Hydrogeology and hydrogeochemistry of a small, hard-rock island — the heavily stressed aquifer of Jersey

The fractured basement aquifer of Jersey provides 30% of the total water needs of the island plus baseflow to surface catchment storage. A 3-year field study has attempted to describe the groundwater resources in terms of quantity and quality. Borehole yields are typically less than 11s −1; the isla...

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Published inJournal of hydrology (Amsterdam) Vol. 163; no. 3; pp. 249 - 269
Main Authors Robins, N.S., Smedley, P.L.
Format Journal Article
LanguageEnglish
Published Amsterdam Elsevier B.V 1994
Elsevier Science
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Abstract The fractured basement aquifer of Jersey provides 30% of the total water needs of the island plus baseflow to surface catchment storage. A 3-year field study has attempted to describe the groundwater resources in terms of quantity and quality. Borehole yields are typically less than 11s −1; the island-wide estimate of transmissivity is 3 m 3 day −1 and effective aquifer thickness is 30–40 m although deeper circulation occurs in selected fracture systems. It is estimated that much of the renewable resource is exploited. Groundwaters are predominantly derived from recent recharge, most being oxidising with measurable tritium contents. There is widespread pollution from agricultural nutrients but natural denitrification is apparent in some areas.
AbstractList The fractured basement aquifer of Jersey provides 30% of the total water needs of the island plus baseflow to surface catchment storage. A 3-year field study has attempted to describe the groundwater resources in terms of quantity and quality. Borehole yields are typically less than 11s super(-1); the island-wide estimate of transmissivity is 3 m super(3) day super(-1) and effective aquifer thickness is 30-40 m although deeper circulation occurs in selected fracture systems. It is estimated that much of the renewable resource is exploited. Groundwaters are predominantly derived from recent recharge, most being oxidising with measurable tritium contents. There is widespread pollution from agricultural nutrients but natural denitrification is apparent in some areas.
The fractured basement aquifer of Jersey provides 30% of the total water needs of the island plus baseflow to surface catchment storage. A 3-year field study has attempted to describe the groundwater resources in terms of quantity and quality. Borehole yields are typically less than 11s −1; the island-wide estimate of transmissivity is 3 m 3 day −1 and effective aquifer thickness is 30–40 m although deeper circulation occurs in selected fracture systems. It is estimated that much of the renewable resource is exploited. Groundwaters are predominantly derived from recent recharge, most being oxidising with measurable tritium contents. There is widespread pollution from agricultural nutrients but natural denitrification is apparent in some areas.
The groundwater resources of the island of Jersey, the largest of the British Channel Islands group, were studied. The island was formed principally of Precambrian rocks. The fractured basement aquifer provided 30 per cent of the total water needs of the island, together with baseflow to surface catchment storage. Quantitative and qualitative aspects of groundwater resources were assessed in a 3-year field study. The aquifer had an average transmissivity of 3 m3 per d and an effective saturated thickness of 30-40 m. Deeper groundwater circulation occurred in selected fracture systems. The aquifer was stressed by heavy exploitation and anthropogenic pollution, particularly from agriculture.
Author Robins, N.S.
Smedley, P.L.
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Cites_doi 10.1180/minmag.1984.048.348.12
10.1016/0143-6228(89)90048-9
10.1111/j.1745-6584.1972.tb03586.x
10.1016/0022-1694(86)90155-1
10.1016/0043-1354(91)90203-3
10.1016/0022-1694(78)90001-X
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Issue 3
Keywords basement
tritium
thickness
ground water
hydrogeology
pollution
transmissivity
agriculture
drainage basins
boreholes
water resources
water storage
aquifers
water quality
islands
recharge
fresh water
fractures
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Elsevier Science
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  article-title: Granite-water interactions in relation to Hot Dry Rock geothermal development
  publication-title: British geological Survey Tech. Rpt.
  contributor:
    fullname: Edmunds
– start-page: 569
  year: 1987
  ident: 10.1016/0022-1694(94)90143-0_BIB12
  article-title: Hydrology in an island-continent context
  contributor:
    fullname: Matalas
– start-page: 93
  year: 1991
  ident: 10.1016/0022-1694(94)90143-0_BIB16
  article-title: Hydrogeological and hydrogeochemical survey of Jersey
  publication-title: British Geological Survey, Tech. Rep.
  contributor:
    fullname: Robins
– start-page: 117
  year: 1989
  ident: 10.1016/0022-1694(94)90143-0_BIB19
  article-title: Fluid circulation in the Carnmenellis granite: hydrogeological, hydrogeochemical and palaeofluid evidence
  publication-title: British Geological Survey Res. Rep.
  contributor:
    fullname: Smedley
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Snippet The fractured basement aquifer of Jersey provides 30% of the total water needs of the island plus baseflow to surface catchment storage. A 3-year field study...
The groundwater resources of the island of Jersey, the largest of the British Channel Islands group, were studied. The island was formed principally of...
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StartPage 249
SubjectTerms Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
Hydrogeology
Hydrology. Hydrogeology
Pollution, environment geology
Title Hydrogeology and hydrogeochemistry of a small, hard-rock island — the heavily stressed aquifer of Jersey
URI https://dx.doi.org/10.1016/0022-1694(94)90143-0
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