Abrupt sand-dune accumulation at the northeastern margin of the Tibetan Plateau challenges the wet MIS3a inferred from numerous lake-highstands

dc.bibliographicCitation.firstPage25820
dc.bibliographicCitation.volume6
dc.contributor.authorLong, Hao
dc.contributor.authorFuchs, Markus
dc.contributor.authorYang, Linhai
dc.contributor.authorCheng, Hongyi
dc.date.accessioned2023-03-30T05:20:38Z
dc.date.available2023-03-30T05:20:38Z
dc.date.issued2016
dc.description.abstractWe report on hollow shell-shell nanogels with two polymer shells that have different volume phase transition temperatures. By means of small angle neutron scattering (SANS) employing contrast variation and molecular dynamics (MD) simulations we show that hollow shell-shell nanocontainers are ideal systems for controlled drug delivery: The temperature responsive swelling of the inner shell controls the uptake and release, while the thermoresponsive swelling of the outer shell controls the size of the void and the colloidal stability. At temperatures between 32 °C < T < 42 °C, the hollow nanocontainers provide a significant void, which is even larger than the initial core size of the template and they possess a high colloidal stability due to the steric stabilization of the swollen outer shell. Computer simulations showed, that temperature induced switching of the permeability of the inner shell allows for the encapsulation in and release of molecules from the cavity.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11816
dc.identifier.urihttp://dx.doi.org/10.34657/10849
dc.language.isoeng
dc.publisher[London] : Macmillan Publishers Limited, part of Springer Nature
dc.relation.doihttps://doi.org/10.1038/srep25820
dc.relation.essn2045-2322
dc.relation.ispartofseriesScientific reports 6 (2016)
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectChinaeng
dc.subjectsedimenteng
dc.subjectvalidityeng
dc.subject.ddc500
dc.subject.ddc600
dc.titleAbrupt sand-dune accumulation at the northeastern margin of the Tibetan Plateau challenges the wet MIS3a inferred from numerous lake-highstandseng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleScientific reports
tib.accessRightsopenAccess
wgl.contributorLIAG
wgl.subjectGeowissenschaftenger
wgl.subjectUmweltwissenschaftenger
wgl.typeZeitschriftenartikelger
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