TY - JOUR
T1 - Reduction of fecal indicator bacteria (FIB) in the Ballona Wetlands saltwater marsh (Los Angeles County, California, USA) with implications for restoration actions
AU - Dorsey, John H.
AU - Carter, Patrick M.
AU - Bergquist, Sean
AU - Sagarin, Rafe
N1 - Funding Information:
We wish to sincerely thank the following students who enthusiastically participated in the field and laboratory studies: Loyola Marymount University – Sarika Doshi, Nick Fugate, Tim Tawakol, Anh Nguyen, Arthur Bilikian, Lindsay Vitort; UCLA – Liz Bernier and Natalie Diaz; Chadwick High School – Swati Yanamadala. This study would not have been possible without their help. Dr. Eric Stein and Ken Schiff, both from the Southern California Coastal Water Research Project, kindly reviewed the manuscript, providing many valuable suggestions. We also wish to acknowledge the anonymous reviewers who also made excellent recommendations to improve the manuscript. Funding for this study was provided through several sources: a LMU Continuing Faculty Summer Grant, a grant from the Santa Monica Bay Restoration Commission , and in part from a University of California Marine Council grant to Stanley Grant ( UCI ) and Richard Ambrose ( UCLA ).
PY - 2010/8
Y1 - 2010/8
N2 - A benefit of wetland preservation and restoration is the ecosystem service of improving water quality, typically assessed based on bacterial loading. The Ballona Wetlands, a degraded salt marsh of approximately 100 ac located on the southern border of Marina Del Rey (Los Angeles County, California, USA) are currently the focus of publicly funded restoration planning. The wetlands receive tidal water, usually contaminated with fecal indicator bacteria (FIB: total and fecal coliforms, Escherichia coli, enterococci) from the adjacent Ballona Creek and Estuary. During the summer of 2007, two 24-h studies were conducted to determine FIB tidal dynamics within the wetland. Measurements of water flow and mean FIB concentrations (n = 3) were measured every 1.5 h to determine total FIB load estimates. FIB loading rates (MPN/s) were greatest during flood tides as water entered the wetlands, and then again during spring tide conditions when sediments were resuspended during swifter spring ebb flows. During daylight hours, the wetland acted as a sink for these bacteria as loads diminished, presumably by sunlight and other processes. Conversely, during late afternoon and night, the wetlands shifted to being a source as excess FIB departed on ebb flows. Therefore, the wetlands act as both a source and sink for FIB depending on tidal conditions and exposure to sunlight. Future restoration actions would result in a tradeoff - increased tidal channels offer a greater surface area for FIB inactivation, but also would result in a greater volume of FIB-contaminated resuspended sediments carried out of the wetlands on stronger ebb flows. As levels of FIB in Ballona Creek and Estuary diminish through recently established regulatory actions, the wetlands could shift into a greater sink for FIB.
AB - A benefit of wetland preservation and restoration is the ecosystem service of improving water quality, typically assessed based on bacterial loading. The Ballona Wetlands, a degraded salt marsh of approximately 100 ac located on the southern border of Marina Del Rey (Los Angeles County, California, USA) are currently the focus of publicly funded restoration planning. The wetlands receive tidal water, usually contaminated with fecal indicator bacteria (FIB: total and fecal coliforms, Escherichia coli, enterococci) from the adjacent Ballona Creek and Estuary. During the summer of 2007, two 24-h studies were conducted to determine FIB tidal dynamics within the wetland. Measurements of water flow and mean FIB concentrations (n = 3) were measured every 1.5 h to determine total FIB load estimates. FIB loading rates (MPN/s) were greatest during flood tides as water entered the wetlands, and then again during spring tide conditions when sediments were resuspended during swifter spring ebb flows. During daylight hours, the wetland acted as a sink for these bacteria as loads diminished, presumably by sunlight and other processes. Conversely, during late afternoon and night, the wetlands shifted to being a source as excess FIB departed on ebb flows. Therefore, the wetlands act as both a source and sink for FIB depending on tidal conditions and exposure to sunlight. Future restoration actions would result in a tradeoff - increased tidal channels offer a greater surface area for FIB inactivation, but also would result in a greater volume of FIB-contaminated resuspended sediments carried out of the wetlands on stronger ebb flows. As levels of FIB in Ballona Creek and Estuary diminish through recently established regulatory actions, the wetlands could shift into a greater sink for FIB.
KW - FIB loading
KW - Fecal indicator bacteria
KW - Tidal flux
KW - Wetlands
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U2 - 10.1016/j.watres.2010.06.012
DO - 10.1016/j.watres.2010.06.012
M3 - Article
C2 - 20591461
AN - SCOPUS:77955279254
SN - 0043-1354
VL - 44
SP - 4630
EP - 4642
JO - Water research
JF - Water research
IS - 15
ER -