These substitutions give a descent time t [the time interval between the parachute opening to the point where a speed of (1.01) v 2 is attained] of approximately 4.2 seconds, and a minimum altitude at which the parachute must be opened of y ≈ 55 meters (a little higher than 180 feet).
Simple harmonic motion. Consider a spring fastened to a wall, with a block attached to its free end at rest on an essentially frictionless horizontal table. The block can be set into motion by pulling or pushing it from its original position and then letting go, or by striking it (that is, by giving the block a nonzero initial velocity). The force exerted by the spring keeps the block oscillating on the tabletop. This is the prototypical example ofsimple harmonic motion.
The force exerted by a spring is given by Hooke's Law; this states that if a spring is stretched or compressed a distance x from its natural length, then it exerts a force given by the equation
The positive constant k is known as the spring constant and is directly realted to the spring's stiffness: The stiffer the spring, the larger the value of k. The minus sign implies that when the spring is stretched (so that x is positive), the spring pulls back (because F is negative), and conversely, when the spring is compressed (so that x is negative), the spring pushes outward (because F is positive). Therefore, the spring is said to exert arestoring force, since it always tries to restore the block to its equilibrium position (the position where the spring is neither stretched nor compressed). The restoring force here is proportional to the displacement ( F = −kx α x), and it is for this reason that the resulting periodic (regularly repeating) motion is called simple harmonic.
Newton's Second Law can be applied to this spring‐block system. Once the block is set into motion, the only horizontal force that acts on it is the restoring force of the spring. Therefore, the equation
This is a homogeneous second‐order linear equation with constant coefficients. The auxiliary polynomial equation is , which has distinct conjugate complex roots Therefore, the general solution of this differential equation is
This expression gives the displacement of the block from its equilibrium position (which is designated x = 0).
Example 2: A block of mass 1 kg is attached to a spring with force constant N/m. It is pulled 3/ 10 m from its equilibrium position and released from rest. Obtain an equation for its position at any time t; then determine how long it takes the block to complete one cycle (one round trip).
All that is required is to adapt equation (*) to the present situation. First, since the block is released from rest, its intial velocity is 0:
Since c 2 = 0, equation (*) reduces to Now, since x(0) = + 3/ 10m, the remaining parameter can be evaluated:
Finally, since and Therefore, the equation for the position of the block as a function of time is given by
where x is measured in meters from the equilibrium position of the block. This function is periodic, which means it repeats itself at regular intervals. The cosine and sine functions each have a period of 2π, which means every time the argument increases by 2π, the function returns to its previous value. (Recall that if, say, x = cosθ, then θ is called the argument of the cosine function.) The argument here is 5/ 2 t, and 5/ 2 t will increase by 2π every time t increases by 4/ 5π. Therefore, this block will complete one cycle, that is, return to its original position ( x = 3/ 10 m), every 4/5π ≈ 2.5 seconds.
The length of time required to complete one cycle (one round trip) is called the period of the motion (and denoted by T.) It can be shown in general that for the spring‐block oscillator,
Note that the period does not depend on where the block started, only on its mass and the stiffness of the spring. The maximum distance (greatest displacement) from equilibrium is called the amplitude of the motion. Therefore, it makes no difference whether the block oscillates with an amplitude of 2 cm or 10 cm; the period will be the same in either case. This is one of the defining characteristics of simple harmonic motion: the period is independent of the amplitude.
Another important characteristic of an oscillator is the number of cycles that can be completed per unit time; this is called the frequency of the motion [denoted traditionally by v (the Greek letter nu) but less confusingly by the letter f]. Since the period specifies the length of time per cycle, the number of cycles per unit time (the frequency) is simply the reciprocal of the period: f = 1/ T. Therefore, for the spring‐block simple harmonic oscillator,
Frequency is usually expressed in hertz (abbreviated Hz); 1 Hz equals 1 cycle per second.
The quantity √ k/ m (the coefficient of t in the argument of the sine and cosine in the general solution of the differential equation describing simple harmonic motion) appears so often in problems of this type that it is given its own name and symbol. It is called the angular frequency of the motion and denoted by ω (the Greek letter omega). Note that ω = 2π f.
Damped oscillations. The spring‐block oscillator is an idealized example of a frictionless system. In real life, however, frictional (or dissipative) forces must be taken into account, particularly if you want to model the behavior of the system over a long period of time. Unless the block slides back and forth on a frictionless table in a room evacuated of air, there will be resistance to the block's motion due to the air (just as there is for a falling sky diver). This resistance would be rather small, however, so you may want to picture the spring‐block apparatus submerged in a large container of clear oil. The viscosity of the oil will have a profound effect upon the block's oscillations. The air (or oil) provides a damping force, which is proportional to the velocity of the object. (Again, recall the sky diver falling with a parachute. At the relatively low speeds attained with an open parachute, the force due to air resistance was given as Kv, which is proportional to the velocity.)
With a restoring force given by − kx and a damping force given by − Kv (the minus sign means that the damping force opposes the velocity), Newton's Second Law ( F net = ma) becomes − kx − Kv = ma, or, since v = and a = ,
This second‐order linear differential equation with constant coefficients can be expressed in the more standard form
The auxiliary polynomial equation is mr 2 + Kr + k = 0, whose roots are
The system will exhibit periodic motion only if these roots are distinct conjugate complex numbers, because only then will the general solution of the differential equation involve the periodic functions sine and cosine. In order for this to be the case, the discriminant K 2 – 4 mk must be negative; that is, the damping constant K must be small; specifically, it must be less than 2 √ mk . When this happens, the motion is said to beunderdamped, because the damping is not so great as to prevent the system from oscillating; it just causes the amplitude of the oscillations to gradually die out. [If the damping constant K is too great, then the discriminant is nonnegative, the roots of the auxiliary polynomial equation are real (and negative), and the general solution of the differential equation involves only decaying exponentials. This implies there would be no sustained oscillations.]
In the underdamped case , the roots of the auxiliary polynomial equation can be written as
and consequently, the general solution of the defining differential equation is
Example 3: (Compare to Example 2.) A block of mass 1 kg is attached to a spring with force constant N/m. It is pulled 3/ 10m from its equilibrium position and released from rest. If this spring‐block apparatus is submerged in a viscous fluid medium which exerts a damping force of – 4 v (where v is the instantaneous velocity of the block), sketch the curve that describes the position of the block as a function of time.
The net force on the block is , so Newton's Second Law becomes
because m = 1. Since the roots of the auxiliary polynomial equation, , are
the general solution of the differential equation is
Because the block is released from rest, v(0) = (0) = 0:
This implies And, since ,
Therefore, and the equation that gives the position of the block as a function of time is
where x is measured in meters from the equilibrium position of the block.
This expression for the position function can be rewritten using the trigonometric identity cos(α – β) = cos α cos β + sin α sin β, as follows:
The phase angle, φ, is defined here by the equations cos φ = 3/ 5 and sin φ = 4/ 5, or, more briefly, as the first‐quadrant angle whose tangent is 4/ 3 (it's the larger acute angle in a 3–4–5 right triangle). The presence of the decaying exponential factor e −2 t in the equation for x( t) means that as time passes (that is, as t increases), the amplitude of the oscillations gradually dies out. See Figure .