热管换热器的计算机设计

本文给出计算和设计重力式热管换热器所需的主要公式与数据,并在此基础上给出计算机框图,根据实验与经验资料得出的计算与设计程序可以得出热管元件与换热器的外型图,这种图可直接应用于生产,为热管换热器的设计提供快速而准确的方法。     

Cellular responses to mild heat stress

Since its discovery in 1962 by Ritossa, the heat shock response has been extensively studied by a number of investigators to understand the molecular mechanism underlying the cellular response to heat stress. The most well characterized heat shock response is induction of the heat shock proteins that function as molecular chaperones and exert cell cycle regulatory and anti-apoptotic activities. While most investigators have focused their studies on the toxic effects of heat stress in organisms such as severe heat stress-induced cell cycle arrest and apoptosis, the cellular response to fever-ranged mild heat stress has been rather underestimated. However, the cellular response to mild heat stress is likely to be more important in a physiological sense than that to severe heat stress because the body temperature of homeothermic animals increases by only 1–2°C during febrile diseases. Here we provide information that mild heat stress does have some beneficial role in organisms via positively regulating cell proliferation and differentiation, and immune response in mammalian cells.Received 14 May 2004; received after revision 2 August 2004; accepted 16 August 2004     

Geothermal field and its relation with coalbed methane distribution of the Qinshui Basin

The average geothermal gradient in the Qin-shui Basin, Shanxi Province, North China, estimated from temperature logging data of 20 boreholes is 28.2±1.03℃/km. The thermal conductivities of 39 rock samples are measured and 20 heat flow values are obtained. The estimated heat flow ranges from 44.75 mW7m2 to 101.81 mW/m2, with a mean of 62.69±15.20 mW/m2. The thermal history reconstruction from the inversion of vitrinite data, using Ther-model for Windows 2004, reveals that the average paleo-heat flow at the time of maximum burial in late Jurassic to early Cretaceous is 158.41 mW/m2 for the north part, 119.57 mW/m2 for the central part and 169.43 mW/m2for the south part of the basin respectively. The reconstruction of the buried history of the strata indicates that the age for the end of sedimentation and the beginning of erosion for the basin is 108-156 Ma, and that the eroded thickness of the strata is 2603 m in the north, 2291 m in the central, and 2528.9 m in the south of the basin respectively. The "higher in the north and the south, lower in the central" distribution pattern of the paleo-heat flow coincides with the distribution of the coal-bed methane spatially and temporally, which shows that the coal-bed methane is controlled by the paleo-geotem-perature field in the basin.     

"热寂说"、"宇宙"和宇宙

对批判"热寂说"的三种说法做出评论.指出"大爆炸"理论所描写的我们所在的这个"宇宙"与无限的宇宙是不同的.对于无限的宇宙,"热寂说"不成立."大爆炸"理论所描写的我们的"宇宙",有可能趋向"热寂状态",也有可能不会趋向"热寂状态".     

试论农业生态气候工程

主要论述热量和水分在农业生态系统中的作用及现有的农业生态气候工程。     

面向脉冲噪声环境的多径信道鲁棒估计方法

在低压电力线通信(power line communication,PLC)中,由于脉冲噪声的干扰和阻抗不匹配引起的多径信道的影响,传统的在加性高斯白噪声环境下的信道估计算法运用到电力线通信时,往往效果很差,甚至得到的结果毫无意义。针对电力线通信中的脉冲噪声,采用了Middleton Class A脉冲噪声模型。通过基于高阶矩的方法对脉冲噪声的参数进行估计。根据估计得到的脉冲噪声参数,提出了新颖的、在脉冲噪声环境中鲁棒的信道估计算法。通过仿真,验证了提出的算法是可靠的,并且具有一定的灵活性。     

群机器人狭窄通道相遇问题的解决方法

对于群机器人狭窄通道相遇问题提出一种方法——最大有效时长法。该方法能够有效解决机器人死锁问题,并降低机器人的决策难度。与人工力矩控制器配合,能使机器人高效、迅速地通过狭窄通道到达目的地;并且方法简单、计算量少。最后,仿真结果证明能有效解决群机器人狭窄通道问题。