I should have thought that the temperance drinks referred to could be made sufficiently attractive without the addition of water ice.
In order to model it we used a water ice sample covered by several centimetres of sand with a weight fraction of organic matter (glucose) y10-5-10-4.
A small part of them consist of very large bodies, quite comparable to planets of terrestrial type, but including a very significant share of water ice.
This potentially very important result is still awaiting confirmation, but if water ice is present it is most likely derived from the impacts of comets with the lunar surface.
In order to model these processes we used a water ice sample covered by several centimetres of sand containing organic matter.
Therefore, evaporation of adsorption water in porous soil happens on time scales, which exceed those of sublimation of water ice by orders of magnitude.
This adsorption enthalpy is a measure for the energetic bond of water molecules, which are adsorbed on the surface of water ice.
In the lower layers above the microscopic surfaces of sorbent minerals, adsorption water has a much stronger bond to these surfaces than water ice.
