排序方式: 共有35条查询结果,搜索用时 15 毫秒
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含碳铬矿团块高温还原特性研究 总被引:3,自引:0,他引:3
在1250~1450℃高温范围内研究内配碳铬矿团块中Cr2O3还原率和总还原率与内配碳比和渣相碱度的关系,并分析了含碳铬矿团块还原过程中金属相和渣相聚集和分离状态的变化。结果表明,Cr2O3还原率主要受还原温度和内配碳比的影响,当还原温度高于1400℃时,控制适宜的渣相组成和内配碳比,可以实现还原产物中金属相和渣相的完全分离。利用实验得到的条件,可望开发一种新的廉价碳素铬铁的生产方法。 相似文献
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探讨了粉状铬铁矿在流化床内的流化性质、还原过程和加煤条件。通过实验,得到流化过程中煤粉与铬铁矿粉的相对分布规律,给出使煤粉沿流化床高度方向较均匀分布的条件,测试了流化还原气组成、空塔流速、外配煤量、还原时间及还原温度等因素对铬铁矿粉化还原的影响规律。给出还原条件局部优化结果。 相似文献
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Xieite, a new mineral, occurs in the shock vein of the Suizhou meteorite. The mineral has an orthorhombic structure and its space group is Bbmm. The cell parameters are a = 9.462(6) A, b = 9.562(9) A, c = 2.916(1)A. The crystal-chemical formula is (Fe0.87Mg0.13Mn0.01)1.01(Cr1.62AI0.25Ti0.08V0.02)1.97O4, or simply formula FeCr2O4. Stronger X-ray diffraction lines are [d (A), I/Io]: (2.675, 100), (2.389, 20), (2.089, 10), (1.953, 90), (1.566, 60), (1.439, 15), (1.425, 15), (1.337, 40). Xieite is a high pressure polymorph of FeCr2O4 and formed by solid-state transformation of chromite under shock-induced high pressure and temperature, in association with other high-pressure minerals including ringwoodite, majorite, lingunite and tuite. The P-Tcondition for the formation of xieite is estimated to be 18--23 GPa and 1800--1950℃, respectively. Xieite has recently been approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA 2007-056). The mineral name, xieite, is named after Xiande Xie. 相似文献
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亚铬酸盐滴定法测定高铁酸钾 总被引:11,自引:0,他引:11
以亚铬酸盐氧化还原反应为基础建立了高铁酸钾的滴定分析方法,对滴定分析条件进行了优化研究,结果表明,用碱度为11~12M的亚铬酸盐溶液测定高铁时,测定结果稳定,与用亚砷盐酸法测的结果一致,方法简便、快速、准确,与亚砷酸盐法相比,该法特别适合于低浓度的高铁酸钾溶液的定量分析。 相似文献
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通过浇注合金钢铸件试块并借助电子显微镜观察和X-Ray分析,研究了钢液对铬铁矿高温致密涂料层的影响.结果表明:涂层的致密度与钢液作用的激烈程度成正比关系;从钢液中吸收大量的Fe是形成致密涂层的主要原因;涂层中Fe的主要物相为铁橄榄石及赤铁矿. 相似文献
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采用碱熔法分解铬铁矿,并用硫酸亚铁铵滴定法测定三氧化二铬质量分数,对比了不同熔剂对测定结果的影响.结果表明,以质量比为2∶1的过氧化钠和氢氧化钠作为熔剂熔融分解铬铁矿,样品分解完全,测定结果准确可靠. 相似文献
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用穆斯堡尔谱学研究了河南西峡铬铁矿3个矿物样品。两个铬铁矿的谱被拟合成3套双峰,一个谱被拟合成4套双峰。然后用次近邻效应和B位上阳离子二项式分布计算结果解释了出现3套或4套双峰的原因。 相似文献
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对铬铁精矿球团烧结新工艺以及球团烧结矿冶金性能和固结机理进行研究。研究结果表明:铬铁精矿粒度粗,成球差,必须经过球磨机细磨,使其比表面积达到1 700 cm2/g,才具有良好的成球性;在膨润土配比为1.5%(质量分数)、造球水分为9.0%(质量分数)、造球时间为12 min的条件下,生球落下强度5次/(0.5 m),抗压强度11 N/个,爆裂温度480℃。优化的球团烧结工艺参数为:焦粉用量7%(质量分数)(内配比例30%),烧结混合料水分为9.5%,料层高度为650 mm,干燥温度为300~350℃,干燥负压为4 kPa,干燥时间为3 min,点火温度为1 100℃,点火负压为5 kPa,点火时间为1.5 min,烧结负压为8 kPa,取得了良好的指标:烧结矿产量为3.01 t/(m2.h),转鼓强度为89.33%,固体燃耗为79.19 kg/t。铬铁精矿球团烧结矿在900℃时很难还原,但还原膨胀率只有5%~6%,还原粉化率RDI+3.15大于94%,还原过程将具有较好的强度;在烧结料层的中上部,烧结矿的宏观结构以单个散状球团为主;在烧结料层下部以葡萄状烧结矿为主。铬铁精矿球团烧结矿矿物组成以铁铬尖晶石和硅酸盐矿物为主,单颗粒的球状烧结矿以固相固结为主,葡萄状烧结矿中液相量占30%左右,由固相固结和液相黏结共同维持烧结矿强度。 相似文献
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The Cr:Fe ratio (chromium-to-iron mass ratio) of chromite affects the production of chrome-based ferroalloys. Although the literature contains numerous reports related to the magnetic separation of different minerals, limited work concerning the application of magnetic separation to fine chromite from the Sukinda region of India to enhance its Cr:Fe ratio has been reported. In the present investigation, magnetic separation and mineralogical characterization studies of chromite fines were conducted to enhance the Cr:Fe ratio. Characterization studies included particle size and chemical analyses, X-ray diffraction analysis, automated mineral analysis, sink-and-float studies, and magnetic susceptibility measurements, whereas magnetic separation was investigated using a rare earth drum magnetic separator, a rare earth roll magnetic separator, an induced roll magnetic separator, and a wet high-intensity magnetic separator. The fine chromite was observed to be upgraded to a Cr:Fe ratio of 2.2 with a yield of 55.7% through the use of an induced roll magnetic separator and a feed material with a Cr:Fe ratio of 1.6. 相似文献