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Mercury: Uses, Production, and Environmental Impact


Background

Mercury (Hg) is a dense, silvery liquid metal that has been used since antiquity for its unique properties. Historically valued for alloying with gold and silver, its role expanded during the 19th‑century California Gold Rush, when mercury ore deposits were extensively mined. Today, mercury’s applications are largely confined to chlorine and caustic soda production, as well as select electrical devices such as fluorescent lamps and mercury‑vapor lamps.

Archaeological evidence shows mercury was present in Egyptian tombs around 1500 B.C., likely for cosmetic or medicinal use. The Greek philosopher Aristotle described cinnabar processing in 350 B.C., and the Romans coined the term “hydrargyrum” (liquid silver), the origin of the chemical symbol Hg.

In the 16th century, mercury was employed to extract silver from ore, and in 1643 Torricelli introduced the mercury barometer. Subsequent inventions included the mercury thermometer (Fahrenheit, 1714) and, in 1828, the first dental amalgam fillings—though concerns over toxicity limited adoption until 1895 when G. V. Black demonstrated safety.

Throughout the 20th century, mercury appeared in batteries, paints, explosives, light bulbs, pharmaceuticals, fungicides, pesticides, and various manufacturing processes (paper, felt, glass, plastics). By the 1980s, growing awareness of mercury’s health and environmental hazards prompted a steep decline in use. In the United States, battery use fell to <5 % of 1988 levels by 1992, and electrical device usage dropped by 50 % during the same period. Paints, fungicides, and pesticides have been banned nationwide, while mercury use in paper, felt, and glass production has been voluntarily discontinued.

Global production is now limited to a handful of countries with less stringent environmental regulations. Spain ceased mining in 1989; the U.S. has also stopped primary mining, though small amounts are recovered during gold refining to mitigate contamination. In 1992, China, Russia (formerly USSR), Mexico, and Algeria were the leading producers.

Raw Materials

Mercury is rarely found in its elemental form; it is almost always extracted from ores. The most common ore is cinnabar (HgS), but other minerals include corderoite (Hg₃S₂Cl₂), livingstonite (HgSb₄S₈), montroydite (HgO), and calomel (HgCl). These ores form underground when mineral‑laden solutions ascend toward the surface, often in faulted and fractured rock at depths between 1 m and 1000 m.

Historical mining sites and tailings from older, less efficient operations also contribute secondary sources of mercury.

The Manufacturing Process

Extraction has remained essentially unchanged since Aristotle’s time. Cinnabar ore is crushed, heated, and the released mercury vapor is cooled and condensed. Nearly 95 % of the mercury can be recovered using this method.

Mining

Cinnabar deposits are typically near the surface; about 90 % require underground mining via tunnels, while 10 % can be extracted by open‑pit methods.

Roasting

Due to high concentration, cinnabar can be processed directly. The ore undergoes crushing and grinding to a fine powder, then heated in a furnace or rotary kiln. Combustion of natural gas or other fuels supplies heat, and the ore reacts with atmospheric oxygen to release sulfur dioxide, while mercury vapor rises.

Condensing

Refining

Commercial‑grade mercury is typically 99.9 % pure and ready for use. For applications requiring higher purity, further refining—mechanical filtration, chemical oxidation, or electrolytic purification—is employed. The most common method is triple distillation, which progressively removes residual impurities and yields ultrapure mercury.

Shipping

Quality Control

Prime virgin‑grade mercury (99.9 % purity) is verified through spot checks for foreign metals such as gold, silver, and base metals. Ultrapure mercury undergoes triple‑distillation, followed by evaporation or spectrographic analysis to confirm absence of contaminants.

Health and Environmental Effects

Mercury is a potent toxin. Exposure routes include inhalation, ingestion, and dermal absorption, with inhalation of vapor being the most hazardous. Short‑term vapor exposure can cause weakness, chills, nausea, vomiting, and diarrhea; long‑term exposure leads to tremors, irritability, insomnia, confusion, and excessive salivation.

In typical diets, mercury primarily enters the body through fish consumption, where bioaccumulation occurs. Although gastrointestinal absorption is limited, chronic ingestion can result in cumulative effects.

Industrial exposure—especially in mining, ore processing, chlorine and caustic soda production, and dental amalgam placement—poses significant risks to workers.

In 1988, global human activities released approximately 24 million lb (11 million kg) of mercury into air, land, and water. The U.S. Environmental Protection Agency (EPA) has prohibited many mercury applications and set goals to reduce municipal refuse mercury from 1.4 million lb (0.64 million kg) in 1989 to 0.35 million lb (0.16 million kg) by 2000 through product reduction and recycling.

The Future

While mercury remains integral to certain products and processes, its use is expected to decline further. Advances in handling, recycling, and regulatory enforcement aim to minimize environmental releases and associated health risks.


Manufacturing process

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