摘要
用热学方法推导干燥空气大气压公式，弄清了大气层中温度随高度增加而线性降低的原因及确定系数的关系式，并在这个基础上进一步讨论了干燥空气大气压公式的意义．
Abstract The formula of atmospheric pressure about dry air,is derived by thermal motion theory.The cause of why the temperature decreases linearly with the height increased is clearly shown and the relation of coefficient is defined.The significance of the formula of atmospheric pressure about dry air is also discussed.Keyworks:dry air;atmospheric pressure;adiabatic process
出处
《广西师范大学学报（自然科学版）》
CAS
1994年第2期33-37,共5页
Journal of Guangxi Normal University:Natural Science Edition
