晶质铀矿是花岗岩中广泛产出的副矿物,其铀离子价态的变化及比例关系,对于岩浆氧逸度具有一定的指示意义。笔者利用硅酸盐熔浆中U^(6+)-U^(4+)的平衡关系,推导出花岗岩副矿物——晶质铀矿的氧逸度计热力学计算方程,以及氧逸度(f O2)、温...晶质铀矿是花岗岩中广泛产出的副矿物,其铀离子价态的变化及比例关系,对于岩浆氧逸度具有一定的指示意义。笔者利用硅酸盐熔浆中U^(6+)-U^(4+)的平衡关系,推导出花岗岩副矿物——晶质铀矿的氧逸度计热力学计算方程,以及氧逸度(f O2)、温度(T)和不同价态铀离子比值(U^(6+)/U^(4+))的对数关系。以赣南五里亭花岗岩体为例,借助X射线光电子能谱分析,获得U^(6+)与U^(4+)的比例关系(U^(6+)/U^(4+)=0.30~0.46);利用晶质铀矿氧逸度计热力学方程,计算出该岩体形成时的平均氧逸度(为FMQ+0.58)。在温度(T)与氧逸度(lg f O2)协变图中,该结果靠近矿物反应缓冲线(FMQ),显示岩浆为弱还原性。因此,晶质铀矿U^(6+)/U^(4+)氧逸度计算结果能够代表岩浆源区的氧逸度特征,可作为常规氧逸度计算方法的一种有效补充。展开更多
The effects of Mo on the microstructure and mechanical properties of Ti(C,N)-based cermets with low Ni have been studied systematically. Different contents of Mo (4-12 wt.%) were added into Tl(C,N)-based cermets...The effects of Mo on the microstructure and mechanical properties of Ti(C,N)-based cermets with low Ni have been studied systematically. Different contents of Mo (4-12 wt.%) were added into Tl(C,N)-based cermets. Specimens were fabricated by conventional powder metallurgy and vacuum sintered at temperatures of 1440, 1450, and 1460℃ individually. The microstructure and fracture morphology were investigated by scanning electron microscope, and the mechanical properties such as transverse strength and hardness were measured. The results show that the microstructure is uniform and the thickness of rim phase is moderate when the content of Mo is 8 wt.%; the mechanical properties of the specimens sintered at 1450℃ are better than those sintered at 1440 and 1460℃. The integrated properties of transverse strength and hardness are the best when the content of Mo is 8 wt.% and the sintering temperature is 1450℃.展开更多
This study analyzed the composition and uranium valence of pitchblendes sampled from the hydrothermal Guidong and Zhuguang uranium deposits of the middle Nanling metallogenic belt, Southern China using X-ray photoelec...This study analyzed the composition and uranium valence of pitchblendes sampled from the hydrothermal Guidong and Zhuguang uranium deposits of the middle Nanling metallogenic belt, Southern China using X-ray photoelectron spectroscopy(XPS).A revolutionary discovery is that the uranium not only exists in the forms of tetravalent and hexavalent uranium oxides, but also occurs in the form of native uranium.This is the first discovery of the existence of native uranium in nature.It greatly helps to reveal the origin of hydrothermal mineralization of uranium, and also has great significance for studying the thermal energy, formation and evolution of the earth.展开更多
Objective Oxygen fugacity is an important physicochemical parameter of magmas in addition to temperature,pressure and elemental concentrations,representing a major research topic in natural and experimental petrology....Objective Oxygen fugacity is an important physicochemical parameter of magmas in addition to temperature,pressure and elemental concentrations,representing a major research topic in natural and experimental petrology.Aside from oxygen probe work,where a direct measurement is made using an oxygen sensor to detect the oxygen content in the fluid and molten metal.展开更多
文摘晶质铀矿是花岗岩中广泛产出的副矿物,其铀离子价态的变化及比例关系,对于岩浆氧逸度具有一定的指示意义。笔者利用硅酸盐熔浆中U^(6+)-U^(4+)的平衡关系,推导出花岗岩副矿物——晶质铀矿的氧逸度计热力学计算方程,以及氧逸度(f O2)、温度(T)和不同价态铀离子比值(U^(6+)/U^(4+))的对数关系。以赣南五里亭花岗岩体为例,借助X射线光电子能谱分析,获得U^(6+)与U^(4+)的比例关系(U^(6+)/U^(4+)=0.30~0.46);利用晶质铀矿氧逸度计热力学方程,计算出该岩体形成时的平均氧逸度(为FMQ+0.58)。在温度(T)与氧逸度(lg f O2)协变图中,该结果靠近矿物反应缓冲线(FMQ),显示岩浆为弱还原性。因此,晶质铀矿U^(6+)/U^(4+)氧逸度计算结果能够代表岩浆源区的氧逸度特征,可作为常规氧逸度计算方法的一种有效补充。
基金This work was financially supported by the National Natural Science Foundation of China (No. 50074017) the Natural Science Foundation of Hubei Province, China (No. 2003ABA092).
文摘The effects of Mo on the microstructure and mechanical properties of Ti(C,N)-based cermets with low Ni have been studied systematically. Different contents of Mo (4-12 wt.%) were added into Tl(C,N)-based cermets. Specimens were fabricated by conventional powder metallurgy and vacuum sintered at temperatures of 1440, 1450, and 1460℃ individually. The microstructure and fracture morphology were investigated by scanning electron microscope, and the mechanical properties such as transverse strength and hardness were measured. The results show that the microstructure is uniform and the thickness of rim phase is moderate when the content of Mo is 8 wt.%; the mechanical properties of the specimens sintered at 1450℃ are better than those sintered at 1440 and 1460℃. The integrated properties of transverse strength and hardness are the best when the content of Mo is 8 wt.% and the sintering temperature is 1450℃.
文摘This study analyzed the composition and uranium valence of pitchblendes sampled from the hydrothermal Guidong and Zhuguang uranium deposits of the middle Nanling metallogenic belt, Southern China using X-ray photoelectron spectroscopy(XPS).A revolutionary discovery is that the uranium not only exists in the forms of tetravalent and hexavalent uranium oxides, but also occurs in the form of native uranium.This is the first discovery of the existence of native uranium in nature.It greatly helps to reveal the origin of hydrothermal mineralization of uranium, and also has great significance for studying the thermal energy, formation and evolution of the earth.
基金financially supported by the National Key R&D Program of China(Grant No.2017YFC0602600)Nuclear Power Development(No.HXS1403)Uranium Geology Research Program of China Nuclear Geology(No.201588)。
文摘Objective Oxygen fugacity is an important physicochemical parameter of magmas in addition to temperature,pressure and elemental concentrations,representing a major research topic in natural and experimental petrology.Aside from oxygen probe work,where a direct measurement is made using an oxygen sensor to detect the oxygen content in the fluid and molten metal.