Quote from: mikelepage on 03/25/2017 11:41 amThanks for responding David, but my question was not just about matching inclination (which I now see can be done easily), but also matching argument of Phobos' ascending node. As you say, the vector of any approaching ship is parallel with Mars', so does that not mean that a direct approach to Phobos would only be possible twice per year?Am drawing some pictures to help me think about this.Deimos and Phobos aren't exactly coplanar with Mars' equatorial plane but close. I'll call them equatorial because it makes it easier to visualize and I can use some well known words.Coming in from a Hohmann transfer, the Vinf velocity vector is perpendicular to the heliocentric position vector. This Vinf vector needs to lie in the equatorial plane to have the ship enter on a coplanar orbit. Over a complete circuit of the moon's orbit, the moon's velocity vectors will point in every direction in that plane. The ship's Vinf velocity vector must be parallel to one of the moon's velocity vectors.The only time a moon's velocity vector is perpendicular to the heliocentric position vector is when the moon's high in the sky at Martian noon or midnight.Also the moon's high noon or midnight velocity vectors must occur at a time when Mars equatorial plane forms a 23.5º angle with the sun's position vector. When does this happen? At Mars' summer and winter solstice.You might be right. A vexing observation I can't ignore.If you just do a small braking burn to park into a large capture orbit, plane change expense is minor in the neighborhood of apoapsis. But a large capture orbit can last month to two months. Less of an option when humans are aboard but possibly a way to get less time sensitive supplies and infrastructure on the Martian moons.
Thanks for responding David, but my question was not just about matching inclination (which I now see can be done easily), but also matching argument of Phobos' ascending node. As you say, the vector of any approaching ship is parallel with Mars', so does that not mean that a direct approach to Phobos would only be possible twice per year?
Quote from: docmordrid on 05/20/2016 07:12 amAIUI Phobos may be a dust coated rubble pile with tidal issues. Not sure that's a stable platform for a base.And because of this uncertainty I find it un-be-lie-vab-le that we still have not found time, money & interest to send even a modest lander / orbiter to Phobos or Deimos...! Those moons are near Mars, are two interesting targets on their own, are also asteroids, give possibility to do Mars observations at the same time, give knowledge for future manned mission... Looking at all this, it seems so weird NASA has no interest at all for those Martian moons.OK, Russians have tried, but...
AIUI Phobos may be a dust coated rubble pile with tidal issues. Not sure that's a stable platform for a base.
Strange thought here; Anybody ever thought to send a number of cube sats as probes to Phobos?
Quote from: JasonAW3 on 03/27/2017 05:02 pmStrange thought here; Anybody ever thought to send a number of cube sats as probes to Phobos? Yes. Look: http://www.lpi.usra.edu/meetings/lpsc2017/pdf/1707.pdf
Quote from: redliox on 03/27/2017 05:20 pmQuote from: JasonAW3 on 03/27/2017 05:02 pmStrange thought here; Anybody ever thought to send a number of cube sats as probes to Phobos? Yes. Look: http://www.lpi.usra.edu/meetings/lpsc2017/pdf/1707.pdfOk, I stand corrected. So, why hasn't anyone done anything with this idea?
I've attached a rough pic indicating different hyperbolic orbits entering the SOI at different latitudes.
I asked a astrogator friend of mine if we needed to come in at Mars winter or summer solstice if we wanted an easy slide into a near equatorial orbit.He replied with the attached illustration from Bates Mueller and White. It's a pic of envelope of outgoing hyperbolas but it could just as well be incoming hyperbolas. In his words "You can pick any inclination available by rotating around the incoming asymptote."
Coming in from a Hohmann transfer, the Vinf velocity vector is perpendicular to the heliocentric position vector. This Vinf vector needs to lie in the equatorial plane to have the ship enter on a coplanar orbit. Over a complete circuit of the moon's orbit, the moon's velocity vectors will point in every direction in that plane. The ship's Vinf velocity vector must be parallel to one of the moon's velocity vectors.The only time a moon's velocity vector is perpendicular to the heliocentric position vector is when the moon's high in the sky at Martian noon or midnight.Also the moon's high noon or midnight velocity vectors must occur at a time when Mars equatorial plane forms a 23.5º angle with the sun's position vector. When does this happen? At Mars' summer and winter solstice.You might be right. A vexing observation I can't ignore.If you just do a small braking burn to park into a large capture orbit, plane change expense is minor in the neighborhood of apoapsis. But a large capture orbit can last month to two months. Less of an option when humans are aboard but possibly a way to get less time sensitive supplies and infrastructure on the Martian moons.
Reviving this thread because of discussion here:https://forum.nasaspaceflight.com/index.php?topic=50157.300The discussion was about my post #100 upthread about whether it's possible to get to Phobos or Deimos as a "way-station" more than twice a year. Quote from: Hop_David on 03/26/2017 04:49 pmComing in from a Hohmann transfer, the Vinf velocity vector is perpendicular to the heliocentric position vector. This Vinf vector needs to lie in the equatorial plane to have the ship enter on a coplanar orbit. Over a complete circuit of the moon's orbit, the moon's velocity vectors will point in every direction in that plane. The ship's Vinf velocity vector must be parallel to one of the moon's velocity vectors.The only time a moon's velocity vector is perpendicular to the heliocentric position vector is when the moon's high in the sky at Martian noon or midnight.Also the moon's high noon or midnight velocity vectors must occur at a time when Mars equatorial plane forms a 23.5º angle with the sun's position vector. When does this happen? At Mars' summer and winter solstice.You might be right. A vexing observation I can't ignore.If you just do a small braking burn to park into a large capture orbit, plane change expense is minor in the neighborhood of apoapsis. But a large capture orbit can last month to two months. Less of an option when humans are aboard but possibly a way to get less time sensitive supplies and infrastructure on the Martian moons.
Anywhere on the surface of Phobos will reduce radiation simply because the body of Phobos blocks about 50% of the sources. The bottom of Stickney will not be very much different (it's not really very steep and deep), and from the bottom of the crater that stunning view will be somewhat reduced as well.