Dysbarisms, Dive Injuries, and Decompression Illness

133 Dysbarisms, Dive Injuries, and Decompression Illness





Epidemiology


Dysbarisms refer to the pathophysiologic effects of changes in ambient (surrounding) pressure on the body. Decompression illness (DCI) includes decompression sickness (DCS or “the bends”) and arterial gas embolism (AGE). DCI occurs during or after ascent (decompression) when dissolved gases come out of solution, form bubbles, and then become lodged in various tissues (instead of being filtered by the lungs). Diagnosis of DCI in the emergency department (ED) is vital because delayed treatment or missed cases can have permanent sequelae (Box 133.1).



With the advent of “extreme sports” that involve water contact, sport diving, and the increasing number of people engaging in breath-hold diving, a sharp increase in diving injuries has been seen in EDs (Box 133.2). Deaths from breath-hold diving alone have almost doubled in the last 5 years, thus illustrating the potential for injury associated with this form of diving.1 With acute DCI, rapid assessment and treatment are the foundation of management. Three keys to successful ED treatment are having a high index of suspicion (DCI may have nonspecific findings), performing a thorough neurologic examination, and obtaining hyperbaric medicine consultation when DCI is suspected.




Pathophysiology


Dysbarism refers to the effects of variations in ambient (surrounding) pressure on the body. Hypobaric (low-pressure) exposure, such as that experienced by climbers, pilots, and astronauts, can result in symptoms and injuries similar to those found in divers with DCI who are exposed to high pressure while at depth. Decompression injuries during high-pressure (hyperbaric) exposure are far more common.



Diving Physiology


Evaluation of a diver with a water-associated injury requires a basic understanding of diving physiology and the physics of pressure and gases. Different gases have different properties at different depths, which allows gases to be used alone or in combination for different types of diving. The gases of most interest are air, oxygen, nitrogen, helium, and occasionally argon. Deep diving (past 180 feet of sea water [fsw]) often requires helium-oxygen combinations (heliox) to mitigate the effects of nitrogen narcosis (discussed later). Moreover, enriched nitrogen-oxygen combinations (nitrox) may be used to reduce obligations for decompression stops, which is the time spent at more shallow depths to help divers offload the nitrogen built up in the body before exiting a dive.


In general, most recreational divers breathe compressed air and use a self-contained underwater breathing apparatus (SCUBA) when diving to depths of less than 135 fsw. Nitrogen represents about 78% of the gas inhaled with compressed air diving. During diving, hydrostatic pressure “pushes” nitrogen into tissues; nitrogen (an inert gas) then becomes dissolved in plasma and permeates tissues. While at depth, gases remain in solution, and most divers experience minimal difficulty. The deeper that divers travel and the longer that they remain at depth, the more saturated the blood and tissues become with nitrogen (or other inspired inert gases). One of the tenets of diving is to ascend slowly when resurfacing. Doing so allows the dissolved (inert) gases to escape the tissues slowly and be cleared via normal respiration. If a person ascends to the surface too quickly, the dissolved gases come out of solution and form bubbles in tissues or within the vasculature. When these bubbles are not cleared by the lungs (“blown off”) they can embolize and cause downstream injury or they can cause local damage at the site of formation (autochthonous bubbles). When bubbles cause symptoms, the disorder is called DCI. Depending on the size, number, and location of the bubbles, DCI has a wide range of manifestations, from pain (most common symptom), numbness, and fatigue to severe neurologic symptoms such as seizure, paralysis, and loss of consciousness (LOC).



Bubble Physiology


Knowledge of bubble mechanics and the effects of bubbles in various tissues is critical to understanding the pathophysiology and treatment of DCI. Venous bubbles are not usually problematic because the lungs can filter large gas loads. Bubbles have damaging effects when they remain within tissues or embolize. Bubbles can pass from the venous circulation to the arterial circulation via a right-to-left shunt (patent foramen ovale or arteriovenous malformation). Bubbles can grow from “nucleation sites” within body tissues, such as the joint spaces, tendon sheaths, periarticular sheaths, and peripheral nerves.2 Once inside these areas, bubbles can act as emboli and block perfusion of distal tissues or act as foreign bodies with resultant vascular damage through activation of the inflammatory and clotting cascades. Interestingly, scientists are now evaluating a possible biologic marker of DCI. As gas emboli within the circulation induce decompression stress, endothelial cells release microparticles in response to cellular activation or cell death. These microparticles may, in the future, reflect a biologic marker of decompression stress that can be used to gauge the extent of disease, efficacy of treatment, or prophylaxis.3



Principles of Gas Laws and Dysbarism


An understanding of the pertinent diving gas laws, units of measurement, abbreviations, and mathematic conversions helps facilitate the treatment and disposition of dive-injured patients. At sea level, the pressure of the atmosphere on the body (ambient pressure) is 760 mm Hg, which equals 1 atm. The term for the absolute pressure on a diver at sea level is called atmospheres absolute (ATA), and it represents the total sum of the pressure on a diver. Therefore, at sea level, a dive computer gauge reads zero, but sea level also represents one surrounding atmosphere of pressure (1 ATA). This knowledge helps the physician better comprehend the circumstances surrounding a dive injury. Although there are a large number of gas laws, the two that are the most important in diving medicine are Boyle’s law and Dalton’s law.





Presenting Signs and Symptoms



Barotrauma


Barotrauma is sustained from failure to equalize the pressure of an air-containing space with that of the surrounding environment. The most common examples of barotrauma occur during air travel and scuba diving.1,4 Barotrauma occurs only in gas-containing (compressible) body spaces. More than 95% of the body is composed of water (incompressible). Typical gas-filled spaces include the sinuses, middle and inner ears, air-filled areas within carious or filled teeth, and hollow viscous organs such as the intestines and lungs. Barotrauma incurred during descent is called a “squeeze.” Barotrauma incurred during ascent is called a “reverse squeeze,” “reverse block,” or expansion injury.



Differential Diagnosis and Medical Decision Making


Table 133.1 lists the differential diagnosis for dive injuries based on the time of onset of symptoms.


Table 133.1 Differential Diagnosis of Dive Injuries Based on the Onset of Symptoms





















SYMPTOM ONSET INJURIES TO CONSIDER
Descent
Bottom
Ascent
15 min after resurfacing
15 min to 24 hr after resurfacing

Jun 14, 2016 | Posted by in EMERGENCY MEDICINE | Comments Off on Dysbarisms, Dive Injuries, and Decompression Illness

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