The need to reduce both point and diffuse phosphorus pollution to aquatic ecosystems is widely recognised and in order to achieve this, identification of the different pollutant sources is essential. Recently, a stable isotope approach using oxygen isotopes within phosphate (delta O-18(pO4)) has been used in phosphorus source tracing studies. This approach was applied in a one-off survey in September 2013 to the River Taw catchment in south-west England where elevated levels of phosphate have been reported. River water delta O-18(pO4) along the main channel varied little, ranging from +17.1 to + 18.8%0. This was no >0.3%0 different to that of the isotopic equilibrium with water (E delta O-18(pO4)). The delta O-18(pO4) in the tributaries was more variable (+ 17.1 to +18.8%0), but only deviated from E delta O-18(pO4) by between 0.4 and 0.9%0. Several potential phosphate sources within the catchment were sampled and most had a narrow range of delta O-18(PO4) values similar to that of river E delta O-18(pO4). Discharge from two waste water treatment plants had different and distinct delta O-18(pO4) from one another ranging between +16.4 and +19.6%0 and similar values to that of a dairy factory final effluent (+16.5 to +17.8%0), mains tap water (+17.8 to +18.4%0), and that of the phosphate extracted from river channel bed sediment (+ 16.7 to +17.6L). Inorganic fertilizers had a wide range of values (+13.3 to +25.9%0) while stored animal wastes were consistently lower (+12.0 to +15.0%0) than most other sources and E delta O-18(pO4). The distinct signals from the waste water treatment plants were lost within the river over a short distance suggesting that rapid microbial cycling of phosphate was occurring, because microbial cycling shifts the isotopic signal towards E delta O-18(pO4). This study has added to the global inventory of phosphate source delta O-18(pO4) values, but also demonstrated the limitations of this approach to identifying phosphate sources, especially at times when microbial cycling is high. (C) 2016 The Authors. Published by Elsevier B.V.
机构:
Univ Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
US EPA, Natl Res Council, Western Ecol Div, 200 SW 35th St, Corvallis, OR 97333 USAUniv Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
Lin, Jiajia
Bohlke, John K.
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US Geol Survey, Reston, VA 20192 USAUniv Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
Bohlke, John K.
Huang, Sheng
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Univ Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
DC Dept Energy & Environm, Washington, DC 20002 USAUniv Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
Huang, Sheng
Gonzalez-Meler, Miguel
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Univ Illinois, Dept Biol Sci, Chicago, IL 60607 USAUniv Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
Gonzalez-Meler, Miguel
Sturchio, Neil C.
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Univ Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
Univ Delaware, Dept Geol Sci, Newark, DE 19716 USAUniv Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA
机构:
State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
University of Chinese Academy of SciencesState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
Yongxue Ji
Jingan Chen
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State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of SciencesState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
Jingan Chen
Runyu Zhang
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State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of SciencesState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
Runyu Zhang
Yong Liu
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State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
University of Chinese Academy of SciencesState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
Yong Liu
Jingfu Wang
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State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of SciencesState Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences
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State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
University of Chinese Academy of Sciences, BeijingState Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
Ji Y.
Chen J.
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State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, GuiyangState Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
Chen J.
Zhang R.
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State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, GuiyangState Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
Zhang R.
Liu Y.
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State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
University of Chinese Academy of Sciences, BeijingState Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
Liu Y.
Wang J.
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State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, GuiyangState Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang