Characterization of clay particle surfaces for contaminant sorption in soil barriers using flow microcalorimetry


Kaya A.

JOURNAL OF ENVIRONMENTAL ENGINEERING-ASCE, vol.130, no.8, pp.918-921, 2004 (SCI-Expanded) identifier identifier

  • Publication Type: Article / Article
  • Volume: 130 Issue: 8
  • Publication Date: 2004
  • Doi Number: 10.1061/(asce)0733-9372(2004)130:8(918)
  • Journal Name: JOURNAL OF ENVIRONMENTAL ENGINEERING-ASCE
  • Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Page Numbers: pp.918-921
  • Keywords: clays, adsorption, contaminants, barriers, waste, ACID-BASE, FREE-ENERGY
  • Dokuz Eylül University Affiliated: No

Abstract

Clays such as kaolinite and bentonite are widely used in various industries as sorbents. The sorptive characteristics of clays are exploited when they are used in contaminant barrier systems. To use clays effectively, their surface characteristics need to be known; especially, when they are used for contaminant sorption. Available surface area of clay minerals and the characteristics that depend on it are very sensitive to environmental changes such as those that can be induced by changes in the composition of pore fluid. Flow microcalorimetry with a down-stream concentration was used to determine the heats and amounts of adsorption of acids and bases on the clays. Test results presented herein revealed that both kaolinite and bentonite exhibit significantly different adsorption isotherms and heat of wetting under high pH and low pH conditions. Kaolinite has the capacity to adsorb both acidic and basic molecules almost equally. However, it has a tendency to adsorb more base than acid because of its stronger complexation capacity with acids than with bases. On the other hand, bentonite has a tendency to adsorb more acidic than basic molecules per gram. These results also indicate that both kaolinite and bentonite have different heats of wetting characteristics. As the concentrations of the acids and bases increase, the heat of wetting of kaolinite decreases while that of bentonite increases.