Spectroscopic measurements and imaging of soil colour for field scale estimation of soil organic carbon

被引:54
作者
Gholizadeh, Asa [1 ]
Saberioon, Mohammadmehdi [2 ]
Rossel, Raphael A. Viscarra [3 ]
Boruvka, Lubos [1 ]
Klement, Ales [1 ]
机构
[1] Czech Univ Life Sci Prague, Fac Agrobiol Food & Nat Resources, Dept Soil Sci & Soil Protect, Kamycka 129, Prague 16500, Czech Republic
[2] Univ South Bohemia Ceske Budejovice, FFPW, South Bohemian Res Ctr Aquaculture & Biodivers Hy, Inst Complex Syst, Zamek 136, Nove Hrady 37333, Czech Republic
[3] Curtin Univ, Sch Mol & Life Sci, Soil & Landscape Sci, Fac Sci & Engn, GPO Box U1987, Perth, WA 6845, Australia
关键词
Soil organic carbon; Soil colour; Colour indices; Digital camera; Spectral VIS imaging; DIFFUSE-REFLECTANCE SPECTROSCOPY; NEAR-INFRARED SPECTROSCOPY; AGRICULTURAL SOILS; TOTAL NITROGEN; PREDICTION; CLASSIFICATION; REGRESSION; TEXTURE; MATTER; SENSITIVITY;
D O I
10.1016/j.geoderma.2019.113972
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Effective measurement and management of soil organic carbon (SOC) are essential for ecosystem function and food production. SOC has an important influence on soil properties and soil quality. Conventional SOC analysis is expensive and time-consuming. The development of spectral imaging sensors enables the acquisition of larger amounts of data using cheaper and faster methods. In addition, satellite remote sensing offers the potential to perform surveys more frequently and over larger areas. This research aimed to measure SOC content with colour as an indirect proxy. The measurements of soil colour were made at an agricultural site of the Czech Republic with an inexpensive digital camera and the Sentinel-2 remote sensor. Various soil colour spaces and colour indices derived from the (i) reflectance spectroscopy in the selected wavelengths of the visible (VIS) range (400-700 nm), (ii) RGB digital camera, and (iii) Sentinel-2 visible bands were used to train models for prediction of SOC. For modelling, we used the machine learning method, random forest (RF), and the models were validated with repeated 5-fold cross-validation. For prediction of SOC, the digital camera produced R-2 = 0.85 and FtMSEp = 0.11%, which had higher R-2 and similar RMSEp compared to those obtained from the spectroscopy (R-2 = 0.78 and RMSEp = 0.09%). Sentinel-2 predicted SOC with lower accuracy than other techniques; however, the results were still fair (R-2 = 0.67 and RMSEp = 0.12%) and comparable with other methods. Using a digital camera with simple colour features was efficient. It enabled cheaper and accurate predictions of SOC compared to spectroscopic measurement and Sentinel-2 data.
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页数:10
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