Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (4/4 displayed)

  • 2019 An experimental study of SO 2 reactions with silicate glasses and supercooled melts in the system anorthite–diopside–albite at high temperature 11citations
  • 2013In situ metal imaging and Zn ligand-speciation in a soil-dwelling sentinel10citations
  • 2012Qualitative and quantitative analysis of three-phase distributions of oil, water and gas in Bentheimer sandstone using micro-CT imagingcitations
  • 2002XEUS - the X-ray Evolving Universe Spectroscopy Missioncitations

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Chart of shared publication
Guagliardo, P.
1 / 2 shared
Henley, R. W.
1 / 2 shared
Middleton, J. P.
1 / 2 shared
King, Penelope
1 / 11 shared
Mcmorrow, L.
1 / 1 shared
Renggli, C. J.
1 / 1 shared
Morgan, A. J.
1 / 1 shared
Harmer, Jane
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Mosselmans, J. F. W.
1 / 1 shared
Kille, P.
1 / 1 shared
Winters, C.
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Oreilly, M.
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Bennett, A.
1 / 2 shared
Gunning, P.
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Fisher, P.
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Charnock, J. M.
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Knackstedt, M.
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Pinczewski, W. V.
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Cinar, Y.
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Feali, M.
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Francois, N.
1 / 1 shared
Arns, Ji Youn
1 / 2 shared
Arns, C. H.
1 / 6 shared
Parmar, Arvind
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Hasinger, G.
1 / 2 shared
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2013
2012
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Co-Authors (by relevance)

  • Guagliardo, P.
  • Henley, R. W.
  • Middleton, J. P.
  • King, Penelope
  • Mcmorrow, L.
  • Renggli, C. J.
  • Morgan, A. J.
  • Harmer, Jane
  • Mosselmans, J. F. W.
  • Kille, P.
  • Winters, C.
  • Oreilly, M.
  • Bennett, A.
  • Gunning, P.
  • Fisher, P.
  • Charnock, J. M.
  • Knackstedt, M.
  • Pinczewski, W. V.
  • Cinar, Y.
  • Feali, M.
  • Francois, N.
  • Arns, Ji Youn
  • Arns, C. H.
  • Parmar, Arvind
  • Hasinger, G.
OrganizationsLocationPeople

document

Qualitative and quantitative analysis of three-phase distributions of oil, water and gas in Bentheimer sandstone using micro-CT imaging

  • Knackstedt, M.
  • Pinczewski, W. V.
  • Cinar, Y.
  • Feali, M.
  • Francois, N.
  • Arns, Ji Youn
  • Arns, C. H.
  • Turner, M.
Abstract

<p>It is now widely acknowledged that continuous oil spreading films observed in two-dimensional glass micro-model studies for strongly water wet three-phase oil, water and gas systems are also present in real porous media and result in lower tertiary gas flood residual oil saturations than for corresponding negative spreading systems which do not display oil spreading behavior. However, it has not been possible to directly confirm the presence of spreading films in real porous media in threedimensions and little is understood of the distribution of the phases within the complex geometry and topology of actual porous media for different spreading conditions. This paper describes a preliminary study using high resolution X-ray microtomography to image the distribution of oil, water and gas after tertiary gas flooding to recover waterflood residual oil for two set of fluids, one positive spreading and the other negative spreading, for strongly water wet conditions in Bentheimer sandstone. We show that for strongly water-wet conditions and a positive spreading system the oil phase remains connected throughout the pore space and results in a low tertiary gas flood residual oil saturation. The residual oil saturation for the corresponding negative spreading system is significantly higher and this is shown to be related to the absence of oil films in this system. The presence of films for positive spreading systems and the absence of such films for negative spreading systems is further confirmed by the computation of the Eurler characteristic for each phase.</p>

Topics
  • porous
  • impedance spectroscopy
  • pore
  • phase
  • glass
  • glass
  • two-dimensional
  • quantitative determination method