In this study,the properties of sinter mineral phases were investigated by X-ray diffraction,optical microscopy quantitative observation,electron probe microanalysis,and the nanoindentation technique. The mechanisms t...In this study,the properties of sinter mineral phases were investigated by X-ray diffraction,optical microscopy quantitative observation,electron probe microanalysis,and the nanoindentation technique. The mechanisms that form return fines are discussed with respect to the factors of microregion composition,sintering temperature,and the reactive behavior of pisolite. The study results indicate the following:( 1) Sinter mineral assemblage mainly comprises hematite,magnetite,calcium ferrite,and glass. In addition,the mineral assemblage of sinter products includes a great deal of calcium ferrite and melt-erosive magnetite,an abundance of secondary hematite,and a small amount of primary iron ore; whereas the mineral assemblage of return fines contains plentiful amounts of euhedral magnetite and secondary hematite,a large amount of relic pisolite with particle sizes less than1 mm,and relatively less calcium ferrite. In particular,some calcium ferrite was found to coexist with relic iron ore in a fiber-like microstructure.( 2) Dentritic calcium ferrite has less SiO_2 and Al_2O_3,higher basicity( w_(CaO)/w_(SiO_2))and a mole ratio of Fe_2O_3/CaO,whereas platy and blocky calcium ferrites have more SiO_2 and Al_2O_3,lower basicity and a mole ratio of Fe_2O_3/CaO.( 3) The hardness of hematite is the highest( around 18-22 GPa),those of calcium ferrite and magnetite are relatively lower,and that of glass is the lowest. In terms of the formation mechanism of return fines,because of their weak ability to resist external shocks,these sorts of mineral phases and microstructures-(1) euhedral magnetite and glass formed in microregions with low basicity;(2) SFCA-Ⅰand relic iron ore formed in regions with a relatively low sintering temperature; and(3) relic pisolite and its nearby reaction regions-are inclined to form return fines.展开更多
为充分利用广域测量系统WAMS(wide area measurement system)信息实现电力系统暂态稳定性快速在线识别,提出一种基于实测响应轨迹稳定边界的暂态不稳定识别方法.根据单机"位能脊"推导了单机-无穷大系统在相平面上的暂态稳定边...为充分利用广域测量系统WAMS(wide area measurement system)信息实现电力系统暂态稳定性快速在线识别,提出一种基于实测响应轨迹稳定边界的暂态不稳定识别方法.根据单机"位能脊"推导了单机-无穷大系统在相平面上的暂态稳定边界;证明单机无穷大系统任意比例剖分点处,由扰动能与电压相角构成的平面上的轨迹与相平面轨迹具有相似的几何特征,为间接利用发电机端口外网络测量信息识别电力系统暂态不稳定性提供了依据;证明了临界机组对的相轨迹上二阶导数等于零的点构成了系统的不返回边界,提出用临界机组对的相轨迹几何特征来识别系统暂态稳定性.为避免判据在线应用时受参数及不确定性干扰可能造成误判,对判据进行了实用性改进.利用PSASP 6.28 WEPRI 36节点仿真算例验证了所提判据的有效性.展开更多
为进行亚轨道飞行器返回段飞行仿真实验,详细划分返回段动力学虚拟样机层次结构,建立虚拟样机各子系统数学模型,并以此为基础在VPM(Virtual Prototype and Modeling)仿真平台上实现亚轨道飞行器返回段的动力学虚拟样机设计.使用现有的...为进行亚轨道飞行器返回段飞行仿真实验,详细划分返回段动力学虚拟样机层次结构,建立虚拟样机各子系统数学模型,并以此为基础在VPM(Virtual Prototype and Modeling)仿真平台上实现亚轨道飞行器返回段的动力学虚拟样机设计.使用现有的亚轨道飞行器总体方案在该虚拟样机系统上完成虚拟实验,仿真结果表明,该虚拟样机系统设计合理,可以为今后的亚轨道飞行器研制工作提供一定的技术支持.展开更多
基金the support of the National Key R& D Program of China ( No. 2017YFB0304300 & 2017YFB0304301)
文摘In this study,the properties of sinter mineral phases were investigated by X-ray diffraction,optical microscopy quantitative observation,electron probe microanalysis,and the nanoindentation technique. The mechanisms that form return fines are discussed with respect to the factors of microregion composition,sintering temperature,and the reactive behavior of pisolite. The study results indicate the following:( 1) Sinter mineral assemblage mainly comprises hematite,magnetite,calcium ferrite,and glass. In addition,the mineral assemblage of sinter products includes a great deal of calcium ferrite and melt-erosive magnetite,an abundance of secondary hematite,and a small amount of primary iron ore; whereas the mineral assemblage of return fines contains plentiful amounts of euhedral magnetite and secondary hematite,a large amount of relic pisolite with particle sizes less than1 mm,and relatively less calcium ferrite. In particular,some calcium ferrite was found to coexist with relic iron ore in a fiber-like microstructure.( 2) Dentritic calcium ferrite has less SiO_2 and Al_2O_3,higher basicity( w_(CaO)/w_(SiO_2))and a mole ratio of Fe_2O_3/CaO,whereas platy and blocky calcium ferrites have more SiO_2 and Al_2O_3,lower basicity and a mole ratio of Fe_2O_3/CaO.( 3) The hardness of hematite is the highest( around 18-22 GPa),those of calcium ferrite and magnetite are relatively lower,and that of glass is the lowest. In terms of the formation mechanism of return fines,because of their weak ability to resist external shocks,these sorts of mineral phases and microstructures-(1) euhedral magnetite and glass formed in microregions with low basicity;(2) SFCA-Ⅰand relic iron ore formed in regions with a relatively low sintering temperature; and(3) relic pisolite and its nearby reaction regions-are inclined to form return fines.
文摘为进行亚轨道飞行器返回段飞行仿真实验,详细划分返回段动力学虚拟样机层次结构,建立虚拟样机各子系统数学模型,并以此为基础在VPM(Virtual Prototype and Modeling)仿真平台上实现亚轨道飞行器返回段的动力学虚拟样机设计.使用现有的亚轨道飞行器总体方案在该虚拟样机系统上完成虚拟实验,仿真结果表明,该虚拟样机系统设计合理,可以为今后的亚轨道飞行器研制工作提供一定的技术支持.