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钠硼解石——水体系溶解和相平衡的研究(英文)

Study on Dissolution and Phase Equilibrium in Ulexite-water System

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【作者】 陈若愚高世扬冯守华夏树屏陈正隆

【Author】 CHEN Ruo-Yu*,1 GAO Shi-Yang 2 FENG Shou-Hua3 XIA Shu-Ping2 CHEN Cheng-Lung4(1Department of Chemical Engineering, Jiangsu Polytechnic University, Changzhou 213016)(2Institute of Salt Lakes, Xian Branch, Academia Sinica, Xi’an 710043)(3Key Lab of Inorganic Hydrothermal Synthesis and Preparation, Jilin University, Changchun 130023)(4Department of Chemistry, Taiwan SUN Yat-Sen University, Kaohsiung 80424)

【机构】 江苏工业学院化学工程系中科院盐湖所西安二部吉林大学水热合成实验室台湾中山大学化学系 常州213016西安710043长春130023高雄80424

【Abstract】 Ulexite dissolution in water has been studied in the wide temperature range from 10℃ to 93 ℃ and two higher temperatures at 120 ℃ and 240 ℃. The analytical results showed that ulexite dissolved congruently from 10 ℃ to 35 ℃ and incongruently from 40 to 68 ℃. The solid component of ulexite, NaCaB5O6(OH)6·5H2O was dehydrated to form NaCaB5O6(OH)6·H2O from 50 to 68 ℃ and finally amorphous solid at 68 ℃. This amorphous solid converted into priceite at 71 ℃ and then converted completely to priceite at the boiling point(93 ℃) of the solution. At both 120 and 240 ℃, the dissolution of ulexite was an incongruent process. Above 120 ℃, ulexite became amorphous solid and then transformed into priceite. In addition to the solid to solid transformation, crystallization of priceite from the solution has also been observed. Based on our experimental results, mechanisms of dissolution, transformation, and crystallization of borate in ulexite-water system are discussed.

【基金】 国家自然科学基金资助项目(No.29971032)。
  • 【文献出处】 无机化学学报 ,Chinese Journal of Inorganic Chemistry , 编辑部邮箱 ,2004年07期
  • 【分类号】O642
  • 【被引频次】9
  • 【下载频次】118
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