4.7 Article

Complementary effects of surface water and groundwater on soil moisture dynamics in a degraded coastal floodplain forest

Journal

JOURNAL OF HYDROLOGY
Volume 398, Issue 3-4, Pages 221-234

Publisher

ELSEVIER
DOI: 10.1016/j.jhydrol.2010.12.019

Keywords

Dynamic factor analysis; Soil moisture; Vadose zone; Surface water; Groundwater; Floodplain

Funding

  1. South Florida Water Management District (SFWMD)
  2. University of Florida

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Restoration of degraded floodplain forests requires a robust understanding of surface water, groundwater, and vadose zone hydrology. Soil moisture is of particular importance for seed germination and seedling survival, but is difficult to monitor and often overlooked in wetland restoration studies. This research hypothesizes that the complex effects of surface water and shallow groundwater on the soil moisture dynamics of floodplain wetlands are spatially complementary. To test this hypothesis, 31 long-term (4-year) hydrological time series were collected in the floodplain of the Loxahatchee River (Florida, USA), where watershed modifications have led to reduced freshwater flow, altered hydroperiod and salinity, and a degraded ecosystem. Dynamic factor analysis (DFA), a time series dimension reduction technique, was applied to model temporal and spatia variation in 12 soil moisture time series as linear combinations of common trends (representing shared but unexplained, variability) and explanatory variables (selected from 19 additional candidate hydrological time series). The resulting dynamic factor models yielded good predictions of observed soil moisture series (overall coefficient of efficiency = 0.90) by identifying surface water elevation, groundwater elevation, and net recharge (cumulative rainfall-cumulative evapotranspiration) as important explanatory variables. Strong and complementary linear relationships were found between floodplain elevation and surface water effects (slope = 0.72, R-2 = 0.86, p < 0.001), and between elevation and groundwater effects (slope = -0.71, R-2 = 0.71, p = 0.001), while the effect of net recharge was homogenous across the experimental transect (slope = 0.03, R-2 = 0.05, p = 0.242). This study provides a quantitative insight into the spatial structure of groundwater and surface water effects on soil moisture that will be useful for refining monitoring plans and developing ecosystem restoration and management scenarios in degraded coastal floodplains. (C) 2010 Elsevier B.V. All rights reserved.

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