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Mode of Occurrence and Distribution of Bauxite Deposits in Andhra Pradesh and Feasibility of Aluminum Industry

机译:Andhra Pradesh铝土矿矿床的发生和分布方式及铝业可行性

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Bauxite forms four groups of capping in high hills of the Eastern Ghats which are form SW to NE the Gurtedu group, Chintapalli group, Paderu group and Araku (or Anantagiri) group in a belt 130 km long and 20 km wide. It occurs both on Khondalite and charnockite. The capping on the khondalite are more in number than on the latter. The in situ formation of bauxite by alteration on khondalite is indicated by the relict foliation of khondalite in bauxite, parallel to the foliation of the underlying khondalite, the pseudomorophs of the bauxite mineral gibbsite after garnet, silliminate and feldspar and the boulders with core of fresh rock and cover of bauxite. Boehmite differs from diaspore in that it has a lower specific gravity and occurs in the form of minute crystals (rhombic or bladed) which can only be seen with a microscope. Both minerals, if separated from impurities are usually colourless. Gibbsite (or hydragillite) is the only alumuna mineral found in trihydrated bauxites both in the crystalline and non-crystalline forms. It is colourless like the monohydrated minerals but has a lower specific gravity (2.35). Aluminium manufacture consists of two phases, i.e., manufacture of alumina from bauxite (Al_2O_3) and the alumina is to be refined and fabricated. The location of the smelters is being controlled by the location of the ore deposits and the power sites. The ore moves to power if they are wide apart as this industry is very power intensive and the cost of transportation determine the exact site. From the alumina by electrolysis process aluminium is manufactured by the application of cryolite, India is being used to import entirely from S.W.Greenland. At present synthetic Cryolite is being used as a substitute which is prepared from fluorspar. Alumina is a light metal and can stand long haulage. Hence the source of power has become the most dominant factor for the location of aluminium plants which subsequently fabricate the aluminium.
机译:铝土矿形成了四组封盖了东仓的高山丘,在腰带上形成了Gurtedu集团,Chintapalli集团,Paderu集团和Araku(或Anantagiri)组合在130公里长,宽20公里。它在Khondalite和Charnockite上发生。 Khondalite上的封盖比后者更多。通过改变铝土矿的原位形成铝土矿中青石叶,平行于石岩矿物矿山矿物矿床的薄荷矿床,石榴石矿物矿石叶片,含有新鲜的核心和新鲜核心铝土矿的岩石和覆盖物。 Boehmite与副血晶不同,因为它具有较低的比重,并且以微晶(菱形或叶片)的形式发生,其只能用显微镜观察。如果与杂质分离,矿物质都是无色的。 Gibbsite(或含芦珠)是在结晶和非结晶形式中的三丁烷铝土矿中发现的唯一alumuna矿物质。它是无色的像一氢矿物,但具有较低的比重(2.35)。铝制造包括两相,即来自铝土矿(Al_2O_3)的氧化铝的制造,并将其精制和制造氧化铝。冶炼厂的位置由矿石沉积物和电力部位的位置控制。如果这种行业很广泛,矿石移动到电源,因为这个行业非常电力密集,并且运输成本决定了确切的网站。通过电解过程从氧化铝通过电解过程制造通过应用德罗特,印度正在从S.W.Greenland进口。目前,合成冰晶石被用作由萤石制备的替代品。氧化铝是一款轻金属,可以长时间搭载。因此,功率来源已成为铝植物的位置的最主要因素,随后制造铝的植物的位置。

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