无机矿质颗粒悬浮物对富营养化水体氨氮的吸附特性

利用蒙脱土、高岭土和太湖沉积物矿质组分3种材料,模拟研究了水体悬浮矿质颗粒物对富营养化水体中氨氮的吸附特性.实验表明,30min内3种材料对氨氮的吸附基本可达到平衡;等温平衡吸附均符合Henry吸附模式,在无机矿质颗粒悬浮物浓度1000mg/L,初始氨氮浓度1.0mg/L,pH=7.00实验条件下,吸附分配系数分别依次为548.30,287.36,191.27L/kg.相同实验条件下,随着pH、盐度和温度的增大或升高,矿质颗粒对氨氮的平衡吸附量均有不同程度的减小趋势,pH的影响较显著.随着悬浮颗粒物浓度在1000mg/L以下范围增大,固相氨氮平衡吸附量显著减小.

Property of Adsorption about Ammonium on Suspended Mineral Matters in Eutrophic Water

Static experiments were performed to investigate the adsorption characteristics of ammonium by suspended mineral matters(SPM). Three kinds of suspended mineral matters including montmorillonite, kaolin and the particles separated from the sediments of the Taihu Lake were used as the sorbent. The experiments show that the equation could be gotten within 30 min, and that the ammonium adsorption on mineral particles conformed to Herry isotherm. The parting coefficient of the adsorption about ammonium could reach 548.30,287.36,191.27 L/kg in experimental condition that there were 1 000 mg/L mineral particles and 1.0 mg/L ammonium in water with pH 7.00. Some effectors such as temperature, pH and salinity of the water on the adsorption about ammonium were observed. The results show that the quantity of adsorbed ammonium slightly decrease with the increasing of temperature and salinity, and greatly do with increasing of pH. The quantity decrease rapidly also with the increasing of the content of mineral particles below 1 000 mg/L.