Geology Reference
In-Depth Information
The natural exergy bonus lost on Earth since the beginning of the 20th century
B .
The velocity of the Earth's exergy degradation due to mineral extraction ( B )
throughout the 20th century and the beginning of the 21st, and for comparative
purposes between 1996 and 2008.
The depletion degree of the reserves (% R. loss), calculated as B =(R 2010 +
B )
The years until depletion of the commodities (R/P).
The theoretical year where the peak of production is reached.
Table 13.3 shows a summary of the results obtained for the 54 mineral com-
modities 13 .
Table 13.3: The worldwide depletion of the exergy reservoir of the main mineral
commodities
B ,
ktoe/yr
(1900-
2008)
B ,
ktoe/yr
(1996-
2008)
B ,
ktoe
(1900-
2008)
Substance
reported
by USGS
Mineral
ore
P,
tonnes
(1900-
2008)
% R
loss
R/P,
yrs
Aluminium
(Bauxite)
Gibbsite
4.93E+09 2.63E+07 2.41E+05 8.20E+05 15.4
132
Antimony
Stibnite
6.00E+06 6.98E+04 6.41E+02 1.61E+03 74.1
11
Arsenic
Arsenopyrite
3.67E+06 1.66E+04 1.52E+02 2.16E+02 75.0
23
Barium
Barite
3.13E+08 N.A.
N.A.
N.A.
64.8
21
Beryllium
Beryl
1.61E+04 5.19E+01 4.80E-01
6.05E-01
N.A.
N.A.
Bismuth
Bismuthinite
2.40E+05 3.44E+01 3.16E-01
7.30E-01
42.9
42
Boron
Kernite
1.18E+08 N.A.
N.A.
N.A.
41.0
39
Cadmium
Greenockite
1.03E+06 1.49E+05 1.36E+03 2.82E+03 63.5
30
Cesium
Pollucite
8.53E+02 N.A.
N.A.
N.A.
1.2
N.A.
Chromium
Chromite
1.76E+08 4.06E+04 3.72E+02 1.16E+03 42.4
34
Cobalt
Linnaeite
1.88E+06 4.87E+05 4.47E+03 1.32E+04 22.1
87
Copper
Chalcopyrite
5.26E+08 1.43E+06 1.31E+04 3.70E+04 49.4
35
Feldspar
Orthoclase
3.23E+08 N.A.
N.A.
N.A.
N.A.
N.A.
Fluorspar
Fluorite
2.40E+08 1.08E+06 9.86E+03 2.19E+04 51.0
38
Gallium
Ga in baux-
ite
1.00E+06 N.A.
N.A.
N.A.
N.A.
N.A.
Germanium Ge in sulfide
ores
3.74E+03 N.A.
N.A.
N.A.
N.A.
N.A.
Gold
Native gold
1.33E+05 1.91E+06 1.75E+04 3.52E+04 73.9
21
Graphite
Graphite
4.08E+07 N.A.
N.A.
N.A.
36.5
63
Gypsum
Gypsum
4.78E+09 1.81E+06 1.66E+04 4.77E+04 N.A.
N.A.
Continued on next page :::
13 Uranium has been included in the non-fuel mineral classification, using the statistics published
by the World Nuclear Association (WNA, 2012) (see Table D.12). Uranium assured reserves were
estimated by the WNA at 5.5 Mtons in 2010. The average ore grade of U 3 O 8 assumed constitutes
0.33% or 0.28% of U (Table 6.9). The nuclear exergy of uranium, which is huge compared to its
chemical one (see Chap. 6), has not been taken into account.
 
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