Science Inventory

EFFECTS OF TEMPERATURE ON TRICHLOROETHYLENE DESORPTION FROM SILICA GEL AND NATURAL SEDIMENTS. 1. ISOTHERMS. (R822626)

Citation:

Werth, C. J. AND M. Reinhard. EFFECTS OF TEMPERATURE ON TRICHLOROETHYLENE DESORPTION FROM SILICA GEL AND NATURAL SEDIMENTS. 1. ISOTHERMS. (R822626). ENVIRONMENTAL SCIENCE & TECHNOLOGY. American Chemical Society, Washington, DC, 31(3):689-696, (1997).

Description:

Aqueous phase isotherms were calculated from vapor phase desorption isotherms
measured at 15, 30, and 60 C for
trichloroethylene on a silica gel, an aquifer sediment, a soil, a sand fraction,
and a clay and silt fraction, all at 100% relative humidity. Isosteric heats of
adsorption (Qst(q)) were calculated as a function of
the sorbed concentration, q, and examined with respect to the following
mecha nisms: adsorption on water wet mineral surfaces, sorption in amorphous
organic matter (AOM), and adsorption in hydrophobic micropores. Silica gel, sand
fraction, and clay and silt fraction 60 C
isotherms are characterized by a Freundlich region and a region at very low
concentrations where isotherm points deviate from log-log linear behavior. The
latter is designated the non-Freundlich region. For the silica gel, values of
Qst(q) (9.5-45 kJ/mol) in both regions are consistent
with adsorption in hydrophobic micropores. For the natural solids, values of
Qst(q) in the Freundlich regions are less than or equal
to zero and are consistent with sorption on water wet mineral surfaces and in
AOM. In the non-Freundlich regions, diverging different temperature isotherms
with decreasing q and a Qst(q) value of 34
kJ/mol for the clay and silt fraction suggest that adsorption is occurring in
hydrophobic micropores. The General Adsorption Isotherm is used to capture this
adsorption heterogeneity.

Record Details:

Record Type:DOCUMENT( JOURNAL/ PEER REVIEWED JOURNAL)
Product Published Date:01/01/1997
Record Last Revised:12/22/2005
Record ID: 66647