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Phase-mineral and chemical composition of fractions separated from composite fly ashes at the Soma power station, Turkey

机译:在土耳其索马电站从复合粉煤灰分离出的馏分的相矿物学和化学组成

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The phase-mineral and chemical composition of six fractions recovered from two fly ashes (FAs) produced in the Soma power station (Turkey) was characterized to predict their possible environmental concerns and potential utilization directions. A combination of conventional separation procedures including sieving, hand picking, sink-float and magnetic separations, as well as leaching and evaporation, was used to isolate the following fractions: (1) char concentrates (CCs); (2) light fractions (<1 g cm~(-3)) (LFs); (3) water-soluble residues (WRs); (4) magnetic fractions (MFs); (5) nonmagnetic coarse-grained fractions (>63 mu m) (NCFs); and (6) nonmagnetic fine-grained fractions (<63 mu m) (NFFs). CCs (3.3-3.4 percent) are composed of char (61-68 percent) and some inorganic phases, and are highly enriched in U>S>Mn>Mo>Fe>Sb. LFs (0.4-0.8 percent) contain porous cenosphere, spongy, and vesicular char types (21-54 percent) impregnated by calcite, anhydrite, portlandite. and clay minerals. These fractions show high concentrations of Sb>Se>As. WRs (1.7-2.6 percent) consist of gypsum, portlandite, Ca oxalate, and calcite (92-98 percent), and are highly enriched in water-soluble Sb>Mo>S>Ca. The greatest amounts (1-37 percent) leached from FAs reveal Sb>Mo>S>Ca>Sr>Se>(B, Na)>Li. MFs (1.4-2.3 percent) are concentrated in magnetite, hematite, and Fe-spinel (31-39 percent), and are highly enriched in Mn>Fe>Co>Cu>Ni>Zn>(Mo, Yb)>(Lu, Tm, Y)>(Er, Ho, Mg)>Sb. NCFs (49-56 percent) include mostly coarse-grained glass, quartz, calcite, and mullite, and these are the poorest in trace elements fractions. NFFs (39-47 percent) contain dominantly fine-grained glass, calcite, quartz, char, and mullite, and are slightly enriched in some chalcophile elements. Possible environmental concerns are related mainly to the trace element mobility in WRs, LFs, and CCs, while the potential utilization directions are connected mostly with the composition of MFs, WRs, CCs, LFs, and NFFs.
机译:从在索马电站(土耳其)生产的两个粉煤灰(FA)中回收的六种馏分的矿物相和化学组成,可预测其可能的环境问题和潜在的利用方向。结合了传统的分离程序,包括筛分,手工采摘,沉池浮选和磁力分离以及浸出和蒸发,分离出以下馏分:(1)炭精矿(CC); (2)轻馏分(<1 g cm〜(-3))(LFs); (3)水溶性残留物(WRs); (4)磁性分数(MFs); (5)非磁性粗粒级分(> 63微米)(NCFs); (6)非磁性细粒级分(<63微米)(NFF)。 CC(3.3-3.4%)由炭(61-68%)和一些无机相组成,并且高度富集U> S> Mn> Mo> Fe> Sb。 LF(0.4-0.8%)包含多孔方孔,海绵状和囊状炭(21-54%),由方解石,硬石膏和硅酸盐浸渍。和黏土矿物。这些馏分显示出高浓度的Sb> Se> As。 WR(1.7-2.6%)由石膏,硅酸盐,钙钛矿,草酸钙和方解石(92-98%)组成,并且高度富含水溶性Sb> Mo> S> Ca。从FA中浸出的最大量(1-37%)显示为Sb> Mo> S> Ca> Sr> Se>(B,Na)> Li。 MF(1.4-2.3%)集中在磁铁矿,赤铁矿和Fe-尖晶石(31-39%)中,并高度富集Mn> Fe> Co> Cu> Ni> Zn>(Mo,Yb)>(Lu ,Tm,Y)>(Er,Ho,Mg)> Sb。 NCF(49-56%)主要包括粗粒玻璃,石英,方解石和莫来石,而这些是微量元素中最差的。 NFF(占39-47%)主要包含细颗粒的玻璃,方解石,石英,炭和莫来石,并略微富含一些亲硫族元素。可能的环境问题主要与WR,LF和CC中的痕量元素迁移率有关,而潜在的利用方向主要与MF,WR,CC,LF和NFF的组成有关。

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