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无序材料在液-玻相变区域的时间温度关系
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作者 曹万强 胡俊丽 刘俊刁 《哈尔滨理工大学学报》 CAS 2002年第6期10-11,共2页
运用极限动力学模型和Adam-Gibbs理论,由β的温度关系容易得出玻璃化液体的VFI方程.根据关联区域内构型熵S_c的概念及其与弛豫时间的基本关系式,可得出伸展因子与构型熵的关系式;描述了液-玻相变温区构型熵的温度变化规律及其与等压热... 运用极限动力学模型和Adam-Gibbs理论,由β的温度关系容易得出玻璃化液体的VFI方程.根据关联区域内构型熵S_c的概念及其与弛豫时间的基本关系式,可得出伸展因子与构型熵的关系式;描述了液-玻相变温区构型熵的温度变化规律及其与等压热容的关系. 展开更多
关键词 无序材料 液-玻相变区域 时间温度关系 玻璃化液体 构型重排区域 构型熵 VFT方程 极限动力学模型
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中式烹饪用时间温度积分器的构建与验证 被引量:2
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作者 邓力 黄德龙 +4 位作者 彭静 汪孝 崔俊 曾雪峰 何腊平 《农业工程学报》 EI CAS CSCD 北大核心 2017年第7期281-288,共8页
蛋白质变性能够较广泛地表征烹饪加热品质变化,因而寻找到一种z值为7.36℃的耐高温α-淀粉酶,与蛋白质热变性z值5~10℃相近。以该酶溶液为指示剂,在玻璃毛细管中封装后置入烹饪耐受性高的、特定形状的魔芋凝胶(g-KGM)载体,从而构建了烹... 蛋白质变性能够较广泛地表征烹饪加热品质变化,因而寻找到一种z值为7.36℃的耐高温α-淀粉酶,与蛋白质热变性z值5~10℃相近。以该酶溶液为指示剂,在玻璃毛细管中封装后置入烹饪耐受性高的、特定形状的魔芋凝胶(g-KGM)载体,从而构建了烹饪研究用时间温度积分器(time temperature integrators,TTIs)装置。随后,在模拟烹饪过程而设定的对流传热条件下,通过传热学试验结合非稳态传热以及酶失活动力学数学模型计算得到剩余酶活,与TTIs装置指示剂酶活实测值比较,两者误差小于2.24%。进一步,应用该TTIs装置测定了实际烹饪爆炒过程的表面换热系数。所构建的TTIs装置,结合数值模拟,可以分析测量常规试验传热学方法无法应用的激烈烹饪中流体-颗粒的传热过程,也可应用于其他领域的移动颗粒传热学研究。 展开更多
关键词 传热学 温度 中式烹饪 时间温度积分器 温度-时间关系 表面换热系数
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A study on the temporal and spatial characteristics of droughts following earthquakes
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作者 张凯 汤懋苍 高晓清 《Applied Geophysics》 SCIE CSCD 2013年第4期488-495,513,共9页
According to the "jacking-up" theory, which relates the cause of earthquakes to outer core convection ascension bodies, the crust will gradually recover after an earthquake. In such cases, the crust is stretched, th... According to the "jacking-up" theory, which relates the cause of earthquakes to outer core convection ascension bodies, the crust will gradually recover after an earthquake. In such cases, the crust is stretched, the underground temperature is reduced, precipitation decreases, and drought occurs. In this paper, precipitation is compared with ground temperature and seismic data to determine the spatial and temporal relationship between earthquakes and subsequent droughts. Our objective is to develop a new method of drought prediction. With a few exceptions in location, the analysis of the first drought to occur after the Ms 〉 7 earthquakes in China's Mainland and the adjacent areas since 1950 shows that droughts tended to occur in regions near earthquake epicenters and in the eastern regions of the epicenters at the same latitude within six months after the earthquakes. In addition, and the differences between the starting time of the earthquakes and the droughts nearly share the same probability of 0 to 6 months. After careful analysis of 34 Ms 〉 6.5 earthquakes occurring in western China from 1980 to 2011, we determined that a second drought tends to occur approximately six months following the first drought, indicating a quasi-half-year period. Moreover, the duration of the quasi-half-year fluctuation increases with the magnitude of earthquake, at approximately 2.5 years for Ms 6.5 earthquake and approximately 5 years for Ms 8 earthquake. 展开更多
关键词 EARTHQUAKE crust recovery quasi-half-year period epicenter drought area side drought area
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