极大局部边连通有向图的度条件

对有向图D=(V(D),E(D)),顶点u和v的局部边连通度λ(u,v)=min {X:X∈E(D),D-X中不存在从u到v的路}.若对D中任意两个顶点u和v,λ(u,v)=nin{d+(u),d-(v)},称D为极大局部边连通的.笔者得到了有向图是极大局部边连通的两个度条件.推广了别人的三个结果.     

Serum levels of perfluorinated compounds in the general population in Shenzhen, China

Perfluorinated compounds (PFCs) have been detected in many environmental matrices, biota, and nonoccupationally exposed populations in China recently. However, little is known about the distribution and levels of various PFCs in the general population living in areas where there is PFC exposure. In the present study, the levels and prevalence of ten target PFCs were determined in 227 serum samples from a population of nonoccupationally exposed individuals in Shenzhen, China. Results indicated that human exposure to PFCs was prevalent in Shenzhen. Perfluorooctanoate (PFOA) was the dominant PFC contaminant in the serum samples, with a median concentration of 6.72 ng/mL, followed by perfluorooctane sulfonate (PFOS) with a median concentration of 2.07 ng/mL. Other PFCs were detected at much lower concentrations, with median concentrations ranging from 0.02 to 0.87 ng/mL. Statistically, no significant (P>0.05) gender differences were observed for any of the PFCs. Significant (P<0.01) positive correlations were found between age and serum concentrations of the target PFCs, except for perfluorobutane sulfonate (R = 0.16, P = 0.01), perfluorohexanoic acid (R = 0.08, P = 0.22), and perfluoroheptanoic acid (R = 0.11, P = 0.10). Based on the one-compartment pharmacokinetic model, the total daily intakes of PFOA and PFOS for the general population in Shenzhen were calculated as 0.63 and 0.20 ng/kg body weight/day, respectively.     

Zircon U-Pb ages of granites at Changba and Huangzhuguan in western Qinling and implications for source nature

Mesozoic granitoids are widespread in the Qinling-Dabie-Sulu orogenic belt. Precise U-Pb dating on these granitoids can reveal the evolution of the continental collision orogen and thus provide information on the nature of magma sources. This study presents zircon LA-ICP-MS U-Pb dating and whole-rock geochemical analyses for two intrusions at Changba and Huangzhuguan in western Qinling. Zircon U-Pb ages for central and marginal phases of the Huangzhuguang intrusion are 214±1 Ma and 213±3 Ma, respectively. Zircons from the Changba intrusion yield a dominant cluster with an U-Pb age of 213±2 Ma. Collectively, these ages are younger than ages of 220 to 240 Ma for ultrahigh-pressure metamorphism due to the continental collision between the South China Block and the North China Block, corresponding to syn-exhumation magmatism. Some inherited zircons occur in the Changba intrusion, yielding a weighted mean of ²⁰⁶Pb/²³⁸U ages at 757±14 Ma. This indicates that the Changba intrusion has the crustal source of mid-Neoproterozoic ages and a tectonic affinity to the South China Block. Geochemically, the two intrusuons are both rich in LILE and LREE but depleted in HFSE and HREE, similar to arc-type igneous rocks. The Huangzhuguang intrusion exhibits linear correlations between SiO₂ and the other major oxides, implying chemical evolution from a cognate magma source. It contains mafic enclaves, suggesting possible mixing of felsic-mafic magmas. The Changba granite is rich in Si and K but poor in Fe and Mg as well as has a high value of Fe*, suggesting strong differentiation of granitic magma. Therefore, the two intrusions were derived from the Late Triassic anatexis of the continental crust of different compositions in the northern margin of South China Block. This process may be coupled with exhumation of the subducted continental crust in the stage of late collision.     

半B-(E,F)-凸约束单目标规划的对偶性

利用半B-(E,F)-凸函数的有关性质讨论了半B-(E,F).凸函数单目标规划的弱对偶定理,强对偶定理和逆对偶定理.     

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.     

基于GIS的昭通市烤烟种植动态气候区划评估(预测)研究

首先构建了昭通市烤烟种植气候区划定量评价指标体系和评价方法,然后探讨了用多元线性回归结合GIS技术的气候要素空间小网格插值的问题,突破了传统气候变化影响研究总以离散点或区域平均来表达的局限,启动了面上气候波动变化影响的业务服务应用.研究了烤烟种植动态气候区划评估(预测)方法,力图把传统作物气候区划的功能从空间静态性评价提升到空间+时间动态性评估(或预评估)水平,着力反映地方立体气候和气候变化对烟草业的影响.显著提高了烤烟气候区划的生产实用指导性和应用价值.     

南汇东滩围垦湿地大型底栖动物的种类组成、数量分布和季节变动

于2009年10月至2010年7月对南汇东滩围垦湿地大型底栖动物的种类组成、密度和生物量以及生物多样性进行了研究.结果显示,被围垦潮滩共鉴定大型底栖动物9种,自然潮滩有29种;围垦潮滩的年平均密度和生物量分别为130.80ind/m2和1.89g/m2,自然潮滩为49.21ind/m2和4.08g/m2;围垦潮滩的优势...