1 00:00:10,289 --> 00:00:08,640 all right Thank You Brett and thank you 2 00:00:13,289 --> 00:00:10,299 to the AB grad Con organizers this has 3 00:00:14,730 --> 00:00:13,299 been rfg was a lot of fun and I'm 4 00:00:17,010 --> 00:00:14,740 looking forward to the rest of AB grad 5 00:00:19,440 --> 00:00:17,020 con so I'd like to really talk to you 6 00:00:21,600 --> 00:00:19,450 about complex molecule formation and 7 00:00:23,790 --> 00:00:21,610 terahertz spectroscopy and really this 8 00:00:25,830 --> 00:00:23,800 is all about Astra chemistry so Brett 9 00:00:27,060 --> 00:00:25,840 gave a really great warm up talk so I 10 00:00:28,800 --> 00:00:27,070 think you guys actually have a lot of 11 00:00:32,070 --> 00:00:28,810 the basics actually he stoled a lot of 12 00:00:33,720 --> 00:00:32,080 my thunder so what I'm going to really 13 00:00:36,930 --> 00:00:33,730 tell you about is the importance of 14 00:00:39,450 --> 00:00:36,940 molecules really we think in how life 15 00:00:40,950 --> 00:00:39,460 came to exist on this planet so we've 16 00:00:43,290 --> 00:00:40,960 just heard a bit about protoplanetary 17 00:00:45,750 --> 00:00:43,300 disks so this is a artists cartoon of 18 00:00:48,060 --> 00:00:45,760 one when you go from say a 19 00:00:49,529 --> 00:00:48,070 protoplanetary disc to a solar system we 20 00:00:52,920 --> 00:00:49,539 understand pretty well the role that 21 00:00:55,500 --> 00:00:52,930 molecules play but what was less clear 22 00:00:57,060 --> 00:00:55,510 is if you have a solar system and a 23 00:00:59,369 --> 00:00:57,070 solar system like ours we know we have 24 00:01:00,840 --> 00:00:59,379 life right so really one of the 25 00:01:03,479 --> 00:01:00,850 important questions in Astro chemistry 26 00:01:06,600 --> 00:01:03,489 is how do you go from a solar system to 27 00:01:09,480 --> 00:01:06,610 a solar system with life and really 28 00:01:11,609 --> 00:01:09,490 we're encouraged that we can learn 29 00:01:14,010 --> 00:01:11,619 something from the chemistry of space 30 00:01:15,660 --> 00:01:14,020 that will tell us about life on say a 31 00:01:18,330 --> 00:01:15,670 planet like Earth because of the 32 00:01:21,150 --> 00:01:18,340 Stardust mission and when we you know we 33 00:01:25,980 --> 00:01:21,160 know that now that we've seen glycine in 34 00:01:28,760 --> 00:01:25,990 the cometary tail of the comet that 35 00:01:31,589 --> 00:01:28,770 Stardust sampled and this gives us 36 00:01:33,839 --> 00:01:31,599 really a thought that well okay complex 37 00:01:35,490 --> 00:01:33,849 molecules are forming in space so maybe 38 00:01:37,109 --> 00:01:35,500 one of the important ways that we 39 00:01:38,880 --> 00:01:37,119 actually wind up with the precursors of 40 00:01:42,359 --> 00:01:38,890 life the prebiotic species that we need 41 00:01:43,859 --> 00:01:42,369 are some complex molecule formation in 42 00:01:46,680 --> 00:01:43,869 space that is then subsequently 43 00:01:48,630 --> 00:01:46,690 delivered to a planet and so if we 44 00:01:50,520 --> 00:01:48,640 really want to then understand complex 45 00:01:52,350 --> 00:01:50,530 chemistry in space the place that we 46 00:01:55,770 --> 00:01:52,360 have to think about our icy death 47 00:01:58,199 --> 00:01:55,780 screens if you remember something about 48 00:02:00,870 --> 00:01:58,209 chemistry at some point you might have 49 00:02:03,059 --> 00:02:00,880 or even physics to have three three 50 00:02:05,699 --> 00:02:03,069 different species come together and all 51 00:02:07,139 --> 00:02:05,709 hit each other at the same time it's not 52 00:02:08,760 --> 00:02:07,149 a straightforward process and in the 53 00:02:11,010 --> 00:02:08,770 case of having them hitting each other 54 00:02:13,949 --> 00:02:11,020 and then react that's going to be a very 55 00:02:15,810 --> 00:02:13,959 rare event but if you have say a third 56 00:02:16,920 --> 00:02:15,820 body like a dust grain that's just 57 00:02:18,720 --> 00:02:16,930 floating around you can have some 58 00:02:20,610 --> 00:02:18,730 molecule come down and stick to its 59 00:02:22,530 --> 00:02:20,620 surface now it's there first 60 00:02:24,660 --> 00:02:22,540 amount of time if another molecule comes 61 00:02:26,339 --> 00:02:24,670 down it can diffuse around find it on 62 00:02:30,690 --> 00:02:26,349 this guy who is sitting there first and 63 00:02:31,770 --> 00:02:30,700 react over the course of time you and by 64 00:02:34,440 --> 00:02:31,780 time we're talking about millions of 65 00:02:36,990 --> 00:02:34,450 years in you know a star-forming system 66 00:02:38,910 --> 00:02:37,000 you can build up a layer of ice on the 67 00:02:41,100 --> 00:02:38,920 surface of this dust grain and the 68 00:02:43,190 --> 00:02:41,110 molecules that are on this surface will 69 00:02:45,899 --> 00:02:43,200 affect the the subsequent chemistry and 70 00:02:48,680 --> 00:02:45,909 this is really what we're thinking about 71 00:02:51,420 --> 00:02:48,690 in our lab so we want to investigate 72 00:02:53,369 --> 00:02:51,430 Isis and we're going to take we're not 73 00:02:55,440 --> 00:02:53,379 going to try to actually say we are 74 00:02:57,720 --> 00:02:55,450 gonna make what's in space no we're 75 00:03:00,330 --> 00:02:57,730 gonna go simpler we're going to try and 76 00:03:02,729 --> 00:03:00,340 look at simple things and slowly build 77 00:03:05,009 --> 00:03:02,739 up into a bigger and bigger picture so 78 00:03:06,839 --> 00:03:05,019 that we can understand and try to 79 00:03:09,300 --> 00:03:06,849 disentangle the complex picture that's 80 00:03:12,059 --> 00:03:09,310 happening in space from laboratory 81 00:03:13,259 --> 00:03:12,069 experiments and again this is important 82 00:03:15,030 --> 00:03:13,269 because if you want to make anything 83 00:03:17,610 --> 00:03:15,040 more complicated than as Brett was 84 00:03:19,020 --> 00:03:17,620 saying methyl formate or methanol there 85 00:03:20,640 --> 00:03:19,030 is no way that you can do this in the 86 00:03:22,619 --> 00:03:20,650 gas phase so we really need to look at 87 00:03:24,210 --> 00:03:22,629 Isis so in order for me to take you 88 00:03:26,039 --> 00:03:24,220 there I do have to take you through a 89 00:03:28,800 --> 00:03:26,049 quick diversion to the electromagnetic 90 00:03:30,720 --> 00:03:28,810 spectrum and the region that I'm gonna 91 00:03:32,460 --> 00:03:30,730 be focusing on here is what I call the 92 00:03:35,670 --> 00:03:32,470 terahertz region or it's often known as 93 00:03:37,289 --> 00:03:35,680 the far infrared and the reason is the 94 00:03:39,539 --> 00:03:37,299 far infrared is because you come down 95 00:03:41,550 --> 00:03:39,549 from the visible and the near IR mid IR 96 00:03:44,490 --> 00:03:41,560 you hit the far infrared and it's a 97 00:03:47,190 --> 00:03:44,500 region that really corresponds to low 98 00:03:49,470 --> 00:03:47,200 energy vibrations and solids long range 99 00:03:51,689 --> 00:03:49,480 interactions you need lots of molecules 100 00:03:55,409 --> 00:03:51,699 participating in in order to actually 101 00:03:56,550 --> 00:03:55,419 see these vibrational modes and it's 102 00:03:58,470 --> 00:03:56,560 kind of an interesting region because 103 00:04:00,449 --> 00:03:58,480 historically it's been a difficult place 104 00:04:02,309 --> 00:04:00,459 to actually make making detect photons 105 00:04:03,689 --> 00:04:02,319 and so we're excited to be working here 106 00:04:05,849 --> 00:04:03,699 because there's a lot of new stuff to 107 00:04:07,259 --> 00:04:05,859 learn the reason why it's important for 108 00:04:09,119 --> 00:04:07,269 a stroke a mystery however is that 109 00:04:10,439 --> 00:04:09,129 fundamentally there are things that we 110 00:04:12,270 --> 00:04:10,449 can learn from terahertz spectroscopy 111 00:04:14,610 --> 00:04:12,280 that we'll never be able to learn from 112 00:04:17,279 --> 00:04:14,620 the near infrared so if you take this 113 00:04:19,020 --> 00:04:17,289 nice picture of an edge on disk as taken 114 00:04:22,050 --> 00:04:19,030 by the Hubble Space Telescope you can 115 00:04:23,310 --> 00:04:22,060 see in the middle here it's black and 116 00:04:25,589 --> 00:04:23,320 that's because even though there is a 117 00:04:27,810 --> 00:04:25,599 star at the center of this disk that's 118 00:04:30,540 --> 00:04:27,820 giving off lots of light there's so much 119 00:04:32,430 --> 00:04:30,550 material it's so dense through that 120 00:04:34,409 --> 00:04:32,440 section that we don't see any light 121 00:04:37,830 --> 00:04:34,419 making it to our tell us 122 00:04:39,780 --> 00:04:37,840 so if we actually have all this stuff 123 00:04:41,340 --> 00:04:39,790 there and we want to learn something 124 00:04:42,379 --> 00:04:41,350 about say maybe the colder part of the 125 00:04:45,000 --> 00:04:42,389 disk 126 00:04:47,520 --> 00:04:45,010 we'd like there to be some thermal 127 00:04:50,400 --> 00:04:47,530 excitation of molecules that would then 128 00:04:52,770 --> 00:04:50,410 emit photons we can detect if we want to 129 00:04:54,420 --> 00:04:52,780 look at Isis those need to be cold 130 00:04:56,370 --> 00:04:54,430 temperatures and if you just take a look 131 00:04:58,409 --> 00:04:56,380 at my math here at the bottom if we're 132 00:05:00,090 --> 00:04:58,419 looking or at somewhere in the mid 133 00:05:01,620 --> 00:05:00,100 infrared around you know a thousand wave 134 00:05:03,870 --> 00:05:01,630 numbers in order to have thermal 135 00:05:05,550 --> 00:05:03,880 excitation and actually see emission 136 00:05:07,409 --> 00:05:05,560 from the outer region of the disk the 137 00:05:09,990 --> 00:05:07,419 disk would have to be around 1400 Kelvin 138 00:05:11,820 --> 00:05:10,000 there's not going to be any ice at 1400 139 00:05:13,740 --> 00:05:11,830 Kelvin so we have to go to the terahertz 140 00:05:15,600 --> 00:05:13,750 and that's why there are things we can 141 00:05:19,740 --> 00:05:15,610 learn there that we can't learn anywhere 142 00:05:21,570 --> 00:05:19,750 else so what do I actually do so I have 143 00:05:23,760 --> 00:05:21,580 a vacuum chamber in my laboratory and 144 00:05:25,529 --> 00:05:23,770 inside I have a substrate and I can cool 145 00:05:27,300 --> 00:05:25,539 that substrate all the way down to 10 146 00:05:30,210 --> 00:05:27,310 Kelvin I can control the temperature 147 00:05:32,700 --> 00:05:30,220 between 10 Kelvin at about 300 Kelvin 148 00:05:34,379 --> 00:05:32,710 and I have this little pipe here that is 149 00:05:37,230 --> 00:05:34,389 connected to a dosing line where I'd 150 00:05:38,580 --> 00:05:37,240 have a cylinder or some sample of a 151 00:05:41,730 --> 00:05:38,590 liquid that I'll get in the gas phase 152 00:05:44,190 --> 00:05:41,740 and I can leak a few molecules into the 153 00:05:45,659 --> 00:05:44,200 chamber and those molecules will stick 154 00:05:47,430 --> 00:05:45,669 to the cold surface they'll stick 155 00:05:49,170 --> 00:05:47,440 everywhere but you know as long as they 156 00:05:51,450 --> 00:05:49,180 stick to the surface here which is 157 00:05:54,920 --> 00:05:51,460 actually a silicon substrate I can then 158 00:05:57,839 --> 00:05:54,930 take spectroscopy of them so so I have 159 00:05:59,159 --> 00:05:57,849 terahertz pall source that Brandon is 160 00:06:01,110 --> 00:05:59,169 actually gonna describe in a little more 161 00:06:03,000 --> 00:06:01,120 detail but it's pretty cool because we 162 00:06:05,939 --> 00:06:03,010 actually ionize the air in the 163 00:06:08,490 --> 00:06:05,949 laboratory and make plasma and that's 164 00:06:10,140 --> 00:06:08,500 actually our terahertz source and so the 165 00:06:11,870 --> 00:06:10,150 pulse comes in it interacts with the 166 00:06:14,490 --> 00:06:11,880 sample it gets absorbed by the sample 167 00:06:18,120 --> 00:06:14,500 sample reom it's a pulse that then we 168 00:06:19,800 --> 00:06:18,130 detect in our spectrometer so let me 169 00:06:21,870 --> 00:06:19,810 show you then just some of the spectra 170 00:06:24,779 --> 00:06:21,880 that we've collected and you can see 171 00:06:26,670 --> 00:06:24,789 here this is kind of a almost butterfly 172 00:06:28,710 --> 00:06:26,680 collecting slide but the the purpose of 173 00:06:31,589 --> 00:06:28,720 it is to show you that different 174 00:06:33,300 --> 00:06:31,599 molecules really have distinct spectral 175 00:06:35,129 --> 00:06:33,310 fingerprints in the terahertz region so 176 00:06:37,650 --> 00:06:35,139 we've got more simple molecules like 177 00:06:39,750 --> 00:06:37,660 water water and co2 178 00:06:42,270 --> 00:06:39,760 we've got more complex molecules here 179 00:06:45,779 --> 00:06:42,280 like acetone and methanol and you can 180 00:06:46,750 --> 00:06:45,789 see again these features are very 181 00:06:48,730 --> 00:06:46,760 distinct from 182 00:06:50,770 --> 00:06:48,740 spectrum to the next which gives us hope 183 00:06:52,930 --> 00:06:50,780 that we'll be able to actually identify 184 00:06:56,170 --> 00:06:52,940 different species if they're in a more 185 00:06:57,610 --> 00:06:56,180 complicated ice now what are some of the 186 00:07:01,030 --> 00:06:57,620 useful things that we can learn from 187 00:07:02,140 --> 00:07:01,040 these spectra it's actually oh it would 188 00:07:03,910 --> 00:07:02,150 be great if we could look at a 189 00:07:06,160 --> 00:07:03,920 protoplanetary disc and learn something 190 00:07:09,400 --> 00:07:06,170 about and know with certainty the local 191 00:07:12,010 --> 00:07:09,410 temperature so if you look at our 192 00:07:14,950 --> 00:07:12,020 terahertz spectra this is this is carbon 193 00:07:16,780 --> 00:07:14,960 dioxide ice and I've I've taken spectra 194 00:07:18,430 --> 00:07:16,790 with the ice health at three different 195 00:07:21,430 --> 00:07:18,440 temperatures and you can see in the 196 00:07:22,690 --> 00:07:21,440 inset as I wore as I saw as a cool the 197 00:07:25,180 --> 00:07:22,700 ice down to colder and colder 198 00:07:28,330 --> 00:07:25,190 temperatures the the peak of a spectral 199 00:07:29,950 --> 00:07:28,340 feature actually shifts and this is 200 00:07:31,510 --> 00:07:29,960 great so this means that now if I if I 201 00:07:33,940 --> 00:07:31,520 were to actually see something you know 202 00:07:35,470 --> 00:07:33,950 here versus here I can actually tell you 203 00:07:37,330 --> 00:07:35,480 what the temperature is and you can do 204 00:07:39,480 --> 00:07:37,340 this in the laboratory obviously it'll 205 00:07:42,370 --> 00:07:39,490 be more difficult in space but this is a 206 00:07:44,560 --> 00:07:42,380 potentially and interesting result so 207 00:07:46,810 --> 00:07:44,570 what are these vibrations and I just 208 00:07:49,720 --> 00:07:46,820 really you know have to show you some 209 00:07:51,250 --> 00:07:49,730 some cartoons from some DFT calculations 210 00:07:53,650 --> 00:07:51,260 where we've simulated the spectra of 211 00:07:55,270 --> 00:07:53,660 these of these features and you can see 212 00:07:58,270 --> 00:07:55,280 here that they really are collective 213 00:08:00,520 --> 00:07:58,280 motions these are entire planes of of 214 00:08:01,930 --> 00:08:00,530 co2 molecules in this solid that are 215 00:08:03,700 --> 00:08:01,940 sliding against each other or in the 216 00:08:05,710 --> 00:08:03,710 case of the second mode that you saw in 217 00:08:08,140 --> 00:08:05,720 the spectrum kind of moving with respect 218 00:08:12,310 --> 00:08:08,150 to one another so really think of these 219 00:08:15,520 --> 00:08:12,320 as as phonon modes as large long range 220 00:08:17,920 --> 00:08:15,530 interactions that really require very 221 00:08:19,720 --> 00:08:17,930 little energy to tweak but and as a 222 00:08:23,230 --> 00:08:19,730 result they're very very sensitive to 223 00:08:25,000 --> 00:08:23,240 the structure of the material which 224 00:08:26,680 --> 00:08:25,010 means they're sensitive to the structure 225 00:08:28,780 --> 00:08:26,690 that we're going to see really 226 00:08:30,970 --> 00:08:28,790 interesting differences when we talk 227 00:08:32,890 --> 00:08:30,980 about mixtures and that's what I have on 228 00:08:35,050 --> 00:08:32,900 this slide you can see we start off with 229 00:08:36,940 --> 00:08:35,060 water and I'm going with increasing the 230 00:08:39,400 --> 00:08:36,950 methanol concentration as I go down the 231 00:08:40,930 --> 00:08:39,410 slide until I have pure methanol and you 232 00:08:43,390 --> 00:08:40,940 can see I start with with features 233 00:08:44,740 --> 00:08:43,400 either the very characteristic features 234 00:08:46,510 --> 00:08:44,750 here of water this feature really 235 00:08:49,180 --> 00:08:46,520 actually corresponds to the sort of 236 00:08:52,690 --> 00:08:49,190 bilayer of a water ice stretching like 237 00:08:55,390 --> 00:08:52,700 this and and as I as I add methanol this 238 00:08:56,800 --> 00:08:55,400 feature slowly goes away when I have a 239 00:08:59,920 --> 00:08:56,810 sort of one-to-one mixture I really have 240 00:09:01,750 --> 00:08:59,930 this big almost amorphous blob 241 00:09:03,220 --> 00:09:01,760 as I add more methanol we start to see 242 00:09:04,780 --> 00:09:03,230 maybe these aren't maybe these are the 243 00:09:08,079 --> 00:09:04,790 methanol features growing in here and 244 00:09:09,880 --> 00:09:08,089 then pure methanol is very clear and and 245 00:09:17,040 --> 00:09:09,890 this is the same spectrum like I had on 246 00:09:20,290 --> 00:09:17,050 the first light so so one of the really 247 00:09:21,610 --> 00:09:20,300 bringing this to one more thing that we 248 00:09:23,740 --> 00:09:21,620 really think is interesting about the 249 00:09:25,540 --> 00:09:23,750 chemistry of say a place like a 250 00:09:28,300 --> 00:09:25,550 protoplanetary disk terahertz 251 00:09:30,699 --> 00:09:28,310 spectroscopy really seems to give us the 252 00:09:33,340 --> 00:09:30,709 chance to say something maybe about the 253 00:09:36,250 --> 00:09:33,350 thermal history of an ice and so what do 254 00:09:38,139 --> 00:09:36,260 I mean by that well everything I've 255 00:09:40,840 --> 00:09:38,149 shown you so far as a crystalline solid 256 00:09:42,490 --> 00:09:40,850 so that means when I when I showed you I 257 00:09:44,590 --> 00:09:42,500 was depositing my ice and I had that 258 00:09:46,180 --> 00:09:44,600 substrate that I could change the 259 00:09:48,699 --> 00:09:46,190 temperature I actually kept that 260 00:09:50,410 --> 00:09:48,709 substrate warmer and the idea is when 261 00:09:51,970 --> 00:09:50,420 when the substrate is warmer when the 262 00:09:53,920 --> 00:09:51,980 molecules leak into the chamber and they 263 00:09:56,410 --> 00:09:53,930 hit the substrate they have enough 264 00:09:59,620 --> 00:09:56,420 energy to relax and find sort of their 265 00:10:00,880 --> 00:09:59,630 lowest energy position and in that case 266 00:10:04,480 --> 00:10:00,890 we're actually going to wind up with a 267 00:10:06,430 --> 00:10:04,490 nice ordered crystal structure if I 268 00:10:08,980 --> 00:10:06,440 actually instead of doing that I 269 00:10:10,810 --> 00:10:08,990 actually kept my substrate colder 270 00:10:12,160 --> 00:10:10,820 I would actually wind up with an 271 00:10:14,650 --> 00:10:12,170 amorphous solid because when the 272 00:10:16,750 --> 00:10:14,660 molecules come in and stick they don't 273 00:10:19,030 --> 00:10:16,760 have enough energy to reorient they 274 00:10:21,310 --> 00:10:19,040 can't actually find their lowest energy 275 00:10:23,530 --> 00:10:21,320 equilibrium position relative to all of 276 00:10:25,180 --> 00:10:23,540 the other molecules in the solid so we 277 00:10:27,010 --> 00:10:25,190 wind up with this big amorphous blob and 278 00:10:29,140 --> 00:10:27,020 if you look again you know this this is 279 00:10:31,390 --> 00:10:29,150 water and there's this feature here that 280 00:10:32,980 --> 00:10:31,400 kind of you know maybe if you squint I 281 00:10:35,440 --> 00:10:32,990 mean it looks like this but it's bigger 282 00:10:39,010 --> 00:10:35,450 and broader and doesn't have as clean of 283 00:10:40,960 --> 00:10:39,020 features so we compare you know this 284 00:10:42,340 --> 00:10:40,970 spectrum taking at 10 Kelvin here with 285 00:10:43,780 --> 00:10:42,350 this spectrum take it at 10 Kelvin here 286 00:10:46,150 --> 00:10:43,790 there's an obvious there's an obvious 287 00:10:48,160 --> 00:10:46,160 difference okay but that's not a thermal 288 00:10:51,550 --> 00:10:48,170 history effect because I've just these 289 00:10:54,850 --> 00:10:51,560 are two separate ices but if I take this 290 00:10:57,310 --> 00:10:54,860 ice and I warm it up so you think if I 291 00:10:59,290 --> 00:10:57,320 warm something up all the way up to this 292 00:11:02,350 --> 00:10:59,300 say that the state same temperature at 293 00:11:03,970 --> 00:11:02,360 which I deposited the first ice it would 294 00:11:05,889 --> 00:11:03,980 have enough energy to reorient and 295 00:11:07,780 --> 00:11:05,899 become a crystalline solid in my 296 00:11:09,819 --> 00:11:07,790 spectrum should look just like this but 297 00:11:12,160 --> 00:11:09,829 as you can see from this top spectrum 298 00:11:13,310 --> 00:11:12,170 that's not the case so there is a 299 00:11:15,110 --> 00:11:13,320 feature that that looks 300 00:11:17,180 --> 00:11:15,120 like this but it's actually shifted 301 00:11:18,470 --> 00:11:17,190 relative to this peak and you know 302 00:11:21,680 --> 00:11:18,480 there's a lot more structure here than 303 00:11:23,360 --> 00:11:21,690 there is here so one of the things you 304 00:11:25,460 --> 00:11:23,370 can imagine happening is hey you are in 305 00:11:27,500 --> 00:11:25,470 a protoplanetary disk and some dust 306 00:11:29,450 --> 00:11:27,510 grain with some ice on it goes from you 307 00:11:31,130 --> 00:11:29,460 know colder spot to a warmer spot back 308 00:11:32,300 --> 00:11:31,140 to a colder spot you might actually be 309 00:11:35,600 --> 00:11:32,310 able to learn something about the 310 00:11:38,000 --> 00:11:35,610 history of that dust grain and thus the 311 00:11:40,670 --> 00:11:38,010 chemistry of what's going on in the disk 312 00:11:42,410 --> 00:11:40,680 and so with that the take home thoughts 313 00:11:44,750 --> 00:11:42,420 are really that you know terahertz 314 00:11:47,720 --> 00:11:44,760 spectroscopy is really sensitive to both 315 00:11:49,670 --> 00:11:47,730 the structure and a temperature of Isis 316 00:11:52,970 --> 00:11:49,680 we can just distinguish them with their 317 00:11:54,500 --> 00:11:52,980 thermal history and when we think that 318 00:11:56,360 --> 00:11:54,510 this is a this is going to be a useful 319 00:11:58,100 --> 00:11:56,370 tool to understanding complex molecule 320 00:11:59,840 --> 00:11:58,110 formation and to bring it all back to 321 00:12:01,190 --> 00:11:59,850 astrobiology if we can understand 322 00:12:02,870 --> 00:12:01,200 complex molecule formation 323 00:12:04,970 --> 00:12:02,880 maybe we can understand how we wind up 324 00:12:07,640 --> 00:12:04,980 with life on this planet and with that 325 00:12:09,320 --> 00:12:07,650 I'd like to say my lab mates and my 326 00:12:11,060 --> 00:12:09,330 advisor at all the people for funding 327 00:12:17,070 --> 00:12:11,070 and everybody for their attention thank 328 00:12:36,040 --> 00:12:31,930 questions for Marco Marco thanks for the 329 00:12:38,020 --> 00:12:36,050 talk so in one slice you show the ratio 330 00:12:42,190 --> 00:12:38,030 different ratio of the water and the 331 00:12:45,520 --> 00:12:42,200 methyl whatever the two organics so I'm 332 00:12:48,280 --> 00:12:45,530 just wondering if you can predict that 333 00:12:51,130 --> 00:12:48,290 when you get spectrum together I don't 334 00:12:52,840 --> 00:12:51,140 know if it is proportional four and if 335 00:12:56,650 --> 00:12:52,850 you can predict the ratio of the water 336 00:12:58,930 --> 00:12:56,660 to the organics are you saying could I 337 00:13:03,400 --> 00:12:58,940 could I predict what the spectrum looks 338 00:13:05,380 --> 00:13:03,410 like I would say that we we could maybe 339 00:13:07,660 --> 00:13:05,390 try although I think the theory these 340 00:13:10,150 --> 00:13:07,670 are kind of hard theoretical problems 341 00:13:14,920 --> 00:13:10,160 because they they do really require a 342 00:13:16,960 --> 00:13:14,930 picture that involves say what the what 343 00:13:20,440 --> 00:13:16,970 the unit cell structure looks like of 344 00:13:23,290 --> 00:13:20,450 say a crystalline material and if it's 345 00:13:25,300 --> 00:13:23,300 not crystalline it gets even harder so I 346 00:13:27,250 --> 00:13:25,310 would say it's possible but it's it's 347 00:13:34,840 --> 00:13:27,260 definitely a hard fioretto problem it's 348 00:13:37,750 --> 00:13:34,850 it's not one that we've looked at oh oh 349 00:13:39,550 --> 00:13:37,760 I see what you're saying okay sure the 350 00:13:41,080 --> 00:13:39,560 answer is yes and but what you'd have to 351 00:13:42,720 --> 00:13:41,090 do is you we'd have to do you know we'd 352 00:13:44,830 --> 00:13:42,730 have to have built up a library of 353 00:13:47,260 --> 00:13:44,840 spectra so they're taking spectra at 354 00:13:49,810 --> 00:13:47,270 different ratios and then we we would be 355 00:13:50,950 --> 00:13:49,820 able to figure out then say if we had a 356 00:13:53,080 --> 00:13:50,960 blank spectrum we didn't know what the 357 00:13:57,450 --> 00:13:53,090 ratio was we could compare it to our 358 00:13:59,470 --> 00:13:57,460 laboratory database and go from there