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Calcite prism

Calprismin, a novel member of mol-luskan shell proteins. Calprismin is a glycosylated protein (Mr 38 kDa) isolated from the shell calcitic prisms of the Mediterranean fan mussel Pinna no-hUis. It is soluble in acetic acid, and is acidic due to its high Asp content. It has been assumed that calprismin may act as calcite crystal-binding rather than a Ca -binding protein [F. Marin etal.,/. Biol. Chem. 2005, 280, 33895]. [Pg.61]

We adopted the prismatic layer of a bivalve shell as a model for in vitro repairing (Fig. 28). °° The prismatic layer is comprised of calcite prisms elongated in the c axis and an interprismatic organic framework. In the original prismatic layer, calcite polygonal columns 10-50 pm in diameter... [Pg.21]

In Akkin et al, a polarization-sensitive low coherence fiber interferometer was used to measure -0.5 nm, 1 ms displacements in crayfish leg nerves. Calcite prisms are used to compensate for optical path delay between the nerve reflection and a reference cover glass. The authors suggested that the technology may allow noninvasive detection of various neuropathies. [Pg.226]

Figure 11.5. Three examples showing different Habitus of later-grown calcite crystals preferentially nucleated on the edges and corners of earlier-formed calcite crystal. Changes in Habitus depending on crystallization stages or growth temperatures are indicated [3]. (a) Earlier-formed hexagonal prism (A) and later-formed scalenohedral crystal (B). (b) Earlier-formed hexagonal prism (b) and later-formed thicker crystal (a), (c) The shaded area shows an earlier-formed rhombohedral crystal, and the remaining area represents later-formed scalenohedral crystals. Figure 11.5. Three examples showing different Habitus of later-grown calcite crystals preferentially nucleated on the edges and corners of earlier-formed calcite crystal. Changes in Habitus depending on crystallization stages or growth temperatures are indicated [3]. (a) Earlier-formed hexagonal prism (A) and later-formed scalenohedral crystal (B). (b) Earlier-formed hexagonal prism (b) and later-formed thicker crystal (a), (c) The shaded area shows an earlier-formed rhombohedral crystal, and the remaining area represents later-formed scalenohedral crystals.
When light is passed through a polarizer such as a calcite Nicol prism, the electric vector is parallel to the plane of polarization. The electric vector transforms in different ways when the polarized light is transmitted through a single crystal of a mineral, depending on its crystal symmetry. [Pg.74]

Hexagonal Four axes three in a plane at 60 degrees to each other, and one through the intersection of those axes Prism, pyramid, rhombohedron Quartz, beryl, tourmaline, calcite... [Pg.5]

Elmer Photoelectric Polarimeter, Model 141. Optical rotatory dispersion measurements were made either with the Perkin-Elmer instrument equipped with a Bausch and Lomb High Intensity Grating Monochromator, or with a manual spectropolarimeter constructed by Kirschner and co-workers (1) at Wayne State University. This instrument has been modified by replacing the calcite polarizing and analyzing prisms with quartz prisms and changing light source to a 500-watt Hanovia Xenon Arc Lamp. [Pg.368]

Crossed Nicol prisms An arrangement of two materials (calcite polarizing prisms or Polaroid discs) such that the first, the polarizer, transmits plane-polarized light that passes through the second, the analyzer, only if oriented in specific ways. [Pg.176]


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