Estimating soil organic carbon density in Northern China's agro-pastoral ecotone using vis-NIR spectroscopy

被引:15
作者
Chen, Yun [1 ,2 ]
Li, Yuqiang [1 ,2 ,3 ]
Wang, Xuyang [1 ,3 ]
Wan, Jinliang [4 ]
Gong, Xiangwen [5 ]
Niu, Yayi [1 ,2 ]
Liu, Jing [1 ,2 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Naiman Desertificat Res Stn, Tongliao 028300, Peoples R China
[4] Yunnan Normal Univ, Coll Tourism & Geog Sci, Kunming 650500, Yunnan, Peoples R China
[5] Chongqing Inst Geol & Mineral Resources, Wansheng Min Chongqing Conservat & Repair Ecol En, Chongqing 400042, Peoples R China
基金
中国国家自然科学基金; 国家重点研发计划;
关键词
Soil organic carbon density; Spectroscopy; Estimation; Agro-pastoral ecotone; DIFFUSE-REFLECTANCE SPECTROSCOPY; NEAR-INFRARED SPECTROSCOPY; BULK-DENSITY; MIDINFRARED SPECTROSCOPY; CALIBRATION METHODS; CLAY CONTENT; LOCAL SCALE; MATTER; PREDICTION; STORAGE;
D O I
10.1007/s11368-020-02668-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Purpose Traditional soil organic carbon density (SOCD) measurement is time-consuming and costly, from field sampling to laboratory analysis. However, visible to near-infrared reflectance (vis-NIR) spectroscopy can rapidly estimate SOCD and thereby permit rapid, inexpensive measurements that support environmental management. Our aim was to explore the relationship between SOCD and vis-NIR spectra, with the goal of establishing a spectral SOCD estimation method. Materials and methods In this study, we sampled soils throughout northern China's agro-pastoral ecotone and performed SOCD and spectral measurements. After pre-processing the data, we transformed the spectral reflectance into seven forms: the reciprocal logarithm, first-order differential, second-order differential, logarithmic first-order differential, logarithmic second-order differential, reciprocal first-order differential (RFOD), and reciprocal second-order differential. We then explored the relationship between SOCD and these indexes. We also analyzed spectral SOCD estimation models based on stepwise multiple linear regression and partial least-squares regression. Results and discussion We found that the spectral reflectance decreased with increasing SOCD, and the most sensitive bands for SOCD were between 745 and 840 nm. RFOD greatly improved estimation accuracy. The performance of a stepwise multiple linear regression estimation model based on RFOD provided the best fit (R-2 = 0.77) and the lowest root-mean-square error (0.75 kg C m(-2)), and the best ratio of percent deviation (2.11). Conclusion Our results suggest a high potential for fast and reliable estimation of SOCD using spectral techniques and provides a theoretical basis and technical support for rapid monitoring of SOCD in northern China's agro-pastoral ecotone.
引用
收藏
页码:3698 / 3711
页数:14
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