Gas Exchange & Partial Pressures: Comprehensive Study Notes

Definition & Directionality of Gas Exchange
  • Gas exchange = bidirectional diffusion of O<em>2O<em>2 and CO</em>2CO</em>2 along their partial-pressure (P) gradients.

    • Pulmonary interface (alveolus blood):

    • O<em>2O<em>2: P{O2\,\text{alv}} > P{O_2\,\text{blood}} \Rightarrow diffusion into blood.

    • CO<em>2CO<em>2: P{CO2\,\text{blood}} > P{CO_2\,\text{alv}} \Rightarrow diffusion into alveolus.

    • Systemic interface (blood tissue): reverse directions.

  • Both gases are non-polar → highly lipid-soluble → move by simple diffusion through any cell membrane.

Partial Pressure Fundamentals
  • Gas pressure = force of random molecular impacts on container walls.

  • Partial pressure (PXP_X) = share of total pressure contributed by gas species X.

  • Total pressure (P<em>TP<em>T) of a mixture = sum of all P</em>XP</em>X.

  • Fractional composition of dry atmospheric air (memorize):

    • 79%79\% N<em>2N<em>2 | 21%21\% O</em>2O</em>2 | Trace 0%\approx 0\% physiologically.

Example: Dry-air partial pressures at sea level (Chicago)

(P<em>T=760mmHg)(P<em>T = 760\,\text{mmHg}) (P</em>N<em>2=0.79×760=600mmHg)(P</em>{N<em>2}=0.79\times760\,=600\,\text{mmHg}) (P</em>O2=0.21×760=160mmHg)(P</em>{O_2}=0.21\times760\,=160\,\text{mmHg})

Humidification in Conducting Zone
  • Inhaled air is warmed to core body T and becomes 100 % humidified by the airway water film.

  • Water-vapor partial pressure at 37 °C and 100 % RH is constant:
    P<em>H</em>2O=47mmHgP<em>{H</em>2O}=47\,\text{mmHg} (commit to memory).

  • Humidification displaces other gases:
    P<em>O</em>2(humid)=0.21×(PT47)P<em>{O</em>2\,(humid)} = 0.21 \times (P_T - 47)
    =0.21×(76047)=0.21×713150mmHg=0.21 \times (760-47)=0.21\times 713 \approx 150\,\text{mmHg}

  • Consequences

    • Slight “dilution” of O<em>2O<em>2 and N</em>2N</em>2.

    • Unavoidable body-water loss with every breath.

Equilibrium vs. Solubility
  • At partial-pressure equilibrium: P<em>O</em>2gas=P<em>O</em>2liquidP<em>{O</em>2\,\text{gas}} = P<em>{O</em>2\,\text{liquid}} (similarly for CO2CO_2).

  • BUT concentrations differ because gases are poorly water-soluble.

    • Plasma holds few O<em>2O<em>2 molecules even at P</em>O2=100mmHgP</em>{O_2}=100\,\text{mmHg}.

    • CO<em>2CO<em>2 is ≈ 20× more soluble than O</em>2O</em>2, yet still on hydrophobic side.

  • Necessitates auxiliary carriers (e.g.
    Hb in RBCs) for adequate transport — preview of next lecture.

Typical Resting Partial-Pressure Values

Location (rest)

P<em>O</em>2P<em>{O</em>2} (mmHg)

P<em>CO</em>2P<em>{CO</em>2} (mmHg)

Alveolus

100

40

Pulm. artery / systemic vein

40

46

Pulm. vein / systemic artery

≈100

40

Systemic tissue (average rest)

30

46

  • Exercise ↓ tissue P<em>O</em>2P<em>{O</em>2} (e.g. 20 mmHg) & ↑ tissue P<em>CO</em>2P<em>{CO</em>2} → steeper gradients → faster diffusion.

Factors Determining Rate of Diffusion (Fick-like)
  1. Diffusible Surface Area (A)

    • More A → higher flux.

    • Physiological maximization: each alveolar sac is engulfed by capillary network.

    • Pathology – Emphysema

      • Cigarette smoke → inflammatory destruction of shared alveolar walls → coalesced large “blebs”.

      • ↓ capillary contacts → ↓A → impaired gas exchange → hypoxemia, hypercapnia.

  2. Functional Membrane Thickness (Δx)

    • Thicker barrier → slower diffusion.

    • Pneumonia: exudate/water in alveoli lengthens path; gases are hydrophobic so extra fluid is major obstacle.

    • Similar in pulmonary edema, fibrosis.

  3. Partial-Pressure Gradient (ΔP)

    • Determined by alveolar vs. blood values; modulated by ventilation, metabolism, altitude.

  4. Diffusion Coefficient (D)

    • Encodes solubility & molecular weight; D{CO2} >> D{O2} → CO₂ diffuses 20× faster.

Alveolar Partial Pressures & Their Modifiers
  1. Inspired Partial Pressure (P<em>IO</em>2P<em>{I\,O</em>2}, P<em>ICO</em>2P<em>{I\,CO</em>2})

    • Governed by altitude.

    • At higher elevation: P<em>TP<em>T falls ⇒ despite 21 % fraction, P</em>IO2P</em>{I\,O_2} drops ("thin air").

    • Clinical relevance: hypoxic challenge on Everest; worksheet explores compensation mechanisms.

  2. Minute Alveolar Ventilation (V˙A\dot V_A)

    • Definition: volume reaching alveoli per minute.
      V˙<em>A=V˙</em>EV˙<em>D\dot V<em>A = \dot V</em>E - \dot V<em>D where V˙</em>E\dot V</em>E = minute ventilation, V˙D\dot V_D = dead-space ventilation.

    • Rule of thumb:

      • V˙<em>A\dot V<em>A ⇒ alveolar values trend toward humidified atmospheric values. • P</em>AO<em>2P</em>{A\,O<em>2} rises toward 150 mmHg (ceiling). • P</em>ACO2P</em>{A\,CO_2} falls toward ≈0 mmHg (cannot reach 0 because blood keeps adding CO₂).

      • V˙A\dot V_A (hypoventilation) does opposite (risk of respiratory acidosis).

    • Graphically: curves asymptotically approach limits; plateau reflects water-vapor ceiling for $O_2$ & constant CO₂ addition.

  3. Metabolic Rate (VO₂ & VCO₂)

    • Brainstem reflexes normally match ventilation to demand.

    • ↑ metabolic rate (exercise, fever) →
      • faster O<em>2O<em>2 extraction, CO</em>2CO</em>2 production → steeper gradients.
      • Reflex ↑V˙A\dot V_A (hyperpnea) restores alveolar pressures.

    • Failure to match (e.g.
      ventilatory muscle fatigue) leads to hypoxemia/hypercapnia.

Numerical / Formula Summary to Memorize
  • Fractional dry-air composition: F<em>O</em>2=0.21F<em>{O</em>2}=0.21, F<em>N</em>2=0.79F<em>{N</em>2}=0.79.

  • Water-vapor pressure at 37 °C: 47mmHg47\,\text{mmHg}.

  • Humidified inspired P<em>O</em>2P<em>{O</em>2} (sea level): 150mmHg\approx150\,\text{mmHg}.

  • Resting alveolar: P<em>AO</em>2100mmHgP<em>{A\,O</em>2}\approx100\,\text{mmHg}, P<em>ACO</em>240mmHgP<em>{A\,CO</em>2}\approx40\,\text{mmHg}.

  • Typical tissue at rest: P<em>tO</em>230mmHgP<em>{t\,O</em>2}\approx30\,\text{mmHg}.

  • Diffusion relationship (simplified Fick):
    Flux=DAΔPΔx\text{Flux} = D\,A\,\dfrac{\Delta P}{\Delta x}.

Clinical & Practical Implications
  • Emphysema: chronic smoking → ↓A; patients present with dyspnea, need supplemental O2O_2.

  • Pneumonia/Pulmonary edema: ↑Δx; risk of hypoxemia; positive-pressure ventilation or diuretics may help.

  • High-altitude exposure: ↓P<em>IO</em>2P<em>{I\,O</em>2}; acclimatization involves hyperventilation, polycythemia, 2,3-BPG rise.

  • Everyday water loss: humidification of each breath obligates insensible water loss → underscores importance of hydration.

  • Ethical/philosophical: Public-health need to reduce smoking due to preventable emphysema; awareness of altitude sickness for climbers.

Study Suggestions / Worksheet Connections
  • Practice converting total pressure to partial pressures (worksheet #1).

  • Include humidification step (worksheet #2).

  • Predict changes with altered V˙A\dot V_A, metabolism, or altitude (remaining worksheet problems).

  • Re-draw diffusion pathways & label numerical values for both rest and exercise.