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<article>
<title>Role of non-Noether symmetry in integrability of dispersiveless long wave system</title>
<author>George Chavchanidze</author>
<affiliation>Department of Theoretical Physics,
A. Razmadze Institute of Mathematics,
1 Aleksidze Street, Tbilisi 0193, Georgia</affiliation>
<abstract>We show that infinite sequence of conserved 
quantities and bi-Hamiltonian structure of DLW hierarchy of integrable models 
are related to the non-Noether symmetry of dispersiveless water wave system.
</abstract>
<keywords>Non-Noether symmetry; bi-Hamiltonian system; Disperseless long wave system; Integrability;</keywords>
<msc> 70H33; 70H06; 58J70; 53Z05; 35A30</msc>

<paragraph>
Symmetries play essential role in dynamical systems, because they usually 
simplify analysis of evolution equations and often provide quite elegant 
solution of problems that otherwise would be difficult to handle. In the present 
paper we show how knowing just single generator of non-Noether symmetry one can 
construct infinite involutive sequence of conserved quantities and bi-Hamiltonian 
structure of one of the remarkable integrable models — dispersiveless long 
wave system. In fact among nonlinear partial differential equations that 
describe propagation of waves in shallow water there are many interesting 
integrable models. And most of them seem to have non-Noether symmetries leading 
to the infinite sequence of conservation laws and bi-Hamiltonian realization of 
these equations. In dispersiveless long wave system such a symmetry appears to 
be local, that in some sense simplifies and investigation of its properties and 
calculations of conserved quantities.</paragraph>
<paragraph>
Evolution of dispersiveless long wave system is governed by the following set of 
nolinear partial differential equations 
<formula xml:id="e1">
v<sub>t</sub> = v<sub>x</sub>w + vw<sub>x</sub><line />
w<sub>t</sub> = v<sub>x</sub> + ww<sub>x</sub>
</formula>
Each symmetry of this system must satisfy linear equation 
<formula>
E(v)<sub>t</sub> = (wE(v))<sub>x</sub> + (vE(w))<sub>x</sub><line />
E(w)<sub>t</sub> = E(v)<sub>x</sub> + (wE(w))<sub>x</sub>
</formula>
obtained by substituting infinitesimal transformations 
<formula>
v  → v + aE(v) + O(a<sup>2</sup>)<line />
w  → w + aE(w) + O(a<sup>2</sup>)
</formula>
into equations of motion <a href="#e1">(1)</a> and grouping first order (in <math>a</math>) terms. One of the 
solutions of this equation yields the following symmetry of dispersiveless water 
wave system 
<formula xml:id="e4">
E(v) = 4vw + 2x(vw)<sub>x</sub> + 3t(v<sup>2</sup> + vw<sup>2</sup>)<sub>x</sub><line />
E(w) = w<sup>2</sup> + 4v + 2x(ww<sub>x</sub> + v<sub>x</sub>) + t(6vw + w<sup>3</sup>)<sub>x</sub>
</formula>
and it is remarkable that this symmetry is local in sense that <math>E(u)</math> in point <math>x</math> 
depends only on <math>u</math> and its derivatives evaluated in the same point (this is not 
the case in Korteweg-de Vriez, modified Korteweg-de Vriez and nonlinear Schrödinger 
equations where similar symmetries appear to be non local <a href="#r3">[3]</a>)</paragraph>
<paragraph>
Before we proceed let us note that dispersive water wave system is actually 
infinite dimensional Hamiltonian dynamical system. Assuming that <math>u, v</math> and <math>w</math> 
fields are subjected to zero boundary conditions 
<formula>
v(± ∞) = w(± ∞) = 0
</formula>
it is easy to verify that equations <a href="#e1">(1)</a> can be represented in Hamiltonian form 
<formula>
v<sub>t</sub> = {h , v}<line />
w<sub>t</sub> = {h , w}
</formula>
with Hamiltonian equal to 
<formula xml:id="e7">
h = − ½ <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>(vw<sup>2</sup> + v<sup>2</sup>)dx 
</formula>
and Poisson bracket defined by the following Poisson bivector field 
<formula xml:id="e8">
W = <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>(<fraction><num>δ</num><den>δv</den></fraction> ∧ {<fraction><num>δ</num><den>δw</den></fraction>}<sub>x</sub>) dx 
</formula>
Now using our symmetry that appears to be non-Noether, one can calculate second 
Poisson bivector field involved in the bi-Hamiltonian realization of 
dispersiveless long wave system 
<formula xml:id="e9">
Ŵ = [E , W] = − 2 <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under> (v<fraction><num>δ</num><den>δv</den></fraction> ∧ {<fraction><num>δ</num><den>δv</den></fraction>}<sub>x</sub> 
+ w <fraction><num>δ</num><den>δv</den></fraction> ∧ {<fraction><num>δ</num><den>δw</den></fraction>}<sub>x</sub> 
+ <fraction><num>δ</num><den>δw</den></fraction> ∧ {<fraction><num>δ</num><den>δw</den></fraction>}<sub>x</sub>) dx 
</formula>
Note that <math>Ŵ</math> give rise to the second Hamiltonian realization of the model 
<formula>
v<sub>t</sub> = {ĥ , v}<sub>∗</sub><line />
w<sub>t</sub> = {ĥ , w}<sub>∗</sub>
</formula>
where 
<formula>
ĥ = − ½ <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>vwdx 
</formula>
and <math>{ , }<sub>∗</sub></math> is Poisson bracket defined by bivector field <math>Ŵ</math>. 
</paragraph>
<paragraph>
Now let us pay attention to conservation laws. By integrating third equation of 
dispersive water wave system <a href="#e1">(1)</a> it is easy to show that 
<formula>
J<sup>(0)</sup> = <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>wdx 
</formula>
is conservation law. Using non-Noether symmetry one can construct other 
conservation laws by taking Lie derivative of <math>J<sup>(0)</sup></math> along the generator of 
symmetry and in this way entire infinite sequence of conservation laws of 
dispersive water wave system can be reproduced 
<formula xml:id="e13">
J<sup>(0)</sup> = <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>wdx<line />
J<sup>(1)</sup> = L<sub>E</sub>J<sup>(0)</sup> = 2 <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>vdx<line />
J<sup>(2)</sup> = L<sub>E</sub>J<sup>(1)</sup> = (L<sub>E</sub>)<sup>2</sup>J<sup>(0)</sup> = 4 <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>vwdx<line />
J<sup>(3)</sup> = L<sub>E</sub>J<sup>(2)</sup> = (L<sub>E</sub>)<sup>3</sup>J<sup>(0)</sup> = 12 <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>(vw<sup>2</sup> + v<sup>2</sup>)dx<line />
J<sup>(4)</sup> = L<sub>E</sub>J<sup>(3)</sup> = (L<sub>E</sub>)<sup>4</sup>J<sup>(0)</sup> = 48 <under><over><sat>+ ∞</sat><ope>∫</ope></over><sat>− ∞</sat></under>(3v<sup>2</sup>w + vw<sup>3</sup>)dx<line />
J<sup>(n)</sup> = L<sub>E</sub>J<sup>(n − 1)</sup> = (L<sub>E</sub>)<sup>n</sup>J<sup>(0)</sup>
</formula>
So as we see non-Noether symmetry <a href="#e4">(4)</a> naturally leads to infinite sequence of 
conserved quantities and second Hamiltonian realization of dispersiveless water 
wave system.</paragraph>
<acknowledgements>
Author thanks organizers of 11th Regional Conference  on Mathematical Physics for kind hospitality. This work was supported by INTAS (00-00561). 
</acknowledgements>
<references>
<cite xml:id="r1">
	<who>G. Bluman, S. Kumei</who>
	<what>Symmetries and differential equations</what>
	<where>Springer-Verlag, New York</where>
	<when>1989</when>
</cite>
<cite xml:id="r2" eprint="math-ph/0211014">
	<who>G. Chavchanidze</who>
	<what>Non-Noether symmetries and their influence on phase space geometry</what>
	<where>J. Geom. Phys. 48, 190-202</where>
	<when>2003</when>
</cite>
<cite xml:id="r3">
	<who>G. Chavchanidze</who>
	<what>Non-Noether symmetries in Hamiltonian dynamical  systems</what>
	<where>math-ph/0405003</where>
	<when>2004</when>
</cite>
<cite xml:id="r4">
	<who>P. Olver</who>
	<what>Applications of Lie groups to differential equations</what>
	<where>GTM 107, Springer Verlag, New York</where>
	<when>1986</when>
</cite>
</references>
</article>