Zinc is a chemical element with the symbol Zn. It is a low-melting metal that
belongs to Group IIb (zinc group) of the periodic table. The atomic number of
zinc is 30. With an atomic weight of 65.39, zinc makes up an average of 65 grams
of every ton of Earth's crust, which makes it a little more abundant than
copper. The melting point of zinc is 420 degrees Celsius and its boiling point
is 907 degrees Celsius (Britannica Online). Zinc is the second most common trace
metal, after iron, that is found naturally in the human body. It is also the
third most used nonferrous metal (after aluminum and copper), of which the U.S.
consumes more than one million metric tons annually (American Zinc Association).

According to the U.S. Bureau of Mines, the average person will use 730 pounds of
zinc in his or her lifetime. Metallic zinc appeared much later in history than
the other common metals. "The Ancient Egyptians were the first to use zinc
although they did so unintentionally! They made their brass from copper ores
that were contaminated with zinc" (Knapp, 4). There is some evidence that
the Greeks knew of zinc's existence. They called it pseudargyras, or "false
silver," but they had no method of producing it in quantity. The Romans
produced considerable quantities of brass, an alloy of zinc and copper, as early
as 200 B.C. The metallurgists of India seem to have isolated the individual
metal as early as the 13th century; and by the 16th century, China had achieved
large-scale production. In the West, commercial zinc production got under way by
the middle of the 18th century in England under the leadership of William

Champion (Britannica Online). The first complete study of zinc was published in

1746 by Sigismund Marggraf, a German chemist (World Book). Canada is the leading
producer of zinc followed by Australia, China, Peru, the U.S. and Mexico. In the

U.S., mine production comes mostly from Alaska, Tennessee, New York, and

Missouri (World Almanac, 151). There are 47 tons of zinc in one cubic mile of
seawater. Zinc deposits occur in two quite different ways: first, as
hydrothermal or contact metamorphic deposits, and second, as sedimentary
deposits. Zinc was used as a component of brass until the 18th century. More
than 50% of production is consumed in the preparation of alloys for die-cast
products, and in anticorrosion treatment of iron and steel (Skinner, 19). A
large share of the zinc produced today is used for galvanizing iron and steel
(that is, coating them with zinc to make them rustproof). For many purposes,
zinc is simply flattened into sheets called "rolled zinc." These
sheets are used in the manufacture of many roofing products, refrigerator
linings, and printing plates. The compounds of zinc have numerous uses. Because
of its high heat conductivity, zinc oxide is used in rubber as a heat
dissipater. It is also used in the making of cosmetics, plastics, skin
ointments, and soaps. Zinc sulfate is used in weed killers. Zinc sulfide has
been used in X-ray screens and in luminous dials for clocks and watches
(Compton's Encyclopedia). Zinc is also used in electric batteries and is
required for the normal growth and healing of plants and animals. Zinc can also
be combined with other metals to form many other alloys (mixtures). For example,
brass is an alloy of copper and zinc. Bronze is copper, tin, and zinc. And
nickel silver is copper, nickel, and zinc (World Book). The following statistics
are stated in the U.S. Geological survey, U.S. Dept. of the Interior. As of
mid-1996, the world mineral reserve for zinc was 330 million metric tons. U.S.

Zinc Production, 1950-95 (in thousand metric tons) 1950 565,516 1989 275,883

1960 395,013 1990 515,355 1965 554,429 1991 517,804 1970 484,560 1992 523,440

1975 425,792 1993 488,283 1980 317,103 1994 570,162 1985 226,545 1995 601,000 In

1950 the total production of zinc was 565,515 thousand metric meters. The
estimated total reserves for 1950 was 85,000,000 metric tons, but that was
before the enormous amount of native zinc was discovered in Australia (Skinner,

62). In the year 2000, the projected total of zinc production is 550,000
thousand metric meters and the total world reserve will be at an estimated

320,500,000 metric tons. In the year 2050, I expect the total production of zinc
to be around significantly greater than it was 100 years from then. From
examining the chart above, I have come to the conclusion that the world reserve
will not be that greatly affected (considering the increasing amount of
technology that is available to us and the large amount of the total reserves
today). The mineral zinc has not been over mined since its existence, and I do
not expect it to be completely exhausted by the year 2050. I think that in the
year 2050 the world is going to be completely different as we know it. I expect
the downfall of computers to be solved by then and a huge increase in the
industrial development. Hence, creating a greater demand for all resources
including zinc.


Knapp, Brian; Zinc,Cadium,and Mercury. New York: Atlantic Europe Publishing

Company Limited, 1996. Rosenbaum, Garvin; World Without Plenty. Skokle, Ill:

National Textbook Co.,1975. Skinner, Brian; Earth Resources. New Jersey:

Prentice Hall Inc., 1969. Matthews, Robert; Beyond 2000. Providence, RH: Global

Dynamics Press, 1989. The World Almanac. United States: K-III Reference

Corporation, 1996. "Zinc" Compton's Encyclopedia Online.
*"http://www.optonline.com/comptons/ceo* "Zinc group elements"

Encyclopedia Britannica Online. *http://www.members.eb.com/bol/* "American

Zinc Association" *http://www.org/zincfacts.html "World Book"
http:// medusa.fs.altip.oclc.org/