Q: I have often wondered: if there is
"groundwater" beneath the earth's surface, there must also be
groundwater beneath the ocean floor too. Is it true? How deep does it go? Is it
all salt water? How salty? (Marshall)
A: Yes, its
true! Well, to a certain point. When you say, “ocean floor”, think of the
shoreline. That’s where the groundwater
is. There’s a very new, very exciting
line of study of groundwater discharge.
Its fascinating, and its possible that there is a significant amount of
water exchange between the fresh and saltwater bodies that we really didn’t
know about before. It doesn’t go all
that deep – maybe 100 m or so. And it is
certainly not all saltwater – using radon as a tracer, people have shown that
there are significant amounts of freshwater seeping out. However, saltwater can also seep into the
freshwater, and there are freshwater aquifers that are often an important
source of drinking water for coastal communities, that are becoming contaminated
by saltwater intrusions. This is
exacerbated by draining the aquifers: if
you’re pulling water out, laws of physics indicate that new water will fill in,
and saltwater may be more readily available, especially at the ocean’s
shoreline. So the water may be saline,
fresh, or brackish (usually salt water is defined as having above 20 parts per
thousand of salt, whereas freshwater has zero).
Also, in the deep ocean at the hydrothermal vents and spreading centers
(the Mid-Ocean Ridges) there is significant water exchange into the rocks and
sediment. This is all saltwater,
though.
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