| dc.contributor.author |
Droulia, FE |
en |
| dc.contributor.author |
Kati, V |
en |
| dc.contributor.author |
Giannopolitis, CN |
en |
| dc.date.accessioned |
2014-06-06T06:51:27Z |
|
| dc.date.available |
2014-06-06T06:51:27Z |
|
| dc.date.issued |
2011 |
en |
| dc.identifier.issn |
03601234 |
en |
| dc.identifier.uri |
http://dx.doi.org/10.1080/03601234.2011.572506 |
en |
| dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/5526 |
|
| dc.subject |
3,4-dca |
en |
| dc.subject |
Distribution coefficients |
en |
| dc.subject |
Freundlich equation |
en |
| dc.subject |
Soil sorption |
en |
| dc.subject |
Sorption isotherms |
en |
| dc.subject.other |
3,4-dca |
en |
| dc.subject.other |
Distribution coefficients |
en |
| dc.subject.other |
Freundlich equations |
en |
| dc.subject.other |
Soil sorption |
en |
| dc.subject.other |
Sorption isotherms |
en |
| dc.subject.other |
Adsorption isotherms |
en |
| dc.subject.other |
Biogeochemistry |
en |
| dc.subject.other |
Biological materials |
en |
| dc.subject.other |
Organic compounds |
en |
| dc.subject.other |
Polyvinyl alcohols |
en |
| dc.subject.other |
Soils |
en |
| dc.subject.other |
Sorption |
en |
| dc.subject.other |
Soil pollution |
en |
| dc.subject.other |
3,4 dichloroaniline |
en |
| dc.subject.other |
3,4-dichloroaniline |
en |
| dc.subject.other |
aniline derivative |
en |
| dc.subject.other |
calcium derivative |
en |
| dc.subject.other |
calcium oxide |
en |
| dc.subject.other |
oxide |
en |
| dc.subject.other |
pesticide |
en |
| dc.subject.other |
agricultural soil |
en |
| dc.subject.other |
calcareous soil |
en |
| dc.subject.other |
enzyme activity |
en |
| dc.subject.other |
ion exchange |
en |
| dc.subject.other |
isotherm |
en |
| dc.subject.other |
liming |
en |
| dc.subject.other |
pH |
en |
| dc.subject.other |
sandy clay loam |
en |
| dc.subject.other |
soil organic matter |
en |
| dc.subject.other |
soil type |
en |
| dc.subject.other |
sorption |
en |
| dc.subject.other |
adsorption |
en |
| dc.subject.other |
agriculture |
en |
| dc.subject.other |
article |
en |
| dc.subject.other |
chemistry |
en |
| dc.subject.other |
evaluation |
en |
| dc.subject.other |
Greece |
en |
| dc.subject.other |
methodology |
en |
| dc.subject.other |
soil |
en |
| dc.subject.other |
soil pollutant |
en |
| dc.subject.other |
Adsorption |
en |
| dc.subject.other |
Agriculture |
en |
| dc.subject.other |
Aniline Compounds |
en |
| dc.subject.other |
Calcium Compounds |
en |
| dc.subject.other |
Greece |
en |
| dc.subject.other |
Oxides |
en |
| dc.subject.other |
Pesticides |
en |
| dc.subject.other |
Soil |
en |
| dc.subject.other |
Soil Pollutants |
en |
| dc.subject.other |
Greece |
en |
| dc.title |
Sorption of 3, 4-dichloroaniline on four contrasting Greek agricultural soils and the effect of liming |
en |
| heal.type |
journalArticle |
en |
| heal.identifier.primary |
10.1080/03601234.2011.572506 |
en |
| heal.publicationDate |
2011 |
en |
| heal.abstract |
Sorption of 3, 4-dichloroaniline (3, 4-DCA) on four typical Greek agricultural soils, with distinct texture, organic matter content andcation exchange capacities, was compared by using sorption isotherms and the parameters calculated from the fitted Freundlichequations. The sorption process of 3, 4-DCA to the soil was completed within 48-72 h. The 3, 4-DCA sorption on all soils was welldescribed by the Freundlich equation and all sorption isotherms were of the L-type. The sandy clay loam soil with the highest organicmatter content and a slightly acidic pH was the most sorptive, whereas the two other soil types, a high organic matter and neutralpH clay and a low organic matter and acidic loam, had an intermediate sorption capacity. A typical calcareous soil with low organicmatter had the lowest sorption capacity which was only slightly higher than that of river sand. The 3, 4-DCA sorption correlated bestto soil organic matter content and not to clay content or cation exchange capacity, indicating the primary role of organic matter.The distribution coefficient (Kd) decreased with increasing initial 3, 4-DCA concentration and the reduction was most pronouncedwith the highly sorptive sandy clay loam soil, suggesting that the available sorption sites of the soils are not unlimited. Liming of thetwo acidic soils (the sandy clay loam and the loam) raised their pH (from 6.2 and 5.3, respectively) to 7.8 and reduced their sorptioncapacity by about 50 %, indicating that soil pH may be the second in importance factor (after organic matter) determining 3, 4-DCAsorption. © Taylor & Francis Group, LLC. |
en |
| heal.journalName |
Journal of Environmental Science and Health - Part B Pesticides, Food Contaminants, and Agricultural Wastes |
en |
| dc.identifier.issue |
5 |
en |
| dc.identifier.volume |
46 |
en |
| dc.identifier.doi |
10.1080/03601234.2011.572506 |
en |
| dc.identifier.spage |
404 |
en |
| dc.identifier.epage |
410 |
en |