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Sources of Nutrients and Fecal Indicator Bacteria to Nearshore Waters on the North Shore of Kaua`i (Hawai`i, USA)

Karen L. Knee1, 3 Contact Information, Blythe A. LaytonContact Information, Joseph H. Street1, 3 Contact Information, Alexandria B. BoehmContact Information and Adina PaytanContact Information

(1)  Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
(2)  Environmental and Water Studies, Department of Civil and Environmental Engineering, Stanford University, Stanford, CA 94305, USA
(3)  Institute of Marine Sciences, University of California, Santa Cruz, CA 95064, USA

Received: 12 December 2007  Revised: 7 May 2008  Accepted: 28 May 2008  Published online: 2 July 2008

Abstract  Water quality monitoring in Hanalei Bay, Kaua`i (Hawai`i, USA) has documented intermittent high concentrations of nutrients (nitrate, phosphate, silica, and ammonium) and fecal indicator bacteria (FIB, i.e., enterococci and Escherichia coli) in nearshore waters and spurred concern that contaminated groundwater might be discharging into the bay. The present study sought to identify and track sources of nutrients and FIB to four beaches in Hanalei Bay and one beach outside the bay, together representing a wide range of land uses. 223Ra and 224Ra activity, salinity, nutrient and FIB concentrations were measured in samples from the coastal aquifer, the nearshore ocean, springs, the Hanalei River, and smaller streams. In addition, FIB concentrations in beach sands were measured at each site, and the enterococcal surface protein (esp) gene assay was used to investigate whether the observed FIB originated from a human source. Nutrient concentrations in groundwater were significantly higher than in nearshore water, inversely correlated to salinity, and highly site specific, indicating local controls on groundwater quality. Fluxes of groundwater into Hanalei Bay were calculated using a mass-balance approach and represented at least 2–10% of river discharges. However, submarine groundwater discharge (SGD) may provide 2.7 times as much nitrate + nitrite to Hanalei Bay as does the Hanalei River. It may also provide significant fluxes of phosphate and ammonium, comprising 15% and 20% of Hanalei River inputs, respectively. SGD-derived silica inputs to the bay comprised less than 3% of Hanalei River inputs. FIB concentrations in groundwater were typically lower than those in nearshore water, suggesting that significant FIB inputs from SGD are unlikely. Positive esp gene assays suggested that some enterococci in environmental samples were of human fecal origin. Identifying how nutrients and FIB enter nearshore waters will help environmental managers address pressing water quality issues, including exceedances of the state Enterococcus water quality standard and nutrient loading to coral reefs.

Keywords  Hanalei (Kaua`i, Hawai`i, USA) - Submarine groundwater discharge (SGD) - Coastal water quality - Nutrients - Fecal indicator bacteria (FIB) - Radium isotopes - Land use


Contact Information Karen L. Knee (Corresponding author)
Email: klknee@stanford.edu

Contact Information Blythe A. Layton
Email: laytonba@stanford.edu

Contact Information Joseph H. Street
Email: jstreet@stanford.edu

Contact Information Alexandria B. Boehm
Email: aboehm@stanford.edu

Contact Information Adina Paytan
Email: apaytan@ucsc.edu

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