% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@INPROCEEDINGS{Rezaeyan:863047,
      author       = {Rezaeyan, A. and Pipich, V. and Bertier, P. and Seemann, T.
                      and Leu, L. and Kampman, N. and Feoktystov, A. and Barnsley,
                      L. and Busch, A.},
      title        = {{Q}uantitative {A}nalysis of the {P}ore {S}tructure of
                      {P}remature-{T}o-{P}ostmature {O}rganic {R}ich {M}udrocks
                      {U}sing {S}mall {A}ngle {N}eutron {S}cattering},
      reportid     = {FZJ-2019-03169},
      pages        = {},
      year         = {2019},
      abstract     = {The pore structure of organic rich mudrocks is associated
                      with both inorganic and organic constituents. The
                      contribution of organic matter to the pore structure has
                      been investigated on Posidonia and Bossier Shale samples
                      having different organic carbon content and thermal
                      maturity. Development and distribution of organic matter
                      pores were studied by using small angle neutron scattering
                      technique at a broad pore scale size investigation, from 2
                      nm to 2 µm. The pore structure of the mudrocks studied is
                      highly complicated at which total pore volume and specific
                      surface area are not significantly affected by thermal
                      maturation, however, the maturity attribute contributes to
                      different pore size distribution on meso- and macro-pores.
                      Thermal maturation is likely to be the factor of
                      amalgamating small organic matter pores into larger pores in
                      overmature organic rich mudrocks, potentially causing an
                      increase in pore volume at macroscale pores. Although not
                      considerably, the increased macroporosity can enhance the
                      permeability of pore network for viscous gas flow in organic
                      rich mudrocks.},
      month         = {Apr},
      date          = {2019-04-28},
      organization  = {Sixth EAGE Shale Workshop, Bordeaux
                       (France), 28 Apr 2019 - 1 May 2019},
      cin          = {JCNS-FRM-II / Neutronenstreuung ; JCNS-1 / MLZ},
      cid          = {I:(DE-Juel1)JCNS-FRM-II-20110218 /
                      I:(DE-Juel1)JCNS-1-20110106 / I:(DE-588b)4597118-3},
      pnm          = {6G4 - Jülich Centre for Neutron Research (JCNS) (POF3-623)
                      / 6G15 - FRM II / MLZ (POF3-6G15)},
      pid          = {G:(DE-HGF)POF3-6G4 / G:(DE-HGF)POF3-6G15},
      experiment   = {EXP:(DE-MLZ)KWS1-20140101 / EXP:(DE-MLZ)KWS3-20140101},
      typ          = {PUB:(DE-HGF)8},
      doi          = {10.3997/2214-4609.201900309},
      url          = {https://juser.fz-juelich.de/record/863047},
}