期刊文献+

热处理对凹凸棒石结构、形貌和表面性质的影响 被引量:179

EFFECT OF HEAT TREATMENT ON STRUCTURE, MORPHOLOGY AND SURFACE PROPERTIES OF PALYGORSKITE
下载PDF
导出
摘要 通过差热、热重、X射线衍射、透射电镜综合分析研究了凹凸棒石在热处理过程中脱水作用、结构、形貌变化之间的关系。结果表明在65℃,凹凸棒石开始脱去外表面吸附水,98℃脱去孔道水,凹凸棒石结构、形貌没有任何变化,微孔孔道直径未变。到230℃,部分脱去凹凸棒石的结晶水,由于脱出部分结晶水,凹凸棒石结构开始出现折叠。在481℃,脱去凹凸棒石的剩余结晶水。在595℃左右,缓慢脱去凹凸棒石的结构水,孔道结构完全塌陷,链层结构和形貌基本保持不变。高于800℃,凹凸棒石晶体开始变形弯曲,并变为无定形态。在827℃出现放热效应,形成方石英,这与1000℃出现严重烧结形貌特征一致。 The dehydration, structural and morphological properties of palygorskite during heat treatment were studied by thermogravimetric and differential thermal analysis, X-ray diffrction and high resolution transmission electron microscopy. The results indicate that water is absorbed in the channel and outside surface of the palygorskite samples, causing dehydration at 65℃ and 98℃, respectively; however, the structure and morphology of the samples are remained and unchanged. Some of the water in the samples is lost at 230℃, resulting in a structural fold in the structure of palygorskite. Residual water in the samples is lost at 481℃ and hydroxyls are lost at 595℃, degrading the channel structure, but the ribbon-like structure and morphology of palygorskite are retained. The morphology of palygorskite fibers is curved after heat treatment over 800℃, and the structure is transformed from a crystal structure to an amorphous structure. Then an exothermic reaction occurs at 827℃, and two new phases of cristobalite and enstatite are formed, which is similar to the sintering state at 1 000℃.
出处 《硅酸盐学报》 EI CAS CSCD 北大核心 2006年第11期1406-1410,共5页 Journal of The Chinese Ceramic Society
基金 国家自然科学基金(40472026)资助项目。
关键词 凹凸棒石 热处理 透射电镜 表面改性 晶体结构 palygorskite heat treatment high resolution transmission electron microscope surface improvement crystal structure
  • 相关文献

参考文献10

  • 1[1]GALAN E.Properties and applications ofpalygorskite-sepiolite clays[J].Clay Miner,1996,31(4):443-453.
  • 2CHEN Tianhu1,,XU Huifang2,LU Anhuai3,XU Xiaochun1,PENG Shuchuan1 2 &YUE Shucang1 1.College of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009,China,2.Department of Geology and Geophysics,University of Wisconsin,Madison,WI53706,USA,3.Department of Geology,Peking University,Beijing 100871,China Correspondence should be addressed to Chen Tianhu(email: tianhu@mail.hf.ah.cn or cth168@hotmail.com).Direct evidence of transformation from smectite to palygorskite:TEM investigation[J].Science China Earth Sciences,2004,47(11):985-994. 被引量:16
  • 3[3]BARRIOS M S,GONZALEZ L V F,RODRIGUEZ M A V.Acid activation of a palygorskite of with HC1:development of physicochemical,textural and surface-properties[J].Appl Clay Sci,1995,10(3):247-258.
  • 4[4]YACAMAN J,RENDON L,ARENAS J,et al.Maya blue paint:an ancient nanostructured material[J].Science,1996,273(5272):223-225.
  • 5[5]NEAMAN A,SINGER A.Rheological properties of aqueous suspensions of palygorskite[J].Soil Sci Soc Am J,2000,64(1):427-436.
  • 6[8]SHARIATMADARI H,MERMUT A R,BENKE M B.Sorption of selected cationic and neutral organic molecules on palygorskite and sepiolite[J].Clays Clay Miner,1999,47(1):44-53.
  • 7[10]GARCIA A S,ALVAREZ A A,JUNENEZ O B.Sorption of heavy metals from industrial waste water by low cost mineral silicates (palygorskite,smectite)[J].Clay Miner,1999,34(3):469-478.
  • 8[11]QIU Zunan,ZHANG Yi,FANG Yuqiao.Removal ofoil from concentrated wastewater by attapulgite and coagulant[J].Water Quality Res J Can,1995,30(1):89-99.
  • 9[19]KUANG Wenxing,FACEY GA,DETLLIER C.Dehydration and rehydration of palygorskite and the influence of water on the nanoporous[J].Clay Clay Miner,52(5):635-642.
  • 10[21]McHALE J M,AUROUX A,PERROTTA AJ,et al.Surface energies and thermodynamic phase stability in nanocrystalline aluminas[J].Science,1997,277(8):788-791.

共引文献15

同被引文献1620

引证文献179

二级引证文献720

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部