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https://doi.org/10.5194/nhessd-3-2537-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/nhessd-3-2537-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
15 Apr 2015
Status: this preprint was under review for the journal NHESS but the revision was not accepted.
Movement of the Donglingxin landslide, China, induced by reservoir inundation and rainfall
Abstract. With numerous high mountains, deep valleys and turbulent rivers, many hydropower plants have been constructed in the south-west China. Reservoir bank slopes are very common in this area, these slopes are widespread and quite often involved in deformation that can result in serious damage and casualties. In case of the Donglingxin landslide, for an in-depth study of processes that can trigger these events, the deformation characteristics and the failure mechanisms of the slope were performed on a detail scale, based on an intensive monitoring of rainfall events, reservoir level fluctuation and groundwater movement. The deformation of the upper part of slope is mainly induced by rainfall events, reservoir level fluctuation affects the deformation of the lower part of slope. The increase of pore water pressure may result in the failure of slope. The filed investigation suggest that the slope is unstable. Drainages is the only stabilization measure which can be implemented, due to very complex geological and geomorphology condition.
How to cite. Yu, J., Wang, R. B., Xu, W. Y., Yan, L., Zhang, J. C., and Meng, Q. X.: Movement of the Donglingxin landslide, China, induced by reservoir inundation and rainfall, Nat. Hazards Earth Syst. Sci. Discuss., 3, 2537–2564, https://doi.org/10.5194/nhessd-3-2537-2015, 2015.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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RC C638: 'This is a potentially interesting paper but a careful editorial review by a native English speaking editor is required.', Anonymous Referee #1, 07 May 2015
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AC C687: 'Thank you very much for your constructive comments and valuable recommendations. My responses to several comments are listed below', Wang Rubin, 13 May 2015
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AC C687: 'Thank you very much for your constructive comments and valuable recommendations. My responses to several comments are listed below', Wang Rubin, 13 May 2015
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SC C724: 'Referee comments', bo Wen, 20 May 2015
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AC C837: 'Reply to a comment of Mr bo Wen', Wang Rubin, 30 May 2015
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AC C837: 'Reply to a comment of Mr bo Wen', Wang Rubin, 30 May 2015
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RC C734: 'Review of the manuscript "Movement of the Donglingxin landslide, China, induced by reservoir inundation and rainfall"', Anonymous Referee #2, 21 May 2015
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AC C841: 'Answers to anonymous referee', Wang Rubin, 31 May 2015
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AC C841: 'Answers to anonymous referee', Wang Rubin, 31 May 2015
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EC C1191: 'Editor comment on “Movement of the Donglingxin landslide, China, induced by reservoir inundation and rainfall”', Paolo Tarolli, 30 Jun 2015
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
- Printer-friendly version
- Supplement
-
RC C638: 'This is a potentially interesting paper but a careful editorial review by a native English speaking editor is required.', Anonymous Referee #1, 07 May 2015
-
AC C687: 'Thank you very much for your constructive comments and valuable recommendations. My responses to several comments are listed below', Wang Rubin, 13 May 2015
-
AC C687: 'Thank you very much for your constructive comments and valuable recommendations. My responses to several comments are listed below', Wang Rubin, 13 May 2015
-
SC C724: 'Referee comments', bo Wen, 20 May 2015
-
AC C837: 'Reply to a comment of Mr bo Wen', Wang Rubin, 30 May 2015
-
AC C837: 'Reply to a comment of Mr bo Wen', Wang Rubin, 30 May 2015
-
RC C734: 'Review of the manuscript "Movement of the Donglingxin landslide, China, induced by reservoir inundation and rainfall"', Anonymous Referee #2, 21 May 2015
-
AC C841: 'Answers to anonymous referee', Wang Rubin, 31 May 2015
-
AC C841: 'Answers to anonymous referee', Wang Rubin, 31 May 2015
-
EC C1191: 'Editor comment on “Movement of the Donglingxin landslide, China, induced by reservoir inundation and rainfall”', Paolo Tarolli, 30 Jun 2015
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J. Yu
Research Institute of Geotechnical Engineering, Hohai University, Nanjing, China
Key Laboratory of the Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, China
Research Institute of Geotechnical Engineering, Hohai University, Nanjing, China
Key Laboratory of the Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, China
W. Y. Xu
Research Institute of Geotechnical Engineering, Hohai University, Nanjing, China
Key Laboratory of the Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, China
L. Yan
Research Institute of Geotechnical Engineering, Hohai University, Nanjing, China
Key Laboratory of the Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, China
J. C. Zhang
Research Institute of Geotechnical Engineering, Hohai University, Nanjing, China
Key Laboratory of the Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, China
Q. X. Meng
Research Institute of Geotechnical Engineering, Hohai University, Nanjing, China
Key Laboratory of the Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, China
Short summary
In case of the Donglingxin landslide, for an in-depth study of processes that can trigger these events, the deformation characteristics and the failure mechanisms of the slope were performed on a detail scale, based on an intensive monitoring of rainfall events, reservoir level fluctuation and groundwater movement. The deformation of the upper part of slope is mainly induced by rainfall events, reservoir level fluctuation affects the deformation of the lower part of slope.
In case of the Donglingxin landslide, for an in-depth study of processes that can trigger these...
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