Groundwater is the portion of the
Earth's water cycle that flows underground. Groundwater originates from
precipitation that percolates into the ground. The
ocean is the natural sink for groundwater flows.
Unlike surface water, groundwater
does not recycle readily. Rates of groundwater turnover vary from days to
years, and from centuries to millennia, depending on aquifer location, type,
depth, properties, and connectivity. The average time for the renewal of
groundwater is 1,400 years . Shorter renewal times
tend to be associated with shallow groundwater, while longer renewal times are
associated with deep groundwater. Significantly, renewal rates of deep
groundwater are about 1/15 of those of shallow groundwater. To
some extend, the groundwater is practically nonrenewable; once used, they are
not likely to recharge any time soon.
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