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Generation of hydrogen sulfide in the deepest part of a reservoir under anoxic water conditions

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Abstract

The generation of hydrogen sulfide in a reservoir can be characterized by a massive influx of organic matter, manifest thermal stratification, and an extreme anoxic state specifically at the hypolimnion layer in summer. It has been reported that in this deep layer of a thermally stratified water body, where dissolved oxygen is depleted and redox potential falls sharply below the value of zero, the prolonged oxygen-free period and negative redox potential may potentiate the production of toxic hydrogen sulfide. The main aim of this study was to simulate the varying concentration of hydrogen sulfide at the deepest part of the reservoir based on intensive monitoring of water quality parameters. A one-dimensional hydraulic ecosystem model was applied to simulate vertical distribution of dissolved oxygen (DO) continuously in time. Based on the simulated DO, the length of continuous oxygen-free state in the deepest layer was specified and then utilized to estimate the temporal changes of oxidation–reduction potential (ORP) using a polynomial regression model. Finally, a linear regression model for hydrogen sulfide was fitted from the observed ORP, based on which, the temporal changes of hydrogen sulfide concentration were modeled using the simulated ORP. The introduction of several calculations gave good simulated results of hydrogen sulfide concentration, and this approach can be considered useful for predictive and explanatory purposes in further research investigating toxic hydrogen sulfide at the hypolimnion of the reservoir.

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References

  • Carla MK, Andrew M, Ryan JS, Christine S (2012) Redox stratification and salinization of three kettle lakes in Southwest Michigan, USA. Water Air Soil Pollut 223:1415–1427

    Article  Google Scholar 

  • Dake JMK, Harleman DRF (1969) Thermal stratification in lakes: analytical and laboratory studies. Water Resour Res 5:484

    Article  Google Scholar 

  • Dunnette DA, Chynoweth DP, Mancy KH (1985) The source of hydrogen sulfide in anoxic sediment. Water Res 19:875–884

    Article  CAS  Google Scholar 

  • Harada M, Hiramatsu K, Saitoh T, Mori M, Marui A (2009) Dynamics of water qualities in a eutrophic water body under scarce underwater light environment. J Rainwater Catchment Syst 14:87–96

    Google Scholar 

  • Henderson-Sellers B (1985) A simple formula for vertical eddy diffusion coefficients under conditions of nonneutral stability. J Geophys Res 87:5860

    Article  Google Scholar 

  • Herlihy AT, Mills AL (1985) Sulfate reduction in freshwater sediments receiving acid mine drainage. Appl Environ Microbiol 49:179–186

    CAS  PubMed Central  PubMed  Google Scholar 

  • Kent WT, Bruce LK, Forrest EP (1990) Anonymous reservoir limnology. Wiley, Canada

    Google Scholar 

  • Kondo J, Yasuhiro S, Tetsuo I (1979) On wind-driven current and temperature profiles with diurnal period in the oceanic planetary boundary layer. J Phys Oceanogr 9:360

    Article  Google Scholar 

  • Luther G, Glazer B, Ma S, Trouwborst R, Shultz B, Druschel G, Kraiya C (2003) Iron and sulfur chemistry in a stratified lake: evidence for iron-rich sulfide complexes. Aquat Geochem 9:87–110

    Article  CAS  Google Scholar 

  • Mortimer CH (1941) The exchange of dissolved substances between mud and water in lakes. J Ecol 29:280–329

    Article  CAS  Google Scholar 

  • Smith LL, Donavon MO, Ira RA, Stven JB (1976) Effect of hydrogen sulfide on fish and invertebrates. EPA, Waterloo Wind Farm

    Google Scholar 

  • Stumm W, Morgan JJ (1973) Aquatic chemistry an introduction emphasizing chemical equilibria in natural waters. 1970, 583 S. Wiley, New York, London, Sydney, Toronto, p 117

    Google Scholar 

  • Zerkle AL, Kamyshny A Jr, Kump LR, Farquhar J, Oduro H, Arthur MA (2010) Sulfur cycling in a stratified euxinic lake with moderately high sulfate: constraints from quadruple S isotopes. Geochim Cosmochim Acta 74:4953–4970

    Article  CAS  Google Scholar 

Download references

Acknowledgments

This research was partly supported by a JSPS Grant-in-Aid for Scientific Research (B) (Project number: 19380138) and the Kyushu University New Campus Planning Office.

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Correspondence to Nguyen Thuy Do.

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Thuy Do, N., Yoshimura, Y., Harada, M. et al. Generation of hydrogen sulfide in the deepest part of a reservoir under anoxic water conditions. Paddy Water Environ 13, 101–113 (2015). https://doi.org/10.1007/s10333-013-0412-0

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  • DOI: https://doi.org/10.1007/s10333-013-0412-0

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