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西宁降尘的柠檬酸酸溶特性研究
  • ISSN号:1000-4734
  • 期刊名称:《矿物学报》
  • 时间:0
  • 分类:P579[天文地球—矿物学;天文地球—地质学] X513[环境科学与工程—环境工程]
  • 作者机构:[1]西南科技大学固体废物处理与资源化教育部重点实验室,四川绵阳621010, [2]西南科技大学环境与资源学院,四川绵阳621010
  • 相关基金:国家自然基金重点项目(批准号:41130746)
中文摘要:

以西宁降尘为研究对象,探讨柠檬酸溶解2d过程中体系的pH及电导率变化,借助XRD、FTIR、SEM和ICP等表征手段,对降尘经酸处理后的残余固体及上清液进行分析。降尘加入柠檬酸的前4h,反应溶液pH迅速上升;电导率从初始的4.3lms/cm迅速升高到5.61ms/cm,然后缓慢下降;8h后,pH和电导率基本达到稳定。根据XRD分析,白云石特征峰(d=-0.2886nm、0.2190nm等)和方解石特征峰(d=-0.3031nm、0.2282nm等)完全消失;根据红外分析,代表碳酸盐矿物的特征峰(1430cm0和877Clrl。)也消失,结合XRD结果可以得出方解石和白云石在柠檬酸作用2d后完全溶解。柠檬酸溶出了降尘中大量的Ca2+,K+,Mg2+,Fe3+,Al3+,Si等元素,其中Ca2+的溶出量达到711.63mg/L。柠檬酸对不同元素溶出的促进作用由强到弱依次为:Fe〉AI〉Si〉Ca〉Mg〉K。在柠檬酸的作用下,降尘中的矿物被全部或部分溶解,其中碳酸盐矿物几乎完全溶解。

英文摘要:

pH and conductivity was tested during dissolution process for Xining dustfall in citric acid to evaluate changes of reaction solution. After 2 days' dissolution, SEM, FTIR, SEM and ICP analysis method was applied to analyze the residual solid and filtrate. PH of reaction solution increased fast in 4 hours, and conductivity sharply increases from initial 4.31 ms/cm to 5.61 ms/cm in 1 minute after addition of dustfall, then followed a slowing down stage. After 4 hours, both the pH and conductivity become stable. Based on comparatively analyzing of XRD for dustfall and residual solid, characteristic peak of calcite (e.g. 20=-30.986°, 41.182°) and dolomite (e.g. 20=-29.455°, 39.507°) are disappeared. Similar results can be seen from FTIR analysis, with absorption peak (1430 cmland 877cm-1) of carbonate minerals disappeared. Combined above two analysis results, we can demonstrate that calcite and dolomite in dustfall are dissolved in the 0.5 mol/L citric acid solution. Amount of metal cations including Ca2+, K+, Mg2+, Fe3+, A13+ and Si are extracted from dustfall during the dissolution, of which the dissolution quantity of Ca reached 711.63 mg/L. Compared with dissolution in distilled water, effect of citric acid on different elements can be rank as follow: Fe〉Al〉Si〉Ca〉Mg〉K. After dissolved in 0.5 mol/L citric acid, some minerals in dustfall disappear and amount of metal elements are extracted, especially the carbonate minerals almost dissolved completely, and structure of silicate minerals changed as the extraction of elements.

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期刊信息
  • 《矿物学报》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院地球化学研究所 中国矿物岩石地球化学学会
  • 主编:胡瑞忠
  • 地址:贵州省贵阳市观山湖区林城西路99号
  • 邮编:550081
  • 邮箱:kwxb@ms.gyig.ac.cn
  • 电话:0851-5891352
  • 国际标准刊号:ISSN:1000-4734
  • 国内统一刊号:ISSN:52-1045/P
  • 邮发代号:66-17
  • 获奖情况:
  • 国内外数据库收录:
  • 被引量:10998