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Equation of Fluid Statics

The sum of all forces acting on a fluid element equals the product of its density, volume, and the acceleration due to gravity.
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The statement of the theorem

The Equation of Fluid Statics is derived from the principle of mechanical equilibrium applied to a differential volume element dV\mathrm{d}\mathcal{V} within a continuous fluid domain ΩR3\Omega \subset \mathbb{R}^3 at rest. Let ρ\rho be the fluid density, PP be the thermodynamic pressure, and g\vec{g} be the gravitational acceleration vector. The condition for static equilibrium requires that the net force Fnet\vec{F}_{net} acting on dV\mathrm{d}\mathcal{V} vanishes.\n\nFormally, the governing equation is expressed as the balance of forces per unit volume:\n\nP+ρg=0\nabla P + \rho \vec{g} = \vec{0} \n\nThis vector equation implies three scalar partial differential equations (PDEs) in Cartesian coordinates (x,y,z)(x, y, z): \n\nPx+ρgx=0    Px=ρgx(x-component)\frac{\partial P}{\partial x} + \rho g_x = 0 \quad \implies \quad \frac{\partial P}{\partial x} = -\rho g_x \quad \text{(x-component)}\nPy+ρgy=0    Py=ρgy(y-component)\frac{\partial P}{\partial y} + \rho g_y = 0 \quad \implies \quad \frac{\partial P}{\partial y} = -\rho g_y \quad \text{(y-component)}\nPz+ρgz=0    Pz=ρgz(z-component)\frac{\partial P}{\partial z} + \rho g_z = 0 \quad \implies \quad \frac{\partial P}{\partial z} = -\rho g_z \quad \text{(z-component)}\n\nIntegrating these partial derivatives yields the fundamental hydrostatic pressure relation:\n\nP(z)=P0+z0zρgzdzP(z) = P_0 + \int_{z_0}^{z} \rho g_z \mathrm{d}z'
Source: Wikipedia