La_(0.67)Sr_xMnO_(3-δ)的制备及表征

利用固态反应法制得名义组份为La0 .67SrxMnO3-δ(x=0 .33,0 .2 8,0 .2 3,0 .1 8和 0 .1 3)的多晶样品。X射线衍射表明当 0 .1 8≤x≤ 0 .33时样品是单相的钙钛矿型结构 ,这表明A位可以存在较多的空位。红外吸收光谱显示 ,随着A位空位增多 ,MnO6 八面体基团的伸缩振动模 (波数约为 60 0cm- 1 )的红外活性增强 ,同时电声子散射也随之增强。     

Al—11.7%Si合金锶变质效果的预报

针对Ｓｒ变质Ａｌ－１１．７％Ｓｉ共晶合金,通过实测获得冷却曲线,计算出结晶过程固相生长速率曲线。结果表明,固相生长速率最大值是表征Ａｌ－Ｓｉ合金变质效果的有效参数,通过计算机检测该参数可实现变质效果的准确预报。     

Coral Sr thermometer simplified from Sr/Ca thermometer

Cubic sub-samples obtained from a Porites coral slice collected from Xisha Islands, South China Sea, were weighed with precise micro-balance. The Sr and Ca concentrations were analyzed with isotope dilution thermal ionization mass spectrometry. Our results demonstrate that Ca concentrations in all samples are very uniform ( mean = 9.52mmol/g, la = 0.02mmol/g) ; Sr concentrations and Sr/Ca ratios are well correlated (correlation coefficient r = 0.9968) . It implies that the Sr thermometer can replace Sr/Ca thermometer and the determination of Ca can be omitted. This can save up to 50% time and cost, and more importantly, paleoclimate study using coral proxy can now be carried out in routine Sr isotope laboratories.     

Sr掺杂SiO2膜的制备及其脱盐性能研究

以正硅酸四乙酯(TEOS)为硅烷前驱体,以氯化锶(SrCl₂)为Sr源,采用溶胶-凝胶法制备了Sr掺杂的SiO₂膜.通过系列表征结果证实:在水解缩合反应过程中Sr被掺杂到SiO₂骨架中,形成了水热稳定的Si—O—Sr键,明显地改变了膜的表面形貌、微观结构和亲水性,从而提高了膜的脱盐性能和稳定性.在优化合成条件(n(Sr):n(TEOS)=0.075:1.000)下所制备的Sr/SiO₂膜的脱盐性能最佳.在60 ℃条件下,当以质量分数为3.5%的NaCl溶液为进料液时,该膜的水通量高达20.7 kg·m^-2·h^-1,盐截留率接近100.0%.此外,在35～60 ℃连续性温度循环测试中,该膜显示出了优异的水热稳定性.     

磁性光催化剂La_(0.7)Sr_(0.3)Mn_(0.9)Ti_(0.1)O_(3-δ)的制备其光催化性能研究

合成了一种具有磁性的Ti掺杂的La(0.7)Sr_(0.3)Mn_(0.9)Ti_(0.1)O_3光催化剂,即La(0.7)Sr_(0.3)Mn_(0.9)Ti_(0.1)O_(3-δ).并且利用了X射线衍射(XRD),紫外-可见固体漫反射(UV-vis DRS)、扫描电子显微镜(SEM)和磁性分析(VSM)等分析方法对其进行了表征.实验结果表明:La(0.7)Sr_(0.3)Mn_(0.9)Ti_(0.1)O_(3-δ)显示软铁磁性能,具有较高的磁化强度和较低的矫顽力和剩余磁化强度,其可利用外加磁场将其容易回收.在太阳光下,La(0.7)Sr_(0.3)Mn_(0.9)Ti_(0.1)O_(3-δ)在模拟罗丹明B(Rh B)废水中具有明显增强的光催化作用,催化效果好,且其重复使用5次后仍然表现出高的光催化活性.因此,制备的La(0.7)Sr_(0.3)Mn_(0.9)Ti_(0.1)O_(3-δ)是一种高效率的太阳光驱动光催化剂.     

Bi2（Sr,Ca）3Cu2Oy超导体的EXAFS研究

利用扩展Ｘ射线吸收精细结构（ＥＸＡＦＳ），研究了Ｂｉ２（Ｓｒ，Ｃａ）２Ｃｕ２Ｏｙ超导体中Ｃｕ原子与Ｂｉ原子的局域结构．结果表明：Ｃｕ原子第一配位层是五配位的氧原子，第二配位层是四配位的Ｃａ原子和一配位的Ｃｕ原子，但不含Ｓｒ原子的结构信息，这是Ｓｒ－Ｏ层与Ｃｕ－Ｏ层层间距较大所致；同时测定Ｂｉ原子第一配住层含有２．３个氧原子，用非公度调制结构模型解释了Ｂｉ原子的配位状况．     

上扬子石炭纪锶碳同位素和微量元素铝与海平面变化的关系

研究表明海相碳酸盐锶、碳同位素与海平面变化有一定的相关关系,其中碳同位素反应灵敏。此外,微量元素Al的变化也是海侵海退旋回的良好标志。     

Identifying paleoflood deposits archived in Zhongba Site, the Three Gorges reservoir region of the Yangtze River, China

Based on the principle that the present is the key to the past, detailed analyses, such as AMS ^14C dating, grain size, component and morphology of heavy minerals, micro-morphology of zircon, Rb/Sr, magnetic susceptibility and total organic carbon （TOC）, were conducted to identify paleoflood sediments archived in Zhongba Site. The results indicate that the plaeoflood sediments bear great similarities with modern flood sediments in the following aspects： （1） probability cumulative curves mainly show a pattern of 3-4 segments; （2） grain-size distribution of suspended matter ranges between 3 and 10（I）; （3） the sediments are well-sorted, most of which are suspended matter （〉50%）; （4） the same species, quantity and morphology of heavy minerals; （5） scanning electronic microscope images show that shapes of zircon are mainly oval and nearly spheral, rounded due to long-distance transport; （6） higher Rb/Sr values （0.55-0.66）than those of sediments from cultural layers （0.03-0.26）; （7） magnetic susceptibility values （133.73-433.05 10^-6m^3/kg） are lower than those of sediments from cultural layers （959.25-2442.44 10^-6 m^3/kg）; （8） TOC （0.14%- 0.33%） are lower than those of sediments from cultural layers （1.13%-2.95%）. Our results demonstrate that, except for the 1981 flood, there are at least six paleoflood events that occurred during the Qing Dynasty, the middle of Song Dynasty, the early Warring States （400BC-350BC）, the West Zhou Dynasty （920BC-900BC）, the Xia Dynasty （2070BC-1600BC）, and the late Neolithic Age （3000BC-2300BC）, respectively.     

Ba,Sr,Y,Zr在广东白菜中的转移系数

测量了Ｂａ，Ｓｒ，Ｙ，Ｚｒ四种核素从土壤到白菜的转移系数，研究了不同季节、不同元素浓度、不同施放方式以及不同生长期对转移系数的影响，并对元素从土壤到植物的转移系数的有关问题作了讨论