The % of open space pores, cracks in material compared to the amount of total volume.

the model or diagam used to illustrate the movement of water at Earth's surface

particles that are the same size- have high porosity

natural liquid water flows at Earth's surface

the boundary between zone saturation, aeration

particles of mixed sizes- can have low porosity due to compaction

preciptation thats stored on land as ice, snow

subsurface water found beneath the water table

ability of material to allow water to pass through

water enters, sinks due to gravity becomes subsurface water

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