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二氧化硫在脱钙后海水体系中的溶解平衡

谢英惠 曹海楠 赵颖颖 袁俊生

化工进展2016,Vol.35Issue(4):1012-1016,5.
化工进展2016,Vol.35Issue(4):1012-1016,5.DOI:10.16085/j.issn.1000-6613.2016.04.007

二氧化硫在脱钙后海水体系中的溶解平衡

Solubility equilibrium of SO2 in the decalcified seawater

谢英惠 1曹海楠 1赵颖颖 1袁俊生1

作者信息

  • 1. 河北工业大学海洋科学与工程学院,天津 300130
  • 折叠

摘要

Abstract

Compared with normal seawater,the content of HCO3− in the seawater of calcium removed using CO2 is higher. Because HCO3− can react with hydrogen sulfite produced by sulfur dioxide dissolving in water,which in return helps increase the solubility of sulfur dioxide. Therefore,the effect of the amount of HCO3− and Ca2+ on the solubility of sulfur dioxide in seawater was studied at temperatures of 34.0—63.9℃ with N2 as inert carrier gas and under 1atm. The results showed that the solubility of SO2 in standard seawater significantly reduced linearly with increasing temperature. The increase of HCO3− ion concentration in demineralized seawater will enhance the solubility of SO2 in water. But there is no significant effect of the reduction of Ca2+ ion concentration on the SO2solubility within the studied scope. It can be concluded that sulfur dioxide shows a better dissolution performance in the seawater decalcified by CO2 than in the standard seawater,and this study provides a theoretical support to the coupling of flue gas desulfurization and seawater decalcification using CO2.

关键词

脱钙海水/溶解性能/二氧化硫

Key words

decalcified seawater/solubility/sulfur dioxide

分类

化学化工

引用本文复制引用

谢英惠,曹海楠,赵颖颖,袁俊生..二氧化硫在脱钙后海水体系中的溶解平衡[J].化工进展,2016,35(4):1012-1016,5.

基金项目

国家“十二五”科技支撑计划(2015BAB09B00)、国家自然科学基金(21306037)、天津市自然科学基金(13JCQNJC05600、14JCYBJC20700)及河北省高层次人才资助项目(C2013003041)。 ()

化工进展

OA北大核心CSCDCSTPCD

1000-6613

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