Oriented crystallization of calcium carbonate under self-organized monolayers of amide-containing phospholipids

Langmuir

Volumn 17, Issue 12, 2002, Pages 3623-3628

  Buijnsters, Peter J J A ^a,b   Donners, Jack J J M ^c   Hill, Susan J ^d   Heywood, Brigid R ^d   Nolte, Roeland J M ^b,c   Zwanenburg, Binne ^b   Sommerdijk, Nico A J M ^c  

^a JANSSEN RESEARCH FOUNDATION   (Belgium)

^b RADBOUD UNIVERSITY NIJMEGEN   (Netherlands)

^c EINDHOVEN UNIVERSITY OF TECHNOLOGY   (Netherlands)

^d KEELE UNIVERSITY   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

AQUEOUS PHASE;

CALCITE; CONFORMATIONS; CRYSTAL ORIENTATION; HYDROGEN BONDS; NUCLEATION; PHASE INTERFACES; PHOSPHOLIPIDS; SELF ASSEMBLY;

CRYSTALLIZATION;

EID: 0037067269     PISSN: 07437463     EISSN: None     Source Type: Journal    
DOI: 10.1021/la001765n     Document Type: Article

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47. s symmetry and is triangular in projection with only two of the four basal edges being expressed. Type II calcite can be formed through nucleation from different faces, that is, [00.1] (n-eicosyl sulphate) and [1-10] (stearic acid). The calcite formed in the present case is of type II and has nucleated from the (10.0) face. Type I calcite is thought to arise from a realignment and subsequent secondary growth of type II calcite at the monolayer surface.
48. Under liquid expanded monolayers also a small amount of type I vaterite was formed (approximately 15% of the crystals). When the experiments were performed under compressed monolayers, this number was reduced to approximately 8%.
49. 17.
50. In addition, a significant amount of vaterite crystals was observed.
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54. 2 deduced from these models is in good agreement with the value obtained from the π-A isotherm.