Ground and surface water interactions in karst terrains: Some observations from along the Cody Scarp - PowerPoint PPT Presentation

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Ground and surface water interactions in karst terrains: Some observations from along the Cody Scarp

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Some observations from along the Cody Scarp. Jon Martin. Liz Screaton, PJ Moore ... Cody Scarp. 5. Martin and Gordon, 1997 ~21 cm of rain. Dye return ... – PowerPoint PPT presentation

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Title: Ground and surface water interactions in karst terrains: Some observations from along the Cody Scarp


1
Ground and surface water interactions in karst
terrainsSome observations from along the Cody
Scarp
  • Jon Martin
  • Liz Screaton, PJ Moore
  • Acknowledgements NSF, DEP, SRWMD
  • OLeno State Park, Ichetucknee State Park
  • Sheryl Gordon, Randy Dean, Brooke Sprouse,
    Jennifer Martin

2
How does flow in conduits and matrix interact?-
What can be learned from chemistry of spring
discharge?
Modified from White, 2002
3
  • Karst aquifers have two distinct ground water
    reservoirs
  • Conduits (gt 1 cm2)
  • Matrix (fracture and intergranular porosity)
  • Flow unimportant in low porosity matrix, e.g.
    Paleozoic aquifers
  • High porosity matrix important flow path and for
    storage, e.g. Floridan aquifer

4
StudyAreaCody Scarp
5
Mill Pond Spring, Ichetucknee River
21 cm of rain
Dye return
Martin and Gordon, 1997
6
Santa Fe RiverSink/Rise area
Sink Well
Rise Well
7
Travel time Sink ? Rise
8
Flow velocity, two floods
  1. Velocity constant through conduits
  2. Velocity depends on stage and discharge
  3. Discharge can be used to determine conduit size
  4. Determine residence time chemical sampling

9
Discharge at sink and riseevidence for
conduit-matrix exchange
10
Cl- concentrations vs. distance and through time
following 1998 El Nino floods
11
Seawater Sr Isotopes Through Time
12
Mixing Ocala Ls and seawater radiogenic
Sr?Some wells have more Ocala Sr than
othersRadiogenic Sr from Hawthorn Gp?
Modern Seawater 0.70917
0.7079Upper Ocala
13
Noble gas non-reactive in inorganic or organic
reactions. ? Loss from evasion to atmosphere.
14
Rn input and decay
10.53 masl
Excess Rn
222Rnmeas.-222Rncalc.
9.78 masl
Rn Deficit
12.2 masl
Distance from sink (m)
N 222Rn activity N0 initial 222Rn activity l
decay constant t time
15
Conclusions and Questions
  • Water exchanges between conduits and matrix (T,
    physical models, Cl concentrations)
  • Several sources of recharged water from
    confined region (Sr and Rn isotopes)
  • What roles do diffuse recharge and epikarst have
    in flow in conduits and matrix?
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