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Minor elements

The summary of the bulk chemical compositions (major elements, minor elements, rare earth elements), Sr/ Sr (Farrell et al., 1978 Farrell and Holland, 1983), microscopic observation, and chemistry of spinel of unaltered basalt clarifies the tectonic setting of Kuroko deposits. Based on the geochemical data on the selected basalt samples which suffered very weak alteration, it can be pointed out that the basalt that erupted almost contemporaneously with the Kuroko mineralization was BABB (back-arc basin basalt) with geochemical features of which are intermediate between Island arc tholeiite and N-type MORE. This clearly supports the theory that Kuroko deposits formed at back-arc basin at middle Miocene age. [Pg.19]

Elements, minor or trace (agricultural chemicals) Exterminating products, for household and industrial use Fly sprays Fungicides... [Pg.474]

Regarding group V and VI elements, minor additions of P, Se and Te are effective to decrease the oxidation rate and the resultant scales are rich in A1203 [33,35], This was explained again by VCR [33, 35], There are optimal amounts for these elements. On the other hand, the influence of V, Nb and Ta belonging to group VA varies very wide-... [Pg.64]

Inorganic elements Organic elements Composition of impurities Surface composition Major elements Minor elements Trace elements Inorganic species Organic species Crystallinity... [Pg.130]

Tsao (1949). Pollen from Hippc.astrum sp. Sucrose, major mineral elements, minor mineral elements, yeast extract, casein,. succinic acid, sodium succinate, nn-malic acid, n-malic acid, fmnaric, citric, lactic, pyruvic, glutaric, and glutamic acids, peptone, and 3-indoleacotic acid. [Pg.364]

Tables I and II clearly show some of the major chemical differences between basalt and granite. A rock consisting chiefly of quartz and feldspar, granite shows high Si, Na and K values basalt, which is made up chiefly of Fe-Mg silicates and Ca-Na feldspar, is rich in Fe, Mg, and Ca. (Since the oceanic crast is largely basalt, its inclusion in the average analysis would result in largervalues for these latter three elements.) Minor elements in the two rocks tend to follow major elements of similar chemical properties thus Ba, Rb, and La are more abundant in granite, while V, Cr, and Ni predominate in basalt. Some elements, for example, Al, Ga, and Nb, show little difference from one rock to the other and are also the same in the cmstal average. Tables I and II clearly show some of the major chemical differences between basalt and granite. A rock consisting chiefly of quartz and feldspar, granite shows high Si, Na and K values basalt, which is made up chiefly of Fe-Mg silicates and Ca-Na feldspar, is rich in Fe, Mg, and Ca. (Since the oceanic crast is largely basalt, its inclusion in the average analysis would result in largervalues for these latter three elements.) Minor elements in the two rocks tend to follow major elements of similar chemical properties thus Ba, Rb, and La are more abundant in granite, while V, Cr, and Ni predominate in basalt. Some elements, for example, Al, Ga, and Nb, show little difference from one rock to the other and are also the same in the cmstal average.
If the speciation of trace elements is to be studied, measurements must be performed immediately after sampling. If for some elements minor changes in original speciation are acceptable, then the samples should be stored unacidified but frozen (see also the storage of As, Sb and Ge outlined in Chapter 12) to preserve as much as possible the original distribution of species. A few studies indicate, however, that some metal associations with humic substances might be stable even down to pH 2.3 (e.g., Helmers, 1994). [Pg.39]

Alloy conqiosition major elements, minor elements, impurities Passive film characteristics... [Pg.50]

Iron is a relatively abundant element in the universe. It is found in the sun and many types of stars in considerable quantity. Its nuclei are very stable. Iron is a principal component of a meteorite class known as siderites and is a minor constituent of the other two meteorite classes. The core of the earth — 2150 miles in radius — is thought to be largely composed of iron with about 10 percent occluded hydrogen. The metal is the fourth most abundant element, by weight that makes up the crust of the earth. [Pg.57]

Gr. molybdos, lead) Before Scheele recognized molybdenite as a distinct ore of a new element in 1778, it was confused with graphite and lead ore. The metal was prepared as an impure form in 1782 by Hjelm. Molybdenum does not occur native, but is obtained principally from molybdenite. Wulfenite, and Powellite are also minor commercial ores. [Pg.78]

Modeling the elements discussed in this section is fairly similar to modeling organic compounds. This is primarily because d and/orbitals play a minor role in their chemistry. When d and/ orbitals do affect the chemistry, their effect is well defined and for the most part understood. [Pg.285]

The second class of atomic manipulations, the perpendicular processes, involves transfer of an adsorbate atom or molecule from the STM tip to the surface or vice versa. The tip is moved toward the surface until the adsorption potential wells on the tip and the surface coalesce, with the result that the adsorbate, which was previously bound either to the tip or the surface, may now be considered to be bound to both. For successful transfer, one of the adsorbate bonds (either with the tip or with the surface, depending on the desired direction of transfer) must be broken. The fate of the adsorbate depends on the nature of its interaction with the tip and the surface, and the materials of the tip and surface. Directional adatom transfer is possible with the apphcation of suitable junction biases. Also, thermally-activated field evaporation of positive or negative ions over the Schottky barrier formed by lowering the potential energy outside a conductor (either the surface or the tip) by the apphcation of an electric field is possible. FIectromigration, the migration of minority elements (ie, impurities, defects) through the bulk soHd under the influence of current flow, is another process by which an atom may be moved between the surface and the tip of an STM. [Pg.204]

Organic compounds are a major constituent of the FPM at all sites. The major sources of OC are combustion and atmospheric reactions involving gaseous VOCs. As is the case with VOCs, there are hundreds of different OC compounds in the atmosphere. A minor but ubiquitous aerosol constituent is elemental carbon. EC is the nonorganic, black constituent of soot. Combustion and pyrolysis are the only processes that produce EC, and diesel engines and wood burning are the most significant sources. [Pg.374]

Analysis of Trace or Minor Components. Minor or trace components may have a significant impact on quaHty of fats and oils (94). Metals, for example, can cataly2e the oxidative degradation of unsaturated oils which results in off-flavors, odors, and polymeri2ation. A large number of techniques such as wet chemical analysis, atomic absorption, atomic emission, and polarography are available for analysis of metals. Heavy metals, iron, copper, nickel, and chromium are elements that have received the most attention. Phosphoms may also be detectable and is a measure of phosphoHpids and phosphoms-containing acids or salts. [Pg.134]

Other uses of oxyacetylene flames in mill operations are in building up or hardfacing metal, lancing (piercing a hole in a metal mass), and a variety of metal cleaning procedures. A minor but interesting fuel use of acetylene is in flame spectrophotometry where oxygen and nitrous oxide are used as oxidants in procedures for a wide variety of the elements. [Pg.394]

For specific applications, other minor impurities may be requited to be controlled to limiting maxima by agreement between the purchaser and the seller. Includes elements for which no specific limit is shown. [Pg.323]

Refining Processes. AH the reduction processes yield an impure metal containing some of the minor elements present in the concentrate, eg, cadmium in 2inc, or some elements introduced during the smelting process, eg, carbon in pig iron. These impurities must be removed from the cmde metal in order to meet specifications for use. Refining operations may be classified according to the kind of phases involved in the process, ie, separation of a vapor from a Hquid or soHd, separation of a soHd from a Hquid, or transfer between two Hquid phases. In addition, they may be characterized by whether or not they involve oxidation—reduction reactions. [Pg.169]

Minor amounts of tantalum, tin, lead, bismuth, and other elements also occur ia the ferroniobium. After cooling for 12—30 h, the metal is separated from the slag and cmshed and si2ed for shipment. The recovery of niobium ia the alurninothermic reaction is 87—93%. Larger reactions generally give better recoveries. [Pg.22]

Piezoresistive Sensors. The distinction between strain-gauge sensors and pie2oresistive (integrated-circuit) sensors is minor. Both function by measuring the strain on an elastic element as it is subjected to pressure. A pie2oresistive transducer is a variation of the strain gauge that uses bonded... [Pg.24]


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Coal minor elements

Conservative elements minor

Elements, essential minority

Human effects on total ocean minor element budgets

Influence of minor element addition

Major and minor elements

Mineral matter minor elements

Minor element additions, influence

Minor element distribution

Minor elements ocean

Minors of an element

Speciation minor elements

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