1 00:00:05,510 --> 00:00:07,010 BABATUNDE OGUNLADE: Hello, everyone. 2 00:00:07,010 --> 00:00:08,718 Today we'll be working through Goodie Bag 3 00:00:08,718 --> 00:00:10,552 3, which is on ionic solids. 4 00:00:10,552 --> 00:00:12,260 In order to work through this Goodie Bag, 5 00:00:12,260 --> 00:00:15,080 you'll need a conductivity meter, some small measuring 6 00:00:15,080 --> 00:00:19,310 cups, some medium sized cups, a small scale, a writing utensil, 7 00:00:19,310 --> 00:00:21,800 some nitrile gloves, some stirrers, 8 00:00:21,800 --> 00:00:23,240 and four unique solids. 9 00:00:23,240 --> 00:00:26,480 Today, I'll be using sodium chloride, magnesium sulfate, 10 00:00:26,480 --> 00:00:29,240 magnesium oxide, and sucrose. 11 00:00:29,240 --> 00:00:32,540 Our main objective today is to use solubility and conductivity 12 00:00:32,540 --> 00:00:34,580 measurements to determine if a given solid is 13 00:00:34,580 --> 00:00:36,850 an ionic or covalent compound. 14 00:00:36,850 --> 00:00:39,720 And as we do this, I'd like you to think about two questions. 15 00:00:39,720 --> 00:00:42,530 First, how do solids dissolve in water? 16 00:00:42,530 --> 00:00:45,590 And second, what factors may influence how conductive 17 00:00:45,590 --> 00:00:47,920 a given solid is in water? 18 00:00:47,920 --> 00:00:50,420 So first we're going to look at the solubility of our solids 19 00:00:50,420 --> 00:00:51,680 in water. 20 00:00:51,680 --> 00:00:54,590 And to do this, we're going to dissolve 1 gram of each solid 21 00:00:54,590 --> 00:00:56,660 in 30 milliliters of water. 22 00:00:56,660 --> 00:00:59,040 I've already weighed out my solids here. 23 00:00:59,040 --> 00:01:01,610 And I've also already weighed out my water. 24 00:01:01,610 --> 00:01:04,012 Notice how I'm wearing a pair of nitrile gloves. 25 00:01:04,012 --> 00:01:05,720 The compounds that I'm working with today 26 00:01:05,720 --> 00:01:08,210 aren't that dangerous, but just as general safety, 27 00:01:08,210 --> 00:01:11,160 it's good to wear gloves when handling compounds. 28 00:01:11,160 --> 00:01:13,970 So I'm going to pour each solute into each respective cup 29 00:01:13,970 --> 00:01:17,330 of water and stir and mix for about a minute to two minutes 30 00:01:17,330 --> 00:01:21,120 and see if the compound dissolves. 31 00:01:21,120 --> 00:01:23,760 So after one to two minutes of stirring and dissolving, 32 00:01:23,760 --> 00:01:26,910 you can see that our magnesium oxide right here has not 33 00:01:26,910 --> 00:01:28,150 dissolved in our water. 34 00:01:28,150 --> 00:01:30,548 You can see a very clear boundary between the solute, 35 00:01:30,548 --> 00:01:32,340 which has settled at the bottom of the cup, 36 00:01:32,340 --> 00:01:34,320 and the water, which is on top. 37 00:01:34,320 --> 00:01:36,510 If you compare that to our sodium chloride, 38 00:01:36,510 --> 00:01:38,320 though, if you look very carefully, 39 00:01:38,320 --> 00:01:40,860 you can see that our solute has dissolved 40 00:01:40,860 --> 00:01:43,302 very well in our water. 41 00:01:43,302 --> 00:01:44,760 So the next thing we'll be doing is 42 00:01:44,760 --> 00:01:47,220 measuring the conductivity of our compounds 43 00:01:47,220 --> 00:01:48,875 when dissolved in water. 44 00:01:48,875 --> 00:01:50,250 And to do that, we're going to be 45 00:01:50,250 --> 00:01:54,010 using a handy dandy conductivity meter that I have right here. 46 00:01:54,010 --> 00:01:56,820 So I have some cups of water prepared here 47 00:01:56,820 --> 00:01:59,880 to be used as both a baseline correction 48 00:01:59,880 --> 00:02:02,580 when we're measuring our conductivity of our compounds 49 00:02:02,580 --> 00:02:06,750 and as a water bath to clean our probe in between measurements. 50 00:02:06,750 --> 00:02:09,600 OK, so first I'm going to turn on my conductivity measure. 51 00:02:12,447 --> 00:02:14,280 And I'm going to make sure that my units are 52 00:02:14,280 --> 00:02:16,320 set to microsiemens per centimeter, 53 00:02:16,320 --> 00:02:18,580 or some equivalent unit. 54 00:02:18,580 --> 00:02:21,650 And first I'm going to measure a baseline of just regular water 55 00:02:21,650 --> 00:02:22,150 here. 56 00:02:22,150 --> 00:02:24,030 I have tap water here. 57 00:02:24,030 --> 00:02:28,290 And so when I do that, I see that I'm 58 00:02:28,290 --> 00:02:31,000 measuring around 900 microsiemens per centimeter. 59 00:02:31,000 --> 00:02:33,355 So that is the connectivity of my water as is. 60 00:02:33,355 --> 00:02:34,980 And I'm going to use that as a baseline 61 00:02:34,980 --> 00:02:36,438 when I'm measuring the connectivity 62 00:02:36,438 --> 00:02:37,800 of my other compounds. 63 00:02:40,650 --> 00:02:42,530 So since this is water, it's already clean, 64 00:02:42,530 --> 00:02:44,300 and now I'm going to measure my sodium chloride, which 65 00:02:44,300 --> 00:02:44,883 is right here. 66 00:02:50,960 --> 00:02:55,080 And so right now I'm reading around 4,700 microsiemens 67 00:02:55,080 --> 00:02:56,758 per centimeter for my sodium chloride. 68 00:02:56,758 --> 00:02:58,050 I'm going to take note of that. 69 00:02:58,050 --> 00:02:59,883 And eventually, when I'm collecting my data, 70 00:02:59,883 --> 00:03:04,230 I'm going to subtract my water baseline from this value here. 71 00:03:04,230 --> 00:03:05,970 Make sure in between each measurement 72 00:03:05,970 --> 00:03:09,240 that you dip the probe in the water bath to clean it, 73 00:03:09,240 --> 00:03:13,210 and you can continue on with the rest of your measurements. 74 00:03:13,210 --> 00:03:15,180 So the last experiment we're going to do today 75 00:03:15,180 --> 00:03:17,460 is to measure the solubility of our compounds 76 00:03:17,460 --> 00:03:21,270 in water, except with 2 grams instead of 1 gram. 77 00:03:21,270 --> 00:03:23,820 So I've measured out an additional 1 gram of each solid 78 00:03:23,820 --> 00:03:25,590 here, and I'm just going to pour each one 79 00:03:25,590 --> 00:03:27,875 into each respective cup, mix and stir. 80 00:03:27,875 --> 00:03:29,250 And after one to two minutes, I'm 81 00:03:29,250 --> 00:03:32,750 going to see if each compound is dissolved. 82 00:03:32,750 --> 00:03:35,030 So again, we have our magnesium oxide 83 00:03:35,030 --> 00:03:37,060 after round two of solubility. 84 00:03:37,060 --> 00:03:39,380 Again, we can see that our solute has not 85 00:03:39,380 --> 00:03:40,190 dissolved in water. 86 00:03:40,190 --> 00:03:43,100 There's a very clear boundary between the water on top 87 00:03:43,100 --> 00:03:44,640 and the solute on the bottom. 88 00:03:44,640 --> 00:03:47,120 So in this case, round one solubility and round 89 00:03:47,120 --> 00:03:49,340 two solubility look identical, but it may not 90 00:03:49,340 --> 00:03:52,160 be the case for our other three solutes. 91 00:03:52,160 --> 00:03:54,650 All right, so now that we've finished our last solubility 92 00:03:54,650 --> 00:03:56,960 test, let's put all our data-- 93 00:03:56,960 --> 00:03:59,840 our first solubility test, our connectivity test, 94 00:03:59,840 --> 00:04:01,370 and our second solubility test-- 95 00:04:01,370 --> 00:04:03,320 on the board. 96 00:04:03,320 --> 00:04:07,230 So here we have a chart of all the data from our experiments. 97 00:04:07,230 --> 00:04:10,140 I have the compounds that we use going down right here. 98 00:04:10,140 --> 00:04:13,470 And I have solubility here at 1 gram and 2 grams, 99 00:04:13,470 --> 00:04:16,660 and conductivity after water subtraction here. 100 00:04:16,660 --> 00:04:19,440 So before going into this data, first thing 101 00:04:19,440 --> 00:04:22,019 I would like us to notice is that for sodium chloride 102 00:04:22,019 --> 00:04:25,890 and for magnesium sulfate, these conductivity values 103 00:04:25,890 --> 00:04:27,990 are much lower than I expected. 104 00:04:27,990 --> 00:04:30,230 This should be close to the 10,000 microsiemens, 105 00:04:30,230 --> 00:04:32,430 and this should be closer to 8,000 microsiemens 106 00:04:32,430 --> 00:04:34,260 per centimeter, but the fact that we're 107 00:04:34,260 --> 00:04:37,380 able to measure conductivity for these respective compounds 108 00:04:37,380 --> 00:04:40,570 gives us insight into what type of compounds they are. 109 00:04:40,570 --> 00:04:42,640 So first, if we look at sodium chloride, 110 00:04:42,640 --> 00:04:46,320 we could see that at both 1 gram and 2 grams, 111 00:04:46,320 --> 00:04:48,720 our sodium chloride was able to dissolve in water. 112 00:04:48,720 --> 00:04:52,020 And we were able to measure conductivity readings for this. 113 00:04:52,020 --> 00:04:53,970 This means our sodium chloride was 114 00:04:53,970 --> 00:04:57,420 able to dissociate into ions when dissolved in water. 115 00:04:57,420 --> 00:04:59,040 And this is an extra check for us 116 00:04:59,040 --> 00:05:01,125 to determine that sodium chloride is indeed 117 00:05:01,125 --> 00:05:02,085 an ionic compound. 118 00:05:06,030 --> 00:05:08,370 Next we can look at magnesium oxide. 119 00:05:08,370 --> 00:05:13,770 And we see that for magnesium oxide, at 1 gram and 2 grams, 120 00:05:13,770 --> 00:05:16,550 we weren't able to dissolve the magnesium oxide in water. 121 00:05:16,550 --> 00:05:18,570 And not only that, because of that, 122 00:05:18,570 --> 00:05:20,490 we weren't able to measure any conductivity. 123 00:05:20,490 --> 00:05:24,600 But we know that magnesium oxide is an ionic compound 124 00:05:24,600 --> 00:05:26,770 just from our understanding of bonding. 125 00:05:26,770 --> 00:05:30,670 So we had to think more closely about why this is the case. 126 00:05:30,670 --> 00:05:33,630 So magnesium oxide and sodium chloride 127 00:05:33,630 --> 00:05:36,480 are both ionic compounds, but magnesium oxide 128 00:05:36,480 --> 00:05:39,810 has a much higher lattice energy than sodium chloride. 129 00:05:39,810 --> 00:05:43,800 This means that when magnesium oxide is placed in water, 130 00:05:43,800 --> 00:05:45,780 it's more energetically favorable for it 131 00:05:45,780 --> 00:05:50,070 to stay as a solid than it is to dissociate into ions 132 00:05:50,070 --> 00:05:56,100 of magnesium and oxygen. So magnesium oxide is still 133 00:05:56,100 --> 00:05:58,380 an ionic compound, but it's lattice energy 134 00:05:58,380 --> 00:06:01,410 is high enough such that it does not dissolve and does not give 135 00:06:01,410 --> 00:06:04,470 us conductivity measurements. 136 00:06:04,470 --> 00:06:06,630 So it's still ionic. 137 00:06:06,630 --> 00:06:08,700 Now we can look at magnesium sulfate. 138 00:06:08,700 --> 00:06:12,530 And we see that for 1 gram, we do get some solubility. 139 00:06:12,530 --> 00:06:15,635 And at 2 grams, we get no solubility. 140 00:06:15,635 --> 00:06:17,700 It was not able to dissolve. 141 00:06:17,700 --> 00:06:20,220 And we're able to measure some conductivity. 142 00:06:20,220 --> 00:06:23,620 This means that magnesium sulfate dissociated 143 00:06:23,620 --> 00:06:26,460 into respective ions and we're able to measure 144 00:06:26,460 --> 00:06:28,650 some conductivity while in water. 145 00:06:28,650 --> 00:06:31,410 But magnesium sulfate has a limited solubility 146 00:06:31,410 --> 00:06:33,397 in water, which is why at 2 grams 147 00:06:33,397 --> 00:06:34,980 it wasn't able to dissolve completely. 148 00:06:34,980 --> 00:06:40,020 So magnesium sulfate is still an ionic compound. 149 00:06:40,020 --> 00:06:42,090 Finally, if we look at sucrose, we 150 00:06:42,090 --> 00:06:44,580 see that we were able to get 1 gram of sucrose 151 00:06:44,580 --> 00:06:47,010 to dissolve in water, and 2 grams of sucrose 152 00:06:47,010 --> 00:06:48,540 was able to dissolve in water. 153 00:06:48,540 --> 00:06:51,570 But we were not able to get any conductivity. 154 00:06:51,570 --> 00:06:54,090 This means that sucrose dissolved in water, 155 00:06:54,090 --> 00:06:57,750 but did not dissociate into respective ions. 156 00:06:57,750 --> 00:06:59,790 So if you think about the structure of sucrose, 157 00:06:59,790 --> 00:07:05,790 sucrose has a bunch of polar groups on it, which make 158 00:07:05,790 --> 00:07:07,530 it able to dissolve in water. 159 00:07:07,530 --> 00:07:10,570 But sucrose does not dissociate into ions, 160 00:07:10,570 --> 00:07:13,050 which is why we were not able to measure any conductivity. 161 00:07:13,050 --> 00:07:15,325 So sucrose is a covalent compound. 162 00:07:20,560 --> 00:07:23,490 So by using our knowledge of bonding and our solubility 163 00:07:23,490 --> 00:07:26,550 and conductivity data, we're able to affirm 164 00:07:26,550 --> 00:07:29,190 the identity of our compounds. 165 00:07:29,190 --> 00:07:32,490 That is, whether or not they're ionic or covalent. 166 00:07:32,490 --> 00:07:34,080 So today we looked at how the type 167 00:07:34,080 --> 00:07:36,300 and strength of bonding of a solid 168 00:07:36,300 --> 00:07:38,280 influences its properties. 169 00:07:38,280 --> 00:07:41,100 Specifically, we looked at how these aspects of bonding 170 00:07:41,100 --> 00:07:44,100 influence these solubility and conductivity 171 00:07:44,100 --> 00:07:46,670 of these solids in water.