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פותח על ידי קלירמאש פתרונות בע"מ -
Adsorption and desorption of parathion by attapulgite as affected by the mineral structure
Year:
1978
Authors :
גרסטל, זאב
;
.
Volume :
26
Co-Authors:
Gerstl, Z., Division of Soil Residues Chemistry, Institute of Soils and Water, Volcani Center, Bet Dagan, Israel
Yaron, B., Division of Soil Residues Chemistry, Institute of Soils and Water, Volcani Center, Bet Dagan, Israel
Facilitators :
From page:
569
To page:
573
(
Total pages:
5
)
Abstract:
Adsorption of parathion by pretreated attapulgites was studied in both organic and aqueous media. In organic media the presence of hygroscopic moisture resulted in competition between parathion and water so that an increase in the clay's moisture content reduced parathion adsorption. Heating the clays above 250 °C resulted in structural changes that cause a decrease in parathion adsorption. Adsorption of parathion in aqueous solution was found to be inversely related to the release of parathion from highly loaded clays under equilibrium conditions. Saturating clays with an organocation altered their properties favoring increased adsorption and decreased desorption. The results indicate that pretreatment of the clay might affect both the rate and amount of release to the external environment. © 1978 American Chemical Society.
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DOI :
Article number:
Affiliations:
Database:
סקופוס
Publication Type:
מאמר
;
.
Language:
אנגלית
Editors' remarks:
ID:
20064
Last updated date:
02/03/2022 17:27
Creation date:
16/04/2018 23:33
Scientific Publication
Adsorption and desorption of parathion by attapulgite as affected by the mineral structure
26
Gerstl, Z., Division of Soil Residues Chemistry, Institute of Soils and Water, Volcani Center, Bet Dagan, Israel
Yaron, B., Division of Soil Residues Chemistry, Institute of Soils and Water, Volcani Center, Bet Dagan, Israel
Adsorption and desorption of parathion by attapulgite as affected by the mineral structure
Adsorption of parathion by pretreated attapulgites was studied in both organic and aqueous media. In organic media the presence of hygroscopic moisture resulted in competition between parathion and water so that an increase in the clay's moisture content reduced parathion adsorption. Heating the clays above 250 °C resulted in structural changes that cause a decrease in parathion adsorption. Adsorption of parathion in aqueous solution was found to be inversely related to the release of parathion from highly loaded clays under equilibrium conditions. Saturating clays with an organocation altered their properties favoring increased adsorption and decreased desorption. The results indicate that pretreatment of the clay might affect both the rate and amount of release to the external environment. © 1978 American Chemical Society.
Scientific Publication
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