• Journal of the Korean GEO-environmental Society
• /
• v.2 no.3
• /
• pp.17-35
• /
• 2001

In this study, we conducted a combined adsorption-sequential extraction analysis(CASA) to investigate temperature effects of single adsorption of lead, copper, zinc and cadmium on natural clays. As a result, it was found that in a single adsorption of lead and copper, about 50% of adsorption was occluded in carbonate phase, and in case of cadmium, about 80% of adsorption was occluded in exchangeable phase. At temperature below $25^{\circ}C$ about 60% of zinc was occluded in exchangeable phase but above $40^{\circ}C$ about 50% of zinc was occluded in carbonate phase. The effect of temperature on each occluded phase was largely observed in Fe-oxide, Mn-oxide and organic occluded phases. Besides, the adsorption of metals on natural clays was an endothermic reaction with the exception of exchangeable phase adsorption.

• Journal of the Korean Geotechnical Society
• /
• v.16 no.2
• /
• pp.91-102
• /
• 2000

자연점토지반에서의 중금속 흡착시 온도변화에 따른 영향은 지금까지 2차적인 것으로 간주되었다. 그러나 최근 몇몇 연구자들에 의하면 온도변화가 중금속 흡착 거동에 큰 영향을 미친다고 보고하였다. 따라서 본 연구에서는 자연점토 지반에 대한 중금속 아연(Zn) 흡착시 온도변화에 따른 흙의 각 구성성분별 흡착거동을 살펴보기 위해 혼합 흡착-연속추출법(combined absorption-sequential extraction analysis, CASA)을 사용하였다. 실험결과 중금속 아연의 농도가 저농도(50mg/L 미만)일 경우 자연지반에서의 분배양상은 주로 탄산염 형태로 존재하고, 또한 온도의 증가에 따라 탄산염 형태의 흡착량이 증가하는 것을 알 수 있다. 하지만 고농도(50mg/L 이상)의 경우 분배양상은 주로 이온교환형태로 존재한다는 것을 알 수 있다. 그러나 고농도에서의 이러한 분배형태는 온도의 증가에 따라 탄산염형태의 흡착량이 약 20%정도 증가하는 결과를 얻었다. 결론적으로 중금속 아연의 자연점토지반의 각 구성성분 별 흡착거동은 이온교환 형태를 제외하고 온도증가에 따라 증가하는 흡열반응(ΔH0>0)인 것으로 나타났고, 또한 고농도에서의 분배형태는 이온교환 형태에서 탄산염 형태로 변화되는 것을 알 수 있다. 그리고 이온교환 형태의 경우 온도변화에 따라 독립적인 거동을 보였다.

• Journal of the Korean Geotechnical Society
• /
• v.16 no.4
• /
• pp.157-170
• /
• 2000

In this study, we conducted a combined adsorption-sequential extraction analysis(CASA) to investigate temperature effects of single and competitive adsorption of zinc and copper on natural clays. As a result, it was found out that in a single adsorption of zinc, the adsorption was mostly in the exchangeable phase, with increase n temperature. In a competitive adsorption of zinc, this trend was so strong that the exchangeable phase adsorption increase up to 80~90%. On the other hand, about 50% of copper was adsorbed in the carbonate occluded phase in single and competitive adsorptions. In the single adsorption the adsorption of carbonate occluded phase increased by 5% with the temperature increase and in the competitive adsorption the increase rate is about twice. The adsorption of zinc and copper on natural clays is an endothermic reaction with the exception of exchangeable phase adsorption.