Page 1850 - Hall et al (2015) Principles of Critical Care-McGraw-Hill
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CHAPTER 132: Diving Medicine and Drowning   1319


                                                           . Continuing CO 2   to distinguish it from unconsciousness after breath-hold swimming
                    as the alveolar P CO 2  approaches the mixed venous P CO 2
                                                   , which then allows the alve-  events performed entirely in shallow water, such as in pools.  Both types
                                                                                                                     3
                    production increases the mixed venous P CO 2
                                                    causes breathing to resume   of events are responsible for many episodes of drowning.
                    olar P CO 2  to increase further. The rising P CO 2
                    at the so-called break point. The time to the break point can be extended   In breath-hold diving, the physiology is modified by a diving response
                                                        such as hyperventila-  induced by apnea and facial immersion, particularly if the water is cold.
                    by maneuvers that lower the P CO 2  or raise the P O 2
                    tion or O 2 breathing. Hyperventilation does not appreciably increase the   This diving response, manifested by the triad of apnea, bradycardia,
                                                            resulting from a   and redistribution of organ blood flow is most pronounced in young
                    body’s O 2 stores because the increase in alveolar P O 2
                                      only increases blood O 2 content slightly. Thus,   children. It has been interpreted as an O 2-conserving response that
                    decrease in alveolar P CO 2
                    hyperventilation extends breath-hold time, but profound hypoxia may   redistributes blood flow from organs resistant to hypoxia to organs with
                    develop before the CO 2 reaches the break point.      continuous O 2 needs such as heart and brain. This diving response may
                     The physiology of breath-holding is altered by underwater descent   convey a small advantage to trained human apnea divers, and it probably
                    because the thoracic compression decreases the lung volume, which   does contribute to the survival of children after submersion in cold water.
                    increases the partial pressures of O 2, CO 2, and N 2 in the lungs (Fig. 132-1).
                    The alveolar O 2 and CO 2 concentrations decrease faster than the inert   DIVING WITH COMPRESSED GASES
                    gas (N 2) because those gases are transferred more quickly to the pulmo-
                    nary capillary blood as O  is consumed and since CO 2 is more soluble   The practical utility of underwater breath-hold diving is limited by time
                                      2
                    than nitrogen.                                        and depth, although today there are still working free divers, such as the
                                                                  initially   Japanese Ama, and competitive, “no-limit” apnea divers have achieved
                     Compared with a simple breath-hold in air, the alveolar P O 2
                    increases during a breath-hold dive due to the increase in pressure on   depths exceeding 200 m. The use of pressurized underwater breathing
                    the thorax. The transfer of CO 2 during the early descent is opposite    apparatus provides the diver with a continuous supply of breathing gas
                    normal, and CO 2 moves from alveoli to pulmonary capillary blood.   at almost any depth. In shallow water, for instance, 0 to 135 fsw, diving
                    During ascent, the lung re-expands, and as the pressure decreases, so   is usually carried out with compressed air because it is inexpensive
                                                                    may   and readily available, even at remote locations. Air divers are usually
                    do the alveolar P O 2  and P CO 2 . Near the surface, the alveolar P O 2
                                           , and during ascent from particularly   free swimming, that is, they use a self-contained underwater breathing
                    approach the mixed venous P O 2
                    strenuous dives, the expansion of hypoxic alveoli may result in reverse   apparatus (SCUBA). Special gas mixtures, such as 32% nitrogen-oxygen
                    O 2 transfer from mixed venous blood to alveoli (see Fig. 132-1). Carbon   (nitrox), used to extend the bottom time and/or provide an extra safety
                    dioxide in the blood during the dive also leaves during ascent as alveolar   margin, are increasingly being used by recreational divers.
                        decreases. Carbon dioxide elimination continues after the dive as   The recommended maximum safe depth for Scuba divers is 135 fsw
                    P CO 2
                    does the elimination of the small amount of N 2 that entered the blood   and approximately 200 fsw for divers tethered to a safety line.  Safety
                                                                                                                        4
                    during the dive.                                      concerns are brought about by three factors: nitrogen narcosis, safe
                     Hyperventilation before a breath-hold dive is a dangerous way to   decompression,  and  oxygen  toxicity.  The  problems  of  importance  to
                                                           initially increases   the intensive care specialist are related to decompression illness and
                    extend the duration of dive. Because the alveolar P O 2
                    from thoracic compression, the primary signal to return to the surface is   pulmonary overpressurization as discussed below. The other problems
                         . If the diver hyperventilates before the breath-hold, the arterial   are covered in standard textbooks on diving medicine.
                    the P CO 2
                        begins at a lower level, which extends the time to the break point.   To dive beyond the practical range of compressed air, special gas mix-
                    P CO 2
                    During the longer dive, the alveolar O 2 concentration decreases to lower   tures, such as helium-oxygen (heliox) or oxygen-enriched air (nitrox)
                    levels, and as the diver approaches the surface, life-threatening hypoxia   must be supplied. In heliox operations, inspired oxygen pressure is
                    and loss of consciousness may occur. Traditionally, this is called shallow   usually maintained at a constant 0.4 to 1.0 ATA, and the helium may
                    water blackout, although free divers may refer to it as deep water blackout   be recycled by gas reconditioning equipment. Surface-supplied heliox
                                         A                                       D

                                               Pa    Pa                                Pa     Pa
                                       Pv        O 2   CO 2  Pa                 Pv       O 2   CO 2   Pa
                                         O 2   120    25       O 2                O 2   30     45       O 2
                                         40                   110                35                    30

                                       Pv                   Pa                  Pv                    Pa
                                         CO 2                 CO 2                CO 2                 CO 2
                                         46                   25                 55                    45
                                                     Descent                                 Ascent


                                         B                                       C


                                          Pv O 2  150  25   Pa O 2                Pv O 2  35  50    Pa O 2
                                          40                135   Breath-hold time  35               35
                                         Pv                Pa                     Pv                Pa
                                           CO 2              CO 2                  CO 2               CO 2
                                          46                30                     55                50
                    FIGURE 132-1.  Mechanism of shallow water blackout. All values are expressed in millimeters of mercury. A. The breath-hold diver hyperventilates before the dive to bring down the
                                                                 ) increase as the alveoli are compressed by hydrostatic pressure. C. At the end of the breath-hold dive, CO 2
                    alveolar partial pressure of CO 2 (Pa CO 2 ). B. At depth, arterial CO 2 (Pa CO 2 ) and O 2 (Pa O 2
                                                                                                            decrease as the alveoli reexpand;
                    increases toward the break point, and the diver begins to ascend. Note the decreased Pa O 2  and Pa O 2  at this point. D. When approaching the surface, Pa CO 2  and Pa O 2
                    O 2 leaves the pulmonary capillaries and enters the alveoli. This may result in profound hypoxemia and produce unconsciousness.






            section11.indd   1319                                                                                      1/19/2015   10:56:09 AM
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