(ASD)光谱辐射仪和机载高光谱传感器(AHS-160)在卢森堡大公国的新鲜耕地上测量的。该方法基于可见光谱中的土壤垂直照片的拍摄,以及通过对阴影和照明土壤区域的“反射率”进行比较而得出的阴影校正因子的推导。此外,对阴影土壤样品的实验室ASD反射率的研究表明,阴影对反射率的影响随波长而变化。因此,计算了整个[350-2500 nm]光谱范围内的校正因子,以消除这种差异影响。我们的结果表明,通过校正土壤相对阴影的影响,现场光谱数据的SOCa改善了27%,空中光谱数据的SOCa改善了25%。但是,与能够消除由于粗糙度引起的土壤反照率变化的光谱(一阶导数等)的简单数学处理相比,所提出的方法只能使SOCa稍微精确一些。

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