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利用土壤近红外光谱特征测量土壤含水量

[Measuring soil water content by using near infrared spectral characteristics of soil].

作者信息

Li Mei-ting, Wu Hong-qi, Jiang Ping-an, Lu Xiang-jun, Fu Yan-bo

机构信息

College of Pratacultural & Environmental Science, Xinjiang Agricultural University, Urumqi, China.

出版信息

Guang Pu Xue Yu Guang Pu Fen Xi. 2012 Aug;32(8):2117-21.

Abstract

Different textured soils (sandy loam, silty clay loam and clay) from Manas County, Xinjiang were researched with indoor spectral reflectance, continuum removal was used to process soil spectra curve, and correlation analysis was made about normalized spectral reflectance and water content for modeling. The results show that different textured soils have reflectance in a order that clay>silty clay loam>sandy loam; the critical points of field capacity in sandy loam, silty clay loam and clay were 20.01%, 24.10% and 30.43% respectively, and water content was inversely proportional to spectral reflectance below such critical points while proportional above the points. Within 1390-1623 nm band, the negative correlation coefficients of soil water content and normalized spectra reflectance show better negative correlation and reaching significant levels, R2 of the model established for soil water content prediction exceeded mostly 0.8, and the average relative error of the model was 10%. The model could accurately reflect the soil moisture content, Its advantages such as accuracy, non-destruction and rapidness provide a new approach to measuring soil water content.

摘要

对新疆玛纳斯县不同质地土壤(砂壤土、粉质粘壤土和粘土)进行室内光谱反射率研究,采用连续统去除法处理土壤光谱曲线,并对归一化光谱反射率与含水量进行相关性分析以建立模型。结果表明,不同质地土壤的反射率顺序为粘土>粉质粘壤土>砂壤土;砂壤土、粉质粘壤土和粘土的田间持水量临界点分别为20.01%、24.10%和30.43%,低于该临界点时含水量与光谱反射率呈反比,高于该临界点时呈正比。在1390 - 1623nm波段内,土壤含水量与归一化光谱反射率的负相关系数呈现出较好的负相关性且达到显著水平,建立的土壤含水量预测模型R2大多超过0.8,模型平均相对误差为10%。该模型能够准确反映土壤含水量,其具有的准确性、无损性和快速性等优点为测量土壤含水量提供了一种新途径。

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