Visible and Near-Infrared Diffuse Reflectance Spectroscopy for Prediction of Soil Properties near a Copper Smelter

被引:58
作者
Xie Xian-Li [2 ]
Pan Xian-Zhang [2 ]
Sun Bo [1 ]
机构
[1] Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
[2] Chinese Acad Sci, Inst Soil Sci, Key Lab Soil Environm & Pollut Remediat, Nanjing 210008, Peoples R China
基金
中国国家自然科学基金;
关键词
heavy metal; organic matter; partial least squares regression; soil environment monitoring; spectral preprocessing; PARTIAL LEAST-SQUARES; NIR SPECTROSCOPY; ORGANIC-MATTER; HEAVY-METALS; FOREST SOILS; CLAY CONTENT; SPECTRA; CARBON; CONTAMINATION; QUALITY;
D O I
10.1016/S1002-0160(12)60022-8
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Spatial and temporal monitoring of soil properties in smelting regions requires collection of a large number of samples followed by laboratory cumbersome and time-consuming measurements. Visible and near-infrared diffuse reflectance spectroscopy (VNIR-DRS) provides a rapid and inexpensive tool to predict various soil properties simultaneously. This study evaluated the suitability of VNIR-DRS for predicting soil properties, including organic matter (OM), pH, and heavy metals (Cu, Pb, Zn, Cd, and Fe), using a total of 254 samples collected in soil profiles near a large copper smelter in China. Partial least square regression (PLSR) with cross-validation was used to relate soil property data to the reflectance spectral data by applying different preprocessing strategies. The performance of VNIR-DRS calibration models was evaluated using the coefficient of determination in cross-validation (R-cv(2)) and the ratio of standard deviation to the root mean standard error of cross-validation (SD/RMSEcv). The models provided fairly accurate predictions for OM and Fe (R-cv(2) > 0.80, SD/RMSEcv > 2.00), less accurate but acceptable for screening purposes for pH, Cu, Pb, and Cd (0.50 < R-cv(2) < 0.80, 1.40 < SD/RMSEcv < 2.00), and poor accuracy for Zn (R-cv(2), < 0.50, SD/RMSEcv < 1.40). Because soil properties in contaminated areas generally show large variation, a. comparative large number of calibrating samples, which are variable enough and uniformly distributed, are necessary to create more accurate and robust VNIR-DRS calibration models. This study indicated that VNIR-DRS technique combined with continuously enriched soil spectral library could be a nondestructive alternative for soil environment monitoring.
引用
收藏
页码:351 / 366
页数:16
相关论文
共 64 条
[1]  
[Anonymous], 1984, Chemometrics: Mathematics and Statistics in Chemistry, DOI [10.1007/978, DOI 10.1007/978, 10.1007/978-94-017-1026-8_2, DOI 10.1007/978-94-017-1026-8_2]
[2]  
[Anonymous], 2010, KEYS SOIL TAX
[3]  
Baumgardner M. F., 1986, ADV AGRON, V38, P1
[4]   Quantitative remote sensing of soil properties [J].
Ben-Dor, E .
ADVANCES IN AGRONOMY, VOL 75, 2002, 75 :173-243
[5]   NEAR-INFRARED ANALYSIS (NIRA) AS A METHOD TO SIMULTANEOUSLY EVALUATE SPECTRAL FEATURELESS CONSTITUENTS IN SOILS [J].
BENDOR, E ;
BANIN, A .
SOIL SCIENCE, 1995, 159 (04) :259-270
[6]   Near infrared reflectance spectroscopy as a tool to predict pesticide sorption in soil [J].
Bengtsson, S. ;
Berglof, T. ;
Kylin, H. .
BULLETIN OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY, 2007, 78 (05) :295-298
[7]   Diagnostic screening of urban soil contaminants using diffuse reflectance spectroscopy [J].
Bray, J. G. P. ;
Rossel, R. Viscarra ;
McBratney, A. B. .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 2009, 47 (04) :433-442
[8]   Global soil characterization with VNIR diffuse reflectance spectroscopy [J].
Brown, David J. ;
Shepherd, Keith D. ;
Walsh, Markus G. ;
Mays, M. Dewayne ;
Reinsch, Thomas G. .
GEODERMA, 2006, 132 (3-4) :273-290
[9]   Near-infrared reflectance spectroscopy-principal components regression analyses of soil properties [J].
Chang, CW ;
Laird, DA ;
Mausbach, MJ ;
Hurburgh, CR .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2001, 65 (02) :480-490
[10]   REFLECTANCE SPECTROSCOPY - QUANTITATIVE-ANALYSIS TECHNIQUES FOR REMOTE-SENSING APPLICATIONS [J].
CLARK, RN ;
ROUSH, TL .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB7) :6329-6340