微波铁氧体双模新器件的推广及应用

本文叙述了微波铁氧体双模新器件的原理和性能，这些新器件在现代雷达技术和通信技术等微波高频设备中具有广泛的使用前途。     

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．     

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．     

M型锶钙铁氧体的研究

Ｃａ离子在Ｍ型锶钙六角铁氧体中的最大固溶量Ｘｍ≈０．５。在固溶范围内，Ｃａ离子代换Ｓｒ离子对材料的本征磁性能如居里温度θｆ，比饱和磁化强度δｓ，以及磁晶各向异性场ＨＡ没有明显的影响，这有可能在保证材料性能不下降的前提下，在Ｍ型锶钙六角铁氧体中加入廉价的钙来降低材料成本。     

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。     

(LiFe)xZn1-2xFe2O4铁氧体的吸波性能研究

采用固相烧结工艺,按不同配方分别制备了(LiFe)xZn1-2xFe2O4(x=0.1、0.2、0.3、0.4、0.45、0.5),用Agilent8510c矢量网络分析仪测试,在0.5～13GHz频段内材料的吸波性能.实验发现(LiFe)0.45Zn0.1Fe2O4有较强的吸波性能,然后再对(LiFe)0.45Zn0.1Fe2O4进行不同搀杂,并在0.5～18GHz频段内测试材料的吸波性能,发现掺入1wt%的Al2O3对增加-10dB带宽非常有效果.     

Characteristics of strontium isotopes and their implications in the Qixing Cave of Guizhou,China

The strontium isotopic compositions (87Sr/86Sr) of samples including soils, bedrock, soil waters, drip waters and their corresponding speleothems in the Qixing Cave (QXC), Guizhou Province, China, were systemically measured and analyzed. The results indicate that there are significant Sr isotopic differences among samples. The mean 87Sr/86Sr ratios in drip water for the samples 1#, 4# and 9# were 0.709568, 0.709139 and 0.708761, respectively, which possibly result from different flow paths, residence times, and other hydrogeological processes in the unsaturated zone overlying QXC. Meanwhile, levels of 40.8%, 57.6% and 72.4% of Sr in drip waters for 1#, 4# and 9#, respectively, were derived from bedrock dissolution, which was calculated by the mixture model of the two end-members (soil and bedrock). There is, however, no positive correlation between the relative proportion from bedrock dissolution (δ13C value is 1.8‰) and drip water δ13CDIC values. The mean drip water δ13CDIC value in 1# is the heaviest (–4.5‰) with the lowest contribution rate of bedrock dissolution, whereas the value in 9# is the lightest (–9.3‰) with the highest contribution rate of bedrock dissolution. The proportion from host rock dissolution in 4# is higher than that in 1# and lower than that in 9#, while its mean drip water δ13CDIC value (–8.6‰) is higher than that of 9# and lower than that for 1#. This suggests that the prior calcite precipitation (PCP) processes in the unsaturated zone overlying the cave are responsible for the δ13CDIC value differences between different drip waters, and not bedrock dissolution. Furthermore, this study also demonstrates that the 87Sr/86Sr ratios of speleothems in the 1# and 4# mainly reflect the variation in the relative proportions from the soil system (soil water) and bedrock dissolution overlying the cave. It is, therefore, feasible to use the strontium isotopic signals of speleothems as an indicator for soil chemical weathering intensity, and consequently as a monsoon proxy in the study area.     

SrWO_4-ZnO复合物的制备及光致发光与光催化性质的研究

采用溶剂热法制备纯的和复合ZnO的SrWO4,利用XRD、TG、PL、ICP和UV-Vis等手段对样品进行表征,研究ZnO含量对SrWO4-ZnO复合物的光致发光及光催化降解次甲基蓝活性的影响.结果表明:适量ZnO的复合引起SrWO4-ZnO复合物PL光谱强度降低,当ZnO复合量为7%时,复合物的PL光谱强度最低,光催化次甲基蓝溶液效率最高.表明复合物的PL光谱与其光催化活性有着一定的联系.     

锶铁氧体的结构特征及制备方法研究现状

对锶铁氧体的结构、性能特征以及主要制备方法进行了综合评述.锶铁氧体为六角晶系,属于M型铁氧体,其矫顽力主要取决于磁晶各向异性;制备方法主要有陶瓷法、化学共沉淀法、水热法、溶胶-凝胶法、熔盐合成法和自蔓延高温合成法等.水热法和溶胶-凝胶法因具有工艺简单、产品磁性能高等优点,是今后高性能锶铁氧体制备技术的主要研究方向.