1933
DOI: 10.1524/zkri.1933.86.1.340
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Kristallstruktur und Quellung von Montmorillonit

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Cited by 108 publications
(66 citation statements)
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“…Alternatively, osmotic swelling potentially represents a gentler, cheap and scalable route to utterly separate a layered material into singular layers. Langmuir 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 The principle of osmotic swelling goes back to the swelling of graphite oxide (1932) (13) and montmorillonite (14). Here we report a systematic study of the exfoliation of a synthetic 2D layered silicate via osmotic swelling that provides direct insight into the conditions for ionic layer separation and the build-up of the electric double layer, and outlines the lyotropic phase behavior at extreme aspect ratios of the resulting layered material over more than 4 orders of magnitude in concentration from the dry powder to highly dilute solutions.…”
Section: Introductionmentioning
confidence: 99%
“…Alternatively, osmotic swelling potentially represents a gentler, cheap and scalable route to utterly separate a layered material into singular layers. Langmuir 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 The principle of osmotic swelling goes back to the swelling of graphite oxide (1932) (13) and montmorillonite (14). Here we report a systematic study of the exfoliation of a synthetic 2D layered silicate via osmotic swelling that provides direct insight into the conditions for ionic layer separation and the build-up of the electric double layer, and outlines the lyotropic phase behavior at extreme aspect ratios of the resulting layered material over more than 4 orders of magnitude in concentration from the dry powder to highly dilute solutions.…”
Section: Introductionmentioning
confidence: 99%
“…Pauling (1930a,b) published detailed XRD spectra of clays and established the structure of micas, brittle micas, talc, pyrophyllite, and chlorites. Th e structure of other clays quickly followed, such as kaolinite (Ross and Kerr, 1931), montmorillonite (Hofmann et al, 1933;Ross and Hendricks, 1945), and vermiculite (Gruner, 1934).…”
Section: X-ray Diffractionmentioning
confidence: 99%
“…At the Technische Hochschule in Berlin, Hofmann et al (1933) suggested an atomic arrangement for montmorillonite that featured an expanding structure. Variable numbers of layers of water molecules were possible between the silicate sheets, thereby providing a variable c-axis dimension.…”
Section: Development Of the "Clay Minerals" Conceptmentioning
confidence: 99%