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Physics · Ch 5 — Gravitation

Projection of Satellite

5.8.1

Projection of Satellite

Launching an artificial satellite into a stable orbit requires giving it a very specific COMBINATION of speed and direction -- something a single-stage rocket cannot achieve, which is why a minimum of a TWO-stage rocket is always used. When the first stage's fuel is ignited at the Earth's surface, it lifts the satellite VERTICALLY, straight upward, imparting a vertical velocity of projection. If this vertical (upward) velocity is less than the escape velocity vev_e, the satellite would simply fall back to the Earth if released with only this vertical motion; equalling or exceeding vev_e in the purely vertical direction would instead send it escaping outward to infinity -- neither of which gives a satellite that ORBITS the Earth. This is precisely why a single-stage vertical launch alone can never place a satellite into orbit.

Instead, once the first rocket stage has carried the payload to the desired height, the launcher is reoriented through 90 degrees (using remote control) into the HORIZONTAL direction, the first stage is detached, and a second rocket stage then imparts a specific HORIZONTAL velocity vhv_h to the satellite, so that it can circle the Earth rather than simply falling back or flying off. The precise horizontal velocity of projection, at a given height, needed to make the satellite move in a stable CIRCULAR orbit at that height is called the critical velocity or orbital velocity, vcv_c.

For a satellite of mass m orbiting at height h (so its orbital radius is R+hR+h), the necessary centripetal force for its circular motion is supplied entirely by the Earth's gravitational pull on it: Centripetal force=Gravitational force⟹mvc2R+h=GMm(R+h)2.\text{Centripetal force}=\text{Gravitational force}\quad\Longrightarrow\quad\dfrac{mv_c^2}{R+h}=\dfrac{GMm}{(R+h)^2}. Cancelling m and one factor of (R+h)(R+h) from both sides gives vc2=GMR+h⟹vc=GMR+h=gh(R+h),v_c^2=\dfrac{GM}{R+h}\quad\Longrightarrow\quad v_c=\sqrt{\dfrac{GM}{R+h}}=\sqrt{g_h(R+h)}, where ghg_h is the acceleration due to gravity at that height. This critical speed depends only on the mass of the Earth and the height of the orbit (or, equivalently, the local gravitational acceleration there) -- it is completely INDEPENDENT of the satellite's own mass, and it DECREASES as the orbital height increases (a higher orbit needs a smaller circular speed).

A special case worth remembering: for a satellite orbiting very close to the Earth's surface, h≪Rh\ll R so R+h≈RR+h\approx R, giving vc≈GM/R=gR≈7.92v_c\approx\sqrt{GM/R}=\sqrt{gR}\approx7.92 km/s -- the MAXIMUM possible critical speed for any Earth-orbiting satellite, and, notably, at least 25 times faster than the fastest passenger aircraft. …

Figure 5.10Fig. 5.10: Various possible orbits of a satellite depending on the value of $v_h$

What this figure shows. A circle representing the Earth, with a satellite launch/injection point marked on a horizontal tangent line above the surface (the point where the vertical boost from the first rocket stage ends and a horizontal velocity vhv_h is imparted). From this single point, FIVE distinct trajectory curves fan out, each labelled by case: (I) vh<vcv_h<v_c -- an ELLIPSE with the injection point as the farthest point (apogee) from Earth, curving back in toward Earth on the far side; (II) vh=vcv_h=v_c -- a closed CIRCLE centred on the Earth's centre, passing through the injection point at constant radius; (III) vc<vh<vev_c<v_h<v_e -- a larger ELLIPSE with the injection point now as the nearest point (perigee), swinging far out before returning; (IV) vh=vev_h=v_e -- an open PARABOLA that never returns, escaping to infinity with zero final speed; (V) vh>vev_h>v_e -- an open HYPERBOLA, escaping to infinity with nonzero speed remaining, curving away most sharply of all five paths. The Earth sits inside the closed curves (ellipses, cir …

Misc Ex.9Example 5.9: Critical velocity of a satellite orbiting close to a planet's surface, in terms of mean density

Worked out. For a satellite orbiting very close to a planet's surface (h=0, so vc=GM/Rv_c=\sqrt{GM/R}), substituting the planet's mass in terms of its mean density ρ\rho and radius R via M=43πR3ρM=\frac{4}{3}\pi R^3\rho gives vc=43πGρR2=R4πGρ3v_c=\sqrt{\frac{4}{3}\pi G\rho R^2}=R\sqrt{\frac{4\pi G\rho}{3}}, i.e. the close-orbit critical speed depends only on the planet's radius and mean density, not on the satellite's own mass or on any external data about the planet's total mass. …