电渣重熔过程电磁场和温度场数值模拟

建立了考虑电流集肤效应的三维电渣重熔电磁场和温度场数学模型,并采用电磁场和金属熔池形貌测量方法分别验证了数学模型的准确性,分析了电流频率和渣池厚度对电渣重熔过程电流密度、磁感应强度、电磁力、焦耳热、温度、熔池深度的影响规律.结果表明:随着电流频率增加,电极和钢锭表面电流集肤效应明显,渣池内部电流分布基本不变;电渣重熔系统内最大焦耳热位于平底电极与渣池接触角部,然而高温区位于渣池内部电极下方靠近渣金界面处.当渣池厚度从015m增加到021m,渣池中心轴线上最高温度从1826℃降低到1721℃,金属熔池深度从022m降低到016m.     

Origin of middle Miocene leucogranites and rhyolites on the Tibetan Plateau: Constraints on the timing of crustal thickening and uplift of its northern boundary

Leucogranites play a significant role in understanding crustal thickening, melting within continental collisional belts, and plateau uplift. Field investigations show that Miocene igneous rocks from the Hoh Xil Lake area mainly consist of two-mica leucogranites and rhyolites. We studied the Bukadaban two-mica leucogranites and the Kekao Lake, Malanshan and Hudongliang rhyolites by zircon U-Pb, muscovite and sanidine 40Ar/39Ar geochronology, and whole-rock geochemical and Sr-Nd isotopic analysis. Results yielded crystallization and cooling ages for the Bukadaban leucogranites of 9.7±0.2 and 6.88±0.19 Ma, respectively. Extrusive ages of the Kekao Lake and Malanshan rhyolites are 14.5±0.8 and 9.37±0.30 Ma, respectively. All rocks are enriched in SiO2 (70.99%-73.59%), Al2O3 (14.39%-15.25%) and K2O (3.78%-5.50%) but depleted in Fe2O3 (0.58%-1.56%), MgO (0.11%- 0.44%) and CaO (0.59%-1.19%). The rocks are strongly peraluminous (A/CNK=1.11?1.21) S-type granites characterized by negative Eu anomalies (δ Eu=0.18-0.39). In also considering their Sr-Nd isotopic compositions (87Sr/86Sri=0.7124 to 0.7143; δ Nd (9 Ma) =-5.5 to -7.1), we propose that these igneous rocks were generated through dehydration melting of muscovite in the thickened middle or lower crust of northern Tibet. Melting was probably triggered by localized E-W stretching decompression in the horse tails of Kunlun sinistral strike-slip faults. Reactivation of the Kunlun strike-slip faults, accompanied by emplacement of leucogranite and eruption of rhyolite in the Hoh Xil Lake area, indicates that large-scale crustal shortening and thickening in northern Tibet mainly occurred before 15 Ma. In addition, these findings suggest that the northern Tibetan Plateau attained its present elevation (~5000 m) at least 15 Ma ago.     

T型导电结晶器电渣重熔空心钢锭过程的数值模拟

基于新开发的电渣重熔空心钢锭技术,建立了渣池和空心钢锭的三维准稳态数学模型.利用商业软件ANSYS模拟并得到了非导电和导电结晶器工况下,电渣重熔空心钢锭过程的电磁场、流场与温度场.计算结果表明:导电结晶器工况下,渣池的电流密度和焦耳热最大值均出现在T型结晶器的导电段部分,导电结晶器附近的熔池流动速度较快,渣池的温度场更为均匀,金属熔池形状更为浅平.导电结晶器在交换电极时持续保持渣池和金属熔池温度,能够避免渣池温度迅速下降而导致靠近结晶器壁的钢水迅速凝固而出现渣沟,可大大提高钢锭的凝固质量和表面质量.     

Detachment within subducted continental crust and multi-slice successive exhumation of ultrahigh-pressure metamorphic rocks: Evidence from the Dabie-Sulu orogenic belt

Although tectonic models were presented for exhumation of ultrahigh-pressure （UHP） metamorphic rocks during the continental collision, there is increasing evidence for the decoupling between crustal slices at various depths within deeply subducted continental crust. This lends support to the multi-slice successive exhumation model of the UHP metamorphic rocks in the Dabie-Sulu orogen. The available evidence is summarized as follows： （1） the low-grade metamorphic slices, which have geotectonic affinity to the South China Block and part of them records the Triassic metamorphism, occur in the northern margin of the Dabie-Sulu UHP metamorphic zone, suggesting decoupling of the upper crust from the underlying basement during the initial stages of continental subduction; （2） the Dabie and Sulu HP to UHP metamorphic zones comprise several HP to UHP slices, which have an increased trend of metamorphic grade from south to north but a decreased trend of peak metamorphic ages correspondingly; and （3） the Chinese Continental Science Drilling （CCSD） project at Donghai in the Sulu orogen reveals that the UHP metamorphic zone is composed of several stacked slices, which display distinctive high and low radiogenic Pb from upper to lower parts in the profile, suggesting that these UHP crustal slices were derived from the subducted upper and middle crusts, respectively. Detachment surfaces within the deeply subducted crust may occur either along an ancient fault as a channel of fluid flow, which resulted in weakening of mechanic strength of the rocks adjacent to the fault due to fluid-rock interaction, or along the low-viscosity zones which resulted from variations of geotherms and lithospheric compositions at different depths. The multi-slice successive exhumation model is different from the traditional exhumation model of the UHP metamorphic rocks in that the latter assumes the detachment of the entire subducted continental crust from the underlying mantle lithosphere and its subsequent exhumation as a whol     

电渣重熔用CaO-Al_2O_3-SiO_2三元无氟渣系的研究

根据电渣重熔工艺要求和渣相平衡的特点,提出电渣重熔用渣化学组成的设计原则。据此原则,研究了CaO-Al_2O_3-SiO_2,三元系中8个共晶组成和二个同分化合物的性质,测定了其电导率和导热系数。根据其性质和电渣重熔实验,从中选出了两个适于电渣重熔用无氟渣系,其共晶组成(wt％):49.5％CaO-43.7％Al_2O_3-6.8％SiO_2和52.0％CaO-41.2％Al_2O_3-6.8％SiO_2。工业实验表明,其冶金性能与ANF-6渣相当,而电耗可降低30％,从根本上消除了氟化物对环境的污染。     

大渡河金川水电站区域地壳稳定性定量化评价

金川水电站地理位置处于不同构造单元的多组构造交汇复合地带,新生代以来构造活动、地震活动和水热活动均较强烈.为服务于大渡河金川水电工程规划建设的需要,作者对大渡河流域金川地区进行了地壳稳定性评价.依据地壳稳定性定量评价的原则和方法,将地壳稳定性划分为四个等级:稳定、次稳定、次不稳定和不稳定.综合各项研究资料确定定量评价指标,并采用模糊数学方法对地壳稳定性进行综合评价,结论表明,该地区适宜修建大型水电工程.     

大型板坯电渣重熔过程的脱氧热力学模型

以12Cr2Mo1R钢所用渣系为研究对象,选择Al作为脱氧剂,建立脱氧热力学模型.在不同的Al添加量条件下对12Cr2Mo1R钢熔渣-金属界面处各物质的平衡质量分数进行计算,分析各物质平衡质量分数随Al添加量的变化规律,为在给定Al添加量条件下进行终点成分预报,以及根据钢种成分要求选择Al添加量范围提供理论依据.结果表明,随Al添加量的增加,Si,Mn,Al,Al2O3的平衡质量分数呈上升趋势;SiO2,MnO,FeO的平衡质量分数呈下降趋势.若仅从Si,Mn,Al成分合格的角度考虑,Al的添加量占吨钢的百分比不能超过02%.     

感应重熔对高速轧机轴承热喷涂层微观组织性能的影响

为了改善高速轧机轴承热喷涂层的微观组织性能,采用感应重熔技术对GCr15轴承钢表面预制备的高能火焰喷涂Ni60A涂层进行感应重熔处理,并利用金相显微镜、扫描电镜、X射线衍射仪、显微硬度计对感应重熔前后涂层的孔隙率、微观组织、显微硬度等进行对比研究,探讨感应重熔对涂层以及界面微观组织、显微硬度的影响.结果表明,高能火焰喷...