T134 Springs: Groundwater-Influenced Ecosystems, Gaining Streams, and Wetlands
Monday, 5 November 2018
1:30 PM - 5:30 PM
Room 133
HYDROLOGIC MONITORING AND MANAGEMENT OF GROUNDWATER-FED WETLANDS IN THE SOUTHERN APPALACHIANS
Paper number: T134-10
Program: Technical Sessions
Time: 3:50 PM – 4:05 PM
Authors
-
Rebekah ReidAsheville Ecological Services Field Office, Asheville, NC
Abstract
Garland Seep can be classified for most of the year as a hypocrene wetland, where groundwater flow doesn’t reach the surface due to low discharge rates and high evapotranspiration. The site has been subject to controlled burns since the early 1900s, however, and the Nature Conservancy has continued the practice to combat woody vegetation and open the canopy. The burns reduce evapotranspiration (at least initially), cause a rapid rise in water levels (up to 0.3m), and have helped maintain a thriving population of federally-endangered green pitcher plants (Sarracenia oreophila).
Butt Pasture was an unsightly, overgrown agricultural field along a railroad track that nonetheless supported a population of the endangered Bunched Arrowhead (Sagittaria fasciculata) in spring-fed ditches. A restoration project in 2015 lowered the overall elevation of the pasture and created a series of channels and swales. New seeps along each of these features provide continuous and consistent water flow, and the bunched arrowhead are thriving.
Finally, Riverbend Bog (actually a fen) features standing water where the water table intersects channels or depressions and a large population of endangered mountain sweet pitcher plants (Sarracenia rubra ssp. Jonesii). It is frequently subjected to large volumes of nutrient-rich stormflow from upgradient residential development and pastureland. In addition to stimulating the growth of invasive and woody vegetation, the stormflow has also led to sediment deposition and/or scouring in various parts of the site. A hydrologic restoration planned for next year will attempt to retain or reroute stormwater, maintain the groundwater-fed features, and ultimately protect the Sarracenia.
Geological Society of America Abstracts with Programs. Vol. 50, No. 6
doi: 10.1130/abs/2018AM-324484
© Copyright 2018 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.