原文服务方: 地球化学学报(英文)       
摘要:
In order to clarify the dynamic process of feldspar dissolution–precipitation and explore the formation mechanism of secondary porosity, six batch reactor experiments were conducted at 200℃ and pH = 7 measured at room temperature. Temporal evolution of fluid chemistry was analyzed with an inductively coupled plasma optical emission spectrometer (ICP-OES). Solid reaction products were retrieved from six batch experiments terminated after 36, 180, 276, 415, 766 and 1008 h. Scanning electron microscopy (SEM) revealed dissolution features and significant secondary mineral adhered on the feldspar surface. The process of feldspar dissolution–precipitation proceeded slowly and full equilibrium was not achieved after 1008 h. Saturation indices suggested that the albite and K-feldspar dissolution occurred throughout the experiments. The average dissolution rates for albite and K-feldspar were 2.28 × 10-10 and 8.51 × 10-11 mol m-2 s-1 , respectively. Based on the experimental data, the reaction process of alkaline feldspar was simulated and the secondary porosity had increased 0.3% after the experiment.
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篇名 An experimental study on dynamic coupling process of alkaline feldspar dissolution and secondary min
来源期刊 学科 地球科学
关键词 Alkaline feldspar Dissolution rate Precipitation Mineral conversion Secondary porosity
年,卷(期) 2022,(6) 所属期刊栏目
研究方向 页码范围 872-882
页数 10页 分类号
字数 语种 英文
DOI 10.1007/s11631-019-00326-0
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Alkaline feldspar
Dissolution rate
Precipitation
Mineral conversion
Secondary porosity
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地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
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230
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