The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir

Chen Yixiang; Wu Jiangqiang; Huang Qibo; Gan Fuping; Han Kai; Yang Chuchang; Zheng Zhijie

doi:doi:10.11648/j.sd.20180603.11

| Peer-Reviewed

The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir

Chen Yixiang, Wu Jiangqiang, Huang Qibo, Gan Fuping, Han Kai, Yang Chuchang, Zheng Zhijie

Published in Science Discovery (Volume 6, Issue 3)

Received: 20 June 2018 Accepted: Published: 22 June 2018

Views: Downloads:

Download PDF

Share This Article

Twitter
Linked In
Facebook

Abstract

As a result of karst development, water leakage from reservoirs and waste water leakage from mine tailings impoundments often occur in karst region of southwestem China. The geophysical prospecting methods commonly used in the investigation of karst leakage passage are mostly located in the dam, abutment and other land of the reservoir area, which are fail to detect and evaluate the karst collapse at the bottom of the reservoir directly. This will result that the effect of detection and governance are often poor. This paper takes the detection of karst leakage passage beside culvert of the first class hydropower station in Jinjihe reservoir in North Guangxi as an example, studying the principle, field working method and detection effect of detecting karst leakage passage in reservoir by self-potential method on the water. Outcropping formation in the study area mainly consist by the limestone clipped dolomite, dolomitic limestone of Devonian Liujiang formation (D_3L) and dolomite, limestone, argillaceous limestone of the Devonian Donggangling order (D_2d). The hidden karst is secondary development. That outlet pipe of the first class hydropower station in the district releases water can cause a strong negative center regional field of self-potential on the water. By dividing the regional field of self-potential on the water using the circumferential mean method and calculating the residual local anomaly separate 6 secondary negative center residual local anomaly of self-potential on the water covered by a strong regional field like an equiaxed or elliptical shape. After check in the reservoir by the diver, the 6 negative center residual local anomaly zone correspond to karst collapse, karst opening or leaking skylight at the bottom of the reservoir. Among them, the negative center residual local anomaly like an equiaxed shape near the survey points 46-48 of line 16 correspond to the largest karst collapse at the bottom of the reservoir. Through the simple connected experiment of internal and external water and the engineering geological drilling, the effect of geophysical anomaly detection is good. The self-potential method on the water can be used in the investigation of karst geological problems, such as the emergency on the water of the karst sick reservoir, and the rapid delineation of the range of the shallow karst leakage passage.

Published in	Science Discovery (Volume 6, Issue 3)
DOI	10.11648/j.sd.20180603.11
Page(s)	137-146
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Reservoir, Karst Leakage Passage, Self-Potential Method on the Water, Leakage Mechanism, Detection Effect

References

[1]	石昆法，戚洪彬，王斌.地层含水性研究的地球物理方法[J].地球物理学进展，2002,17（4）:636-643。
[2]	王俊业.应用自然电场法研究地下水流场[J].物探与化探，2002,26（2）：140-142。
[3]	郑灿堂.应用自然电场法检测土坝渗漏隐患的技术[J]. 地球物理学进展，2005,20（3）:854-858。
[4]	赫健，孙从炎，陈夷.自然电场法和高密度电阻率法在天子岗水库副坝渗漏隐患探测中的应用[J]. 浙江水利科技，2007, 153（5）:45-47。
[5]	冷元宝,朱文仲,何剑,等.我国堤坝隐患及渗漏探测技术现状及展望[J].水利水电科技进展,2002,22(2):59-62。
[6]	赵瑞,许模.水库岩溶渗漏及防渗研究综述[J]. 地下水, 2011, 33(2):20-22。
[7]	葛双成,江影,颜学军.综合物探方法在堤防质量检测中的应用[J].地球物理学进展,2006,21(1):263-272。
[8]	陈贻祥,甘伏平,卢呈杰,韦吉益.岩溶塌陷自然电场及其应用[J].中国岩溶，2013, 32(4): 480-486。
[9]	杨磊，周启友.基于自然电位方法的非饱和带水分分布和运移情况探测[J].工程勘察，2012,（12）：84-89。
[10]	韩凯，陈玉玲，陈贻祥，等.岩溶病害水库的渗漏通道探测方法——以广西全州县洛潭水库为例[J].水力发电学报，2015,34(11):116-125。
[11]	程亚平，蒋灵芝，黎柳月，等.综合物探技术探测平果铝厂赤泥堆场岩溶发育特征[J].中国岩溶，2016, 35(6): 688-698。
[12]	Fritjof Fagerlund, Graham Heinson. Detecting subsurface groundwater flow in fractured rock using self-potential(sp) methods [J]. Environmental Geology, 2003, 43: 782–794.
[13]	A. Revil, K. Titov, C. Doussan, and V. Lapenna. Applications of the self-potential method to hydrological problems [M]. Applied Hydrogeophysics, 255–292.
[14]	Jeffrey R. Moore, Alexandre Boleve , Johnny W. Sanders , Steven D. Glaser. Self-potential investigation of moraine dam seepage [J]. Journal of Applied Geophysics, 74 (2011): 277–286.

Cite This Article

Plain Text BibTeX RIS

APA Style

Chen Yixiang, Wu Jiangqiang, Huang Qibo, Gan Fuping, Han Kai, et al. (2018). The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir. Science Discovery, 6(3), 137-146. https://doi.org/10.11648/j.sd.20180603.11

Copy | Download

ACS Style

Chen Yixiang; Wu Jiangqiang; Huang Qibo; Gan Fuping; Han Kai, et al. The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir. Sci. Discov. 2018, 6(3), 137-146. doi: 10.11648/j.sd.20180603.11

Copy | Download

AMA Style

Chen Yixiang, Wu Jiangqiang, Huang Qibo, Gan Fuping, Han Kai, et al. The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir. Sci Discov. 2018;6(3):137-146. doi: 10.11648/j.sd.20180603.11

Copy | Download

@article{10.11648/j.sd.20180603.11,
  author = {Chen Yixiang and Wu Jiangqiang and Huang Qibo and Gan Fuping and Han Kai and Yang Chuchang and Zheng Zhijie},
  title = {The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir},
  journal = {Science Discovery},
  volume = {6},
  number = {3},
  pages = {137-146},
  doi = {10.11648/j.sd.20180603.11},
  url = {https://doi.org/10.11648/j.sd.20180603.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.sd.20180603.11},
  abstract = {As a result of karst development, water leakage from reservoirs and waste water leakage from mine tailings impoundments often occur in karst region of southwestem China. The geophysical prospecting methods commonly used in the investigation of karst leakage passage are mostly located in the dam, abutment and other land of the reservoir area, which are fail to detect and evaluate the karst collapse at the bottom of the reservoir directly. This will result that the effect of detection and governance are often poor. This paper takes the detection of karst leakage passage beside culvert of the first class hydropower station in Jinjihe reservoir in North Guangxi as an example, studying the principle, field working method and detection effect of detecting karst leakage passage in reservoir by self-potential method on the water. Outcropping formation in the study area mainly consist by the limestone clipped dolomite, dolomitic limestone of Devonian Liujiang formation (D3L) and dolomite, limestone, argillaceous limestone of the Devonian Donggangling order (D2d). The hidden karst is secondary development. That outlet pipe of the first class hydropower station in the district releases water can cause a strong negative center regional field of self-potential on the water. By dividing the regional field of self-potential on the water using the circumferential mean method and calculating the residual local anomaly separate 6 secondary negative center residual local anomaly of self-potential on the water covered by a strong regional field like an equiaxed or elliptical shape. After check in the reservoir by the diver, the 6 negative center residual local anomaly zone correspond to karst collapse, karst opening or leaking skylight at the bottom of the reservoir. Among them, the negative center residual local anomaly like an equiaxed shape near the survey points 46-48 of line 16 correspond to the largest karst collapse at the bottom of the reservoir. Through the simple connected experiment of internal and external water and the engineering geological drilling, the effect of geophysical anomaly detection is good. The self-potential method on the water can be used in the investigation of karst geological problems, such as the emergency on the water of the karst sick reservoir, and the rapid delineation of the range of the shallow karst leakage passage.},
 year = {2018}
}

Copy | Download

TY  - JOUR
T1  - The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir
AU  - Chen Yixiang
AU  - Wu Jiangqiang
AU  - Huang Qibo
AU  - Gan Fuping
AU  - Han Kai
AU  - Yang Chuchang
AU  - Zheng Zhijie
Y1  - 2018/06/22
PY  - 2018
N1  - https://doi.org/10.11648/j.sd.20180603.11
DO  - 10.11648/j.sd.20180603.11
T2  - Science Discovery
JF  - Science Discovery
JO  - Science Discovery
SP  - 137
EP  - 146
PB  - Science Publishing Group
SN  - 2331-0650
UR  - https://doi.org/10.11648/j.sd.20180603.11
AB  - As a result of karst development, water leakage from reservoirs and waste water leakage from mine tailings impoundments often occur in karst region of southwestem China. The geophysical prospecting methods commonly used in the investigation of karst leakage passage are mostly located in the dam, abutment and other land of the reservoir area, which are fail to detect and evaluate the karst collapse at the bottom of the reservoir directly. This will result that the effect of detection and governance are often poor. This paper takes the detection of karst leakage passage beside culvert of the first class hydropower station in Jinjihe reservoir in North Guangxi as an example, studying the principle, field working method and detection effect of detecting karst leakage passage in reservoir by self-potential method on the water. Outcropping formation in the study area mainly consist by the limestone clipped dolomite, dolomitic limestone of Devonian Liujiang formation (D3L) and dolomite, limestone, argillaceous limestone of the Devonian Donggangling order (D2d). The hidden karst is secondary development. That outlet pipe of the first class hydropower station in the district releases water can cause a strong negative center regional field of self-potential on the water. By dividing the regional field of self-potential on the water using the circumferential mean method and calculating the residual local anomaly separate 6 secondary negative center residual local anomaly of self-potential on the water covered by a strong regional field like an equiaxed or elliptical shape. After check in the reservoir by the diver, the 6 negative center residual local anomaly zone correspond to karst collapse, karst opening or leaking skylight at the bottom of the reservoir. Among them, the negative center residual local anomaly like an equiaxed shape near the survey points 46-48 of line 16 correspond to the largest karst collapse at the bottom of the reservoir. Through the simple connected experiment of internal and external water and the engineering geological drilling, the effect of geophysical anomaly detection is good. The self-potential method on the water can be used in the investigation of karst geological problems, such as the emergency on the water of the karst sick reservoir, and the rapid delineation of the range of the shallow karst leakage passage.
VL  - 6
IS  - 3
ER  -

Copy | Download

Author Information

Chen Yixiang

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China
Wu Jiangqiang

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China
Huang Qibo

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China
Gan Fuping

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China
Han Kai

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China
Yang Chuchang

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China
Zheng Zhijie

Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, China; Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, China

Download PDF

Sections

Plain Text BibTeX RIS

APA Style

Chen Yixiang, Wu Jiangqiang, Huang Qibo, Gan Fuping, Han Kai, et al. (2018). The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir. Science Discovery, 6(3), 137-146. https://doi.org/10.11648/j.sd.20180603.11

Copy | Download

ACS Style

Chen Yixiang; Wu Jiangqiang; Huang Qibo; Gan Fuping; Han Kai, et al. The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir. Sci. Discov. 2018, 6(3), 137-146. doi: 10.11648/j.sd.20180603.11

Copy | Download

AMA Style

Chen Yixiang, Wu Jiangqiang, Huang Qibo, Gan Fuping, Han Kai, et al. The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir. Sci Discov. 2018;6(3):137-146. doi: 10.11648/j.sd.20180603.11

Copy | Download

@article{10.11648/j.sd.20180603.11,
  author = {Chen Yixiang and Wu Jiangqiang and Huang Qibo and Gan Fuping and Han Kai and Yang Chuchang and Zheng Zhijie},
  title = {The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir},
  journal = {Science Discovery},
  volume = {6},
  number = {3},
  pages = {137-146},
  doi = {10.11648/j.sd.20180603.11},
  url = {https://doi.org/10.11648/j.sd.20180603.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.sd.20180603.11},
  abstract = {As a result of karst development, water leakage from reservoirs and waste water leakage from mine tailings impoundments often occur in karst region of southwestem China. The geophysical prospecting methods commonly used in the investigation of karst leakage passage are mostly located in the dam, abutment and other land of the reservoir area, which are fail to detect and evaluate the karst collapse at the bottom of the reservoir directly. This will result that the effect of detection and governance are often poor. This paper takes the detection of karst leakage passage beside culvert of the first class hydropower station in Jinjihe reservoir in North Guangxi as an example, studying the principle, field working method and detection effect of detecting karst leakage passage in reservoir by self-potential method on the water. Outcropping formation in the study area mainly consist by the limestone clipped dolomite, dolomitic limestone of Devonian Liujiang formation (D3L) and dolomite, limestone, argillaceous limestone of the Devonian Donggangling order (D2d). The hidden karst is secondary development. That outlet pipe of the first class hydropower station in the district releases water can cause a strong negative center regional field of self-potential on the water. By dividing the regional field of self-potential on the water using the circumferential mean method and calculating the residual local anomaly separate 6 secondary negative center residual local anomaly of self-potential on the water covered by a strong regional field like an equiaxed or elliptical shape. After check in the reservoir by the diver, the 6 negative center residual local anomaly zone correspond to karst collapse, karst opening or leaking skylight at the bottom of the reservoir. Among them, the negative center residual local anomaly like an equiaxed shape near the survey points 46-48 of line 16 correspond to the largest karst collapse at the bottom of the reservoir. Through the simple connected experiment of internal and external water and the engineering geological drilling, the effect of geophysical anomaly detection is good. The self-potential method on the water can be used in the investigation of karst geological problems, such as the emergency on the water of the karst sick reservoir, and the rapid delineation of the range of the shallow karst leakage passage.},
 year = {2018}
}

Copy | Download

TY  - JOUR
T1  - The Application of Self-Potential Method on Top of Water Surface for the Detection of Karst Leakage Channel in the Morbid Reservoir
AU  - Chen Yixiang
AU  - Wu Jiangqiang
AU  - Huang Qibo
AU  - Gan Fuping
AU  - Han Kai
AU  - Yang Chuchang
AU  - Zheng Zhijie
Y1  - 2018/06/22
PY  - 2018
N1  - https://doi.org/10.11648/j.sd.20180603.11
DO  - 10.11648/j.sd.20180603.11
T2  - Science Discovery
JF  - Science Discovery
JO  - Science Discovery
SP  - 137
EP  - 146
PB  - Science Publishing Group
SN  - 2331-0650
UR  - https://doi.org/10.11648/j.sd.20180603.11
AB  - As a result of karst development, water leakage from reservoirs and waste water leakage from mine tailings impoundments often occur in karst region of southwestem China. The geophysical prospecting methods commonly used in the investigation of karst leakage passage are mostly located in the dam, abutment and other land of the reservoir area, which are fail to detect and evaluate the karst collapse at the bottom of the reservoir directly. This will result that the effect of detection and governance are often poor. This paper takes the detection of karst leakage passage beside culvert of the first class hydropower station in Jinjihe reservoir in North Guangxi as an example, studying the principle, field working method and detection effect of detecting karst leakage passage in reservoir by self-potential method on the water. Outcropping formation in the study area mainly consist by the limestone clipped dolomite, dolomitic limestone of Devonian Liujiang formation (D3L) and dolomite, limestone, argillaceous limestone of the Devonian Donggangling order (D2d). The hidden karst is secondary development. That outlet pipe of the first class hydropower station in the district releases water can cause a strong negative center regional field of self-potential on the water. By dividing the regional field of self-potential on the water using the circumferential mean method and calculating the residual local anomaly separate 6 secondary negative center residual local anomaly of self-potential on the water covered by a strong regional field like an equiaxed or elliptical shape. After check in the reservoir by the diver, the 6 negative center residual local anomaly zone correspond to karst collapse, karst opening or leaking skylight at the bottom of the reservoir. Among them, the negative center residual local anomaly like an equiaxed shape near the survey points 46-48 of line 16 correspond to the largest karst collapse at the bottom of the reservoir. Through the simple connected experiment of internal and external water and the engineering geological drilling, the effect of geophysical anomaly detection is good. The self-potential method on the water can be used in the investigation of karst geological problems, such as the emergency on the water of the karst sick reservoir, and the rapid delineation of the range of the shallow karst leakage passage.
VL  - 6
IS  - 3
ER  -

Copy | Download