VIAF

Virtual International Authority File

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Leader     00000nz a2200037n 45 0
001     WKP|Q84973509  (VIAF cluster)  (Authority/Source Record)
003     WKP
005     20241121000130.0
008     241121nneanz||abbn n and d
035 ‎‡a  (WKP)Q84973509‏
024 ‎‡a  0000-0001-8270-3006‏ ‎‡2  orcid‏
035 ‎‡a  (OCoLC)Q84973509‏
100 0 ‎‡a  Yi Yang‏ ‎‡c  researcher (ORCID 0000-0001-8270-3006)‏ ‎‡9  en‏
670 ‎‡a  Author's A mechanistic understanding of plagioclase dissolution based on Al occupancy and T-O bond length: from geologic carbon sequestration to ambient conditions‏
670 ‎‡a  Author's Direct Observation of Coupled Geochemical and Geomechanical Impacts on Chalk Microstructure Evolution under Elevated CO2 Pressure‏
670 ‎‡a  Author's Dissolved CO2 Increases Breakthrough Porosity in Natural Porous Materials.‏
670 ‎‡a  Author's Impact of microstructure evolution on the difference between geometric and reactive surface areas in natural chalk‏
670 ‎‡a  Author's In-Situ X-ray Tomography Study of Cement Exposed to CO2 Saturated Brine‏
670 ‎‡a  Author's Patterns of entropy production in dissolving natural porous media with flowing fluid‏
670 ‎‡a  Author's Retraction of the dissolution front in natural porous media.‏
670 ‎‡a  Author's Structure-dependent interactions between alkali feldspars and organic compounds: implications for reactions in geologic carbon sequestration.‏
909 ‎‡a  (orcid) 0000000182703006‏ ‎‡9  1‏
919 ‎‡a  patternsofentropyproductionindissolvingnaturalporousmediawithflowingfluid‏ ‎‡A  Patterns of entropy production in dissolving natural porous media with flowing fluid‏ ‎‡9  1‏
919 ‎‡a  impactofmicrostructureevolutiononthedifferencebetweengeometricandreactivesurfaceareasinnaturalchalk‏ ‎‡A  Impact of microstructure evolution on the difference between geometric and reactive surface areas in natural chalk‏ ‎‡9  1‏
919 ‎‡a  dissolvedco2increasesbreakthroughporosityinnaturalporousmaterials‏ ‎‡A  Dissolved CO2 Increases Breakthrough Porosity in Natural Porous Materials.‏ ‎‡9  1‏
919 ‎‡a  directobservationofcoupledgeochemicalandgeomechanicalimpactsonchalkmicrostructureevolutionunderelevatedco2pressure‏ ‎‡A  Direct Observation of Coupled Geochemical and Geomechanical Impacts on Chalk Microstructure Evolution under Elevated CO2 Pressure‏ ‎‡9  1‏
919 ‎‡a  mechanisticunderstandingofplagioclasedissolutionbasedonaloccupancyandtobondlengthfromgeologiccarbonsequestrationtoambientconditions‏ ‎‡A  A mechanistic understanding of plagioclase dissolution based on Al occupancy and T-O bond length: from geologic carbon sequestration to ambient conditions‏ ‎‡9  1‏
919 ‎‡a  insitu10raytomographystudyofcementexposedtoco2saturatedbrine‏ ‎‡A  In-Situ X-ray Tomography Study of Cement Exposed to CO2 Saturated Brine‏ ‎‡9  1‏
919 ‎‡a  structuredependentinteractionsbetweenalkalifeldsparsandorganiccompoundsimplicationsforreactionsingeologiccarbonsequestration‏ ‎‡A  Structure-dependent interactions between alkali feldspars and organic compounds: implications for reactions in geologic carbon sequestration.‏ ‎‡9  1‏
919 ‎‡a  retractionofthedissolutionfrontinnaturalporousmedia‏ ‎‡A  Retraction of the dissolution front in natural porous media.‏ ‎‡9  1‏
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997 ‎‡a  0 0 lived 0 0‏ ‎‡9  1‏