Dissolution feature differences of carbonate rock within hydro-fluctuation belt located in the Three Gorges Reservoir Area

The stability of geological environment in the Three Gorges Reservoir Area (TGRA) has experienced severe challenges due to the 30 m hydro-fluctuation belt (HFB). The vertical dissolution features vary with the mechanism of water and rock interaction. Although dissolution features have been adequatel...

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Published inEngineering geology Vol. 327; p. 107362
Main Authors Chen, Chiwei, Yang, Haiqing, Song, Kanglei, Liang, Dan, Zhang, Yuhan, Ni, Jianghua
Format Journal Article
LanguageEnglish
Published Elsevier B.V 20.12.2023
Subjects
algorithms
Carbonate rock deterioration
carbonate rocks
carbonates
Dissolution features
geometry
geomorphology
Hydro-fluctuation belt
hydrology
Hyperspectral imaging technique
Intelligent algorithm
rain
spectral analysis
Three Gorges Reservoir Area
Triassic period
Carbonate rock deterioration
Intelligent algorithm
Hyperspectral imaging technique
Dissolution features
Hydro-fluctuation belt
Three Gorges Reservoir Area
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Abstract The stability of geological environment in the Three Gorges Reservoir Area (TGRA) has experienced severe challenges due to the 30 m hydro-fluctuation belt (HFB). The vertical dissolution features vary with the mechanism of water and rock interaction. Although dissolution features have been adequately explained by physical and mechanical parameters, the characterization of chemical changes in dissolution is vital but frequently neglected information. For this purpose, the hyperspectral characteristics and mineralogical composition variation of rock HFB in different areas of the Triassic Daye Formation are tested to elucidate the dissolution behaviors. Then, the deterioration degree of dissolution is quantified by a multi-objective data integration based on Random Forest Regression (RFR) model. The spatial distribution of dissolution and the seasonal deterioration characteristics are identified depending on the spectral response of carbonate. Specifically, the dissolution degree is proportional to elevation, and inverse to the bedding angle at 0–40° in the investigated stratum. Combined with the hydrological characteristics of study area, the corresponding regional phenomena can be distinguished as reservoir water dominated, rainfall dominated, and coupled action. Affected by reservoir water and acid rainfall, the HFB may deteriorate most severely from January to April. In addition, the contribution of RFR model integrated spectral and geometric data to the deterioration evaluation of the HFB is discussed, which can effectively enhance the identification of rock mass boundary in a single spectral data model. Thus, these results are conducive to the rapid evaluation of regional geomorphological characteristics and the monitoring of geological disasters in the TGRA. •Dissolution of hydro-fluctuation belt is characterized by hyperspectral response.•Reservoir level and rainfall have different effects on carbonate rock dissolution.•Deterioration mechanism of rock with seasonal hydrological feature is revealed.•A rock deterioration evaluation model based on spectra and geometry is proposed.
AbstractList The stability of geological environment in the Three Gorges Reservoir Area (TGRA) has experienced severe challenges due to the 30 m hydro-fluctuation belt (HFB). The vertical dissolution features vary with the mechanism of water and rock interaction. Although dissolution features have been adequately explained by physical and mechanical parameters, the characterization of chemical changes in dissolution is vital but frequently neglected information. For this purpose, the hyperspectral characteristics and mineralogical composition variation of rock HFB in different areas of the Triassic Daye Formation are tested to elucidate the dissolution behaviors. Then, the deterioration degree of dissolution is quantified by a multi-objective data integration based on Random Forest Regression (RFR) model. The spatial distribution of dissolution and the seasonal deterioration characteristics are identified depending on the spectral response of carbonate. Specifically, the dissolution degree is proportional to elevation, and inverse to the bedding angle at 0–40° in the investigated stratum. Combined with the hydrological characteristics of study area, the corresponding regional phenomena can be distinguished as reservoir water dominated, rainfall dominated, and coupled action. Affected by reservoir water and acid rainfall, the HFB may deteriorate most severely from January to April. In addition, the contribution of RFR model integrated spectral and geometric data to the deterioration evaluation of the HFB is discussed, which can effectively enhance the identification of rock mass boundary in a single spectral data model. Thus, these results are conducive to the rapid evaluation of regional geomorphological characteristics and the monitoring of geological disasters in the TGRA. •Dissolution of hydro-fluctuation belt is characterized by hyperspectral response.•Reservoir level and rainfall have different effects on carbonate rock dissolution.•Deterioration mechanism of rock with seasonal hydrological feature is revealed.•A rock deterioration evaluation model based on spectra and geometry is proposed.
The stability of geological environment in the Three Gorges Reservoir Area (TGRA) has experienced severe challenges due to the 30 m hydro-fluctuation belt (HFB). The vertical dissolution features vary with the mechanism of water and rock interaction. Although dissolution features have been adequately explained by physical and mechanical parameters, the characterization of chemical changes in dissolution is vital but frequently neglected information. For this purpose, the hyperspectral characteristics and mineralogical composition variation of rock HFB in different areas of the Triassic Daye Formation are tested to elucidate the dissolution behaviors. Then, the deterioration degree of dissolution is quantified by a multi-objective data integration based on Random Forest Regression (RFR) model. The spatial distribution of dissolution and the seasonal deterioration characteristics are identified depending on the spectral response of carbonate. Specifically, the dissolution degree is proportional to elevation, and inverse to the bedding angle at 0–40° in the investigated stratum. Combined with the hydrological characteristics of study area, the corresponding regional phenomena can be distinguished as reservoir water dominated, rainfall dominated, and coupled action. Affected by reservoir water and acid rainfall, the HFB may deteriorate most severely from January to April. In addition, the contribution of RFR model integrated spectral and geometric data to the deterioration evaluation of the HFB is discussed, which can effectively enhance the identification of rock mass boundary in a single spectral data model. Thus, these results are conducive to the rapid evaluation of regional geomorphological characteristics and the monitoring of geological disasters in the TGRA.
ArticleNumber 107362
Author Zhang, Yuhan
Chen, Chiwei
Song, Kanglei
Ni, Jianghua
Liang, Dan
Yang, Haiqing
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  givenname: Haiqing
  surname: Yang
  fullname: Yang, Haiqing
  email: yanghaiqing@cqu.edu.cn
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– sequence: 3
  givenname: Kanglei
  surname: Song
  fullname: Song, Kanglei
  organization: State Key Laboratory of Coal Mine Disaster Dynamics and Control, School of Civil Engineering, Chongqing University, Chongqing 400045, China
– sequence: 4
  givenname: Dan
  surname: Liang
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  organization: State Key Laboratory of Coal Mine Disaster Dynamics and Control, School of Civil Engineering, Chongqing University, Chongqing 400045, China
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  givenname: Yuhan
  surname: Zhang
  fullname: Zhang, Yuhan
  organization: School of Information and Electronics, Beijing Institute of Technology, Beijing 100081, China
– sequence: 6
  givenname: Jianghua
  surname: Ni
  fullname: Ni, Jianghua
  organization: State Key Laboratory of Coal Mine Disaster Dynamics and Control, School of Civil Engineering, Chongqing University, Chongqing 400045, China
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Keywords Carbonate rock deterioration
Intelligent algorithm
Hyperspectral imaging technique
Dissolution features
Hydro-fluctuation belt
Three Gorges Reservoir Area
Language English
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Snippet The stability of geological environment in the Three Gorges Reservoir Area (TGRA) has experienced severe challenges due to the 30 m hydro-fluctuation belt...
The stability of geological environment in the Three Gorges Reservoir Area (TGRA) has experienced severe challenges due to the 30 m hydro-fluctuation belt...
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StartPage 107362
SubjectTerms algorithms
Carbonate rock deterioration
carbonate rocks
carbonates
Dissolution features
geometry
geomorphology
Hydro-fluctuation belt
hydrology
Hyperspectral imaging technique
Intelligent algorithm
rain
spectral analysis
Three Gorges Reservoir Area
Triassic period
Title Dissolution feature differences of carbonate rock within hydro-fluctuation belt located in the Three Gorges Reservoir Area
URI https://dx.doi.org/10.1016/j.enggeo.2023.107362
https://www.proquest.com/docview/3153803832
Volume 327
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