A lot of that will depend on the soil under and around your pond. If you have heavy clay, your seepage will likely be minimal. If the soil is sandy, it may be hard to keep any water in it at all without a rubber liner.
An example of seepage is water slowly leaking through a crack in a dam or water slowly infiltrating into the ground from a leaking pipe.
The answer will depend on the size of the pond!
897.662 gallons in this pond.
Unsteady seepage refers to the flow of water through soil or porous media that varies with time. This can occur when there are changes in the water level, pressure, or other influencing factors that cause fluctuations in the seepage characteristics. It is important to consider unsteady seepage in engineering and environmental applications to properly assess the behavior of water flow.
alot
a hole pond
Carmen A Burton has written: 'Well-construction, water-quality, and water-level data, and pond-infiltration estimates, for three ground-water subbasins, Riverside County, California' -- subject(s): Measurement, Water quality, Water table, Wells, Seepage
When water oozes gradually through a porous substance
To find out how much solid is dissolved in pond water, you can perform a process called gravimetric analysis. This involves evaporating the water from a known volume of pond water and then measuring the mass of the residue left behind, which represents the dissolved solids. By comparing the initial and final masses, you can calculate the amount of solid dissolved in the pond water.
If water is coming into your hose through the outside wall it is said to be 'seeping' in - you have a water 'seepage'. The term can be used for any fluid not just water.
If fluid pressures in a soil deposit are uniformly increasing with depth according to then hydrostatic conditions will prevail and the fluids will not be flowing through the soil. is the depth below the water table. However, if the water table is sloping or there is a perched water table as indicated in the accompanying sketch, then seepage will occur. For steady state seepage, the seepage velocities are not varying with time. If the water tables are changing levels with time, or if the soil is in the process of consolidation, then steady state conditions do not apply.
Percolation