Cadmium Adsorption and Exchangeable Cations Desorption in Soils: Effects of pH and Organic Matter Content

토양에서 카드뮴의 흡착과 치환성양이온의 탈착 : pH와 유기물함량의 영향

  • 박병윤 (대구효성가톨릭대학교 환경보건학과) ;
  • 신현무 (경성대학교 환경공학과)
  • Published : 1996.04.01

Abstract

In order to investigate the effects of pH and organic matter content on cadmium adsorption and exchangeable cations desorption in soils, the adsorption isotherms of cadmium and the desorption isotherms of calcium and magnesium on four New jersey soils at four pH values were plotted, and the cadmium partition coefficients (Kd) were also calculated. The slopes of cadmium adsorption isotherms dramatically increased with increasing solution pH. Judging from Langmuir adsorption equations, the maximum adsorption quantities(b) of cadmium at high pH values were much greater than those at low pH values for the same soil. The partition coefficients increased greatly with increasing solution pH. The slopes of regression equations between partition coefficients and pH values were steep in the order of the organic matter content of the soils. The correlation coefficients (r2) between partition coefficient and organic matter content for soils. The correlation coefficients (r2) between partition coefficient and organic matter content for $1\times10^{-4}$M increased from 0.3027 at pH 4.0 to 0.9964 at pH 8.5 and from 0.2093 at pH4.0 at 0.9657 at pH 8.5 for$2\times10^{-4}$M ${Cd(NO_3)}_2$. The desorption quantities of calcium and magnesium decreased with increasing solution pH and increased with- increasing cadmium adsorption.

미국 New Jersey주에서 채취한 4종류의 토양사료를 이용하여 토양에서 카드뮴 흡착과 치환성양이온의 탈착에 미치는 pH와 유기뮬함령의 영향을 조사하였다. 카드뮴용액으로는 $1\times10^{-5}$M,$1\times10^{-4}$M, $2\times10^{-4}$M, $3\times10^{-4}$M ${Cd(NO_3)}_2$ 용액을 사용하였고, 흡착평형시의 토양용액의 pH는 4.0,5.5, 7.0, 8.5로 맞추었다. 카드뮴흡착등온선의 기울기는 토양용액의 pH가 증가하였으며, partition coefficient($K_4$)도 용액의 pH가 증가할수록 크게 증가하였다. 또한 Langmuir흡착방정식에 의하여 구한 카드뮴대흡착량도 용액의 pH가 높은 경구가 낮은 경우보다 훨씬 많았다. $1\times10^{-4}$M ${Cd(NO_3)}_2$ 용액을 사용한 실험에서 유기물함량과 partition coefficient사이의 correltion coefficient($r^2$)는 용액의 pH가 4.0인 경우의 0.3027에서 pH가 8.5인 경우의 0.9964로 증가하였으며, $2\times10^{-4}$M ${Cd(NO_3)}_2$ 용액을 사용한 실험에서는 pH가 4.0인 경우의 0.2093에서 pH가 8.5인 경우의 0.9657로 증가하였다. 칼슘과 마그네슘의 탈착량은 토양용액의 pH가 증가할수롱, 흡착된 카드뮴의 양이 증가할수록 감소하였다.

Keywords

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