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Estimation of membrane diffusion coefficients and equilibration times for low-density polyethylene passive diffusion
Craig E Divine1, John E McCray
1Department of Geology and Geological Engineering, Colorado School of Mines, Golden, Colorado 80401, USA. cdivine@mines.edu
Environmental Science & Technology
|April 13, 2004
Summary
Passive diffusion (PD) samplers offer cost-effective groundwater monitoring. Their equilibration time depends on sampler design and analyte diffusion, with models predicting accurate in situ measurements.
Area of Science:
- Environmental Science
- Analytical Chemistry
- Geochemistry
Background:
- Passive diffusion (PD) samplers provide technical and cost advantages for groundwater monitoring.
- They are particularly useful for measuring dissolved gases and volatile organic compounds (VOCs) at contaminated sites.
Purpose of the Study:
- To determine the diffusion coefficients for various gases and VOCs in low-density polyethylene membranes.
- To predict PD sampler equilibration times based on sampler dimensions and diffusion coefficients.
- To develop and validate a numerical model for assessing PD sampler concentration "lag time".
Main Methods:
- Measured diffusion coefficients (Dm) for He, Ne, H2, O2, and N2 in laboratory experiments.
- Estimated Dm values for common VOCs using existing empirical data.
- Developed a numerical model to evaluate concentration "lag time" for temporally variable in situ concentrations.
Main Results:
- Measured Dm values for gases ranged from 1.1 to 1.9 x 10(-7) cm2 sec(-1) at 21°C.
- Estimated Dm values for VOCs ranged from 1.7 to 4.4 x 10(-7) cm2 sec(-1) at 21°C.
- The numerical model accurately predicted lag time in laboratory experiments.
Conclusions:
- PD sampler equilibration time is influenced by sampler dimensions, membrane thickness, and analyte diffusion coefficients.
- The developed numerical model can predict lag time and assess the suitability of PD samplers for various field conditions.
- Appropriately designed PD samplers can provide near-instantaneous measurements of in situ groundwater concentrations.