WEBVTT

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<v Voiceover>Hello all.</v>

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This is Dr. Megan Sindelar

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and we are going to continue

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our sample calculations here

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in soil physical properties.

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This one for water content calculations.

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So this video assumes you have a general idea

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of the concept of soil water content

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and just want to see a worked problem.

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Here is the data set that we have been working with

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so a sample was collected in the field

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and there is our wet weight,

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goes in the oven at 105 degrees celsius

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for 24 hours to drive off the water

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and so we have a dry weight.

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So the difference between these two then

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would be considered to be the weight of water.

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So there are two ways that you can calculate

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water content.

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The first is water content by mass.

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So this is generally represented in textbooks

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with a lower case "w" or an italic lowercase "w".

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You may also see a sort of a percent,

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water by weight type of demarcation

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so this is mass of water over the mass of solids.

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Simply put a wet sample in the oven, dry it;

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you've got the weight of water,

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the weight of just solids.

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So that is water content by mass,

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sometimes called gravimetric water content.

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Then we've got water content by volume,

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sometimes called volumetric water content,

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generally represented in textbooks

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by the Greek letter theta

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or you might say theta "v"

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or you might see percent water by volume.

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All of those are for volumetric water content.

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So the mass water content is really easy to measure

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but it's not necessarily the most useful

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because as we look at the soil,

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mass water content doesn't really tell us

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relative amount of water.

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You need to know a volumetric water for that

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so our soil is 50% solids and then of our pores,

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what percent is water, what percent is air.

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That's what we really want to know.

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So volumetric water content is more useful.

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However, how do you measure volume of water?

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You really can't.

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So instead we have to get the mass of water

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and then use the density of water

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to convert that to a volume of water.

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So the density of water

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is one gram per cubic centimeter

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so it's a very simple conversion.

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Likewise, if we don't have volume total

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we could use bulk density in order to convert

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from our mass of solids to our volume total.

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So therefore if we have a mass of water,

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we have a mass of solids and we know the density

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of our water and our solids,

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we could calculate volumetric water content

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this way so water content by mass

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times the bulk density

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divided by the density of water.

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In this case I am using ROE to represent density.

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Alright let's do an example.

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So here's the formula, mass of water.

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Here then is our data

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so our mass of water

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would be the wet mass

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minus the dry mass

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and our mass of solids would be the dry mass

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minus the tin.

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So 215 minus 182 is 32 grams,

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183 minus 32 is 151 grams

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so 32 divided by 151,

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we've got zero point two one gram per gram.

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That's it.

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That's our gravimetric water content.

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Now even though you might think the grams cancel,

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please keep them.

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Write gram per gram so that

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when we look at this number,

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we know it is the water content by mass

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and not the water content by volume.

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Another thing to remember is that you need to use

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just the mass of solids here on the bottom.

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Most of our other calculations have mass total,

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volume total, total on the bottom.

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But the mass of solids is constant.

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The mass total would change as the mass of water

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change and it gets kind of messy

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if you have an equation where both the top

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and bottom are changing.

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So we use mass of solids on the bottom,

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please make sure that you do that.

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Okay so that's water content by mass.

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Like I said, it's easy to do.

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Water content by volume.

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So in this case, we do have the total volume

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of the soil so we can go ahead and use that.

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So our volume of water,

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we still need to come up with our mass of water.

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215 minus 183 and then it's basically

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divide this number by one.

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So one gram per centimeters cubed.

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Okay then on the bottom we've got 118.

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Okay so that's 32 grams

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divided by one gram per cubic centimeter

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over 118 cubic centimeters is 32 cubic centimeters.

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See, divide bottom by the bottom loops

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to the top?

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Over one 118 cubic centimeters

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is zero point two seven cubic centimeter

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per cubic centimeter

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for the volumetric water content.

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So again, you might think

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"Well these units cancel, I don't need em"

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but no, please keep these so that we know

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we're talking about water content by volume

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since we've got units of volume.

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Cause as you can see, this is a different number

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than our water content by mass was.

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Okay so this could be converted into a percent.

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This soil is 27% water.

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As you look over here, that seems pretty typical

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so we've got half solids, half pores

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that could be either water or air.

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In this one, slightly more than half of the pores

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is water.

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Seems normal.

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Okay but if we didn't have our volume total

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for this particular soil

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but we did have a bulk density

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then we could calculate

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our volumetric water content this way.

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So our water content by mass that we calculated

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was zero point two one gram per gram

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times our bulk density, previously calculated

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be one point two eight grams per cubic centimeter

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and then divide all of that

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by the density of water which is one gram

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per cubic centimeter.

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Okay so these grams are gonna cancel out

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with this and then what's on the bottom

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of the bottom will loop around to the top

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and so we'll be left with the answer in units

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of cubic centimeter per cubic centimeter

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which is appropriate for a volumetric water content

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and zero point two one times one point two eight

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divided by one is zero point two seven.

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The exact same volumetric water content

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that we got from calculating it the other way.

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So got a little self test there,

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we have done it correctly.

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Incidentally, what is the maximum

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volumetric water content that a soil can have?

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Yeah look at this right here.

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The water content at saturation

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would be equal to the porosity.

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You cannot have greater volume of water

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than you have volume of pores.

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So if we had a compacted soil

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with a low amount of porosity

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then our maximum water content would be

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a small number and if we had a really porous soil

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then our saturated water content could be

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a quite high number but generally,

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we're looking for something around 50%

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in an ideal, healthy soil.

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So those are some examples

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of calculating water content

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both by mass and by volume.

