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Article Navigation >  Acta Sedimentologica Sinica  > 2001  >  19(2): 309-314

CHEN Ji zhou, LIU Chang ling, LIU Qin fu, WANG Jun qiao, ZHANG Beng fei, CHEN Xin bang. The Study on Pianlinite Structure[J]. Acta Sedimentologica Sinica, 2001, 19(2): 309-314.
Citation: CHEN Ji zhou, LIU Chang ling, LIU Qin fu, WANG Jun qiao, ZHANG Beng fei, CHEN Xin bang. The Study on Pianlinite Structure[J]. Acta Sedimentologica Sinica, 2001, 19(2): 309-314.
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The Study on Pianlinite Structure

  • 1 Institute of material physics,Tianjin Institute of Technology, Tianjin 300191;

  • 2 Tianjin Institute of Geology, Tianjin 300061

  • Received Date: 2000-04-11
  • Using the wide angle x-rav scattering( WAXS ) and radial distribution function(RDF),the structure of pianlinitc occuring in China has been discussed.It is shown that pianlinitc is mainly composed of amorphous phase with less amount of order phase.The structural units constructing pianlinitc are tetrahedron[M04]( M=Si, Al)and octahetron[ AlO6 ](O=O,OH).The connecting of neighbour tctrahcdran with common vertex angle forms M-O lavcr( M=Al, Si),and the conncction of neighbour octahcdran with common edge or plane forms Al-0 layer. The structure of pianlinitc is formed from the such kind layers.Its structure change with temperatures is mainly caused by that of the correlation or order between structural units, and its structure in neighbour range is nearly unchanged.Pianlinitc is a clay rock with the structure different from that of the metakaolinites.
  • [1] 1 刘长龄等. 偏岭石—粘土矿物新种[J]. 科学通报，1963，（10）：59

    2 刘长龄. 沉积岩新种—偏岭石粘土岩研究[J]. 科学通报，1979（13）：611

    3 刘长龄. 晋北煤层夹矸粘土岩，偏岭石及紫矸的物质来源与成因[J].沉积学报，1990，8（1）：65

    4 刘长龄. 偏岭石矿物新资料[J]. 科学通报，1979，（12）：553

    5 陈济舟，王俊桥，毕于润. 非晶质岩石结构的RDF 研究[J]. 科学通报，1999，43（7），1875

    6 Wright A C，Desa J A E，Weeks R A J.Noncrys[J]. Solid，1984，6（7 1 / 3）：35

    7 Warren B E. X-Ray Diffraction[M]. Addison-Wesley，Reading，Mass，1969
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  • Received:  2000-04-11

The Study on Pianlinite Structure

  • 1 Institute of material physics,Tianjin Institute of Technology, Tianjin 300191;
  • 2 Tianjin Institute of Geology, Tianjin 300061
  • Received Date: 2000-04-11

Abstract: Using the wide angle x-rav scattering( WAXS ) and radial distribution function(RDF),the structure of pianlinitc occuring in China has been discussed.It is shown that pianlinitc is mainly composed of amorphous phase with less amount of order phase.The structural units constructing pianlinitc are tetrahedron[M04]( M=Si, Al)and octahetron[ AlO6 ](O=O,OH).The connecting of neighbour tctrahcdran with common vertex angle forms M-O lavcr( M=Al, Si),and the conncction of neighbour octahcdran with common edge or plane forms Al-0 layer. The structure of pianlinitc is formed from the such kind layers.Its structure change with temperatures is mainly caused by that of the correlation or order between structural units, and its structure in neighbour range is nearly unchanged.Pianlinitc is a clay rock with the structure different from that of the metakaolinites.

CHEN Ji zhou, LIU Chang ling, LIU Qin fu, WANG Jun qiao, ZHANG Beng fei, CHEN Xin bang. The Study on Pianlinite Structure[J]. Acta Sedimentologica Sinica, 2001, 19(2): 309-314.
Citation: CHEN Ji zhou, LIU Chang ling, LIU Qin fu, WANG Jun qiao, ZHANG Beng fei, CHEN Xin bang. The Study on Pianlinite Structure[J]. Acta Sedimentologica Sinica, 2001, 19(2): 309-314.
shu

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