Environmental medicine

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Chapter 18 Environmental medicine

Disease and the environment

The incidence and prevalence of disease and causes of death within a community are a reflection of interrelated factors:

Some of these environmental effects have been clearly documented within the last decade, e.g. the massive civilian mortality and morbidity during the current Afghan and previous Iraq wars, and loss of life and disease prevalence following the 2006 tsunami, the earthquakes in Sechuan (2008) and Haiti (2010) and cyclone Nargris in the Irawaddy delta. Flooding caused by El Niño in East Africa not only resulted in an increase in breeding sites for mosquito vectors but a major outbreak of Rift Valley fever due to the enforced close proximity of cattle with humans.

Smoking (active and passive), obesity and excess alcohol consumption also play a significant role in disease. Worldwide health programmes have been established in most countries to reduce their effects.

Heat

Body core temperature (TCore) is maintained at 37°C by the thermoregulator centre in the hypothalamus.

Heat is produced by cellular metabolism and is dissipated through the skin by both vasodilatation and sweating and in expired air via the alveoli. When the environmental temperature (TEnv) is >32.5°C, profuse sweating occurs. Sweat evaporation is the principal mechanism for controlling TCore following exercise or in response to an increase in TEnv.

Heat acclimatization. Acclimatization to heat takes place over several weeks. The sweat volume increases and the sweat salt content falls. Increased evaporation of sweat reduces TCore.

Heat cramps. Painful muscle cramps, usually in the legs, often occur in fit people when they exercise excessively, especially in hot weather. Cramps are probably due to low extracellular sodium caused by excess intake of water over salt. Cramps can be prevented by increasing dietary salt. They respond to combined salt and water replacement, and in the acute stage to stretching and muscle massage. TCore remains normal.

Heat illness. At any environmental temperature (especially with TEnv of >25°C), and with a high humidity, strenuous exercise in clothing that inhibits sweating such as a wetsuit can cause an elevation in TCore in <15 minutes. Weakness/exhaustion, cramps, dizziness and syncope, with TCore >37°C, define heat illness (heat exhaustion). Elevation of TCore is more critical than water and sodium loss. Heat illness may progress to heat injury, a serious emergency.

Heat injury

Heat injury (heat stroke) is an acute life-threatening situation when TCore rises above 41°C. There is headache, nausea, vomiting and weakness, progressing to confusion, coma and death. The skin feels intensely hot to the touch. Sweating is often absent, but not invariably.

Heat injury can develop in unacclimatized people in hot, humid windless conditions, even without exercise. Sweating may be limited by prickly heat (plugging or rupture of the sweat ducts, leading to a pruritic papular erythematous rash). Excessive exercise in inappropriate clothing, e.g. exercising on land in a wetsuit, can lead to heat injury in temperate climates. Diabetes, alcohol and drugs, e.g., antimuscarinics, diuretics and phenothiazines, can contribute. Heat injury can lead to a fall in cardiac output, lactic acidosis and intravascular coagulation.

Cold

Hypothermia is defined as a core temperature of <32°C. It is frequently lethal when TCore falls below 30°C. Survival, with full recovery has however been recorded with TCore of <16°C. Cold injury includes:

Hypothermia

Hypothermia occurs in many settings.

At home. Hypothermia can occur when TEnv is below 8°C, when there is poor heating, inadequate clothing and poor nutrition. Depressant drugs, e.g. hypnotics, as well as alcohol, hypothyroidism or intercurrent illness also contribute. Hypothermia is commonly seen in the poor, frail and elderly. The elderly have diminished ability to sense cold and also have little insulating fat. Neonates and infants become hypothermic rapidly because of a relatively large surface area in proportion to subcutaneous fat.

Outdoors on land. Hypothermia is a prominent cause of death in climbers, skiers, polar travellers and in wartime. Wet, cold conditions with wind chill, physical exhaustion, injuries and inadequate clothing are contributory. Babies and children are at risk because they cannot take action to warm them themselves.

Cold water immersion. Dangerous hypothermia can develop following immersion for more than 30 min to 1 hour in water temperatures of 15–20°C. In TWater below 12°C limbs rapidly become numb and weak. Recovery takes place gradually, over several hours following rescue.

Sequelae

Pulse rate and systemic BP fall. Cardiac output and cerebral blood flow are low in hypothermia and can fall further if the upright position is maintained, the thorax restrained by a harness or by hauling during evacuation. This is why helicopter and lifeboat winch rescues are often carried out with a stretcher, rather than a chest harness.

Respiration becomes shallow and slow. Muscle stiffness develops; tendon reflexes become sluggish, then absent. As coma ensues, pupillary and other brainstem reflexes are lost; pupils are fixed and may be dilated in severe hypothermia. Metabolic changes are variable, with either metabolic acidosis or alkalosis. Arterial PO2 may appear normal, i.e. falsely high.

There is shift of the oxygen dissociation curve to the left because of the reduction in temperature of haemoglobin. Thus, if an arterial blood sample from a hypothermic patient is analysed at 37°C, the PO2 will be falsely high. Within the range 37–33°C this factor is around 7% per °C. Many blood gas machines also calculate the arterial saturation; this too will be falsely high. When a patient is monitored using a pulse oximeter, the level of arterial oxygen saturation (SaO2) will however be correct – but if SaO2 is then converted by calculation to PaO2, a downwards correction must be applied – simply due to hypothermia.

Bradycardia with ‘J’ waves (rounded waves above the isoelectric line at the junction of the QRS complex and ST segment) are pathognomonic of hypothermia. Prolongation of PR and QT intervals and QRS complex also occur. Ventricular dysrhythmias (tachycardia/fibrillation) or asystole are the usual causes of death.

Cold injury

Management

Transport the patient – or if this is impossible, make them walk, even on frostbitten feet – to a place of safety before commencing warming. Warm the frozen part by immersion in hand hot water at 39–42°C, if feasible. Assess hypothermia. Continue warming until obvious thawing occurs; this can be painful. Vasodilator drugs have no part in management. Blisters form within several days and, depending on the depth of frostbite, a blackened shell – the carapace – develops as blisters regress or burst. Dry, non-adherent dressings and aseptic precautions are essential, though hard to achieve. Frostbitten tissues are anaesthetic and at risk from further trauma and infection. Recovery takes place over many weeks, and may be incomplete. Surgery may be needed, but should be avoided in the early stages.

High altitudes

The partial pressure of atmospheric oxygen – and hence alveolar and arterial oxygen – falls in a near-linear relationship as barometric pressure falls with increasing altitude (Fig. 18.1).

Commercial aircraft are pressurized to 2750 m (lowering the oxygen saturation by 3–4%). The incidence of deep venous thrombosis and pulmonary embolism is slightly greater in sedentary passengers on long-haul flights than in a similar population at sea level. Dehydration and alcohol probably contribute. Prophylactic aspirin is not recommended.

On land, below 3000 m there are few clinical effects. The resulting hypoxaemia causes breathlessness only in those with severe cardiorespiratory disease. Above 3000–3500 m hypoxia causes a spectrum of related syndromes that affect high-altitude visitors, principally climbers, trekkers, skiers and troops (Table 18.1), especially when they exercise. These conditions occur largely during acclimatization, a process that takes several weeks and once completed can enable man to live – permanently if necessary – up to about 5600 m. At greater heights, although people can survive for days or weeks, deterioration due to chronic hypoxia is inevitable.

Table 18.1 Conditions caused by sustained hypoxia

Condition Incidence (%) Usual altitude (m)

Acute mountain sickness

70

3500–4000

Acute pulmonary oedema

2

4000

Acute cerebral oedema

1

4500

Retinal haemorrhage

50

5000

Deterioration

100

6000 and above

Chronic mountain sickness

Rare

3500–4000

The world’s highest railway is to Lhasa, reaching altitudes over 5000 m. Emergency oxygen is provided in the carriages. Roads at similar altitudes in central Asia are used extensively but since road passengers do not exercise, serious altitude-related illnesses are unusual. Climbing the world’s highest summits is just possible without supplementary oxygen, though it is often used on peaks above 7500 m. At the summit of Everest (8848 m) the barometric pressure is 34 kPa (253 mmHg). An acclimatized mountaineer has an alveolar PO2 of 4.0–4.7 kPa (30–35 mmHg) – near man’s absolute physiological limit.

Acute mountain sickness (AMS)

AMS describes malaise, nausea, headache and lassitude and affects the majority of people for a few days, above 3500 metres. Following arrival at this altitude there is usually a latent interval of 6–36 hours before symptoms begin. Treatment is rest, with analgesics if necessary. Recovery is usually spontaneous over several days.

Prophylactic treatment with acetazolamide, a carbonic anhydrase inhibitor and a respiratory stimulant, is of some value in preventing AMS. Acclimatizing, i.e. ascending gradually, provides better and more natural prophylaxis.

In the minority, more serious sequelae – high-altitude pulmonary oedema and high-altitude cerebral oedema develop.

Diving

Free diving by breath-holding is possible to around 5 metres, or with practice to greater depths. Air can be supplied to divers by various methods. With a snorkel, providing air to a depth of c. 0.5 metres, inspiratory effort is the limiting factor. At depths >0.5 metres, i.e. with a longer snorkel tube, forced negative-pressure ventilation can cause pulmonary capillary damage with haemorrhagic alveolar oedema. Scuba divers, i.e. recreational sports divers descending to 30 metres, carry bottled compressed air, or a nitrogen–oxygen mixture. Divers who work at great depths commercially breathe helium–oxygen or nitrogen–oxygen mixtures, delivered by hose from the surface. Ambient pressures at various depths are shown in Table 18.2.

Table 18.2 Depth and pressure

Water depth (m) Pressure
Atmospheres mmHg

0

1

760

10

2

1520

50

6

4560

90

10

7600

Problems during and following ascent

Free divers who breath-hold often hyperventilate deliberately prior to plunging in. This drives off CO2 – reducing the stimulus to inspire. During the subsequent breath-hold PaCO2 rises; PaO2 falls. On surfacing, decompression lowers PaO2 further. This can lead to syncope, known as a shallow water blackout. Since loss of consciousness can take place in the water, this can lead to fatalities.

Decompression sickness

Decompression sickness (the bends) are caused by release of bubbles of nitrogen or helium and follow returning too rapidly to the surface. Decompression tables indicate the duration for safe return from a given depth to the surface.

The bends can be mild (type 1, non-neurological bends), with skin irritation and mottling and/or joint pain. Type 2, neurological bends, are more serious – cortical blindness, hemiparesis, sensory disturbances or cord lesions develop.

If bubbles form in pulmonary vessels, divers experience retrosternal discomfort, breathlessness and cough, known as the chokes. These develop within minutes or hours of a dive. Decompression problems do not only occur immediately on reaching the surface, they may take some hours to become apparent. Over the subsequent 24 h, further ascent, e.g. air travel, can occasionally provoke the bends.

Other problems during ascent include paranasal sinus pain and nosebleeds – medically minor but dramatic, with excruciating pain and a mask full of bloody fluid. Toothache can be caused by gas bubbles within rotten fillings.

Management. All but the mildest forms of decompression sickness, e.g. skin mottling alone, require recompression in a pressure chamber, following strict guidelines. Recovery is usual. A long-term problem is aseptic necrosis of the hip due to nitrogen bubbles causing infarction. Focal neurological damage may persist, but complaints of fatigue and poor concentration are issues compounded by litigation that commonly follows diving accidents. Objective, evidence-based assessments are essential.

Drowning and near-drowning

Drowning is a common cause of accidental death worldwide. In the UK, some 40% of drownings occur in children under 5 years of age. Drowning can also follow a seizure or a myocardial infarct. Exhaustion, alcohol, drugs and hypothermia all contribute to deaths following immersion.

Ionizing radiation

Ionizing radiation is either penetrating (X-rays, γ-rays or neutrons) or non-penetrating (α- or β-particles). Penetrating radiation affects the skin and deeper tissues, while non-penetrating radiation affects the skin alone. All radiation effects depend on the type of radiation, the distribution of dose and the dose rate.

Dosage is measured in joules per kilogram (J/kg); 1 J/kg = 1 gray (1 Gy) = 100 rads.

Radioactivity is measured in becquerels (Bq). 1 Bq is defined as the activity of a quantity of radioactive material in which one nucleus decays per second; 3.7 × 1010 Bq = one curie (Ci), the older, non-SI unit.

Radiation differs in the density of ionization it causes. Therefore a dose-equivalent called a sievert (Sv) is used. This is the absorbed dose weighted for the damaging effect of the radiation. The annual background radiation is approximately 2.5 mSv. A chest X-ray delivers 0.02 mSv, and CT of the abdomen/pelvis about 10 mSv (see Table 9.5). A cumulative risk of cancer following repeated imaging procedures has been established and reduction of X-ray exposures should be made if possible.

Excessive exposure to ionizing radiation follows accidents in industry, nuclear power plants and hospitals and deliberate nuclear explosions designed to eliminate populations – and exceptionally, by poisoning, e.g. with polonium.

Acute radiation sickness

Many systems are affected; the extent depends on the dose of radiation (Table 18.3).

Table 18.3 Systemic radiation effects

Acute effects Delayed effects

Haemopoietic syndrome

Infertility

Gastrointestinal syndrome

Teratogenesis

CNS syndrome

Cataract

Radiation dermatitis

Neoplasia:

 

 Acute myeloid leukaemia

 

 Thyroid

 

 Salivary glands

 

 Skin

 

 Others

Bioterrorism/biowarfare

Interest in biological warfare and bioterrorism intensified during the 1991 Iraq war and later following the destruction of the Twin Towers in New York in 2001. The potential of bacteria as weapons is illustrated by a suggestion that several kilograms of anthrax spores might kill as many people as a Hiroshima-sized nuclear weapon.

Potential pathogens

The US Centers for Disease Control and Prevention in Atlanta, Georgia, have developed a classification of potential biological agents (Table 18.4).

Table 18.4 Critical biological agents

Category Pathogens

A.Very infectious and/or readily disseminated organisms: high mortality with a major impact on public health

Smallpox, anthrax, botulinism, plague

B.Moderately easy to disseminate organisms causing moderate morbidity and mortality

Q fever, brucellosis, glanders, food-/water-borne pathogens, influenza

C.Emerging and possible genetically engineered pathogens

Viral haemorrhagic fevers, encephalitis viruses, drug-resistant TB

Adapted from Khan AS, Morse S, Lillibridge S. Public health preparedness for biological terrorism in the USA. Lancet 2000; 356:1179–1182, reprinted with permission from Elsevier.

Smallpox

Smallpox is a highly infectious disease with a mortality >30%. There is no proven therapy, but there is an effective vaccine. Universal vaccination was stopped in the early 1970s: the vast majority of the world’s population is now unprotected against the variola virus (see p. 101). The potential exists for a worldwide epidemic of smallpox, possibly initiated by a bioterrorist act.

Smallpox has an incubation period of around 12 days, allowing any initial source of infection to go undetected until the rash (Fig. 18.2), similar to chickenpox, develops on the 2nd or 3rd day of the illness. Infection is transmitted by the airborne route; the patient becomes infectious to others 12–24 hours before the rash appears, thus allowing a potential infected volunteer to pass infection to others before being recognized as suffering from smallpox. If vaccines were to be administered widely to those potentially infected within 3 days of contact, an epidemic might well be prevented. Smallpox virus is stored in two secure laboratories – in Russia and in the USA. Supplies of vaccine are potentially available worldwide.

Plague

Plague (see p. 136) could be transmitted as a bioweapon either by air-borne dissemination or by infected rats. Immunization is of limited value.

Other potential infective agents are listed in Table 18.4.

Travel

Building-related illnesses

Specific building-related illnesses

Legionnaires’ disease (see p. 836) can follow contamination of air-conditioning systems.

Humidifier fever (see p. 854) is also due to contaminated systems, probably by fungi, bacteria and protozoa. Many common viruses are potentially transmissible in an enclosed environment, e.g. the common cold, influenza and rarely pulmonary TB. Allergic disorders, e.g. rhinitis, asthma and dermatitis, also occur following exposure to indoor allergens such as dust mites and plants. Office equipment, e.g. fumes from photocopiers, has also been implicated. Passive smoking (see p. 807) is no longer an issue in Europe and North America, following legislation against smoking.