Portal:Electronics/Selected article/1: Difference between revisions

From formulasearchengine
Jump to navigation Jump to search
en>VolkovBot
 
en>P1ayer
No edit summary
 
Line 1: Line 1:
Hi there. Allow me start by introducing the writer, her title is Sophia. Since he was 18 he's been working as an information clairvoyant [http://www.herandkingscounty.com/content/information-and-facts-you-must-know-about-hobbies good psychic] - [http://kpupf.com/xe/talk/735373 http://kpupf.com], officer but he plans on altering it. Alaska is the only place I've been residing in but now I'm contemplating other choices. To play lacross is some thing he would by no means give up.<br><br>Also visit my webpage are psychics real ([http://m-card.co.kr/xe/mcard_2013_promote01/29877 Test by click the "Remove Empty Lines" button and watch these blank lines between this text disappear.])
{{Expert-subject|Physics|date=November 2008}}
 
In [[fluid dynamics]], the '''Kirchhoff equations''', named after [[Gustav Kirchhoff]], describe the motion of a [[rigid body]] in an [[ideal fluid]].
 
: <math>
\begin{align}
{d\over{dt}} {{\partial T}\over{\partial \vec \omega}}
& = {{\partial T}\over{\partial \vec \omega}} \times \vec \omega + {{\partial
T}\over{\partial \vec v}} \times \vec v + \vec Q_h + \vec Q, \\[10pt]
{d\over{dt}} {{\partial T}\over{\partial \vec v}}
& = {{\partial T}\over{\partial \vec v}} \times \vec \omega + \vec F_h + \vec F, \\[10pt]
T & = {1 \over 2} \left( \vec \omega^T \tilde I \vec \omega + m v^2 \right) \\[10pt]
\vec Q_h & =-\int p \vec x \times \hat n \, d\sigma, \\[10pt]
\vec F_h & =-\int p \hat n \, d\sigma
\end{align}
</math>
 
where <math>\vec \omega</math> and <math>\vec v</math> are the angular and linear velocity vectors at the point <math>\vec x</math>, respectively; <math>\tilde I</math> is the moment of inertia tensor, <math>m</math> is the body's mass; <math>\hat n</math> is
a unit normal to the surface of the body at the point <math>\vec x</math>;
<math>p</math> is a pressure at this point; <math>\vec Q_h</math> and <math>\vec F_h</math> are the hydrodynamic
torque and force acting on the body, respectively;
<math>\vec Q</math> and <math>\vec F</math> likewise denote all other torques and forces acting on the
body. The integration is performed over the fluid-exposed portion of the
body's surface.
 
If the body is completely submerged body in an infinitely large volume of irrotational, incompressible, inviscid fluid, that is at rest at infinity, then the vectors <math>\vec Q_h</math> and <math>\vec F_h</math> can be found via explicit integration, and the dynamics of the body is described by the [[Gustav Kirchhoff|Kirchhoff]] – [[Clebsch]] equations:
 
: <math>
{d\over{dt}}
{{\partial L}\over{\partial \vec \omega}} = {{\partial L}\over{\partial \vec \omega}} \times \vec \omega + {{\partial L}\over{\partial \vec v}} \times \vec v, \quad  {d\over{dt}}
{{\partial L}\over{\partial \vec v}} = {{\partial L}\over{\partial \vec v}} \times \vec \omega,
</math>
 
: <math>
L(\vec \omega, \vec v) = {1 \over 2} (A \vec \omega,\vec \omega) + (B \vec \omega,\vec v) + {1 \over 2} (C \vec v,\vec v) + (\vec k,\vec \omega) + (\vec l,\vec v).
</math>
 
Their first integrals read
 
: <math>
J_0 = \left({{\partial L}\over{\partial \vec \omega}}, \vec \omega \right) + \left({{\partial L}\over{\partial \vec v}}, \vec v \right) - L, \quad
J_1 = \left({{\partial L}\over{\partial \vec \omega}},{{\partial L}\over{\partial \vec v}}\right), \quad J_2 = \left({{\partial L}\over{\partial \vec v}},{{\partial L}\over{\partial \vec v}}\right)
</math>.
 
Further integration produces explicit expressions for position and velocities.  
 
== References ==
* Kirchhoff G. R. ''Vorlesungen ueber Mathematische Physik, Mechanik''. Lecture 19. Leipzig: Teubner. 1877.
* Lamb, H., ''Hydrodynamics''. Sixth Edition Cambridge (UK): Cambridge University Press. 1932.
 
[[Category:Mechanics]]
[[Category:Classical mechanics]]
[[Category:Rigid bodies]]
 
{{fluiddynamics-stub}}

Latest revision as of 12:09, 26 July 2013

Template:Expert-subject

In fluid dynamics, the Kirchhoff equations, named after Gustav Kirchhoff, describe the motion of a rigid body in an ideal fluid.

ddtTω=Tω×ω+Tv×v+Qh+Q,ddtTv=Tv×ω+Fh+F,T=12(ωTI~ω+mv2)Qh=px×n^dσ,Fh=pn^dσ

where ω and v are the angular and linear velocity vectors at the point x, respectively; I~ is the moment of inertia tensor, m is the body's mass; n^ is a unit normal to the surface of the body at the point x; p is a pressure at this point; Qh and Fh are the hydrodynamic torque and force acting on the body, respectively; Q and F likewise denote all other torques and forces acting on the body. The integration is performed over the fluid-exposed portion of the body's surface.

If the body is completely submerged body in an infinitely large volume of irrotational, incompressible, inviscid fluid, that is at rest at infinity, then the vectors Qh and Fh can be found via explicit integration, and the dynamics of the body is described by the KirchhoffClebsch equations:

ddtLω=Lω×ω+Lv×v,ddtLv=Lv×ω,
L(ω,v)=12(Aω,ω)+(Bω,v)+12(Cv,v)+(k,ω)+(l,v).

Their first integrals read

J0=(Lω,ω)+(Lv,v)L,J1=(Lω,Lv),J2=(Lv,Lv).

Further integration produces explicit expressions for position and velocities.

References

  • Kirchhoff G. R. Vorlesungen ueber Mathematische Physik, Mechanik. Lecture 19. Leipzig: Teubner. 1877.
  • Lamb, H., Hydrodynamics. Sixth Edition Cambridge (UK): Cambridge University Press. 1932.

Template:Fluiddynamics-stub