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Mineralization matrix development

The polymetallic veins are poorly exposed at surface and are characterized by the presence of gossans with remnants of breccias with quartz matrix and oxidized sulfide clasts. Hypogene polymetallic mineralization is characterized by the presence of massive and banded sulfide veins and sulfide breccias up to 13 m thick. This mineralization is developed In... [Pg.170]

Skeletal structures with matrix development. Cyanobacterium species of the Genus Geitleria are known to form a thick mineral deposit on their surface, which is composed of successive layers of elongated needle-shaped calcite crystals (Lowenstam, 1981) 73). [Pg.29]

Three distinct periods of osteoblast differentiation at the genetic level have been identified during in vitro examination of developing osteoblasts after initial adhesion to a surface (1) cell proliferation and extracellular matrix synthesis, (2) extracellular matrix development and maturation, and (3) extracellular matrix mineralization (Stein and Lian, 1993). A schematic of the time course of osteoblast function and synthesis of extracellular matrix proteins on a newly implanted biomaterial is shown in Fig. 6. [Pg.136]

In addition to mediating cell adhesion, it has been demonstrated that integrin expression by osteoblasts determines their phenotypic expression (see the section Osteoblasts The Bone-Forming Cells ). For example, addition of either soluble concentrations of RGD (Moursi et al, 1996) or antibodies of the integrin pair avp() (Moursi et al., 1997) to confluent osteoblast cultures, blocked initiation and formation of mineral nodules these results provided evidence that integrin-fibronectin interactions leading to extracellular matrix development play a crucial role in osteoblast function (Moursi etal., 1996,1997). [Pg.144]

A method has been developed, utilizing sink float procedures, which calculates the H/C and N/C ratios in raw shales. In addition the technique eliminates the need for acid extraction to obtain kerogen and also estimates the H and N content of the mineral matrix. [Pg.397]

Calcium and phosphorus are major minerals that are needed for the development of healthy bones and teeth. These two minerals are found in a crystalline calcium phosphate mineral known as hydroxyapatite, [Cajo(P04) (OH)2l, that makes up the mineral matrix of bone and teeth. In addition, calcium is required for normal blood clotting and muscle function. The RDA for calcium is 1200 mg/day for adults between nineteen and twenty-four years of age and 800 mg/day for adults over age twenty-five. Milk, cheese, canned salmon, and dark green leafy vegetables are all rich sources of dietary calcium. [Pg.789]

R. U. Vaidya and K. K. Chawla, in K. Upadhya, ed.. Developments in Metal and Ceramic Matrix Composites, The Minerals, Metals and Matedals Society,... [Pg.205]

Cemented tungsten carbides also find use as a support for polycrystalline diamond (PCD) cutting tips, or as a matrix alloy with cobalt, nickel, copper, and iron, ia which diamond particles are embedded. These tools are employed ia a variety of iadustries including mineral exploration and development oil and gas exploration and production and concrete, asphalt, and dimension stone cutting. [Pg.447]

Applications of geological reference samples to mineral prospecting and economic evaluation of ore potential is the only application with a history dating back before the issuance of G-i and W-i in 1951. It is an area in which data quality or lack thereof has serious economic impacts, hence the very early development of certified reference materials mentioned previously. An extensive study of the state of ore analysis was undertaken by the Institute of Geological Sciences (now the British Geological Survey). Nineteen ores and concentrates, of varied matrix, were distributed to 38 laboratories more than 1532 results were received (Lister and Galagher 1970). [Pg.225]

As a soil develops, OM decomposes to produce humus, which is black. Additionally, release of iron from minerals by weathering yields various reds and yellows. Both mechanisms yield soil coloring agents. Under oxidizing conditions, where soil is not saturated with water, the iron will be oxidized and thus in the ferric state [Fe(III)]. When the iron and OM are deposited on the surfaces of sand, silt, clay, and peds, they develop a coat that gives them a surface color. However, soil color is not only a surface characteristic but extends through the soil matrix. Under oxidizing conditions, soil has a reddish color. The chroma of this color depends to some extent on the amount of and the particular iron oxide present. [Pg.54]

In the virtual mineral space, the rock composition is projected onto the plane made by the vectors enstatite [0,1,0]T and diopside [0,0,1]T. Although these vectors are not orthogonal in the original oxide composition space, which can be verified by constructing the dot product of columns 2 and 3 in the matrix BT, the particular choice of the projection makes the vectors orthogonal in the transformed space. According to the projector theory developed above, we project the rock composition onto the column-space of the matrix A such that... [Pg.71]


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See also in sourсe #XX -- [ Pg.144 , Pg.145 ]




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Mineral matrices

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