Adsorption of halocarbons to micro-, meso-and non-porous particulate materials

Mark H. Kleinman; C. Brindle; K. Griffiths; H. Forman; G. W. Flynn; P. Schlosser; N. J. Turro

Adsorption of halocarbons to micro-, meso-and non-porous particulate materials

Mark H. Kleinman, C. Brindle, K. Griffiths, H. Forman, G. W. Flynn, P. Schlosser, N. J. Turro

Research output: Contribution to journal › Conference article › peer-review

Abstract

Different types of soil constituents were evaluated in terms of their efficiency for binding and possibly degrading halocarbons, e.g., CCl₄, CCl₃F, and CCl₂F, at the liquid-solid or gas-solid interface. Halocarbon could bind in appreciable amounts to the internal volumes of zeolites, e.g., SiO₂, Al₂O₃, and Fe₂O₃, and silica gels. Although these types of materials were present in small amounts in many geographical regions, their presence might considerably alter the adsorption of small halocarbons. The amount of these nonspecific microporous sinks and the internal volume of soil samples should be accounted for when using small molecules trace groundwater. This is an abstract of a paper presented at the 222nd ACS National Meting (Chicago, IL 8/26-30/2001).

Original language	English (US)
Pages (from-to)	350-352
Number of pages	3
Journal	ACS Division of Environmental Chemistry, Preprints
Volume	41
Issue number	2
State	Published - 2001
Externally published	Yes
Event	222nd ACS National Meeting - Chicago, IL, United States Duration: Aug 26 2001 → Aug 30 2001

ASJC Scopus subject areas

General Chemical Engineering

Cite this

@article{8cab489691ca4b3d91c9d2d356b4a552,

title = "Adsorption of halocarbons to micro-, meso-and non-porous particulate materials",

abstract = "Different types of soil constituents were evaluated in terms of their efficiency for binding and possibly degrading halocarbons, e.g., CCl4, CCl3F, and CCl2F, at the liquid-solid or gas-solid interface. Halocarbon could bind in appreciable amounts to the internal volumes of zeolites, e.g., SiO2, Al2O3, and Fe2O3, and silica gels. Although these types of materials were present in small amounts in many geographical regions, their presence might considerably alter the adsorption of small halocarbons. The amount of these nonspecific microporous sinks and the internal volume of soil samples should be accounted for when using small molecules trace groundwater. This is an abstract of a paper presented at the 222nd ACS National Meting (Chicago, IL 8/26-30/2001).",

author = "Kleinman, {Mark H.} and C. Brindle and K. Griffiths and H. Forman and Flynn, {G. W.} and P. Schlosser and Turro, {N. J.}",

year = "2001",

language = "English (US)",

volume = "41",

pages = "350--352",

journal = "ACS Division of Environmental Chemistry, Preprints",

issn = "0093-3066",

publisher = "American Chemical Society",

number = "2",

note = "222nd ACS National Meeting ; Conference date: 26-08-2001 Through 30-08-2001",

}

TY - JOUR

T1 - Adsorption of halocarbons to micro-, meso-and non-porous particulate materials

AU - Kleinman, Mark H.

AU - Brindle, C.

AU - Griffiths, K.

AU - Forman, H.

AU - Flynn, G. W.

AU - Schlosser, P.

AU - Turro, N. J.

PY - 2001

Y1 - 2001

N2 - Different types of soil constituents were evaluated in terms of their efficiency for binding and possibly degrading halocarbons, e.g., CCl4, CCl3F, and CCl2F, at the liquid-solid or gas-solid interface. Halocarbon could bind in appreciable amounts to the internal volumes of zeolites, e.g., SiO2, Al2O3, and Fe2O3, and silica gels. Although these types of materials were present in small amounts in many geographical regions, their presence might considerably alter the adsorption of small halocarbons. The amount of these nonspecific microporous sinks and the internal volume of soil samples should be accounted for when using small molecules trace groundwater. This is an abstract of a paper presented at the 222nd ACS National Meting (Chicago, IL 8/26-30/2001).

AB - Different types of soil constituents were evaluated in terms of their efficiency for binding and possibly degrading halocarbons, e.g., CCl4, CCl3F, and CCl2F, at the liquid-solid or gas-solid interface. Halocarbon could bind in appreciable amounts to the internal volumes of zeolites, e.g., SiO2, Al2O3, and Fe2O3, and silica gels. Although these types of materials were present in small amounts in many geographical regions, their presence might considerably alter the adsorption of small halocarbons. The amount of these nonspecific microporous sinks and the internal volume of soil samples should be accounted for when using small molecules trace groundwater. This is an abstract of a paper presented at the 222nd ACS National Meting (Chicago, IL 8/26-30/2001).

UR - http://www.scopus.com/inward/record.url?scp=23844507343&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=23844507343&partnerID=8YFLogxK

M3 - Conference article

AN - SCOPUS:23844507343

SN - 0093-3066

VL - 41

SP - 350

EP - 352

JO - ACS Division of Environmental Chemistry, Preprints

JF - ACS Division of Environmental Chemistry, Preprints

IS - 2

T2 - 222nd ACS National Meeting

Y2 - 26 August 2001 through 30 August 2001

ER -

Adsorption of halocarbons to micro-, meso-and non-porous particulate materials

Abstract

ASJC Scopus subject areas

Other files and links

Fingerprint

Cite this