TY - JOUR
T1 - Improving riparian wetland conditions based on infiltration and drainage behavior during and after controlled flooding
AU - Russo, Tess A.
AU - Fisher, Andrew T.
AU - Roche, James W.
N1 - Funding Information:
This research was supported by the Committee on Research (University of California, Santa Cruz), the US National Science Foundation Graduate Fellowship Program, and the US National Park Service (Award J8CO790007). Critical lab and field support was provided by Dan Sampson, Lucas Beem, Kerri Johnson, Ted Baker, Brianne Davidson, Aaron Rinehart, Josh Baccei, and Roger Putnam. This manuscript benefited from thoughtful reviews by G. Stock and M. Buhler, and two anonymous reviewers.
PY - 2012/4/11
Y1 - 2012/4/11
N2 - We present results of an observational and modeling study of the hydrologic response of a riparian wetland to controlled flooding. The study site is located in Poopenaut Valley, Yosemite National Park (USA), adjacent to the Tuolumne River. This area is flooded periodically by releases from the Hetch Hetchy Reservoir, and was monitored during one flood sequence to assess the relative importance of inundation versus groundwater rise in establishing and maintaining riparian wetland conditions, defined on the basis of a minimum depth and duration of soil saturation, and to determine how restoration benefits might be achieved while reducing total flood discharge. Soil moisture data show how shallow soils were wetted by both inundation and a rising water table as the river hydrograph rose repeatedly during the controlled flood. The shallow groundwater aquifer under wetland areas responded quickly to conditions in the adjacent river, demonstrating a good connection between surface and subsurface regimes. The observed soil drainage response helped to calibrate a numerical model that was used to test scenarios for controlled flood releases. Modeling of this groundwater-wetland system suggests that inundation of surface soils is the most effective mechanism for developing wetland conditions, although an elevated water table helps to extend the duration of soil saturation. Achievement of wetland conditions can be achieved with a smaller total flood release, provided that repeated cycling of higher and lower river elevations is timed to benefit from the characteristic drainage behavior of wetland soils. These results are robust to modest variations in the initial water table elevation, as might result from wetter or dryer conditions prior to a flood. However, larger changes to initial water table elevation, as could be associated with long term climate change or drought conditions, would have a significant influence on wetland development. An ongoing controlled flooding program in Poopenaut Valley should help to distribute fine grained overbank deposits in wetland areas, extending the period of soil water retention in riparian soils.
AB - We present results of an observational and modeling study of the hydrologic response of a riparian wetland to controlled flooding. The study site is located in Poopenaut Valley, Yosemite National Park (USA), adjacent to the Tuolumne River. This area is flooded periodically by releases from the Hetch Hetchy Reservoir, and was monitored during one flood sequence to assess the relative importance of inundation versus groundwater rise in establishing and maintaining riparian wetland conditions, defined on the basis of a minimum depth and duration of soil saturation, and to determine how restoration benefits might be achieved while reducing total flood discharge. Soil moisture data show how shallow soils were wetted by both inundation and a rising water table as the river hydrograph rose repeatedly during the controlled flood. The shallow groundwater aquifer under wetland areas responded quickly to conditions in the adjacent river, demonstrating a good connection between surface and subsurface regimes. The observed soil drainage response helped to calibrate a numerical model that was used to test scenarios for controlled flood releases. Modeling of this groundwater-wetland system suggests that inundation of surface soils is the most effective mechanism for developing wetland conditions, although an elevated water table helps to extend the duration of soil saturation. Achievement of wetland conditions can be achieved with a smaller total flood release, provided that repeated cycling of higher and lower river elevations is timed to benefit from the characteristic drainage behavior of wetland soils. These results are robust to modest variations in the initial water table elevation, as might result from wetter or dryer conditions prior to a flood. However, larger changes to initial water table elevation, as could be associated with long term climate change or drought conditions, would have a significant influence on wetland development. An ongoing controlled flooding program in Poopenaut Valley should help to distribute fine grained overbank deposits in wetland areas, extending the period of soil water retention in riparian soils.
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U2 - 10.1016/j.jhydrol.2012.02.022
DO - 10.1016/j.jhydrol.2012.02.022
M3 - Article
AN - SCOPUS:84858442169
SN - 0022-1694
VL - 432-433
SP - 98
EP - 111
JO - Journal of Hydrology
JF - Journal of Hydrology
ER -