空间站密封舱空气龄分布数值模拟及试验研究

介绍了空气龄理论,阐述了空气龄在空间站密封舱内空气品质评价方面的作用,对国内外在空间站密封舱内空气龄数值模拟、空气龄分布验证试验的研究进展进行了综述,并给出了对空间站密封舱进行空气龄数值模拟及试验研究的建议。     

Are older workers more active copers? Longitudinal effects of age‐contingent coping on strain at work

This study addresses coping processes as explanation of age‐related differences in strain experience. Based on the life‐span theory of control, we posit that older workers employ more active problem‐focused and more active emotion‐focused coping strategies than younger workers, which should mediate age effects on strain at work. The correlation between age and passive avoidance coping, in contrast, is expected to be qualified by external resources such as job control. Hypotheses were tested in a two‐wave panel study (8 months lag) with 634 workers (age range 16–65 years). Job demands were considered as control variables. As predicted, older as compared with younger workers reported more active problem‐focused coping, which mediated age differences on strain in the longitudinal analysis. No mediation was found for active emotion‐focused coping. Moreover, age‐contingent effects of passive avoidance coping were moderated by job control. When job control was low, younger as compared with older workers reported more avoidance coping, which in turn decreased strain in the longitudinal analysis. Finally, reverse longitudinal effects of age‐contingent strain on active problem‐focused and active emotion‐focused coping provide initial evidence for age‐contingent resource spirals. Together, the results reveal specific strengths of older workers for stress management at work. Copyright © 2015 John Wiley & Sons, Ltd.     

Assessment of the Age Structure of Sable Samples Using Three Methods of Age Determination

The age structure of sable samples has been analyzed on the basis of parameters obtained by three methods of age determination: by annual cementum layers (Klevezal, 1988), canine root canal width (Smirnov, 1960), and the degree of development of the mastication muscles and sagittal crest on the skull (Timofeev and Nadeev, 1955). It has been found that the first two methods produce similar results (r = 0.95) that are suitable for use in the practice of monitoring and commercial game management. The third method is simpler but less accurate and can be recommended only for the preliminary assessment of age ratios in populations. The results of such assessment by the method proposed by Klevezal are sufficiently accurate for a detailed analysis of population structure and dynamics of its reproductive core, but this method is laborious and involves a complicated histological procedure. When large samples are studied for the purposes of monitoring and management planning, the method proposed by Smirnov is preferable.     

短期填埋龄垃圾堆体内微生物群落结构与种群分布特征

填埋垃圾的稳定化过程一般经历好氧过渡、水解酸化、初期产甲烷及稳定产甲烷阶段,固相垃圾的厌氧水解酸化阶段常被视为垃圾降解的限速步骤,而这一阶段微生物的降解作用是影响垃圾稳定化进程的关键.以青岛市小涧西生活垃圾填埋场短期填埋龄垃圾为研究对象,采用MiSeq高通量测序研究了填埋龄0～1、1.0～1.5、1.5～2 a垃圾堆体内微生物的群落结构多样性及种群分布特征.结果表明,0～1 a填埋龄垃圾微生物多样性高于1.0～1.5 a和1.5～2 a垃圾堆体,且微生物多样性整体上随填埋深度呈降低趋势.参与垃圾降解细菌多样性比真菌更丰富,而真菌多样性随填埋区域、填埋龄的不同呈现更显著的差异.参与短期填埋龄垃圾降解的细菌中,Firmicutes在填埋层上层为优势菌门,最大比例达到65%,Proteobacteria在填埋层中下层为优势菌门,最大比例达到88%.填埋上层细菌菌属以Defluviitoga、Aerococcus、Clostridium III和Proteiniphilum为主,而在中下层以Thiopseudomonas、Sporosarcina和Eionea为主.真菌主要包括3个菌门,Ascomycota在各点位均为最优势菌门,属水平上Kernia及Aspergillus作为常见的腐生菌属,在不同点位均有较高的丰度.冗余分析表明短期填埋龄垃圾堆体内微生物不同时空分布存在显著差异性,且细菌群落结构的变化受pH值影响较大,而真菌群落结构的变化与垃圾有机质密切相关.     

PM2.5对小鼠和H9C2细胞心肌肥大相关因子mRNA表达的影响

用采自太原市4个不同季节的细颗粒物(PM_(2.5))对小鼠心肌细胞H9C2进行染毒后,采用荧光定量PCR技术检测心肌肥大相关因子ANP和TGF-β的mRNA水平.采用浓度分别为0、1、3、10μg·mL~(-1)的冬季PM_(2.5)处理H9C2细胞后,检测心肌肥大相关因子ANP、β-MHC、MMP2和MMP9的mRNA水平.之后分别选取4周龄、4月龄、10月龄C57BL/6雌性小鼠作为实验模型,采用咽后壁滴注的方法用3 mg·kg~(-1) PM_(2.5)暴露4周.采用苏木素-伊红染色(HE)对小鼠心脏组织病理切片进行观察,并检测ANP和β-MHC的mRNA水平.结果发现,与对照组相比,冬季PM_(2.5)诱导H9C2细胞中ANP和TGF-β的mRNA水平升高最为显著;其中,当冬季PM_(2.5)染毒浓度较高时可诱导ANP、β-MHC、MMP2和MMP9的mRNA水平均显著升高.经PM_(2.5)暴露4周后,幼年和老年小鼠心肌细胞核质比显著降低.老年小鼠心脏组织中ANP和β-MHC的mRNA表达水平显著上升.实验表明,冬季PM_(2.5)诱导心肌肥大标志物表达改变的效应要强于其他季节,且有一定的剂量效应关系,而老年小鼠对PM_(2.5)诱导的心肌肥大效应最为敏感.     

帕米尔高原冰川流域碎屑颗粒的铀同位素组成及其对沉积物搬运的指示

铀(U)同位素作为一种新的地球化学示踪手段,被逐渐用于研究陆地和海洋沉积物的搬运过程。然而,这一新技术能否有效指示不同环境中各类沉积物的搬运还需更多流域数据的支持。本文选取位于帕米尔高原东北部具有显著海拔梯度和气候差异的盖孜河冰川流域作为研究对象,通过该流域河流沉积物细颗粒中的U同位素的活度比((~(234)U/~(238)U)_(AR))的空间变化,探索U同位素指示内陆冰川流域沉积物搬运的可行性。流域内河流沉积物的矿物组成以石英和长石(占51%—77%)为主,表明较弱的风化作用。流域内受冰川侵蚀控制的上游山区支流康西瓦河和木吉河沉积物的(~(234)U/~(238)U)_(AR)范围分别是0.990—1.017和0.988—1.009,盖孜河中下游段河流沉积物的(~(234)U/~(238)U)_(AR)则为0.913—0.997。从上游山区至中下游段显示了一个明显的下降趋势,指示了沉积物搬运过程中(~(234)U/~(238)U)_(AR)的确发生了系统的变化。然而,盖孜河流域碎屑颗粒比表面积和分形维数计算得到的反冲损失参数太低,未能利用U同位素破碎年龄模型获得合理的沉积物搬运时间,该模型如何用到冰川流域尚需更多的研究工作。