Line Integral Harmonization












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Is there a connection between line integrals over scalar fields and line integrals over vector fields? For example, do the pair $f(x, y)$ and $F(x, y)$ which stand in a potential function and gradient relationship have the same line integral for any specified curve, when $F(x, y)$ is drawn in the $xy$-plane of the $3$-space where $f(x, y)$ lives? I feel like I'm missing some geometric connection that justifies calling both by the name "line integral."










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    1












    $begingroup$


    Is there a connection between line integrals over scalar fields and line integrals over vector fields? For example, do the pair $f(x, y)$ and $F(x, y)$ which stand in a potential function and gradient relationship have the same line integral for any specified curve, when $F(x, y)$ is drawn in the $xy$-plane of the $3$-space where $f(x, y)$ lives? I feel like I'm missing some geometric connection that justifies calling both by the name "line integral."










    share|cite|improve this question









    $endgroup$















      1












      1








      1





      $begingroup$


      Is there a connection between line integrals over scalar fields and line integrals over vector fields? For example, do the pair $f(x, y)$ and $F(x, y)$ which stand in a potential function and gradient relationship have the same line integral for any specified curve, when $F(x, y)$ is drawn in the $xy$-plane of the $3$-space where $f(x, y)$ lives? I feel like I'm missing some geometric connection that justifies calling both by the name "line integral."










      share|cite|improve this question









      $endgroup$




      Is there a connection between line integrals over scalar fields and line integrals over vector fields? For example, do the pair $f(x, y)$ and $F(x, y)$ which stand in a potential function and gradient relationship have the same line integral for any specified curve, when $F(x, y)$ is drawn in the $xy$-plane of the $3$-space where $f(x, y)$ lives? I feel like I'm missing some geometric connection that justifies calling both by the name "line integral."







      calculus geometry multivariable-calculus definite-integrals line-integrals






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      asked Jan 3 at 17:17









      user10478user10478

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          2 Answers
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          $begingroup$

          Line integrals over scalar and vector fields have different physical interpretations. A line integral over a scalar field is like finding the area between the graph of the curve and the xy plane. A line integral over a vector field is interpreted as work.






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            same comment as above
            $endgroup$
            – G Cab
            Jan 3 at 20:26



















          0












          $begingroup$

          The scalar field $f(x,y)$ is a function $f:mathbb{R}^2 to mathbb{R}$ and can be thinked as the ''height'' of a surface over the $xy$ plane.
          Given a line $gamma(t)=(x(t),y(t))$ parametrized by $tin[a,b]$, the line integral of $f$ on this line is defined as
          $$
          int_gamma f(x,y)ds=int_a^b f(x(t),y(t)sqrt{left(frac{dx}{dt}right)^2+left(frac{dy}{dt}right)^2} dt
          $$

          (note that here the $ds$ is a length along the path $gamma$)



          This is essentially an extension to a ''curved coordinate'' of the usual integral of a real function of a real variable and represents the area between the surface $z=f(x,y)$ and the line $gamma$, as you can see intuitively in the nice animated figure in the wikipedia.



          The integral of a vector field $vec F(x,y)$ over $gamma$ is an entirely different thing.
          In this case $vec F(x,y)$ cannot be wieved as a surface, and the intuitive meaning of the integral is not an area but the work done by the force $vec F$ on the path $gamma$.



          In this case the integral is defined as
          $$
          int_gamma vec Fcdot dvec r = int_gamma left(F_x dx+F_ydyright)=int_a^b left(F_x(x(t),y(t))frac{dx}{dt}+F_y(x(t),y(t))frac{dy}{dt} right)dt
          $$

          (note that here $dvec r$ is a vector, and $F_x dx+F_ydy$ is a differential 1-form)



          If $vec F(x,y)$ is the gradient of the scalar field $f(x,y)$ than this means that $F_x dx+F_ydy$ is an exact form and we have:



          $$
          int_gamma vec Fcdot dvec r=f(b)-f(a)
          $$

          that is essentially a generalization of the fundamental theorem of calculus.






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
            $endgroup$
            – G Cab
            Jan 3 at 20:26











          Your Answer





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          2 Answers
          2






          active

          oldest

          votes








          2 Answers
          2






          active

          oldest

          votes









          active

          oldest

          votes






          active

          oldest

          votes









          0












          $begingroup$

          Line integrals over scalar and vector fields have different physical interpretations. A line integral over a scalar field is like finding the area between the graph of the curve and the xy plane. A line integral over a vector field is interpreted as work.






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            same comment as above
            $endgroup$
            – G Cab
            Jan 3 at 20:26
















          0












          $begingroup$

          Line integrals over scalar and vector fields have different physical interpretations. A line integral over a scalar field is like finding the area between the graph of the curve and the xy plane. A line integral over a vector field is interpreted as work.






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            same comment as above
            $endgroup$
            – G Cab
            Jan 3 at 20:26














          0












          0








          0





          $begingroup$

          Line integrals over scalar and vector fields have different physical interpretations. A line integral over a scalar field is like finding the area between the graph of the curve and the xy plane. A line integral over a vector field is interpreted as work.






          share|cite|improve this answer









          $endgroup$



          Line integrals over scalar and vector fields have different physical interpretations. A line integral over a scalar field is like finding the area between the graph of the curve and the xy plane. A line integral over a vector field is interpreted as work.







          share|cite|improve this answer












          share|cite|improve this answer



          share|cite|improve this answer










          answered Jan 3 at 19:59









          TimTim

          1




          1












          • $begingroup$
            same comment as above
            $endgroup$
            – G Cab
            Jan 3 at 20:26


















          • $begingroup$
            same comment as above
            $endgroup$
            – G Cab
            Jan 3 at 20:26
















          $begingroup$
          same comment as above
          $endgroup$
          – G Cab
          Jan 3 at 20:26




          $begingroup$
          same comment as above
          $endgroup$
          – G Cab
          Jan 3 at 20:26











          0












          $begingroup$

          The scalar field $f(x,y)$ is a function $f:mathbb{R}^2 to mathbb{R}$ and can be thinked as the ''height'' of a surface over the $xy$ plane.
          Given a line $gamma(t)=(x(t),y(t))$ parametrized by $tin[a,b]$, the line integral of $f$ on this line is defined as
          $$
          int_gamma f(x,y)ds=int_a^b f(x(t),y(t)sqrt{left(frac{dx}{dt}right)^2+left(frac{dy}{dt}right)^2} dt
          $$

          (note that here the $ds$ is a length along the path $gamma$)



          This is essentially an extension to a ''curved coordinate'' of the usual integral of a real function of a real variable and represents the area between the surface $z=f(x,y)$ and the line $gamma$, as you can see intuitively in the nice animated figure in the wikipedia.



          The integral of a vector field $vec F(x,y)$ over $gamma$ is an entirely different thing.
          In this case $vec F(x,y)$ cannot be wieved as a surface, and the intuitive meaning of the integral is not an area but the work done by the force $vec F$ on the path $gamma$.



          In this case the integral is defined as
          $$
          int_gamma vec Fcdot dvec r = int_gamma left(F_x dx+F_ydyright)=int_a^b left(F_x(x(t),y(t))frac{dx}{dt}+F_y(x(t),y(t))frac{dy}{dt} right)dt
          $$

          (note that here $dvec r$ is a vector, and $F_x dx+F_ydy$ is a differential 1-form)



          If $vec F(x,y)$ is the gradient of the scalar field $f(x,y)$ than this means that $F_x dx+F_ydy$ is an exact form and we have:



          $$
          int_gamma vec Fcdot dvec r=f(b)-f(a)
          $$

          that is essentially a generalization of the fundamental theorem of calculus.






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
            $endgroup$
            – G Cab
            Jan 3 at 20:26
















          0












          $begingroup$

          The scalar field $f(x,y)$ is a function $f:mathbb{R}^2 to mathbb{R}$ and can be thinked as the ''height'' of a surface over the $xy$ plane.
          Given a line $gamma(t)=(x(t),y(t))$ parametrized by $tin[a,b]$, the line integral of $f$ on this line is defined as
          $$
          int_gamma f(x,y)ds=int_a^b f(x(t),y(t)sqrt{left(frac{dx}{dt}right)^2+left(frac{dy}{dt}right)^2} dt
          $$

          (note that here the $ds$ is a length along the path $gamma$)



          This is essentially an extension to a ''curved coordinate'' of the usual integral of a real function of a real variable and represents the area between the surface $z=f(x,y)$ and the line $gamma$, as you can see intuitively in the nice animated figure in the wikipedia.



          The integral of a vector field $vec F(x,y)$ over $gamma$ is an entirely different thing.
          In this case $vec F(x,y)$ cannot be wieved as a surface, and the intuitive meaning of the integral is not an area but the work done by the force $vec F$ on the path $gamma$.



          In this case the integral is defined as
          $$
          int_gamma vec Fcdot dvec r = int_gamma left(F_x dx+F_ydyright)=int_a^b left(F_x(x(t),y(t))frac{dx}{dt}+F_y(x(t),y(t))frac{dy}{dt} right)dt
          $$

          (note that here $dvec r$ is a vector, and $F_x dx+F_ydy$ is a differential 1-form)



          If $vec F(x,y)$ is the gradient of the scalar field $f(x,y)$ than this means that $F_x dx+F_ydy$ is an exact form and we have:



          $$
          int_gamma vec Fcdot dvec r=f(b)-f(a)
          $$

          that is essentially a generalization of the fundamental theorem of calculus.






          share|cite|improve this answer









          $endgroup$













          • $begingroup$
            not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
            $endgroup$
            – G Cab
            Jan 3 at 20:26














          0












          0








          0





          $begingroup$

          The scalar field $f(x,y)$ is a function $f:mathbb{R}^2 to mathbb{R}$ and can be thinked as the ''height'' of a surface over the $xy$ plane.
          Given a line $gamma(t)=(x(t),y(t))$ parametrized by $tin[a,b]$, the line integral of $f$ on this line is defined as
          $$
          int_gamma f(x,y)ds=int_a^b f(x(t),y(t)sqrt{left(frac{dx}{dt}right)^2+left(frac{dy}{dt}right)^2} dt
          $$

          (note that here the $ds$ is a length along the path $gamma$)



          This is essentially an extension to a ''curved coordinate'' of the usual integral of a real function of a real variable and represents the area between the surface $z=f(x,y)$ and the line $gamma$, as you can see intuitively in the nice animated figure in the wikipedia.



          The integral of a vector field $vec F(x,y)$ over $gamma$ is an entirely different thing.
          In this case $vec F(x,y)$ cannot be wieved as a surface, and the intuitive meaning of the integral is not an area but the work done by the force $vec F$ on the path $gamma$.



          In this case the integral is defined as
          $$
          int_gamma vec Fcdot dvec r = int_gamma left(F_x dx+F_ydyright)=int_a^b left(F_x(x(t),y(t))frac{dx}{dt}+F_y(x(t),y(t))frac{dy}{dt} right)dt
          $$

          (note that here $dvec r$ is a vector, and $F_x dx+F_ydy$ is a differential 1-form)



          If $vec F(x,y)$ is the gradient of the scalar field $f(x,y)$ than this means that $F_x dx+F_ydy$ is an exact form and we have:



          $$
          int_gamma vec Fcdot dvec r=f(b)-f(a)
          $$

          that is essentially a generalization of the fundamental theorem of calculus.






          share|cite|improve this answer









          $endgroup$



          The scalar field $f(x,y)$ is a function $f:mathbb{R}^2 to mathbb{R}$ and can be thinked as the ''height'' of a surface over the $xy$ plane.
          Given a line $gamma(t)=(x(t),y(t))$ parametrized by $tin[a,b]$, the line integral of $f$ on this line is defined as
          $$
          int_gamma f(x,y)ds=int_a^b f(x(t),y(t)sqrt{left(frac{dx}{dt}right)^2+left(frac{dy}{dt}right)^2} dt
          $$

          (note that here the $ds$ is a length along the path $gamma$)



          This is essentially an extension to a ''curved coordinate'' of the usual integral of a real function of a real variable and represents the area between the surface $z=f(x,y)$ and the line $gamma$, as you can see intuitively in the nice animated figure in the wikipedia.



          The integral of a vector field $vec F(x,y)$ over $gamma$ is an entirely different thing.
          In this case $vec F(x,y)$ cannot be wieved as a surface, and the intuitive meaning of the integral is not an area but the work done by the force $vec F$ on the path $gamma$.



          In this case the integral is defined as
          $$
          int_gamma vec Fcdot dvec r = int_gamma left(F_x dx+F_ydyright)=int_a^b left(F_x(x(t),y(t))frac{dx}{dt}+F_y(x(t),y(t))frac{dy}{dt} right)dt
          $$

          (note that here $dvec r$ is a vector, and $F_x dx+F_ydy$ is a differential 1-form)



          If $vec F(x,y)$ is the gradient of the scalar field $f(x,y)$ than this means that $F_x dx+F_ydy$ is an exact form and we have:



          $$
          int_gamma vec Fcdot dvec r=f(b)-f(a)
          $$

          that is essentially a generalization of the fundamental theorem of calculus.







          share|cite|improve this answer












          share|cite|improve this answer



          share|cite|improve this answer










          answered Jan 3 at 20:11









          Emilio NovatiEmilio Novati

          52.2k43474




          52.2k43474












          • $begingroup$
            not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
            $endgroup$
            – G Cab
            Jan 3 at 20:26


















          • $begingroup$
            not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
            $endgroup$
            – G Cab
            Jan 3 at 20:26
















          $begingroup$
          not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
          $endgroup$
          – G Cab
          Jan 3 at 20:26




          $begingroup$
          not only work ! it could be for instance the resultant force on a wire subject to distributed load (pressures)
          $endgroup$
          – G Cab
          Jan 3 at 20:26


















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