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Plane wave

From Wikipedia, the free encyclopedia

Type of wave propagating in 3 dimensions

Inphysics, aplane wave is a special case of awave orfield: a physical quantity whose value, at any given moment, is constant through any plane that is perpendicular to a fixed direction in space.[1]

For any positionx{\displaystyle {\vec {x}}} in space and any timet{\displaystyle t}, the value of such a field can be written asF(x,t)=G(xn,t),{\displaystyle F({\vec {x}},t)=G({\vec {x}}\cdot {\vec {n}},t),}wheren{\displaystyle {\vec {n}}} is aunit-length vector, andG(d,t){\displaystyle G(d,t)} is a function that gives the field's value as dependent on only tworeal parameters: the timet{\displaystyle t}, and the scalar-valueddisplacementd=xn{\displaystyle d={\vec {x}}\cdot {\vec {n}}} of the pointx{\displaystyle {\vec {x}}} along the directionn{\displaystyle {\vec {n}}}. The displacement is constant over each plane perpendicular ton{\displaystyle {\vec {n}}}.

The values of the fieldF{\displaystyle F} may be scalars, vectors, or any other physical or mathematical quantity. They can becomplex numbers, as in acomplex exponential plane wave.

When the values ofF{\displaystyle F} are vectors, the wave is said to be alongitudinal wave if the vectors are always collinear with the vectorn{\displaystyle {\vec {n}}}, and atransverse wave if they are always orthogonal (perpendicular) to it.

Special types

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Traveling plane wave

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Thewavefronts of a plane wave traveling in3-space

Often the term "plane wave" refers specifically to atraveling plane wave, whose evolution in time can be described as simple translation of the field at a constantwave speedc{\displaystyle c} along the direction perpendicular to the wavefronts. Such a field can be written asF(x,t)=G(xnct){\displaystyle F({\vec {x}},t)=G\left({\vec {x}}\cdot {\vec {n}}-ct\right)\,}whereG(u){\displaystyle G(u)} is now a function of a single real parameteru=dct{\displaystyle u=d-ct}, that describes the "profile" of the wave, namely the value of the field at timet=0{\displaystyle t=0}, for each displacementd=xn{\displaystyle d={\vec {x}}\cdot {\vec {n}}}. In that case,n{\displaystyle {\vec {n}}} is called thedirection of propagation. For each displacementd{\displaystyle d}, the moving plane perpendicular ton{\displaystyle {\vec {n}}} at distanced+ct{\displaystyle d+ct} from the origin is called a "wavefront". This plane travels along the direction of propagationn{\displaystyle {\vec {n}}} with velocityc{\displaystyle c}; and the value of the field is then the same, and constant in time, at every one of its points.[2]

Sinusoidal plane wave

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Main article:Sinusoidal plane wave

The term is also used, even more specifically, to mean a "monochromatic" orsinusoidal plane wave: a travelling plane wave whose profileG(u){\displaystyle G(u)} is asinusoidal function. That is,F(x,t)=Asin(2πf(xnct)+φ){\displaystyle F({\vec {x}},t)=A\sin \left(2\pi f({\vec {x}}\cdot {\vec {n}}-ct)+\varphi \right)}The parameterA{\displaystyle A}, which may be a scalar or a vector, is called theamplitude of the wave; the scalar coefficientf{\displaystyle f} is its "spatial frequency"; and the scalarφ{\displaystyle \varphi } is its "phase shift".

A true plane wave cannot physically exist, because it would have to fill all space. Nevertheless, the plane wave model is important and widely used in physics. The waves emitted by any source with finite extent into a large homogeneous region of space can be well approximated by plane waves when viewed over any part of that region that is sufficiently small compared to its distance from the source. That is the case, for example, of thelight waves from a distant star that arrive at a telescope.

Plane standing wave

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Astanding wave is a field whose value can be expressed as the product of two functions, one depending only on position, the other only on time. Aplane standing wave, in particular, can be expressed asF(x,t)=G(xn)S(t){\displaystyle F({\vec {x}},t)=G({\vec {x}}\cdot {\vec {n}})\,S(t)}whereG{\displaystyle G} is a function of one scalar parameter (the displacementd=xn{\displaystyle d={\vec {x}}\cdot {\vec {n}}}) with scalar or vector values, andS{\displaystyle S} is a scalar function of time.

This representation is not unique, since the same field values are obtained ifS{\displaystyle S} andG{\displaystyle G} are scaled by reciprocal factors. If|S(t)|{\displaystyle \left|S(t)\right|} is bounded in the time interval of interest (which is usually the case in physical contexts),S{\displaystyle S} andG{\displaystyle G} can be scaled so that the maximum value of|S(t)|{\displaystyle \left|S(t)\right|} is 1. Then|G(xn)|{\displaystyle \left|G({\vec {x}}\cdot {\vec {n}})\right|} will be the maximum field magnitude seen at the pointx{\displaystyle {\vec {x}}}.

Properties

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A plane wave can be studied by ignoring the directions perpendicular to the direction vectorn{\displaystyle {\vec {n}}}; that is, by considering the functionG(z,t)=F(zn,t){\displaystyle G(z,t)=F(z{\vec {n}},t)} as a wave in a one-dimensional medium.

Anylocal operator,linear or not, applied to a plane wave yields a plane wave. Any linear combination of plane waves with the same normal vectorn{\displaystyle {\vec {n}}} is also a plane wave.

For a scalar plane wave in two or three dimensions, thegradient of the field is always collinear with the directionn{\displaystyle {\vec {n}}}; specifically,F(x,t)=n1G(xn,t){\displaystyle \nabla F({\vec {x}},t)={\vec {n}}\partial _{1}G({\vec {x}}\cdot {\vec {n}},t)}, where1G{\displaystyle \partial _{1}G} is the partial derivative ofG{\displaystyle G} with respect to the first argument.

Thedivergence of a vector-valued plane wave depends only on the projection of the vectorG(d,t){\displaystyle G(d,t)} in the directionn{\displaystyle {\vec {n}}}. Specifically,F(x,t)=n1G(xn,t){\displaystyle \nabla \cdot {\vec {F}}({\vec {x}},t)\;=\;{\vec {n}}\cdot \partial _{1}G({\vec {x}}\cdot {\vec {n}},t)}In particular, a transverse planar wave satisfiesF=0{\displaystyle \nabla \cdot {\vec {F}}=0} for allx{\displaystyle {\vec {x}}} andt{\displaystyle t}.

See also

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Look upplane wave in Wiktionary, the free dictionary.

References

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  1. ^Brekhovskikh, L. (1980).Waves in Layered Media (2 ed.). New York:Academic Press. pp. 1–3.ISBN 9780323161626.
  2. ^Jackson, John David (1998).Classical Electrodynamics (3 ed.). New York:Wiley. p. 296.ISBN 9780471309321.
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