Lagrangian mechanics

Lagrangian mechanics is a re-formulation of classical mechanics that combines conservation of momentum with conservation of energy. It was introduced by Italian mathematician Lagrange in 1788. In Lagrangian mechanics, the trajectory of a system of particles is derived by solving Lagrange's equation, given herein, for each of the system's generalized coordinates. The fundamental lemma of calculus of variations shows that solving Lagrange's equation is equivalent to finding the path that minimizes the action functional, a quantity that is the integral of the Lagrangian over time.

The use of generalized coordinates may considerably simplify a system's analysis. For example, consider a small frictionless bead traveling in a groove. If one is tracking the bead as a particle, calculation of the motion of the bead using Newtonian mechanics would require solving for the time-varying constraint force required to keep the bead in the groove. For the same problem using Lagrangian mechanics, one looks at the path of the groove and chooses a set of "independent" generalized coordinates that completely characterize the possible motion of the bead. This choice eliminates the need for the constraint force to enter into the resultant system of equations. There are fewer equations since one is not directly calculating the influence of the groove on the bead at a given moment.

Lagrange's equations

The equations of motion in Lagrangian mechanics are "Lagrange's equations", also known as "Euler–Lagrange equations". Below, we sketch out the derivation of Lagrange's equation. Please note that in this context, V is used rather than U for potential energy and T replaces K for kinetic energy. See the references for more detailed and more general derivations.

Start with D'Alembert's principle for the virtual work of applied forces, mathbf{F}_i, and inertial forces on a three dimensional accelerating system of n particles, i, whose motion is consistent with its constraints:cite book |last=Torby |first=Bruce |title=Advanced Dynamics for Engineers |series=HRW Series in Mechanical Engineering |year=1984 |publisher=CBS College Publishing |location=United States of America |isbn=0-03-063366-4 |chapter=Energy Methods] rp|269

:delta W = sum_{i=1}^n ( mathbf {F}_{i} - m_i mathbf{a}_i )cdot delta mathbf r_i = 0.::delta W is the virtual work::delta mathbf r_i is the virtual displacement of the system, consistent with the constraints::m_i are the masses of the particles in the system::mathbf a_i are the accelerations of the particles in the system::m_i mathbf a_i together as products represent the time derivatives of the system momenta, aka. inertial forces::i is an integer used to indicate (via subscript) a variable corresponding to a particular particle::n is the number of particles under consideration

Break out the two terms:

:delta W = sum_{i=1}^n mathbf {F}_{i} cdot delta mathbf r_i - sum_{i=1}^n m_i mathbf{a}_i cdot delta mathbf r_i = 0.

Assume that the following transformation equations from m independent generalized coordinates, q_j, hold:rp|260

:mathbf{r}_1=mathbf{r}_1(q_1, q_2, ..., q_m, t),:mathbf{r}_2=mathbf{r}_2(q_1, q_2, ..., q_m, t), ...:mathbf{r}_n=mathbf{r}_n(q_1, q_2, ..., q_m, t).::m (without a subscript) indicates the total number generalized coordinates

An expression for the virtual displacement (differential), delta mathbf{r}_i, of the system isrp|264

:delta mathbf{r}_i = sum_{j=1}^m frac {partial mathbf {r}_i} {partial q_j} delta q_j.::j is an integer used to indicate (via subscript) a variable corresponding to a generalized coordinate

The applied forces may be expressed in the generalized coordinates as generalized forces, Q_j,rp|265

:Q_j = sum_{i=1}^n mathbf {F}_{i} cdot frac {partial mathbf {r}_i} {partial q_j}.

Combining the equations for delta W, delta mathbf{r}_i, and Q_j yields the following result after pulling the sum out of the dot product in the second term:rp|269

:delta W = sum_{j=1}^m Q_j delta q_j - sum_{j=1}^m sum_{i=1}^n m_i mathbf{a}_i cdot frac {partial mathbf {r}_i} {partial q_j} delta q_j = 0.

Substituting in the result from the kinetic energy relations to change the inertial forces into a function of the kinetic energy leavesrp|270

:delta W = sum_{j=1}^m Q_j delta q_j - sum_{j=1}^m left ( frac {d}{d t} left ( frac {partial T}{partial dot{q}_j} ight ) - frac {partial T}{partial q_j} ight ) delta q_j = 0.

In the above equation, delta q_j is arbitrary, though it is—by definition—consistent with the constraints. So the relation must hold term-wise:rp|270

:Q_j = frac {d}{d t} left ( frac {partial T}{partial dot{q}_j} ight ) - frac {partial T}{partial q_j}.

If the mathbf F_i are conservative, they may be represented by a scalar potential field, V:rp|266 & 270

mathbf F_i = - abla V Rightarrow Q_j = - sum_{i=1}^n abla V cdot frac {partial mathbf {r}_i} {partial q_j} = - frac {partial V}{partial q_j}.

The previous result may be easier to see by recognizing that V is a function of the mathbf {r}_i, which are in turn functions of q_j, and then applying the chain rule to the derivative of V with respect to q_j.

The definition of the Lagrangian isrp|270

:mathcal{L} = T - V.

Since the potential field is only a function of position, not velocity, Lagrange's equations are as follows:rp|270

:0 = frac {d}{d t} left ( frac {partial mathcal L}{partial dot{q}_j} ight ) - frac {partial mathcal L}{partial q_j}.

This is consistent with the results derived above and may be seen by differentiating the right side of the Lagrangian with respect to dot{q}_j and time, and solely with respect to q_j, adding the results and associating terms with the equations for mathbf F_i and Q_j .

In a more general formulation, the forces could be both potential and viscous. If an appropriate transformation can be found from the mathbf F_i, Rayleigh suggests using a dissipation function, D, of the following form:rp|271

:D = frac {1}{2} sum_{j=1}^m sum_{k=1}^m C_{j k} dot{q}_j dot{q}_k.::C_{j k} are constants that are related to the damping coefficients in the physical system, though not necessarily equal to them

If D is defined this way, thenrp|271

:Q_j = - frac {partial V}{partial q_j} - frac {partial D}{partial dot{q}_j} and:0 = frac {d}{d t} left ( frac {partial mathcal L}{partial dot{q}_j} ight ) - frac {partial mathcal L}{partial q_j} + frac {partial D}{partial dot{q}_j}.

Kinetic energy relations

The kinetic energy, T, for the system of particles is defined byrp|269

:T = frac {1}{2} sum_{i=1}^n m_i mathbf {v}_i cdot mathbf {v}_i.

The partial derivative of T with respect to the time derivatives of the generalized coordinates, dot{q}_j, isrp|269

:frac {partial T}{partial dot{q}_j} = sum_{i=1}^n m_i mathbf {v}_i cdot frac {partial mathbf {v}_i} {partial dot{q}_j}.

The previous result may be difficult to visualize. As a result of the product rule, the derivative of a general dot product frac{d}{dx} ( mathbf{f}(x) cdot mathbf{g}(x) ) is mathbf{f}(x) cdot frac{d}{dx} mathbf{g}(x) + mathbf{g}(x) cdot frac{d}{dx} mathbf{f}(x) This general result may be seen by briefly stepping into a Cartesian coordinate system, recognizing that the dot product is (there) a term-by-term product sum, and also recognizing that the derivative of a sum is the sum of its derivatives. In our case, f and g are equal to v, which is why the factor of one half disappears.

According to the chain rule and the coordinate transformation equations given above for mathbf{r}, its time derivative, mathbf{v}, is:rp|264

:mathbf{v}_i = sum_{k=1}^m frac {partial mathbf{r}_i}{partial q_k} dot{q}_k + frac {partial mathbf{r}_i}{partial t}.

Together, the definition of mathbf v_i and the total differential, d mathbf {r}_i, suggest thatrp|269

:frac {partial mathbf {v}_i}{partial dot{q}_j} = frac {partial mathbf {r}_i}{partial q_j}.

[ Remember that : frac {partial } {partial {dot{q}_k {A}{dot{q}_k} = A . Also remember that in the sum, there is only one {dot{q}_j} . ]

Substituting this relation back into the expression for the partial derivative of T givesrp|269

:frac {partial T}{partial dot{q}_j} = sum_{i=1}^n m_i mathbf v_i cdot frac {partial mathbf {r}_i}{partial q_j}.

Taking the time derivative givesrp|270

:frac {d}{d t} left ( frac {partial T}{partial dot{q}_j} ight ) = sum_{i=1}^n left [ m_i mathbf a_i cdot frac {partial mathbf {r}_i}{partial q_j} + m_i mathbf {v}_i cdot frac {d}{d t} left ( frac {partial mathbf {r}_i}{partial q_j} ight ) ight ] .

Using the chain rule on the last term givesrp|270

:frac {d}{d t} left ( frac {partial mathbf {r}_i}{partial q_j} ight ) = sum_{k=1}^m frac {partial^2 mathbf r_i}{partial q_j partial q_k} dot{q_k} + frac {partial^2 mathbf r_i}{partial q_j partial t}.

From the expression for mathbf v_i, one sees thatrp|270

:frac {d}{d t} left ( frac {partial mathbf {r}_i}{partial q_j} ight ) = frac {partial mathbf {v}_i}{partial q_j}.

This allows simplification of the last term,rp|270

:frac {d}{d t} left ( frac {partial T}{partial dot{q}_j} ight ) = sum_{i=1}^n left [ m_i mathbf a_i cdot frac {partial mathbf {r}_i}{partial q_j} + m_i mathbf {v}_i cdot frac {partial mathbf {v}_i}{partial q_j} ight ] .

The partial derivative of T with respect to the generalized coordinates, q_j, isrp|270

:frac {partial T}{partial q_j} = sum_{i=1}^n m_i mathbf {v}_i cdot frac {partial mathbf {v}_i} {partial q_j}.Clarifyme|date=March 2008

[This last result may be obtained by doing a partial differentiation directly on the kinetic energy definition represented by the first equation.] The last two equations may be combined to give an expression for the inertial forces in terms of the kinetic energy:rp|270

:frac {d}{d t} left ( frac {partial T}{partial dot{q}_j} ight ) - frac {partial T}{partial q_j} = sum_{i=1}^n m_i mathbf a_i cdot frac {partial mathbf {r}_i}{partial q_j}

Old Lagrange's equations

Consider a single particle with mass "m" and position vector old{r}, moving under an applied force, old{F}, which can be expressed as the gradient of a scalar potential energy function V (old{r},t):

:old{F} = - old{ abla} V.

Such a force is independent of third- or higher-order derivatives of old{r}, so Newton's second law forms a set of 3 second-order ordinary differential equations. Therefore, the motion of the particle can be completely described by 6 independent variables, or "degrees of freedom". An obvious set of variables is { old{r}_j, dot{old{r_j | j = 1, 2, 3}, the Cartesian components of old{r} and their time derivatives, at a given instant of time (i.e. position (x,y,z) and velocity (v_x,v_y,v_z)).

More generally, we can work with a set of generalized coordinates, q_j, and their time derivatives, the generalized velocities, dot{q_j}. The position vector, old{r}, is related to the generalized coordinates by some "transformation equation":

:old{r} = old{r}(q_i , q_j , q_k, t).

For example, for a simple pendulum of length "l", a logical choice for a generalized coordinate is the angle of the pendulum from vertical, θ, for which the transformation equation would be

:old{r}( heta, dot{ heta} , t) = (l sin heta, l cos heta).

The term "generalized coordinates" is really a holdover from the period when Cartesian coordinates were the default coordinate system.

Consider an arbitrary displacement delta old{r} of the particle. The work done by the applied force old{F} is W = old{F} cdot delta old{r}. Using Newton's second law, we write:

:egin{matrix} old{F} cdot delta old{r} = mddot{old{r cdot delta old{r}.end{matrix}

Since work is a physical scalar quantity, we should be able to rewrite this equation in terms of the generalized coordinates and velocities. On the left hand side,

: egin{matrix} old{F} cdot old{delta} old{r} & = & - old{ abla} V cdot displaystylesum_i {partial old{r} over partial q_i} delta q_i \ \ & = & - displaystylesum_{i,j} {partial V over partial r_j} {partial r_j over partial q_i} delta q_i \ \ & = & - displaystylesum_i {partial V over partial q_i} delta q_i. \ end{matrix}

On the right hand side, carrying out a change of coordinatesClarifyme|date=March 2008, we obtain:

m ddot{old{r cdot delta old{r} = m sum_{i,j} ddot{r_i} {partial r_i over partial q_j} delta q_j

Rearranging Slightly:

m ddot{old{r cdot delta old{r} = m sum_j left [ sum_i ddot{r_i} {partial r_i over partial q_j} ight] delta q_j

Now, by performing an "integration by parts" transformation, with respect to t:

m ddot{old{r cdot delta old{r} = m sum_j left [ sum_i left [ {mathrm{d} over mathrm{d}t} left( dot{r_i} {partial r_i over partial q_j} ight) - dot{r_i} {mathrm{d} over mathrm{d}t}left( {partial r_i over partial q_j} ight) ight] ight] delta q_j

Recognizing that {mathrm{d} over mathrm{d}t}{partial r_j over partial q_i} = {partial dot{r_j} over partial q_i} and {partial r_j over partial q_i} = {partial dot{r_j} over partial dot{q_i, we obtain:

m ddot{old{r cdot delta old{r} = m sum_j left [ sum_i left [ {mathrm{d} over mathrm{d}t} left( dot{r_i} {partial dot{r_i} over partial dot{q_j ight) - dot{r_i} {partial dot{r_i} over partial q_j} ight] ight] delta q_j

Now, by changing the order of differentiation, we obtain:

m ddot{old{r cdot delta old{r} = m sum_j left [ sum_i left [ {mathrm{d} over mathrm{d}t} {partial over partial dot{q_j left( frac{1}{2} dot{r_i}^2 ight) - {partial over partial q_j} left( frac{1}{2} dot{r_i}^2 ight) ight] ight] delta q_j

Finally, we change the order of summation:

m ddot{old{r cdot delta old{r} = sum_j left [ {mathrm{d} over mathrm{d}t} {partial over partial dot{q_j left( sum_i frac{1}{2} m dot{r_i}^2 ight) - {partial over partial q_j} left( sum_i frac{1}{2} m dot{r_i}^2 ight) ight] delta q_j

Which is equivalent to:

: m ddot{old{r cdot delta old{r}= sum_i left [{mathrm{d} over mathrm{d}t}{partial T over partial dot{q_i-{partial T over partial q_i} ight] delta q_i

where T=frac{1}{2}mdot{old{rcdotdot{old{r is the kinetic energy of the particle. Our equation for the work done becomes

:sum_i left [{mathrm{d} over mathrm{d}t}{partial{T}over partial{dot{q_i}-{partial{(T-V)}over partial q_i} ight] delta q_i = 0.

However, this must be true for "any" set of generalized displacements delta q_i, so we must have

:left [ {mathrm{d} over mathrm{d}t}{partial{T}over partial{dot{q_i}-{partial{(T-V)}over partial q_i} ight] = 0

for "each" generalized coordinate delta q_i. We can further simplify this by noting that "V" is a function solely of r and "t", and r is a function of the generalized coordinates and "t". Therefore, "V" is independent of the generalized velocities:

:{mathrm{d} over mathrm{d}t}{partial{V}over partial{dot{q_i} = 0.

Inserting this into the preceding equation and substituting "L" = "T" - "V", called the Lagrangian, we obtain Lagrange's equations:

:{partial{mathcal{Lover partial q_i} = {mathrm{d} over mathrm{d}t}{partial{mathcal{Lover partial{dot{q_i}.

There is one Lagrange equation for each generalized coordinate qi. When qi = ri (i.e. the generalized coordinates are simply the Cartesian coordinates), it is straightforward to check that Lagrange's equations reduce to Newton'ssecond law.

The above derivation can be generalized to a system of "N" particles. There will be 6"N" generalized coordinates, related to the position coordinates by 3"N" transformation equations. In each of the 3"N" Lagrange equations, "T" is the total kinetic energy ofthe system, and "V" the total potential energy.

In practice, it is often easier to solve a problem using the Euler–Lagrange equations than Newton's laws. This is because appropriate generalized coordinates "q"i may be chosen to exploit symmetries in the system.

Examples

In this section two examples are provided in which the above concepts are applied. The first example establishes that in a simple case, the Newtonian approach and the Lagrangian formalism agree. The second case illustrates the power of the above formalism, in a case which is hard to solve with Newton's laws.

Falling mass

Consider a point mass "m" falling freely from rest. By gravity a force "F = m g" is exerted on the mass (assuming "g" constant during the motion). Filling in the force in Newton's law, we find ddot x = g from which the solution:x(t) = frac{1}{2} g t^2 follows (choosing the origin at the starting point). This result can also be derived through the Lagrange formalism. Take "x" to be the coordinate, which is "0" at the starting point. The kinetic energy is T = frac{1}{2} m v^2 and the potential energy is V = - m g x, hence :mathcal{L} = T - V = frac{1}{2} m dot{x}^2 + m g x. Now we find:0 = frac{partial mathcal{L{partial x} - frac{mathrm{d{mathrm{d}t} frac{partial mathcal{L{partial dot x} = m g - m frac{mathrm{d} dot x}{mathrm{d} t} which can be rewritten as ddot x = g, yielding the same result as earlier.

Pendulum on a movable support

Consider a pendulum of mass "m" and length "l", which is attached to a support with mass "M" which can move along a line in the "x"-direction. Let "x" be the coordinate along the line of the support, and let us denote the position of the pendulum by the angle "θ" from the vertical. The kinetic energy can then be shown to be:T = frac{1}{2} M dot{x}^2 + frac{1}{2} m left( dot{x}_mathrm{pend}^2 + dot{y}_mathrm{pend}^2 ight) = frac{1}{2} M dot{x}^2 + frac{1}{2} m left [ left( dot x + l dot heta cos heta ight)^2 + left( l dot heta sin heta ight)^2 ight] , and the potential energy of the system is

: V = m g operatorname{y}_mathrm{pend} = - m g l cos heta .

Now carrying out the differentiations gives for the support coordinate "x":frac{mathrm{d{mathrm{d}t} left [ (M + m) dot x + m l dot heta cos heta ight] = 0, therefore:: (M + m) ddot x + m l ddot hetacos heta-m l dot heta ^2 sin heta = 0 indicating the presence of a constant of motion. The other variable yields:frac{mathrm{d{mathrm{d}t}left [ m( l^2 dot heta + dot x l cos heta ) ight] + m (dot x l dot heta + g l) sin heta = 0;therefore:ddot heta + frac{ddot x}{l} cos heta + frac{g}{l} sin heta = 0 .These equations may look quite complicated, but finding them with Newton's laws would have required carefully identifying all forces, which would have been much harder and prone to errors. By considering limit cases (ddot x o 0 should give the equations of motion for a pendulum, ddot heta o 0 should give the equations for a pendulum in a constantly accelerating system, etc.) the correctness of this system can be verified.

Hamilton's principle

The action, denoted by mathcal{S}, is the time integral of the Lagrangian::mathcal{S} = int mathcal{L},mathrm{d}t.

Let "q0" and "q1" be the coordinates at respective initial and final times "t0" and "t1". Using the calculus of variations, it can be shown the Lagrange's equations are equivalent to "Hamilton's principle":

:"The system undergoes the trajectory between t0 and t1 whose action has a stationary value."

By "stationary", we mean that the action does not vary to first-order for infinitesimal deformations of the trajectory, with the end-points ("q0", "t0") and ("q1","t1") fixed. Hamilton's principle can be written as:

:delta mathcal{S} = 0. ,!

Thus, instead of thinking about particles accelerating in response to applied forces, one might think of them picking out the path with a stationary action.

Hamilton's principle is sometimes referred to as the "principle of least action". However, this is a misnomer: the action only needs to be stationary, and the correct trajectory could be produced by a maximum, saddle point, or minimum in the action.

We can use this principle instead of Newton's Laws as the fundamental principle of mechanics, this allows us to use an integral principle (Newton's Laws are based on differential equations so they are a differential principle) as the basis for mechanics. However it is not widely stated that Hamilton's principle is a variational principle only with holonomic constraints, if we are dealing with nonholonomic systems then the variational principle should be replaced with one involving d'Alembert principle of virtual work. Working only with holonomic constraints is the price we have to pay for using an elegant variational formulation of mechanics.

Extensions of Lagrangian mechanics

The Hamiltonian, denoted by "H", is obtained by performing a Legendre transformation on the Lagrangian. The Hamiltonian is the basis for an alternative formulation of classical mechanics known as Hamiltonian mechanics. It is a particularly ubiquitous quantity in quantum mechanics (see Hamiltonian (quantum mechanics)).

In 1948, Feynman invented the path integral formulation extending the principle of least action to quantum mechanics for electrons and photons. In this formulation, particles travel every possible path between the initial and final states; the probability of a specific final state is obtained by summing over all possible trajectories leading to it. In the classical regime, the path integral formulation cleanly reproduces Hamilton's principle, and Fermat's principle in optics.

ee also

* Canonical coordinates
* Functional derivative
* Generalized coordinates
* Hamiltonian mechanics
* Lagrangian analysis (applications of Lagrangian mechanics)
* Nielsen form
* Restricted three-body problem

References

* Goldstein, H. "Classical Mechanics," second edition, pp.16 (Addison-Wesley, 1980)
* Moon, F. C. "Applied Dynamics With Applications to Multibody and Mechatronic Systems", pp. 103-168 (Wiley, 1998).

Further reading

* Landau, L.D. and Lifshitz, E.M. "Mechanics", Pergamon Press.
* Gupta, Kiran Chandra, "Classical mechanics of particles and rigid bodies" (Wiley, 1988).

External links

* Tong, David, [http://www.damtp.cam.ac.uk/user/tong/dynamics.html Classical Dynamics] Cambridge lecture notes
* [http://www.eftaylor.com/software/ActionApplets/LeastAction.html Principle of least action interactive] Excellent interactive explanation/webpage
* [http://ocw.mit.edu/NR/rdonlyres/Aeronautics-and-Astronautics/16-61Aerospace-DynamicsSpring2003/D453E02B-5218-4154-8531-DB35ECD76A6C/0/lecture9.pdf Aerospace dynamics lecture notes on Lagrangian mechanics]
* [http://ocw.mit.edu/NR/rdonlyres/Aeronautics-and-Astronautics/16-61Aerospace-DynamicsSpring2003/53F21B11-4F88-4870-967A-0C05AD85B104/0/lecture10.pdf Aerospace dynamics lecture notes on Rayleigh dissipation function]


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