Ba0.6Sr0.4TiO3 (BST) thin films were fabricated on Pt coated Si (100) substrates by sol-gel techniques with molar ratio of (Ba+Sr) to Ti changing from 0.76 to 1.33. The effect of (Ba+Sr)/Ti ratio deviating from the st...Ba0.6Sr0.4TiO3 (BST) thin films were fabricated on Pt coated Si (100) substrates by sol-gel techniques with molar ratio of (Ba+Sr) to Ti changing from 0.76 to 1.33. The effect of (Ba+Sr)/Ti ratio deviating from the stoichiometry on microstructure, grain growth, dielectric and tunable properties of BST thin films were investigated. TiO2 and (Ba,Sr)2TiO4 were found as a second phase at the ratios of 0.76 and 1.33, respectively. The variation of the ratio reveals more significant effect on the grain size in B-site rich samples than that in A-site rich samples. The dissipation factor decreases rapidly from 0.1 to 0.01 at 1 MHz with decreasing (Ba+Sr)/Ti ratio. The tunability increases with decreasing ratio from 1.33 to 1.05, and then decreases with decreasing ratio from 1.05 to 0.76. The film with (Ba+Sr)/Ti ratio of 1.05 has a maximum tunability of 32% and a dissipation factor of 0.03 at 1 MHz.展开更多
采用分步沉积法制备不同Sr/Ti摩尔比例的Sr/Ti O2催化剂,以X射线衍射(XRD)、扫描电镜(SEM)、透射电镜(TEM)、傅里叶变换红外(FT-IR)光谱、紫外-可见漫反射光谱(UV-Vis RDS)等手段对样品进行了表征,以可见光催化降解亚甲基蓝为模型反应...采用分步沉积法制备不同Sr/Ti摩尔比例的Sr/Ti O2催化剂,以X射线衍射(XRD)、扫描电镜(SEM)、透射电镜(TEM)、傅里叶变换红外(FT-IR)光谱、紫外-可见漫反射光谱(UV-Vis RDS)等手段对样品进行了表征,以可见光催化降解亚甲基蓝为模型反应考察样品光催化活性.结果表明,催化剂的活性和结构随Sr/Ti摩尔比(n(Sr)/n(Ti))的变化而变化,当n(Sr)/n(Ti)≤3/2时,催化剂呈由Ti O2和Sr Ti O3组成的球状结构;而当n(Sr)/n(Ti)在3/2与4/1之间时,催化剂呈片状结构,且随着n(Sr)/n(Ti)增大,催化剂组成由Sr Ti O3和Sr2Ti O4变为Sr2Ti O4和Sr(OH)2H2O;当n(Sr)/n(Ti)=9/1时,催化剂呈以Sr(OH)2H2O为主的针状结构.其中,n(Sr)/n(Ti)=4/1的样品表现出最高的光催化活性,一级反应速率为Sr Ti O3钙钛矿催化剂的5.0倍,商用P25的86.7倍.展开更多
Molar ratios of Mg/Ca and Sr/Ca were measured in two species of ostracod shells preserved in the upper core (15-55 m) of the Heqing Basin in Yunnan Province, southwest China. By correlating the molar ratios between Mg...Molar ratios of Mg/Ca and Sr/Ca were measured in two species of ostracod shells preserved in the upper core (15-55 m) of the Heqing Basin in Yunnan Province, southwest China. By correlating the molar ratios between Mg/Ca and Sr/Ca and comparing them with Sr concentrations of the sediments, we suggested that: (1) the molar Mg/Ca and Sr/Ca ratio variations in respective ostracod primo re- flected the changes in its ambient water composition and ecology; (2) the molar Sr/Ca ratios responded better to the salinity change linearly than Mg/Ca without aragonite precipitation in the system, and otherwise there was no linear relation between them; and (3) the molar Sr/Ca ratios were mainly con- trolled by salinity and authigenic carbonate precipitation, whereas the molar Mg/Ca ratios were related to both salinity and temperature. In fact, the rate of ostracod growth owing to temperature controls the fluctuation of Mg/Ca in shells. Here, more attentions should be paid to the constraint of authigenic mineral precipitation processes on the trace elements in ostracod shells and to the correlation between these trace elements in biogenic carbonates and compositions of the sediments in systems and in fu- ture in vitro experiments.展开更多
基金Project (50332030) supported by the National Natural Science Foundation of China
文摘Ba0.6Sr0.4TiO3 (BST) thin films were fabricated on Pt coated Si (100) substrates by sol-gel techniques with molar ratio of (Ba+Sr) to Ti changing from 0.76 to 1.33. The effect of (Ba+Sr)/Ti ratio deviating from the stoichiometry on microstructure, grain growth, dielectric and tunable properties of BST thin films were investigated. TiO2 and (Ba,Sr)2TiO4 were found as a second phase at the ratios of 0.76 and 1.33, respectively. The variation of the ratio reveals more significant effect on the grain size in B-site rich samples than that in A-site rich samples. The dissipation factor decreases rapidly from 0.1 to 0.01 at 1 MHz with decreasing (Ba+Sr)/Ti ratio. The tunability increases with decreasing ratio from 1.33 to 1.05, and then decreases with decreasing ratio from 1.05 to 0.76. The film with (Ba+Sr)/Ti ratio of 1.05 has a maximum tunability of 32% and a dissipation factor of 0.03 at 1 MHz.
文摘采用分步沉积法制备不同Sr/Ti摩尔比例的Sr/Ti O2催化剂,以X射线衍射(XRD)、扫描电镜(SEM)、透射电镜(TEM)、傅里叶变换红外(FT-IR)光谱、紫外-可见漫反射光谱(UV-Vis RDS)等手段对样品进行了表征,以可见光催化降解亚甲基蓝为模型反应考察样品光催化活性.结果表明,催化剂的活性和结构随Sr/Ti摩尔比(n(Sr)/n(Ti))的变化而变化,当n(Sr)/n(Ti)≤3/2时,催化剂呈由Ti O2和Sr Ti O3组成的球状结构;而当n(Sr)/n(Ti)在3/2与4/1之间时,催化剂呈片状结构,且随着n(Sr)/n(Ti)增大,催化剂组成由Sr Ti O3和Sr2Ti O4变为Sr2Ti O4和Sr(OH)2H2O;当n(Sr)/n(Ti)=9/1时,催化剂呈以Sr(OH)2H2O为主的针状结构.其中,n(Sr)/n(Ti)=4/1的样品表现出最高的光催化活性,一级反应速率为Sr Ti O3钙钛矿催化剂的5.0倍,商用P25的86.7倍.
基金the National Basic Research Program of China (Grant No. 2004CB720205)the National Natural Science Foundation of China (Grant Nos. 40599423 and 40373004)
文摘Molar ratios of Mg/Ca and Sr/Ca were measured in two species of ostracod shells preserved in the upper core (15-55 m) of the Heqing Basin in Yunnan Province, southwest China. By correlating the molar ratios between Mg/Ca and Sr/Ca and comparing them with Sr concentrations of the sediments, we suggested that: (1) the molar Mg/Ca and Sr/Ca ratio variations in respective ostracod primo re- flected the changes in its ambient water composition and ecology; (2) the molar Sr/Ca ratios responded better to the salinity change linearly than Mg/Ca without aragonite precipitation in the system, and otherwise there was no linear relation between them; and (3) the molar Sr/Ca ratios were mainly con- trolled by salinity and authigenic carbonate precipitation, whereas the molar Mg/Ca ratios were related to both salinity and temperature. In fact, the rate of ostracod growth owing to temperature controls the fluctuation of Mg/Ca in shells. Here, more attentions should be paid to the constraint of authigenic mineral precipitation processes on the trace elements in ostracod shells and to the correlation between these trace elements in biogenic carbonates and compositions of the sediments in systems and in fu- ture in vitro experiments.
