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01:14
I just got in from dinner man its been a long day
I only pick David Dunlop Brain today he's a guy who got me here so I kind of had to
now I know the drill I can be online through the day tomorrow
@TildalWave I don't see that in the blur of notes I have
the poster session is tomorrow that's what I should have the most chance to talk to people directly
@kimholder I left a comment there, it was just a couple of slides when that lunar volatiles site was mentioned
the one that's for the next couple of days still password protected (pass: lunar)
it was all volatiles
yeah wait I'd have to check the program to see who mentioned it
My hotel WiFi is crappy right now
Peak usage I guess
I paid for extra bandwidth but I am getting a trickle
not sure either Robinson or Plescia, I think Robinson
01:26
Well if I have an excuse to ask him a question that works for me
hmmm wait maybe it was Gruener
oh gee dunno
I think I want to try and accost Jim Keravala tomorrow. I watched the opportunity slip away today because I was talking to somebody else
ah yes file name says Carpenter so it was Gruener J. E. et al. on International Coordination of Lunar Polar Volatiles Exploration
okay he chatted briefly today with Dave well I was there so I have a bit of an in with him
boobies it looks like the audio recordings I did today all worked out
3
yeah I think you'll want James D. Carpenter of ESA for that, it's his slides and they really hurried through that during the LEAG ones, I was like wooot I couldn't even take a printscreen LOL
01:32
groovy not boobies
it looks like most of the goodies on slides are in cooperation with Russkies and maybe that isn't all that certain now
@kimholder hahaha didn't even see it
sorry but I gotta star that :))
your android is a bit of a perv isn't it? LOL
but of course
okay today I tested the waters
So you had a good time? It looked relaxed enough, I saw the final slide :P
thet seem very approachable its just I know so little compared to everyone else
01:37
I wanted to ask why nobody was thinking about getting liquid oxygen From regolith
well isn't the main volatiles session actually tomorrow?
but I was to shY they. Seem so dead set that the only thing to do was to get water from the poles
is it you see I don't even know anymore
but if you have water you have oxygen
but the water isn't really so easy to get at as they seem to all claim
and anyhow where are the aternative proposals
the thing is I just can't stand up and say why don't you do this instead
agreed and it's really unclear how much of it is there, those Chandrayaan maps could be basically just topmost layer and nearly none of it there
plus, why is everyone forgetting about the possibility of deep embedded pockets of ice?
01:41
I'm trying to decide how best to approach this
I mean, the Moon could as well have karst-like features beneath its surface with big pockets of ice inside melt bubbles
I think I need to get there much earlier tomorrow
I want to check in with somebody near the top about what questions I can ask
if you're not sure I can ask them for you then
no that doesn't seem like a good approach
I want to get into what I really want to know I just want to do it in a way where I'm not different speckled anybody's time
disrespectful of anybody's time
I was thinking how melt bubbles could trap volatiles ... so basically you have these big pockets of basically nothing that was filled with volatiles as the melt slowly cooled down, and small surface gravity means those bubbles would hold, they wouldn't be "in a hurry" to escape up
so any volatiles would basically evaporate and then condense on the ceiling,... and this for quite some time
... karst on the moon
If they're not going anywhere inside meteorites that hit the Earth then why would they escape there? For all we know deep lunar rock could be wet
especially since we now know how much wetter the Earth is deep below than any previous estimates
@kimholder different speckled :))
The Space Show w/ S. Wolfe & S. Gonzalez re SpaceCom, the Space Commerce Conference & Exposition is now podcast live. More info in the newsletter
02:16
Just on the phone with hubby
tomorrow is the poster session at the end of the day
that's when I give away the t-shirts and all the other stuff
guys I'm really going to try and be online and be in touch with the pod bay all day tomorrow
but you have space jokes and want pass along go ahead
basalt product samples ooooo
and voice recognition actually knew the word for salt
ok wEll even once impresses me
hey nice
what's on those sticks?
looks like ninja leftovers :))
02:31
They're basalt rebar
oh nice, how heavy are they?
pretty lights and they clink like glass
yeah I just checked and apparently it's 89% lighter than steel
well there you go
I'm going to need a table tomorrow
I got the basalt stuf. And all the stack exchange stuff
and moonwards
02:40
I gave it a business card today the guy said where is your name
I said what you don't need my name
Yeah did you check if they can provide you with a table there? Otherwise I'd try to find a big cardboard box and some table cloth
then I took it and wrote it on the back
I got together early tomorrow anyhow I'll check into it
03:14
they said they didn't record that talks today but they could they already have the streaming service they just have to press record
send the techie said but its going to be a pretty big file I said if you can just do it we can make sure it gets online and I invoked SX
so I need to ask clive tomorrow
by the way the guy I gave my business card to was Larry Turner
and now I'm reading his excellent article on 20 different ways to extract oxygen on the moon
I can't seem to copy the address on my tablet
but it comes up first if you google lunar oxygen production
 
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05:07
 
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1 hour later…
14:21
FAA Commercial Space Transportation Advisory Committee (COMSTAC) Meeting is now accessible live. Agenda here (PDF)
14:34
OK a lot of good explaining at LEAG now re amount of lunar polar volatiles and that it can't be just immediate surface layer, it has to be replenished from subsurface
14:44
Interesting The contrast with mercury
15:05
I'm still curious about ways to retain volatiles hitting the lunar surface... can't get my hands on any good estimates of flux density (solar proton flux, solar plasma when the Moon is grazing Earth's magnetosphere, orbit intersecting comets trajectories, and also surface disturbance like micrometeorites, quakes,...)
it seems there's possibility of such transport occurring naturally at the low solar angle polar craters and concentrating volatiles in the wake (of dielectric / photoelectric charged surface), so size of any collectors could be greatly reduced
 
2 hours later…
17:25
posted on October 21, 2015

The galaxy cluster MS 0735.6+7421 is home to one of the most powerful eruptions ever observed. X-rays detected by NASA's Chandra X-Ray Observatory (blue) show the hot gas that comprises much of the mass of this enormous object. This image is part of a collection of new images released from the Chandra archive to celebrate American Archive Month.


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