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Slideshow is from the University of Michigan Medical School's M1 Cardiovascular / Respiratory sequence View additional course materials on Open.Michigan: openmi.ch/med-M1Cardio
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Author(s): Louis D’Alecy, 2009
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3
Alveolar Ventilation
M1 – Cardiovascular/Respiratory Sequence
Louis D Alecy, Ph.D.
Fall 2008
4
Monday 11/17/08, 9:00
Ventilation 20 slides, 50 minutes
1. Static Volumes a)Tidal volume b)Dead space volume c) Alveolar volume
2. Minute volumes 3. Alveolar Ventilation 4. Composition of Respiratory Gases
5
Functional Volumes (mL)
VT
VD
VA
Tidal volume is the volume of each breath.
Dead space volume has no gas exchange.- conducting airways (anatomic)- non-perfused alveoli (alveolar)
Alveolar volume has gas exchange.
6
DEAD SPACE VD
Physiological Dead space (volume)
sum of anatomical and alveolar dead space
Anatomical Dead Space (volume)volume of air in airways that can not exchangegases with blood - typical value about 150 mlor 1 ml per pound body weight.
Alveolar Dead Space (volume)volume of alveoli that are ventilated but do
not receive a blood flow and thus no gas exchange. Small in normal lung but can be very large in some pulmonary diseases.
7
Tidal Volume (VT)VT = VD + VA
VA = VT - VD
The tidal volume is the sum of the dead space volume and the alveolar volume.
The alveolar volume is the difference between the tidal volume and the dead space volume.
8
Breaths per Minute & Alveolar Ventilation
Normal respiratory rate is about
12 to 15 breaths /minute.
Alveolar ventilation (VA) is calculated by
multiplying the respiratory rate times the volume.
Indicates a rate or “per min” as in mL/min.
9
Minute Volume (Rate X VT) orTotal Ventilation or Minute Ventilation
VT = Rate X VT
6000 mL/min = 12 b/min X 500 mL/bor from previous example
7500 mL/min = 15 b/min X 500 mL/b
BUT
Same rate applies to VD + VA
VT = VE
10
Breaths per Minute (book example)
VT = VE
Source Undetermined
11
Alveolar Ventilation
VA = VE - VD
which is the same as
VA = Rate (VE - VD) or = Rate (VT - VD)
VT = VE
VA = VT - VD or
But
12
end expiration
end inspiration
anatomical
dead space 150 ml
tidal volume
450 ml
450 ml
300 ml
3000 ml
FRC
Alveolar Ventilation
D’Alecy
13
Alveolar VentilationIs the exchange of gas between the
alveoli and the external environment.
Bulk Flow
Diffusion
Source Undetermined
14
= 15 X 500= b/min X mL/b
Dead space ventilation
= b/min X mL/b = 15 X 150= 2250 mL/min
Alveolar ventilation = Total ventilation - Dead space ventilation
b/min X mL/b = b/min X mL/b - b/min X mL/b17 X 350 = 15 X 500 - 15 X 1505250 ml/min = 7500 ml/min - 2250 ml/min
Alveolar ventilation is approximately
equal to pulmonary blood flow (cardiac output).
Source Undetermined
15
Effect of rate & tidal volume on ALVEOLAR VENTILATION
VT R VE VA
ml/min ml/min
150 40 6000 0 no alveolar ventilation
500 12 6000 4200 normal ventilation
1000 6 6000 5100 excess ventilation
VA = R (VT - VD)
4200 mL/min = 12 ( 500 - 150)
Fixed VE & VD
16
Composition of Respiratory Gas
What do we breath? Air
What do we breath in? Air & moisture
What do we breath out? Air, CO2 & H2O
What is air made of? N2 and O2 mostly
How measure? Partial Pressure
Partial pressure of a gas is equal to its fractional concentration times
the total pressures of all gases in mixture. (Dalton’s Gas Law)
17
STEPS IN RESPIRATION
Bulk Flow
Diffusion
Source Undetermined
18
Dalton s Law of Partial Pressures
The total pressure exerted by a mixture of gases is equal to the sum of the partial pressures that each gas would exert if it alone occupied the entire volume.
Total pressure of air (barometric)
Pair = PO2 + PCO2 + PN2 + Px
760 mm Hg = 160 + 0.2 + 593 + 7
100% = 21% + 0.03% + 78% + 0.9%
PO2 = 21% x 760 = 160 mm Hg
Where does the 760 mmHg come from ??
19
Origin of 760 mmHg - effect of ALTITUDE
Altitude PB % O2 PO2 ft mm Hg mm Hg
Sea level 0 760 21% 160
Ann Arbor 800 737 21% 155
Denver 5,200 640 21% 134
Mt Everest 29,028 253 21% 53
20
Standard Conditions for Measuring Gas Volumes
Standard Temperature, Pressure, Dry = STPD
T = 273 ° absolute (0 ° Celsius)
Pb = 760 mm Hg at sea level 21% of dry air pressure is due to oxygen thus 0.21 X 760 = 160 mmHg PO2
Dry (no water vapor)
The volume of a pure gas (V) at STPD is directly proportional to the number of
moles (n) of that gas (1 mole gas = 22.4 liters STPD), R (gas constant) and T
n RT
P V =
PV = nRT
constant
21
WATER PARTIAL PRESSURE
The water added by the body dilutes the other gases such that all their partial pressures go down !!
760 = 47 + 713
P = 0.21 ( - ) = 150 mm Hg
Not the 160 mmHg of dry air
Pb PH O
2O2
Pb = PH2O + Pdry
PH2O = 47 mmHg
The gas partial pressure of water in equilibrium with liquidwater depends only on the temperature. The higher the temperature the higher partial pressure due to water.
At body temperature (37 C °) the
22
P = inspired oxygenI O
2
PI = % O2 (Pb - PH20)O2
The partial pressure of oxygen in the air that enters the body is reduced by the addition of water vapor.
Inspired air is diluted with water vapor until saturated.
That is why the partial pressure of oxygen
in inspired air is lower than dry room air.
23
PI = % O2 (Pb - PH20) = 0.21 x 713 = 150 mm Hg O
2
P = 104 mm Hg A
O 2
P = % O2 Pb = 160 mm Hg bO
2
Dry air
Humidified air
??Alveolar air partial pressure of oxygen ??
So why alveolar PO2 so low??
D’Alecy
Slide 10: Source Undetermined
Slide 12: D’Alecy
Slide 13: Source Undetermined
Slide 14: Source Undetermined
Slide 17: Source Undetermined
Slide 23: D’Alecy
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