2009China Environmental ScienceRequires access

Effect of adding four metal ions on distribution of anthracene on kaolin colloid

Yu Sheng, Peng Zou, Xiao Lin, Yang LiuYan

Open publisher page 0 citations

Abstract

In order to understand the effect of metal ions on distribution and adsorption of anthracene on soils (water/soil = 10), Fe3+, Cu2+, Zn2+ and Ca2+ were added in the colloid solution of contaminated kaolin to probe the varies of anthracene concentrations in supernatants after 180 r/min of shaking at 28℃. The adsorption equilibrium time and equilibrium concentration of Fe3+, Cu2+, Zn2+ and Ca2+ by kaolin were about 24 h and (20 ± 3) mg/g, respectively. When contents of metal ions added were more than 30 mg/g for kaolin, the lowest concentration of kaolin colloid was (40±3)mg/L in supernatant. The total colloid concentrations in supernatants increased from 52 mg/L to 133 mg/L for adding Fe3+, 52 mg/L to 110 mg/L for adding Cu2+ or Zn2+, and 52 mg/L to 73 mg/L for adding Ca2+, respectively. Meanwhile, the increasing trends of anthracene in the supernatants were similar to those of total colloid concentrations, which were from 30 ng/L to 73 ng/L for adding Fe3+, 28, 35ng/L to 65, 66 ng/L for adding Cu2+ or Zn2+, and 40 ng/L to 50 ng/L for adding Ca2+, respectively. Thus, the sequences of the increase of anthracene in supernatants were the same as those of the charge densities of metal ions (Fe3+ Cu2+, Zn2+). However, adding Ca2+ at pH 6.5 only led to a minor increase of anthracene in supernatant.

About this research paper

What this paper is about

In order to understand the effect of metal ions on distribution and adsorption of anthracene on soils (water/soil = 10), Fe3+, Cu2+, Zn2+ and Ca2+ were added in the colloid solution of contaminated kaolin to probe the varies of anthracene concentrations in supernatants after 180 r/min of shaking at 28℃. The adsorption equilibrium time and equilibrium concentration of Fe3+, Cu2+, Zn2+ and Ca2+ by kaolin were about 24 h and (20 ± 3) mg/g, respectively. When contents of metal ions added were more than 30 mg/g for kaolin, the lowest concentration of kaolin colloid was (40±3)mg/L in supernatant. The total colloid concentrations in supernatants increased from 52 mg/L to 133 mg/L for adding Fe3+, 52 mg/L to 110 mg/L for adding Cu2+ or Zn2+, and 52 mg/L to 73 mg/L for adding Ca2+, respectively. Meanwhile, the increasing trends of anthracene in the supernatants were similar to those of total colloid concentrations, which were from 30 ng/L to 73 ng/L for adding Fe3+, 28, 35ng/L to 65, 66 ng/L for adding Cu2+ or Zn2+, and 40 ng/L to 50 ng/L for adding Ca2+, respectively. Thus, the sequences of the increase of anthracene in supernatants were the same as those of the charge densities of metal ions (Fe3+ Cu2+, Zn2+). However, adding Ca2+ at pH 6.5 only led to a minor increase of anthracene in supernatant.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

In order to understand the effect of metal ions on distribution and adsorption of anthracene on soils (water/soil = 10), Fe3+, Cu2+, Zn2+ and Ca2+ were added in the colloid solution of contaminated kaolin to probe the varies of anthracene concentrations in supernatants after 180 r/min of shaking at 28℃. The adsorption equilibrium time and equilibrium concentration of Fe3+, Cu2+, Zn2+ and Ca2+ by kaolin were about 24 h and (20 ± 3) mg/g, respectively. When contents of metal ions added were more than 30 mg/g for kaolin, the lowest concentration of kaolin colloid was (40±3)mg/L in supernatant. The total colloid concentrations in supernatants increased from 52 mg/L to 133 mg/L for adding Fe3+, 52 mg/L to 110 mg/L for adding Cu2+ or Zn2+, and 52 mg/L to 73 mg/L for adding Ca2+, respectively. Meanwhile, the increasing trends of anthracene in the supernatants were similar to those of total colloid concentrations, which were from 30 ng/L to 73 ng/L for adding Fe3+, 28, 35ng/L to 65, 66 ng/L for adding Cu2+ or Zn2+, and 40 ng/L to 50 ng/L for adding Ca2+, respectively. Thus, the sequences of the increase of anthracene in supernatants were the same as those of the charge densities of metal ions (Fe3+ Cu2+, Zn2+). However, adding Ca2+ at pH 6.5 only led to a minor increase of anthracene in supernatant.

Key concepts: Anthracene, Colloid, Chemistry, Metal ions in aqueous solution, Metal, Adsorption, Ion, Nuclear chemistry

Related papers

Back to paper searchBrowse research topicsOriginal source
Effect of adding four metal ions on distribution of anthracene on kaolin colloid — Research Paper | ScholarLens