Use of Hydrologic Time Series Data for Analysis the Karstic Drought Characteristic

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Karstification creates significant heterogeneity of hydraulic conductivity within the aquifer, where flows are organized to a hierarchical structure, from the surface to the spring. A karstic aquifer subjected to groundwater flood and drought, as a site for the occurrence of karst groundwater, is the main or unique focus for groundwater development and utilization in southwestern China. The present paper introduces a methodology devoted to groundwater drought hazard assessment. It focuses on groundwater drought by applying of the spring time series for an estimate and categorization of operating resources of groundwater. The results show that a permit for use of water for ER1+ER2 up to 0.48 m3/s, with the exceeding probability 80% selected for representing dry. The longest drought duration time was happened in the year 1993 with the 2.9×106m3 shortage of water volume. Groundwater drought frequency analysis provides a useful tool for water management.

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127-131

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September 2014

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© 2014 Trans Tech Publications Ltd. All Rights Reserved

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[1] Morrison, J.E. and Smith, J.A., Stochastic modelling of flood peaks using the generalized extreme value distribution, Water Resources Research 38 (12) (2002), 1305-1317.

DOI: 10.1029/2001wr000502

Google Scholar

[2] Mitosek, H.T., Strupczewski, W.G., Singh, V.P., Three procedures for selection of annual flood peak distribution, Journal of Hydrology 323 (2006), 57-73.

DOI: 10.1016/j.jhydrol.2005.08.016

Google Scholar

[3] Beretta, G.P., Avanzini, M., Pagotto, A., Managing groundwater rise: experimental results and modelling of water pumping from a quarry lake in Milan urban area (Italy), Environmental Geology 45 (2004), 600-608.

DOI: 10.1007/s00254-003-0918-7

Google Scholar

[4] Mangin, A., Progrès récents dans l'étude hydrogéologique des karsts , [Recent progress in the study of karst hydrogeology]. Stygologia 1(3) (1985), 239-257.

Google Scholar

[5] Yuan, D.X., Aspects on the new round land and resources survey in karst rock desertification areas of south China (in Chinese), J Carsolog Sin 19(2) (2000), 103-108.

Google Scholar

[6] Yu, J.B., Yang, L.Z., Fang, M.Z. Typical study on developmental regularity of karst China: assessment and utilization of water resources in the southern Puding, Guizhou province (in Chinese),. Publishing House of Science, Beijing (1990).

Google Scholar

[7] Liu, LH., Shu, L.C., Chen, X.H. et al The Hydrologic functionand behaviors of the Houzhai underground river basin, GuizhouProvince, southwestern China, Hydrogeol J 18(2010a), 509-518.

DOI: 10.1007/s10040-009-0518-z

Google Scholar

[8] Liu, LH., Shu, L.C., Chen, X.H. et al Rainfall-Driven Spring Hydrograph Modeling in a Karstic Water System, Southwestern China, Water Resources Management 24(2010b), 2689-2701.

DOI: 10.1007/s11269-009-9574-3

Google Scholar