Peak copper is a hypothetical point in time at which the maximum global copper production rate is reached. Since copper is a finite resource, at some point in the future new production from within the earth will diminish, and at some earlier time production will reach a maximum. When this will occur is a matter of dispute. Unlike fossil fuels, however, copper is scrapped and reused and it has been estimated that at least 80% of all copper ever mined is still available (having been repeatedly recycled). Copper is among the most important industrial metals, valued for its heat and electrical conductivities and malleability. Copper is used in electrical power cables, data cables, electrical equipment, automobile radiators, cooling and refrigeration tubing, heat exchangers, artillery shell casings, small arms ammunition, water pipes, and jewellery.
Copper has been in use at least 10,000 years, but more than 95% of all copper ever mined and smelted has been extracted since 1900. As of 2006, the Indian and Chinese economies were racing to catch up with the West, straining the copper supply, leading to increased prices and an increase in copper theft.
- 1 History
- 2 Copper demand
- 3 Copper supply
- 4 Polities
- 5 Copper prices
- 6 Criticism
- 7 See also
- 8 References
- 9 External links
Concern about the copper supply is not new. In 1924, noted geologist and copper-mining expert Ira Joralemon warned:
- "... the age of electricity and of copper will be short. At the intense rate of production that must come, the copper supply of the world will last hardly a score of years. ... Our civilization based on electrical power will dwindle and die."
Total world production is about 18 million metric tons per year. Copper demand is increasing by more than 575,000 tons annually and accelerating. Based on 2006 figures for per capita consumption, Tom Graedel and colleagues at Yale University calculate that by 2100 global demand for copper will outstrip the amount extractable from the ground. China accounted for more than 22% of world copper demand in 2008, and is nearly 40% in 2014.
For some purposes, other metals can substitute. During a copper shortage in the 1970s, aluminium wire was substituted in many applications, but improper design caused a fire danger. The safety issues have since been solved by use of larger sizes of aluminium wire (#8AWG and up), and properly designed aluminium wiring is still being installed in place of copper. For example, the Airbus A380 uses aluminum wire in place of copper wire for electrical power transmission.
Globally, economic copper resources are being depleted with the equivalent production of three world-class copper mines being consumed annually. Environmental analyst Lester Brown suggested in 2008 that copper might run out within 25 years based on what he considered a reasonable extrapolation of 2% growth per year.
New copper discoveries
56 new copper discoveries have been made during the three decades 1975–2005. World discoveries of new copper deposits are said to have peaked in 1996. However, according to the US Geological Survey, remaining world copper reserves have more than doubled since then, from 310 million metric tons in 1996 to 690 million metric tons in 2013.
Per the table below, the three chief national producers of copper, respectively, in 2002, were Chile, Indonesia, and the United States. In 2013, they were Chile, China, and Peru. 21 of the 28 largest copper mines in the world are not amenable to expansion. Many large copper mines will be exhausted between 2010 and 2015.
Copper is a fairly common element, with an estimated concentration of 50–70 ppm (0.005–0.007%) in Earth's crust (1 kg of copper per 15–20 tons of crustal rock). If all this copper were extractable, that would provide humans with a nearly inexhaustible supply of the element (millions of years worth), from that concentration adding up to around 2 quadrillion tons over the mass of the crust. However, most of it can not be extracted profitably at the current level of technology and the current market value. At the present time, copper deposits are considered potentially profitable if they are located sufficiently close to the surface and they contain at least 0.3–0.5% of copper.
The U.S. Geological Survey reported a current total reserve base of copper in potentially recoverable ores of 1.6 billion tonnes as of 2005, of which 950 million tonnes was considered economically recoverable. A 2013 global assessment identified "455 known deposits (with well-defined identified resources) that contain about 1.8 billion metric tons of copper", and predicted "a mean of 812 undiscovered deposits within the uppermost kilometer of the earth’s surface" containing another 3.1 billion metric tons of copper "which represents about 180 times 2012 global copper production from all types of copper deposits."
|Country||1996 Reserves||Percent||2014 Reserves||Percent|
Known conventional resources
Each year in the USA, more copper is recovered and put back into service from recycled material than is derived from newly mined ore. Copper’s recycle value is so great that premium-grade scrap normally has at least 95% of the value of primary metal from newly mined ore.
As of 2011, recycled copper provided 35 percent of total worldwide copper usage.
Undiscovered conventional resources
Based on discovery rates and existing geologic surveys, researchers estimated in 2006 that 1.6 billion metric tons of copper could potentially be brought into use. This figure relied on the broadest possible definition of available copper as well as a lack of energy constraints and environmental concerns.
The US Geological Survey estimated that, as of 2013, there remained 3.5 billion metric tons of undiscovered copper resources worldwide in porphyry and sediment-hosted type deposits, two types which currently provide 80% of mined copper production. This was in addition to 2.1 billion metric tons of identified resources. Combined identified and estimated undiscovered copper resources were 5.6 billion metric tons, 280 times the annual global consumption of newly refined copper of 20 million metric tons.
Deep-sea nodules are estimated to contain 700 million tonnes of copper.
Chile is the world's largest copper producer, and in 2007 accounted for 37% of the world's primary copper production (see table above). One researcher has stated that Chile copper production may begin to decline irreversibly in 2008. However, this is contradicted by the Chilean Copper Commission, which has projected that, based on planned expansion projects, Chilean copper production will continue to increase through at least 2012.
The price of copper struck a first peak level on 6 March 2008, on the London Metal Exchange (LME), surging 5.8 percent over the previous trading day to US$4.02 per pound. The previous record was set on 12 May 2006, at $3.98/lb. The international copper price increased rapidly in early 2008, rising 23 percent in February 2008, then declined 40% before December 2008, and reached $1.30 by year's end. In February 2011 the price peaked at over US$10,100/tonne ($4.58/lb) but soon fell to below $8,000, around where it was fairly stable during 2012, with a decline to around $7000 ($3.18/lb) during 2013.
Julian Simon was a senior fellow at the Cato Institute and a professor of business and economics. In his book The Ultimate Resource 2 (first printed in 1981 and reprinted in 1998), he extensively criticizes the notion of "peak resources", and uses copper as one example. He argues that, even though "peak copper" has been a persistent scare since the early 20th century, "known reserves" grew at a rate that outpaced demand, and the price of copper was not rising but falling in the long run. For example, even though world production of copper in 1950 was only 1/8 of what it was in early 2000s, known reserves were also much lower at the time – around 100 million metric tons – making it appear that the world would run out of copper in 40 to 50 years at most.
Simon's own explanation for this development is that the very notion of known reserves is deeply flawed, as it does not take into account changes in mining profitability. As richer mines are exhausted, developers turn their attention to poorer sources of the element and eventually develop cheap methods of extracting it, raising "known reserves". Thus, for example, copper was so abundant 5000 years ago, occurring in pure form as well as in highly concentrated copper ores, that prehistoric peoples were able to collect and process it with very basic technology. As of the early 21st century, copper is commonly mined from ores that contain 0.3% to 0.6% of copper by weight. Yet, despite the material being far less "widespread", the cost of, for example, a copper pot was vastly lower in the late 20th century than 5000 years ago.
Simon essentially states that not all viable copper has been discovered and that not all technological advancements in mining and refining have occurred, so statements that the point of peak copper has been or will be reached must be false. Simon supports his argument by showing that copper supplies have increased and prices have fallen. Simon's thesis of peak resources is not based on current scientific analysis or geological measurements, but the analysis of historical trends and the assumption that they can and will continue.
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