13288d85b725fc2c1"" onMouseOver=""InfoBubble.show('infobubble_2','mlktLink_2')"" onMouseOut=""InfoBubble.timeout()"">Time series analyses for Karst/River interactions asses... Journal of Hydrology |
Journal of Hydrology, Volume 349, Issues 1-2, 30 January 2008, Pages 98-114 V. Bailly-Comte, H. Jourde, A. Roesch, S. Pistre, C. Batiot-Guilhe Abstract SummaryIn many karst systems throughout the world, numerous karst features facilitate the exchange of water between the surface, the vadose zone and the saturated zone of the aquifer. These interactions play actually a prominent role in the ground and surface waters circulation. This study aims at assessing Karst/River interactions by the way of flood hydrograph analysis and new tools for time series analysis in this field of research.As in many others binary karst system the captured waters of the Coulazou river travel through conduits and preferential flow paths in the vadose zone, and join the saturated zone of the aquifer. This river is an ephemeral river in a Mediterranean context where rapid and intense floods occur each year. This hydrologic behaviour is appropriate to study the transfer of a flood through a karst area. The water level in caves, the rainfall all over the karst aquifer catchment area, the piezometric level within the karst aquifer and the discharge in the river upstream and downstream of the karst aquifer are measured in order to understand the Karst/River exchanges. During a flood the modification of the surface flows in the river is treated as a Linear Time-Invariant system (LTI system). Correlation and spectral analyses are used to understand how the LTI system dissipates or enhances the flood wave energy. For several floods, the frequency response function estimations are interpreted in term of flood wave modification through the karst area. In this way, according to the initial state of the Karst/River system, the autogenic and/or allogenic recharge of the aquifer may induce surge flows and a significant karst contribution to surface flows. |
Sinkholes in karst mining areas in China and some metho... Engineering Geology |
Engineering Geology, Volume 52, Issues 1-2, March 1999, Pages 45-50 Li Gongyu, Zhou Wanfang Abstract Mining of coal, lead and zinc, gold, and iron ore deposits in karst areas has been closely associated with sinkholes in China. Surface collapse causes an increase in mine water drainage and the possibility of major water inflow from karst aquifers, which threatens the environment in mining areas and endangers the mine safety. A combination of factors including soil weight, buoyancy, suffusion process and vacuum suction can contribute to the sinkhole formation. The key measures to prevent sinkholes in mining areas are to control the amount of mine drainage, reduce water level fluctuation, seal-off karst conduits and subsurface cavities in the overlying soil, prevent water inflow, and/or to increase gas pressure in the karst conduits. |
View More Related Articles |
Engineering and environmental problems in karst — An introduction