The application of proximal visible and near-infrared spectroscopy to estimate soil organic matter on the Triffa Plain of Morocco

被引:23
|
作者
Lazaar, Ayoub [1 ]
Mouazen, Abdul Mounem [2 ]
EL Hammouti, Kamal [1 ]
Fullen, Michael [3 ]
Pradhan, Biswajeet [4 ]
Memon, Muhammad Sohail [5 ]
Andich, Karim [6 ]
Monir, Abdelilah [7 ]
机构
[1] Mohammed First Univ, Fac Sci, Dept Geol, Lab Appl Geosci, Oujda, Morocco
[2] Univ Ghent, Dept Environm, Coupure Links 653, Coupure Links 653, B-9000 Ghent, Belgium
[3] Univ Wolverhampton, Fac Sci & Engn, Wolverhampton WV1 1LY, England
[4] Univ Technol Sydney, Fac Engn & Informat Technol, Ctr Adv Modelling & Geospatial Informat Syst CAMG, Sydney, NSW 2007, Australia
[5] Sindh Agr Univ, Fac Agr Engn, Tandojam 70060, Pakistan
[6] Natl Inst Agron Res INRA, Lab Appl Geomat & Soil Sci, Oujda, Morocco
[7] Moulay Ismail Univ, Dept Math, EDP & Sci Comp Team, Meknes, Morocco
关键词
Soil organic matter; VIS-NIR spectroscopy; Reflectance spectra; SOM estimation; SOM analysis; REFLECTANCE SPECTROSCOPY; NIR SPECTROSCOPY; TOTAL NITROGEN; LEAST-SQUARES; PREDICTION; CARBON; CLAY; SPECTRA; QUALITY; FIELD;
D O I
10.1016/j.iswcr.2020.04.005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil organic matter (SOM) is a fundamental soil constituent. The estimation of this parameter in the laboratory using the classical method is complex time-consuming and requires the use of chemical reagents. The objectives of this study were to assess the accuracy of two laboratory measurement setups of the VIS-NIR spectroscopy in estimating SOM content and determine the important spectral bands in the SOM estimation model. A total of 115 soil samples were collected from the non-root zone (0-20 cm) of soil in the study area of the Triffa Plain and then analysed for SOM in the laboratory by the Walkley-Black method. The reflectance spectra of soil samples were measured by two protocols, Contact Probe (CP) and Pistol Grip (PG)) of the ASD spectroradiometer (350-2500 nm) in the laboratory. Partial least squares regression (PLSR) was used to develop the prediction models. The results of coefficient of determination (R-2) and the root mean square error (RMSE) showed that the pistol grip offers reasonable accuracy with an R-2 = 0.93 and RMSE = 0.13 compared to the contact probe protocol with an R-2 = 0.85 and RMSE = 0.19. The near-Infrared range were more accurate than those in the visible range for predicting SOM using the both setups (CP and PG). The significant wavelengths contributing to the prediction of SOM for (PG) setup were at: 424, 597, 1432, 1484, 1830,1920, 2200, 2357 and 2430 nm, while were at 433, 587, 1380, 1431, 1929, 2200 and 2345 nm for (CP) setup. (c) 2020 International Research and Training Center on Erosion and Sedimentation and China Water and Power Press. Production and Hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:195 / 204
页数:10
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