以钙基蒙脱石、钠基蒙脱石、酸活化蒙脱石为原料制备了载铜蒙脱石并研究它们对嗜水气单胞菌的吸附性能.蒙脱石和嗜水气单胞菌的Zeta电位随pH值升高而降低;载铜蒙脱石的Zeta电位随pH值升高而增大,当pH=4~6时Zeta电位从负值转变为正值.酸活化蒙脱石、钠基蒙脱石和钙基蒙脱石对细菌的平衡吸附率分别为36.5%、20.1%和14.3%,其相应的载铜蒙脱石对细菌的平衡吸附率分别为99.6%、93.1%和87.4%.蒙脱石对细菌的吸附率随着pH的增加而减小,载铜蒙脱石对细菌的吸附率先随pH值的增大而减小,到pH=5.0后随pH值的增大而增大.载铜蒙脱石Cu2+脱附实验表明,经过脱附后的沉淀物基本保持着原来的吸附活性,而经过脱附后的上清液对细菌的吸附率很低.载铜蒙脱石的抗菌作用是静电吸附细菌与铜离子抗菌的综合作用.
参考文献
[1] | Hawkins P R,Griffiths D J.J.Water Res,1987,21:475-480. |
[2] | 李吉东,李玉宝,王学江,等(LI Ji-Dong,et al).无机材料学报(Journal of Inorganic Materials),2006,21(1):162-168. |
[3] | 侯文生,魏丽乔,戴晋明,等(HOU Weng-Sheng,et al).无机材料学报(Journal of Inorganic Materials),2005,20(4):907-913. |
[4] | 胡彩虹,夏枚生(HU Cai-Hong,et al).硅酸盐学报(J.Chin.Ceram.Soc.),2005,33 (11):1376-1380. |
[5] | Xia M S,Hu C H,Xu Z R.J.Poultr.Sci.,2004,83 (11):1868-1875. |
[6] | Hu C H,Xia M S,Xu Z R.J.Asian-Aust J Anim.Sci.,2004,17 (11):1575-1581. |
[7] | Xia M S,Hu C H,Xu Z R.J.Anim.Feed.Sci.Technol.,2005,118 (3-4):307-317. |
[8] | Theng B K G,Hayashi S,Soma M,et al.J.Clays.Clay.Miner.,1997,45:718-723. |
[9] | Van Loosdrecht M C C,Lyklema J,Nored W.J.Microbial Ecology,1989,17:1-15. |
[10] | Davis J A,Kent D B.Surface complexation modeling in aqueous geochemistry.Mineral-water interface geochemistry.In:Hochella M.F.Jr.,White A.F.Eds..Reviews in Mineralogy and Mineralogical Society of American,Washington,D.C,1990.177-260. |
[11] | Bahranowski K,Dula R,Labanowska M,et al.Appl.Spectr.,1996,50:1439-1445. |
[12] | Stadler M,Schindler P W.J.Clays and Clay Miner,1993,41:288-296. |
[13] | Mosser C,Michot L J,Villierns F,et al.J.Clays.Clay.Miner.,1997,45:789-802. |
[14] | He H P,Guo J G,Xie X D,et al.J.Environ.Int.,2001,26:347-352. |
[15] | Fowle D A,Fein J B.J.Geochimica Cosmochimica Acta,1999,63:3059-3067. |
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