Given a particle of mass m and position vector r,
the second law states that the force F acting on the particle
is equal to the time derivative of the momentum p of the particle:
F=dtdpā
If the mass of the particle is constant, then the second law can be written
in terms of the acceleration a of the particle:
Given a frame of reference S and another frame of reference Sā² moving
with equation of motion s=s(t) with respect to S,
and rotation with respect to S with orthogonal matrix O(t),
the transformation of the position vector rā² in Sā² to r in S is given by:
r=O(t)rā²+s(t)
And the transformation of the force Fā² in Sā² to F in S is given by:
F=O(t)Fā²
Assume in S, the second law holds, then in Sā²:
mrĀØ=OĀØrā²+2OĖrā²Ė+rā²ĀØO+sĀØ=Fī =O(t)Fā²
However, if O is a constant orthogonal matrix, and s
is a linear function of time, then the second law holds in Sā².
Such frames are called inertial frames.
And the corresponding transformation is called Galileo transformation.
Given a constant vector a,
if the net external force acting on the system is zero in the direction of a,
then the total momentum of the system in the direction of a is conserved:
Given a particle of mass m and position vector r,
and a force F acting on the particle,
the torque Ļ of the particle with respect to the origin is given by:
Ļ=rĆF
The torque represent the tendency of the force to rotate the particle.
Given a particle of mass m and position vector r,
and a force F acting on the particle,
the time derivative of the angular momentum L of the particle with respect to the origin is given by:
Given a constant vector a,
if the net external torque acting on the system is zero in the direction of a,
then the total angular momentum of the system in the direction of a is conserved:
Given two particles i and j with forces Fijā and Fjiā acting on them,
the third law states that the forces are equal in magnitude and opposite in direction:
The gravitational constant G is a fundamental constant in physics.
It is defined as the constant of proportionality in Newton's law of universal gravitation:
F=ār2Gm1ām2āār^
where F is the force between two point masses m1ā and m2ā separated by a distance r,
and r^ is the unit vector pointing from m1ā to m2ā.
The value of G is approximately 6.67430Ć10ā11m3kgā1sā2.
Given a particle of mass m near the surface of the Earth with acceleration due to gravity g,
the gravitational force Fgā acting on the particle is given by:
Fgā=āār2Gm1ām2āār^
where m1ā is the mass of the Earth, m2ā is the mass of the particle, and r is the distance between the particle and the center of the Earth.
As the particle is near the surface of the Earth, the distance r is approximately the radius of the Earth R. And the mass of the Earth is a constant m1ā=M.
Therefore, the gravitational force Fgā acting on the particle is given by:
Fgā=āR2GMmār^
where M is the mass of the Earth.
Given the acceleration due to gravity g=R2GMā, the gravitational force Fgā acting on the particle is given by:
Fgā=āmgr^
where g is the acceleration due to gravity.
The common value of g is approximately 9.81m/s2.
Given a moving object on a surface with coefficient of kinetic friction μkā,
and normal force R acting on the object,
the frictional force Fkā acting on the object is given by:
Given a force F acting on a particle,
if the force is conservative, then the force can be expressed as the gradient of a scalar function:
F=āāU
where U is the potential energy of the particle.
For conservative forces, on a simply connected domain (the domain is path connected and any closed curve can be shrunk to a point without leaving the domain),
the work done by the force F on the particle is path independent:
At point x1ā,
the particle has speed xĖ=0 and potential energy Vā²(x)<0.
Thus, the particle has to move to the right.
At point x2ā,
the particle has speed xĖ=0 and potential energy Vā²(x)>0.
Thus, the particle has to move to the left.
If the initial position of the particle is inside [x1ā,x2ā],
then the particle will oscillate between x1ā and x2ā.
As it can not go beyond x1ā and x2ā.
As when xāā, the potential energy V(x)ā0,
the speed of the particle xĖām2Eāā.
Given a particle of mass m and position vector r,
the work W done by a force F on the particle is equal to the change in kinetic energy T of the particle:
If we are working with some coordinate that are not Cartesian (e.g. Polar Coordinate),
we can use the Lagrangian mechanics to describe the motion of the system.
Given a system of particles with generalized coordinates qiā,
as the system evolves in time,
which means the generalized coordinates qiā are functions of time t,
we are also given qĖāiā.
The Lagrangian L of the system is given by:
L=TāU
where T is the kinetic energy of the system,
and U is the potential energy of the system,
and both are functions of the generalized coordinates qiā and their time derivatives qĖāiā and possibly time t.
Given a system of particles with generalized coordinates qiā,
if the Lagrangian L does not depend on a generalized coordinate qiā,
then the generalized coordinate qiā is called a cyclical coordinate.
If the Lagrangian L does not depend on a cyclical coordinate qiā,
then the momentum āqĖāiāāLā is conserved.
Which means āqĖāiāāLā is a constant.
Given a particle of mass m moving in a plane with polar coordinates (r,Īø),
with potential energy U(r) that depends only on the distance r from the origin,
As, the potential is independent of the angle Īø,
the force acting on the particle is radial.
The Lagrangian L of the particle is given by:
L=21ām(rĖ2+r2ĪøĖ2)āU(r)
The Euler-Lagrange equation for the angular coordinate Īø is given by:
The energy of the particle is conserved.
And we usually call E the total energy of the particle.
And also the effective potential:
Ueffā(r)=U(r)+2mr2J2ā
If we are give the effective potential Ueffā(r),
the energy and angular momentum of the particle,
then the equation of motion of the particle can be determined by solving two
first order ODEs:
Given a system of particles with generalized coordinates qiā,
if the generalized coordinates qiā are subject to constraints f(q1ā,ā¦,qiā,t)=0,
then the constraints are called holonomic constraints.
Any constraints that can not be expressed in the form f(q1ā,ā¦,qiā,t)=0 are called non-holonomic constraints.
Example: Object with air resistance is a non-holonomic constraint, as the air resistance is independent of the speed of the object.
Given a system of particles with generalized coordinates qiā,
if the constraints fjā(qiā,t)=0 are independent of the time t,
then the constraints are called unforced or natural constraints.
Example: A particle moving on a sphere of radius R.
Given a system of particles with generalized coordinates qiā,
if the constraints fjā(qiā,t)=0 are dependent of the time t,
then the constraints are called forced constraints.
Example: A particle moving on a sphere of radius R with the sphere rotating.
Example: A pendulum with the suspension point moving.
Given a system of particles with masses miā and position vectors riā,
the total angular momentum L of the system with respect to the origin is given by:
Given a system of particles with masses miā and position vectors riā,
and the total mass of the system M,
the total kinetic energy T of the system is given by:
Given a system of particles with masses miā and position vectors riā,
and the total mass of the system M,
the total potential energy U of the system is given by:
Uā=iāāUiā=iāāUiā(riā)āā
If the potential energy U is separable, that is, the potential energy can be expressed as:
U=URā(R)+iāāUiā(riā)
Then the generalised coordinates qiā can be reformulated
using the center of mass R and the relative coordinates riāāR.
And the Lagrangian L can be expressed in terms of the center of mass R and the relative coordinates riāāR.
Example: A constant gravitational field acting on a system of particles is a separable potential energy. And the total potential energy U of the system is given by: U=URā(R), which only depend on the center of mass R.
A rigid body is a system of particles with fixed relative distances between the particles.
For rigid body, we use R to denote the position of the center of mass of the rigid body,
and Ļiā=(Ļiā,Ļiā) in polar coordinates to denote the position of the i-th particle with respect to the center of mass.
As, the relative distances between the particles are fixed,
Ļiā is a constant of time.
And also, the angular velocity ĻĖāiā is the same for all particles,
in convention, we use ĻĖāiā=Ļ to denote the angular velocity of the rigid body.
Given a rigid body with mass M and position vector R,
and the i-th particle with mass miā and position vector Ļiā,
the kinetic energy T of the rigid body is given by:
Given a cylinder of radius R and mass M rolling on an inclined plane with angle α,
the question can be simplified by considering the following system:
Where α is again the angle of the inclined plane,
Ļ is the rolling angle of the cylinder,
and R=(x,y) is the position of the center of mass of the cylinder.
As the cylinder is rolling on the plane with no sliding,
we can formulate the constraints as:
yxā=āRĻsin(α)=RĻcos(α)āā
Thus, the velocity of the center of mass of the cylinder is given by:
Thus, v is an eigenvector of the matrix Mā1K with eigenvalue Ļ2,
where Ļ is the angular frequency of the normal mode.
And, c(t) is a solution of the following ODE:
cĀØ+Ļ2c=0
Thus, the general solution of the normal mode is given by:
Given a system of particles with generalized coordinates qiā,
and the Lagrangian L of the system,
the generalised momentum piā of the system is given by:
piā=āqĖāiāāLā
And we can solve this implicit equation to get qĖāiā in terms of qiā and piā.
Given a system of particles with generalized coordinates qiā,
if the potential energy is independent of qĖā,
and the kinetic energy T of the system is quadratic in the generalized velocities qĖāiā, which means there is a positive definite symmetric matrix M=M(q,t) such that:
As the Hamiltonian H does not depend on the generalized coordinate Ļ,
the generalized coordinate Ļ is a cyclical coordinate.
And the momentum pĻā is a constant.
Thus,
dpĻādHāmz2pĻāāā=ĻĖā=ĻĖāāā
For z coordinate,
dpzādHā2mpzāāā=zĖ=zĖāā
If we are given the initial energy of the particle E,
then the Hamiltonian H of the particle is given by:
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
the phase space Ī of the system is the space of generalized coordinates qiā and momenta piā.
The phase space of the system is a 2n dimensional space,
where n is the number of generalized coordinates qiā.
The trajectory of the system together with the change of the momentum of the system,
generate a path in t in the phase space of the system, and the Hamiltonian canonical equations describe the flow of the system in the phase space.
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
the volume of the phase space of the system is conserved.
In other words,
the Hamiltonian flow of the system is incompressible.
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
the phase space portrait of the system is the plot of the trajectory of the system in the phase space of the system.
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
the Poisson bracket of two functions f and g of the phase space of the system is given by:
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
the Poisson bracket of two functions f and g of the phase space of the system has the following properties:
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
the fundamental Poisson brackets of the system are given by:
Given a system of particles with generalized coordinates qiā,
and the Hamiltonian H of the system,
and a function f of the phase space of the system,
then time derivative of the function f is given by:
dtdfāā={f,H}+ātāfāāā
Thus, if the function f is independent of time,
then the function f is a constant of motion.