Divergence in non cartesian coordinates
$begingroup$
Suppose I have some vector field $X$ in $mathbb{R^3}$ and a submanifold $M$ such that $dim(M)=2$. I want to calculate the flux of $X$ through $M$, $Phi_X(M)$. I would have two ways to do it, either go by the definition of flux or use the divergence theorem:
$$Phi_X(M)=int_Vdiv(X)dV$$
where $V$ is the solid enclosed by $M$. Now, suppose that $M$ is some kind of quadric surface so that the use of a parametrization, $psi$, would the make the integration much easier (Polar, spherical, etc.). If $X$ is given in the cartesian coordinate system along with the euclidean metric then the divergence of $X$ is straightforward, but if I'm using a parametrization $psi$ for $V$ then I would practically be using a different coordinate system because $dim V=3$, and so in that case, the divergence of $X$ would not be so straightforward as can be seen in this question and answer:Divergence in curvilinear coordinates. However I know very little (nothing actually) of covariance, contravariance and tensors, and this answer is only strict to orthogonal coordinate systems, and I'm wondering what other options are there to compute the flux by the divergence theorem and not calculate the divergence in a separate coordinate systems.
For example, if I have $M={(x,y,z)in mathbb{R^3}: z=x^2+y^2, 0leq zleq 1}$ and the vector field $X:mathbb{R^3} to mathbb{R^{3times 1}}, (x,y,z)to begin{bmatrix} xz \ z \ -frac{z}{2}end{bmatrix}$. Then the euclidean divergence of $X$ is $div (X)=z-1/2$. Using $psi$ as a parametrization of $V$, such that $psi=begin{bmatrix} psi^1 \ psi^2 \ psi^3end{bmatrix}$, would the flux be:
$$Phi_X(M)=int_{psi^{-1}(V)}bigg(psi^3-frac{1}{2}bigg)dV$$
such that $dV=sqrt{det(G(psi;(x,y,z)))}dpsi^1dpsi^2dpsi^3$, where $G(psi;(x,y,z))$ is the gram matrix of $psi$ at $(x,y,z)$?
differential-geometry divergence
$endgroup$
add a comment |
$begingroup$
Suppose I have some vector field $X$ in $mathbb{R^3}$ and a submanifold $M$ such that $dim(M)=2$. I want to calculate the flux of $X$ through $M$, $Phi_X(M)$. I would have two ways to do it, either go by the definition of flux or use the divergence theorem:
$$Phi_X(M)=int_Vdiv(X)dV$$
where $V$ is the solid enclosed by $M$. Now, suppose that $M$ is some kind of quadric surface so that the use of a parametrization, $psi$, would the make the integration much easier (Polar, spherical, etc.). If $X$ is given in the cartesian coordinate system along with the euclidean metric then the divergence of $X$ is straightforward, but if I'm using a parametrization $psi$ for $V$ then I would practically be using a different coordinate system because $dim V=3$, and so in that case, the divergence of $X$ would not be so straightforward as can be seen in this question and answer:Divergence in curvilinear coordinates. However I know very little (nothing actually) of covariance, contravariance and tensors, and this answer is only strict to orthogonal coordinate systems, and I'm wondering what other options are there to compute the flux by the divergence theorem and not calculate the divergence in a separate coordinate systems.
For example, if I have $M={(x,y,z)in mathbb{R^3}: z=x^2+y^2, 0leq zleq 1}$ and the vector field $X:mathbb{R^3} to mathbb{R^{3times 1}}, (x,y,z)to begin{bmatrix} xz \ z \ -frac{z}{2}end{bmatrix}$. Then the euclidean divergence of $X$ is $div (X)=z-1/2$. Using $psi$ as a parametrization of $V$, such that $psi=begin{bmatrix} psi^1 \ psi^2 \ psi^3end{bmatrix}$, would the flux be:
$$Phi_X(M)=int_{psi^{-1}(V)}bigg(psi^3-frac{1}{2}bigg)dV$$
such that $dV=sqrt{det(G(psi;(x,y,z)))}dpsi^1dpsi^2dpsi^3$, where $G(psi;(x,y,z))$ is the gram matrix of $psi$ at $(x,y,z)$?
differential-geometry divergence
$endgroup$
add a comment |
$begingroup$
Suppose I have some vector field $X$ in $mathbb{R^3}$ and a submanifold $M$ such that $dim(M)=2$. I want to calculate the flux of $X$ through $M$, $Phi_X(M)$. I would have two ways to do it, either go by the definition of flux or use the divergence theorem:
$$Phi_X(M)=int_Vdiv(X)dV$$
where $V$ is the solid enclosed by $M$. Now, suppose that $M$ is some kind of quadric surface so that the use of a parametrization, $psi$, would the make the integration much easier (Polar, spherical, etc.). If $X$ is given in the cartesian coordinate system along with the euclidean metric then the divergence of $X$ is straightforward, but if I'm using a parametrization $psi$ for $V$ then I would practically be using a different coordinate system because $dim V=3$, and so in that case, the divergence of $X$ would not be so straightforward as can be seen in this question and answer:Divergence in curvilinear coordinates. However I know very little (nothing actually) of covariance, contravariance and tensors, and this answer is only strict to orthogonal coordinate systems, and I'm wondering what other options are there to compute the flux by the divergence theorem and not calculate the divergence in a separate coordinate systems.
For example, if I have $M={(x,y,z)in mathbb{R^3}: z=x^2+y^2, 0leq zleq 1}$ and the vector field $X:mathbb{R^3} to mathbb{R^{3times 1}}, (x,y,z)to begin{bmatrix} xz \ z \ -frac{z}{2}end{bmatrix}$. Then the euclidean divergence of $X$ is $div (X)=z-1/2$. Using $psi$ as a parametrization of $V$, such that $psi=begin{bmatrix} psi^1 \ psi^2 \ psi^3end{bmatrix}$, would the flux be:
$$Phi_X(M)=int_{psi^{-1}(V)}bigg(psi^3-frac{1}{2}bigg)dV$$
such that $dV=sqrt{det(G(psi;(x,y,z)))}dpsi^1dpsi^2dpsi^3$, where $G(psi;(x,y,z))$ is the gram matrix of $psi$ at $(x,y,z)$?
differential-geometry divergence
$endgroup$
Suppose I have some vector field $X$ in $mathbb{R^3}$ and a submanifold $M$ such that $dim(M)=2$. I want to calculate the flux of $X$ through $M$, $Phi_X(M)$. I would have two ways to do it, either go by the definition of flux or use the divergence theorem:
$$Phi_X(M)=int_Vdiv(X)dV$$
where $V$ is the solid enclosed by $M$. Now, suppose that $M$ is some kind of quadric surface so that the use of a parametrization, $psi$, would the make the integration much easier (Polar, spherical, etc.). If $X$ is given in the cartesian coordinate system along with the euclidean metric then the divergence of $X$ is straightforward, but if I'm using a parametrization $psi$ for $V$ then I would practically be using a different coordinate system because $dim V=3$, and so in that case, the divergence of $X$ would not be so straightforward as can be seen in this question and answer:Divergence in curvilinear coordinates. However I know very little (nothing actually) of covariance, contravariance and tensors, and this answer is only strict to orthogonal coordinate systems, and I'm wondering what other options are there to compute the flux by the divergence theorem and not calculate the divergence in a separate coordinate systems.
For example, if I have $M={(x,y,z)in mathbb{R^3}: z=x^2+y^2, 0leq zleq 1}$ and the vector field $X:mathbb{R^3} to mathbb{R^{3times 1}}, (x,y,z)to begin{bmatrix} xz \ z \ -frac{z}{2}end{bmatrix}$. Then the euclidean divergence of $X$ is $div (X)=z-1/2$. Using $psi$ as a parametrization of $V$, such that $psi=begin{bmatrix} psi^1 \ psi^2 \ psi^3end{bmatrix}$, would the flux be:
$$Phi_X(M)=int_{psi^{-1}(V)}bigg(psi^3-frac{1}{2}bigg)dV$$
such that $dV=sqrt{det(G(psi;(x,y,z)))}dpsi^1dpsi^2dpsi^3$, where $G(psi;(x,y,z))$ is the gram matrix of $psi$ at $(x,y,z)$?
differential-geometry divergence
differential-geometry divergence
edited Dec 20 '18 at 19:20
Bidon
asked Dec 20 '18 at 18:58
BidonBidon
1218
1218
add a comment |
add a comment |
0
active
oldest
votes
Your Answer
StackExchange.ifUsing("editor", function () {
return StackExchange.using("mathjaxEditing", function () {
StackExchange.MarkdownEditor.creationCallbacks.add(function (editor, postfix) {
StackExchange.mathjaxEditing.prepareWmdForMathJax(editor, postfix, [["$", "$"], ["\\(","\\)"]]);
});
});
}, "mathjax-editing");
StackExchange.ready(function() {
var channelOptions = {
tags: "".split(" "),
id: "69"
};
initTagRenderer("".split(" "), "".split(" "), channelOptions);
StackExchange.using("externalEditor", function() {
// Have to fire editor after snippets, if snippets enabled
if (StackExchange.settings.snippets.snippetsEnabled) {
StackExchange.using("snippets", function() {
createEditor();
});
}
else {
createEditor();
}
});
function createEditor() {
StackExchange.prepareEditor({
heartbeatType: 'answer',
autoActivateHeartbeat: false,
convertImagesToLinks: true,
noModals: true,
showLowRepImageUploadWarning: true,
reputationToPostImages: 10,
bindNavPrevention: true,
postfix: "",
imageUploader: {
brandingHtml: "Powered by u003ca class="icon-imgur-white" href="https://imgur.com/"u003eu003c/au003e",
contentPolicyHtml: "User contributions licensed under u003ca href="https://creativecommons.org/licenses/by-sa/3.0/"u003ecc by-sa 3.0 with attribution requiredu003c/au003e u003ca href="https://stackoverflow.com/legal/content-policy"u003e(content policy)u003c/au003e",
allowUrls: true
},
noCode: true, onDemand: true,
discardSelector: ".discard-answer"
,immediatelyShowMarkdownHelp:true
});
}
});
Sign up or log in
StackExchange.ready(function () {
StackExchange.helpers.onClickDraftSave('#login-link');
});
Sign up using Google
Sign up using Facebook
Sign up using Email and Password
Post as a guest
Required, but never shown
StackExchange.ready(
function () {
StackExchange.openid.initPostLogin('.new-post-login', 'https%3a%2f%2fmath.stackexchange.com%2fquestions%2f3047865%2fdivergence-in-non-cartesian-coordinates%23new-answer', 'question_page');
}
);
Post as a guest
Required, but never shown
0
active
oldest
votes
0
active
oldest
votes
active
oldest
votes
active
oldest
votes
Thanks for contributing an answer to Mathematics Stack Exchange!
- Please be sure to answer the question. Provide details and share your research!
But avoid …
- Asking for help, clarification, or responding to other answers.
- Making statements based on opinion; back them up with references or personal experience.
Use MathJax to format equations. MathJax reference.
To learn more, see our tips on writing great answers.
Sign up or log in
StackExchange.ready(function () {
StackExchange.helpers.onClickDraftSave('#login-link');
});
Sign up using Google
Sign up using Facebook
Sign up using Email and Password
Post as a guest
Required, but never shown
StackExchange.ready(
function () {
StackExchange.openid.initPostLogin('.new-post-login', 'https%3a%2f%2fmath.stackexchange.com%2fquestions%2f3047865%2fdivergence-in-non-cartesian-coordinates%23new-answer', 'question_page');
}
);
Post as a guest
Required, but never shown
Sign up or log in
StackExchange.ready(function () {
StackExchange.helpers.onClickDraftSave('#login-link');
});
Sign up using Google
Sign up using Facebook
Sign up using Email and Password
Post as a guest
Required, but never shown
Sign up or log in
StackExchange.ready(function () {
StackExchange.helpers.onClickDraftSave('#login-link');
});
Sign up using Google
Sign up using Facebook
Sign up using Email and Password
Post as a guest
Required, but never shown
Sign up or log in
StackExchange.ready(function () {
StackExchange.helpers.onClickDraftSave('#login-link');
});
Sign up using Google
Sign up using Facebook
Sign up using Email and Password
Sign up using Google
Sign up using Facebook
Sign up using Email and Password
Post as a guest
Required, but never shown
Required, but never shown
Required, but never shown
Required, but never shown
Required, but never shown
Required, but never shown
Required, but never shown
Required, but never shown
Required, but never shown