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中国南方酸性水稻土对铜吸附过程中铝的溶出机制及动力学

Mechanism and kinetics of aluminum dissolution during copper sorption by acidity paddy soil in South China.

作者信息

Liu Peiya, Li Yujiao, Wen Qinliang, Dong Changxun, Pan Genxing

机构信息

College of Sciences, Nanjing Agricultural University, Nanjing 210095, China.

College of Sciences, Nanjing Agricultural University, Nanjing 210095, China.

出版信息

J Environ Sci (China). 2015 Aug 1;34:100-6. doi: 10.1016/j.jes.2015.02.008. Epub 2015 Jun 3.

DOI:10.1016/j.jes.2015.02.008
PMID:26257352
Abstract

Soil aggregates were prepared from a bulk soil collected from paddy soil in the Taihu Lake region and aluminum (Al) dissolution, solution pH changes during copper (Cu(2+)) sorption were investigated with static sorption and magnetic stirring. Kinetics of Cu(2+) sorption and Al dissolution were also studied by magnetic stirring method. No Al dissolution was observed until Cu(2+) sorption was greater than a certain value, which was 632, 450, 601 and 674 mg/kg for sand, clay, silt, and coarse silt fractions, respectively. Aluminum dissolution increased with increasing Cu(2+) sorption and decreasing solution pH. An amount of dissolved Al showed a significant positive correlation with non-specific sorption of Cu(2+) (R(2)>0.97), and it was still good under different pH values (R(2)>0.95). Copper sorption significantly decreased solution pH. The magnitude of solution pH decline increased as Cu(2+) sorption and Al dissolution increased. The sand and clay fraction had a less Al dissolution and pH drop due to the higher ferric oxide, Al oxide and organic matter contents. After sorption reaction for half an hour, the Cu(2+) sorption progress reached more than 90% while the Al dissolution progress was only 40%, and lagged behind the Cu(2+) sorption. It indicated that aluminum dissolution is associated with non-specific sorption.

摘要

土壤团聚体由采集自太湖地区水稻土的原状土制备而成,通过静态吸附和磁力搅拌研究了铝(Al)的溶解以及铜(Cu(2+))吸附过程中溶液pH值的变化。还采用磁力搅拌法研究了Cu(2+)吸附和Al溶解的动力学。在Cu(2+)吸附量大于某一特定值之前未观察到Al溶解,该特定值对于砂、黏土、粉砂和粗粉砂组分分别为632、450、601和674 mg/kg。Al溶解随着Cu(2+)吸附量的增加和溶液pH值的降低而增加。溶解Al的量与Cu(2+)的非特异性吸附呈显著正相关(R(2)>0.97),并且在不同pH值下仍然良好(R(2)>0.95)。Cu吸附显著降低溶液pH值。溶液pH值下降的幅度随着Cu(2+)吸附量和Al溶解量的增加而增大。砂和黏土组分由于较高的氧化铁、氧化铝和有机质含量,Al溶解和pH下降较少。吸附反应半小时后,Cu(2+)吸附进程达到90%以上,而Al溶解进程仅为40%,且滞后于Cu(2+)吸附。这表明铝溶解与非特异性吸附有关。

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