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In [[mathematics]], particularly in [[integral calculus]], the '''localization theorem''' allows, under certain conditions, to infer the nullity of a function given only information about its continuity and the value of its integral.
Let {{math|<var>F</var>(<var>x</var>)}} be a real-valued function defined on some open [[interval]] <var>Ω</var> of the real line that is [[Continuous function|continuous]] in <var>Ω</var>. Let <var>D</var> be an arbitrary subinterval contained in <var>Ω</var>. The theorem states the following implication:
: <math>\int\limits_D F(x) \, dx = 0 ~ \forall D \subset \Omega ~ \Rightarrow ~ F(x) = 0 ~ \forall x \in \Omega</math>
[[File:Localization Theorem.svg|float|right]]
A simple proof is as follows: if there were a point <var>x</var><sub>0</sub
The theorem is easily generalized to [[multivariate calculus|multivariate function]]s, replacing intervals with the more general concept of connected open sets, that is, [[Domain (mathematics)#Real and complex analysis|___domain]]s, and the original function with some {{math|<var>F</var>(<var>'''x'''</var>) : '''R'''<sup>''n''</sup>→'''R'''}}, with the constraints of continuity and nullity of its integral over any subdomain {{math|<var>D</var>⊂<var>Ω</var>}}. The proof is completely analogous to the single variable case, and concludes with the impossibility of finding a point {{math|<var>'''x'''</var><sub>0</sub
{{clear}}
==Example==
An example of the use of this theorem in physics is the law of [[conservation of mass]] for fluids, which states that the mass of any [[fluid volume]] must not change:
<math>\int\limits_{V_f} \rho(\vec x, t) d\Omega = 0</math>▼
▲: <math>\int\limits_{V_f} \rho(\vec x, t) \, d\Omega = 0</math>
Applying the [[Reynolds transport theorem]], one can change the reference to an arbitrary (non-fluid) [[control volume]] <var>V<sub>c</sub></var>. Further assuming that the [[density|density function]] is continuous (i.e. that our fluid is monophasic and thermodinamically metastable) and that <var>V<sub>c</sub></var> is not moving relative to the chosen system of reference, the equation becomes:▼
<math>\int\limits_{V_c} \left [ {{\partial \rho} \over {\partial t}} + \nabla \cdot (\rho \vec v) \right ] d\Omega = 0</math>▼
▲Applying the [[Reynolds transport theorem]], one can change the reference to an arbitrary (non-fluid) [[control volume]] <var>V<sub>c</sub></var>. Further assuming that the [[density|density function]] is continuous (i.e. that our fluid is monophasic and thermodinamically metastable) and that <var>V<sub>c</sub></var> is not moving relative to the chosen system of reference, the equation becomes:
▲: <math>\int\limits_{V_c} \left [ {{\partial \rho} \over {\partial t}} + \nabla \cdot (\rho \vec v) \right ] \, d\Omega = 0</math>
As the equation holds for ''any'' such control volume, the localization theorem applies, rendering the common [[partial differential equation]] for the conservation of mass in monophase fluids:
: <math>
[[Category:Integral calculus]]
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