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Energy, Environment, and Industrial Development. Michael B. McElroy Frederick H. Abernathy Lecture 14 April 3, 2006. Photosynthesis: a mechanism for conversion of solar energy to chemical potential energy Sunlight + CO 2 + H 2 O  CH 2 O + O 2

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Energy environment and industrial development

Energy, Environment, and Industrial Development

Michael B. McElroy

Frederick H. Abernathy

Lecture 14

April 3, 2006


organic matter

oxygen released to atmosphere


graphite



Lignite
Lignite temperatures, its chemical composition is altered

  • Lowest rank of coal. Used almost exclusively for steam-electric power generation

  • Brownish-black in color with high inherent moisture content – sometimes as high as 45%

  • Heat content ranges from 9 ~ 17 million BTU/ton. Computed on a moist, mineral matter free, basis.


Sub bituminous coal
Sub-bituminous coal temperatures, its chemical composition is altered

  • Intermediate between lignite and bituminous

  • Color ranges from dull, dark brown, to black. Relatively soft and crumbly

  • 20~30% inherent moisture content

  • Heat content 17 ~ 24 million BTU/ton on moist, mineral-matter free, basis.

  • Major US source in Powder River Basin of Wyoming. Used mainly for electric power generation


Bituminous coal
Bituminous coal temperatures, its chemical composition is altered

  • Most abundant US source

  • Moisture content < 20%

  • Heat content 21~30 million BTU/ton

  • Dense, black, matter

  • Used for power generation but also for heat and as a source of coke


Anthracite coal
Anthracite coal temperatures, its chemical composition is altered

  • Hard, brittle, black, lustrous color

  • High in C with low content of volatiles

  • Moisture content < 15%

  • Heat content 22~28 million BTU/ton, average for US 25x106 BTU/ton


  • Primary sources of coal in the US: Appalachia, Mid-west, West

  • Sulfur content of western coal is relatively low, typically about 0.7%

  • Sulfur content of Eastern coal is relatively high, typically 3~4%

  • Up to 1970, Eastern sources dominated US production. More recent shift to Western sources

  • Coal consumption in US is dominated now by electric power production. Prior to 1945, railroads and residential heating were comparable to power generation


Origins of coal
Origins of Coal West

  • Products of land-based plants

  • Recall that life expanded to land at about 440x106 yr BP (November 25, 7am)

  • Carboniferous period 360~290x106 yr BP

  • England at that time was close to the equator


320 Ma (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

410 Ma (Paleozoic/Silurian/Pridoli)

Picture source: Windley, Brian F. The Evolving Continents. West Sussex: John Wiley & Sons Ltd., 1995.

Figures adopted from http://www.dinosauria.com/dml/maps.htm


Origins of coal1
Origins of Coal (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

  • Think of primitive jungles with massive trees – lepidodendron, sigillaria (see story in Coal – Barbara Freeze)

  • Slow decay led to preservation of large quantities of plant material

  • Decay often took place in environments flooded episodically with sea water

  • Sea water is high in sulfur


Origins of coal2
Origins of Coal (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

  • Decay resulted in depletion of oxygen. SO42- would have been reduced. Sulfur retained often in form of pyrite, FeS2. Pyrite is the most abundant sulfide mineral, sometimes known as “fool’s gold”.

  • In addition to combustible C, coal contains variable amounts of Ca, Mg, K, S, Cl and other chemical elements bound up in mineral form.


Environmental problems associated with coal
Environmental problems associated with coal (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

  • Problems with mining:

     black lung disease

     mine collapse

     explosions CH4, CO

     CO2

     flooding

  • Residues from mining

     pollution of soils and waters

     devastation of landscapes


Environmental problems associated with coal1
Environmental problems associated with coal (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

  • Problems with coal combustion

     particles released to air

     soot

     sulfur

     mercury, etc


Acid rain
Acid Rain (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

  • Combustion of coal converts S to SO2

  • SO2 in the atmosphere is oxidized to H2SO4 (sulfuric acid)

    SO2 x-4 = 0, x = 4

    H2SO4  x+2-8=0, x = 6

  • In rain

    H2SO4 H+ + H+ + SO42-

  • pH of rain in equilibrium with atmospheric CO2 pH = 5.6


Figure 18.5 (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)


Figure 18.5 continued (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)


Figure 18.6 (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)


Figure 18.6 continued (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)


http://www.eia.doe.gov/oiaf/ieo/figure_56.html (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)


Coal consumption top 25 countries
Coal consumption: Top 25 countries (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)

http://www.nationmaster.com/red/graph-T/ene_coa_con#


http://www.eia.doe.gov/oiaf/ieo/figure_55.html (Paleozoic/Carboniferous/Pennsylvanian/Bashkirian/Yeadonian)


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