What is pulmomary ventilation ?
Total volume of air breathed in and out per minute
-MV = tidal volume (L/breath) x Respiratory Rate (breath/min)
-e .g. = 0.5 L X 12 breath/min = 6 L/min under resting conditions
-Max MV (MMV) could up to 180L/min
Aka minute ventilation
What is Alveolar Ventilation ?
Volume of air that reaches the alveoli and participate in gas exchange per minute
-AV= (tidal volume – dead space volume) x Respiratory Rate
-E.g = (0.5 – 0.15) x 12 = 4.2 L/min under resting conditions.
Not all inhaled air gets to gas exchange
What is anatomical dead space ?
Some inspired air remains in the airways where it is not available for gas exchange ( 150ml)
-Helps condition incoming air (warm, humidify, filter)
How does Kinetic gas theory explain gas pressure ?
Gases are a collection of molecules moving randomly around a space
-Pressure is generated by collisions of molecules with a surface
-The more frequent and harder the collisions the higher the pressure generated by the gas
What is the ideal gas equation ?
Properties of gases can be described by the ideal gas equation:
PV = nRT
Where:
P = pressure
V = volume
n = number of moles of gas
R = gas constant
T = absolute temperature (Kelvin)
Gas molecule speed depends almost all on temp
What is Boyle’s law ?
Pressure (P) of a gas is inversely proportional to its volume (V) for a given temp and no. of moles in closed systen
P∝ 1/𝑉
How is breathing an example of Boyle’s Law ?
Breathing occurs because of pressure gradients:
Diaphragm contracts → thoracic volume ↑ → alveolar pressure ↓ → air flows into lungs
When muscles relax → thoracic volume ↓ → alveolar pressure ↑ → air flows out
Mechanism of inspiration & expiration is an example of Boyle’s Law
What is Dalton’s Law ?
In a mixture of gases, the total pressure = the sum of the partial pressures of the individual gases
-Air pressure = sum of p02 + pN2 (mostly)
How does altitude affect pressure ?
At sea level: 101 kilopascals (kPa) = 1 atmosphere = 760 mmHg
At high altitudes atmospheric pressure is lower (weight of air pressing down is less)
What are the partial pressures of the air gases at sea level ?
Partial pressure of O2 = 101 x 20.9% = 21.1 kPa
Partial pressure of N2 = 101 x 78 % = 78.7 kPa
Partial pressure of CO2 = 101 x 0.03%= 0.03 kPa
Atmospheric Pressure at sea level =101 kiloPascals (kPa)
How do gases dissolve and diffuse ?
According to their partial pressure
-Gases diffuse down partial pressure gradients from area of higher to lower in body e.g. movement of oxygen from alveolar air ↔ blood
-Partial pressures used instead of conc to describe gases in body
Gases in mix can move independently and in different directions to other
How is partial pressure denoted ?
Denoted by ‘p’ - as in pO2, pCO2, pN2
What happens when inspired gases come into contact with the thin layer of water lining the airways and alveoli ?
1) Gas molecules
-Gas molecules will enter water to dissolve in liquid
-According to Henry law: PP X Solubility
2) Water molecules evaporate to enter air
-Humidify
-Reduced other gases PP (helpful for continous flow of oxygen from upper airway to lower airway; lower parts more humid than upper parts)
Gas dissolving in liquid depends on PP and solublity
What is vapour pressure ?
Water molecules entering the air exert ‘vapour pressure’
At equilibrium,
-Rate of H2O evaporation = rate of H2O condensation
-The air is saturated with vapour
-Saturated Vapour Pressure (SVP) = 6.28kPa at body temp
-Inhaled air becomes saturated with water, in the upper respiratory tract
How is equilibrium of a dissolved gas reached ?
Dissolved gas molecules also exert pressure in the liquid
At equilibrium:
-Rate of gas entering water = rate of gas leaving the water.
-Partial pressure of the gas in the liquid = partial pressure of the gas in the air above it
another term used for partial pressure of a gas in the liquid is ‘tension’ (e.g. oxygen tension in blood)
How much oxygen dissolved in plasma ?
Solubility coefficient of O2 in plasma = 0.01 mmol L-1 kPa-1 at body temp.
pO2 of 13.3 kPa (as in alveolar air)
-0.01 x 13.3 = 0.13 mmol of O2 will dissolve (15ml/min)
(this is no where near enough, needs 250ml/min, heart would need to beat 17 times as fast for thsi to work which it very much cant do)
What is the partial pressure of oxygen at both ends of the resp tract ?
Breathed in at 21.1 kPa
Alveolar air is 13.3 kPA
How can the blood absorb enough oxygen ?
O2 dissolves in plasma and enters RBC to bind to Hb
-This must complete before equilibrium is reached and partial pressure is established.
-Blood contains both dissolved and Hb bound oxygen
pO2 is a measure of dissolved O2 in the blood (proportional)
When does plasma oxygen binding to Hb stop and what does this achieve ?
-Process continues till Hb fully saturated (each Hb molecules binds 4 O2 molecules)
-After Hb is fully saturated, O2 continues to dissolve till equilibrium is reached
-At equilibrium, pO2 of plasma = pO2 of alveolar air
How does Hb bound oxygen travel to tissues ?
-Dissolved O2 is available to diffuse into tissues down its partial pressure gradient
-As dissolved O2 leaves the blood, it will be replaced by O2 bound to Hb
-In this way, the oxygen bound to Hb will be downloaded and diffuse into tissues
The pO2 is a measure of dissolved O2 in the blood (proportional)
What are the partial pressures of 02 and C02 in alveolar air and why ?
pO2 =13.3 kPa (lower than inhaled air)
pCO2 =5.3 kPa (higher than in inhaled air)
Because
-Inhaled air mixes with residual volume
-Effect of O2 diffusing across the alveolar wall
-Effect of CO2 entering the alveoli
-Alveolar air composition stays constant around this level;
-Blood equilibrates to this level
How do partial pressures of 02 and C02 at the alveoli determine their movement ?
Alveolar PO2 > PO2 in mixed venous blood
Alveolar PCO2 < PCO2 in mixed venous blood
So, oxygen will diffuse into blood and carbon dioxide out
Which are the factors affecting the rate of diffusion ?
Partial pressure difference (gradient) across membrane (P1 – P2 )
A - the surface area available for diffusion
T – (thickness) i.e. distance molecules must diffuse
D - diffusion coefficient of the individual gas
Rate is inversely proportional to T