Articles | Volume 2, issue 2
https://doi.org/10.5194/se-2-283-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-2-283-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Erosion rates deduced from seasonal mass balance along the upper Urumqi River in Tianshan
Y. Liu
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, 1 rue Jussieu, 75238 Paris Cedex 05, France
Key Laboratory of Water Environment and Resource, Tianjin Normal University, 393 Binshui west road, Tianjin 300387, China
F. Métivier
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, 1 rue Jussieu, 75238 Paris Cedex 05, France
J. Gaillardet
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, 1 rue Jussieu, 75238 Paris Cedex 05, France
B. Ye
The States Key laboratory of Cryospheric Science, Cold and Arid Region Environmental and Engineering and Research Institute, Chinese Academy of Sciences 260 Donggang west road, Lanzhou, China
P. Meunier
Département de Géologie, UMR8538, CNRS, Ecole Normale Supérieure, 24 rue Lhomond, 75005 Paris, France
C. Narteau
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, 1 rue Jussieu, 75238 Paris Cedex 05, France
E. Lajeunesse
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, 1 rue Jussieu, 75238 Paris Cedex 05, France
T. Han
The States Key laboratory of Cryospheric Science, Cold and Arid Region Environmental and Engineering and Research Institute, Chinese Academy of Sciences 260 Donggang west road, Lanzhou, China
L. Malverti
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, 1 rue Jussieu, 75238 Paris Cedex 05, France
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We studied the mobility and sedimentary characteristics of rock avalanches influenced by initial discontinuity sets with experimental methods. In the experiments, we set different initial configurations of blocks. The results revealed that the mobility and surface structures of the mass flows differed significantly. In the mass deposits, the block orientations were affected by their initial configurations and the motion processes of the mass flows.
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François Clapuyt, Veerle Vanacker, Marcus Christl, Kristof Van Oost, and Fritz Schlunegger
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Robert A. Watson, Eoghan P. Holohan, Djamil Al-Halbouni, Leila Saberi, Ali Sawarieh, Damien Closson, Hussam Alrshdan, Najib Abou Karaki, Christian Siebert, Thomas R. Walter, and Torsten Dahm
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The fall of the Dead Sea level since the 1960s has provoked the formation of over 6000 sinkholes, a major hazard to local economy and infrastructure. In this context, we study the evolution of subsidence phenomena at three area scales at the Dead Sea’s eastern shore from 1967–2017. Our results yield the most detailed insights to date into the spatio-temporal development of sinkholes and larger depressions (uvalas) in an evaporite karst setting and emphasize a link to the falling Dead Sea level.
Djamil Al-Halbouni, Eoghan P. Holohan, Abbas Taheri, Robert A. Watson, Ulrich Polom, Martin P. J. Schöpfer, Sacha Emam, and Torsten Dahm
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Bruno Cagnoli and Antonio Piersanti
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Enric Vázquez-Suñé, Miguel Ángel Marazuela, Violeta Velasco, Marc Diviu, Andrés Pérez-Estaún, and Joaquina Álvarez-Marrón
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Different stages of soil removal, transfer, preparation and placement in laboratory plots cause significant changes in soil structure and, subsequently, the results of runoff, sediment concentration and soil loss. The increasing rates of runoff coefficient, sediment concentration and soil loss due to the study soil preparation method for laboratory soil erosion plots were 179, 183 and 1050 % (2.79, 2.83 and 11.50 times), respectively.
Jozef Gallik and Lenka Bolešová
Solid Earth, 7, 1033–1042, https://doi.org/10.5194/se-7-1033-2016, https://doi.org/10.5194/se-7-1033-2016, 2016
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Technology is moving ahead very fast, and so researchers have new possibilities for their research. We tried to demonstrate benefits of using remote-sensing technology (Phantom 1 drone) such as its accuracy in the terrain, easy access to hardly accessible areas, and the possibility to collect data even during unfavourable weather conditions. The high mountainous environment provided us great conditions for testing the drone as a device for very easy and accurate mapping of natural phenomena.
Mohammad Hassan Sadeghravesh, Hassan Khosravi, and Soudeh Ghasemian
Solid Earth, 7, 673–683, https://doi.org/10.5194/se-7-673-2016, https://doi.org/10.5194/se-7-673-2016, 2016
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Select appropriate strategies according to all effective criteria in combating desertification process can be so useful in controlling and rehabilitation of degraded lands, and avoid degradation in vulnerable fields. This study provides systematic and optimal strategies of combating desertification by group decision-making model. To this end, in the framework of Multi Attribute Decision Making (MADM) and by using Delphi model (Delphi), the preferences of indexes were obtained.
Guang Jie Luo, Shi Jie Wang, Xiao Yong Bai, Xiu Ming Liu, and An Yun Cheng
Solid Earth, 7, 457–468, https://doi.org/10.5194/se-7-457-2016, https://doi.org/10.5194/se-7-457-2016, 2016
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For accurately reflecting the eco-hydrological process of the dual structure of the surface and subsurface, we propose a new method for the extraction of small watersheds in karst regions. In this study, we think that the minimum karst watershed has an exit at the corrosion–erosion datum, and the further karst sub-watershed division may cause an eco-hydrological fault. The watersheds delineated by our method accurately reflect the hydrological process in the Sancha River.
J. Rodrigo Comino, C. Brings, T. Lassu, T. Iserloh, J. M. Senciales, J. F. Martínez Murillo, J. D. Ruiz Sinoga, M. Seeger, and J. B. Ries
Solid Earth, 6, 823–837, https://doi.org/10.5194/se-6-823-2015, https://doi.org/10.5194/se-6-823-2015, 2015
M. Arian and Z. Aram
Solid Earth, 5, 1277–1291, https://doi.org/10.5194/se-5-1277-2014, https://doi.org/10.5194/se-5-1277-2014, 2014
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The Kermanshah area in the High Zagros, Iran (the collision of the Arabian and Eurasian plates) has been affected by four classes of tectonic variation. These regions were identified as very high, high, moderate and low relative tectonic activity by calculation and analysis of six geomorphic indices.
A. Gómez-Ortiz, M. Oliva, F. Salvador-Franch, M. Salvà-Catarineu, D. Palacios, J. J. de Sanjosé-Blasco, L. M. Tanarro-García, J. Galindo-Zaldívar, and C. Sanz de Galdeano
Solid Earth, 5, 979–993, https://doi.org/10.5194/se-5-979-2014, https://doi.org/10.5194/se-5-979-2014, 2014
M. Oliva, G. Vieira, P. Pina, P. Pereira, M. Neves, and M. C. Freitas
Solid Earth, 5, 901–914, https://doi.org/10.5194/se-5-901-2014, https://doi.org/10.5194/se-5-901-2014, 2014
R. Sutinen, I. Aro, P. Närhi, M. Piekkari, and M. Middleton
Solid Earth, 5, 683–691, https://doi.org/10.5194/se-5-683-2014, https://doi.org/10.5194/se-5-683-2014, 2014
H. C. Ho
Solid Earth, 2, 155–158, https://doi.org/10.5194/se-2-155-2011, https://doi.org/10.5194/se-2-155-2011, 2011
A. Limare, M. Tal, M. D. Reitz, E. Lajeunesse, and F. Métivier
Solid Earth, 2, 143–154, https://doi.org/10.5194/se-2-143-2011, https://doi.org/10.5194/se-2-143-2011, 2011
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