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231223s2010 xx |||||o 00| ||eng c |
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|a 10.1021/la100377s
|2 doi
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|a eng
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| 100 |
1 |
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|a Tenório, Rômulo P
|e verfasserin
|4 aut
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| 245 |
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|a Intercalated water in synthetic fluorhectorite clay
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|c 2010
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
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|a Date Completed 31.08.2010
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|a Date Revised 10.06.2010
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|a published: Print
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|a Citation Status PubMed-not-MEDLINE
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|a (7)Li and (1)H nuclear magnetic resonance together with X-ray diffraction measurements in powdered samples and pseudocrystalline films of synthetic fluorhectorite as a function of relative ambient humidity permit to address several aspects of the structure and dynamics of intercalated water molecules. The role of proton exchange as a possibly dominant mechanism of charge transport in the one-water layer regime of hydration is reexamined. The experimental results in Li-fluorhectorite support the result of molecular simulations which predict, for Li-montmorillonite, the existence of an intermediate regime, between one-water layer and two-water layer states
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|a Journal Article
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|a Engelsberg, M
|e verfasserin
|4 aut
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|a Fossum, Jon Otto
|e verfasserin
|4 aut
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| 700 |
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|a da Silva, Geraldo J
|e verfasserin
|4 aut
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| 773 |
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|i Enthalten in
|t Langmuir : the ACS journal of surfaces and colloids
|d 1999
|g 26(2010), 12 vom: 15. Juni, Seite 9703-9
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|g volume:26
|g year:2010
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|g month:06
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