ANALYSIS OF GEOLOGIC SETTINGS AND HYDROLOGIC CONDITIONS THAT AFFECT RESTORED PITCHER PLANT BOG HABITAT, SUSSEX COUNTY, VIRGINIA
The tidal-flat facies of the Bacons Castle Formation underlie the rolling landscape of the Preserve. Analysis of split-spoon cores, and vibracore samples revealed bogs in that setting formed at toeslopes where groundwater seeps from extensive sand layers sandwiched between thick clay beds. Examination of bog stratigraphy across the toeslope using ground-penetrating radar reveals colluvial sand sheets overlie dense clay layers. Hydrographs from monitoring wells in those sand beds show relative stable water table elevations above the bog root zone existed even during summer drought conditions in 2010. Diurnal water table fluctuations reflected evapotranspiration cycles. Comparisons of ET rates between adjacent areas with different vegetation densities indicate a 103% increase in the volume of groundwater withdrawn by dense mixed pine/deciduous hardwood forest compared to sparsely-wooded longleaf pine savanna. Also, analysis of groundwater fluctuations before and after prescribed burning of the long-leaf savanna ecosystem in spring 2011 show a reduction in post-burn evapotranspiration rates. These results suggest long-leaf pine savanna ecosystems managed with annual prescribed burning withdraw less groundwater than loblolly pine woodlands, effectively increasing the volume of water available to supply the pitcher plant bog. This study will provide resource managers with information critical for restoring these rare wetland habitats.