Fundamentals

Gas Pressure, Units, and Basic Concepts

  • Three main pressure units encountered in respiratory care:

    • millimeters of mercury (mmHg) and torr (torr ∼ mmHg)

    • centimeters of water (cmH₂O) for many respiratory devices

    • pounds per square inch (psi) for cylinders and some equipment

  • Other related units you may see (less commonly used in this course): atmospheres (atm), inches of water, inches of mercury

  • At sea level, standard atmospheric pressure is: 1 atm=760 mmHg1~\text{atm} = 760~\text{mmHg}

  • Everyday reference: 1 atmosphere corresponds to about 33 feet of water column; this is a rough physical intuition rather than a practical calculation in therapy screens

  • The main pressure concepts you’ll need to select correct values on tests: inspired oxygen partial pressure (PIO₂), alveolar oxygen partial pressure (PAO₂), and total pressures as sums of partial pressures (Dalton’s law)

Oxygen in the Atmosphere and Partial Pressures

  • The ambient atmosphere contains 21% oxygen by volume: FiO₂=0.21.\text{FiO₂} = 0.21\,.

  • Partial pressure of inspired O₂ in air depends on barometric pressure (PB) and water vapor pressure (PH₂O):

    • In dry gas at sea level: P<em>IO2=P</em>B×FiO2P<em>{IO₂} = P</em>B \times FiO₂

    • When considering humidified air (air entering the lungs after water vapor), use: P<em>IO2=(P</em>BP<em>H</em>2O)×FiO2P<em>{IO₂} = (P</em>B - P<em>{H</em>2O}) \times FiO₂

  • At sea level, typically: P<em>B=760 mmHg,P</em>H2O47 mmHgP<em>B = 760~\text{mmHg}, \quad P</em>{H_2O} \approx 47~\text{mmHg}

  • Example: room air inhalation (FiO₂ = 0.21):

    • Without subtracting water vapor: PIO2=760×0.21159 mmHgP_{IO₂} = 760 \times 0.21 \approx 159~\text{mmHg}

    • With water vapor subtraction (PB - PH₂O = 713): PIO2=713×0.21150 mmHgP_{IO₂} = 713 \times 0.21 \approx 150~\text{mmHg}

The Alveolar Gas Equation (PAO₂)

  • The alveolar gas equation relates alveolar O₂ to barometric pressure, humidity, FiO₂, and PaCO₂ with a respiratory quotient (R):

    • General form: P<em>AO2=(P</em>BP<em>H</em>2O)FiO2PaCO2RP<em>{AO₂} = \big(P</em>B - P<em>{H</em>2O}\big) \cdot FiO₂ - \frac{P_{aCO₂}}{R}

  • Example values and calculation used in lecture:

    • PB = 760 mmHg, PH₂O = 47 mmHg, FiO₂ = 0.55, PaCO₂ = 48 mmHg, R = 0.80

    • Compute: PAO2=(76047)0.55480.8=7130.5560=392.1560332 mmHgP_{AO₂} = (760 - 47) \cdot 0.55 - \frac{48}{0.8} = 713 \cdot 0.55 - 60 = 392.15 - 60 \approx 332~\text{mmHg}

  • Why this matters: PAO₂ represents the available oxygen tension at the alveolar site; if measured PaO₂ is lower than expected (e.g., 80–100 mmHg), diffusion, shunt, or ventilation–perfusion mismatch may be implicated

  • A related, simpler calculation shown:

    • In atmosphere, with FiO₂ = 0.55, PB − PH₂O = 713, the alveolar equation yields approximately 332 mmHg under the given conditions

The Gas Laws (Foundational Concepts for Respiratory Therapy)

  • Avogadro’s Law (brief, less tested): equal volumes of gas at the same T and P contain the same number of molecules. Focus is on molecule count; not a common direct exam question here

  • Bernoulli’s Principle (Venturi masks and entrainment)

    • As velocity of gas increases, the surrounding pressure decreases

    • Venturi masks use this to entrain ambient air to achieve a precise FiO₂ by changing the adapter size and the entrained flow

    • Example: a Venturi device may deliver 40% FiO₂ by delivering 12 L/min of 100% O₂ through a narrow jet, entraining room air to reach the target FiO₂

  • Boyle’s Law (PV, inversely proportional at constant T)

    • In our breathing, diaphragm downward movement expands the lung volume, decreasing intrapulmonary pressure and drawing air in

  • Charles’ Law (V ∝ T at constant P)

    • Volume changes with temperature when pressure is held constant

  • Gay-Lussac’s Law (P ∝ T at constant V)

    • Pressure changes with temperature when volume is held constant

  • Dalton’s Law of Partial Pressures

    • Total pressure is the sum of the partial pressures: P{tot} = P{1} + P{2} + P{3} + \

Gas Pressure, Units, and Basic Concepts
  • Three main pressure units encountered in respiratory care:

    • millimeters of mercury (mmHg) and torr (torr

  • mmHg). These are commonly used for physiological measurements like blood pressure and arterial gas tensions.

    • centimeters of water (cmH

O) for many respiratory devices. This unit is often seen in ventilator settings, CPAP, and BiPAP devices due to its relevance to airway pressures.

  • pounds per square inch (psi) for cylinders and some equipment. This unit indicates the high pressures involved in compressed gas cylinders and related regulators.

    • Other related units you may see (less commonly used in this course): atmospheres (atm), inches of water, inches of mercury. Understanding these units is crucial for accurate equipment operation, monitoring, and patient assessment.

    • At sea level, standard atmospheric pressure is: 1~\text{atm} = 760~\text{mmHg}</p></li><li><p>Everydayreference:1atmospherecorrespondstoabout33feetofwatercolumn;thisisaroughphysicalintuitionratherthanapracticalcalculationintherapyscreens.Thisillustratesthesignificantforceexertedbyatmosphericpressure.</p></li><li><p>Themainpressureconceptsyoullneedtoselectcorrectvaluesontests:inspiredoxygenpartialpressure(PIO</p></li></ul></li></ul><p>),alveolaroxygenpartialpressure(PAO</p><p>),andtotalpressuresassumsofpartialpressures(Daltonslaw).</p><h5collapsed="false"seolevelmigrated="true">OxygenintheAtmosphereandPartialPressures</h5><ul><li><p>Theambientatmospherecontains21</p></li><li><p>Everyday reference: 1 atmosphere corresponds to about 33 feet of water column; this is a rough physical intuition rather than a practical calculation in therapy screens. This illustrates the significant force exerted by atmospheric pressure.</p></li><li><p>The main pressure concepts you’ll need to select correct values on tests: inspired oxygen partial pressure (PIO</p></li></ul></li></ul><p>), alveolar oxygen partial pressure (PAO</p><p>), and total pressures as sums of partial pressures (Dalton’s law).</p><h5 collapsed="false" seolevelmigrated="true">Oxygen in the Atmosphere and Partial Pressures</h5><ul><li><p>The ambient atmosphere contains 21% oxygen by volume:\text{FiO₂} = 0.21\,.Thisisaconstantvalueundernormalconditions.</p></li><li><p>PartialpressureofinspiredO</p><p>inairdependsonbarometricpressure(PB)andwatervaporpressure(PH2O):</p><ul><li><p>Indrygasatsealevel:This is a constant value under normal conditions.</p></li><li><p>Partial pressure of inspired O</p><p>in air depends on barometric pressure (PB) and water vapor pressure (PH₂O):</p><ul><li><p>In dry gas at sea level:\text{P_IO₂} = \text{P_B} \times \text{FiO₂}</p></li><li><p>Whenconsideringhumidifiedair(airenteringthelungsafterwatervapor),use:</p></li><li><p>When considering humidified air (air entering the lungs after water vapor), use:\text{P_IO₂} = (\text{P_B} - \text{P_H_2O}) \times \text{FiO₂}.Watervapordisplacesothergasesintheair,soitspressuremustbesubtractedfromthetotalbarometricpressuretofindthepartialpressureofthedrygases.</p></li><li><p>Atsealevel,typically:. Water vapor displaces other gases in the air, so its pressure must be subtracted from the total barometric pressure to find the partial pressure of the dry gases.</p></li><li><p>At sea level, typically:\text{P_B} = 760~\text{mmHg}, \quad \text{P_H_2O} \approx 47~\text{mmHg}(atbodytemperature(at body temperature37^{\circ}\text{C}).</p></li></ul></li><li><p>Example:roomairinhalation(FiO2=0.21):</p><ul><li><p>Withoutsubtractingwatervapor:).</p></li></ul></li><li><p>Example: room air inhalation (FiO₂ = 0.21):</p><ul><li><p>Without subtracting water vapor:\text{P_IO₂} = 760 \times 0.21 \approx 159~\text{mmHg}</p></li><li><p>Withwatervaporsubtraction(PBPH2O=713):</p></li><li><p>With water vapor subtraction (PB - PH₂O = 713):\text{P_IO₂} = 713 \times 0.21 \approx 150~\text{mmHg}Thelattercalculationismorephysiologicallyaccurateforgasesreachingthealveoli.</p></li></ul></li></ul><h5collapsed="false"seolevelmigrated="true">TheAlveolarGasEquation(PAO2)</h5><ul><li><p>ThealveolargasequationrelatesalveolarO2tobarometricpressure,humidity,FiO2,andPaCO2witharespiratoryquotient(R):</p><ul><li><p>Generalform:The latter calculation is more physiologically accurate for gases reaching the alveoli.</p></li></ul></li></ul><h5 collapsed="false" seolevelmigrated="true">The Alveolar Gas Equation (PAO₂)</h5><ul><li><p>The alveolar gas equation relates alveolar O₂ to barometric pressure, humidity, FiO₂, and PaCO₂ with a respiratory quotient (R):</p><ul><li><p>General form:\text{P_AO₂} = \big(\text{P_B} - \text{P_H_2O}\big) \cdot \text{FiO₂} - \frac{\text{P_aCO₂}}{\text{R}}.Therespiratoryquotient(R)typicallyrangesfrom0.8to1.0andrepresentstheratioofcarbondioxideproductiontooxygenconsumptionwithinthebody.</p></li><li><p>Examplevaluesandcalculationusedinlecture:</p></li><li><p>PB=760mmHg,PH2O=47mmHg,FiO2=0.55,PaCO2=48mmHg,R=0.80</p></li><li><p>Compute:. The respiratory quotient (R) typically ranges from 0.8 to 1.0 and represents the ratio of carbon dioxide production to oxygen consumption within the body.</p></li><li><p>Example values and calculation used in lecture:</p></li><li><p>PB = 760 mmHg, PH₂O = 47 mmHg, FiO₂ = 0.55, PaCO₂ = 48 mmHg, R = 0.80</p></li><li><p>Compute:\text{P_AO₂} = (760 - 47) \cdot 0.55 - \frac{48}{0.8} = 713 \cdot 0.55 - 60 = 392.15 - 60 \approx 332~\text{mmHg}Thiscalculationhelpsdeterminethedrivingpressureforoxygentodiffusefromthealveoliintotheblood.</p></li></ul></li><li><p>Whythismatters:PAO2representstheavailableoxygentensionatthealveolarsite;ifmeasuredPaO2islowerthanexpected(e.g.,80100mmHg),diffusion,shunt,orventilationperfusionmismatchmaybeimplicated.Itisacriticalvalueforassessinglungfunction.</p></li><li><p>Arelated,simplercalculationshown:</p><ul><li><p>Inatmosphere,withFiO2=0.55,PBPH2O=713,thealveolarequationyieldsapproximately332mmHgunderthegivenconditions.</p></li></ul></li></ul><h5collapsed="false"seolevelmigrated="true">TheGasLaws(FoundationalConceptsforRespiratoryTherapy)</h5><ul><li><p>AvogadrosLaw(brief,lesstested):equalvolumesofgasatthesameTandPcontainthesamenumberofmolecules.Focusisonmoleculecount;notacommondirectexamquestionhere,butfundamentaltounderstandinggasmolarvolumes.</p></li><li><p>BernoullisPrinciple(Venturimasksandentrainment)</p><ul><li><p>Asvelocityofgasincreases,thesurroundingpressuredecreases.Thisprincipleisvitalinrespiratorydevices.</p></li><li><p>VenturimasksusethistoentrainambientairtoachieveapreciseFiO2bychangingtheadaptersizeandtheentrainedflow.Thisallowsforpreciseoxygendeliverybeyondsimpleflowrates,ensuringaccurateFiO2forpatients.</p></li><li><p>Example:aVenturidevicemaydeliver40This calculation helps determine the driving pressure for oxygen to diffuse from the alveoli into the blood.</p></li></ul></li><li><p>Why this matters: PAO₂ represents the available oxygen tension at the alveolar site; if measured PaO₂ is lower than expected (e.g., 80–100 mmHg), diffusion, shunt, or ventilation–perfusion mismatch may be implicated. It is a critical value for assessing lung function.</p></li><li><p>A related, simpler calculation shown:</p><ul><li><p>In atmosphere, with FiO₂ = 0.55, PB − PH₂O = 713, the alveolar equation yields approximately 332 mmHg under the given conditions.</p></li></ul></li></ul><h5 collapsed="false" seolevelmigrated="true">The Gas Laws (Foundational Concepts for Respiratory Therapy)</h5><ul><li><p>Avogadro’s Law (brief, less tested): equal volumes of gas at the same T and P contain the same number of molecules. Focus is on molecule count; not a common direct exam question here, but fundamental to understanding gas molar volumes.</p></li><li><p>Bernoulli’s Principle (Venturi masks and entrainment)</p><ul><li><p>As velocity of gas increases, the surrounding pressure decreases. This principle is vital in respiratory devices.</p></li><li><p>Venturi masks use this to entrain ambient air to achieve a precise FiO₂ by changing the adapter size and the entrained flow. This allows for precise oxygen delivery beyond simple flow rates, ensuring accurate FiO₂ for patients.</p></li><li><p>Example: a Venturi device may deliver 40% FiO₂ by delivering 12 L/min of 100% O₂ through a narrow jet, entraining room air to reach the target FiO₂. This principle is also seen in nebulizers to atomize medication.</p></li></ul></li><li><p>Boyle’s Law (P<span data-name="left_right_arrow" data-type="emoji">↔</span>V, inversely proportional at constant T)</p><ul><li><p>In our breathing, diaphragm downward movement expands the lung volume, decreasing intrapulmonary pressure and drawing air in. Conversely, exhalation involves a decrease in lung volume, increasing pressure and expelling air. This describes the mechanics of ventilation.</p></li></ul></li><li><p>Charles’ Law (V ∝ T at constant P)</p><ul><li><p>Volume changes with temperature when pressure is held constant. For example, a gas warmed will expand if not contained, or its pressure will rise if contained. This is relevant for gas storage and delivery systems in varying ambient temperatures.</p></li></ul></li><li><p>Gay-Lussac’s Law (P ∝ T at constant V)</p><ul><li><p>Pressure changes with temperature when volume is held constant. This means a gas in a sealed cylinder will experience pressure changes with temperature fluctuations, which is important for safety and gauge readings of medical gas cylinders.</p></li></ul></li><li><p>Dalton’s Law of Partial Pressures</p><ul><li><p>Total pressure is the sum of the partial pressures:\text{P_tot} = \text{P_1} + \text{P_2} + \text{P_3} + \text{…}$$ This law is fundamental for understanding gas exchange in the lungs, as