首页> 外文OA文献 >Thermodynamic evaluation of pozzolanic reactions between activated pozzolan mix of clay waste/fly ash and calcium hydroxide
【2h】

Thermodynamic evaluation of pozzolanic reactions between activated pozzolan mix of clay waste/fly ash and calcium hydroxide

机译:粘土废料/粉煤灰的活化火山灰混合物与氢氧化钙之间火山灰反应的热力学评估

摘要

The mixture of activated paper sludge and fly ash can successfully be used as pozzolans for the manufacture of a more ecological portland cement. The saturation indexes and the mineral stability fields of a pozzolanic reaction are studied at 1, 3, 7, 28, 90, and 360 days into the reaction. The system is formed of a pozzolanic mix (activated clay waste and fly ash) and a saturated solution of Ca(OH)2Ca(OH)2 at 40°C. The behavior of the reactions is predicted in this study by means of a thermodynamic model running on a computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations. The concentration of soluble species in the aqueous solution is determined by inductively coupled plasma mass spectrometry. The evolution of the hydrated phases formed in this study and the mineral stability fields are evaluated with the geochemical programs PHREEQC and SUPCRT92. The hydrated phases produced during the pozzolanic reactions were C─ S─ H gels, C4AH13C4AH13 (calcium aluminate hydrate), C4AcH12C4AcH12 (calcium monosulfoaluminate), and layered double hydroxide (LDH)–type structures or hydrotalcite are anionic clays. The saturation index values indicate that the LDH-type structures (phyllosilicate/carbonate) are the most thermodynamically stable phase in the activated clay/fly ash–Ca(OH)2Ca(OH)2 system after 7 days of reaction. Mineral stability fields situate all the samples among the LDH-type structures (phyllosilicate/carbonate).
机译:活性纸污泥和粉煤灰的混合物可以成功地用作火山灰,以生产更生态的硅酸盐水泥。研究了火山灰反应的饱和指数和矿物稳定性场,该反应发生在第1、3、7、28、90和360天。该系统由火山灰混合物(活化的粘土废料和粉煤灰)和Ca(OH)2Ca(OH)2在40°C下的饱和溶液形成。在本研究中,通过在计算机程序上运行的热力学模型来预测反应的行为,该热力学模型用于形态分析,批反应,一维迁移和逆地球化学计算。水溶液中可溶性物质的浓度通过电感耦合等离子体质谱法测定。用地球化学程序PHREEQC和SUPCRT92评估了本研究中形成的水​​合相的演化和矿物稳定性场。火山灰反应期间产生的水合相为C–H凝胶,C4AH13C4AH13(铝酸钙水合物),C4AcH12C4AcH12(单硫酸铝钙)和层状双氢氧化物(LDH)型结构或水滑石为阴离子粘土。饱和指数值表明,经过7天的反应,LDH型结构(页硅酸盐/碳酸盐)是活化粘土/粉煤灰-Ca(OH)2Ca(OH)2系统中最热力学稳定的相。矿物稳定性场将所有样品置于LDH型结构(层状硅酸盐/碳酸盐)中。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号