Chapter 139 Unlike other animals that live outside the tropics, humans are susceptible to peripheral cold injuries. The highest homeostatic priority is to maintain the body’s core temperature. This is accomplished through peripheral vasoconstriction and shunting, which prevent adequate heat distribution to the extremities. As a result, failure to achieve adequate protection from the environment results in injuries that are usually preventable.1–3 Peripheral cold injuries include both freezing and nonfreezing syndromes, which may occur independently or in conjunction with systemic hypothermia.4 Frostbite is the most common freezing injury.5 Trench foot and immersion foot are nonfreezing injuries that result from exposure to wet cold.6 Nonfreezing injury that usually occurs after exposure to dry cold is termed chilblains (pernio).7 The incidence and severity of frostbite correlate with predisposing factors as well as with the degree of cold stress. Most cases of civilian frostbite result from exposure to cold by individuals who have not given due consideration to risk factors for cold injury.8,9 Well-equipped ascents of the world’s highest peaks have been completed without cold injury when appropriate steps have been taken to address these factors.10,11 An increase in outdoor recreational activities has increased the number of people exposed to severe cold conditions.12,13 Unsheltered homeless people are no longer the most likely group at risk in areas with moderate climates.14 Military history is replete with accounts of the effects of cold injury on combat troops.15,16 Amputations and time lost to local cold injuries in both world wars and the Korean conflict were extensive. Trench foot was common among Argentine and British forces in the Falkland Islands.4,17 Napoleon’s Surgeon General, Baron Larrey, first recorded the disastrous effects of the freeze-thaw-refreeze cycle.18 During the 1812 to 1813 Russian invasion and retreat, soldiers would acutely thaw frozen extremities directly over open fires. The subsequent refreeze further increased tissue destruction. Unfortunately, the resultant gangrene was misattributed to this rapid thawing of frostbite and trench foot injuries. Therefore, gradual thawing, often including friction massage with snow, remained the standard treatment regimen until the 1950s.19,20 In 1961, Mills ultimately popularized rapid warm immersion rewarming after extensive experience with severe Alaskan frostbite cases.20,21 In contrast to heat exposure, humans do not appear to display significant physiologic adaptation to the cold. Exposure of extremities to temperatures down to 15° C results in maximal peripheral vasoconstriction with minimal blood flow. Continued exposure to progressively colder temperatures down to 10° C produces the “hunting response,” which is cold-induced vasodilation.22 These periods of vasodilation, recurring in 5- to 10-minute cycles, interrupt vasoconstriction and serve to protect the extremity. Eskimos as well as Lapps and others of Nordic extraction are capable of stronger cold-induced vasodilation than that in individuals from tropical regions. Measurement of the speed of cold-induced vasodilation may help predict an individual’s risk for cold injury.23 There is evidence of adaptation rather than pure genetic control.24 The pathologic phases that occur with local cold injury often overlap and vary with the extent and rapidity of the cold response (Box 139-1). Frostbite occurs when the tissue supercools well below 0° C. The required temperature is at least −4° C and may be as low as −10° C. There are two putative mechanisms of tissue injury: architectural cellular damage from ice crystal formation and microvascular thrombosis and stasis.25 In the prefreeze phase, tissue temperatures drop below 10° C and cutaneous sensation is lost. Before ice crystal formation, microvascular vasoconstriction occurs along with endothelial leakage of plasma into the interstitium. Radiation and conduction of heat from deeper tissues prevent crystallization until the skin temperature drops well below 0° C.26 In the freeze-thaw phase, the timing, location, and rate of ice crystal formation depend on the exposure circumstances. In addition to ambient temperatures, wind and moisture increase the freezing rate. An additional insult, progressive dermal ischemia, is partially mediated by thromboxane.27 Fluid analysis of clear vesicles identifies prostaglandins. When subdermal vascular plexuses are injured, hemorrhagic blisters develop that also contain these prostanoids. The arachidonic acid breakdown products released from underlying damaged tissue into the blister fluid include both prostaglandins and thromboxane. These mediators produce platelet aggregation, vasoconstriction, and leukocyte immobilization.28 Edema progresses for 48 to 72 hours after tissue is thawed. Leukocyte infiltration, thrombosis, and early necrosis become apparent as this edema resolves. The dry gangrene carapace of frostbite is superficial in comparison to arteriosclerosis-induced, full-thickness gangrene. Although the historical surgical aphorism was “frostbite in January, amputate in July,” advances in imaging modalities can accelerate the identification of the demarcation between viable and nonviable tissue.21 The extent of peripheral cold injury is determined by the type and duration of cold contact with the skin (Box 139-2).29 Predisposing risks include physiologic, mechanical, psychological, environmental, and cardiovascular factors. Although air alone is a poor thermal conductor, associated cold and wind (wind chill index) markedly increase heat loss. Direct skin contact with good thermal conductors such as metal, water, and volatile liquids affects the extent and rapidity of tissue destruction. Commercial aerosol spray propellants, such as propane and butane, and carbon dioxide in fire extinguishers are potentially hazardous.30 Liquid oxygen and Freon can also cause frostbite.31,32 Overenthusiastic application of standard ice packs in the treatment of soft tissue injuries can also result in tissue loss.33 Cryotherapy is commonly prescribed in sports medicine. In addition to improper use of cold packs, vapor coolant sprays such as chloroethane can cause frostbite.34,35 Classically, the initial presentation of frostbite is deceptively benign. Most patients do not arrive in the emergency department with frozen, insensate tissue. Frozen tissues often appear mottled or violaceous-white, waxy, or pale yellow. In severe cases, the examiner will not be able to roll the dermis over bone prominences. Rapid rewarming results in an initial hyperemia, even in severe cases. After thawing, partial return of sensation should be expected until blebs form.21 Classification by degrees is often incorrect in relation to the actual severity of the frostbite and thus therapeutically misleading. Mills suggests two simple retrospective classifications.20,21 Superficial or mild frostbite does not entail eventual tissue loss, whereas deep or severe frostbite does result in tissue loss. As a result, it is not feasible to predict, on presentation, the eventual tissue loss. Another classification attempts to establish severity on the basis of clinical features coupled with early bone scan results.17,36 Significant pain usually accompanies reestablishment of perfusion. With partial tissue destruction, intermittent pain may be noticed during ongoing exposure. The dull continuous ache evolves into a throbbing sensation in 48 to 72 hours. This often persists until tissue demarcation several weeks to months later. Nonfreezing cold injury occurs when tissue fluids have not frozen. Chilblain (pernio) is a mild form of cold injury that often follows repetitive exposure. These “cold sores” appear less than 24 hours after exposure and usually affect facial areas, the dorsa of the hands and feet, and the pretibial areas. Young women with a history of Raynaud’s phenomenon or systemic lupus erythematosus or with antiphospholipid antibodies are especially at risk. Persistent vasospasm and vasculitis result in burning, pruritus, erythema, and mild edema. Plaques, blue nodules, and ulcerations can develop and last 1 to 2 weeks. The other common nonfreezing cold injury is trench foot (immersion foot). This remains a significant threat during recreational activities and military expeditions in cold, wet climates. Trench foot is produced by prolonged exposure to wet cold at temperatures above freezing.6 It usually develops slowly during several days and results in neurovascular damage in the absence of ice crystal formation. Immersion foot commonly develops while a person is wearing sweat-dampened or neoprene socks, vapor-barrier boots, or constrictive gaiters. Patients who soak their feet for hours each night in cool water for pain relief are also at risk. The clinical presentation varies. Most patients’ symptoms include cool, pale feet that are numb or tingle. Later the feet appear cyanotic, cold, and edematous. Often, numbness and leg cramping are present. The clinical hallmark is that after rewarming, the skin remains erythematous, dry, and very painful to touch. Rubor on dependency and pallor on elevation are caused by vasomotor paralysis. Infrared thermography in response to a cold stress may support the diagnosis and assess its severity.17
Frostbite
Perspective
Principles of Disease
Pathophysiology
Predisposing Factors
Clinical Features
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Frostbite
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