以环己烷为溶剂测定萘分子量探讨

在用凝固点降低法萘分子量过程中，通过测定不同时刻溶剂环守的重量变化和不册时刻吸收空气中的微量水份，得出这两种因互对以环己烷为溶剂测定萘分子量的影响。     

废橡胶胶粉利用现状及发展趋势

简述了废橡胶利用现状,指出废橡胶利用胶粉化是发展趋势,描述了我国废橡胶胶粉利用现状,分析了其未来科研和生产动态,以便和该领域同行的讨论交流。     

大型冷冻站制冷控制仿真培训系统

结合研制“大型冷冻站制冷控制仿真培训系统”的实践,介绍了从数学模型、仿真模型的建立到系统软、硬件设计的仿真培训系统开发全过程,并首创了数学模型建模的“复合法”     

Spatiotemporal characteristics of freezing and thawing of the active layer in the source areas of the Yellow River （SAYR）

Based on the analysis of data on temperatures and moisture of soils in the active layer at four different permafrost sites in the source areas of the Yellow River(SAYR)in 2010–2012,the freeze–thaw processes of soils in the active layer were compared and contrasted for understanding the spatiotemporal variations.At the four studied sites,the thickness and mean annual temperature of permafrost are different.The temperatures at the top of permafrost(TTOP),i.e.,the maximum depth(s)of seasonal frost and/or thaw penetration,are-1.9°C at the Chalaping site(CLP),-0.9°C at the site on the southern bank of the Zhaling Lake(ZLH),-0.4°C at the Maduo Town site(MDX),and 1.1°C at the site on the northern bank of the Eling Lake(ELH).Differences in the mean annual ground temperature of permafrost and TTOPs may be responsible for the differentiations in the freeze–thaw processes of soils in the active layer.With rising TTOPs,the ground thawing started earlier:CLP in early June,ZLH in late May,MDX in early May,and ELH in mid-April,while the freezing began later:CLP in early October,ZLH in early to midOctober,MDX in mid-October,and ELH in the mid-to late October.With increasing TTOPs,the freeze-up periods for permafrost sites were shortened:202 days at CLP,130 days at ZLH,100 days at MDX,and the period of complete thaw was 89 days at ELH.At the CLP and ZLH sites,the two-directional ground freezing(downwards from ground surfaces and upwards from the permafrost table)and thawing finished in the same year,but the ground freezing at the MDX continued to the end of the nextJanuary,with very slow freezing rates in the end.At the ELH site,ground freezing kept on until early May when thawing began on the surface,and upward and downward thawing became increasingly stable in late June to early July.At each site,with rising TTOPs,the downward freezing accelerated in comparison with the upward freezing,and with an increasing proportion of downward frozen depth,and with the larger ratios of freezing to thawing duration.In summary,the patterns of thawing and freezing processes in the active layer in the SAYR differ from those in other parts of the Qinghai–Tibet Plateau to a noticeable extent.     

含细粒土夹层粗颗粒硫酸盐渍土盐胀实验分析

为研究含细粒夹层粗颗粒硫酸盐渍土经多次冻融循环后的盐胀特性,对取自甘肃河西走廊地区敦煌飞机场某天然料场的粗颗粒盐渍土进行了室内多次冻融循环盐胀实验。结果表明:含细粒土层与不含细粒土层的硫酸盐渍土的盐胀主要集中在-5~15℃,在这个温度区间盐胀量变化较小;随着温度的升高,盐胀量有所减少,升温过程中盐胀减少量约为降温过程中盐胀增加量的0.5倍左右,但最终都趋于一个大于零的稳定值。含细粒土夹层粗颗粒硫酸盐渍土的盐胀量大于不含细粒土夹层的盐渍土,且前者盐胀量是后者盐胀量的1.5倍左右。     

山东地区引种的5种石楠属植物抗寒性比较

对引种到山东省济南市长清区、兖州市兴隆庄镇、临沂市罗庄区3个试验地的石楠(Photinia serrulata)、椤木石楠(P.davidsoniae)、红罗宾(P.xfraseri'Red Robin')、鲁宾斯(P.glabra var.Robens)、金红(P.xfraseri'Jin Hong')5种植物进行越冬期间植物外部形态冻害观察,并运用电导法进行抗寒能力的测定.结果表明,采用室内模拟自然界低温胁迫处理测试叶片的相对电导率,计算得出的各树种半致死温度(LT50)能定量地反映这些树种本身的抗寒能力高低,并且与越冬适应性观察结果基本相一致.济南市长清区和兖州市兴隆庄镇两试验地各树种抗寒力从强到弱依次为:鲁宾斯、红罗宾、金红、石楠、椤木石楠;而临沂市罗庄区试验地各树种抗寒力从强到弱依次为:红罗宾、鲁宾斯、金红、石楠、椤木石楠.     

浅谈低温生物医学技术的现状与展望

本文介绍了低温生物医学技术的发展现状 ,研究热点 ,并展望了其前景     

关于凝固点降低的几点讨论

本文对溶液凝固点的降低进行了讨论,认为挥发性的溶质也能使凝固点降低。且凝固点的降低不仅与溶液中溶质质点数目有关,而且与溶质种类有关。     

雨雪冰冻灾害对竹阔混交林植物多样性的影响

2008年雨雪冰冻灾害后,在崇义县选取了2块竹阔混交林固定样地,连续5年监测了雨雪冰冻灾害对竹阔混交林植物多样性的影响。结果表明,雨雪冰冻灾害后的5年内,林内郁闭度先减小后增大,新生毛竹数量明显增多。阔叶树种多的乔木植物层样地毛竹死亡率为9.8%,伴生树种死亡率为8.7%;伴生树种少的样地毛竹死亡率为72.0%,伴生树种死亡率为40.5%。乔木植物层物种丰富度指数、均匀度指数、生物多样性等指数变化较小。雨雪冰冻灾害后,竹阔混交林下物种种类数和物种个体数总数都增加了,但增加幅度都较小。2块样地的林下植物物种多样性指数变化幅度很小,丰富度指数和生物多样性指数增加或减少的幅度都不超1.0,均匀度指数增加或减少的幅度均不超过0.2。可见,雨雪冰冻灾害干扰后5年对竹阔混交林植物多样性影响较小,这可能与毛竹生长恢复较快有关。