Groundwater in the Coastal Zones of Asia-Pacific

Volume 7 of the series Coastal Research Library pp 27-46


A Geochemical and Geophysical Assessment of Coastal Groundwater Discharge at Select Sites in Maui and O’ahu, Hawai’i

  • P. W. SwarzenskiAffiliated withU.S. Geological Survey Email author 
  • , H. DulaiovaAffiliated withDepartment of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii
  • , M. L. DailerAffiliated withDepartment of Botany, University of Hawaii, Manoa
  • , C. R. GlennAffiliated withDepartment of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii
  • , C. G. SmithAffiliated withU.S. Geological Survey
  • , C. D. StorlazziAffiliated withU.S. Geological Survey

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This chapter summarizes fieldwork conducted to derive new estimates of coastal groundwater discharge and associated nutrient loadings at select coastal sites in Hawai’i, USA. Locations for this work were typically identified based on pronounced, recent ecosystem degradation that may at least partially be attributable to sustained coastal groundwater discharge. Our suite of tools used to evaluate groundwater discharge included select U/Th series radionuclides, a broad spectrum of geochemical analytes, multi-channel electrical resistivity, and in situ oceanographic observations.

Based on the submarine groundwater discharge tracer 222Rn, coastal groundwater discharge rates ranged from about 22–50 cm per day at Kahekili, a site in the Ka’anapali region north of Lahaina in west Maui, while at Black Point in Maunalua Bay along southern O’ahu, coastal groundwater discharge rates ranged up to 700 cm per day, although the mean discharge rate at this site was 60 cm per day. The water chemistry of the discharging groundwater can be dramatically different than ambient seawater at both coastal sites. For example, at Kahekili the average concentrations of dissolved inorganic nitrogen (DIN), dissolved silicate (DSi) and total dissolved phosphorus (TDP) were roughly 188-, 36-, and 106-times higher in the discharging groundwater relative to ambient seawater, respectively. Such data extend our basic understanding of the physical controls on coastal groundwater discharge and provide an estimate of the magnitude and physical forcings of submarine groundwater discharge and associated trace metal and nutrient loads conveyed by this submarine route.