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Books on the topic 'Methane. Carbon dioxide. Hydrates'

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Published: 4 June 2021
Last updated: 16 February 2022

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1

Mei ceng xi fu te zheng ji chu qi ji li. Beijing Shi: Ke xue chu ban she, 2013.

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2

United States. Department of Agriculture. Global Change Program Office. U.S. agriculture and forestry greenhouse gas inventory: 1990-2008. Washington, D.C.?]: U.S. Dept. of Agriculture, Office of the Chief Economist, Global Change Program Office, 2011.

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3

Savage, Kathleen. BOREAS TGB-1 [i.e. TGB-3] CH4 and CO2 chamber flux data over NSA upland sites. Greenbelt, Md: NASA Goddard Space Flight Center, 2000.

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4

Savage, Kathleen. BOREAS TGB-1 [i.e. TGB-3] CH4 and CO2 chamber flux data over NSA upland sites. Greenbelt, Md: NASA Goddard Space Flight Center, 2000.

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5

Jaques, A. P. Trends in Canada's greenhouse gas emissions (1990-1995). Ottawa: Air Pollution Prevention Directorate, Pollution Data Branch, Environment Canada, 1997.

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6

Jaques, A. P. Trends in Canada's greenhouse gas emissions (1990-1995). Ottawa: Air Pollution Prevention Directorate, Pollution Data Branch, Environment Canada, 1997.

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7

Ciborowski, Peter. Minnesota greenhouse gas inventory, 1990. [St. Paul: Air Quality Division, Minnesota Pollution Control Agency, 1995.

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8

Burniaux, Jean-Marc. A multi-gas assessment of the Kyoto Protocol. Paris: OECD, 2000.

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9

Burniaux, Jean-Marc. A multi-gas assessment of the Kyoto Protocol. Paris: O.E.C.D., 2000.

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10

Burniaux, Jean-Marc. A multi-gas assessment of the Kyoto Protocol. Paris: OECD, 2000.

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11

United States. Dept. of Agriculture. Global Change Program Office. U.S. agriculture and forestry greenhouse gas inventory, 1990-2005. [Washington, D.C.]: U.S. Dept. of Agriculure, Office of the Chief Economist, Global Change Program Office, 2008.

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12

Pascale, Collas, Olsen K, Canada Environment Canada, and Canada. Air Pollution Prevention Directorate., eds. Canada's greenhouse gas inventory: 1997 emissions and removals with trends. [Ottawa]: Environment Canada, 1999.

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13

Development of a carbon formation reactor for carbon dioxide reduction: Final report. Windsor Locks, Conn: United Technologies Corporation, Hamilton Standard Division, 1985.

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14

How restricting carbon dioxide and methane emissions would affect the Indian economy. Washington, DC (1818 H St. NW, Washington 20433): Office of the Vice President, Development Economics, World Bank, 1992.

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15

Liu, Guoxiang. Greenhouse gases: Capturing, utilization and reduction. 2012.

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16

1964-, Liu Chang-jun, Mallinson Richard G. 1954-, Aresta M. 1940-, American Chemical Society. Division of Fuel Chemistry, and American Chemical Society Meeting, eds. Utilization of greenhouse gases. Washington, DC: American Chemical Society, 2003.

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17

Control of methane production and exchange in northern peatlands: Final report. [Washington, DC: National Aeronautics and Space Administration, 1998.

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18

United States. National Aeronautics and Space Administration., ed. Control of methane production and exchange in northern peatlands: Final report. [Washington, DC: National Aeronautics and Space Administration, 1998.

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19

Flexible pipes: Permeation of methane, carbon dioxide and water through Tefzel ETFE - experiments 1996. Austin, Tex: [Texas Research Institute, 1997.

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20

Canada, Canada Environment, and Canada. Air Pollution Prevention Directorate., eds. Canada's greenhouse gas inventory: 1990-2003. Ottawa: Environment Canada, 2005.

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21

R, Herring J., and Geological Survey (U.S.), eds. Methane, carbon dioxide, oxygen, and nitrogen in soil gas overlying coal beds of the Upper Cretaceous Fruitland Formation in the San Juan Basin, La Plata County, southwestern Colorado. [Denver, Colo.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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22

R, Thomas S., and United States. National Aeronautics and Space Administration., eds. Numerical study of contaminant effects on combusstion if hydrogen,ethaneand methane in air. [Washington, DC]: National Aeronautics and Space Administration, 1995.

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23

Solid waste management and greenhouse gases: A life-cycle assessment of emissions and sinks. 3rd ed. [Washington, D.C.]: U.S. Environmental Protection Agency, 2006.

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24

R, Moore Tim, and Goddard Space Flight Center, eds. BOREAS TGB-1 [i.e. TGB-3] CH4 and CO2 chamber flux data over NSA upland sites. Greenbelt, Md: NASA Goddard Space Flight Center, 2000.

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25

Trends '93: A compendium of data on global change. Oak Ridge, Tenn: Carbon Dioxide Information Analysis Center, World Data Center-A for Atmospheric Trace Gases, Environmental Sciences Division, Oak Ridge National Laboratory, 1994.

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26

J, Arkebauer Timothy, and United States. National Aeronautics and Space Administration., eds. Field micrometeorological measurements, process-level studies and modeling of methane and carbon dioxide fluxes in a boreal wetland ecosystem: Final technical report ... grant # NAG 5-2585. [Washington, DC: National Aeronautics and Space Administration, 1998.

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27

Canada, Canada Environment, and Canada Greenhouse Gas Division, eds. Canada's greenhouse gas inventory: Overview, 1990-2002. [Ottawa]: Environment Canada, 2004.

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28

Afshin, Matin, Canada Environment Canada, and Canada Greenhouse Gas Division, eds. Canada's greenhouse gas inventory: 1990-2002. Ottawa: Environment Canada, 2004.

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29

Kirchman, David L. Processes in anoxic environments. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0011.

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During organic material degradation in oxic environments, electrons from organic material, the electron donor, are transferred to oxygen, the electron acceptor, during aerobic respiration. Other compounds, such as nitrate, iron, sulfate, and carbon dioxide, take the place of oxygen during anaerobic respiration in anoxic environments. The order in which these compounds are used by bacteria and archaea (only a few eukaryotes are capable of anaerobic respiration) is set by thermodynamics. However, concentrations and chemical state also determine the relative importance of electron acceptors in organic carbon oxidation. Oxygen is most important in the biosphere, while sulfate dominates in marine systems, and carbon dioxide in environments with low sulfate concentrations. Nitrate respiration is important in the nitrogen cycle but not in organic material degradation because of low nitrate concentrations. Organic material is degraded and oxidized by a complex consortium of organisms, the anaerobic food chain, in which the by-products from physiological types of organisms becomes the starting material of another. The consortium consists of biopolymer hydrolysis, fermentation, hydrogen gas production, and the reduction of either sulfate or carbon dioxide. The by-product of sulfate reduction, sulfide and other reduced sulfur compounds, is oxidized back eventually to sulfate by either non-phototrophic, chemolithotrophic organisms or by phototrophic microbes. The by-product of another main form of anaerobic respiration, carbon dioxide reduction, is methane, which is produced only by specific archaea. Methane is degraded aerobically by bacteria and anaerobically by some archaea, sometimes in a consortium with sulfate-reducing bacteria. Cultivation-independent approaches focusing on 16S rRNA genes and a methane-related gene (mcrA) have been instrumental in understanding these consortia because the microbes remain uncultivated to date. The chapter ends with some discussion about the few eukaryotes able to reproduce without oxygen. In addition to their ecological roles, anaerobic protists provide clues about the evolution of primitive eukaryotes.
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30

Schrijver, Karel. Habitability of Planets and Moons. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198799894.003.0010.

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The author takes us to visit Saturn’s moon Titan, and Venus, Mars, and to the unconfirmed planet GJ581d. Although we find unearthly conditions on these bodies’ surfaces today, things were different in the past. Even now, there are oceans deep below Titan’s frozen ice shell that itself sees liquid methane rains and vast ethane-filled lakes. Venus and Mars both had liquid water long ago, while Venus may even have been comfortably warm and humid before modern complex life developed on Earth. Many potentially habitable exoplanets are likely locked in their rotation to always face their star with the same side, causing incredible differences between their day and night sides. This chapter reviews how oceans and atmospheres are lost by the Sun’s magnetism or protected by that of the planets’, how masses of carbon dioxide can be stored in solid limestone, and how habitable zones shift to and from planets.
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31

Kirchman, David L. Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0001.

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The goal of this chapter is to introduce the field of microbial ecology and some terms used in the rest of the book. Microbial ecology, which is the study of microbes in natural environments, is important for several reasons. Although most are beneficial, some microbes cause diseases of higher plants and animals in aquatic environments and on land. Microbes are also important because they are directly or indirectly responsible for the food we eat. They degrade pesticides and other pollutants contaminating natural environments. Finally, they are important in another “pollution” problem: the increase in greenhouse gases such as carbon dioxide and methane in the atmosphere. Because microbes are crucial for many biogeochemical processes, the field of microbial ecology is crucial for understanding the effect of greenhouse gases on the biosphere and for predicting the impact of climate change on aquatic and terrestrial ecosystems. Even if the problem of climate change were solved, microbes would be fascinating to study because of the weird and wonderful things they do. The chapter ends by pointing out the difficulties in isolating and cultivating microbes in the laboratory. In many environments, less than one percent of all bacteria and other microbes can be grown in the laboratory. The cultivation problem has many ramifications for identifying especially viruses, bacteria, and archaea in natural environments, and for connecting up taxonomic information with biogeochemical processes.
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