Isopycnic typically describes surfaces, not processes.
2.
Another applicable technique is cofractionation in sucrose ( or other material ) gradients using isopycnic centrifugation.
3.
In other words, it is a flow in which isobaric surfaces are isopycnic surfaces and vice versa.
4.
In general isopycnic surfaces will occur in fluids in hydrostatic equilibrium coinciding with equipotential surfaces formed by gravity.
5.
Isopycnic surfaces contrast with isobaric or isothermal surfaces, which describe surfaces of constant pressure and constant temperature respectively.
6.
Isopycnic centrifugation refers to a method wherein a density gradient is either pre-formed or forms during high speed centrifugation.
7.
If the ocean surface were isopycnic ( of constant density ) and undisturbed by tides, currents, or weather, it would closely approximate the geoid.
8.
The density of most liquids is nearly constant ( isopycnic ), so it can be stated that their densities vary only weakly with pressure and temperature.
9.
Water masses can travel across the ocean as turbulent eddies, or parcels of water usually along constant density ( isopycnic ) surfaces where the expenditure of energy is smallest.
10.
It is common in conversational use to hear isopycnic surfaces referred to simply as " iso-density " surfaces, which while strictly incorrect, is nonetheless abundantly more clear.
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