A good source to start the study of how much energy is required to produce NiMH batteries can be found here:
Inside the NiMH battery
Gives a basic overview of the elements needed to create such a battery. Each of those obviously requires energy during their production.
Drawing on that document, we need to find out the following:
-energy cost of producing potassium hydroxide (the electrolyte)
-energy cost of producing nickel oxide – metal hydride (electrodes)
-energy cost of producing the steel used in the casings of the batteries
:: For the Nickel oxide we can be short: nickel must be mined. So we need to look at the mining industry.
:: For the metal hydride alloys, they are produced under high vacuum. Does anyone know if this is an energy intensive process?
The metals combined in these alloys are, for the
A group: Mischmetal, La, Ce, Ti
B group: Ni, Co, Mn, Al
So we have to look at the energy used in mining and producing:
>Mischmetal: wikipedia: alloy of rare earth elements in various naturally occurring proportions. A typical composition includes approximately 50% cerium and 45% lanthanum.
>Lanthanum: see wikipedia: Monazite (Ce, La, Th, Nd, Y)PO4, and bastnasite (Ce, La, Y)CO3F, are principal ores in which lanthanum occurs in percentages up to 25 percent and 38 percent. See also category:Lanthanide minerals
>Cerium: wikipedia: found in a number of minerals including allanite (also known as orthite)—(Ca, Ce, La, Y)2(Al, Fe)3(SiO4)3(OH), monazite (Ce, La, Th, Nd, Y)PO4, bastnasite(Ce, La, Y)CO3F, hydroxylbastnasite (Ce, La, Nd)CO3(OH, F), rhabdophane (Ce, La, Nd)PO4-H2O, and synchysite Ca(Ce, La, Nd, Y)(CO3)2F. Monazite and bastnasite are presently the two most important sources of cerium.
Cerium is most often prepared via an ion exchange process that uses monazite sands as its cerium source.
Large deposits of monazite, allanite, and bastnasite will supply cerium, thorium, and other rare-earth metals for many years to come
>Titanium: wikipedia: Titanium metal is not found unbound to other elements in nature but the element is the ninth most abundant element in the Earth's crust (0.63% by mass) and is present in most igneous rocks and in sediments derived from them (as well as in living things and natural bodies of water). It is widely distributed and occurs primarily in the minerals anatase, brookite, ilmenite, perovskite, rutile, titanite (sphene), as well in many iron ores. Of these minerals, only ilmenite and rutile have significant economic importance, yet even they are difficult to find in high concentrations. Because it reacts easily with oxygen and carbon at high temperatures it is difficult to prepare pure titanium metal, crystals, or powder. Significant titanium ore deposits are in Australia, Scandinavia, North America and Malaysia.
>>the production table shows that many NiMH battery factories will have to import this metal, which means: energy used in transporting it
>Nickel: The bulk of the nickel mined comes from two types of ore deposits. The first are laterites where the principal ore minerals are nickeliferous limonite: (Fe,Ni)O(OH) and garnierite (a hydrous nickel silicate): (Ni,Mg)3Si2O5(OH). The second are magmatic sulfide deposits where the principal ore mineral is pentlandite: (Ni,Fe)9S8.
In terms of supply, the Sudbury region of Ontario, Canada, produces about 30 percent of the world's supply of nickel. The Sudbury deposit was created by a massive meteorite impact event early in the geologic history of Earth. Russia contains about 40% of the world's known resources at the massive Norilsk deposit in Siberia. Russia mines this primarily for its own domestic supply, and for export of palladium. Other deposits of nickel are found in New Caledonia, Australia, Cuba, and Indonesia.
>>this means: importing it: energy involved in transporting nickel in ships over oceans to NiMH battery factories.
>Cobalt: Cobalt is not found as a free metal and is generally found in the form of ores. Cobalt is usually not mined alone, and tends to be produced as a by-product of nickel and copper mining activities. The main ores of cobalt are cobaltite, erythrite, glaucodot, and skutterudite. The world's major producers of cobalt are the Democratic Republic of the Congo, mainland China, Zambia, Russia and Australia. It is also found in Finland, Azerbaijan, and Kazakhstan.
>>importing it: energy used in transporting Cobalt in ships over oceans to NiMH battery manufacturing plants
>Manganese: Manganese occurs principally as pyrolusite (MnO2), and to a lesser extent as rhodochrosite (MnCO3). Land-based resources are large but irregularly distributed; those of the United States are very low grade and have potentially high extraction costs. South Africa and Ukraine account for more than 80% of the world's identified resources; South Africa accounts for more than 80% of the total exclusive of China and Ukraine.
US Import Sources (1998-2001): Manganese ore: Gabon, 70%; South Africa, 10%; Australia, 9%; Mexico, 5%; and other, 6%. Ferromanganese: South Africa, 47%; France, 22%; Mexico, 8%; Australia, 8%; and other, 15%. Manganese contained in all manganese imports: South Africa, 31%; Gabon, 21%; Australia, 13%; Mexico, 8%; and other, 27%.
>>importing it: energy used in transporting Cobalt in ships over oceans to NiMH battery manufacturing plants
>Aluminium: Although aluminium is the most abundant metallic element in Earth's crust (believed to be 7.5% to 8.1%), it is very rare in its free form and was once considered a precious metal more valuable than gold.
Aluminium is a reactive metal and it is hard to extract it from its ore, aluminium oxide (Al2O3). Direct reduction, with carbon for example, is not economically viable since aluminium oxide has a melting point of about 2000 °C. Therefore, it is extracted by electrolysis — the aluminium oxide is dissolved in molten cryolite and then reduced to the pure metal. By this process, the actual operational temperature of the reduction cells is around 950 to 980 °C. Cryolite was originally found as a mineral on Greenland, but has been replaced by a synthetic cryolite. Cryolite is a mixture of aluminium, sodium, and calcium fluorides: (Na3AlF6). The aluminium oxide (a white powder) is obtained by refining bauxite, which is red since it contains 30 to 40% iron oxide. This is done using the so-called Bayer process. Previously, the Deville process was the predominant refining technology.
The electrolytic process replaced the Wöhler process, which involved the reduction of anhydrous aluminium chloride with potassium. Both of the electrodes used in the electrolysis of aluminium oxide are carbon. Once the ore is in the molten state, its ions are free to move around. The reaction at the negative cathode is
Al3+ + 3 e- → Al
Here the aluminium ion is being reduced (electrons are added). The aluminium metal then sinks to the bottom and is tapped off.
At the positive electrode (anode) oxygen gas is formed:
2 O2- → O2 + 4 e-
This carbon anode is then oxidised by the oxygen. The anodes in a reduction must therefore be replaced regularly, since they are consumed in the process:
O2 + C → CO2
Unlike the anodes, the cathodes are not consumed during the operation, since there is no oxygen present at the cathode. The carbon cathode is protected by the liquid aluminium inside the cells. Cathodes do erode, mainly due to electrochemical processes. After 5 to 10 years, depending on the current used in the electrolysis, a cell has to be reconstructed completely, because the cathodes are completely worn.
Aluminium electrolysis with the Hall-Héroult process consumes a lot of energy, but alternative processes were always found to be less viable economically and/or ecologically. The world-wide average specific energy consumption is approximately 15±0.5 kilowatt-hours per kilogram of aluminium produced (52 to 56 MJ/kg). The most modern smelters reach approximately 12.8 kW·h/kg (46.1 MJ/kg). Reduction line current for older technologies are typically 100 to 200 kA. State-of-the-art smelters operate with about 350 kA. Trials have been reported with 500 kA cells.
Electric power represents about 20 to 40% of the cost of producing aluminium, depending on the location of the aluminium smelter. Smelters tend to be located where electric power is plentiful and inexpensive, such as South Africa, the South Island of New Zealand, Australia, China, Middle-East, Russia, Iceland and Quebec in Canada.
In 2004, China was the top world producer of aluminium. Suriname depends on aluminium exports for 70% of its export earnings.[5]
>>Aluminium is very energy intensive to produce.
Obviously, the
environmental costs of continuously cleaning up these mining sites are considerable and they need to be taking into account.
Mines pollute rivers, etc... just as fertilisers for energy crops do.
We will definitely take this into account.