WEBVTT - BrainStuff Classics: Why Are the Oceans Salty?

0:00:01.920 --> 0:00:06.840
<v Speaker 1>Welcome to brain Stuff production of iHeart Radio. Hey brain Stuff,

0:00:06.840 --> 0:00:09.680
<v Speaker 1>I'm Lauren vogel Bomb, and today's episode is another classic

0:00:09.720 --> 0:00:14.440
<v Speaker 1>from our archive. Today's question is fairly direct. Why are

0:00:14.480 --> 0:00:18.720
<v Speaker 1>Earth's oceans and select other bodies of water salty whereas

0:00:18.840 --> 0:00:24.040
<v Speaker 1>rivers and most lakes are fresh? Hi brain Stuff, Lauren

0:00:24.120 --> 0:00:26.840
<v Speaker 1>vogel Bomb. Here. Anyone who's taken a dunk in the

0:00:26.880 --> 0:00:30.159
<v Speaker 1>ocean is familiar with the shock and mild sting the

0:00:30.200 --> 0:00:33.800
<v Speaker 1>water is so salty. To understand why the seas are salty,

0:00:33.960 --> 0:00:37.000
<v Speaker 1>look no further than the water cycle. Simply put, the

0:00:37.040 --> 0:00:39.600
<v Speaker 1>water cycle begins when fresh water falls from the sky

0:00:39.680 --> 0:00:42.720
<v Speaker 1>in the form of rain. It eventually ends up in rivers, lakes,

0:00:42.720 --> 0:00:45.559
<v Speaker 1>and oceans, where it soon evaporates to form clouds and

0:00:45.680 --> 0:00:48.720
<v Speaker 1>repeat the cycle. If you dig a little deeper into

0:00:48.720 --> 0:00:51.159
<v Speaker 1>each stage of the water cycle, you'll see just how

0:00:51.200 --> 0:00:54.080
<v Speaker 1>salt gets into the mix. That fresh water that falls

0:00:54.080 --> 0:00:57.960
<v Speaker 1>as rain isn't pure. It mixes with the carbon dioxide

0:00:57.960 --> 0:01:00.280
<v Speaker 1>in the atmosphere on the way down, giving it a

0:01:00.360 --> 0:01:03.760
<v Speaker 1>slightly acidic quality. Once it reaches the Earth's surface, it

0:01:03.840 --> 0:01:07.360
<v Speaker 1>travels over land to reach area waterways. As it passes

0:01:07.400 --> 0:01:09.880
<v Speaker 1>over the land, the acidic nature of the water breaks

0:01:09.880 --> 0:01:13.160
<v Speaker 1>down rocks, capturing ions within these rocks and carrying them

0:01:13.160 --> 0:01:16.959
<v Speaker 1>along to the sea. Roughly of these ions are sodium

0:01:17.040 --> 0:01:21.000
<v Speaker 1>or chloride, which forms salt when they band together. Fresh

0:01:21.000 --> 0:01:24.160
<v Speaker 1>water that reaches the ocean evaporates to form clouds. However,

0:01:24.280 --> 0:01:27.600
<v Speaker 1>these sodium, chloride and other ions remain behind, where they

0:01:27.600 --> 0:01:30.840
<v Speaker 1>accumulate over time to give the sea its characteristic saltiness.

0:01:31.440 --> 0:01:34.720
<v Speaker 1>Hydrothermal vents on the ocean floor release additional dissolved materials,

0:01:34.920 --> 0:01:38.360
<v Speaker 1>including more sodium and chloride, further contributing to the briny

0:01:38.400 --> 0:01:41.760
<v Speaker 1>nature of the sea. What's surprising is just how much

0:01:41.800 --> 0:01:44.399
<v Speaker 1>the salt from runoff and underwater vents has built up

0:01:44.480 --> 0:01:47.720
<v Speaker 1>since the oceans formed. Dissolved salts make up three point

0:01:47.760 --> 0:01:50.400
<v Speaker 1>five percent of the weight of all ocean water, and

0:01:50.600 --> 0:01:52.440
<v Speaker 1>if you could remove the salt from the sea, it

0:01:52.480 --> 0:01:54.880
<v Speaker 1>would form a layer five hundred feet that's a hundred

0:01:54.880 --> 0:01:58.000
<v Speaker 1>and fifty three meters thick over all of Earth's land mass.

0:01:58.400 --> 0:02:02.240
<v Speaker 1>That's about the height of a forty story building. One question, though,

0:02:02.600 --> 0:02:05.400
<v Speaker 1>if these seas get their salinity from runoff, why do

0:02:05.560 --> 0:02:09.360
<v Speaker 1>lakes remain relatively salt free for most lakes. Water flows

0:02:09.400 --> 0:02:12.200
<v Speaker 1>both in and out of the lake via rivers and streams.

0:02:12.520 --> 0:02:14.959
<v Speaker 1>Salt Ions that end up in the water are carried out,

0:02:15.120 --> 0:02:18.720
<v Speaker 1>keeping the lake fresh. These ions eventually end up in oceans,

0:02:18.840 --> 0:02:21.360
<v Speaker 1>which serve as a dumping ground of sorts for runoff

0:02:21.400 --> 0:02:24.880
<v Speaker 1>and the materials it contains. Bodies of water with no outflow,

0:02:24.960 --> 0:02:27.000
<v Speaker 1>such as the Dead Sea or the Great Salt Lake

0:02:27.000 --> 0:02:29.720
<v Speaker 1>in Utah, maintain a level of salinity on par with

0:02:30.040 --> 0:02:36.880
<v Speaker 1>or higher than that of the ocean. Today's episode was

0:02:36.919 --> 0:02:39.520
<v Speaker 1>originally produced by Tristan McNeil and is based on the

0:02:39.600 --> 0:02:42.480
<v Speaker 1>article why is seawater salty? On how stuff works dot

0:02:42.520 --> 0:02:45.720
<v Speaker 1>Com written by Bambi Turner. Brain Stuff is production of

0:02:45.760 --> 0:02:48.320
<v Speaker 1>by Heart Radio in partnership with how stuffworks dot Com

0:02:48.360 --> 0:02:51.440
<v Speaker 1>and is produced by Tylor Clang. Four more podcasts. My

0:02:51.480 --> 0:02:54.560
<v Speaker 1>heart Radio isn't the iHeart Radio app, Apple Podcasts or

0:02:54.600 --> 0:02:56.360
<v Speaker 1>wherever you listen into your favorite shows