4.7 Article

Evaluation of Airborne HySpex and Spaceborne PRISMA Hyperspectral Remote Sensing Data for Soil Organic Matter and Carbonates Estimation

期刊

REMOTE SENSING
卷 15, 期 4, 页码 -

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MDPI
DOI: 10.3390/rs15041106

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remote sensing; imaging spectroscopy; satellite; airborne; organic carbon; soil spectroscopy; spectral modeling

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Remote sensing and soil spectroscopy techniques are valuable for estimating soil properties. This study validated the performance of laboratory and imaging spectroscopy sensors in estimating soil organic matter and calcium carbonate content. The results demonstrate the potential of using these techniques for quantitative predictions of soil properties at larger scales.
Remote sensing and soil spectroscopy applications are valuable techniques for soil property estimation. Soil organic matter (SOM) and calcium carbonate are important factors in soil quality, and although organic matter is well studied, calcium carbonates require more investigation. In this study, we validated the performance of laboratory soil spectroscopy for estimating the aforementioned properties with referenced in situ data. We also examined the performance of imaging spectroscopy sensors, such as the airborne HySpex and the spaceborne PRISMA. For this purpose, we applied four commonly used machine learning algorithms and six preprocessing methods for the evaluation of the best fitting algorithm.. The study took place over crop areas of Amyntaio in Northern Greece, where extensive soil sampling was conducted. This is an area with a very variable mineralogical environment (from lignite mine to mountainous area). The SOM results were very good at the laboratory scale and for both remote sensing sensors with R-2 = 0.79 for HySpex and R-2 = 0.76 for PRISMA. Regarding the calcium carbonate estimations, the remote sensing accuracy was R-2 = 0.82 for HySpex and R-2 = 0.36 for PRISMA. PRISMA was still in the commissioning phase at the time of the study, and therefore, the acquired image did not cover the whole study area. Accuracies for calcium carbonates may be lower due to the smaller sample size used for the modeling procedure. The results show the potential for using quantitative predictions of SOM and the carbonate content based on soil and imaging spectroscopy at the air and spaceborne scales and for future applications using larger datasets.

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