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Basics of Fluid Mechanics, 2014a

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8.2. MASS CONSERVATION 231<br />

Combining equation (8.14) with the change in the control volume (8.9) divided<br />

by infinitesimal control volume, drrdθdz yields<br />

Continuity in Cylindrical Coordinates<br />

∂ρ<br />

∂t + 1 ∂ (rρU r )<br />

+ 1 ∂ρU θ<br />

+ ∂ρU z<br />

=0<br />

(8.15)<br />

r ∂r r ∂θ ∂z<br />

Carrying similar operations for the spherical coordinates, the continuity equation<br />

becomes<br />

∂ρ<br />

∂t + 1 ∂ ( Continuity in Spherical Coordinates<br />

)<br />

r 2 ρU r<br />

r 2 + 1 ∂ (ρU θ sin θ)<br />

+ 1 ∂ρU φ<br />

=0 (8.16)<br />

∂r r sin θ ∂θ r sin θ ∂z<br />

The continuity equations (8.8), (8.15) and (8.16) can be expressed in different coordinates.<br />

It can be noticed that the second part <strong>of</strong> these equations is the divergence<br />

(see the Appendix A.1.2 page 570). Hence, the continuity equation can be written in a<br />

general vector form as<br />

Continuity Equation<br />

∂ρ<br />

+ ∇ · (ρU) =0<br />

(8.17)<br />

∂t<br />

Advance material can be skipped<br />

The mass equation can be written in index notation for Cartesian coordinates.<br />

The index notation really does not add much to the scientific understanding. However,<br />

this writing reduce the amount <strong>of</strong> writing and potentially can help the thinking about<br />

the problem or situation in more conceptional way. The mass equation (see in the<br />

appendix for more information on the index notation) written as<br />

∂ρ<br />

∂t + ∂ (ρU) i<br />

=0 (8.18)<br />

∂x i<br />

Where i is is <strong>of</strong> the i, j, and k 4 . Compare to equation (8.8). Again remember that the<br />

meaning <strong>of</strong> repeated index is summation.<br />

End Advance material<br />

The use <strong>of</strong> these equations is normally combined with other equations (momentum<br />

and or energy equations). There are very few cases where this equation is used on its<br />

own merit. For academic purposes, several examples are constructed here.<br />

8.2.1 Mass Conservation Examples<br />

Example 8.1:<br />

A layer <strong>of</strong> liquid has an initial height <strong>of</strong> H 0 with an uniform temperature <strong>of</strong> T 0 . At<br />

4 notice the irony the second i is the direction and first i is for any one <strong>of</strong> direction x(i), y(j), and<br />

z(k).

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