Pulmonary Physiology Equations

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©2010 Mark Tuttle
Pulmonary Physiology Equations
Name
Equation
Units
Minute
Ventilation
𝑉̇𝐸 = 𝑉𝑇 × π‘Ÿπ‘Ÿ
ml/min
Alveolar
Ventilation
𝑉𝐴̇ = (𝑉𝑇 − 𝑉𝐷 ) × π‘Ÿπ‘Ÿ
ml/min
VT is usually 500ml.
VD is usually 150ml.
VA is usually 4-6 L/min
mm Hg
Since ~ all alveolar CO2 is from metabolic
production, alveolar CO2 is proportionate to
the ratio of flow of CO2 to total airflow.
Alveolar CO2
Tension
𝑃𝐴 𝐢𝑂2 ∝
𝑉̇ 𝐢𝑂2
𝑉𝐴̇
R usually is 0.8
𝑛𝑛𝑂2 final = 𝑛𝑛𝑂2 initial − 𝑛𝑛𝑂2 consumed
𝑃𝐴 𝑂2 = 𝑃𝐼 𝑂2 −
As alveolar ventilation increases, the
alveolar PCO2 decreases (if constant
metabolism), this this increases alveolar
PO2 closer to inspired PO2.
𝑃𝐴 𝐢𝑂2
𝑃𝐴 𝐢𝑂2
= 𝑃𝐼 𝑂2 −
𝑅
𝑉̇ 𝐢𝑂2⁄𝑉̇ 𝑂2
PIO2 = Humidified inspired O2
Alveolar Air
Equation
𝑉̇ 𝐢𝑂2⁄𝑉̇ 𝑂2 = the production of CO2 divided by the
uptake of O2 at a site. GlucoseR=1.0, FatsR=0.7.
𝑃𝐴 𝑂2 = 𝑃𝐼 𝑂2 − 𝑃𝐴 𝐢𝑂2 ×
Note: this represents what alveolar PO2
should be, not necessarily what it is.
mm Hg
𝑉̇ 𝑂2
𝑉̇ 𝐢𝑂2
𝑃𝐴 𝑂2 = 𝑃𝐼 𝑂2 − π‘ƒπΆπ‘œπ‘›π‘ π‘’π‘šπ‘’π‘‘ 𝑂2
Bohr
Equation
physiological
dead space
Fick’s Law
Μ‡
↑ π‘‰π‘”π‘Žπ‘ 
Μ‡
↓ π‘‰π‘”π‘Žπ‘ 
Diffusion
Coefficient
Diffusing
Capacity
𝑉𝐷 π‘ƒπ‘Ž 𝐢𝑂2 − 𝑃𝐸 𝐢𝑂2 𝑃𝐴 𝐢𝑂2 − 𝑃𝐸 𝐢𝑂2
=
=
𝑉𝑇
π‘ƒπ‘Ž 𝐢𝑂2
𝑃𝐴 𝐢𝑂2
%
Physiologic=Alveolar+ Anatomic (Dead spaces)
Μ‡ =
π‘‰π‘”π‘Žπ‘ 
Surface Area × βˆ†π‘ƒ × Diffusion Coefficient
Thickness
↑ Surface Area:
- Exercise
Comments
Expired flow x respiratory rate
Normal: 5-6 L/min οƒ 150 L/min
rr up to 50 in severe exercise
Whatever CO2 is present in the alveoli
originates from the metabolic production of
CO2 by the body (since atmospheric CO2 is
negligible). Thus, we can take the amount of
CO2 in the alveoli and multiply it by an
idealized ratio of O2 consumption to CO2
production to find the amount of O2
consumed. This is helpful since alveolar O2
equals inspired O2 minus consumed O2 (by
metabolism).
The more CO2 expired, the smaller
the deadspace ceteris paribus.
Normal: 0.3, VD = 150ml
Mechanical: ET tube
Anatomic: PP ventilation
Alveolar: PE, low CO, Emphysema, ARDS
ml
↑ ΔP across A-C Membrane (↑PAO2)
- Breathing ↑FIO2
Exercise also increases the rate of diffusion by ↑ uptake
of O2 by RBC due to faster (↓) erythrocyte transit time.
↓ Surface area
- Emphysema
- Tumors
- CO ↓ (de-recruitment)
- BV ↓
- 𝑉⁄𝑄 mismatch
↑ Thickness of barrier
- Interstitial/alveolar
edema
- Interstitial/alveolar
fibrosis
Diffusion Coeffecient =
Solubility Coefficient
√Molecular Weight
A×D
𝑉π‘₯Μ‡
= DL x =
T
Px1 −Px2
↓ ΔP across A-C
mem: (↓PAO2)
- High altitude
- Hypoventilation
%
O2
CO2
Non-Fick:
↓uptake of O2 by RBCs
- Anemia (↓ Hb)
- ↓ BV
Solub. MW
0.024 32
0.592 44
DC
0.004 = 0.4%
0.089 = 8.9%
Measured with Carbon Monoxide
©2010 Mark Tuttle
Equation
Units
βˆ†π‘‰ 1
=
βˆ†π‘ƒ 𝑅 π‘œπ‘“ π‘Ÿπ‘–π‘”π‘–π‘‘ π‘Žπ‘–π‘Ÿπ‘€π‘Žπ‘¦
L/cm H2O
Name
Compliance
Normal: 0.2 L/cm H2O
Resistance
𝑅=
Poiseuille’s
Equation
Hemoglobin carrying capacity:
15𝑔 𝐻𝑏 𝟏. πŸ‘πŸ’ π’Žπ‘³ π‘ΆπŸ
−
= 20.1 π‘šπΏ 𝑂2/𝑑𝐿
100 π‘šπΏ
𝑔 𝐻𝑏
O2 Carrying
Capacity of
the Blood
O2 Extraction
𝑉𝑂̇ 2 = 𝑄𝑑̇ (πΆπ‘Ž 𝑂2 − 𝐢𝑣 𝑂2 ),
Turbulent
Flow
𝑄𝑑̇ =
mmHg
L/min
Law of
Laplace
𝑃=
πΆπ‘Ž 𝑂2 − 𝐢𝑣 𝑂2
𝑉𝑂̇ 2
ρ=density of air
D=diameter of airway
VE=velocity of expired air
η=air viscosity
2𝑇 2 × surface tension
=
π‘Ÿ
radius
𝑝𝐻 = π‘π‘˜ + π‘™π‘œπ‘”
Greater in central airways, not peripheral
οƒ  airways in parallel in periphery
Dissolved O2 Carrying Capacity
𝟎. πŸŽπŸŽπŸ‘ π‘šπΏ 𝑂2
π‘šπΏ 𝑂2
− 40 π‘šπ‘š 𝐻𝑔 = 0.12
100 π‘šπΏ × π‘ƒπ‘‚2
𝑑𝐿
𝜌 × π‘‰πΈΜ‡ × π·
𝑁𝑅 =
πœ‚
Turbulent flow occurs when NR >2000
Reynold’s #
HendersonHasselbalch
βˆ†π‘ƒ π‘ƒπ‘Žπ‘‘π‘š − π‘ƒπ‘Žπ‘™π‘£π‘’π‘œπ‘™π‘Žπ‘Ÿ 8πΏπœ‚
𝟏
=
= 4≈ πŸ’
̇𝑉
π‘“π‘™π‘œπ‘€ π‘Ÿπ‘Žπ‘‘π‘’
πœ‹π‘Ÿ
𝒓
Comments
Compliance ↑: Aging + emphysema
οƒ° Expiration ↓
Compliance ↓: Restrictive lung diz.
οƒ° Inspiration ↓
L=Length of tube
η=viscosity of air
mmHg
[𝐴− ]
[𝐻𝐢𝑂3− ]
= 6.1 + π‘™π‘œπ‘”
[𝐻𝐴]
0.03 ⋅ 𝑃𝐢𝑂2
-
Surfactant: ↓ surface tension
Deficiency: TLC ↓, ARDS/(NB),O2 tox
Normal ratio: 24/1.2 = 20/1
Normal Figures
Substance
Normal Range
Significance
Blood pH
7.35 – 7.45
Indicates acidosis/alkalosis. 6.8-7.8 Compatible w/life
PCO2
35-45 mmHg (40 mmHg)
1.2 mEg/L
Indicates respiratory/non-respiratory cause.
40mmHg x 0.03=1.2 mEq/L
[HCO3-]
22-26 mEq/L (24 mEq/L)
Indicates metabolic/non-metabolic cause
(7.4)
Serum Anion Gap
[Na+]-([HCO3-]+[Cl-])
Unmeasured ions include
phosphate, citrate, sulfate, and
protein.
Delta Anion Gap
βˆ†AGβˆ†[HCO3-]=AG-1224[HCO3-]
V/Q
↑ anionunmeasured to replace [HCO3-]↓in metabolic acidosis
8-16 mEq/L (12 mEq/L)
If anion gap is increased, there is an increase in an unmeasured ion,
usually (phosphate, lactate, β-hydroxybutyrate)
If anion gap is normal in metabolic acidosis, Cl- has likely taken the
place of HCO3-, called hyperchloremic metabolic acidosis.
A delta-delta value below 1:1 indicates a greater fall in [HCO3-] than one would expect given the increase in
the anion gap. This can be explained by a mixed metabolic acidosis, i.e a combined elevated anion gap
acidosis and a normal anion gap acidosis, as might occur when lactic acidosis is superimposed on severe
diarrhea. In this situation, the additional fall in HCO3- is due to further buffering of an acid that does not
contribute to the anion gap. (i.e addition of HCl to the body as a result of diarrhea)
A value above 2:1 indicates a lesser fall in [HCO3-] than one would expect given the change in the anion
gap. This can be explained by another process that increases the [HCO3-],i.e. a concurrent metabolic
alkalosis. Another situation to consider is a pre-existing high HCO3- level eg. chronic respiratory acidosis.
Average: 0.8
3.3 at top, 0.65 at bottom
Acid Base Disorders
Primary Disturbance
Acidosis
Metabolic Acidosis
Respiratory Acidosis
Alkalosis
Metabolic Alkalosis
Respiratory Alkalosis
Compensation
 from normal levels
Appropriate compensation
Respiratory Compensation
Renal Compensation
1.2 x  [HCO3-] ο‚― (from 24)
0.4 x  PCO2 ο‚­ (from 40)
=  PCO2 ο‚― (from 40)
=  [HCO3-] ο‚­ (from 24)
Respiratory Compensation
Renal Copmensation
0.7 x  [HCO3-] ο‚­ (from 24)
0.4 x  PCO2 ο‚― (from 40)
=  PCO2 ο‚­ (from 40)
=  [HCO3-] ο‚― (from 24)
©2010 Mark Tuttle
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