ASEN 5016 Lecture 4: Respiration and
the Oxygen Cascade
OBJECTIVES
1. Define Standard Atmosphere Pressure and Composition
2. Describe Respiration Factors Associated with Increasing Altitude / Decreasing Atmospheric Pressure
3. Identify Critical Parameters for Normoxic Conditions
4. Describe the Oxygen Cascade and Complicating Factors
5. Explain Engineering Trade Factors wrt Cabin Pressure
6. Discuss Current Research into Effects of Space Flight on Pulmonary Function
1. Standard Atmosphere Pressure and Composition
Normoxic Conditions
· 3.1 psia ppO2 (160 torr)
· 21% of 1 standard atm (14.7 psia or 760 torr)
"Shirt Sleeve" Environment
Dalton’s Law of Partial Pressure
Partial pressure of gas in a mixture = total pressure if it was the only gas in same volume
2. Factors Associated with Increasing Altitude
Exponential Pressure Decay
· 14.7 psia at sea level
· ~ 10 psia at 10,000 feet MSL
· ~ 6.7 psia at 20,320 feet MSL
·
At ~15 km (P = 87 torr)
à 100% oxygen needed, since combined
water vapor and CO2 in the lung = total barometric pressure
Above this point, gas exchange becomes physiologically impossible (~transition
from hypoxia to anoxia)
· Above 19.2 km (P = 47 torr) à body fluids boil at 37° C (Armstrong limit)
Discuss Earth’s equatorial ‘bulge’ and
‘Physiological Altitude’ equivalence
3. Critical Parameters for Normoxic Conditions
· Alveolar Oxygen Pressure (PaO2)
The PaO2 relationship given below defines the partial pressure of oxygen in the alveoli as a function of various environmental parameters.
where:
FiO2 = fraction
of oxygen in the inspired air
Pb = ambient barometric pressure
PH2O = water
vapor pressure at 37 C
R = respiratory exchange ratio
When PaO2 reaches 60 mmHg, the blood is only 87% saturated with oxygen and hypoxia sets in.
CO2
· CO2 levels on Earth
~350 - 380 ppm now
Was ~280 ppm pre-industrial revolution era
· Effects on respiration
CO2 Diffuses ~20x faster than O2
Too much = blood becomes acidic – no O2 – fainting
Too little = alkaline – hyperventilation – fainting
· CO2 limits in buildings
ASHRAE standard 62-1989 recommends a maximum CO2 level of 1000 ppm. The proposed new OSHA standard (29CFR Part 1910.1033) calls for investigation if the CO2 level exceeds 800 ppm of CO2.
· CO2 runs in the 2000-3000 ppm range in the orbiter with 10,000 (1%) = safety limit
4. The Oxygen Cascade
· O2 Cycle
· Acquisition – diffusion (breathing)
· Exchange with CO2
· Transportation – blood flow
· Delivery – RBC (takes ~0.75 sec to traverse capillary and ~0.5 sec for diffusion exchange)
· Utilization – Mitochondria
·
Byproduct – CO2
O2 Cascade
· Atmosphere / Lung / Alveoli / Capillaries / Arteries / Capillaries / Tissue (mitochondria) / Veins
· ppO2 is highest in the air, lower in the lungs where it is diluted with CO2 and H2O, and continues to drop in pp down through the cascade
– diagram corresponding delta P across each
Lungs
Tidal volume ~500 ml in/out with each normal
breath
Only about 350 ml of new air reaches the alveoli with each breath
Expired air is still about 16% O2 (sea level)
Inspiratory reserve ~ 3000 ml – max extra volume that
can be inspired over / above tidal
Inspiratory capacity ~3500 ml total
Expiratory reserve ~ 1100 ml – max extra vol that can
be expired after normal breath
Residual volume ~ 1200 ml – remainder after max forceful expiration
Vital capacity = inspiratory reserve (3000) + tidal
volume (500) + expiratory reserve (1100) = (~4600 ml) = max out after max in
Total lung capacity = ~5800 ml (vital + residual) max volume that lungs can be
expanded
Additional (anatomic) dead space ~ 150 ml (everything outside the aveoli)
Physiological dead space – some alveoli non-functional in pulmonary disease
(fluid or foreign material - pulmonary edema, pneumonia, etc.)
(All volumes are ~20-25% less for women and greater in large and athletic individuals)
Normal respiration rate = 12 breaths / min
Max resp rate = 40-50 breaths / min or > 200
liters / min (~53 gal/min)
Diffusion area of the lungs ~750 Sq ft (~100x larger than the chest volume alone)
Lungs literally ‘float’ in the thoracic cavity, surrounded by pleural fluid that acts as a lubricant as the chest expands and contracts
Air rises to within ~ 1 deg F of normal body temp and within 2-3% of H2O saturation in the trachea
· TLC = RV + ERV + TV + IRV
– Total Lung Capacity
– Residual Volume
– Expiratory Reserve Volume
– Tidal Volume
– Inspiratory Reserve Volume
Discuss transport phenomena of O2 and CO2 in
the blood…
Factors Affecting O2 Cascade
Too little O2 = hypoxia
Too much O2 = toxicity
· Exposure time and pressure dependent
· 100% O2 at SL for 6-24 hours can become toxic (chronic issues)
· Apollo astronauts lived for 2 weeks at 5 psia 100% O2
· Saturation / deep diver concerns
· 4 atm O2 leads to acute toxicity, coma likely within 30-40 minutes
Causes of reduced O2 uptake,
some potentially relevant to space flight conditions:
ppO2
Deviation from “normoxic”
standard atmosphere, sea level conditions (see above)
Presence
of other gasses
CO2 - (see above)
CO - Forms
a bond 200x stronger than O2 with hemoglobin
Symptoms include
headache, nausea, confusion, sleepiness, dizziness, or
longer term, memory loss, neurological or psychological problems
Usually reversible if caught in time, dependent on how much
and how long
Even low levels of CO
can lead to permanent damage to heart, brain and CNS, however
When people are said to
be ‘overcome by smoke’ in a fire, the culprit is CO, which can range from
10k-50k ppm
just a few breaths can lead to 100% blood saturation and quickly result in
unconsciousness or death
(cigarette smoking exposes lungs
to 1k-2k ppm CO, smokers typically have CO blood
levels just below concentration considered poisonous)
At
altitude (reduced total pressure) CO has additional advantages over O2
Binding
rate elevated and effects more pronounced of same CO concentration at sea level
due to lack of available O2
Transport
Too few RBC’s
(anemia)
Reduced blood flow
Obstruction
/ disease in the lungs / alveoli
Fibrosis or emphysema
Pneumonia
Asthma
H.A.P.E.
Asbestosis
Mechanical
aspects
Constriction of chest cavity
(reducing tidal volume of lungs)
Diaphragm malfunction
Physiological effects
Environmental effects (aerosols)
Gravity?
‘Train low / sleep high’ athletic performance enhancement concept
5. Engineering Trade Factors related to Oxygen (and Total
Pressure) Levels
Engineering (and Physiological) Trade Variables
· Maintain normoxic (i.e., neither hyperoxic nor hypoxic) conditions
· Minimize flammability (< 30% O2)
· Sufficient density for convective cooling
· Minimize risk of DCS (caisson disease, the bends) during transition to EVA
· Ensure sufficient pressure shell structural strength
· Compensate for cabin leakage
· Remove CO2 and humidity
“An average of 1.76 pounds of oxygen is used per flight crew member per day. Up to 7.7 pounds of nitrogen and 9 pounds of oxygen are expected to be used per day for normal loss of crew cabin gas to space and metabolic usage.”
Critical relationship between cabin pressure, physiology, vehicle
structure and material, launch mass, ECLSS performance, space suit ops, etc…
6. Research into Effects of Space Flight on Pulmonary Function
J Appl Physiol 2000 Sep; 89(3):1239-48 Glenny RW, Lamm WJ, Bernard SL, An D, Chornuk M, Pool SL, Wagner WW Jr, Hlastala MP, Robertson HT.
…both gravity and the geometry of the pulmonary vascular tree influence regional pulmonary blood flow - Selected contribution: redistribution of pulmonary perfusion during weightlessness and increased gravity.
Microgravity and the lung. Prisk GK. Appl Physiol 2000 Jul; 89(1):385-96J
Diffusing capacity increases markedly,
due to increases in both pulmonary capillary blood volume and membrane diffusing
capacity, likely due to more uniform pulmonary perfusion. Both ventilation and
perfusion become more uniform throughout the lung, although much residual inhomogeneity remains. Despite the improvement in the
distribution of both ventilation and perfusion, the range of the
ventilation-to-perfusion ratio seen during a normal breath remains unaltered,
possibly because of a spatial mismatch between ventilation and perfusion on a
small scale. There are unexpected changes in the mixing of gas in the periphery
of the lung, and evidence suggests that the intrinsic inhomogeneity
of the lung exists at a scale of an acinus or a few acini. In addition, aerosol deposition in the alveolar
region is unexpectedly high compared with existing models.
J Appl
Physiol 89:1 379-384, 2000, Historical
Perspectives: Physiology in microgravity, John B. West
Pulmonary function is greatly altered
but apparently not seriously impaired.
The lung is exquisitely sensitive to gravity, which normally causes regional differences in ventilation, blood flow, gas exchange, alveolar size, intrapleural pressure, and parenchymal stress. Therefore, it is not surprising that a variety of changes in pulmonary function have now been described. The distributions of ventilation and blood flow become more uniform, although not entirely so, and there are reductions in some lung volumes, including functional residual capacity and residual volume. However, overall, gas exchange is little affected. One of the reasons for monitoring pulmonary function during spaceflight is because of the vulnerability of the lung to changes in the atmosphere of the spacecraft. A dramatic example was a fire that occurred on Mir, which, fortunately, was rapidly brought under control. Aerosol contamination of the spacecraft is another potential hazard.
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