The partition coefficients of W,Nb,and Ta between the P-rich peraluminous granitic melt and the coexisting aqueous fluid were determined at 800-850 °C and 0.5-1.5 kbar.The experimental results showed that the par...The partition coefficients of W,Nb,and Ta between the P-rich peraluminous granitic melt and the coexisting aqueous fluid were determined at 800-850 °C and 0.5-1.5 kbar.The experimental results showed that the partition coefficients D_w,D_(Nb) and D_(Ta)(D_i^(v/m) = C_i^V/C_i^m,where C_i^V and C_i^m denote the concentrations of an element,i,in the aqueous fluid and the melt,respectively) were less than 0.1.All partition coefficients were affected by pressure,but there was no evidence for the complexation of P2O5 with these elements in the granitic melt or aqueous fluid,except for with W in the fluid.The results showed that W,Nb,and Ta tended to partition into the granitic melt and,in the late period of crystallization of P-rich magma,they formed independent minerals.展开更多
Despite being pursued for a long time, hydrogen production via water splitting is still a huge challenge mainly due to a lack of durable and efficient catalysts. Molybdenum phosphide （MOP） is theoretically capable o...Despite being pursued for a long time, hydrogen production via water splitting is still a huge challenge mainly due to a lack of durable and efficient catalysts. Molybdenum phosphide （MOP） is theoretically capable of efficient hydrogen evolution reaction （HER） catalysis, however, there is still room for further improvement in its performance. Herein, we propose a design for MoP with a P-rich outermost atomic layer for enhancing HER via complementary theoretical and experimental validation. The correlation of computational results suggests that the P-terminated surface of MoP plays a crucial role in determining its high-efficiency catalytic properties. We fabricated a P-rich outermost atomic layer of MoP nanoparticles by using N-doped porous carbon （MoP@NPCNFs） to capture more P on the surface of MoP and limit the growth of nanoparticles. Further, the as-prepared material can be directly employed as a self-supported electrocatalyst, and it exhibits remarkable electrocatalytic activity for HER in acidic media; it also reveals excellent long-term durability for up to 5,000 cycles with negligible loss of catalytic activity.展开更多
江西宜春黄玉-锂云母花岗岩是著名的稀有金属花岗岩,P_2O_5含量较高(平均0.56%)。该花岗岩全岩 Be 含量一般超过100×10^(-6),最高可达720×10^(-6),属于铍矿化花岗岩。本文利用电子探针技术对宜春铍矿化花岗岩中的铍磷酸盐及...江西宜春黄玉-锂云母花岗岩是著名的稀有金属花岗岩,P_2O_5含量较高(平均0.56%)。该花岗岩全岩 Be 含量一般超过100×10^(-6),最高可达720×10^(-6),属于铍矿化花岗岩。本文利用电子探针技术对宜春铍矿化花岗岩中的铍磷酸盐及其共生矿物进行了系统研究。研究发现羟磷铍钙石是该花岗岩中的最重要铍矿物(BeO=15%～16%),偶尔亦可见磷钠铍石,它们主要呈晶间副矿物出现在岩体的中部。与铍矿物共生的矿物仍主要为磷酸盐矿物,如氟磷灰石、磷铝锂石、磷铝钠石,表明铍矿化作用与熔体中磷的聚集作用有显著关系。研究认为,宜春黄玉-锂云母花岗岩中铍以磷酸盐矿物形式结晶,而不是硅酸盐矿物,其主要原因可能为该花岗岩的结晶晚期磷的活度远远高于硅的活度,因此,P 优先作为成网离子与铍结合形成铍磷酸盐矿物。展开更多
采用原位磷注入合成法在高压单晶炉内合成富磷的磷化铟 (In P)熔体 ,并利用液封直拉法 (LEC)生长出了 1 0 0 mm In P掺硫单晶材料。对富磷单晶分别用快速扫描光荧光谱技术、腐蚀金相法和扫描电镜进行了研究。结果表明在富磷量足够大的...采用原位磷注入合成法在高压单晶炉内合成富磷的磷化铟 (In P)熔体 ,并利用液封直拉法 (LEC)生长出了 1 0 0 mm In P掺硫单晶材料。对富磷单晶分别用快速扫描光荧光谱技术、腐蚀金相法和扫描电镜进行了研究。结果表明在富磷量足够大的情况下 ,晶片上会出现孔洞 ,并对孔洞周围位错的形成原因及分布进行了分析。 1 0 0 mm In P单晶的平均位错密度也没有明显的增加 ,为今后生长更大尺寸的完整 In展开更多
基金supported by the Chinese National Natural Science Foundation(Project No.40273030)the Chinese Academy of Sciences through an innovation project (Project No.KZCX3-SW-124)
文摘The partition coefficients of W,Nb,and Ta between the P-rich peraluminous granitic melt and the coexisting aqueous fluid were determined at 800-850 °C and 0.5-1.5 kbar.The experimental results showed that the partition coefficients D_w,D_(Nb) and D_(Ta)(D_i^(v/m) = C_i^V/C_i^m,where C_i^V and C_i^m denote the concentrations of an element,i,in the aqueous fluid and the melt,respectively) were less than 0.1.All partition coefficients were affected by pressure,but there was no evidence for the complexation of P2O5 with these elements in the granitic melt or aqueous fluid,except for with W in the fluid.The results showed that W,Nb,and Ta tended to partition into the granitic melt and,in the late period of crystallization of P-rich magma,they formed independent minerals.
文摘Despite being pursued for a long time, hydrogen production via water splitting is still a huge challenge mainly due to a lack of durable and efficient catalysts. Molybdenum phosphide （MOP） is theoretically capable of efficient hydrogen evolution reaction （HER） catalysis, however, there is still room for further improvement in its performance. Herein, we propose a design for MoP with a P-rich outermost atomic layer for enhancing HER via complementary theoretical and experimental validation. The correlation of computational results suggests that the P-terminated surface of MoP plays a crucial role in determining its high-efficiency catalytic properties. We fabricated a P-rich outermost atomic layer of MoP nanoparticles by using N-doped porous carbon （MoP@NPCNFs） to capture more P on the surface of MoP and limit the growth of nanoparticles. Further, the as-prepared material can be directly employed as a self-supported electrocatalyst, and it exhibits remarkable electrocatalytic activity for HER in acidic media; it also reveals excellent long-term durability for up to 5,000 cycles with negligible loss of catalytic activity.
文摘江西宜春黄玉-锂云母花岗岩是著名的稀有金属花岗岩,P_2O_5含量较高(平均0.56%)。该花岗岩全岩 Be 含量一般超过100×10^(-6),最高可达720×10^(-6),属于铍矿化花岗岩。本文利用电子探针技术对宜春铍矿化花岗岩中的铍磷酸盐及其共生矿物进行了系统研究。研究发现羟磷铍钙石是该花岗岩中的最重要铍矿物(BeO=15%～16%),偶尔亦可见磷钠铍石,它们主要呈晶间副矿物出现在岩体的中部。与铍矿物共生的矿物仍主要为磷酸盐矿物,如氟磷灰石、磷铝锂石、磷铝钠石,表明铍矿化作用与熔体中磷的聚集作用有显著关系。研究认为,宜春黄玉-锂云母花岗岩中铍以磷酸盐矿物形式结晶,而不是硅酸盐矿物,其主要原因可能为该花岗岩的结晶晚期磷的活度远远高于硅的活度,因此,P 优先作为成网离子与铍结合形成铍磷酸盐矿物。
文摘采用原位磷注入合成法在高压单晶炉内合成富磷的磷化铟 (In P)熔体 ,并利用液封直拉法 (LEC)生长出了 1 0 0 mm In P掺硫单晶材料。对富磷单晶分别用快速扫描光荧光谱技术、腐蚀金相法和扫描电镜进行了研究。结果表明在富磷量足够大的情况下 ,晶片上会出现孔洞 ,并对孔洞周围位错的形成原因及分布进行了分析。 1 0 0 mm In P单晶的平均位错密度也没有明显的增加 ,为今后生长更大尺寸的完整 In
