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On the formation of CoFe_2O_4 when drilling hematite with WC-Co drill bit inserts

机译:用WC-Co钻头刀片钻赤铁矿时CoFe_2O_4的形成

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It is commonly observed that WC-Co drill bit inserts wear more rapidly when drilling hematite ore than when drilling other ores of comparable hardness, e.g. ores that contain high percentages of SiO_2. This investigation was carried out to assess if chemical wear is part of the wear process of these inserts, i.e. if chemical reactions occur between hematite (alpha-Fe_2O_3) and WC-Co drill bits, during drilling. The drilling conditions were simulated by high energy-milling of WC-Co and hematite powders mixtures. The effect of milling time on the products formed was monitored. During a total milling time of 30 h, samples were collected at 5 h intervals. The powder samples were analysed by X-ray diffraction (XRD) and Mossbauer spectroscopy (MS) to detect the possible formation of new compounds. The XRD results showed that a new phase, which was identified as cobalt ferrite (CoFe_2O_4), was formed after 25 h of milling a Co/hematite powder mixture. This phase was confirmed by MS which showed a growing magnetic sextet that finally collapses with increasing milling time to a super-paramagnetic doublet [Tsjuji T. Inagaki H. Relation between Coercivity and Mossbauer Spectrum of Cobalt-Adsorbed gamma-Fe_2O_3. ICAME Conf Proc, 1996; 50: 255-8: Kundig W. Bommel H, Constabaris G, Lindquist RH. Some properties of supported small alpha-Fe_2O_3 particles determined with the Mossbauer effect. J Phys Rev 1966; 142:327.]. Results from both analytical techniques showed an increase in abundance of the new phase with increasing milling time. The formation of this phase may contribute to the wear of the WC-Co drill bits when drilling hematite ore.
机译:通常观察到,在钻赤铁矿矿石时,WC-Co钻头嵌件的磨损要比在钻探具有类似硬度的其他矿石时更快。含有高百分比SiO_2的矿石。进行该研究以评估化学磨损是否是这些刀片磨损过程的一部分,即在钻孔过程中赤铁矿(α-Fe_2O_3)与WC-Co钻头之间是否发生化学反应。通过高能研磨WC-Co和赤铁矿粉末混合物来模拟钻井条件。监测研磨时间对形成的产物的影响。在30小时的总研磨时间内,每隔5小时收集一次样品。通过X射线衍射(XRD)和Mossbauer光谱(MS)对粉末样品进行分析,以检测可能形成的新化合物。 XRD结果表明,在研磨Co /赤铁矿粉末混合物25小时后,形成了一个新相,即钴铁氧体(CoFe_2O_4)。 MS证实了这一相,该相显示出不断增长的磁六重体,最终随着碾磨时间的增加而塌陷,形成超顺磁性双峰[Tsjuji T. Inagaki H.钴吸附的γ-Fe_2O_3的矫顽力与莫斯鲍尔光谱之间的关系。 ICAME Con​​f Proc,1996年; 50:255-8:Kundig W. Bommel H,Constabaris G,Lindquist RH。由Mossbauer效应确定的支持的小α-Fe_2O_3微粒的某些性质。物理学报1966年; 142:327。]。两种分析技术的结果均表明,随着研磨时间的增加,新相的丰度增加。当钻探赤铁矿矿石时,该相的形成可能会导致WC-Co钻头的磨损。

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