explain different minerals to use to produce energy
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Almost all Earth Materials are used by humans for something. We require
metals for making machines, sands and gravels for making roads and
buildings, sand
for making computer chips, limestone and gypsum for making concrete,
clays for making ceramics, gold, silver, copper and aluminum for making
electric circuits, and diamonds
and corundum (sapphire,
ruby, emerald) for abrasives and jewelry. A mineral deposit is a
volume of rock enriched in one or more materials. In this sense a mineral
refers to a useful material, a definition that is different from the way
we defined a mineral back in Chapter 2. Here the word mineral can be any
substance that comes from the Earth. Finding and exploiting mineral
deposits requires the application of the principles of geology that you
have learned throughout this course. Some minerals are used as they are
found in the ground, i.e. they require no further processing or very
little processing. For example - gemstones, sand, gravel, and salt
(halite). Most minerals must be processed before they are used. For
example:
Iron is the found in abundance in minerals, but the process of
extracting iron from different minerals varies in cost depending on
the mineral. It is least costly to extract the iron from oxide
minerals like hematite (Fe2O3), magnetite (Fe3O4), or limonite
[Fe(OH)]. Although iron also occurs in olivines, pyroxenes,
amphiboles, and biotite, the concentration of iron in these minerals
is less, and cost of extraction is increased because strong bonds
between iron, silicon, and oxygen must be broken.Aluminum is the third most abundant mineral in the Earth's crust. It
occurs in the most common minerals of the crust - the feldspars
(NaAlSi3O8, KalSi3O8, & CaAl2Si2O8, but the cost of extracting the
Aluminum from these minerals is high. Thus, deposits containing the
mineral gibbsite [Al(OH)3], are usually sought. This explains why
recycling of Aluminum is cost effective, since the Aluminum does not
have to be separated from oxygen or silicon.
Because such things as extraction costs, manpower costs, and energy costs vary with time and from country to country, what constitutes an economically viable deposit of minerals varies considerably in time and place. In general, the higher the concentration of the substance, the more economical it is to mine. Thus we define an ore as a mineral deposit from which one or more valuable substances can be extracted economically. An ore deposit will consist of ore minerals, that contain the valuable substance.
Gangue minerals are minerals that occur in the deposit but do not contain the valuable substance
Since economics is what controls the grade or concentration of the substance in a deposit that makes the deposit profitable to mine, different substances require different concentrations to be profitable.. But, the concentration that can be economically mined changes due to economic conditions such as demand for the substance and the cost of extraction.
Examples: The copper concentration in copper ore deposits has shown changes throughout history. From 1880 to about 1960 the grade of copper ore showed a steady decrease from about 3% to less than 1%, mainly due to increased efficiency of mining. From about 1960 to 1980 the grade increased to over 1% due to increasing costs of energy and an abundant supply produced by cheaper labor in other countries. Gold prices vary on a daily basis. When gold prices are high, old abandoned mines re-open, when the price drops, gold mines close. The cost of labor is currently so high in the U.S. that few gold mines can operate profitably, but in third world countries where labor costs are lower, gold mines that have ore concentrations well below those found in the U.S. can operate with a profit. For every substance we can determine the concentration necessary in a mineral deposit for profitable mining. By dividing this economical concentration by the average crustal abundance for that substance, we can determine a value called the concentration factor. The table below lists average crustal abundances and concentration factors for some of the important materials that are commonly sought. For example, Al, which has an average crustal abundance of 8%, has a concentration factor of 3 to 4. This means that an economic deposit of Aluminum must contain between 3 and 4 times the average crustal abundance, that is between 24 and 32% Aluminum, to be economical
Because such things as extraction costs, manpower costs, and energy costs vary with time and from country to country, what constitutes an economically viable deposit of minerals varies considerably in time and place. In general, the higher the concentration of the substance, the more economical it is to mine. Thus we define an ore as a mineral deposit from which one or more valuable substances can be extracted economically. An ore deposit will consist of ore minerals, that contain the valuable substance.
Gangue minerals are minerals that occur in the deposit but do not contain the valuable substance
Since economics is what controls the grade or concentration of the substance in a deposit that makes the deposit profitable to mine, different substances require different concentrations to be profitable.. But, the concentration that can be economically mined changes due to economic conditions such as demand for the substance and the cost of extraction.
Examples: The copper concentration in copper ore deposits has shown changes throughout history. From 1880 to about 1960 the grade of copper ore showed a steady decrease from about 3% to less than 1%, mainly due to increased efficiency of mining. From about 1960 to 1980 the grade increased to over 1% due to increasing costs of energy and an abundant supply produced by cheaper labor in other countries. Gold prices vary on a daily basis. When gold prices are high, old abandoned mines re-open, when the price drops, gold mines close. The cost of labor is currently so high in the U.S. that few gold mines can operate profitably, but in third world countries where labor costs are lower, gold mines that have ore concentrations well below those found in the U.S. can operate with a profit. For every substance we can determine the concentration necessary in a mineral deposit for profitable mining. By dividing this economical concentration by the average crustal abundance for that substance, we can determine a value called the concentration factor. The table below lists average crustal abundances and concentration factors for some of the important materials that are commonly sought. For example, Al, which has an average crustal abundance of 8%, has a concentration factor of 3 to 4. This means that an economic deposit of Aluminum must contain between 3 and 4 times the average crustal abundance, that is between 24 and 32% Aluminum, to be economical
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