Lj. Musani , P. Valenta , H.W. Nürnberg , Z. Konrad , M. Branica
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引用次数: 28
摘要
采用高压纸电泳技术,在海水和0·55 m NaCl溶液中研究了65Zn、109Cd和210Pb−210Bi与海洋沉积物中腐植酸的相互作用。分别在100%、30%和10%海水条件下进行了模拟实验。腐植酸的浓度从3 ~ 300 mg l−1不等。测定了放射性核素的电泳迁移率随各种体系中腐植酸浓度的变化以及这些体系老化0 ~ 7天的变化。在不向海水中添加腐植酸的情况下,109Cd表现为阳离子,65Zn和210Pb表现为一个阳离子区和第二个非移动区。在0·55 m NaCl中,65Zn和210Pb只产生一个阳离子区。加入腐植酸后,放射性核素的电泳迁移率部分改变为阴离子迁移率,起始点处的区比未加入腐植酸的海水中更明显。总的来说,所获得的结果证实,在公海中溶解的腐殖质物质的量太少,对所研究的微量金属螯合的贡献不大,而在河口水域中,它们对微量金属螯合的贡献可以发挥作用。
On the chelation of toxic trace metals by humic acid of marine origin
The interaction of 65Zn, 109Cd and 210Pb−210Bi with humic acid isolated from marine sediment was investigated by high voltage paper electrophoresis in sea water and 0·55 m NaCl solutions. The experiments were performed in 100, 30 and 10% seawater to simulate also the estuarine conditions. The concentration of humic acid was varied from 3 to 300 mg l−1. The electrophoretic mobility of the radionuclides was measured as function of the concentration of humic acid in the various systems and on aging of these systems from 0 to 7 days. Without addition of humic acid to seawater 109Cd behaves as a cation, 65Zn and 210Pb give one cationic and a second nonmobile zone. In 0·55 m NaCl both 65Zn and 210Pb, give only one cationic zone. By addition of humic acid the radionuclides partly changed their electrophoretic mobility to anionic values and the zone at the starting point became more pronounced than in seawater without addition of humic acid. In general the results obtained confirm that the amounts of humic material dissolved in the open sea are too small to contribute significantly to the chelation of the investigated trace metals while in estuarine waters their contribution to trace metal chelation can play a role.