ABSTRACT
Field comparisons of chemical concentrations
obtained from dialysis samplers, passive diffusion bag samplers, and low-flow
samplers showed generally close agreement in most of the 13 wells tested during
July 2001 at Hickam Air Force Base, Hawaii. The data for chloride, sulfate,
iron, alkalinity, arsenic, and methane appear to show that the dialysis
samplers are capable of accurately collecting a passive sample for these constituents.
In general, the comparisons of volatile organic compound concentrations showed
a relatively close correspondence between the two different types of diffusion samples
and between the diffusion samples and the low-flow samples collected in most wells.
Divergence appears to have resulted primarily from the pumping method, either producing
a mixed sample or water not characteristic of aquifer water moving through the
borehole under ambient conditions. The fact that alkalinity was not detected in
the passive diffusion bag samplers, highly alkaline waters without
volatilization loss from effervescence, which can occur when a sample is
acidified for preservation. Both dialysis and passive diffusion bag samplers
are relatively inexpensive and can be deployed rapidly and easily. Passive diffusion
bag samplers are intended for sampling volatile organic compounds only, but dialysis
samplers can be used to sample both volatile organic compounds and inorganic solutes.
Regenerated cellulose dialysis samplers, however, are subject to biodegradation
and probably should be deployed no sooner than 2 weeks prior to recovery.
1 U.S. Geological Survey,
Columbia, South Carolina.
2 Air Florce Center for
Environmental Excellence, San Antionio, Texas.
--- 2001
By Don A. Vroblesky1 and
Tasha Pravecek2
Department of the Interior,
U.S. Geological Survey
Water Resources
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