WEBVTT 00:01.067 --> 00:03.636 position:10% line:85% size:80% Joan Cartan-Hansen, Host: Soil is more than just dirt. 00:03.636 --> 00:06.106 position:10% line:85% size:80% Without soil, there would be no life on our planet. 00:06.106 --> 00:07.841 position:10% line:85% size:80% So, find out more about soil. 00:07.841 --> 00:15.081 position:10% line:85% size:80% [MUSIC] 00:15.081 --> 00:18.451 position:10% line:85% size:80% Cartan-Hansen: Soil is the top layer of the earth. 00:18.451 --> 00:21.755 position:10% line:85% size:80% It's made of air and gas, bits of rock, minerals, water, 00:21.755 --> 00:25.024 position:10% line:85% size:80% decaying plants and tiny microbes. 00:25.024 --> 00:27.961 position:10% line:85% size:80% Soil forms in different layers on the earth. 00:27.961 --> 00:31.064 position:10% line:85% size:80% When soil scientists study layers of soil, they call it 00:31.064 --> 00:33.700 position:10% line:85% size:80% studying the soil profile. 00:33.700 --> 00:37.470 position:10% line:85% size:80% Topsoil is the layer you see, the layer you typically walk on. 00:37.470 --> 00:40.874 position:10% line:85% size:80% It contains dark organic material which is made up of 00:40.874 --> 00:42.909 position:10% line:85% size:80% decayed plant and animal matter. 00:42.909 --> 00:46.312 position:10% line:85% size:80% Topsoil can be about six inches thick. 00:46.312 --> 00:49.015 position:10% line:85% size:80% Under topsoil is sub-soil. 00:49.015 --> 00:52.018 position:10% line:85% size:80% It's from several inches to several feet thick. 00:52.018 --> 00:55.255 position:10% line:85% size:80% It looks lighter because it contains less humus, is more 00:55.255 --> 00:58.625 position:10% line:85% size:80% tightly packed and has slightly bigger pieces of rock. 00:58.625 --> 01:02.395 position:10% line:85% size:80% Next is the fragmented rock layer or the parent material. 01:02.395 --> 01:04.364 position:10% line:85% size:80% Nothing grows at this layer. 01:04.364 --> 01:08.334 position:10% line:85% size:80% It's made up of rock particles, sand, clay, salts and minerals. 01:08.334 --> 01:11.538 position:10% line:85% size:80% At the deepest level is solid bedrock. 01:11.538 --> 01:14.974 position:10% line:85% size:80% This is the layer of rock from which soil begins to form. 01:14.974 --> 01:18.912 position:10% line:85% size:80% Soil is created over lots of time. 01:18.912 --> 01:23.716 position:10% line:85% size:80% Rocks form when volcanos erupt or when sands get compressed. 01:23.716 --> 01:27.654 position:10% line:85% size:80% Weathering from wind, ice and rain breaks rocks into smaller 01:27.654 --> 01:28.755 position:10% line:85% size:80% parts. 01:28.755 --> 01:32.258 position:10% line:85% size:80% Plants grow in the cracks caused by erosion, creating more holes 01:32.258 --> 01:34.027 position:10% line:85% size:80% for air and water. 01:34.027 --> 01:36.663 position:10% line:85% size:80% They also drop leaves which decay. 01:36.663 --> 01:39.399 position:10% line:85% size:80% Animals leave waste products behind. 01:39.399 --> 01:42.669 position:10% line:85% size:80% Bacteria and fungi help break down dead plant and animal 01:42.669 --> 01:45.438 position:10% line:85% size:80% materials into smaller pieces. 01:45.438 --> 01:49.476 position:10% line:85% size:80% These combine with rock particles to make soil. 01:49.476 --> 01:52.212 position:10% line:85% size:80% Now, there are different types of soil. 01:52.212 --> 01:55.448 position:10% line:85% size:80% The type depends upon the original parent material, how 01:55.448 --> 01:58.785 position:10% line:85% size:80% big the rock particles are, the climate and what else is in the 01:58.785 --> 02:00.019 position:10% line:85% size:80% mixture. 02:00.019 --> 02:04.090 position:10% line:85% size:80% Student One: Clay is the smallest soil particle. 02:04.090 --> 02:09.162 position:10% line:85% size:80% Clay clumps because it can hold water better than some other 02:09.162 --> 02:10.797 position:10% line:85% size:80% types of soil. 02:10.797 --> 02:14.334 position:10% line:85% size:80% Student Two: Silt is powdery and soft to the touch and retains 02:14.334 --> 02:16.169 position:10% line:85% size:80% water well. 02:16.169 --> 02:19.005 position:10% line:85% size:80% Student Three: Sand is the largest soil particle. 02:19.005 --> 02:21.741 position:10% line:85% size:80% It's the least resistant to weathering. 02:21.741 --> 02:25.044 position:10% line:85% size:80% Student Four: Loam has the best soil for growing plants. 02:25.044 --> 02:29.082 position:10% line:85% size:80% It is an even combination of sand, silt and clay particles 02:29.082 --> 02:31.818 position:10% line:85% size:80% with organic materials. 02:31.818 --> 02:35.822 position:10% line:85% size:80% Cartan-Hansen: There are over 25,000 different named soils in 02:35.822 --> 02:37.724 position:10% line:85% size:80% the United States. 02:37.724 --> 02:41.060 position:10% line:85% size:80% Soil scientists are trained to be able to identify different 02:41.060 --> 02:43.997 position:10% line:85% size:80% types of soil and what they mean for the environment. 02:43.997 --> 02:45.732 position:10% line:85% size:80% Soil is very much alive. 02:45.732 --> 02:49.769 position:10% line:85% size:80% One tablespoon of soil contains more microbes than there are 02:49.769 --> 02:51.704 position:10% line:85% size:80% humans on the earth. 02:51.704 --> 02:55.174 position:10% line:85% size:80% Insects, bacteria, earth worms and other creatures live in 02:55.174 --> 02:56.109 position:10% line:85% size:80% soil. 02:56.109 --> 02:59.012 position:10% line:85% size:80% Larger animals do, too, like badgers and snakes. 02:59.012 --> 03:03.149 position:10% line:85% size:80% Soil filters our water, holding back contaminants and taking out 03:03.149 --> 03:04.617 position:10% line:85% size:80% impurities. 03:04.617 --> 03:07.754 position:10% line:85% size:80% Soil is used in construction and provides the foundation upon 03:07.754 --> 03:10.490 position:10% line:85% size:80% which our homes and businesses are built. 03:10.490 --> 03:13.960 position:10% line:85% size:80% And importantly, plants need soils to provide them with 03:13.960 --> 03:15.662 position:10% line:85% size:80% minerals and nutrients. 03:15.662 --> 03:18.998 position:10% line:85% size:80% Soils scientists help farmers understand what plants to grow, 03:18.998 --> 03:23.369 position:10% line:85% size:80% and how to improve the soil to increase their crop yields. 03:23.369 --> 03:26.205 position:10% line:85% size:80% Student: Soil is an essential natural resource. 03:26.205 --> 03:29.475 position:10% line:85% size:80% It's food for some animals and home for others. 03:29.475 --> 03:33.813 position:10% line:85% size:80% Soil cleans our water, provides nutrients for plants and gives 03:33.813 --> 03:35.882 position:10% line:85% size:80% us a place to live. 03:35.882 --> 03:37.817 position:10% line:85% size:80% So learn about soil. 03:37.817 --> 03:39.986 position:10% line:85% size:80% Dig in! 03:39.986 --> 03:43.356 position:10% line:85% size:80% Cartan-Hansen: If you want to learn more about soil, check out 03:43.356 --> 03:44.724 position:10% line:85% size:80% the science trek website. 03:44.724 --> 03:48.027 position:10% line:85% size:80% You'll find it at science trek dot org. 03:48.027 --> 04:06.779 position:10% line:85% size:80% [MUSIC] 04:06.779 --> 04:08.147 position:10% line:85% size:80% ANNOUNCER: Presentation of 04:08.147 --> 04:11.117 position:10% line:85% size:80% Science Trek on Idaho Public Television is made possible 04:11.117 --> 04:13.886 position:10% line:85% size:80% through the generous support of the Laura Moore Cunningham 04:13.886 --> 04:16.856 position:10% line:85% size:80% Foundation, committed to fulfilling the Moore and Bettis 04:16.856 --> 04:20.460 position:10% line:85% size:80% family legacy of building the great state of Idaho. 04:20.460 --> 04:23.796 position:10% line:85% size:80% By the Idaho National Laboratory, mentoring talent and 04:23.796 --> 04:28.067 position:10% line:85% size:80% finding solutions for energy and security challenges, by The 04:28.067 --> 04:31.170 position:10% line:85% size:80% Friends of Idaho Public Television and by the 04:31.170 --> 04:32.171 position:10% line:85% size:80% Corporation for Public