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.     

利用PCR-DGGE技术分析硫化镍矿浸矿体系中的细菌群落演替

 浸矿体系中的菌群结构及其演替规律与浸出率具有密切的关系,为了解硫化镍矿浸矿体系中的这种关系以提高浸出率,利用PCR-DGGE(变性梯度凝胶电泳)技术结合16S rRNA基因序列对体系的细菌种群结构进行分析.研究表明,在硫化镍矿浸矿体系中,菌群组成菌属为嗜酸氧化亚铁硫杆菌属(Acidithiobacillus),并在浸矿体系中具有明显的演替现象,浸矿体系中的菌株演替和浸出率具有明显的相关性,经过21d的浸出,硫化镍矿的浸出率达到70%,探索浸矿体系中细菌的种群结构及其演替与浸出率的关系,对优化浸出体系菌群组成,提高浸出率具有指导作用.     

锥度量空间中两对非相容映象的一个新的公共不动点定理

 自锥度量空间的概念被提出以来,已经有数位学者对其结构和性质进行了探讨.研究了锥度量空间中非相容映象对,并利用非相容映象对的性质和压缩条件得到一类映象的公共不动点定理,其结果推广了相关文献的结果.     

脉冲耦合神经网络的人脸识别方法

 在脉冲耦合神经网络(PCNN,pulse coupled neural network)中,基于神经元脉冲震荡的时间序列概念,利用平均时间序列和平均欧氏距离的方法实现了人脸识别.实验仿真表明了该方法的有效性,对不同人脸和复杂表情的人脸均具有较好的识别效果.     

城市绿地植物群落空气负离子浓度及影响要素研究

通过对上海市6种典型城市绿地植物群落夏、秋两季空气负离子浓度的测定,分析了季节因素和群落因素对空气负离子浓度的影响关系,并重点进行了群落因素对空气负离子浓度影响的定量分析研究.研究结果表明:(1) 城市绿地植物群落空气负离子浓度受到季节和群落两个因素的协同作用;(2)城市绿地植物群落夏季的平均负离子浓度高于秋季;(3)...     

单臂氮氧自由基-抗磁金属Cd(Ⅱ)配合物的合成、结构和磁性研究

采用吡啶取代的单臂氮氧自由基与抗磁金属Cd(Ⅱ)进行配位,得到了一个新的单核配合物[Cd(1M4Py)3(OCN)2·2H2O](其中IM4Py=2-(4'-吡啶基)-4,4,5,5-四甲基咪唑啉-1-氧基自由基).单晶X-射线衍射结果表明,配合物属四方晶系,I4(1)/a空间群;晶胞参数a=1 443 9(3)nm,...     

应用Hermit插值方法修正Dome-A自动气象站记录的雪层温度

随着冰盖表面雪的积累或消融,自动气象站(AWS)上所携带的传感器相对于地表的高度/深度不断变化,给观测数据带来误差.本文利用分段三次Hermit插值的方法对Dome A地区的AWS历史雪层温度数据进行修正.结果表明,雪层的修正量随着雪的积累率的增加而增大,在夏半年为正,在冬半年为负.该方法对于浅层雪温的修正有较好的效果.     

不同恶化程度胃癌细胞系的细胞间隙连接通讯功能及Cx43表达的差异

以人正常胃黏膜上皮细胞系GES-1和不同恶化程度的人胃癌细胞系(低恶化AGS细胞系、中恶化SGC-7901细胞系、高恶化BGC-823细胞系)为研究对象,采用激光共聚焦显微镜的荧光漂白恢复技术及划痕标记荧光染料示踪技术研究不同恶化程度的胃癌细胞系细胞间隙连接通讯(Gap junctional intercellular communication,GJIC)功能的差异;采用荧光定量PCR技术和间接免疫荧光技术检测间隙连接蛋白(Connexin43,Cx43)基因在mRNA和蛋白水平的表达差异,探求其与胃癌恶性程度的相关性.结果表明,在正常胃细胞系和低、中及高恶化胃腺癌细胞系中,细胞间的GJIC功能随着恶性程度的升高而减弱(AGS、SGC-7901)或消失(BGC-823),且Cx43蛋白及mRNA的表达量随着恶性程度的升高而下调(AGS、SGC-7901)或缺失(BGC-823).这提示胃癌恶性程度与胃癌细胞的GJIC功能显著相关(P<0.05),GJIC在胃癌发生中起重要作用.     

制备特定尺寸的纳米金颗粒方法及性能表征

通过化学还原法制备出不同粒径的纳米金颗粒。利用紫外可见分光光度计和透射电子显微镜对纳米金颗粒的形貌及尺寸进行表征。讨论了还原剂种类、还原剂用量、试剂加入顺序、反应温度等因素对纳米金颗粒稳定性、粒径、形貌和分散性的影响。结果表明：Na3C6H5O7为还原剂制得纳米金颗粒粒径在15-20 nm之间,NaBH4为还原剂制得的...     

亚分米级精密定轨的探索

通过分析ENVISAT卫星跟踪的激光和DORIS测量数据,在完整力学模型的基础上,分别采用经验加速度修正和大气密度修正两种模式,对其进行精密轨道确定.经与精密轨道星历解进行比较,其结果达到了2~4 cm的径向轨道精度.