首页> 外文期刊>Transactions of the Institutions of Mining and Metallurgy, Section C. Mineral Processing and Extractive Metallurgy >Phase relations in the Fe-rich part of the system Fe_2O_3(-Fe_3O_4)-CaO-SiO_2 at 1240-1300 deg C and oxygen partial pressure of 5X10~(-3) atm: implications for iron ore sinter
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Phase relations in the Fe-rich part of the system Fe_2O_3(-Fe_3O_4)-CaO-SiO_2 at 1240-1300 deg C and oxygen partial pressure of 5X10~(-3) atm: implications for iron ore sinter

机译:在1240-1300℃和5X10〜(-3)atm的氧分压下,系统Fe_2O_3(-Fe_3O_4)-CaO-SiO_2的富铁部分中的相关系:对铁矿烧结矿的影响

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Equilibrium phase relations in the Fe-rich portion of the system Fe_2O_3(-Fe_3O_4)-CaO-SiO_2 (FCS) have been determined at 1240-1300 deg C and under an oxygen partial pressure of 5Xl0~(-3) atm, typical for iron ore sintering. Experiments were performed with the use of a rapid-quench technique and the chemical compositions of the melts and coexisting condensed phases were determined by combined optical microscopy and electron-probe microanalysis. At temperatures greater than ca 1250 deg C the major phase fields comprise Mt+Liq, C_2S+Liq, G_2S+G_2F+Liq and C_2F+Liq (where Mt represents magnetite, C valence CaO, F valence Fe_2O_3, S valence SiO_2 and Liq denotes a quench liquid phase) plus an extensive, continuous, Liq-only phase field that extends from Fe-rich to SiO_2-rich compositions. At less than about 1250 deg C the Liq-only melt region segregates into two distinct melt fields-one at high Fe contents and basicities greater than 1.8-2.0 and a second melt at low basicities (<1.8) and high SiO_2 contents. At all temperatures examined the reduced oxygen conditions significantly enlarged the field of silicate melt present relative to that of Ca-ferrite melt. Magnetite (predominantly) or hematite may be the stable Fe-oxide phase; however, the occurrence of any particular Fe-oxide phase is strongly linked to the overall basicity (CaO/SiO_2) of the charge.Experiments show that SFC_(ss) (silico-ferrite of calcia solid solution), which is the major ferrite bonding phase in low-Al sinter, cannot be produced as a single, unique, crystalline phase within the FCS system at 5X10~(-3) atm O_2. At this oxygen partial pressure the bulk composition lies within the partially reduced Fe_2O_3(-Fe_3O_4)-CaO-SiO_2 pseudo-ternary with the three-phase assemblage Mt+SFC_(ss)+Liq_(#alpha#) stabilized at low temperatures (1240 deg C). Combined with data for the FCS ternary in air the results indicate that to maximize the formation of SFC_(ss) bonding phase a low-temperature (<1260 deg C), semi-reduced heating environment followed by a relatively slow, oxidizing,
机译:已在1240-1300摄氏度和5X10〜(-3)atm的氧分压下确定了系统Fe_2O_3(-Fe_3O_4)-CaO-SiO_2(FCS)的富铁部分中的平衡相关系。铁矿石烧结。使用快速淬火技术进行了实验,并通过光学显微镜和电子探针显微分析相结合的方法测定了熔体和共存冷凝相的化学成分。在高于约1250摄氏度的温度下,主要相场包括Mt + Liq,C_2S + Liq,G_2S + G_2F + Liq和C_2F + Liq(其中Mt代表磁铁矿,C价CaO,F价Fe_2O_3,S价SiO_2和Liq表示骤冷液相),以及从富铁成分扩展到富SiO_2成分的广泛,连续的仅Liq相场。在小于约1250摄氏度时,仅Liq的熔体区域分离成两个不同的熔体场-一个处于高Fe含量和大于1.8-2.0的碱度,另一个处于低碱度(<1.8)和高SiO_2含量的熔体。在所检查的所有温度下,相对于钙铁氧体熔体,还原的氧气条件显着扩大了存在的硅酸盐熔体的场。磁铁矿(主要是磁铁矿)或赤铁矿可能是稳定的Fe-氧化物相。然而,任何特定的Fe-氧化物相的发生都与电荷的整体碱度(CaO / SiO_2)紧密相关。实验表明,SFC_(ss)(氧化钙固溶体的硅铁氧体)是主要的铁氧体键合低铝烧结矿中的相不能在FX系统中以5X10〜(-3)atm O_2的形式产生为唯一的结晶相。在此氧分压下,本体组成位于部分还原的Fe_2O_3(-Fe_3O_4)-CaO-SiO_2拟三元中,且三相组合Mt + SFC_(ss)+ Liq _(#alpha#)在低温下稳定(1240)摄氏度)。结合空气中FCS三元系的数据,结果表明,要最大程度地形成SFC_(ss)键合相,应采用低温(<1260摄氏度),半还原的加热环境,然后进行相对缓慢的氧化,

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