Inversion of soil carbon, nitrogen, and phosphorus in the Yellow River Wetland of Shaanxi Province using field in situ hyperspectroscopy

IF 2.1 Q3 SOIL SCIENCE
Leichao Nie, Keying Qu, Lijuan Cui, Xiajie Zhai, Xinsheng Zhao, Yinru Lei, Jing Li, Jinzhi Wang, Rumiao Wang, Wei Li
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引用次数: 0

Abstract

Soil nitrogen and phosphorus are directly related to soil quality and vegetation growth and are, therefore, a common research topic in studies on global climate change, material cycling, and information exchange in terrestrial ecosystems. However, collecting soil hyperspectral data under in situ conditions and predicting soil properties, which can effectively save time, manpower, material resources, and financial costs, have been generally undervalued. Recent optimization techniques have, however, addressed several of the limitations previously restricting this technique. In this study, hyperspectral data were taken from surface soils under different vegetation types in the wetlands of the Shaanxi Yellow River Wetland Provincial Nature Reserve. Through in situ original and first-order differential transformation spectral data, three prediction models for soil carbon, nitrogen, and phosphorus contents were established: partial least squares (PLSR), random forest (RF), and Gaussian process regression (GPR). The R2 and RMSR of the constructed models were then compared to select the optimal model for evaluating soil content. The soil organic carbon, total nitrogen, and total phosphorus content models established based on the first-order differential had a higher accuracy when modeling and during model validation than those of other models. Moreover, the PLSR model based on the original spectrum and the Gaussian process regression model had a superior inversion performance. These results provide solid theoretical and technical support for developing the optimal model for the quantitative inversion of wetland surface soil carbon, nitrogen, and phosphorus based on in situ hyperspectral technology.
利用野外原位高光谱技术反演陕西黄河湿地土壤碳氮磷含量
土壤中的氮和磷与土壤质量和植被生长直接相关,因此是全球气候变化、物质循环和陆地生态系统信息交换研究中的常见研究课题。然而,在原位条件下收集土壤高光谱数据并预测土壤特性,可以有效节省时间、人力、物力和财力成本,但却普遍被低估。不过,最近的优化技术已经解决了以前限制这种技术的一些局限性。在本研究中,高光谱数据取自陕西黄河湿地省级自然保护区不同植被类型下的地表土壤。通过原位原始光谱数据和一阶差分变换光谱数据,建立了土壤碳、氮、磷含量的三个预测模型:偏最小二乘法(PLSR)、随机森林(RF)和高斯过程回归(GPR)。然后对所建模型的 R2 和 RMSR 进行比较,以选择最佳模型来评估土壤含量。与其他模型相比,基于一阶差分法建立的土壤有机碳、全氮和全磷含量模型在建模和模型验证时具有更高的准确性。此外,基于原始光谱的 PLSR 模型和高斯过程回归模型的反演性能更优。这些结果为基于原位高光谱技术建立湿地表层土壤碳、氮、磷定量反演的最优模型提供了坚实的理论和技术支持。
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CiteScore
1.90
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