Physiology Oct. 7th

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Last updated 9:39 PM on 11/12/25
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20 Terms

1
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Does surface area scale linearly with mass?

  • No, surface area doesn’t scale linearly with mass as organisms increase in size

    • Ex. Rotifers are an example due to their high surface area relative to mass

<ul><li><p>No, surface area doesn’t scale linearly with mass as organisms increase in size </p><ul><li><p>Ex. Rotifers are an example due to their high surface area relative to mass</p></li></ul></li></ul><p></p>
2
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Explain the Nature of Diffusion

  • Gas exchange occurs through diffusion from areas of high concentration to low concentration.

  • Efficiency of diffusion is time-dependent and correlates with distance.

  • Example: Diffusion across a cell membrane (10 nanometers thick) takes about 100 nanoseconds.

  • In larger distances, such as those in larger organisms (e.g., human nerve cells), reliance on diffusion alone becomes impractical.

<ul><li><p>Gas exchange occurs through diffusion from areas of high concentration to low concentration.</p></li><li><p>Efficiency of diffusion is time-dependent and correlates with distance.</p></li><li><p>Example: Diffusion across a cell membrane (10 nanometers thick) takes about 100 nanoseconds.</p></li><li><p>In larger distances, such as those in larger organisms (e.g., human nerve cells), reliance on diffusion alone becomes impractical.</p></li></ul><p></p>
3
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Explain Gas Exchange in Plants

  • Getting CO2 out of the external medium (air) and into the leaf

  • Within the leaf CO2 needs to get into the chloroplast (Rubisco)

<ul><li><p>Getting CO2 out of the external medium (air) and into the leaf </p></li><li><p> Within the leaf CO2 needs to get into the chloroplast (Rubisco)</p></li></ul><p></p>
4
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Gas Exchange in Animals

  • Getting O2 out of the external medium and into the cells

    • Often via the circulatory system in animals

  • Getting CO2 out of the cells and into the external medium

<ul><li><p>Getting O2 out of the external medium and into the cells</p><ul><li><p>Often via the circulatory system in animals</p></li></ul></li><li><p>Getting CO2 out of the cells and into the external medium</p></li></ul><p></p>
5
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How much CO2 and O2 is found in the air?

  • Air (gases)

    • ~21% O2

    • ~0.04% CO2

  • Cold Seawater (in solution)

    • ~0.8% O2

    • ~93% of global CO2

6
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What is the ideal gas law?

  • Describes how gases behave under various conditions, assuming gas molecules are perfect spheres in constant motion.

  • Involves variables like pressure (P), volume (V), and temperature (T).

  • Pressure and temperature are directly proportional (as one increases, so does the other).

  • Pressure and volume are inversely proportional (as volume decreases, pressure increases).

<ul><li><p>Describes how gases behave under various conditions, assuming gas molecules are perfect spheres in constant motion.</p></li><li><p>Involves variables like pressure (P), volume (V), and temperature (T).</p></li><li><p>Pressure and temperature are directly proportional (as one increases, so does the other).</p></li><li><p>Pressure and volume are inversely proportional (as volume decreases, pressure increases).</p></li></ul><p></p>
7
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What is Daltons Law of Partial Pressures?

  • Total pressure exerted by a system of gases is the sum of the partial pressures of individual gases.

  • Increasing one partial pressure can increase the total pressure without affecting other partial pressures, as each gas contributes independently to the total pressure based on its concentration.

  • Example notations for atmospheric gases:

  • Atmospheric pressure: 101.3 kPa at sea level.

<ul><li><p>Total pressure exerted by a system of gases is the sum of the partial pressures of individual gases.</p></li><li><p>Increasing one partial pressure can increase the total pressure without affecting other partial pressures, as each gas contributes independently to the total pressure based on its concentration.</p></li><li><p>Example notations for atmospheric gases:</p></li><li><p>Atmospheric pressure: 101.3 kPa at sea level.</p></li></ul><p></p>
8
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Ex. What’s the partial pressure of O2 if its 20.95% of air?

<p></p>
9
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What is Henrys Law?

  • Describes the relationship between the partial pressure of a gas and its concentration in a liquid.

  • Solubility varies by gas (e.g. carbon dioxide is more soluble than oxygen)

<ul><li><p>Describes the relationship between the partial pressure of a gas and its concentration in a liquid.</p></li><li><p>Solubility varies by gas (e.g. carbon dioxide is more soluble than oxygen)</p></li></ul><p></p>
10
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What is the diffusion coefficient?

  • Unique for each gas and can be influenced by the medium (air vs water).

    • Diffusion occurs faster in air compared to water (10,000 times faster).

<ul><li><p>Unique for each gas and can be influenced by the medium (air vs water).</p><ul><li><p>Diffusion occurs faster in air compared to water (10,000 times faster).</p></li></ul></li></ul><p></p>
11
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What can effect the rate at which a gas diffuses?

  • The concentration of a gas directly affects its diffusion rate because diffusion depends on the concentration gradient

    • Larger the concentration difference = faster diffusion and vice vera

  • The area available for diffusion effects the the diffusion rate

    • wider the opening of a bottle (or the greater the surface area), the more gas molecules can move across, or out, at once

<ul><li><p>The concentration of a gas directly affects its diffusion rate because diffusion depends on the concentration gradient</p><ul><li><p>Larger the concentration difference = faster diffusion and vice vera</p></li></ul></li><li><p>The area available for diffusion effects the the diffusion rate </p><ul><li><p>wider the opening of a bottle (or the greater the surface area), the more gas molecules can move across, or out, at once</p></li></ul></li></ul><p></p>
12
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What is Fick’s Law of Diffusion?

  • Governs the net rate of movement of gases through diffusion.

    • Important to note that diffusion rates slow with increased distance.

<ul><li><p>Governs the net rate of movement of gases through diffusion.</p><ul><li><p>Important to note that diffusion rates slow with increased distance.</p></li></ul></li></ul><p></p>
13
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What are the factors that affect gas solubility?

  • Temperature

    • Higher temperatures lead to decreased gas solubility.

    • Cold soda holds fizz better because CO₂ stays dissolved. Warm soda goes flat quickly — the CO₂ solubility drops as temperature rises (CO2 molecules move quicker when heated and won’t be able to stay in solution; want to get out into the air)

  • Salinity

    • Increased salinity reduces dissolved gas quantities.

14
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Whats the equation once we put it all together?

<ul><li><p></p></li></ul><p></p>
15
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What variables of the previous equation can be modified?

  • Surface area, Concentration gradients, Distance over which diffusion occurs (A’, C1-C2, and X)

16
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Whats the difference between gases and solutes?

  • For gases, its partial pressure, not concentration, that determines the direction of diffusion.

    • diffusion happens from areas of high partial pressure → low partial pressure, not necessarily from high concentration → low concentration.

  • For solutes (like salt or sugar in water), diffusion depends on concentration gradients — molecules move from high concentration to low concentration.

17
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How does the beetle example explain this?

  • The beetle traps an air bubble under its body while underwater.

  • Inside the bubble: O₂ is used up as the beetle breathes, so PO₂ in the bubble drops.

  • The water around the bubble still has a higher PO₂, even though the O₂ concentration in water is lower than in the bubble (air).

  • Because gases diffuse according to partial pressure, O₂ from the water diffuses into the bubble, replenishing it.

  • (O₂ can move into the bubble even if the bubble still has more O₂ molecules (higher concentration)as long as its partial pressure is lower than the surrounding water’s)

<ul><li><p>The beetle traps an air bubble under its body while underwater.</p></li><li><p>Inside the bubble: O₂ is used up as the beetle breathes, so PO₂ in the bubble drops.</p></li><li><p>The water around the bubble still has a higher PO₂, even though the O₂ concentration in water is lower than in the bubble (air).</p></li><li><p>Because gases diffuse according to partial pressure, O₂ from the water diffuses into the bubble, replenishing it.</p></li></ul><p></p><ul><li><p>(O₂ can move <strong>into</strong> the bubble even if the bubble still has more O₂ molecules (higher concentration)as long as its <strong>partial pressure</strong> is <strong>lower</strong> than the surrounding water’s)</p></li></ul><p></p>
18
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Explain Convection vs.Diffusion

  • Diffusion

    • more passive of gas molecules from high to low concentration (or partial pressure)

    • its slow over long distances

    • works well for small organisms or across thin membranes (like alveoli in lungs)

  • Convection

    • bulk flow of air or fluid, carrying gases with it.

    • It’s much faster than diffusion because it physically moves large amounts of gas.

    • Driven by pressure differences, temperature gradients, or external forces (like stirring or wind).

    • Think of it as air circulation instead of random molecular movement.

      • Blood flow moving oxygen through your body.

19
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  • How does the Prairie Dog example help explain this?

  • The diagram of the prairie dog burrow shows how convection enhances gas exchange underground:

    • Wind moves over the two burrow openings, creating different pressures (low pressure at one end, high pressure at the other).

      • Upwind (left): Air hits directly, slows down, and “piles up” — this creates higher pressure.

      • Downwind (right): Air speeds up as it flows past, which lowers pressure.

      • Result: Air flows from left → right through the burrow (high → low pressure).

  • This pressure difference causes air to flow through the tunnels — that’s convection.

  • The flowing air continuously brings in fresh oxygen (O₂) and removes carbon dioxide (CO₂), which keeps the air in the burrow breathable.

  • If they relied only on diffusion, gas exchange would be much slower, and oxygen might not reach deeper parts of the burrow.

<ul><li><p>The diagram of the prairie dog burrow shows how convection enhances gas exchange underground:</p><ul><li><p>Wind moves over the two burrow openings, creating different pressures (low pressure at one end, high pressure at the other).</p><ul><li><p><span>Upwind (left): Air hits directly, slows down, and “piles up” — this creates higher pressure.</span></p></li><li><p><span>Downwind (right): Air speeds up as it flows past, which lowers pressure.</span></p></li><li><p><span>Result: Air flows from left → right through the burrow (high → low pressure).</span></p></li></ul></li></ul></li></ul><ul><li><p>This pressure difference causes air to flow through the tunnels — that’s convection.</p></li><li><p>The flowing air continuously brings in fresh oxygen (O₂) and removes carbon dioxide (CO₂), which keeps the air in the burrow breathable.</p></li></ul><ul><li><p>If they relied only on diffusion, gas exchange would be much slower, and oxygen might not reach deeper parts of the burrow.</p></li></ul><p></p>
20
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Explain gas transport in animals 

  • Is often a combination of convection and diffusion

  • Tidal Convection Ventilates the Lungs:

    • Convection = bulk movement of air (breathing in and out).

    • Air enters the lungs by tidal ventilation — meaning air flows in during inhalation and out during exhalation.

    • This movement brings fresh O₂ to the alveoli and removes CO₂ from the body.

    • Think of this as the “delivery system” that refreshes the air inside the lungs.

  • Diffusion into the Bloodstream:

    • Once air reaches the alveoli (tiny air sacs), gas exchange happens by diffusion.

    • O₂ diffuses from high partial pressure in alveoli → low partial pressure in blood.

    • CO₂ diffuses the opposite way (from blood → alveoli).

    • This step is microscopic — gases move only a few micrometers across the alveolar and capillary membranes.

  • Unidirectional Flow (Convection) in the Circulatory System:

    • Once gases are in the blood, convection takes over again.

    • The heart pumps blood through vessels — a bulk flow that carries O₂-rich blood to tissues and brings CO₂-rich blood back to the lungs.

    • This is convection on a larger scale, like a delivery route.

  • Diffusion from Capillaries into Tissues:

    • When oxygenated blood reaches body tissues, O₂ diffuses from blood to cells where it’s used for metabolism.

    • CO₂ diffuses from cells to blood to be carried back to the lungs.

    • Again, this happens over short distances, driven by partial pressure gradients.

<ul><li><p>Is often a combination of convection and diffusion</p></li><li><p>Tidal <strong>Convection </strong>Ventilates the Lungs:</p><ul><li><p>Convection = bulk movement of air (breathing in and out).</p></li><li><p>Air enters the lungs by tidal ventilation — meaning air flows in during inhalation and out during exhalation.</p></li><li><p>This movement brings fresh O₂ to the alveoli and removes CO₂ from the body.</p></li><li><p>Think of this as the “delivery system” that refreshes the air inside the lungs.</p></li></ul></li><li><p><strong>Diffusion </strong>into the Bloodstream:</p><ul><li><p>Once air reaches the alveoli (tiny air sacs), gas exchange happens by diffusion.</p></li><li><p>O₂ diffuses from high partial pressure in alveoli → low partial pressure in blood.</p></li><li><p>CO₂ diffuses the opposite way (from blood → alveoli).</p></li><li><p>This step is microscopic — gases move only a few micrometers across the alveolar and capillary membranes.</p></li></ul></li><li><p>Unidirectional Flow (<strong>Convection</strong>) in the Circulatory System:</p><ul><li><p>Once gases are in the blood, convection takes over again.</p></li><li><p>The heart pumps blood through vessels — a bulk flow that carries O₂-rich blood to tissues and brings CO₂-rich blood back to the lungs.</p></li><li><p>This is convection on a larger scale, like a delivery route.</p></li></ul></li><li><p><strong>Diffusion </strong>from Capillaries into Tissues:</p><ul><li><p>When oxygenated blood reaches body tissues, O₂ diffuses from blood to cells where it’s used for metabolism.</p></li><li><p>CO₂ diffuses from cells to blood to be carried back to the lungs.</p></li><li><p>Again, this happens over short distances, driven by partial pressure gradients.</p></li></ul></li></ul><p></p>

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