Arid
DOI10.1016/j.jhydrol.2011.08.060
Estimating recharge in fractured aquifers of a temperate humid to semiarid volcanic island (Jeju, Korea) from water table fluctuations, and Cl, CFC-12 and H-3 chemistry
Hagedorn, Benjamin1,2; El-Kadi, Aly I.1,2; Mair, Alan1,2; Whittier, Robert B.2; Ha, Kyoochul3
通讯作者Hagedorn, Benjamin
来源期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
出版年2011
卷号409期号:3-4页码:650-662
英文摘要

Groundwater table fluctuations (WTF), chloride mass balance (CMB), apparent groundwater chlorofluorocarbon (CFC-12) ages and tritium (H-3) mean residence times were used to assess recharge rates on Jeju Island (Korea), where groundwater is the main source of potable water. Given the limitations of various techniques and the respective data, the methods yield median values of 687 mm/yr (WTF), 429 mm/yr (CMB), 423 mm/yr (CFC-12) and 394 mm/yr (H-3), which are lower than the multi-annual (1993-2002) average value calculated using the soil water budget (SWB) method (911 mm/yr). These underestimates are mainly due to most groundwater samples used for the analyses being located in the more arid low-land areas of the island. All methods yield highest recharge rates in the southern and eastern districts of Jeju implying a strong control of rainfall on the spatial recharge distribution. The spatial variability of recharge at the catchment scale is caused by spatially and temporally variable rainfall and evapotranspiration as well as the wide range in effective porosity and specific yield values of the aquifer lithologies. The WTF method yields reliable results in the coastal regions where low hydraulic gradients prevail. The CMB technique underestimates the recharge values of the SWB in all geographic districts probably as a result of anthropogenic Cl additions to groundwater and unaccounted for atmospheric Cl dry deposition. Median recharge estimates from the CFC-12 and H-3 data show the lowest spatial correlation with those from the SWB mainly as a result of vertical anisotropies and uncertainties in the determination of effective aquifer thicknesses particularly in the perched, high level areas. The here applied methods are useful for local calibration and validation of SWB estimates in lower parabasal regions where thin unsaturated zones prevail; however, due to their inability to predict recharge in the more remote upslope areas from which, as of yet, no groundwater data could be obtained, they cannot be applied to predict average recharge values representative for the whole island. (C) 2011 Elsevier B.V. All rights reserved.


英文关键词Groundwater Recharge Fractured aquifers Volcanic island Geochemistry Korea
类型Article
语种英语
国家USA ; South Korea
收录类别SCI-E
WOS记录号WOS:000296949600006
WOS关键词LUMPED-PARAMETER MODELS ; RESIDENCE TIME ANALYSES ; NITRATE CONTAMINATION ; SOUTH-KOREA ; GROUNDWATER RECHARGE ; SHALLOW GROUNDWATER ; TRACERS H-3 ; CHLOROFLUOROCARBONS CCL3F ; ENVIRONMENTAL ISOTOPES ; ATMOSPHERIC DEPOSITION
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向Engineering ; Geology ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/169290
作者单位1.Univ Hawaii Manoa, Water Resources Res Ctr, Honolulu, HI 96822 USA;
2.Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Dept Geol & Geophys, Honolulu, HI 96822 USA;
3.Korea Inst Geosci & Mineral Resources, Geol Environm & Groundwater Dept, Taejon 305350, South Korea
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Hagedorn, Benjamin,El-Kadi, Aly I.,Mair, Alan,et al. Estimating recharge in fractured aquifers of a temperate humid to semiarid volcanic island (Jeju, Korea) from water table fluctuations, and Cl, CFC-12 and H-3 chemistry[J],2011,409(3-4):650-662.
APA Hagedorn, Benjamin,El-Kadi, Aly I.,Mair, Alan,Whittier, Robert B.,&Ha, Kyoochul.(2011).Estimating recharge in fractured aquifers of a temperate humid to semiarid volcanic island (Jeju, Korea) from water table fluctuations, and Cl, CFC-12 and H-3 chemistry.JOURNAL OF HYDROLOGY,409(3-4),650-662.
MLA Hagedorn, Benjamin,et al."Estimating recharge in fractured aquifers of a temperate humid to semiarid volcanic island (Jeju, Korea) from water table fluctuations, and Cl, CFC-12 and H-3 chemistry".JOURNAL OF HYDROLOGY 409.3-4(2011):650-662.
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