作者: A. B. Kostinski , A. J. Durant , W. I. Rose , R. A. Shaw
DOI:
关键词:
摘要: In the atmosphere, water freezes by heterogeneous ice nucleation at temperatures between -3 °C to -40°C, or homogeneous <-40°C. Saturation describes a state of dynamic equilibrium different phases substance. case pure water, density and pressure saturated vapour over either liquid solid phase depends on temperature. These variables can be calculated specific temperature with respect vapour, phases.