jbriggs444
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Note that ##\rho g h## is not the pressure gradient. It is the pressure. More correctly, it is the pressure difference between the test point and a reference pressure at a point on the surface directly above.Lnewqban said:can't be the traditional ρgh (pressure gradient in the vertical direction).
A "gradient" is a rate of change. It is a vector. Its direction is the direction in which pressure increases most rapidly with displacement. Its magnitude is the rate at which pressure increases with displacement in that direction. In the drawing that you provide (one gee of vertical gravity and one gee of horizontal acceleration), the direction of the gradient is 45 degrees down and to the left. Its magnitude is ##\sqrt{2}\rho g##. As you clearly agree.
But we do not much care how rapidly pressure is increasing in a direction 45 degrees down and to the left. Our reference point is directly above our test point. We care about how rapidly pressure is increasing in the purely vertical direction. We want the vertical component of the pressure gradient.
If you wanted, you could calculate that vertical component as ##\sqrt{2}\rho g \cos 45 \text{ degrees}## That simplifies to ##\rho g##.
Or you could just use the obvious fact that the vertical component is ##\rho g##. Just like the horizontal component is ##a g## (with ##a = g## in the case you portray).
Right. So if you have a column of water ##\frac{h}{\sqrt{2}} \text{meters}## in diagonal extent so that our test point is ##\frac{h}{\sqrt{2}}\text{ meters}## below a reference point at the surface in a direction 45 degrees up and to the right. It will be at a pressure delta of ##\sqrt{2} \rho g h\frac{1}{\sqrt{2}}## above surface pressure.Lnewqban said:That point is supporting the force (each mass x common diagonal acceleration) of all the molecules that are aligned with the resultant acceleration vector and located between that point and the surface.
View attachment 315891
Equivalently, it is ##h \text{ meters}## below a reference point on the surface directly above and is at a pressure delta of ##\rho g h## above surface pressure.
Both calculations yield the same result. But one is simpler than the other.