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重力场中大气温度和压强的探究OA

Exploration of atmospheric temperature and pressure in gravity field

中文摘要英文摘要

利用重力加速度随高度变化的范德瓦尔斯气体模型推导出大气温度和压强公式,并与重力加速度随高度变化的理想气体模型以及重力加速度不变的范德瓦尔斯气体模型进行比较研究.结果表明,3 种模型在描述大气温度时区别较小,而考虑重力加速度随高度变化的范德瓦尔斯气体模型在描述低空大气压强时则有可观测的修正效应.此外,重力加速度随高度变化的范德瓦尔斯气体模型更接近于真实情况,利用该模型研究大气温度和压强不仅有助于简化物理问题,还能在一定程度上描述大气温度和压强的主要特征.

The formulas for atmospheric temperature and pressure are derived respectively within the variation of gravity acceleration with height based on Van der Waals gas model,and compared with the ideal gas model with the variation of gravity acceleration with height and the Van der Waals gas model with constant gravity acceleration.The results indicate that the three models have relatively small differences in describing atmospheric temperature,while the Van der Waals gas model considering the variation of gravity acceleration with altitude has better improvement in describing low altitude atmospheric pressure.In addition,the Van der Waals gas model with the variation of gravity acceleration with height is closer to the real situation.Using this model not only helps to simplify physical problems,but also depicts the main characteristics of atmospheric temperature and pressure to a certain extent.

丁小雪;李博

鞍山师范学院 物理学院,辽宁 鞍山 114007鞍山师范学院 物理学院,辽宁 鞍山 114007

数理科学

理想气体范德瓦尔斯气体多方过程状态方程绝热大气

ideal gasVan der Waals gaspolytropic processstate equationadiabatic atmosphere

《安徽大学学报(自然科学版)》 2026 (1)

41-46,6

辽宁省教育厅高校基本科研项目(LJ212410169004,JYTMS20231707)

10.3969/j.issn.1000-2162.2026.01.006

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