U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
Determination of Surface Area of Soil Components by Sorption
of Nitrogen and Ethylene Glycol Monoethyl Ether Vapors and Evaluation of
Adsorption, Partition and Cation Solvation Processes
by
Cary T. Chiou (U.S. Geological Survey, Box 25046, MS 408, Denver
Federal Center, Denver, CO 80225) and David W. Rutherford (U.S. Geological
Survey, Box 25046, MS 408, Denver Federal Center, Denver, CO 80225)
Abstract
The vapor uptake isotherms of nitrogen and ethylene glycol
monoethyl ether (EGME) were determined for soil and soil
components. The cross sectional area of EGME was determined
to be 40.0 x 10-20 m2 by comparing adsorption isotherms
on reference surface area standards. For samples where
EGME does not penetrate into the solid (Ottawa Sand, hematite,
aluminum oxide, synthetic hydrous iron oxide, and kaolinite),
the EGME and nitrogen isotherms show consistent surface
uptake and the EGME isotherm can be reasonably estimated from
the nitrogen isotherm by multiplying the nitrogen uptake by a
factor of 1.3 to account for different molecular area and molecular
weight. For other samples where the EGME can penetrate
into the solid (peat, Ca-montmorillonite, and illite), the total
uptake can be resolved to surface adsorption, partition into
soil organic matter, and/or cation solvation. For
peat, the nitrogen uptake is very small, resulting in a surface
area of 1.3 square meters per gram; uptake of EGME on peat is
large and linear, which is indicative of large bulk solubility
of EGME in soil organic matter (190 milligrams per gram). For
Ca-montmorillonite, the resulting cation solvation isotherm shows
a stoichiometric interaction of about 4 EGME molecules per
exchangeable Ca ion. Exchange of organic cations for metal ions
in montmorillonite sharply decreases the cation solvation effect
of EGME. This cation exchange may result in a higher surface
area of the clay due to opening of interlayer surfaces.
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