Thursday, 3 January 2013

Biomass Energy

Biomass is a type of material from living organisms that mainly referring to plants or plant-derived material. It could convert to other types of energy through combustion, chemical reaction or biochemical conversion which makes biomass energy become a kind of renewable energy. In many ways biomass can be considered as a form of stored solar energy. The energy of the sun is captured through process of photosynthesis in growing plants.
There are three different types of biomass material according to the IEA:

  • Woody biomass: Forest residues, Fuel wood, Short rotation forestry, Woodlands biomass.
  • Non-woody biomass: Agricultural crops, Crop residues, Processing residues.
  • Other organic wastes: Animal waste, Sewage sludge, Organic wastes produced by households and institutional buildings.
As a fuel, biomass sources could produce energy through Combustion, Gasification, Pyrolysis and Anerobic Digestion. Biomass technology might have impact on the environment when the main methodology is combustion which would emit a large amount of Carbon dioxide to the atmosphere. Furthermore, it also has an impact on the land conservation.

Reference
Roberta Navickis (1978) Biomass  Science News, Vol. 113, No.1, Solar Energy Double Issue, pp. 258-259. Published by: Society for Science & the Public
Encyclopaedia of Energy, 'Biomass for Renewable Energy and Fuels', Donald L.Klass 2004
IEA Bio-energy Education
US Department of Energy, Biomass Program
H. Liu and Y. Neubauer,'Gasification' in 'High Temperature Processes in Chemical Engineering', pp361-408, 2010


Tuesday, 1 January 2013

Geothermal

Early humans may use geothermal water in pool and hot spring for cooking and bathing. The first use of geothermal energy for electric power production was in Italy with experimental work by Prince Gionori Conti between 1904 and 1905. The first commercial power plant (250 kWe) was commissioned in 1913 at Larderello, Italy. An experimental 35 kWe plant was installed in The Geyers in 1932, and provided power to the local resort. These developments were followed in New Zealand at Wairakei in 1958; an experimental plant at Pathe, Mexico in 1959; and the first commercial plant at The Geysers in the United States in 1960. Japan followed with 23 MWe at Matsukawa in 1966. All of these early plants used steam directly from the earth (dry steam fields), except for New Zealand, which was the first to use flashed or separated steam for running the turbines. The former USSR produced power from the first true binary power plant, 680 kWe using 81˚C water at Paratunka on the Kamchatka peninsula – the lowest temperature, at that time. Iceland first produced power at Namafjall in northern Iceland, from a 3 MWe non-condensing turbine. These were followed by plants in El Salvador, China, Indonesia, Kenya, Turkey, Philippines, Portugal (Azores), Greece and Nicaragua in the 1970s and 80s. Later plants were installed in Thailand, Argentina, Taiwan, Australia, Costa Rica, Austria, Guatemala, Ethiopia, with the latest installations in Germany and Papua New Guinea. (See Cataldi, et al., 1999 for more background).
The basic principle of using geothermal energy is based on the heat transfer from the underground and overground. There are mainly seven types of geothermal resources that utilized today.

  • Convective hydrothermal resources
  • Vapor dominated systems 
  • Water dominated systems
  • Sedimentary basins
  • Geopressured resources
  • Radiogenic resources
  • Hot dry rock resources
  • Molten rock or magma resources 



Reference

WORlD GEOTHERMal GENERaTION IN 2007 (2007) Ruggero Bertani, Enel – International Division – Renewable Energy Business Development - Via 
Dalmazia 15, 00198 Rome, Italy
The Future of 
Geothermal Energy (2010)
 
The Future of  
Impact of Enhanced Geothermal  
Systems (EGS) on the United States 
in the 21
st
 Century
Geothermal Energy: 
International Market 
Update (2011) 
 Alison Holm, Leslie Blodgett, 
Dan Jennejohn and Karl Gawell
CHARACTERISTICS, DEVELOPMENT AND UTILIZATION OF GEOTHERMAL RESOURCES (2007) 
John W. Lund, Geo-Heat Center, Oregon Institute of Technology