Carbon isotope anomaly in marbles associated with eclogites from the Dabie Mountains

This is a report of carbon isotope anomaly in marbles associated with the UHP eclogites from the Dabie Mountains. The results place constraints on the degree of crust-mantle interaction during the UHP metamorphism.     

Preliminary study on climatic signals of stable isotopes from Holocene speleothems under monsoon condition

Within the East Asian monsoon zone the change in oxygen isotope of Holocene stalagmite is mainly related to monsoon rain rather than to temperature. And carbon isotope can be taken as a comprehensive signal which contains the natural information and the information of anthropogenic activity. Isotopic analysis is also compared with the annual layer records.     

SrxBa1—xTiO3陶瓷的频域介电谱

用固相反应法制备ＳｒｘＢａ１－ｘＴｉＯ３系列陶瓷．当ｘ＝０．３０时呈现显著的驰豫相变特征．在５Ｈｚ至１ＭＨｚ范围,相对介电常数的实部ε′随频率ｆ的降低而增大．１／ε′与ｌｇｆ的关系曲线呈现折曲的２段直线．高频相对介电常数的实部ε′ｈ随ｘ的增加而增大是与顺电相的增加而对应．测量点（ε′,ε″）随频率ｆ的变化分布在复平面的一条直线上．     

A carbon- and oxygen-isotope record of recent environ- mental change from Qinghai Lake, NE Tibetan Plateau

An understanding of natural climatic variability is essential for evaluating anthropogenic impacts on recent and future climate[1—3]. Due to the lack of lengthy instrumental records, such an understanding must be gained from natural archives of climate change. Palaeolimnological indicators of past lake levels may provide a sensitive record of changes in effective precipitation in closed basins. This approach is particularly relevant on the Tibetan Plateau, where instrumental records are very…     

新显色剂二溴对甲基偶氮羧磺的合成及其与锶显色反应的研究

报道了一种新型二溴对甲基偶氮羧磺染料的合成方法,及其与锶在0 48mol/L盐酸介质中形成的稳定的蓝色络合物.其最大吸收波长位于620nm处,表观摩尔吸光系数为8 88×104L·mol-1·cm-1,锶量在0～0 25μg/25mL范围内符合比尔定律.该试剂与其他测定锶的试剂相比,具有灵敏度高、选择性好等优点.     

SAG法Ba_（1－x）Sr_xTiO_3的介电性质

ＸＲＤ法分析和介电测量结果表明，ＳＡＧ法Ｂａ１－ｘＳｒｘＴｉＯ３（ｘ＝０、０．３、０．５和０．７）微粉和陶瓷的室温结构为立方相．其居里温度明显低于相应Ｂａ１－ｘＳｒｘＴｉＯ３晶体或常规工艺陶瓷的值，但居里温度仍随着Ｓｒ２＋含量的增加而线性下降．晶粒含杂质Ｆｅ３＋以及表面富钡可能使其晶格立方化，从而使居里温度下降以及三方－正交和正交－四方铁电相变消失．     

汉诺坝非橄榄岩类包体的化学和同位素特征

汉诺坝非橄榄岩包体主要是指辉石岩、辉长岩和麻粒岩，其主要元素、微量元素有较大和系统的变化，Ｎｄ、Ｓｒ、Ｐｂ同位素从非常亏损的ＤＭＭ源特征变至具ＥＭＩ和ＥＭＩ源趋势的富化特征．它们与寄主玄武岩及共生的橄榄岩包体无直接成因联系，有不同的形成时代并在不同的空间位置居留     

纳米粉Ba1-xSrxTiO3的合成

根据液相反应胶粒析出机理及实验原理，制备了Ba1-xSrxTiO3的前驱体(Ti(OH)4、SrCO3,BaCO3),然后经过焙烧，在较低温度(450℃)时是碳酸钡锶和二氧化钛分子状态的混合纳米晶，继续焙烧(900℃)成为发育完整的Ba1-xSrxTiO3纳米粉体，经TEM和XRD表征，平均粒径为100m，粒径分布较窄，分散性良好，XRD表明此纳米粉体为钛酸钡锶Ba1-xSrxTiO3。