The zone between the water table and the surface is called the zoneofaeration.
潜水面与地表之间的地带称为饱气带。
2
The zoneofaeration may be treated more efficiently as a single moisture continuum.
包气带可以更有效地作为一个单一的水分连续介质来看待。
3
This article introduces a method for determining hydrogeological parameters such as the field capacity in zoneofaeration and the specific yield in aquifer where water content is varied.