purest123 wrote:
so that means i'll have to live with it.
It should be pretty easy to work around. For your current experimental design, I would recommend that you start with water:sand ratios (by volume) ranging from 1:50 to 1:10. Mix well! You can use more water if you use finer grained sand.
Here are some terms that may be helpful for you:
'Pore space' is the volume in a sediment that is not filled by solid grains.
'Water content' or 'moisture content' is a number that represents the volume of water per volume of sediment. At the lower limit, it is 0. At the upper limit, it is equal to the pore space of the sediment (usually < 0.4, but depends on the particular sediment). For example, a mixture of 1 part water to 10 parts sand, by volume, has a moisture content of 0.1.
A soil or sediment is said to be 'saturated' when all the pore space is filled with water and 'unsaturated' when some of the pore space contains air.
'Hydraulic conductivity' is the ability of a porous substances (like sand) to transmit water. For lower water content, hydraulic conductivity is also lower. For sands, this effect is dramatic. For example, it would not be unusual for a sand to transmit water 10,000 times more slowly (hydraulic conductivity reduced by a factor of 10,000) when the moisture content drops from 0.3 to 0.1.