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Osmosis and Water Potential (Updated)

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    (MUSIC)
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    When we were kids, growing up in West Texas, our winters would be cold, but rarely experienced
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    snow.
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    But we did have ice, which resulted in the roads being salted.
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    As the salt mixes in and dissolves into water on the road, this can lead to a lower freezing
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    point, which can help prevent the roads from icing over.
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    And while this is great for making the roads more safe, it wasn’t so great for the plants
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    that lived right along the roadside.
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    It often caused them to die.
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    Now winter can be hard for many plant species, but I’m talking about this salt affecting
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    even some hardy plant life.
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    This issue with salt and plants isn’t limited to winter.
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    During hurricanes near the coast, salty ocean water can be dumped in large quantities into the
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    soil.
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    This can eventually kill plants- including
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    trees- that had originally survived the hurricane.
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    Why?
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    Do plants just dislike salt that much?
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    Well, it's actually related to a term called osmosis.
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    When you are talking about osmosis, you are talking about the movement of water through a
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    semi-permeable membrane, like a cell membrane.
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    Water molecules are so small that they can travel through the cell membrane unassisted,
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    or they can travel in larger quantities through protein channels like aquaporins.
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    The movement of water molecules traveling across a cell membrane is passive transport,
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    which means, it does not require energy.
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    In osmosis, water molecules travel from areas of a high concentration (of water molecules)
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    to a low concentration (of water molecules).
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    But there’s another way to think about water movement in osmosis.
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    A low water concentration likely means there is a greater solute concentration.
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    Solutes are substances like salt or sugar that can be dissolved within a solvent like
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    water.
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    Water has the tendency to move to areas where there is a higher solute concentration, which
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    would mean less water concentration.
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    So, if you want to easily figure out where the water will travel in osmosis, look to the side
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    where there is a greater solute concentration.
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    Unless we bring in another variable, like pressure, water will generally have a net
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    movement to the area of higher solute concentration.
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    So, let’s bring out a U-tube!
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    Ha, U-tube.
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    That’s funny.
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    There’s a semi-permeable membrane in the middle of it.
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    Let’s assume that it is similar to a cell membrane and that water molecules can squeeze
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    through it—the molecules are quite small—but salt can’t.
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    Right now, there is just water in this U-tube.
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    The water levels on side A and side B are equal.
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    That doesn’t mean that the water molecules aren’t moving---water molecules like to
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    move---but the net movement across the two
    sides is zero.
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    That means, the overall change in the direction of movement is zero.
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    Now let’s imagine on side B, you dump a huge amount of salt there.
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    So, which direction will the water initially move towards, A or B?
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    Think about what we mentioned with osmosis.
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    The answer is B!
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    Side B has a higher solute concentration than side A. Water moves to areas of higher solute
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    concentration, which is also the area of lower water concentration.
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    You will also see the water level on side B rise as the water moves to that area.
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    You can almost think of the water as trying to equalize the concentrations diluting
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    side B. Once equilibrium is reached, the net movement of water across the two sides will
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    be zero, but remember that water still likes to move and movement still occurs.
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    Now here’s some vocabulary to add in here---we call side B hypertonic.
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    That means higher solute concentration!
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    But we can’t just say something is hypertonic without comparing it to something else.
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    We say side B is hypertonic to side A because it has a higher solute concentration than
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    side A. In osmosis, water moves to the hypertonic side.
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    We say side A is hypotonic (hypo rhymes with low which helps me remember that it is the low solute concentration)
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    when compared to side B. Let’s get a little more real life now instead
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    of just the U-tube.
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    As you know, water is important for your body and many processes that occur in the body.
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    When someone gets an IV in a hospital, it may look like the fluid in the IV is just
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    pure water.
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    But it is certainly not pure water.
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    That would be a disaster because of osmosis, let’s explain.
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    Let’s say hypothetically pure water was in an IV.
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    Now an IV tube typically runs through a vein, so that you have access to your blood stream,
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    really useful for running medication through.
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    Blood actually consists of many different types of components and red blood cells are
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    a great example.
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    So, what do you think has a higher solute concentration,
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    the hypothetical pure water in this IV tube
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    or the red blood cells?
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    Well, cells are not empty vessels, they contain solutes.
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    The pure water that hypothetically is running through this IV tube has no solutes.
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    So, where does the water go?
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    It goes to the area of higher solute concentration which in this case is inside the cells.
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    The cells are hypertonic compared to the pure water in the IV tube because the cells have
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    a greater solute concentration,
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    the cells would swell and possibly burst!
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    Exploding red blood cells are not good.
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    If a person needs fluids, they typically will receive a solution that is isotonic to their
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    blood plasma.
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    Isotonic means equal concentration, so you won’t have any swelling or shrinking red
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    blood cells.
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    Another example, let’s talk about the aquarium.
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    I have always wanted a saltwater fish tank, ever since I was a little kid.
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    But I’ve only had freshwater tanks
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    so far.
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    I did often question when I was a kid, why is it that a saltwater fish can’t be in
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    my freshwater tank?
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    Well, let me explain one reason why this would be dangerous to a saltwater fish and how it
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    relates to osmosis.
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    First ask---where is there a higher solute concentration?
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    In the saltwater fish cells
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    or in the freshwater that the fish would be hypothetically placed in?
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    Definitely in the saltwater fish cells.
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    So, where would the water go?
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    It goes to the area where there is a higher solute concentration----the hypertonic side----so
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    it goes into the cells of that poor saltwater fish.
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    If not rescued, it could die.
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    Now one thing to clarify: saltwater fish and freshwater fish are not necessarily isotonic to
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    their surroundings.
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    But they have special adaptations that allow them to live in their environment and usually
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    cannot make a major switch from a saltwater environment to a freshwater one.
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    Now---not all fish have this problem.
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    There are some fish that have this amazing adaptations to switch between fresh and salt water, and
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    they have to deal with this osmosis problem.
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    Salmon for example.
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    I think if I could pick to be a fish, I’d be a salmon.
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    Osmosis
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    explains how many kinds of plants get their water.
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    Sure, many plants have roots.
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    But how does the water get into the roots?
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    When it rains, the soil becomes saturated with water.
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    The root hair cells generally have a higher concentration of solutes within them than
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    the solute concentration in the saturated soil.
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    The water travels into the root hair cells as the root hair cells are hypertonic compared to
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    the hypotonic soil.
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    By the way, you may wonder---well, why don’t those root hair cells burst with all the
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    water that is going in them.
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    That brings us to our next osmosis topic and why plant cell walls are amazing!
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    So, let’s bring in another variable that can influence osmosis: pressure potential.
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    This is when it’s very useful to understand how one can calculate water potential.
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    Water potential considers both solute potential AND pressure potential.
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    In osmosis, water travels to areas of lower water potential.
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    So, the formula is water potential is equal to the pressure potential plus the solute potential.
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    Adding solute actually causes the solute potential to have a negative value and the overall water
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    potential to lower.
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    Water will travel to areas of lower water potential.
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    But exerting pressure can raise the pressure potential, a positive value, therefore raising
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    the total water potential.
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    So, let’s give a quick example.
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    In the popular water potential in potato cores lab---all kinds of neat variations of this
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    lab procedure exist online---you can calculate the water potential in potato cores using
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    the water potential formula.
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    When a potato core is first put into distilled water—that’s pure water---the potato core
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    cells start to gain water.
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    You’d expect that.
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    The water is moving towards the higher solute concentration.
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    Thanks to their higher solute concentration, they have a lower solute potential.
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    That means a lower total water potential than the surroundings and water travels to areas
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    of lower water potential.
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    But over time as the potato core cells gain water, the water that has entered exerts pressure
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    against the plant cell walls from inside the plant cells,
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    therefore raising the overall water potential in the potato core cells.
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    We want to point out that this turgor pressure that results in plant cells, thanks to osmosis
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    and plant cell walls, is critical for overall plant structure and the ability of plants
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    to grow upright and not wilt.
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    Turgor pressure is definitely something to explore.
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    In summary, where would living organisms be without osmosis?
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    After all, it involves movement of one of our very valuable resources: water.
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    Well, that’s it for the Amoeba Sisters and we remind you to stay curious!
Title:
Osmosis and Water Potential (Updated)
Description:

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Video Language:
English
Team:
BYU Continuing Education
Project:
BIO-100 (BYUO)

English subtitles

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