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我国硅灰石矿资源储量居世界第一,且产量居世界前列。随着多年的勘查与开发,硅灰石矿的开发利用已由传统领域向新的应用领域探索拓展。本文在收集整理现有硅灰石矿床、海关进出口等数据资料的基础上,在全国范围内搜集了77个矿产地,其中超大型8处,划分了7个重要成矿区,总结了我国硅灰石矿产开发利用现状、进出口贸易情况,对硅灰石矿产的行业发展提出了建议。 相似文献
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作者首次在该区找到了硅灰石矿。在专题研究基础上，分析了区域地层、构造、岩浆活动和硅灰石矿床地质特征等，提出该硅灰石矿主要产于康古尔断裂带内的花岗岩与碳酸盐地层接触带，属矽卡岩型硅灰石矿。对区内花岗岩、碳酸盐地层、矽卡岩、大地构造等硅灰石成矿条件作了分析，初步提出了该矿主要应用领域为建筑陶瓷工业。 相似文献
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在反应体系pH≤1．5时，硅灰石与盐酸快速反应，经40－100min反应后，体系分为固液两相，固相为水合 二氧化硅沉淀及少量酸不溶性杂质矿物，液相为以溶胶形式存在的二氧化硅和大量CaCl2；当反应pH值在0．3－0．6时，液相中以硅溶胶形式存在的二氧化硅量最大，占总量46％以上。快速反应中仍存在少量具有慢速反应特征的柱状颗粒，该颗粒中心CaSiO3很难反应完全。快速反应产物经表面积较大，若在酸反应前添加有机助剂聚乙二醇（PEG）,反应pH值在0．3－0．6。反应时间40－100min，反应后用KOH溶液中和到pH＝4，可制备高比表面积多孔SiO2，比表面积＞430m^2／g，孔径1－2nm。 相似文献
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This work deals with the identification and kinetics of crystallisation of the wollastonite polytypes which form in the system
CaO-SiO2 in the temperature range 700–1000 °C. The kinetics of phase transformations in the system have been determined from analysis
of in situ synchrotron X-ray powder diffraction data. Two different systems with the same compositions were investigated:
one is more reactive, having grains with a larger surface area per unit volume, the other is less reactive, being composed
of grains with a smaller surface area per unit volume. 1T-wollastonite forms first and progressively transforms in an intermediate
1Td-wollastonite disordered form. Both phases in turn transform into 2M-wollastonite polytype. Differences in the polytypes
forming and reaction kinetics were observed for the two systems. In the more reactive system, the conversion 1T to 1Td polytypes
is the dominant process. The kinetic parameters calculated using the Avrami models fully describe the reaction process of
formation of both polytypes and transformation of one polytype into the other.
Received: 3 August 1999 / Accepted: 20 March 2000 相似文献
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