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dc.contributor.authorPina, Carlos M.-
dc.contributor.authorMiranda, Rodolfo-
dc.contributor.authorGnecco, Enrico-
dc.date.accessioned2012-11-27T12:50:06Z-
dc.date.available2012-11-27T12:50:06Z-
dc.date.issued2012-02-06-
dc.identifier.citationPINA C.M., MIRANDA, R., GNECCO, E. (2012). Anisotropic surface coupling while sliding on dolomite and calcite crystals. Physical Review B, 85, 073402. DOI: 10.1103/PhysRevB.85.073402es_ES
dc.identifier.urihttp://hdl.handle.net/10261/61300-
dc.description.abstractHigh-resolution friction force microscopy has been performed on the (104) surfaces of dolomite and calcite in deionized water. The two rows of oxygen atoms alternating in a zigzag way on top of both surfaces are resolved with similar contrast while scanning along the [421̅ ] direction. Along the [010] direction, only one row is resolved, provided that the normal loading is large enough. The direction-dependent interaction between the probing tip and surface atoms is explained by numeric calculations based on the Prandtl-Tomlinson model.es_ES
dc.language.isoenges_ES
dc.publisherAmerican Physical Societyes_ES
dc.rightsopenAccesses_ES
dc.titleAnisotropic surface coupling while sliding on dolomite and calcite crystalses_ES
dc.typeartículoes_ES
dc.identifier.doi10.1103/PhysRevB.85.073402-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://link.aps.org/doi/10.1103/PhysRevB.85.073402es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextopen-
item.openairetypeartículo-
item.fulltextWith Fulltext-
item.languageiso639-1en-
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