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VADOSE ZONE INTERACTION WITH HYPORHEIC ZONE NITROGEN CYCLING

VADOSE ZONE INTERACTION WITH HYPORHEIC ZONE NITROGEN CYCLING. Doug Higbee BAE 558 – Fluid Mechanics of Porous Materials May 8, 2009.

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VADOSE ZONE INTERACTION WITH HYPORHEIC ZONE NITROGEN CYCLING

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  1. VADOSE ZONE INTERACTION WITH HYPORHEIC ZONE NITROGEN CYCLING Doug Higbee BAE 558 – Fluid Mechanics of Porous Materials May 8, 2009

  2. The Hyporheic Zone is “… that part of the ground water/surface water continuum containing water originating both from the neighboring aquifer and from the river channel.” • Butturini, A., Bernal, S., Sabater,. S., and Sabater, F., 2002. The influence of riparian-hyporheic zone on the bydrological responses in an intermittent stream. Hydrology and Earth System Sciences, Volume 6(3), pp 515-525. Introduction

  3. Introduction

  4. Introduction

  5. Geologic Compartments of the Riparian Zone • Vadose Zone: portion that lies above the annual water table, characterized by variable saturation • Hyporheic Zone: portion that lies below annual water table, characterized by saturated flow Introduction

  6. Riparian Ecosystem • Vegetative growth • Rich soil deposits • Water availability • Benthic organisms • Wildlife habitat • Water quality • Stream biota • ESA (i.e., bull trout) Introduction

  7. Presentation Content • Nitrogen cycle • Delineation of the hyporheic zone • Fluid mechanics of the hyporheic zone • Watershed hydrology and the hyporheic zone • Nitrogen cycling in the hyporheic zone Introduction

  8. Nitrogen Cycle

  9. Benefits of Nitrogen • Essential element for all plants and animals • Creation of proteins • Amino acids (DNA & RNA) • Plant respiration • All nitrogen obtained by animals can be traced back to the eating of plants at some stage of the food chain. Nitrogen Cycle

  10. Nitrogen Fixation • Necessary to free up nitrogen from gas form for use by organisms. Fixation through: • Lightning • Nitrogen fixing bacteria • Through the process of mineralization (ammonification) nitrogen is also converted from organic nitrogen to: • Ammonium (NH4-) • Nitrite (NO2-) • Nitrate (NO3-) Nitrogen Cycle

  11. Nitrification: Conversion of ammonia to nitrates • Primarily by soil bacteria • Also by bacteria in hyporheic zone • Aerobic environment • nitrosomonas • nitrobacter Nitrogen Cycle

  12. Denitrification: reduction of nitrates to nitrogen gas (N2) • Anaerobic environment • Deeper regions of the hyporheic zone • Pseudomonas • Clostridium Nitrogen Cycle

  13. Boundary – surface water/ground water • Does not necessarily extend to outer riparian zone • Oxygenated surface water • Benthic habitat extending below vegetated area • Extents • Can extend hundreds of meters from the stream bank, and greater. • Depending on fluvial geomorphology and surrounding topography • Field methods • Shallow wells • Monitor water chemistry and gradients • Tracer injection • Monitor with time domain reflectometry or ground-penetrating radar Hyporheic Zone Delineation

  14. Monitoring Wells • Dissolved Oxygen (DO) • Dissolved Organic Carbon (DOC) • Groundwater gradient determination Hyporheic Zone Delineation

  15. Tracer Injection Hyporheic Zone Delineation

  16. Tracer Injection • Monitoring with Ground-Penetrating Radar John Bradford (Boise State University) Michael Gooseff (Penn State University) Jim McNamara (Boise State University) http://water.engr.psu.edu/gooseff/gpr_hz_proj.html Hyporheic Zone Delineation

  17. Tracer Injection • Piezometers • 20cm depth • 40cm depth Hyporheic Zone Delineation

  18. Tracer Injection Hyporheic Zone Deliniation

  19. Tracer Injection Hyporheic Zone Delineation

  20. Tracer Injection Hyporheic Zone Delineation

  21. Potentiometric surface maps • Ground water elevation • Horizontal direction of ground water flow • Useful for Qualitative flux analysis • Not useful for quantifying flux Hyporheic Zone Delineation

  22. Flow/flux determination • Fluvial geomorphology • Typically for Saturated Flow • Darcy’s Law: q=K(dh/dx) • Directional • Hyporheic – parallel to stream flow • Vadose/regional groundwater – perpendicular to stream flow • Residence Time Hyporheic Zone Fluid Mechanics

  23. Fluvial Geomorphology Hyporheic Zone Fluid Mechanics

  24. Stream structures and sinuosity Hyporheic Zone Fluid Mechanics

  25. Degree of saturation • Hyporheic saturated flow/non-saturated flow Hyporheic Zone Fluid Mechanics

  26. Residence Time • Average linear velocity • V=(K/n)(dh/dl) • Hyporheic zone deliniation • Operational definition, • open to interpretation • Hours -> Days -> Weeks Hyporheic Zone Fluid Mechanics

  27. Hydrologic Cycles • surface water level fluctuation • flux gradients • Dynamic groundwater surface water interaction Watershed Hydrology and the Hyporheic Zone

  28. Ephemeral Streams Watershed Hydrology and the Hyporheic Zone

  29. Ephemeral Streams Watershed Hydrology and the Hyporheic Zone

  30. Riparian zone hydraulic recharge • Vadose zone • Seasonal recharge (longer) • Hyporheic zone • Flood frequency (shorter) Watershed Hydrology and the Hyporheic Zone

  31. Nitrogen cycle in the hyporheic zone is directly affected by hydraulics and watershed hydrology • Degree of Saturation affects transport • Hydraulics affect residence time • Hyporheic exchange- • Hyporheic zones can be a source or sink of NH4 Nitrogen Cycling in the Hyporheic Zone

  32. Basic diagram of the nitrogen cycle. Nitrogen Cycling in the Hyporheic Zone

  33. Dissolved Oxygen (DO) rich environment enables nitrification (aerobic conditions) • Continuous mixing of surface water and groundwater • Dissolved Organic Carbon (DOC) rich environment enables denitrification (anaerobic conditions) • Flood deposits - colloidal DOC transported through porous media • Typically the most common source of electrons Nitrogen Cycling in the Hyporheic Zone

  34. Reduced mineral phases also contribute to denitrification (Mn2+, Fe2+, S2-) • Clay particles can also be a significant source for denitrification • pH controls this process • Sorption-desorption Nitrogen Cycling in the Hyporheic Zone

  35. Nitrogen Cycling in the Hyporheic Zone

  36. The hyporheic zone can potentially play a significant role in the removal of nitrogen from streams and rivers. • Understanding the factors that influence gradients and hydraulics is essential for analysis. • Calculations of nitrogen load from regional ground water to a river that do not account “…for hyporheic zone chemical and biological transformations, could result in significant errors.” • Hinkle, S.R., Duff, J.H., Triska, F.J., Laenen, A., Gates, E.B., Bencala, K.E., Wentz, D.A., and Silva, S.R., 2001. Linking hyporheic flow and nitrogen cycling near the Willamette River – a large river in Oregon, USA, Journal of Hydrology, Volume 244, Issues 3-4, pp 157-180. Conclusion

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