Show simple item record



Item Description

dc.contributor.author Kanehiro, Brian Y en_US
dc.contributor.author Peterson, Frank L en_US
dc.date.accessioned 2008-07-17T22:54:05Z en_US
dc.date.available 2008-07-17T22:54:05Z en_US
dc.date.issued 1977-07 en_US
dc.identifier.citation Kanehiro BY, Peterson FL. 1977. Groundwater recharge and coastal discharge for the northwest coast of the island of Hawai'i: A computerized water budget approach. Honolulu (HI): Water Resources Research Center, University of Hawaii at Manoa. WRRCT technical report, 110. en_US
dc.identifier.uri http://hdl.handle.net/10125/2008 en_US
dc.description.abstract The basic objectives of this study were to determine the average annual recharge to the groundwater body and the fresh groundwater discharge at the coastline, as well as the aquifer characteristics for an arid area located on the northwest coast of Hawai'i island between Kīholo Bay in the south and Puako in the north, and encompassing the land from the coast to approximately the 762-m (2,500-ft) elevation level. Of equal importance was the development of methodologies, namely, a computerized water budget and groundwater tidal analyses to calculate these quantities. The probable recharge to the groundwater body in this region was computed to be 143.83 x 10^6 m^3/yr (38 bil gal/yr). Due to the lack of hydrologic data for the area, a range of values was determined, with the maximum average annual recharge being 264.95 x 10^6 m3 (70 bil gal) and the minimum being 719.15 x 10^5 m3 (19 bil gal). Since there are 26 km (16 miles) of coastline in this area, this implies a probable average daily flux of 15,006 m^3/km (6.38 mil gal/mile) of coastline. Three different calculations were obtained for the hydraulic conductivity of the groundwater aquifer in the coastal region: two by tidal analysis, and a third based on the coastal discharge as determined by the water budget. The Werner and Noren method of tidal analysis gave an average value for Kz (hydraulic conductivity times average saturated depth of aquifer) in the vicinity of 'Anaeho'omalu Bay of 585,270 m^2/day (6.3 x 106 ft^2/day); the method by Cox gave a value for K in the same area of 1,027 m/day (3,369 ft/day). The coastal flux method gave a value for K of 2,771 m/day (9,092 ft/day). en_US
dc.description.sponsorship U.S. Dept. of the Interior and the Water Resources Research Center, University of Hawaii Grant/Contract No. 14-31-0001-6012 Project No. A-067-HI en_US
dc.format.extent vii + 83 pages en_US
dc.language.iso en-US en_US
dc.publisher Water Resources Research Center, University of Hawaii at Manoa en_US
dc.relation.ispartofseries WRRC Technical Report en_US
dc.relation.ispartofseries 110 en_US
dc.subject.lcsh Groundwater -- Hawaii -- Hawaii Island. en_US
dc.subject.lcsh Groundwater recharge -- Computer simulation. en_US
dc.subject.lcsh Kailua Kona (Hawaii) en_US
dc.subject.lcsh Water-supply -- Hawaii -- Hawaii Island. en_US
dc.title WRRCTR No.110 Groundwater Recharge and Coastal Discharge for the Northwest Coast of the Island of Hawai'i: A Computerized Water Budget Approach en_US
dc.type Report en_US
dc.type.dcmi Text en_US

Item File(s)

Files Size Format View
wrrctr110.pdf 4.283Mb PDF View/Open

This item appears in the following Collection(s)

Show simple item record

Search


Advanced Search

Browse

My Account

Statistics

About