
Review of Chromite Ore Processing Residue (COPR) Current Environmental Engineering, 2014, Vol. 1, No. 2 83 From 1931 - 1972, the Diamond Shamrock Company in Painesville Ohio produced COPR as a ...
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Chromite ore processing residue (COPR) is a waste byproduct of chromate production that contains high levels of hexavalent chromium (Cr [VI]). Although the high temperature chromite process was banned in several countries, its legacy still exists at numerous contaminated sites. For instance, New Jersey alone has over 2 million tons of waste COPR.
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Disposal of Chromite Ore Processing Residue (COPR) is a major concern from an environmental point of view because it consists mainly of Cr(VI) in addition to Cr(III). Cr(VI) is more soluble and mobile when compared to Cr(III). The study primarily concentrated on treatment of COPR using solidification and stabilization (S/S) process.
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When the electricity flows through the circuit they make, the electrolyte splits up and some of the metal atoms it contains are deposited in a thin layer on top of one of the electrodes—it becomes electroplated. All kinds of metals can be plated in this way, including gold, silver, tin, zinc, copper, cadmium, chromium, nickel, platinum, and.
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Safe management and disposal of chromite ore processing residue (COPR) is an unsolved global problem. In spite of several global research efforts, the problemof safe management of COPR and redemption of dump sites has remained unsolved. ... The present paper reviews and analyzes the current status with various remediation methods available ...
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Introduction. Chromite ore processing residue (COPR) is a waste produced in high lime chromium salt production process using chromite ((Mg, Fe)(Cr, Al) 2 O 4).It contains up to 2% of mobile, toxic and carcinogenic Cr(VI) .It is reported that 2-3 tons COPR is generated in the production of 1 ton sodium dichromate by the high lime process .The high lime process has been superseded by the non ...
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While Cr-(VI) treatment remains a challenge, the intentional exhaustion of the heave potential of COPR by transforming all Al sources to ettringite emerges as a possible solution to delayed ettringsite formation, which would hamper site redevelopment. A pilot-scale treatment study was implemented at a deposition site of chromite ore processing residue (COPR) in New Jersey. Ferrous sulfate ...
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The residue has been produced in large quantities worldwide at chromate salt production centers in urban industrial areas in Europe and the US such as Glasgow, U.K., and Jersey City, New Jersey, USA, as well as at chromite ore processing plants operating in Japan, India, Pakistan and the former Soviet Union [1-4]. Due to its
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CIESC Journal ›› 2018, Vol. 69 ›› Issue (6): 2730-2736. doi: 10.11949/j.issn.0438-1157.20171354. Previous Articles Next Articles Characteristics of chromium removing using different ex-situ remediations in soil seriously contaminated by chromite ore processing residue . ZHU Wenhui 1, LI Zhitao 1, WANG Xiahui 1, WANG Xingrun 2
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Chromite ore processing residue (COPR) is a waste byproduct of chromate production that contains high levels of hexavalent chromium (Cr[VI]). Although the high temperature chromite process was banned in several countries, its legacy still exists at numerous contaminated sites. For instance, New Jersey alone has over 2 million tons of waste COPR.
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Chromite ore processing residue (COPR) is a waste byproduct of chromate production that contains high levels of hexavalent chromium (Cr[VI]). Although the high temperature chromite process was banned in several countries, its legacy still exists at numerous contaminated sites. For instance, New Jersey alone has over 2 million tons of waste COPR. Legacy sites are confounded by the fact that a ...
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Dichromic acid prepared from the leachate of chromite ore processing residue was employed as an oxidant [31], while other reagents were purchased from Sinopharm Chemical Reagent Co., Ltd., Shanghai, China. Table 1. Chemical composition (dry wt.%) of chromites. Chromite FeO Fe2O3 Cr2O3 Al2O3 MgO SiO2 Other
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chromite (krōˈmīt), dark brown to black mineral.It is an iron-chromium oxide, FeCr 2 O 4, with traces of magnesium and aluminum.Its crystals are octahedral, but rare; it usually occurs as irregular, granular masses in association with igneous rocks, including ophiolites, which are segments of oceanic crust exposed on land by tectonic processes usually associated with plate convergence (see ...
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