干旱区科学2021,Vol.13Issue(12) :1287-1298.

Estimation of rock Fe content based on hyperspectral indices

WANG Jinlin WANG Wei CHENG Yinyi ZHANG Zhixin WANG Shanshan ZHOU Kefa LI Pingheng
干旱区科学2021,Vol.13Issue(12) :1287-1298.

Estimation of rock Fe content based on hyperspectral indices

WANG Jinlin 1WANG Wei 1CHENG Yinyi 1ZHANG Zhixin 1WANG Shanshan 1ZHOU Kefa 1LI Pingheng2
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作者信息

  • 1. State Key Laboratory of Desert and Oasis Ecology,Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China;Xinjiang Key Laboratory of Mineral Resources and Digital Geology,Urumqi 830011,China;Xinjiang Research Centre for Mineral Resources,Chinese Academy of Sciences,Urumqi 830011,China;University of Chinese Academy of Sciences,Beijing 100049,China
  • 2. Zhejiang A&F University,Hangzhou 311300,China
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Abstract

Information on the Fe content of bare rocks is needed for implementing geochemical processes and identifying mines. However, the influence of Fe content on the spectra of bare rocks has not been thoroughly analyzed in previous studies. The Saur Mountain region within the Hoboksar of the Russell Hill depression was selected as the study area. Specifically, we analyzed six hyperspectral indices related to rock Fe content based on laboratory measurements (Dataset I) and field measurements (Dataset Ⅱ). In situ field measurements were acquired to verify the laboratory measurements. Fe content of the rock samples collected from different fresh and weathered rock surfaces were divided into six levels to reveal the spatial distributions of Fe content of these samples. In addition, we clearly displayed wavelengths with obvious characteristics by analyzing the spectra of these samples. The results of this work indicated that Fe content estimation models based on the fresh rock surface measurements in the laboratory can be applied to in situ field or satellite-based measurements of Fe content of the weathered rock surfaces. It is not the best way to use only the single wavelengths reflectance at all absorption wavelengths or the depth of these absorption features to estimate Fe content. Based on sample data analysis, the comparison with other indices revealed that the performance of the modified normalized difference index is the best indicator for estimating rock Fe content, with R2 values of 0.45 and 0.40 corresponding to datasets I and Ⅱ, respectively. Hence, the modified normalized difference index (the wavelengths of 2220, 2290, and 2370 nm) identified in this study could contribute considerably to improve the identification accuracy of rock Fe content in the bare rock areas. The method proposed in this study can obviously provide an efficient solution for large-scale rock Fe content measurements in the field.

Key words

bare rocks/Fe content/reflectance/spectral indices/modified normalized difference index/Saur Mountain

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基金项目

Xinjiang Science and Technology Major Project(2021A03001-3)

National Key Research and Development Program of China(2018YFC0604001-3)

B&R Team of Chinese Academy of Sciences(2017-XBZG-BR-002)

National Natural Science Foundation of China(U1803117)

National Natural Science Foundation of China(U1803241)

出版年

2021
干旱区科学
中国科学院新疆生态与地理研究所,科学出版社

干旱区科学

CSTPCDCSCDSCI
影响因子:1.743
ISSN:1674-6767
参考文献量2
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