Post by TonyHPost by nobodyPost by MarioHello,
Can any one tell me the average water density of the caribean,
mediterranean, red , black and dead sea ? in metric system please if
possible.
Thanks,
Mario
On a more serious note, you need to clarify your question slightly. Do
you want the density of the water or the solution (ie. water, salt,
minerals, fish piss, algae, etc. etc.?)
The water, by definition, is the same density for the same temperature
and pressure, no matter the location. Generally, the saltier the water,
the lower the density. That's why you need more weight in the ocean vs.
a fresh water lake.
I think you've got that arse about face. The saltier(!), or more correctly
the higher the salinity or salt content, i.e. increasing Kg NaCl/Litres of
H20, the DENSER the solution, therefore the greater the buoyancy, so
requiring MORE ballast (Lead) not less.
Depth of sea, Rock formations of sea-bed & coastline, average ambient
temperature (evaporation issues), where the sea is 'fed' from (freshwater
mountain rivers / streams, underground water table and what rocks the water
passes through, etc.)
Salinity is not a constant, but can be averaged, however, it is highly
variable, especially near a coastline and at the surface due to factors such
as freshwater estuaries (often shown by a visible salocline with a
'shimmering' at the boundary or interface of the two differing densities of
water, and also from surface evaporation.
In addition to salinity water temperature affects it's density, as water is
most dense at 4 degrees Celsius (39.2 Fahrenheit).
Quite right, of course. It reminds me of an interesting thought problem
... that of the elusive "Perpetual Motion Machine". Typically, with
warmer water near the surface, the amount of salt held in solution is
greater, ie. saltier, and therefore denser. Unless there is a lot of
mixing, this is usually the case. So, if one were able to put, say, a
three mile deep vertical pipe, with the upper end just out of the water,
and then apply suction to the top to get the flow going upwards, less
dense water would be in the tube. And thus, the water would flow up and
out of the tube, in theory, forever, with no external energy applied to
the system save the difference in pressure between the external water
and the internal water. Unfortunately, other factors get in the way,
such as friction. But it's an interesting concept.
FWIW,
Bart F.