常红,李利芬,黄丽.皂角苷对红壤和黄褐土中Pb2+、Zn2+的解吸特征[J].农业环境科学学报,2017,36(1):93-100. |
皂角苷对红壤和黄褐土中Pb2+、Zn2+的解吸特征 |
Desorption characteristics of Pb2+ and Zn2+ from red soil and yellow-cinnamon soil by saponin |
投稿时间:2016-07-22 |
DOI:10.11654/jaes.2016-0948 |
中文关键词: 皂角苷 Pb2+ Zn2+ 红壤 黄褐土 解吸 |
英文关键词: saponin Pb2+ Zn2+ red soil yellow-cinnamon soil desorption |
基金项目:教育部留学回国启动基金项目;公益性行业专项(201303101) |
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中文摘要: |
以Pb2+、Zn2+污染的红壤和黄褐土为材料,以皂角苷为解吸剂,研究不同皂角苷浓度(0~20 g·L-1)、pH (3~7)、解吸次数(1~3次)下土壤中重金属的解吸效果。结果表明,随着皂角苷浓度升高,其从土壤中解吸Pb2+和Zn2+的量增大;皂角苷溶液pH越高,对Pb2+和Zn2+的解吸率越低。皂角苷对土壤中Zn2+的解吸率明显高于Pb2+,红壤中Zn2+的解吸率最高可达47%,而黄褐土中Zn2+的解析率则为30%。单次解吸,红壤中含量降低最大的是酸溶态的Pb2+和Zn2+,分别为38%和34%;可氧化态Zn2+的含量下降较少,约为14%,但下降程度仍高于黄褐土。黄褐土中可还原态Pb2+的含量减少最多,达26%,且各形态的解吸量均显著低于红壤。皂角苷对供试红壤中Pb2+、Zn2+的解吸效果好于黄褐土,可能是红壤与黄褐土的矿物组成和表面电荷性质不同所致。加入皂角苷后,红壤的Zeta电位下降,黄褐土的升高,两种土壤的Zeta电位均向零趋近。 |
英文摘要: |
Incubations of Pb2+ and Zn2+ in contaminated red and yellow-cinnamon soil were conducted to investigate the effect of saponin on desorption of heavy metals. Various factors such as concentration of adsorbent(0~20 g·L-1), pH(3~7), extract times(1~3) were studied, the effect of saponins on Pb2+ and Zn2+ desorption was researched by Zeta potential analysis. Results showed that the desorption amounts of Pb2+ and Zn2+ enhanced with the increasing of saponin concentration and were negative with the acidity of saponin solution in tested soils. Under the same condition, saponin could desorb more Zn2+ than Pb2+, the highest desorption rate of Zn2+ was 47%, and 30% in the red and yellow-cinnamon soil, respectively. After single desorption, acid soluble Pb2+(38%) and Zn2+(34%) decreased most in the red soil than in the yellow-cinnamon soil. The declined content of oxidable Zn2+ was relatively less(about 14%), but still higher than that in the yellow-cinnamon soil. The reduction of reducible Pb2+ was more than other forms of Pb2+ in yellow-cinnamon soil, about 26%. The desorption amounts of all forms of Pb2+ and Zn2+ were significantly lower in the yellow-cinnamon soil than those in the red soil. The desorption effects of Pb2+ and Zn2+ by saponin were better in red soil than in yellow-cinnamon soil, these were mainly because of the differences of mineral composition and surface charge properties of the two soils.Compared with the red soil, the yellow-cinnamon soil had more constant charge minerals and less variable charge minerals. After adding saponin, the Zeta potential of the red soil decreased and that of the yellow-cinnamon soil increased, and the Zeta potentials of the two soils were generally close to zero. |
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