CAJ | 학술논문

采用实验室研究方法，研究了SB （Soil Bentonite ）材料对Fe离子的吸附，以及Fe离子在SB Slurry wall 中的穿透行为，实验结果显示，SB 对 Fe 离子的吸附符合 langmuir 等温线，Fe 离子在 SB 中迁移时，导致 SB材料的渗透系数比纯水的渗透系数大一个数量级，Fe 离子流出浓度随着时间的增加在不断增加。
채용실험실연구방법，연구료SB （Soil Bentonite ）재료대Fe리자적흡부，이급Fe리자재SB Slurry wall 중적천투행위，실험결과현시，SB 대 Fe 리자적흡부부합 langmuir 등온선，Fe 리자재 SB 중천이시，도치 SB재료적삼투계수비순수적삼투계수대일개수량급，Fe 리자류출농도수착시간적증가재불단증가。
The method of laboratory research is adopted to study the adsorption of SB materials to Fe 3 + and the break-through behavior of Fe ions in SB Slurry wall .The results show that the adsorption SB material to Fe ion conforms to the Langmuir isotherm ;the migration of Fe3 + in SB causes the permeability coefficient increased to an order of magnitude and Fe3 + outflow concentration increases with the increase of time .