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Groundwater
Tracing in a Density-Stratified Aquifer using a SCUFA Submersible
Fluorometer
Cave-diving
scientists from the Exploration Research Institute (ERI) have conducted
annual research projects to study complex groundwater flows in Mexico's
Yucatan peninsula. Recently, ERI utilized the unique capabilities
of the Turner Designs SCUFA submersible fluorometer to aid in this
study.
Along the eastern
Caribbean coast of the Yucatan Peninsula, nearly all freshwater
discharges to the sea through extensive cave networks and springs
rather than by surface streams. This karst region is underlain by
an extensive network of cave passages that carry fresh groundwater
from the peninsula's interior to springs along the coast. The fresh
groundwater "floats" atop deeper saline groundwater. Within
10 km of the coast, the seaward-flowing freshwater and underlying
saline water begin to mix. The mixing of fresh and saline waters
creates a complex "mixing zone" of brackish water. The
mixing zone is often sharply stratified by the formation of haloclines
and thermoclines that segregate water masses of various densities.
In 2003, ERI
scientists worked in conjunction with the Grupo de Exploration de
Ox Bel Ha (GEO) to begin testing advanced instrumentation that can
quantify aquifer processes. Two applications for the SCUFA Submersible
Fluorometer were evaluated during this project: (i) quantification
of the rate of groundwater flow through a cave conduit, and (ii)
a dispersion study in a very slowly flowing density strata.
Quantifying
Flow Rate in a Cave Conduit
ERI
deployed the SCUFA in conjunction with an acoustic Doppler current
profiler instrument. The current profiler was placed at numerous
points along a network of cave passages to quantify flow velocities
at individual points in the conduits. However, as conduit cross-sections
may change significantly over any distance, the flow velocities
recorded by the current profiler only represent isolated "point
velocities" and may not be representative of average flow rates
on a more regional scale. For this reason, the SCUFA was utilized
to quantify flow rates over longer distances.
In the field
ERI programmed the SCUFA with a laptop computer prior to each dive.
Once set up, the SCUFA was handed over to a project diver for transport
into the cave system. The divers worked in teams of three to measure
flow rates with the SCUFA. The procedure included the following
steps: (i) deployment of the SCUFA, (ii) measurement of the distance
between the SCUFA and the upstream dye release point, (iii) release
of a slug of Rhodamine WT dye, and (iv) recording the time of dye
release using a watch that was synchronized to the SCUFA during
programming.
After release,
the Rhodamine WT slug was carried by groundwater flow to the SCUFA,
where it was recorded as a break-through type curve. Later, the
SCUFA was recovered and the data downloaded on the surface. Flow
rates were calculated according to Equation 1.
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Equation
1
Groundwater
flow rate = D / (TD - TR )
Where
D = distance
TD = time of dye detection at SCUFA
TR = time of dye release
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Dispersion Test in Very Slowly Flowing Water
ERI divers
noted that certain saline water masses in the Yucatan study area
do not appear to have visible flow. In order to determine if this
was true, a simple test was devised using the SCUFA® and a slug
of Rhodamine WT dye.
The SCUFA was
programmed to log at 10 second intervals and was then taken into
the cave system. Divers swam into the cave system in a slightly
flowing brackish strata above the seemingly stagnant saline water
strata. When at the study location, a diver reached through a halocline
to place the SCUFA on the cave conduit floor and into the saline
water body. The diver then injected a slug of Rhodamine WT dye under
the halocline and dive team exited the cave system. Thirty one hours
later the SCUFA was retrieved. The divers noted that the dye slug
was dispersed, but did not appear to have moved significantly. When
the SCUFA data was downloaded and subsequently reviewed it was obvious
that the dye slug had moved.
Based on the
SCUFA data, ERI researchers concluded that (i) the saline water
body flows, (ii) the flow is oscillatory with periods of near stagnation
punctuated by relatively rapid flow, (iii) flow is related to tide
stage, and (iv) the periods of rapid flow cause significant mixing
within the saline water body.
(pictures taken
by Steve Auer)

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