论光学领域基于物理的土壤含水量估算模型的解析性、可解释性和预测能力

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
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引用次数: 0

摘要

土壤水分在地表-大气界面的蒸腾、蒸发和植物生长过程中发挥着重要作用。光学遥感在检索地表土壤水分含量(SMC)方面具有巨大潜力,许多经验数据驱动模型或物理模型都是为解决这一问题而开发的。然而,大多数数据驱动模型都面临着可解释性差的挑战,而许多现有物理模型的应用则受到复杂校准步骤的限制。这项工作的目的是验证基于库贝尔卡-蒙克(KM)辐射传递理论的物理方法的潜力,以便在 SMC 光学估算的物理意义和实际适用性之间取得平衡。具体而言,在实验室条件下,利用中国江汉平原的一个充足的异质土壤数据集对该模型进行逐波长校准。该方法(在最佳波段)的性能与几种常用方法进行了比较。通过验证模型在不同 SOM 水平子集之间的可移植性,研究了土壤有机质(SOM)对 SMC 估算的影响。结果表明,在该方法的全波段分析中,1460 nm 和 1940 nm 附近有两个局部最优波段,1940 nm 附近的性能优于或相当于线性回归、对数回归和光谱指数模型。虽然偏最小二乘回归(PLSR)可以通过丰富波段信息获得更高的预测精度,但这种方法在单波段校准的模型简约性、模型的可解释性以及物理机制和预测能力之间取得了平衡,因而脱颖而出。更重要的是,我们发现该方法可以提高水吸收区的光谱灵敏度,避免低 SMC 时的负预测,并减少 SOM 对 SMC 估计的干扰效应,这可能是由于该方法内部的物理约束。本文证明了基于物理的方法在 SMC 光学估算中的解析性、可解释性和预测能力,并为该方法在机载/卫星假想光谱传感 SMC 中的应用提供了新的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

On the parsimony, interpretability and predictive capability of a physically−based model in the optical domain for estimating soil moisture content

On the parsimony, interpretability and predictive capability of a physically−based model in the optical domain for estimating soil moisture content

Soil moisture plays an important role in the transpiration, evaporation and plant growth processes at the land surface-atmosphere interface. Optical remote sensing has great potential for the retrieval of surface soil moisture content (SMC), with many empirical data-driven models or physical models developed to address this issue. Nevertheless, most data-driven models face the challenge of poor interpretability, while the application of many existing physical models is limited by complicated calibration steps. The aim of this work is to validate the potential of a physically-based approach based on the Kubelka-Munk (KM) radiative transfer theory to strike a balance between physical significance and practical applicability in the optical estimation of SMC. Specifically, an adequate and heterogeneous soil dataset in Jianghan Plain, China was used to calibrate the model wavelength by wavelength under laboratory conditions. The performance of the approach (at the optimal band) was compared with several commonly used methods. The effect of soil organic matter (SOM) on the estimation of SMC was also investigated by validating the model transferability between subsets with different SOM levels. Results showed that there were two local optimal bands at around 1460 and 1940 nm in the full band analysis of the approach, and the performance at around 1940 nm is better or comparable to linear regression, logarithmic regression, and spectral index models. Although partial least squares regression (PLSR) could achieve higher prediction accuracy with the enrichment of band information, this approach stood out for its balance of model parsimony with single-band calibration, model interpretability with the incorporation of physical mechanisms and predictive capability. More importantly, we found that the approach could enhance the spectral sensitivity in the water absorption region, avoid negative predictions at low SMCs, and reduce the interference effect of SOM on the estimation of SMC, probably due to the physical constraints inside the approach. This paper demonstrates the parsimony, interpretability, and predictive capability of the physically-based approach in the optical estimation of SMC, and provides new insights into the application of this approach in the airborne/satellite imaginary spectroscopy sensing of SMC.

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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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