统计物理中三种系综之间的关系

本文从粒子数和能量的涨落和粒子数和能量的平均值与极大值之间的关系，说明统计物理中三种系综之间的区别与联系．     

碳钢在NaHCO3+NaCl溶液中的亚稳态孔蚀特征

用动电位极化和恒电位极化法研究了A3碳钢在不同浓度NaCl的0.5mol/LNaHCO₃溶液中亚稳态孔蚀行为。实验发现亚稳态电流波动峰具有快速上升、缓慢下降的特点。亚稳孔出现电位E_m 服从正态分布,随着Cl^-浓度的提高,E_m 值向负方向移动。亚稳孔的峰频变化规律与电位关系不大。恒电位极化时,当电位高于E_m而大大低于孔蚀电位E_b 时,电流波动保持一定时间后会最终消失,并产生直径为微米级的小蚀孔。当电位接近孔蚀电位时,一段时间的电流波动后电流往往迅速上升,最终转变为稳定蚀孔.     

人工气候条件下的人体着装试验的研究

本文通过物理试验方法对棉、毛、丝、棉麻及毛涤五种面料进行性能测试,得出其风格数值、透湿阻抗.为了反映面料对人的生理、心理的影响,有必要在人工气候条件下进行人体模拟着装试验,得出面料的人体舒适感觉值。借助多元线性回归方法,通过物理测试与人体试验的对照分析,发现它们之间具有良好的一致性。     

介观并联RLC电路的量子化及其量子涨落

从电阻产生的物理机制即电子与品格振动的相互作用出发，对并联电路RLC进行了量子化，并计算了相应物理量的量子涨落．     

钢丝绳断丝定量检测中径向随机晃动误差的补尝

本文论述了钢丝绳断丝定量检测中径向随机晃动误差存在的必然性及该误差对定量检测的影响,基于模拟实验结果,给出了适用于多种类型钢丝绳的V_H-S数学关系式;提出了波形因素的概念与形式,并用软件实现了钢丝绳断丝定量检测中径向随机晃动误差的补偿。     

含信号调制噪声和频率波动的时滞分数阶振子的随机共振

本文研究了含信号调制噪声和频率波动的小时滞线性分数阶振子的随机共振. 利用分数阶Shapiro-Loginov公式和Laplace变换技巧,本文首先推导了系统响应的一阶稳态矩和稳态响应振幅增益（Output Amplitude Gain, OAG）的解析表达式,然后讨论了分数阶、时滞及噪声参数对OAG的影响. 结果显示,各参数对OAG的影响均呈现出非单调变化的特点,表明系统出现广义随机共振. 特别地,分数阶与时滞的协同作用可能诱导随机共振的多样化,这就为在一定范围内调控随机共振提供了可能.     

A continuous 200-ka palaeoclimatic record from stalagmite in Tangshan Cave, Nanjing

An oxygen isotope temperature record from 381 to 166 kaB. P. (²³⁰Th/²³⁴U dating and tuned ages) has been obtained by combining data on the isotopic composition of calcites with that of fluid inclusions trapped in a stalagmite from a limestone cave in which a fossil cranium deposited. Several laminae in microsequence of the stalagmite represent climatic events or shifts. The Nanjing man fossil was older than 381 kaB. P.     

New evidence for the Qinghai-Xizang (Tibet) Plateau as a pilot region of climatic fluctuation in China

Over 40 a observed temperature data in 172 stations in China and historical proxy data were analyzed. Evidence suggested that during 1980–1994, the warmest year appeared first in southeastern part of the Qinghai-Xizang (Tibet) Plateau (henceforth SETP) and then gradually spread northwards and eastwards to eastern China. The climatic change on century time scale in recent 600 a shows 3 relatively warm and clod stages in China. Each warm and cold stage appeared first in Tibet Plateau (henceforth TP) and then in the Qilian Mountains, then in the eastern parts of China. The warm and cold stages in TP were 10–60 a earlier than in the eastern China. The facts show that TP is a pilot region of climatic fluctuation in China on the time scale shorter than 10³a.     

武汉市暴雨气候特征分析

利用武汉市东西湖区,蔡甸区,江夏区气象站１９５９￣１９９６年５￣９月降水资料及武汉城区各雨量站,１９８８￣１９９５年５￣９月降水自记资料,统计分析武汉市暴雨、大暴雨时空分布特征及其变化规律,确定武汉市灾害性暴雨标准,其研究结果可为武汉地区暴雨防灾减灾工作提供背景依据。