1 00:00:12,930 --> 00:00:10,110 chemistry and so first off really why do 2 00:00:15,570 --> 00:00:12,940 we even care about sulfur and so 3 00:00:20,010 --> 00:00:15,580 particularly sulfur compounds are found 4 00:00:21,690 --> 00:00:20,020 throughout Earth's atmosphere and down 5 00:00:24,240 --> 00:00:21,700 in the lower troposphere they mostly get 6 00:00:26,640 --> 00:00:24,250 rained out through because they're 7 00:00:28,800 --> 00:00:26,650 particularly good at being dissolved in 8 00:00:30,860 --> 00:00:28,810 the rain but up in the upper 9 00:00:33,869 --> 00:00:30,870 stratosphere we see this increase in so2 10 00:00:35,940 --> 00:00:33,879 and this is really important because 11 00:00:38,160 --> 00:00:35,950 these are a major source of aerosol 12 00:00:41,759 --> 00:00:38,170 particularly up in the stratosphere and 13 00:00:44,099 --> 00:00:41,769 so what happens is that sulfur gets 14 00:00:47,220 --> 00:00:44,109 oxidized to form sulfuric acid which 15 00:00:49,709 --> 00:00:47,230 thing can then seed aerosol and that 16 00:00:51,599 --> 00:00:49,719 aerosol does a particularly great job of 17 00:00:53,399 --> 00:00:51,609 scattering light and so it becomes 18 00:00:55,610 --> 00:00:53,409 really important when we're looking at 19 00:00:58,889 --> 00:00:55,620 climates and trying to understand 20 00:01:02,000 --> 00:00:58,899 different processes that are driving the 21 00:01:04,170 --> 00:01:02,010 temperature on a planet and so 22 00:01:08,010 --> 00:01:04,180 traditionally the idea with so2 23 00:01:12,450 --> 00:01:08,020 chemistry is the so2 reacts with o H to 24 00:01:14,789 --> 00:01:12,460 make this HS o 3 and that HS o 3 25 00:01:19,200 --> 00:01:14,799 immediately finds itself running into 26 00:01:21,480 --> 00:01:19,210 oxygen to make H 0 2 plus s 0 3 and then 27 00:01:23,520 --> 00:01:21,490 that s 03 through a water catalyzed 28 00:01:25,649 --> 00:01:23,530 reaction will form sulfuric acid and 29 00:01:27,149 --> 00:01:25,659 ultimately leads to these aerosol 30 00:01:30,029 --> 00:01:27,159 particles with through these small 31 00:01:33,060 --> 00:01:30,039 liquid or solid suspended particles in 32 00:01:35,340 --> 00:01:33,070 the atmosphere so I guess really the 33 00:01:37,170 --> 00:01:35,350 question is what's the problem and the 34 00:01:39,480 --> 00:01:37,180 problem is sulfur compounds have been 35 00:01:43,620 --> 00:01:39,490 observed throughout our solar system not 36 00:01:46,170 --> 00:01:43,630 just on earth in particularly there on 37 00:01:48,359 --> 00:01:46,180 Venus where we have these sulfuric acid 38 00:01:51,719 --> 00:01:48,369 clouds from 50 to 70 kilometers through 39 00:01:54,209 --> 00:01:51,729 the atmosphere but once you get above 40 00:01:56,099 --> 00:01:54,219 those clouds starting about 90 41 00:02:00,870 --> 00:01:56,109 kilometers there's this massive increase 42 00:02:02,819 --> 00:02:00,880 in so2 concentration and these increases 43 00:02:05,190 --> 00:02:02,829 in so2 really exceed any model 44 00:02:08,279 --> 00:02:05,200 predictions by orders of magnitude two 45 00:02:09,660 --> 00:02:08,289 or three orders of magnitude and so what 46 00:02:11,790 --> 00:02:09,670 this really is suggesting it there's 47 00:02:13,979 --> 00:02:11,800 some sort of chemical source of so2 in 48 00:02:16,949 --> 00:02:13,989 the middle atmosphere of Venus that we 49 00:02:19,470 --> 00:02:16,959 don't know about and interestingly 50 00:02:20,670 --> 00:02:19,480 enough this area has very 51 00:02:22,890 --> 00:02:20,680 similar conditions to Earth's 52 00:02:24,990 --> 00:02:22,900 stratosphere in miso sphere so similar 53 00:02:26,869 --> 00:02:25,000 temperatures pressures and water content 54 00:02:32,970 --> 00:02:26,879 is specifically what I'm talking about 55 00:02:35,220 --> 00:02:32,980 and so initially one suggested fix for 56 00:02:38,369 --> 00:02:35,230 this is some work that was done in the 57 00:02:41,400 --> 00:02:38,379 Vita group about 15 years ago I'm 58 00:02:45,180 --> 00:02:41,410 specifically looking at ir overtone 59 00:02:47,789 --> 00:02:45,190 stretches or overtone o-h stretches and 60 00:02:50,399 --> 00:02:47,799 the through this overtone you could put 61 00:02:54,420 --> 00:02:50,409 enough energy in to drive the fatah 62 00:02:57,240 --> 00:02:54,430 lysis of sulfuric acid to form wha water 63 00:03:02,400 --> 00:02:57,250 in s 03 and that s 03 can rapidly photo 64 00:03:05,369 --> 00:03:02,410 lies under standard UV conditions and so 65 00:03:07,559 --> 00:03:05,379 the idea behind this is that you put in 66 00:03:09,479 --> 00:03:07,569 your eye our photon you get this oh h 67 00:03:11,849 --> 00:03:09,489 stretch going and that hydrogen starts 68 00:03:15,180 --> 00:03:11,859 hopping around the molecule jumping from 69 00:03:17,910 --> 00:03:15,190 oxygen to oxygen and eventually it finds 70 00:03:20,160 --> 00:03:17,920 its way to the other oxygen that has a 71 00:03:22,710 --> 00:03:20,170 hydrogen and we get out water plus s 03 72 00:03:24,089 --> 00:03:22,720 this is a very fast process so high up 73 00:03:26,370 --> 00:03:24,099 in the atmosphere in these lower 74 00:03:33,390 --> 00:03:26,380 pressures it can actually out-compete 75 00:03:35,460 --> 00:03:33,400 the collisional deactivation and so a 76 00:03:37,140 --> 00:03:35,470 lot of work was done to actually go and 77 00:03:39,300 --> 00:03:37,150 measure these overtone stretches these 78 00:03:42,809 --> 00:03:39,310 going from V equals zero to four and 79 00:03:44,879 --> 00:03:42,819 five transitions and so you can see 80 00:03:48,000 --> 00:03:44,889 these happen in the red so in the 81 00:03:49,710 --> 00:03:48,010 visible this is particularly important 82 00:03:51,990 --> 00:03:49,720 because UV photons required for 83 00:03:53,580 --> 00:03:52,000 photolysis of sulfuric acid simply 84 00:03:56,550 --> 00:03:53,590 aren't available in the atmosphere 85 00:03:58,470 --> 00:03:56,560 they're filtered out via other 86 00:04:01,020 --> 00:03:58,480 absorption processes higher up in the 87 00:04:06,770 --> 00:04:01,030 atmosphere in Venus it's the co2 doing 88 00:04:09,030 --> 00:04:06,780 it and then interestingly enough these 89 00:04:12,240 --> 00:04:09,040 transitions do provide enough energy to 90 00:04:14,909 --> 00:04:12,250 get over this barrier about 40 kcal per 91 00:04:17,939 --> 00:04:14,919 mole to then go to this s 03 plus water 92 00:04:20,400 --> 00:04:17,949 and this does a really great job of 93 00:04:23,310 --> 00:04:20,410 explaining the so2 vertical profile on 94 00:04:25,379 --> 00:04:23,320 earth unfortunately it's still not good 95 00:04:27,529 --> 00:04:25,389 enough for Venus so even when this is 96 00:04:30,630 --> 00:04:27,539 included in the Venus models we are 97 00:04:32,370 --> 00:04:30,640 still in order or to an order of 98 00:04:35,180 --> 00:04:32,380 magnitude or two below 99 00:04:38,640 --> 00:04:35,190 so2 concentrations that are observed and 100 00:04:40,860 --> 00:04:38,650 so our thought was are there any other 101 00:04:44,520 --> 00:04:40,870 reservoirs for so2 anything else that 102 00:04:46,710 --> 00:04:44,530 could be hiding so2 and so what we are 103 00:04:51,050 --> 00:04:46,720 interested in is looking at sulfurous 104 00:04:54,600 --> 00:04:51,060 acid this h2s 03 and the idea is that 105 00:04:58,820 --> 00:04:54,610 through water a water catalyzed reaction 106 00:05:01,800 --> 00:04:58,830 this could go to s 0 2 plus water and 107 00:05:04,560 --> 00:05:01,810 unlike sulfuric acid sulfurous acid is 108 00:05:06,990 --> 00:05:04,570 energetically the unfavored product it's 109 00:05:08,820 --> 00:05:07,000 actually downhill to go to s 0 2 plus 110 00:05:11,070 --> 00:05:08,830 water and so it's actually really hard 111 00:05:12,870 --> 00:05:11,080 to observe this in the gas phase and 112 00:05:17,790 --> 00:05:12,880 actually hasn't ever been observed in 113 00:05:19,020 --> 00:05:17,800 the gas phase before and so you can see 114 00:05:21,030 --> 00:05:19,030 if you start with the sulfurous acid 115 00:05:22,590 --> 00:05:21,040 it's downhill to these products but you 116 00:05:24,690 --> 00:05:22,600 do have to go through this barrier so 117 00:05:27,090 --> 00:05:24,700 it's possible that with this higher 118 00:05:30,750 --> 00:05:27,100 barrier that there could be this so2 or 119 00:05:39,279 --> 00:05:30,760 this H to so3 product hiding in the 120 00:05:49,689 --> 00:05:47,139 I have a big picture no okay so what's 121 00:05:51,489 --> 00:05:49,699 interesting is we want to know how do 122 00:05:54,279 --> 00:05:51,499 you get sulfurous acid and how do you 123 00:05:56,559 --> 00:05:54,289 get up that hill to make that and so 124 00:05:59,499 --> 00:05:56,569 interestingly enough so2 has this strong 125 00:06:01,989 --> 00:05:59,509 absorption from 250 to 300 and 10 10 126 00:06:04,149 --> 00:06:01,999 nanometers in the atmosphere that's not 127 00:06:07,510 --> 00:06:04,159 filtered out in our atmosphere or and 128 00:06:10,119 --> 00:06:07,520 Venus's and so the idea is that you can 129 00:06:12,549 --> 00:06:10,129 excite from the ground state into this 130 00:06:15,159 --> 00:06:12,559 singlet excited state and then you 131 00:06:17,230 --> 00:06:15,169 internally convert you walk your way 132 00:06:19,689 --> 00:06:17,240 down and you find eventually you can get 133 00:06:23,049 --> 00:06:19,699 this internal conversion to a triplet 134 00:06:26,139 --> 00:06:23,059 state and so the direct process that 135 00:06:28,749 --> 00:06:26,149 goes here is forbidden but you can so2 136 00:06:30,909 --> 00:06:28,759 does make its way here it's known to 137 00:06:32,889 --> 00:06:30,919 react with organics to make sulfates and 138 00:06:41,079 --> 00:06:32,899 so the idea is that it can react with 139 00:06:42,369 --> 00:06:41,089 water to make h2s 03 and so we decided 140 00:06:45,549 --> 00:06:42,379 to do some experiments trying to 141 00:06:47,860 --> 00:06:45,559 actually make this sulfurous acid and so 142 00:06:50,499 --> 00:06:47,870 here i show that transition and what we 143 00:06:54,189 --> 00:06:50,509 use is a filter to cut out anything 144 00:06:57,730 --> 00:06:54,199 below about 300 nanometers specifically 145 00:06:59,439 --> 00:06:57,740 to avoid exciting this deeper UV 146 00:07:01,209 --> 00:06:59,449 absorption which can actually lead to 147 00:07:04,029 --> 00:07:01,219 Fatah lysis of so2 and drive other 148 00:07:08,320 --> 00:07:04,039 chemistry that we aren't interested in 149 00:07:10,959 --> 00:07:08,330 right now and so what we used is we have 150 00:07:14,199 --> 00:07:10,969 this simple glass cell with quartz 151 00:07:16,779 --> 00:07:14,209 windows and we used a this filter to cut 152 00:07:20,820 --> 00:07:16,789 out the higher energy UV light but let 153 00:07:24,040 --> 00:07:20,830 through all of this UVA light really and 154 00:07:29,739 --> 00:07:24,050 then we used a green laser to monitor 155 00:07:31,359 --> 00:07:29,749 the aerosol content in our cell and so 156 00:07:34,329 --> 00:07:31,369 interestingly enough when we turn on the 157 00:07:36,820 --> 00:07:34,339 light we immediately start generating 158 00:07:38,350 --> 00:07:36,830 aerosol it's not a secret that there's 159 00:07:40,269 --> 00:07:38,360 something going on it's not something 160 00:07:45,820 --> 00:07:40,279 you can't see you can visibly see this 161 00:07:47,860 --> 00:07:45,830 aerosol formation and so looking at the 162 00:07:50,050 --> 00:07:47,870 controls we wanted to make sure that 163 00:07:52,089 --> 00:07:50,060 this wasn't something that just shows up 164 00:07:52,690 --> 00:07:52,099 all the time and so if you start with 165 00:07:55,210 --> 00:07:52,700 just 166 00:07:58,210 --> 00:07:55,220 water we don't really see any changes or 167 00:08:01,300 --> 00:07:58,220 if we just use so2 we don't see anything 168 00:08:03,190 --> 00:08:01,310 going on but whenever we use a mixture 169 00:08:07,030 --> 00:08:03,200 of the two we immediately see this 170 00:08:08,680 --> 00:08:07,040 aerosol formation this decrease and so 171 00:08:10,870 --> 00:08:08,690 we're looking at this laser going 172 00:08:12,340 --> 00:08:10,880 through and you can immediately actually 173 00:08:14,950 --> 00:08:12,350 see the laser going through you can 174 00:08:17,320 --> 00:08:14,960 watch the particles move through it and 175 00:08:19,210 --> 00:08:17,330 so this is really exciting this is 176 00:08:21,040 --> 00:08:19,220 really some new results coming out of 177 00:08:23,980 --> 00:08:21,050 our group but what we think we're doing 178 00:08:29,020 --> 00:08:23,990 is actually making this so2 or this h2s 179 00:08:30,490 --> 00:08:29,030 03 and so I'd like to acknowledge the 180 00:08:31,740 --> 00:08:30,500 other members of the vitae group who've 181 00:08:35,170 --> 00:08:31,750 helped me with some of this work 182 00:08:37,420 --> 00:08:35,180 particularly a Katie Platt who is now a 183 00:08:40,390 --> 00:08:37,430 professor see you as well as jamie 184 00:08:42,520 --> 00:08:40,400 donaldson who is the collaborator doing 185 00:08:44,130 --> 00:08:42,530 a lot of the work on the theory end of 186 00:08:47,320 --> 00:08:44,140 this looking at the triplet state 187 00:08:48,760 --> 00:08:47,330 reactions of so2 um as well as our 188 00:09:01,150 --> 00:08:48,770 funding and thank you guys for your time 189 00:09:02,620 --> 00:09:01,160 have any questions for Jay all right in 190 00:09:05,530 --> 00:09:02,630 that case I will use my prerogative and 191 00:09:08,190 --> 00:09:05,540 ask question on my own so how would you 192 00:09:10,890 --> 00:09:08,200 go about confirming that it is h 2 sot 193 00:09:14,710 --> 00:09:10,900 one of the things we want to do is maybe 194 00:09:17,440 --> 00:09:14,720 use a mass spectrometer as well as i'm 195 00:09:19,810 --> 00:09:17,450 working and we just got our cavity ring 196 00:09:23,710 --> 00:09:19,820 down experiment up and going so i could 197 00:09:25,870 --> 00:09:23,720 actually use the this red cavity ring 198 00:09:28,120 --> 00:09:25,880 down to look at the o H stretches and 199 00:09:30,430 --> 00:09:28,130 actually confirm that i'm not making 200 00:09:31,810 --> 00:09:30,440 sulfuric acid because it is possible 201 00:09:34,840 --> 00:09:31,820 there are other rats that would take us 202 00:09:38,050 --> 00:09:34,850 to sulfuric acid we've been careful to 203 00:09:39,750 --> 00:09:38,060 try and remove all H so we pump the sell 204 00:09:41,680 --> 00:09:39,760 out overnight to remove everything 205 00:09:43,300 --> 00:09:41,690 unfortunately if we try and put an o H 206 00:09:45,700 --> 00:09:43,310 scavenger in the cell it turns out that 207 00:09:47,770 --> 00:09:45,710 the triplet state so2 really likes to 208 00:09:50,740 --> 00:09:47,780 react with that o H scavenger and 209 00:09:52,060 --> 00:09:50,750 generates even more impressive clouds so 210 00:09:57,910 --> 00:09:52,070 that's actually something that will be 211 00:09:59,350 --> 00:09:57,920 looking into next as well thank you any 212 00:10:01,600 --> 00:09:59,360 other questions everyone looks like 213 00:10:06,590 --> 00:10:01,610 they're about to applaud yeah but we got 214 00:10:12,960 --> 00:10:09,300 maybe I missed this but do you know what 215 00:10:19,020 --> 00:10:12,970 the reaction efficiency or what percent 216 00:10:21,900 --> 00:10:19,030 of sulfur gets transferred converted the 217 00:10:23,460 --> 00:10:21,910 HS 03 the h2s are three yeah we don't 218 00:10:24,810 --> 00:10:23,470 yet so that's the next thing that I'm 219 00:10:26,430 --> 00:10:24,820 really working on is actually getting 220 00:10:28,440 --> 00:10:26,440 the kinetics down for these sorts of 221 00:10:30,060 --> 00:10:28,450 reactions so that we can actually feed 222 00:10:32,940 --> 00:10:30,070 these back into the models and see 223 00:10:34,650 --> 00:10:32,950 what's going on there okay and I just 224 00:10:36,360 --> 00:10:34,660 another quick question maybe you haven't 225 00:10:39,120 --> 00:10:36,370 thought about this but you know if the 226 00:10:41,970 --> 00:10:39,130 sulfur isotope fractionation would be 227 00:10:43,650 --> 00:10:41,980 mass dependent during this process um so 228 00:10:45,990 --> 00:10:43,660 that's the other exciting thing as we 229 00:10:47,700 --> 00:10:46,000 suspect that it will be and because that 230 00:10:51,030 --> 00:10:47,710 internal conversion is dependent on the 231 00:10:53,430 --> 00:10:51,040 masses and that internal conversion is 232 00:10:55,350 --> 00:10:53,440 related to those vibrations and so 233 00:10:57,870 --> 00:10:55,360 that's another thing especially with 234 00:11:00,180 --> 00:10:57,880 that oh h scavenger that we use we want