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Mining ores

The INTROS Flaw Detector is certified by the Russian State Standard Service (GOSSTANDART) as well as approved by the Russian State Mining and Technology Safety Inspection (GOSGORTECHNADZOR). It is used to inspect mining hoist and crane ropes. Fig. 5 illustrates the INTROS use at the mining hoist of an Ural ore mine. The previous model of the instrument, MDK-11 was used to inspect ropes of the air rope ways in Caucasus and Kazakhstan in 1996. Fig. 6 shows the INTROS MDK-11 inspection of 45 mm skyline rope in Almaty, Kazakhstan. [Pg.337]

Rhenium does not occur free in nature or as a compound in a distinct mineral species. It is, however, widely spread throughout the earth s crust to the extent of about 0.001 ppm. Commercial rhenium in the U.S. today is obtained from molybdenum roaster-flue dusts obtained from copper-sulfide ores mined in the vicinity of Miami, Arizona, and elsewhere in Arizona and Utah. [Pg.134]

W. Gericke, "The Establishment of a 500,000 tpa Sinter Plant at Samancor s Mamatwan Manganese Ore Mine," Proceedings of the 5th International Ferroalloys Congress (fnfacon). New Orleans, La., Apr. 1989. [Pg.499]

Fig. 1. Average yield of copper ores mined in the United States. Fig. 1. Average yield of copper ores mined in the United States.
The western phosphates are sedimentary deposits in adjoining areas of Wyoming, Idaho, and Utah derived from a former inland sea. They consist of layers of limestone, phosphate, and chert, now budded and faulted so they are rarely horizontal. The phosphate ore is strip-mined using large earth-moving equipment such as shovels, scrappers, dump tmcks, and bulldozers to mine the overburden and phosphate ore. Mining ratios of overburden to metric ton of recovered ore are from 1—3 m /1 (2—4 yd /short ton). The typical mining practice is to remove ore and overburden from a pit in discrete layers (Lifts) of 10—20 m in depth. Overburden from the pit is back-hauled to a previously mined pit. Extensive land reclamation practices are later carried out to return the mine areas to natural states. [Pg.349]

PGM Concentration. The ore mined from the Merensky Reef in South Africa has a maximum PGM content of 8.1 g/1, of which 50—60% is platinum, and 20—25% palladium. The PGMs are in the form of a ferroplatinum alloy, or as their sulfides, arsenides, or teUurides. The aim of the concentration process is to separate from the ore a cmde metal concentrate, having a PGM content of 60%. The majority of other metals, such as nickel and copper, are separated out at this stage for further refining. [Pg.166]

Bastnasite has been identified in various locations on several continents. The largest recognized deposit occurs mixed with monazite and iron ores in a complex mineralization at Baiyunebo in Inner MongoHa, China. The mineral is obtained as a by-product of the iron ore mining. The other commercially viable bastnasite source is the Mountain Pass, California deposit where the average Ln oxide content of the ore is ca 9%. This U.S. deposit is the only resource in the world that is minded solely for its content of cerium and other lanthanides. [Pg.365]

For each unit process, a reference flow may be defined, and the inputs and outputs to the unit process calculated in relation to the reference flow. For instance, the reference flow for mining of iron ore is the mass of iron ore mined per year, and the emissions to the air may be expressed as kg dust per metric ton of ore. [Pg.1361]

Percoronit Percoronite). A blasting expl which replaced Coronit in stone quarries and ore mines K perchlorate 65, NG 5, aromatic nitrocompds 25, and vegetable meal 5% (See also Perkoronit) Refs l)Bebie (1943), 116 2)PATR2510... [Pg.650]

Perkoronit. Ger perchlorate expls of varying compn, extensively used during and after WWI for blasting purposes (especially in ore mines and quarries). [Pg.654]

Sasaki, A. and Kajiwara, Y. (1971) Evidence of isotopic exchange between seawater sulfate and some syngenetic sulfide ores. Mining Geology Special Issue, 4, 289-294. [Pg.284]

With the passage of time, the average grade of the ores mined for metal production has become progressively leaner, and this trend will continue in the future because metallic... [Pg.745]

The U.S. is the world s third largest primary lead producer, with one-seventh of all production reserves. Over 80% of the lead ore mined domestically comes from Missouri. The majority of lead ore mined in the U.S. is smelted in conventional blast furnaces and refined using pyrometallurgical methods. [Pg.86]

The release of lead to air is now less than the release of lead to land. Most of the lead in inner city soils comes from old houses painted with paint containing lead and previous automotive exhaust emitted when gasoline contained lead. Landfills may contain waste from lead ore mining, ammunition manufacturing, or other industrial activities such as battery production. [Pg.19]

In addition, these precious and special metals have very low concentrations in ores mining, smelting, and refining these metals therefore have a particularly large environmental impact. Recovering these metals from defunct electronic equipment would result in a fraction of the effect on the environment [20]. [Pg.274]

The main factors leading to spontaneous explosions of blasting explosives in sulfide ore mines are identified as presence of ammonium nitrate, presence of pyrites and their weathering products, as well as the pH and temperature. At pH below 2, the critical temperature for spontaneous explosion may be lower than 40°... [Pg.1683]

Jorgensen, H. S., Lung cancer among underground workers in the iron ore mine of Kiruna based on thirty years of observation, Annals. Acad. Med., Singapore, IS (2, Supplement) 371-377, April 1984. [Pg.460]

More than 90% of the world s nickel is obtained from pentlandite ((FeNi)9S8), a nickel-sulfitic mineral, mined underground in Canada and the former Soviet Union (Sevin 1980 IARC 1976 WHO 1991). One of the largest sulfitic nickel deposits is in Sudbury, Ontario (USPHS 1993). Nickeliferous sulfide deposits are also found in Manitoba, South Africa, the former Soviet Union, Finland, western Australia, and Minnesota (Norseth and Piscator 1979 USPHS 1993). Most of the rest of the nickel obtained is from nickel minerals such as laterite, a nickel oxide ore mined by open pit techniques in Australia, Cuba, Indonesia, New Caledonia, and the former Soviet Union (Sevin 1980). Lateritic ores are less well defined than sulfitic ores, although the nickel content (1 to 3%) of both ores is similar (USPHS 1993). Important deposits of laterite are located in New Caledonia, Indonesia, Guatemala, the Dominican Republic, the Philippines, Brazil, and especially Cuba, which holds 35% of the known reserves (USPHS 1993). Nickel-rich nodules are found on the ocean floor, and nickel is also present in fossil fuels (Sevin 1980). [Pg.445]

Natural sources of airborne nickel include soil dust, sea salt, volcanoes, forest fires, and vegetation exudates and account for about 16% of the atmospheric nickel burden (Kasprzak 1987 WHO 1991 Chau and Kulikovsky-Cordeiro 1995). Human sources of atmospheric nickel — which account for about 84% of all atmospheric nickel — include emissions from nickel ore mining, smelting, and refining activities combustion of fossil fuels for heating, power, and motor vehicles ... [Pg.445]

The San Rafael tin mine is one of the richest ore mine in the world, with a head grade of about 5% Sn. The mine actually started in the 1960s as a copper operation, and later tin was discovered and the operation started as a tin operation. The ore is coarse grained, and a portion of the tin was recovered at a relatively coarse-grind size (i.e. 8 mm size). The main gangue minerals found in this ore were silicates, pyrite, pyrrhotite, tourmaline and minor amounts of copper and silver. [Pg.106]

Mamatwan manganese ore mine, 75 545 Mammalian cell culture, 5 346... [Pg.547]

In 1751 Baron Axel Fredrick Cronstedt (1722-1765) used some of the techniques he had learned from his teacher, Georg Brandt (1694—1768), to separate a new metal from copper-hke ore mined in Sweden. He expected to obtain pure copper instead, he ended up with a silver-white metal that did not have the chemical and physical properties of copper. He named this newly identified metal nickel, shortened from the German name the early miners had given the ore kupfernickel. ... [Pg.109]

The Ras-Draa ore mine is located between Tozeur and Nefta, in southern Tunisia. This deposit is a natural continuity of the great Gafsa-Metlaoui phosphatic basin (Fig. 1). [Pg.111]

Iron ore production for the iron and steel industry accounts for more than 99% of the total iron mined. At present, the largest iron ore mine in the world is Mount Whaleback in the Pilbara district of Western Australia. Most of the ore there is in the form of banded iron formations (BIF) and consists of hematite and goethite. [Pg.409]


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See also in sourсe #XX -- [ Pg.564 , Pg.570 ]

See also in sourсe #XX -- [ Pg.453 ]




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