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The capture radius $ r_c $ is below orbit apogee by some asyet undefined amount. The angular velocity will be $ \omega_T $ as before, so the transverse velocity will be $ \omega_T r_c $. The total velocity squared will be the sum of the squares: $ {v_{vc}}^2 + ( \omega_T r_c )^2 $.  The capture radius $ r_c $ is below orbit apogee by some asyet undefined amount. The angular velocity will be $ \omega_T $ as before, so the transverse velocity will be $ \omega_T r_c $. The total velocity squared will be the sum of the squares: $ {v_{vc}}^2 + ( \omega_T r_c )^2 $. 
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MORE LATER 
The capture rail is a long way out of the gravity well, so "natural" vertical deceleration of a vehicle is small. However, there will be some drag from eddy currents in the thin and rather resistive rail. In a production system, the drag profile will be optimized and rather complex. For this analysis, we will just compute the kinetic energy lost by moving up the rail, multiply that by a drag factor, and use that to compute the kinetic energy and velocity left as we approach the dock at GEO. The vertical deceleration is given by: $ acceleration = \omega^2 r  \mu / r^2 $ ` ` . . . zero at GEO, of course! and the specific energy ( J/kg ) can be computed by integrating that: $ E(r) = 0.5 \omega^2 r^2  \mu / r $ The drag factor is $ D $, and will always be greater than 1, so the velocity nearing GEO will be: $ v_{GEO} \approx \sqrt{ {v_{vc}}^2  2 D ( E_{GEO}  E_{capture} ) } $ The velocity at radius $ r $ will be: $ v(r) \approx \sqrt{ {v_{vc}}^2 + D \omega^2 ( r^2  {r_c}^2 )  2 D \mu ( 1 / r_c  1 / r ) } $ The transit time from the capture point to GEO will be: $ time = {\huge\int} _{r_c}^{GEO} { \Large { dr \over {v(r)} } } $ ` ` ... which probably requires numerical integration Since we want to keep the transit time small, we would like to keep the rail very straight and travel up it quickly. So we keep the drag and deceleration relatively low for most of the trip. As we approach GEO, however, we "hit the brakes", decelerating at a much higher rate, so we come quickly and smoothly to a stop at the dock. The transition from low to high deceleration occurs at the '''slowdown radius''' $ r_s $. Here's a closetominimum transit time capture: <4:> '''GEOrail Tether Capture'''   $ v_{vc} $  Vertical V  2700.0000  m/s   $ acc_s $  slowdown deceleration  5.0000  m/s^2^   $ D $  drag factor  2.0000    $ \mu $  gravitational parameter  3.9860E+14  m^3^/s^2^   $ \omega_T $  GEO angular frequency  7.2921151E05  radians/s   $ r_{GEO} $  GEO radius  42164172.37  m   $ v_{GEO} $  GEO velocity  3074.6600  m/s   $ E_{GEO} $  GEO energy / kg  14180301  J/Kg   $ H_{GEO} $  GEO angular momentum/kg  1.2964E+11  m^2^/s   $ r_p $  perigee radius  6458137.0  m   $ v_p $  perigee velocity  10462.7761  m/s   $ e $  eccentricity  0.77363    $ a $  semimajor axis  28529281.45  m   $ r_a $  apogee radius  50600425.91  m   $ v_a $  apogee velocity  1335.3651  m/s   $ \theta $  orbit angle at capture  143.73  degrees   $ r_c $  capture radius  30440398.47  m   $ v_{tc} $  capture tranverse velo.  2219.7489  m/s   $ E_c $  capture energy  15558098  J/kg   $ acc_c $  capture vert. accel.  0.2683  m/s^2^   $H_{capture}$ capture ang. momentum/kg 6.7570E+10  m^2^/s   $ y_s $  slowdown run  177982.60  m   $ r_s $  slowdown radius  41986189.77  m   $ v_s $  slowdown velocity  1334.10  s   $ t_s $  slowdown time  266.82  s    tether climb time  6604.70  s    Partial orbit time  18533.41  s    Launch time  348.76  s    Total time  7.15  hours   $ \Delta v $  velocity increase  854.9111  m/s   $ \Delta E $ radial energy increase/kg 1377796.89  J/kg   $ \Delta H $ radial ang. mom. incr./kg 6.2070E+10  m^2^/s   $ \Delta r $  radius increase  11723773.89  m  Here's a table of transit time versus versus vertical capture velocity. The capture velocity is quite sensitive to launch velocity, which must be controlled to mm/sec. Note that if we launch very fast, we spend a long time heading out and coming back to the tether. These are all "drag=2" times; if we reduce drag, the optimum occurs at a lower launch velocity. <4:>'''Transit time versus vertical tether velocity'''<4:> time, seconds  total   vertical  vp  a  rc launch  orbit  climb  slow  hours   3200.00  10615.08  37940037  30661158  354  24481  4330  446  8.23   3000.00  10551.38  32915772  30569017  352  21591  4991  381  7.59   2800.00  10491.37  29807595  30481967  350  19422  5934  308  7.23   2750.00  10476.96  29148708  30461018  349  18964  6245  288  7.18   2700.00  10462.78  28529281  30440398  349  18533  6605  267  7.15   2650.00  10488.83  27946160  30420112  348  18129  7028  244  7.15   2600.00  10435.13  27396521  30400159  348  17749  7542  220  7.18   2550.00  10421.67  26877836  30380544  347  17390  8193  193  7.26   2500.00  10408.45  26387830  30361268  347  17053  9075  162  7.40   2400.00  10382.74  25485852  30323743  346  16433  13467  70  8.42   MORE LATER 
GEO Rail
"Landing" Launch Loop payloads in a destination without rockets
Imagine a long and heavy orbiting tether, running vertically from 29900 km radius, through GEO (42164 km), to a counterweight above. The tether has a thin, passive conductive rail around it. It will be used to magnetically capture vehicles and move them to GEO, using the sliding rail to push payloads transversely while they magnetically slide upwards.
This is not the normal apogee capture system, where we launch into an orbit whose perigee transverse velocity matches a hanging tether at the right altitude. Instead, we launch the vehicle a little faster and a little later. That puts the vehicle in an orbit with an apogee trailing the tether. The vehicle will never get to that apogee, because we will slide in front of the tether below apogee, where we still have a high (1800 m/s) radial velocity. We will still match the tether's transverse velocity and altitude, though.
In the rotating tether frame of reference, the vehicle will approach from below at high speed, from the rear, and decelerate in the traverse ("horizontal") direction as it approaches the tether. The vehicle is rising radially, conserving angular momentum, and losing angular velocity as the radius increases. In the tether's rotating frame, this looks like Coriolis acceleration, equal to twice the velocity times the tether's angular velocity. The angular orbital velocity for a GEO tether is 7.2921E5 radians per second, and the radial ("vertical") velocity will be around 1800 meters per second, so the Coriolis acceleration is 0.26 m/s^{2}. If the vehicle misses the tether rendezvous, it will continue to accelerate retrograde in the rotating frame, with the backwards velocity turning into downwards Coriolis acceleration in the rotating frame, reaching apogee above the intended attach point but well below GEO.
The tether is made with notexcessivelytapered Kevlar. We will need many tons of it, especially at GEO, as an angular momentum bank. More mass is better for this system. THIS is where we put the hotels, the radiation shielding, and the heavy buffet tables for obese tourists.
We launch a vehicle off the launch loop at 10148.7 m/s, and with very good radar and some trim thrusters, we "land" on the bottom of the rail at 29979.7 km altitude. At that point, we have the same angular frequency and circular orbital velocity, and a large vertical velocity component, 1746.8 m/s .
As the vehicle slides up the tether, the weak gravity slows it down radially, as it accelerates forwards in orbit to remain on the "faster at higher altitude" tether.
As the vehicle slides upwards, it magnetically levitates/pushes against the east side of the rail with Coriolis acceleration. That is 26 centimeters per second squared at 1800 m/s vertically, and 7 centimeters per second squared at 400 m/s, our speed as we approach GEO altitude. The Coriolis acceleration and the eddy currents both reduce with relative velocity  most convenient! The vertical deceleration (gravity minus rotational centrifugal acceleration) decreases to zero as we approach GEO, still with significant velocity, though with less than the velocity of a frictionless ballistic because of the eddy currents.
As the vehicle approaches GEO, it is still moving fast, which is good, because it has 12000 kilometers to travel. The trip will take about 4 hours. About 10000 meters below GEO station, the rail surface changes to increase eddy current drag, slowing down the vehicle. The vehicle reaches the drag section at 400 meters per second, and deceleration increases from a few millimeters per second to 10 m/s^{2}, a bit more than 1 gee (with passengers facing backwards, backs into chairs). The vehicle slows to 25 meters per second about 40 meters below the station, and with the aid of some linear motors, reduces deceleration and velocity to zero over the next 5 seconds. The payload or passenger compartment is plucked off the magnetrail and wing, and pushed into the station through an airlock.
Since the tether rail is not magnetic or active (that would be far too heavy for a 12000 kilometer gossamer structure) the vehicle magnetrail will need to wrap partly around it in some way. 26 cm/s^{2} Coriolis acceleration is far too weak to hold the vehicle against a rippling tether at high speed. For example, a ripple with a 20 kilometer wavelength and a 20 meter peaktopeak amplitude will shake the vehicle back and forth at 0.3 gees ( 12x Coriolis ) and a period of 11 seconds  a mild roller coaster. Such a transverse ripple will not be a standing wave, but traveling up or down the tether at around 1 km per second. It will be a challenge to remove it, perhaps by periodic transverse shaking at GEO by the large momentum mass. It would be more difficult to remove by shaking the bottom counterweight vertically, inducing Coriolis accelerations, because a lot of power is required.
We can reverse the process. Using a magnetic accelerator to launch a vehicle down a rail on the west side of the tether, we falling off the end in a transfer orbit back to the upper atmosphere. This restores most of the GEO rail momentum.
The rocket thrust needed by GEO rail vehicles will be pure velocity correction, centimeters per second if we've done our radar and orbital mechanics calculations correctly. If we miss, we just reenter normally  a delay, but not a disaster. Besides a little correction exhaust, and whatever we need to add to for momentum restoration, the system is mass conservative and mostly energyrecycling.
More rockets bite the dust ...
Restoring GEO Rail orbital momentum
If we deorbit GEO station trash much faster than we receive payloads (aiming for empty and lifeless portions of the ocean) we can add more momentum by exploiting Coriolis force acceleration. We can also receive mass (and momentum) from the moon, or launch mass from the loop in slingshot orbits around the moon. However, the moon will not always be conveniently located for this, and vehicles may make many 20 day orbits before arriving with a suitable orbital position.
A slightly stronger tether can swing like a pendulum. That allows vehicles to arrive from the launch loop with higher angular velocity, and leave with lower angular velocity. This variation needs further study.
We will probably need to make up some energy and momentum losses with plasma rocket engines at GEO station, especially if we accumulate more upward vehicles than downward ones. But overall, the energy will be tiny compared to the the launch loop energies, and we can float a lot of solar cell around GEO as part of our "momentum anchor".
As part of an overall "space antilitter" ethic, we should make sure the plasma rocket engines are offset so they are firing exhaust away from the rest of the geosynchronous ring, and that the rocket exhaust is traveling fast enough to escape the solar system ( >16 km/sec at noon when the rockets are pushing retrograde to the Earth's orbit around the sun, >76 km/sec (!!) at midnight, when the rockets are pushing retrograde ).
A Variable Specific Impulse Magnetoplasma Rocket (VASIMR) engine operates optimally at 50 km/sec, so operation at 80 km/sec is close to optimum. The reaction mass is argon, which can be frozen at 200C with a density of 1600 kg/m3 and a vapor pressure of 0.1 atmosphere for transit from earth. We will need about 1 kg of argon reaction mass shipped up for every 50 kg of uncompensated mass shipped up from Earth. Argon is 0.93% of the atmosphere, and costs about $1/kg (liquid) in high quantities. It is a byproduct of the production of liquid oxygen.
We will expend about 40 kilowatt hours per "uncompensated vehicle kilogram" operating the plasma rockets, including coolers and radiator operation. Typical solar cell weights for existing satellites are 65 kg/kilowatt, so 1 kilogram of solar cells provides enough energy in a year to bring aboard 3.5 kilograms of mass  a power doubling time of 5 months. However, if we can use "server sky" style ultrathin InP cells, closer to 1000 kg/kW, we can approach 50 kilograms of mass per kilogram of solar cell. In the very long term, solar cells made from lunar materials will bring both momentum and cheaper launch to the GEO rail, but solar cells are a hightech undertaking, and it will be a long time before that level of manufacturing technology can operate practically in space.
In the shorter term, we may be forced to get by with lower ISP engines than 80 km/sec VASIMR, perhaps operating only around noon with an exhaust velocity of 20km/sec. That increases our argon needs 4X, but reduces our power needs 16X. We will only be operating our engines with about a 30 percent duty cycle, so our solar panel needs only drop 5.3X. Still, our power doubling time drops to a month or so. Probably worth it during the building phase. We may even be rascals, and run the VASIMR engines 24 hours for a while, dumping a few tons of midnight argon into orbits in the inner solar system.
Operation of an M288 rail base
A similar rail system can supply the M288 server sky orbits
MORE LATER
M288 rail bases for orbital debris capture
Server sky thinsats are cheaper to launch if they are lighter, but below a minimum masstoarea ratio, the orbits are unstable under light pressure. However, we can add mass ballast to a very light satellite, using gramweight chunks of space debris. The processing is simple, just let the debris shatter as it is collisioncaptured inside a cornucopiashaped funnel. Larger chunks can be cut apart at a simple processing plant at the M288 rail base, smaller chunks can be welded together.
Capture vehicles can drop below the tether, in intercept orbits where the debris crosses the equatorial plane. Depending on their orbit, they can return to the same rail base, but more likely a different rail base will be more convenient.
MORE LATER
The Math
We will neglect oblateness, light pressure, and the gravity of other bodies for now. Simple Kepler two body orbits around the earth.
The vehicle leaves the launch loop at 80km altitude, the apogee of an elliptical orbit with a perigee of r_p = 6458.137 km and velocity v_a . The earth's gravitational parameter \mu = 398600.4418 km^{3}/s^{2} = 3.986004418e14 m^{3}/s^{2}. Given those three values, we define the orbit:
h ~ = ~ r_p v_p angular momentum
a ~ = ~ { \Large { r_p \over { 2 ~  ~ \LARGE { { r_p {v_p}^2 } \over { \huge \mu } } } } } semimajor axis
e ~ = ~ 1  { \Large { { r_p } \over a } } ~ = ~ { \Large { { r_p {v_p}^2 } \over \mu } }  1 eccentricity
v_0 ~ = ~ { \Large { { v_p } \over { 1 + e } } } ~ = ~ { \Large { { \mu } \over { r_p v_p } } } characteristic velocity
r_0 ~ = ~ a ( 1  e^2 ) ~ = ~ \Large { { {r_p}^2 {v_p}^2 } \over \mu } characteristic radius
r( \theta ) ~ = ~ \Large { r_0 \over { 1 + e \cos( \theta ) } } orbit radius as a function of \theta , the angle from perigee or true anomaly
{v_T}( \theta ) ~ = ~ v_0 ( 1 + e \cos( \theta ) ) orbit transverse velocity
{v_R}( \theta ) ~ = ~ v_0 e \sin( \theta ) orbit radial velocity
{\omega } ( \theta ) ~ = ~ { \Large { h \over{ r^2 } } } ~ = ~{ \Large { { \mu^2 ( 1 + e \cos( \theta ) )^2 } \over { {r_p}^3 {v_p}^3 } } } orbit angular velocity
r_a ~ = ~ ( 1 + e ) a ~ = ~ { \Large 1 \over { \LARGE { { \huge 2 \mu } \over { r_p {v_p}^2 } } ~  ~1 } } apogee
The angular velocity of the tether in geostationary orbit (defined by the stellar day ) is \omega_T = 2 \pi / 86164.098903691 = 7.29211515E5 radians per second.
At the capture point, the orbit has the same angular velocity as the tether, \omega = \omega_T .
Classical Tether Capture
For the classical ( zero vertical velocity ) tether capture, v_R = 0 and \theta = \pi .
So:
{\omega_T} ~ = ~ { \Large { { \mu^2 ( 1  e )^2 } \over { {r_p}^3 {v_p}^3 } } }
~ ~ ~ ~ ~ ~ = ~ { \Large { { \mu^2 ( 2  r_p {v_p}^2 / \mu )^2 } \over { {r_p}^3 {v_p}^3 } } }
~ ~ ~ ~ ~ ~ = ~ { \Large { { ( 2 \mu  r_p {v_p}^2 )^2 } \over { {r_p}^3 {v_p}^3 } } }
The perigee velocity v_p can be computed by iterating on this equation:
v_p ~ = ~ \sqrt{ 2 \mu / r_p  \sqrt{ \omega_T r_p {v_p}^3 } }
Given v_p , we can compute the capture radius, which is r_a as above.
But we aren't done! We need to do two more things  climb up the tether, and restore momentum to the tether. Assume the tether is massive compared to a vehicle, so it does not deflect much. The will slow down by a tiny amount, and we must restore the momentum, perhaps with rocket engines. We must also supply energy to lift the vehicle up the tether against the small gravity (minus centrifugal force) at that high altitude.
Classical Tether Capture 

\mu 
gravitational parameter 
3.986004418e14 
m^{3}/s^{2} 
\omega_T 
GEO angular frequency 
7.29211515e5 
radians/s 
r_{GEO} 
GEO radius 
42164172.4 
m 
v_{GEO} 
GEO velocity 
3074.66 
m/s 
E_{GEO} 
GEO energy / kg 
14180301.17 
J/kg 
H_{GEO} 
GEO angular momentum/kg 
1.296e11 
m^{2}/s 
r_p 
perigee radius 
6458137.0 
m 
v_p 
perigee velocity 
10074.5754 
m/s 
e 
eccentricity 
0.64446 

a 
semimajor axis 
18164241.20 
m 
r_a 
apogee radius 
29870345.40 
m 
v_a 
apogee velocity 
2178.1800 
m 
acc_a 
apogee radial accel. 
0.2879 
m/s^2 
E_a 
apogee energy / kg 
15716587.30 
J/kg 
H_a 
apogee ang momentum/kg 
6.506e10 
m^{2}/s 
\Delta r 
radius increase 
12293826.96 
m 
\Delta v 
velocity increase 
896.4800 
m/s 
\Delta E 
radial energy increase/kg 
1536286.13 
J/kg 
\Delta H 
radial ang. mom. incr./kg 
6.458e10 
m^{2}/s 
If we haul the payload up with a solar cell power source weighing as much as the payload, then our "hauling power" will be about (16/2) = 8 watts per kilogram using current satellite technology. Against a 0.2879 m/s^{2} acceleration field, we can move at (8/0.2879) = 28 m/s near the bottom, faster near the top. At 8 watts per kilogram, and 1536286 joules per kilogram, climbing the tether will require at least 53 hours. However, at some point we are velocity limited  perhaps 200m/s for our motor. That occurs when the acceleration force is ( 8/200 ) = 0.04 m/s^{2}, about 39800 km high. The velocity limit increases climber time to 55 hours .
If we can use a pulley system without tangling cables, running at 400m/s, climber time is 8.5 hours. We can go a lot faster if we are not moving the motor and the solar cells.
MORE LATER
Rail Tether Capture, with vertical velocity
This is a little trickier. The system moves faster if we have a lousy "lift to drag" ratio, because we can travel the tether faster. It also makes the math a little simpler if we pick a fixed starting speed, as long as it is more than enough to make the climb. Lets start with the energy increase for the classic case, 1.54 MJ/kg , double it, and turn the result into a velocity: about 2500 meters per second. We will arbitrarily choose that as v_{vc} , the vertical speed the vehicle will be moving up the tether when it is captured. Since we are launching from the loop with about 52 MJ/kg anyway, an extra 3% energy loss will not be a show stopper, and we will get to the GEO rail station faster. Time is money!
The capture radius r_c is below orbit apogee by some asyet undefined amount. The angular velocity will be \omega_T as before, so the transverse velocity will be \omega_T r_c . The total velocity squared will be the sum of the squares: {v_{vc}}^2 + ( \omega_T r_c )^2 .
\omega_T r_c ~ = ~ v_0 ( 1 + e \cos( \theta ) )
v_{vc} ~ = ~ v_0 e \sin( \theta )
r_c ~ = ~ r_0 / ( 1 + e \cos( \theta ) )
So:
\sin( \theta ) ~ = ~ { \Large { v_{vc} \over { v_0 e } } }
~ ~ ~ ~ ~ ~ ~ ~ = ~ { \Large { v_{vc} \over { v_p  \mu / r_p v_p } } }
\cos( \theta ) ~ = ~  \sqrt{ 1  \sin( \theta )^2 } . . . Note the quadrant! \theta is near \pi, not 0!
~ ~ ~ ~ ~ ~ ~ ~ = ~  \sqrt{ 1  { \Large \left( { v_{vc} \over { v_p  \mu / r_p v_p } } \right) } ^2 }
\omega_T ~ = ~ ( v_0 / r_0 ) ( 1 + e \cos( \theta ) )^2
~ ~ ~ ~ ~ ~ = ~ { \Large { \mu^2 \over { {r_p}^3 {v_p}^3 } } } ~ \left( 1  \left( { \Large { { r_p {v_p}^2 } \over \mu } }  1 \right) \sqrt{ 1  { \Large \left( { v_{vc} \over { v_p  \mu / r_p v_p } } \right) } ^2 } \right)^2
Let's solve this mess for v_p . We know all the other terms. It will be iterative, as before:
v_p ~ = ~ \LARGE \sqrt{ { \Large { \mu \over r_p } + } { { { \mu \over r_p }  \sqrt{ \Large \omega_T r_p {v_p}^3 } } \over \sqrt{ 1  { \left( { v_{vc} \over { v_p  \mu / r_p v_p } } \right) } ^2 } } }
If v_{vc} = 0, this reduces to the classical case above.
The capture rail is a long way out of the gravity well, so "natural" vertical deceleration of a vehicle is small. However, there will be some drag from eddy currents in the thin and rather resistive rail. In a production system, the drag profile will be optimized and rather complex. For this analysis, we will just compute the kinetic energy lost by moving up the rail, multiply that by a drag factor, and use that to compute the kinetic energy and velocity left as we approach the dock at GEO.
The vertical deceleration is given by:
acceleration = \omega^2 r  \mu / r^2 . . . zero at GEO, of course!
and the specific energy ( J/kg ) can be computed by integrating that:
E(r) = 0.5 \omega^2 r^2  \mu / r
The drag factor is D , and will always be greater than 1, so the velocity nearing GEO will be:
v_{GEO} \approx \sqrt{ {v_{vc}}^2  2 D ( E_{GEO}  E_{capture} ) }
The velocity at radius r will be:
v(r) \approx \sqrt{ {v_{vc}}^2 + D \omega^2 ( r^2  {r_c}^2 )  2 D \mu ( 1 / r_c  1 / r ) }
The transit time from the capture point to GEO will be:
time = {\huge\int} _{r_c}^{GEO} { \Large { dr \over {v(r)} } } ... which probably requires numerical integration
Since we want to keep the transit time small, we would like to keep the rail very straight and travel up it quickly. So we keep the drag and deceleration relatively low for most of the trip. As we approach GEO, however, we "hit the brakes", decelerating at a much higher rate, so we come quickly and smoothly to a stop at the dock. The transition from low to high deceleration occurs at the slowdown radius r_s .
Here's a closetominimum transit time capture:
GEOrail Tether Capture 

v_{vc} 
Vertical V 
2700.0000 
m/s 
acc_s 
slowdown deceleration 
5.0000 
m/s^{2} 
D 
drag factor 
2.0000 

\mu 
gravitational parameter 
3.9860E+14 
m^{3}/s^{2} 
\omega_T 
GEO angular frequency 
7.2921151E05 
radians/s 
r_{GEO} 
GEO radius 
42164172.37 
m 
v_{GEO} 
GEO velocity 
3074.6600 
m/s 
E_{GEO} 
GEO energy / kg 
14180301 
J/Kg 
H_{GEO} 
GEO angular momentum/kg 
1.2964E+11 
m^{2}/s 
r_p 
perigee radius 
6458137.0 
m 
v_p 
perigee velocity 
10462.7761 
m/s 
e 
eccentricity 
0.77363 

a 
semimajor axis 
28529281.45 
m 
r_a 
apogee radius 
50600425.91 
m 
v_a 
apogee velocity 
1335.3651 
m/s 
\theta 
orbit angle at capture 
143.73 
degrees 
r_c 
capture radius 
30440398.47 
m 
v_{tc} 
capture tranverse velo. 
2219.7489 
m/s 
E_c 
capture energy 
15558098 
J/kg 
acc_c 
capture vert. accel. 
0.2683 
m/s^{2} 
H_{capture} 
capture ang. momentum/kg 
6.7570E+10 
m^{2}/s 
y_s 
slowdown run 
177982.60 
m 
r_s 
slowdown radius 
41986189.77 
m 
v_s 
slowdown velocity 
1334.10 
s 
t_s 
slowdown time 
266.82 
s 

tether climb time 
6604.70 
s 

Partial orbit time 
18533.41 
s 

Launch time 
348.76 
s 

Total time 
7.15 
hours 
\Delta v 
velocity increase 
854.9111 
m/s 
\Delta E 
radial energy increase/kg 
1377796.89 
J/kg 
\Delta H 
radial ang. mom. incr./kg 
6.2070E+10 
m^{2}/s 
\Delta r 
radius increase 
11723773.89 
m 
Here's a table of transit time versus versus vertical capture velocity. The capture velocity is quite sensitive to launch velocity, which must be controlled to mm/sec. Note that if we launch very fast, we spend a long time heading out and coming back to the tether. These are all "drag=2" times; if we reduce drag, the optimum occurs at a lower launch velocity.
Transit time versus vertical tether velocity 
time, seconds 
total 

vertical 
vp 
a 
rc 
launch 
orbit 
climb 
slow 
hours 
3200.00 
10615.08 
37940037 
30661158 
354 
24481 
4330 
446 
8.23 
3000.00 
10551.38 
32915772 
30569017 
352 
21591 
4991 
381 
7.59 
2800.00 
10491.37 
29807595 
30481967 
350 
19422 
5934 
308 
7.23 
2750.00 
10476.96 
29148708 
30461018 
349 
18964 
6245 
288 
7.18 
2700.00 
10462.78 
28529281 
30440398 
349 
18533 
6605 
267 
7.15 
2650.00 
10488.83 
27946160 
30420112 
348 
18129 
7028 
244 
7.15 
2600.00 
10435.13 
27396521 
30400159 
348 
17749 
7542 
220 
7.18 
2550.00 
10421.67 
26877836 
30380544 
347 
17390 
8193 
193 
7.26 
2500.00 
10408.45 
26387830 
30361268 
347 
17053 
9075 
162 
7.40 
2400.00 
10382.74 
25485852 
30323743 
346 
16433 
13467 
70 
8.42 

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