Silicosis

Silicosis is an occupational lung disease caused by the inhalation of respirable crystalline silica dust. It is characterized by lung inflammation and fibrosis that most commonly affects the upper lobes and is classified as a form of pneumoconiosis. The disease occurs in chronic (simple and progressive massive fibrosis), accelerated, or acute forms, depending on the intensity and duration of exposure. Common symptoms include shortness of breath, cough, fatigue, and cyanosis in severe cases. Because its clinical and radiographic features can resemble those of tuberculosis, pneumonia, or pulmonary edema, silicosis is sometimes misdiagnosed. There is no curative treatment; management focuses on symptom control and the prevention of complications. Silicosis is largely preventable through effective workplace controls that limit airborne silica exposure, such as engineering controls, ventilation, and appropriate respiratory protection.

Signs and symptoms

Because chronic silicosis is slow to develop, signs and symptoms may not appear until years after exposure. Signs and symptoms include:

Dyspnea (shortness of breath) exacerbated by exertion Cough, often persistent and sometimes severe Fatigue Tachypnea (rapid breathing) which is often labored Loss of appetite and weight loss Chest pain Fever Gradual darkening of skin (blue skin) Gradual dark shallow rifts in nails eventually leading to cracks as protein fibers within nail beds are destroyed In advanced cases, the following may also occur:

Cyanosis, pallor along upper parts of body (blue skin) Cor pulmonale (right ventricle heart disease) Respiratory insufficiency Patients with silicosis are particularly susceptible to tuberculosis (TB) infection—known as silicotuberculosis. The reason for the increased risk—3 fold increased incidence—is not well understood. It is thought that silica damages pulmonary macrophages, inhibiting their ability to kill mycobacteria. Even workers with prolonged silica exposure, but without silicosis, are at a similarly increased risk for TB. Pulmonary complications of silicosis also include chronic bronchitis and airflow limitation (indistinguishable from that caused by smoking), non-tuberculous Mycobacterium infection, fungal lung infection, compensatory emphysema, and pneumothorax. There are some data revealing an association between silicosis and certain autoimmune diseases, including nephritis, scleroderma, and systemic lupus erythematosus, especially in acute or accelerated silicosis. In 1996, the International Agency for Research on Cancer (IARC) reviewed the medical data and classified crystalline silica as "carcinogenic to humans." The risk was best seen in cases with underlying silicosis, with relative risks for lung cancer of 2–4. Numerous subsequent studies have been published confirming this risk. In 2006, Pelucchi et al. concluded, "The silicosis-cancer association is now established, in agreement with other studies and meta-analysis."

Pathophysiology When small crystalline silica dust particles are inhaled, they can embed themselves deeply into the tiny alveolar sacs and ducts in the lungs, where oxygen and carbon dioxide gases are exchanged. There, the lungs cannot clear out the dust by mucus or coughing. When fine particles of crystalline silica dust are deposited in the lungs, macrophages that ingest the dust particles will set off an inflammatory response by releasing tumor necrosis factors, interleukin-1, leukotriene B4 and other cytokines. In turn, these stimulate fibroblasts to proliferate and produce collagen around the silica particle, thus resulting in fibrosis and the formation of the nodular lesions. The inflammatory effects of crystalline silica are apparently mediated by the NLRP3 inflammasome. Characteristic lung tissue pathology in nodular silicosis consists of fibrotic nodules with concentric "onion-skinned" arrangement of collagen fibers, central hyalinization, and a cellular peripheral zone, with lightly birefringent particles seen under polarized light. The silicotic nodule represents a specific tissue response to crystalline silica. In acute silicosis, microscopic pathology shows a periodic acid-Schiff positive alveolar exudate (alveolar lipoproteinosis) and a cellular infiltrate of the alveolar walls.

Silica

Silicon (Si) is the second most common element in the Earth's crust after oxygen. The compound silica, also known as silicon dioxide (SiO2), is formed from silicon and oxygen atoms. Since oxygen and silicon make up about 75% of the Earth's crust, the compound silica is quite common. It is found in many rocks, such as granite, sandstone, gneiss and slate, and in some metallic ores. Silica can be a main component of sand. It can also be in soil, mortar, plaster, and shingles. The cutting, breaking, crushing, drilling, grinding, or abrasive blasting of these materials may produce fine to ultra-fine airborne silica dust. Silica occurs in three forms: crystalline, microcrystalline (or cryptocrystalline) and amorphous (non-crystalline). "Free" silica is composed of pure silicon dioxide, not combined with other elements, whereas silicates (e.g., talc, asbestos, and mica) are SiO2 combined with an appreciable portion of cations.

Crystalline silica exists in seven different forms (polymorphs), depending upon the temperature of formation. The main three polymorphs are quartz, cristobalite, and tridymite. Quartz is the second most common mineral in the world (next to feldspar). Microcrystalline silica consists of minute quartz crystals bonded together with amorphous silica. Examples include flint and chert. Amorphous silica exists either as diatomaceous earth, from the skeletons of diatoms, or as vitreous silica, produced by heating and then rapid cooling of crystalline silica. Amorphous silica is less toxic than crystalline, but not biologically inert, and diatomite, when heated, can convert to tridymite or cristobalite. Silica flour is nearly pure SiO2 finely ground. Silica flour has been used as a polisher or buffer, as well as paint extender, abrasive, and filler for cosmetics. Silica flour has been associated with all types of silicosis, including acute silicosis. Silicosis is due to deposition of fine respirable dust (less than 10 micrometers in diameter) containing crystalline silicon dioxide in the form of alpha-quartz, cristobalite, or tridymite.

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