Inhomogenous nonlinear transport equation $u_t+uu_x = -Du$












2












$begingroup$


We have the following setup: $$u_t+uu_x = -Du \ u(x,0)=sin x.$$ The question is to find the time $T_s$ of a first shock formation. So basically, I need to solve the equation using method of characteristics and go from there.



But when I solve the corresponding quasilinear equation,I am getting the implicit solution $$u(x,t) = dfrac{sin(x-tu)}{1+Dt}$$ which does not seem right.



Can anybody provide a solution using the method of characterisics so I can pinpoint where my mistake is?










share|cite|improve this question











$endgroup$

















    2












    $begingroup$


    We have the following setup: $$u_t+uu_x = -Du \ u(x,0)=sin x.$$ The question is to find the time $T_s$ of a first shock formation. So basically, I need to solve the equation using method of characteristics and go from there.



    But when I solve the corresponding quasilinear equation,I am getting the implicit solution $$u(x,t) = dfrac{sin(x-tu)}{1+Dt}$$ which does not seem right.



    Can anybody provide a solution using the method of characterisics so I can pinpoint where my mistake is?










    share|cite|improve this question











    $endgroup$















      2












      2








      2


      1



      $begingroup$


      We have the following setup: $$u_t+uu_x = -Du \ u(x,0)=sin x.$$ The question is to find the time $T_s$ of a first shock formation. So basically, I need to solve the equation using method of characteristics and go from there.



      But when I solve the corresponding quasilinear equation,I am getting the implicit solution $$u(x,t) = dfrac{sin(x-tu)}{1+Dt}$$ which does not seem right.



      Can anybody provide a solution using the method of characterisics so I can pinpoint where my mistake is?










      share|cite|improve this question











      $endgroup$




      We have the following setup: $$u_t+uu_x = -Du \ u(x,0)=sin x.$$ The question is to find the time $T_s$ of a first shock formation. So basically, I need to solve the equation using method of characteristics and go from there.



      But when I solve the corresponding quasilinear equation,I am getting the implicit solution $$u(x,t) = dfrac{sin(x-tu)}{1+Dt}$$ which does not seem right.



      Can anybody provide a solution using the method of characterisics so I can pinpoint where my mistake is?







      pde characteristics transport-equation






      share|cite|improve this question















      share|cite|improve this question













      share|cite|improve this question




      share|cite|improve this question








      edited Dec 6 '18 at 11:53









      Harry49

      6,17331132




      6,17331132










      asked Aug 23 '17 at 21:18









      dezdichadodezdichado

      6,3711929




      6,3711929






















          2 Answers
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          active

          oldest

          votes


















          2












          $begingroup$

          First, it should be clearly stated what $D$ is here. Many times it represents a differential operator, but here I assume it is meant to be an arbitrary constant. I'll rewrite the equation with $q = u_x, p = u_t, z = u,$ so that $F(p,q,z) = 0,$
          $$p - zq + Dz = 0.$$
          Next, apply the method of characteristics, where only the $z, x$ characteristics are needed since its not fully nonlinear.



          begin{align}
          frac{dz}{dt} &= q partial_q F + p partial_p F = p -zq = -Dz; ;; z(x_0,0) = sin(x_0)\
          frac{dx}{dt} &= partial_q F = -z; ;; x(t = 0) = x_0.
          end{align}
          Solving these gives us our solution,
          begin{align}
          z(x_0,t) &= sin(x_0)e^{-Dt}\
          x &= frac{sin{(x_0)}(e^{-Dt} - 1) + Dx_0}{D}
          end{align}
          Now if we could solve the latter equation for $x_0 = x_0(x,t),$ we could plug this back into the equation for $z(x_0,t)$ to get $u(x,t)$ explicitly.



          If I wanted to show a finite time blow up, I'd formally take the $x$ derivative of $z(x_0,t),$
          begin{align}
          frac{dz}{dx} &= cos{(x_0)}e^{-Dt}frac{dx_0}{dx} = cos{(x_0)}e^{-Dt} frac{1}{frac{dx}{dx_0}}\
          &= frac{Dcos{(x_0)}e^{-Dt}}{cos{(x_0)}(e^{-Dt} - 1) + D}\
          &= frac{De^{-Dt}}{e^{-Dt} + frac{D}{cos{(x_0)}}-1}\
          end{align}
          Perhaps I have errored, but this gradient only blows up if $e^{-Dt} = frac{D}{cos{x_0}} - 1,$ at some $t.$ Therefore, we need $D leq 2$ for this to happen at all.



          I am a little surprised about this, that the RHS forcing term changes this answer from the normal result, i.e. blow up when $t = frac{-1}{cos{(x_0)}}.$






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            Thanks, it looks promising and I will look into it in detail.
            $endgroup$
            – dezdichado
            Aug 24 '17 at 19:16










          • $begingroup$
            @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
            $endgroup$
            – Harry49
            Aug 31 '18 at 11:27



















          1












          $begingroup$

          This (dissipative) Burgers' equation with relaxation is a typical example of conditional shock formation. The method of characteristics gives





          • $frac{text d t}{text d s} = 1$. Letting $t(0) = 0$, we have $t=s$.


          • $frac{text d u}{text d s} = -Du$. Letting $u(0) = sin x_0$, we have $u = sin (x_0), e^{-Ds}$.


          • $frac{text d x}{text d s} = u$. Letting $x(0) = x_0$, we have $x = -frac{1}{D} sin(x_0)(e^{-Ds}-1) + x_0$.


          This is sometimes written in implicit form as $$u = sinleft(x - frac{e^{Dt}-1}{D} uright) e^{-Dt}, .$$
          Now, let us compute the breaking time. Differentiating $x$ w.r.t. $x_0$ , we have $frac{text d x}{text d x_0} = -frac{1}{D} cos(x_0)(e^{-Dt}-1) + 1$. This quantity vanishes at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, where characteristics intersect. The smallest such positive time corresponds to the breaking time $T_s$, i.e.
          $$
          T_s = frac{1}{D}lnleft(frac{1}{1-D}right) ,quad text{if}quad D < 1 , .
          $$

          Otherwise, if $Dgeqslant 1$, no shock occurs.



          Alternatively, one can follow the method leading to Eq. (6.10) p. 36 of (1). Differentiating the PDE with respect to $x$ gives
          $$
          u_{tx} + (u_x)^2 + u u_{xx} = -Du_x , .
          $$

          Now, we introduce $q = u_x$ and the directional derivative $q' = q_t + u q_x$, so that the previous equation rewrites as
          $q' + q^2 = -D q$.
          This Bernoulli differential equation has the solution
          $$
          q(t) = frac{D q_0}{(D + q_0) e^{Dt}- q_0} , ,
          $$

          where $q_0 = q(0) = cos x_0$. Therefore, $q$ blows up at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, and the same expression of $T_s$ is obtained.





          (1) P.D. Lax, Hyperbolic systems of conservation laws and the mathematical theory of shock waves. SIAM, 1973. doi:10.1137/1.9781611970562.ch1






          share|cite|improve this answer











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            2 Answers
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            2 Answers
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            2












            $begingroup$

            First, it should be clearly stated what $D$ is here. Many times it represents a differential operator, but here I assume it is meant to be an arbitrary constant. I'll rewrite the equation with $q = u_x, p = u_t, z = u,$ so that $F(p,q,z) = 0,$
            $$p - zq + Dz = 0.$$
            Next, apply the method of characteristics, where only the $z, x$ characteristics are needed since its not fully nonlinear.



            begin{align}
            frac{dz}{dt} &= q partial_q F + p partial_p F = p -zq = -Dz; ;; z(x_0,0) = sin(x_0)\
            frac{dx}{dt} &= partial_q F = -z; ;; x(t = 0) = x_0.
            end{align}
            Solving these gives us our solution,
            begin{align}
            z(x_0,t) &= sin(x_0)e^{-Dt}\
            x &= frac{sin{(x_0)}(e^{-Dt} - 1) + Dx_0}{D}
            end{align}
            Now if we could solve the latter equation for $x_0 = x_0(x,t),$ we could plug this back into the equation for $z(x_0,t)$ to get $u(x,t)$ explicitly.



            If I wanted to show a finite time blow up, I'd formally take the $x$ derivative of $z(x_0,t),$
            begin{align}
            frac{dz}{dx} &= cos{(x_0)}e^{-Dt}frac{dx_0}{dx} = cos{(x_0)}e^{-Dt} frac{1}{frac{dx}{dx_0}}\
            &= frac{Dcos{(x_0)}e^{-Dt}}{cos{(x_0)}(e^{-Dt} - 1) + D}\
            &= frac{De^{-Dt}}{e^{-Dt} + frac{D}{cos{(x_0)}}-1}\
            end{align}
            Perhaps I have errored, but this gradient only blows up if $e^{-Dt} = frac{D}{cos{x_0}} - 1,$ at some $t.$ Therefore, we need $D leq 2$ for this to happen at all.



            I am a little surprised about this, that the RHS forcing term changes this answer from the normal result, i.e. blow up when $t = frac{-1}{cos{(x_0)}}.$






            share|cite|improve this answer









            $endgroup$













            • $begingroup$
              Thanks, it looks promising and I will look into it in detail.
              $endgroup$
              – dezdichado
              Aug 24 '17 at 19:16










            • $begingroup$
              @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
              $endgroup$
              – Harry49
              Aug 31 '18 at 11:27
















            2












            $begingroup$

            First, it should be clearly stated what $D$ is here. Many times it represents a differential operator, but here I assume it is meant to be an arbitrary constant. I'll rewrite the equation with $q = u_x, p = u_t, z = u,$ so that $F(p,q,z) = 0,$
            $$p - zq + Dz = 0.$$
            Next, apply the method of characteristics, where only the $z, x$ characteristics are needed since its not fully nonlinear.



            begin{align}
            frac{dz}{dt} &= q partial_q F + p partial_p F = p -zq = -Dz; ;; z(x_0,0) = sin(x_0)\
            frac{dx}{dt} &= partial_q F = -z; ;; x(t = 0) = x_0.
            end{align}
            Solving these gives us our solution,
            begin{align}
            z(x_0,t) &= sin(x_0)e^{-Dt}\
            x &= frac{sin{(x_0)}(e^{-Dt} - 1) + Dx_0}{D}
            end{align}
            Now if we could solve the latter equation for $x_0 = x_0(x,t),$ we could plug this back into the equation for $z(x_0,t)$ to get $u(x,t)$ explicitly.



            If I wanted to show a finite time blow up, I'd formally take the $x$ derivative of $z(x_0,t),$
            begin{align}
            frac{dz}{dx} &= cos{(x_0)}e^{-Dt}frac{dx_0}{dx} = cos{(x_0)}e^{-Dt} frac{1}{frac{dx}{dx_0}}\
            &= frac{Dcos{(x_0)}e^{-Dt}}{cos{(x_0)}(e^{-Dt} - 1) + D}\
            &= frac{De^{-Dt}}{e^{-Dt} + frac{D}{cos{(x_0)}}-1}\
            end{align}
            Perhaps I have errored, but this gradient only blows up if $e^{-Dt} = frac{D}{cos{x_0}} - 1,$ at some $t.$ Therefore, we need $D leq 2$ for this to happen at all.



            I am a little surprised about this, that the RHS forcing term changes this answer from the normal result, i.e. blow up when $t = frac{-1}{cos{(x_0)}}.$






            share|cite|improve this answer









            $endgroup$













            • $begingroup$
              Thanks, it looks promising and I will look into it in detail.
              $endgroup$
              – dezdichado
              Aug 24 '17 at 19:16










            • $begingroup$
              @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
              $endgroup$
              – Harry49
              Aug 31 '18 at 11:27














            2












            2








            2





            $begingroup$

            First, it should be clearly stated what $D$ is here. Many times it represents a differential operator, but here I assume it is meant to be an arbitrary constant. I'll rewrite the equation with $q = u_x, p = u_t, z = u,$ so that $F(p,q,z) = 0,$
            $$p - zq + Dz = 0.$$
            Next, apply the method of characteristics, where only the $z, x$ characteristics are needed since its not fully nonlinear.



            begin{align}
            frac{dz}{dt} &= q partial_q F + p partial_p F = p -zq = -Dz; ;; z(x_0,0) = sin(x_0)\
            frac{dx}{dt} &= partial_q F = -z; ;; x(t = 0) = x_0.
            end{align}
            Solving these gives us our solution,
            begin{align}
            z(x_0,t) &= sin(x_0)e^{-Dt}\
            x &= frac{sin{(x_0)}(e^{-Dt} - 1) + Dx_0}{D}
            end{align}
            Now if we could solve the latter equation for $x_0 = x_0(x,t),$ we could plug this back into the equation for $z(x_0,t)$ to get $u(x,t)$ explicitly.



            If I wanted to show a finite time blow up, I'd formally take the $x$ derivative of $z(x_0,t),$
            begin{align}
            frac{dz}{dx} &= cos{(x_0)}e^{-Dt}frac{dx_0}{dx} = cos{(x_0)}e^{-Dt} frac{1}{frac{dx}{dx_0}}\
            &= frac{Dcos{(x_0)}e^{-Dt}}{cos{(x_0)}(e^{-Dt} - 1) + D}\
            &= frac{De^{-Dt}}{e^{-Dt} + frac{D}{cos{(x_0)}}-1}\
            end{align}
            Perhaps I have errored, but this gradient only blows up if $e^{-Dt} = frac{D}{cos{x_0}} - 1,$ at some $t.$ Therefore, we need $D leq 2$ for this to happen at all.



            I am a little surprised about this, that the RHS forcing term changes this answer from the normal result, i.e. blow up when $t = frac{-1}{cos{(x_0)}}.$






            share|cite|improve this answer









            $endgroup$



            First, it should be clearly stated what $D$ is here. Many times it represents a differential operator, but here I assume it is meant to be an arbitrary constant. I'll rewrite the equation with $q = u_x, p = u_t, z = u,$ so that $F(p,q,z) = 0,$
            $$p - zq + Dz = 0.$$
            Next, apply the method of characteristics, where only the $z, x$ characteristics are needed since its not fully nonlinear.



            begin{align}
            frac{dz}{dt} &= q partial_q F + p partial_p F = p -zq = -Dz; ;; z(x_0,0) = sin(x_0)\
            frac{dx}{dt} &= partial_q F = -z; ;; x(t = 0) = x_0.
            end{align}
            Solving these gives us our solution,
            begin{align}
            z(x_0,t) &= sin(x_0)e^{-Dt}\
            x &= frac{sin{(x_0)}(e^{-Dt} - 1) + Dx_0}{D}
            end{align}
            Now if we could solve the latter equation for $x_0 = x_0(x,t),$ we could plug this back into the equation for $z(x_0,t)$ to get $u(x,t)$ explicitly.



            If I wanted to show a finite time blow up, I'd formally take the $x$ derivative of $z(x_0,t),$
            begin{align}
            frac{dz}{dx} &= cos{(x_0)}e^{-Dt}frac{dx_0}{dx} = cos{(x_0)}e^{-Dt} frac{1}{frac{dx}{dx_0}}\
            &= frac{Dcos{(x_0)}e^{-Dt}}{cos{(x_0)}(e^{-Dt} - 1) + D}\
            &= frac{De^{-Dt}}{e^{-Dt} + frac{D}{cos{(x_0)}}-1}\
            end{align}
            Perhaps I have errored, but this gradient only blows up if $e^{-Dt} = frac{D}{cos{x_0}} - 1,$ at some $t.$ Therefore, we need $D leq 2$ for this to happen at all.



            I am a little surprised about this, that the RHS forcing term changes this answer from the normal result, i.e. blow up when $t = frac{-1}{cos{(x_0)}}.$







            share|cite|improve this answer












            share|cite|improve this answer



            share|cite|improve this answer










            answered Aug 24 '17 at 15:02









            MerkhMerkh

            2,297619




            2,297619












            • $begingroup$
              Thanks, it looks promising and I will look into it in detail.
              $endgroup$
              – dezdichado
              Aug 24 '17 at 19:16










            • $begingroup$
              @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
              $endgroup$
              – Harry49
              Aug 31 '18 at 11:27


















            • $begingroup$
              Thanks, it looks promising and I will look into it in detail.
              $endgroup$
              – dezdichado
              Aug 24 '17 at 19:16










            • $begingroup$
              @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
              $endgroup$
              – Harry49
              Aug 31 '18 at 11:27
















            $begingroup$
            Thanks, it looks promising and I will look into it in detail.
            $endgroup$
            – dezdichado
            Aug 24 '17 at 19:16




            $begingroup$
            Thanks, it looks promising and I will look into it in detail.
            $endgroup$
            – dezdichado
            Aug 24 '17 at 19:16












            $begingroup$
            @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
            $endgroup$
            – Harry49
            Aug 31 '18 at 11:27




            $begingroup$
            @dezdichado There is a sign mistake in the expression of the characteristic curves $x=dots$ here (see my answer). This explains the inconsistency pointed out by the answerer.
            $endgroup$
            – Harry49
            Aug 31 '18 at 11:27











            1












            $begingroup$

            This (dissipative) Burgers' equation with relaxation is a typical example of conditional shock formation. The method of characteristics gives





            • $frac{text d t}{text d s} = 1$. Letting $t(0) = 0$, we have $t=s$.


            • $frac{text d u}{text d s} = -Du$. Letting $u(0) = sin x_0$, we have $u = sin (x_0), e^{-Ds}$.


            • $frac{text d x}{text d s} = u$. Letting $x(0) = x_0$, we have $x = -frac{1}{D} sin(x_0)(e^{-Ds}-1) + x_0$.


            This is sometimes written in implicit form as $$u = sinleft(x - frac{e^{Dt}-1}{D} uright) e^{-Dt}, .$$
            Now, let us compute the breaking time. Differentiating $x$ w.r.t. $x_0$ , we have $frac{text d x}{text d x_0} = -frac{1}{D} cos(x_0)(e^{-Dt}-1) + 1$. This quantity vanishes at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, where characteristics intersect. The smallest such positive time corresponds to the breaking time $T_s$, i.e.
            $$
            T_s = frac{1}{D}lnleft(frac{1}{1-D}right) ,quad text{if}quad D < 1 , .
            $$

            Otherwise, if $Dgeqslant 1$, no shock occurs.



            Alternatively, one can follow the method leading to Eq. (6.10) p. 36 of (1). Differentiating the PDE with respect to $x$ gives
            $$
            u_{tx} + (u_x)^2 + u u_{xx} = -Du_x , .
            $$

            Now, we introduce $q = u_x$ and the directional derivative $q' = q_t + u q_x$, so that the previous equation rewrites as
            $q' + q^2 = -D q$.
            This Bernoulli differential equation has the solution
            $$
            q(t) = frac{D q_0}{(D + q_0) e^{Dt}- q_0} , ,
            $$

            where $q_0 = q(0) = cos x_0$. Therefore, $q$ blows up at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, and the same expression of $T_s$ is obtained.





            (1) P.D. Lax, Hyperbolic systems of conservation laws and the mathematical theory of shock waves. SIAM, 1973. doi:10.1137/1.9781611970562.ch1






            share|cite|improve this answer











            $endgroup$


















              1












              $begingroup$

              This (dissipative) Burgers' equation with relaxation is a typical example of conditional shock formation. The method of characteristics gives





              • $frac{text d t}{text d s} = 1$. Letting $t(0) = 0$, we have $t=s$.


              • $frac{text d u}{text d s} = -Du$. Letting $u(0) = sin x_0$, we have $u = sin (x_0), e^{-Ds}$.


              • $frac{text d x}{text d s} = u$. Letting $x(0) = x_0$, we have $x = -frac{1}{D} sin(x_0)(e^{-Ds}-1) + x_0$.


              This is sometimes written in implicit form as $$u = sinleft(x - frac{e^{Dt}-1}{D} uright) e^{-Dt}, .$$
              Now, let us compute the breaking time. Differentiating $x$ w.r.t. $x_0$ , we have $frac{text d x}{text d x_0} = -frac{1}{D} cos(x_0)(e^{-Dt}-1) + 1$. This quantity vanishes at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, where characteristics intersect. The smallest such positive time corresponds to the breaking time $T_s$, i.e.
              $$
              T_s = frac{1}{D}lnleft(frac{1}{1-D}right) ,quad text{if}quad D < 1 , .
              $$

              Otherwise, if $Dgeqslant 1$, no shock occurs.



              Alternatively, one can follow the method leading to Eq. (6.10) p. 36 of (1). Differentiating the PDE with respect to $x$ gives
              $$
              u_{tx} + (u_x)^2 + u u_{xx} = -Du_x , .
              $$

              Now, we introduce $q = u_x$ and the directional derivative $q' = q_t + u q_x$, so that the previous equation rewrites as
              $q' + q^2 = -D q$.
              This Bernoulli differential equation has the solution
              $$
              q(t) = frac{D q_0}{(D + q_0) e^{Dt}- q_0} , ,
              $$

              where $q_0 = q(0) = cos x_0$. Therefore, $q$ blows up at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, and the same expression of $T_s$ is obtained.





              (1) P.D. Lax, Hyperbolic systems of conservation laws and the mathematical theory of shock waves. SIAM, 1973. doi:10.1137/1.9781611970562.ch1






              share|cite|improve this answer











              $endgroup$
















                1












                1








                1





                $begingroup$

                This (dissipative) Burgers' equation with relaxation is a typical example of conditional shock formation. The method of characteristics gives





                • $frac{text d t}{text d s} = 1$. Letting $t(0) = 0$, we have $t=s$.


                • $frac{text d u}{text d s} = -Du$. Letting $u(0) = sin x_0$, we have $u = sin (x_0), e^{-Ds}$.


                • $frac{text d x}{text d s} = u$. Letting $x(0) = x_0$, we have $x = -frac{1}{D} sin(x_0)(e^{-Ds}-1) + x_0$.


                This is sometimes written in implicit form as $$u = sinleft(x - frac{e^{Dt}-1}{D} uright) e^{-Dt}, .$$
                Now, let us compute the breaking time. Differentiating $x$ w.r.t. $x_0$ , we have $frac{text d x}{text d x_0} = -frac{1}{D} cos(x_0)(e^{-Dt}-1) + 1$. This quantity vanishes at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, where characteristics intersect. The smallest such positive time corresponds to the breaking time $T_s$, i.e.
                $$
                T_s = frac{1}{D}lnleft(frac{1}{1-D}right) ,quad text{if}quad D < 1 , .
                $$

                Otherwise, if $Dgeqslant 1$, no shock occurs.



                Alternatively, one can follow the method leading to Eq. (6.10) p. 36 of (1). Differentiating the PDE with respect to $x$ gives
                $$
                u_{tx} + (u_x)^2 + u u_{xx} = -Du_x , .
                $$

                Now, we introduce $q = u_x$ and the directional derivative $q' = q_t + u q_x$, so that the previous equation rewrites as
                $q' + q^2 = -D q$.
                This Bernoulli differential equation has the solution
                $$
                q(t) = frac{D q_0}{(D + q_0) e^{Dt}- q_0} , ,
                $$

                where $q_0 = q(0) = cos x_0$. Therefore, $q$ blows up at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, and the same expression of $T_s$ is obtained.





                (1) P.D. Lax, Hyperbolic systems of conservation laws and the mathematical theory of shock waves. SIAM, 1973. doi:10.1137/1.9781611970562.ch1






                share|cite|improve this answer











                $endgroup$



                This (dissipative) Burgers' equation with relaxation is a typical example of conditional shock formation. The method of characteristics gives





                • $frac{text d t}{text d s} = 1$. Letting $t(0) = 0$, we have $t=s$.


                • $frac{text d u}{text d s} = -Du$. Letting $u(0) = sin x_0$, we have $u = sin (x_0), e^{-Ds}$.


                • $frac{text d x}{text d s} = u$. Letting $x(0) = x_0$, we have $x = -frac{1}{D} sin(x_0)(e^{-Ds}-1) + x_0$.


                This is sometimes written in implicit form as $$u = sinleft(x - frac{e^{Dt}-1}{D} uright) e^{-Dt}, .$$
                Now, let us compute the breaking time. Differentiating $x$ w.r.t. $x_0$ , we have $frac{text d x}{text d x_0} = -frac{1}{D} cos(x_0)(e^{-Dt}-1) + 1$. This quantity vanishes at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, where characteristics intersect. The smallest such positive time corresponds to the breaking time $T_s$, i.e.
                $$
                T_s = frac{1}{D}lnleft(frac{1}{1-D}right) ,quad text{if}quad D < 1 , .
                $$

                Otherwise, if $Dgeqslant 1$, no shock occurs.



                Alternatively, one can follow the method leading to Eq. (6.10) p. 36 of (1). Differentiating the PDE with respect to $x$ gives
                $$
                u_{tx} + (u_x)^2 + u u_{xx} = -Du_x , .
                $$

                Now, we introduce $q = u_x$ and the directional derivative $q' = q_t + u q_x$, so that the previous equation rewrites as
                $q' + q^2 = -D q$.
                This Bernoulli differential equation has the solution
                $$
                q(t) = frac{D q_0}{(D + q_0) e^{Dt}- q_0} , ,
                $$

                where $q_0 = q(0) = cos x_0$. Therefore, $q$ blows up at $t = frac{1}{D}lnleft(frac{cos x_0}{D + cos x_0}right)$, and the same expression of $T_s$ is obtained.





                (1) P.D. Lax, Hyperbolic systems of conservation laws and the mathematical theory of shock waves. SIAM, 1973. doi:10.1137/1.9781611970562.ch1







                share|cite|improve this answer














                share|cite|improve this answer



                share|cite|improve this answer








                edited Dec 6 '18 at 11:41

























                answered Aug 30 '18 at 15:45









                Harry49Harry49

                6,17331132




                6,17331132






























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