Fair response. Most of those are a bit obscure!
[rant mode]
Bernoulli is more complex than most other things taught at the same time. To make it worse it is usually explained in a way that is technically correct but does not bring out its essentials. Thus many students never fully understand it; some become textbook writers and go on to bamboozle later generations of students. Many examples of Bernoulli in textbooks depend on other effects and this causes further confusion.
[\rant mode]
Bernoulli is essentially a statement of conservation of energy in a dynamic fluid. It is expressed as "energy per unit volume" for:
- Gravitational potential energy, GPE
- Kinetic energy, KE
- Pressure energy
The first two are familiar from mechanics where they are mgh and ½mv^2. The third is simply pressure P.
Fluid dynamics is a gruesomely complex part of Physics. Bernoulli simplifies it by imposing several conditions; if these are not met (or not nearly enough met) Bernoulli cannot be used.
For Bernoulli to apply:
- Streamline flow (no turbulence)
- Constant density (no compression)
- Steady state (no transients, unchanging with time)
- Lossless (no friction)
Under these conditions a tiny volume of fluid entering the system goes through various changes of height, velocity and pressure; its energy content does not change. Expressed mathematically:
[tex]{\rho}gh +0.5{\rho}v^2 + p = k[/tex]
where [itex]\rho[/itex] is density, p is pressure and k is the total energy per unity volume.
Often Bernoulli is used to compare the state of the fluid in two places, as in this problem. The value of k is irrelevant and a more useful Bernoulli equation is.
[tex]{\rho}gh_1 + 0.5{\rho}v_{1}^2 + p_1 = {\rho}gh_2 + 0.5{\rho}v_{2}^2 + p_2[/tex]
To find the velocity of water coming out of a hole, consider two points on a streamline flow from the surface of the water (1) to just outside the hole (2).
- GPE: using point 2 as datum (h = 0), GPE(1) is ρgh and GPE(2) is 0.
- KE: KE(1) is 0 (the movement is negligable); KE(2) is ½ρv^2.
- Pressure: at points 1 and 2 the pressure is atmospheric.
Using the second form of Bernoulli's equation:
[tex]{\rho}gh_1 + 0.5{\rho}v_{1}^2 + p_1 = {\rho}gh_2 + 0.5{\rho}v_{2}^2 + p_2[/tex]
[tex]{\rho}gh_1 + 0.5{\rho}0^2 + atmospheric = {\rho}g0 + 0.5{\rho}v_{2}^2 + atmospheric[/tex]
Subtracting atmospheric pressure from both sides, removing the zero terms and dividing by [itex]\rho[/itex]
[tex]gh_1 = 0.5v_{2}^2[/tex]
So now you can use the depths of the holes to find the velocity of the water coming out of them ...