Living and Working on the Moon – some Physiology Issues or The Highs and Lows of Oxygen Johnny Conkin, Ph.D. [with help from Jeff Jones, Richard Scheuring, Mike Gernhardt, Ramachandra Srinivasan, James Wessel, III, and James M. Waligora] Universities Space Research Association March 20, 2008 we will stay longer and do more EVAs topics z CEV (Orion), LSAM, and habitat atmospheres z mild hypoxia - problem with Equivalent Air Altitude concept z unintended consequences - haemoconcentration z yo-yo ppO2 exposures and superoxide radicals z integrated physiological response spacecraft atmosphere trade study - 2006 z Underlying Assumptions: z z z z Efficient and frequent EVAs will drive exploration program. Low pressure suit is always preferred to high pressure suit. There is operational value to a short in-suit prebreathe. Vehicle atmosphere may not prevent risk of DCS during EVA. z z z Shuttle and ISS atmospheres are examples. Dedicated hyperbaric treatment capability may not be present. Atmosphere Design Considerations: z z z No significant risk of fire – bad experience with 100% O2. Limit hypoxia – you need O2 with every breath. Prevent DCS and VGE. z z Better to prevent than treat DCS, or to constantly embolize the lung. Optimize atmosphere to allow safe and efficient EVAs. future spacecraft atmospheres Actual Altitude m ft Equivalent Air Altitude m ft 77 4,877 16,000 1,829 6,000 128 86 4,816 15,800 1,158 3,800 30.0 107 68 5,029 16,500 2,438 8,000 393 32.0 111 71 5,182 17,000 2,286 7,500 7.8 403 34.0 121 80 5,029 16,500 1,524 5,000 7.4 383 30.0 101 63 5,364 17,600 2,895 9,500 PB psia mmHg FIO2 (%) PIO2 mmHg normal 8.0 414 32.0 117 best case 8.2 424 34.0 worse case 7.8 403 normal 7.6 best case worse case Environment PAO2 mmHg CEV + LSAM HABITAT PIO2 is inspired O2 partial pressure, computed as (PB mmHg – 47) * FIO2 (as decimal fraction). PAO2 is computed acute alveolar oxygen partial pressure from alveolar oxygen equation. equivalent air altitude model - ascent on enriched O2 ambient oxygen fraction 0.45 150 0.40 130 0.35 110 0.30 0.25 EAA model 80 0.20 0.15 50 0.10 0.05 250 350 450 550 650 750 ambient pressure (mmHg) 850 FIO2 = PIO2 / (PB – 47) the issue PIO2 = (PB – 47) * FIO2 therefore it follows (PB(1) – 47) * FIO2(1) = (PB(2) – 47) * FIO2(2) but body response 1 ≠ body response 2 certainly when PIO2 is hypoxic acute mountain sickness z Signs and symptoms include headache, nausea, dizziness, fatigue, vomiting and sleeplessness following a recent gain in altitude with at least several hours at the new altitude in a hypoxic environment; likened to a bad hangover. z Anyone here had AMS – not just a hangover? “typical” response to hypobaric hypoxic exposure z Ascent causes a decrease in PaO2 sensed by the peripheral and central chemoreceptors, leading to increased minute ventilation rate (VE) – but some show little change in VE. z Hyperventilation in response to hypoxia increases PAO2 and subsequently decreases PACO2 and leads to a transient alkalosis. z There is also a hypoxia-induced diuresis as the kidney attempts to establish normal pH with the excretion of bicarbonate – but some show little change in urine output. the spectrum of hypoxia z Sudden ascent to high altitude would kill due to acute hypoxia while a gradual ascent could result in AMS or no symptoms at all. z Symptoms of AMS take hours to days to develop – seriously disturbed sleep: frequent arousals, periodic breathing, incessant dreaming. z Severe and prolonged hypoxic exposure may lead to High Altitude Pulmonary Edema, High Altitude Cerebral Edema, and even death. acute hypobaric hypoxia video incidence of mild AMS z The incidence of AMS is highly variable. z z z z z Roach (1998) reports that 25% of people are affected by a quick ascent to 2,000 m (6,600 ft). Montgomery (1989) shows 25% incidence of three or more symptoms at 2,000 m and that half with these symptoms took medication for relief of symptoms. Houston (1982) starts his list of AMS symptoms at altitudes above 2,100 m (7,000 ft). Muhm (2007) reports 11% AMS in large sample during 20 hrs at 2,438 m (8,000 ft). How do results from these actual altitudes translate to Equivalent Air Altitude? Lake Louise AMS Scoring System z Based on this 1991 committee’s recommendations: z A diagnosis of AMS is based on a recent gain in altitude, at least several hours (>2) at the new altitude, and the presence of headache and at least one of the following symptoms: gastrointestinal upset, fatigue or weakness, dizziness or lightheadedness and difficulty sleeping. z A score of three points or greater on the AMS Self-Report Questionnaire alone or in combination with the clinical assessment score is diagnostic of AMS. z Several signs and symptoms of AMS are shared with motion sickness – confounding a diagnosis of each! Self Report Questionnaire Each question asked and the sum is calculated as the AMS self report score. 1. Headache 2. Gastrointestinal Symptoms 3. Fatigue and/or Weakness 4. Dizziness / lightheadedness 5. Difficulty sleeping 0 No headache 1 Mild Headache 2 Moderate Headache 3 Severe Headache, incapacitating 0 No gastrointestinal symptoms 1 Poor appetite or nausea 2 Moderate nausea or vomiting 3 Severe nausea & vomiting, incapacitating 0 Not tired or weak 1 Mild fatigue/weakness 2 Moderate fatigue/weakness 3 Severe fatigue / weakness, incapacitating 0 Not Dizzy 1 Mild dizziness 2 Moderate dizziness 3 Severe dizziness, incapacitating 0 Slept as well as usual 1 Did not sleep as well as usual 2 Woke many times, poor night's sleep 3 Could not sleep at all Clinical Assessment The interviewers ratings of three signs is added to the self-report score. 6. Change in Mental Status 7. Ataxia (heel to toe walking) 8. Peripheral Edema 0 No Change in Mental Status 1 Lethargy / lassitude 2 Disoriented/confused 3 Stupor / semiconsciousness 4 Coma 0 No Ataxia 1 Maneuvers to maintain balance 2 Steps off line 3 Falls down 4 Can't stand 0 No peripheral edema 1 Peripheral edema at one location 2 Edema at two or more locations a debate is underway z Despite over a century of research there is still vigorous debate on the cause of AMS. z Certainly the brain is the target organ of and first responder to O2 deprivation. Paul Bert (1833-1886) z A French Physiologist considered the founder of Aerospace Medicine. z Demonstrated that the symptoms of AMS are prevented or relieved by breathing O2 – enriched air. z So “proved” that it was the decrease in partial pressure of O2 that caused AMS. z The doctrine that low partial pressure of O2 alone is the cause for AMS has dominated our thoughts. observations through the years z Rahn and Fenn (1956) disproved the simple notion of Equivalent Air Altitude, and conclude, “It is evidently not enough to equate the inspired O2 tensions …” z Since 1980s researchers have questioned the conventional wisdom that the symptoms of AMS are solely due to low O2 partial pressure. z Accumulated anecdotal evidence shows descent is more effective for relief of AMS than enriched O2 alone. z Savourey (2003) speaks of the “specific response to hypobaric hypoxia”. z So the door is open to investigate an independent PB effect on AMS. Tucker, 1983 z z Starts his experiments with subjects living at 1,524 m (5,000 ft – Colorado State University). Takes them to 15,000 ft on air and site pressure on 14% O2. Normobaric, PB = 760 mmHg Normoxic, PAO2 = 103 mmHg Hypoxic, PAO2<103 mmHg Altitude 1520 PAO2 = 77 No AMS symptoms Altitude 1520 m PAO2 = 47 Mean AMS Score: 3.2 Hypobaric PB<760 mmHg Environmental Symptoms Questionnaire Altitude 4570 m PB = 430 mmHg PAO2 = 45 Mean AMS Score: 5.7 with denitrogenation and 7.3 without ! Roach and Loeppky, 1996 z z Also starts experiment at 5,000 ft – University of New Mexico. They confirm the PB effect on the incidence of AMS. Normoxic, PAO2 = 103 mmHg Hypoxic, PAO2<103 mmHg Normobaric, PB = 760 mmHg Altitude 1520 m PAO2 = 76 No AMS symptoms Altitude 1520 m PAO2 = 47 Mean AMS Score: 2.0 Hypobaric PB<760 mmHg Altitude 4570 m PAO2 = 74 Mean AMS score: 0.4 Altitude 4570 m PAO2 = 46 Mean AMS Score: 3.7 Lake Louise scoring system the PB effect! z The pressure effect seems real, so to understand the total hypoxic stress means you have to understand the interaction between hypoxic PIO2 and PB. z A variety of explanations have been proposed for a PB effect on AMS. HH versus NH z Decreased gas density in HH z Decreased z Increased z work of breathing. insensible water loss. Transient N2 gradient out of tissues in HH and into tissues in NH condition z Larger N2 gradient in HH for the same PIO2 between HH and NH. z Takes longer in HH to come to new N2 equilibrium. z Potential for VGE in HH mechanics of breathing z Alveolar ventilation (VA) is influenced by PB: z Flow is ∝ to 1/√ gas density z Work of breathing is ∝ to relative density * VE3 z Diffusivity z of a gas is ∝ 1 / gas density These effects combined with differences in transient N2 kinetics do make NH and HH different. consider work of breathing z A decrease in VCO2 and VO2 decreases RER in HH relative to NH. z Loeppky (1997) shows: test PIO2 VE VA VCO2 VO2 mmHg l / min l / min ml / min ml / min NH 80 13.6 9.6 309 335 0.92 HH 80 10.3 7.4 226 263 0.86 RER (15,000 ft) z A decrease in RER decreases PAO2 and PACO2 in HH relative to NH. consider the role of N2 z N2 concentration gradient is into the body in NH and out of the body in HH. z A change in N2 concentration gradient changes the equilibrium FEN2 / FIN2 ratio for a given RQ. z As N2 moves from the lung to the tissues in NH there is a slight decrease in lung gas volume leading to slightly higher PAO2 and PACO2 and a smaller FEN2 / FIN2 ratio. z As N2 moves from the tissues to the lung in HH there is a slight increase in lung gas volume leading to slightly lower PAO2 and PACO2 and a larger FEN2 / FIN2 ratio. z Less work of breathing and N2 movement out of tissues drives PAO2 and PACO2 lower in HH relative to NH. Savourey’s and Loeppky’s summary with PIO2 of 81 mmHg Test PIO2 (mmHg) PETO2 PETCO2 (mmHg) (mmHg) NH 81 higher higher HH 81 lower lower Savourey’s 40 minute test in 15 subjects with PIO2 of 81 mmHg Test NH PIO2 PaO2 PaCO2 (mmHg) (mmHg) (mmHg) 81 51.7 37.9 81 47.8 34.8 (12% O2) HH (15,000 ft) Arterial blood gases obtained at end of 40 min test. consider the brain z For the same hypoxic PIO2 at different PBs: z z z z z PCSFO2 and PCSFCO2 is transiently higher in the NH relative to HH. VE should therefore be higher, and it is. Cerebral blood flow may be lower in HH relative to NH. Presentation of AMS should be different, and it is. One only needs to measure PCSFO2 and pH through time given identical hypoxic PIO2 at two different PBs to test the basic hypothesis. accounting for the PB effect on AMS z A precise model does not yet exist. z A new iso-hypoxic model would be a refinement of the current Equivalent Air Altitude model, which empirical data suggests needs to be refined. z You need to increase both PIO2 and PICO2 a bit in the breathing mix at altitude to achieve the same hypoxic condition tested at sea level. three hypoxic isopleths 0.350 iso-hypoxic model ambient oxygen fraction 0.325 0.300 0.275 90 80 0.250 110 0.225 0.200 100 0.175 0.150 0.125 0.100 250 ____ FIO2 = PIO2 / (PB – 47) 350 450 550 650 750 ambient pressure (mmHg) 850 ----- FIO2 = √(PB – 47) * 100 / (dose + 0.02) * (PB – 47)2 NASA atmosphere experience 1.0 ambient oxygen fraction 0.9 0.8 211-Apollo NASA 148-Skylab 0.7 0.6 0.5 117-CEV 111-habitat 0.4 0.3 0.2 0.1 200 80 ? 127-Shuttle Loeppky 300 400 500 600 700 ambient pressure (mmHg) 800 So….. Are astronauts at risk for AMS? -- yes about 25% worse case probability early in mission with 0% once acclimatization occurs. At greater risk than the 6,000 ft (CEV/LSAM) and 7,500 ft (habitat) Equivalent Air Altitude suggests. Develop a plan to mitigate the risk even if risk is unclear. to reiterate -- performance z We are dealing with performance issues and mission success, not life and death, with the AMS anticipated in the CEV. z We want to maximize performance and minimize any medical issues that impact mission success – our job. prevention and treatment of AMS z Preadaptation z Preselection z z The best predictor of AMS is history of prior episodes. Mild AMS is prevented / treated by: z z z z z Halting or slowing ascent – phased hypoxic exposure Denitrogenation Acclimatization Acetazolamide (125-250 mg BID) O2 therapy via mask or canula other considerations z Does μG modify the likelihood or character of AMS? z z z z Redistribution of lung fluid – 25% increase in CapBV Increased interstitial edema – puffy face response Increased incidence of HAPE? Potential negative synergy on combining mild hypoxia and adaptation to μG – increase in hematocrit leads to increased blood viscosity. z z Six reports suggest this may not be a significant concern – keep hematocrit below 55% Dr. Srinivasan is updating the Skylab Erythropoiesis Model. EP concentration (mU/ml or um/l) erythropoietin -- PIO2 and time 30 28 26 24 22 20 18 16 14 12 10 0 A B C D A = 2805 meters (PIO2 = 103 mmHg) B = 2454 meters (PIO2 = 108 mmHg) C = 2085 meters (PIO2 = 114 mmHg) D = 1780 meters (PIO2 = 119 mmHg) 5 10 15 TIME (HRS) 20 25 Ge Ri-Li, et al. Determinants of erythropoietin release in response to short-term hypobaric hypoxia. J Appl Physiol 92: 2361-67, 2001. Basu M, et al. Erythropoietin levels in lowlanders and high-altitude natives at 3,450 m. Aviat Space Environ Med 78:963-67, 2007. optimum HCT for O2 transport yo-yo ppO2 exposures Repetitive exposure to mild hypoxic (habitat) and mild hyperoxic (suit) environments may have biochemical consequences – no one does this type of repetitive long-term operation. Living at a habitat PIO2 of 111 mmHg for 40 hrs with EVA exposures to 175 mmHg for 8 hrs may have unexpected cumulative effects? This is like living at sea level in 15% O2 for 40 hrs and then 25% O2 for 8 hrs – over and over and over again. The up-and-down regulation of antioxidant enzyme systems (superoxide dismutase and catalase) over many months may exhaust the ability to manage reactive O2 species. additional information? z A copy of this PowerPoint presentation. z Conkin J. Risk assessment of acute mountain sickness in the crew exploration vehicle. NASA/TP-2008-214759, Johnson Space Center, Houston, Tx, January 2008. z Scheuring RA, Conkin J, Jones JA, Gernhardt ML. Risk assessment of physiological effects of atmospheric composition and pressure in Constellation vehicles. Acta Astronautica (in press). z Conkin J, Wessel JH, III. Critique of the equivalent air altitude model. Aviat Space Environ Med (in review). thank you for your time