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Factors influencing the extent and development of the oxic zone in sediments

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Abstract

Dissolved oxygen concentrations in river-sediment porewaters are reported and modelled using a zero-order reaction rate and the Monod equation. After mixing the sediments and allowing settling, the dissolved oxygen profile in the bed-sediment was expected to reach a steady-state rapidly (< 1 h). However changes in the vertical profile of oxygen over a period of 38 days revealed that the penetration of oxygen increased and the dissolved oxygen flux at the interface decreased with time, probably as the oxidation kinetics of organic matter and redox reactions in the sediment changed. Experiments with three contrasting silt and sand dominated sediments (organic matter content between 0.9 and 18%) at two water velocities (ca 10 and 20 cm s−1) showed that the dissolved oxygen profiles were independent of velocity for each of the sediments. The most important controls on the reaction rate were the organic matter content and specific surface area of the sediment. A viscous diffuse-boundary-layer above the sediment was only detected in the experiments with the silt sediment where the sediment oxygen demand was relatively high. In the coarser sediments, the absence of a diffuse layer indicated that slow oxidation processes in the sediment controlled the dissolved oxygen flux at the interface. The problem of determining a surface reference in coarse sediment is highlighted. The results are discussed with reference to other studies including those concerned with estuarine and marine sediments.

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References

  • Allan I.J., House W.A., Warren N., Parker A. and Carter J.E. 2001. A Pilot Study of the Movement of Permethrin into Freshwater Sediments. Symposium Proceedings No. 78. British Crop Protection Council, Brighton, pp. 107–112.

  • Benson B.B. and Krause D. Jr 1980. The concentration and isotopic fractionation of gases dissolved in freshwater in equilibrium with the atmosphere. 1. Oxygen. Limnol. Ocean. 25: 662–671.

    Google Scholar 

  • Barcelona M.J. 1983. Sediment oxygen demand fractionation, kinetics and reduced chemical substances. Water Res. 17: 1081–1093.

    Google Scholar 

  • Berninger U.G. and Markus H. 1997. Impact of flow on oxygen dynamics in photosynthetically active sediments. Aquatic Microbial Ecology 12: 291–302.

    Google Scholar 

  • Boudreau B.P. 1997. Diagenetic Models and Their Implementation. Springer-Verlang, New York.

    Google Scholar 

  • Bouldin D.R. 1968. Models for describing the diffusion of oxygen and mobile constituents across the mud-water interface. J. Ecol. 56: 77–87.

    Google Scholar 

  • Bowman G.T. and Delfino J.J. 1980. Sediment oxygen demand techniques: A review and comparison of laboratory and in situ systems. Water Res. 14: 491–499.

    Google Scholar 

  • Cae W.-J. and Sayles F.L. 1996. Oxygen penetration depths and fluxes in marine sediments. Mar. Chem. 52: 123–131.

    Google Scholar 

  • Chen G.-H., Leong I.-M., Liu J. and Huang J.-C. 1999. Study of the oxygen uptake by tidal river sediment. Wat. Res. 33: 2905–2912.

    Google Scholar 

  • Edwards R.W. and Rolley H.L.J. 1965. Oxygen consumption of river muds. J. Ecology 53: 1–19.

    Google Scholar 

  • Han P. and Bartels D.M. 1996. Temperature dependence of oxygen diffusion in H2O and D2O. J. Phys. Chem. 100: 5597–5602.

    Google Scholar 

  • House W.A., Denison F.H., Smith J.T. and Armitage P.D. 1995. An investigation of the effects of water velocity on inorganic phosphorus influx to a sediment. Environmental Pollution 89: 263–273.

    Google Scholar 

  • House W.A., Denison F.H., Warwick M.S. and Zhmud B.V. 2000. Dissolution of silica and the development of concentration profiles in freshwater sediments. Applied Geochemistry 15: 425–438.

    Google Scholar 

  • Jorgensen B.B. and Marais D.J.D. 1990. The diffusive boundary layer of sediments: Oxygen microgradients over a microbial mat. Limnol. Oceanogr. 35: 1343–1355.

    Google Scholar 

  • Jorgensen B.B. and Revsbech N.P. 1985. Diffusive boundary layers and the oxygen uptake of sediments and detritus. Limnol. Oceanogr. 30: 111–127.

    Google Scholar 

  • Josiam R. and Stefan H. 1999. Effect of flow velocity on sediment oxygen demand: Comparison of theory and experiment. J. American Water Resources Assoc. 35: 433–439.

    Google Scholar 

  • Jubb S., Guymer I., Licht G. and Prochnow J. 2001. Relating oxygen demand to flow: development of an in situ sediment oxygen demand measuring device. Water Sci. Technol. 43: 203–210.

    Google Scholar 

  • Llanso R.J. 1992. Effects of hyoxia on estuarine benthos: the lower Rappahannock River (Chesapeake Bay), a case study. Estuarine Coastal Shelf Sci. 35: 491–515.

    Google Scholar 

  • Mackenthun A.A. and Stefan H.G. 1998. Effect of flow velocity on sediment oxygen demand:experiments. J. Environ. Eng. 124: 222–230.

    Google Scholar 

  • Martin P., Goddeeris B. and Martens K. 1993. Oxygen concentration profiles in soft sediment of Lake Baikal (Russia) near the Selenga delta. Freshwater Biol. 29: 343–349.

    Google Scholar 

  • Nielson L.P., Christensen P.B., Revsbeck N.P. and Sorensen J. 1990. Dentrification and oxygen respiration in biofilms studied with a microsensor for nitrous oxide and oxygen. Microbial. Ecol. 19: 63–72.

    Google Scholar 

  • Nriagu O.J. and Dell C.I. 1974. Diagenetic formation of iron phosphates in recent lake sediments. Amer. Mineral. 59: 934–946.

    Google Scholar 

  • Pamatmat M.M. and Banse K. 1969. Oxygen consumption by the seabed. II In situ measurements to a depth of 180 m. Limnol. Ocean 14: 250–259.

    Google Scholar 

  • Park S.S. and Jaffe P.R. 1999. A numerical model to estimate sediment oxygen levels and demand. J. Environ. Quality 28: 1219–1226.

    Google Scholar 

  • Revsbech N.P., Sorensen J. and Blackburn T.H. 1980. Distribution of oxygen in marine sediments measured with microelectrodes. Limnol. Ocean 25: 403–411.

    Google Scholar 

  • Seiki T., Izawa H., Date E. and Sunahara H. 1994. Sediment oxygen demand in Hiroshima Bay. Water Res. 28: 385–393.

    Google Scholar 

  • Sincovec R.F. and Madsen N.K. 1975. Software for nonlinear partial differential equations. ACM Trans. Math. Software 1: 232–260.

    Google Scholar 

  • Thirkette K.M. and Barrett K.L. 1994. Relationship between sediment handling techniques and emergence success for the midge Chironomus riparius. Proc. Brighton Crop Prot. Conf.-Pests and Diseases 3: 1331–1336.

    Google Scholar 

  • Vink P.M. and Van der Zee S.E.A.T.M. 1977. Effect of oxygen status on pesticide transformation and sorption in undisturbed soil and lake sediments. Environ. Toxicol. Chem. 16: 608–616.

    Google Scholar 

  • Wersin P., Hohener P., Giovanoli R. and Stumm W. 1991. Early diagenetic influences on iron transformations in a fresh-water lake sediment. Chem. Geol. 90: 233–252.

    Google Scholar 

  • Woodruff S., House W.A., Callow M.E. and Leadbeater B.S.C. 1999. The effects of a developing bio-film on chemical changes across the sediment-water interface in a freshwater environment. Intern. Review of Hydrobiol. 84: 509–532.

    Google Scholar 

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  1. William A. House
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House, W.A. Factors influencing the extent and development of the oxic zone in sediments. Biogeochemistry 63, 317–334 (2003). https://doi.org/10.1023/A:1023353318856

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