Thursday, October 18, 2001, at 10:00 a.m.-12:00 Noon
Room #709, EPA Fairchild Building
499 S. Capitol Street
Washington, D.C.
Teleconference audio bridge Phone is 703-648-5032
Conference code #41883
ATTENDEES:
Katherine Lins, USGS/Water
David Wells, EPA/OW/OST
Michael Plastino, EPA/OW/IO
Jim Currens, KY Geologic Survey/UnivKY
Joseph Ray, KY Division of Water
Keven Roth, USGS/Geography
Doug Nebert, FGDC
Hal Hallett, DOI/BLM
Marilyn Ginsberg, EPA/OW/OGWDW
Bob Pierce, USGS/Water
Wendy Blake-Coleman, EPA/EIO
AGENDA
10:00 |
Introductions
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Status of
Watershed Boundaries Datasets (WBD)
Power Point
Presentation - (1,392KB) |
Bob Pierce |
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Affect of
Karst Terrain on Water Delineation (summary below)
(Power
Point Presentation) - (8,392KB) |
James Currens
Kentucky Geological Survey &
Joseph Ray
Kentucky Division of Water
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12:00 |
Adjourn |
Bob Pierce
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Summary of Currens & Ray
Presentation:
The focus of Mr. Curren's and Mr. Ray's was
although water in the Karst basins is considered groundwater, the
flow behavior of the systems is in fact more like
surfacewater. Conduit flow in these systems is typically
convergent, fast, and turbulent. The stated purposes of the HUC
delineation is to provide standardized data sets for "watershed
management, water quality initiatives, watershed modeling,
resource inventory and assessment and establishing total maximum
daily loads" (Federal Standard for Delineation of Hydrologic Unit
Boundaries, draft of June 4, 2001). We argue that all of these
uses are dependent on accurate watershed delineation which the HUC
boundaries do not provide in many Karst areas. This was recently
demonstrated by a fuel spill in the Turnhole Spring basin, a
tributary of the Green River, which discharges within Mammoth Cave
National Park. The HUC map erroneously attributed the drainage
from the spill site to the Barren River. Thus, either the
recommended use for the HuC boundaries must be revised and limited
or the boundaries must be revised when data or karst basins
becomes available. |
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