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Books on the topic 'Oxygen. Soil aeration. Soils'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Murray, E. J. Unsaturated soils: A fundamental interpretation of soil behaviour. Wiley-Blackwell, 2010.

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2

Ng, C. W. W. Unsaturated soil mechanics and engineering. Taylor & Francis, 2007.

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3

Genuchten, M. Th Van. The RETC code for quantifying the hydraulic functions of unsaturated soils. Robert S. Kerr Environmental Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency, 1992.

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4

Genuchten, M. Th Van. The RETC code for quantifying the hydraulic functions of unsaturated soils. Robert S. Kerr Environmental Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency, 1992.

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5

Schäffer, Jürgen. Bodenstruktur, Belüftung und Durchwurzelung befahrener Waldböden: Prozessstudien und Monitoring. Forstliche Versuchs- und Forschungsanstalt Baden-Württemberg, Abteilung Boden und Umwelt, 2012.

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6

Sword, Mary A. Local soils information needed to define the root zone in process models on the Gulf Coastal Plain. Southern Research Station, 2002.

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7

(2010), GeoShanghai International Conference. Experimental and applied modeling of unsaturated soils: Proceedings of the GeoShanghai 2010 International Conference, June 3-5, 2010, Shanghai, China. American Society of Civil Engineers, 2010.

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8

1972-, Hoyos Laureano R., Zhang Xiong 1971-, Puppala Anand J, and American Society of Civil Engineers, eds. Experimental and applied modeling of unsaturated soils: Proceedings of the GeoShanghai 2010 International Conference, June 3-5, 2010, Shanghai, China. American Society of Civil Engineers, 2010.

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9

Doyle, Marie. The effect of forest-harvesting machine traffic on the aeration and pore size distribution in a blanket peat. University College Dublin, 1997.

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10

Sitnikov, Anatoliĭ Borisovich. Dinamika vlagi i soleĭ v pochvogruntakh zony aėrat͡s︡ii. Nauk. dumka, 1986.

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11

Ying, Ouyang. Diffusion of oxygen and carbon dioxide through soil with temperature and water content effects on sink/source strength. 1986.

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12

Ou-yang, Ying. Dynamic mathematical model of oxygen and carbon dioxide exchange between soil and atmosphere. 1986.

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13

J, Leij Feike, and National Exposure Research Laboratory (U.S.), eds. The UNSODA unsaturated soil hydraulic database: User's manual. National Risk Management Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency, 1996.

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14

Advanced Unsaturated Soil Mechanics and Engineering. Taylor & Francis, 2007.

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15

J, Leij F., Yates S. R, and Robert S. Kerr Environmental Research Laboratory, eds. The RETC code for quantifying the hydraulic functions of unsaturated soils: Project summary. U.S. Environmental Protection Agency, Robert S. Kerr Environmental Research Laboratory, 1992.

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16

The RETC code for quantifying the hydraulic functions of unsaturated soils: Project summary. U.S. Environmental Protection Agency, Robert S. Kerr Environmental Research Laboratory, 1992.

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17

Pascoe, Frank. Effects of forest soil compaction on gas diffusion, denitrification, nitrogen mineralization, and soil respiration. 1992.

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18

Unsaturated soil mechanics in geotechnical practice. 2013.

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19

L, Baehr Arthur, and Geological Survey (U.S.), eds. Estimating spatial variability of recharge in southern New Jersey from unsaturated-zone measurements. U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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20

White, Robert E. Understanding Vineyard Soils. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780199342068.001.0001.

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The first edition of Understanding Vineyard Soils has been praised for its comprehensive coverage of soil topics relevant to viticulture. However, the industry is dynamic--new developments are occurring, especially with respect to measuring soil variability, managing soil water, possible effects of climate change, rootstock breeding and selection, monitoring sustainability, and improving grape quality and the "typicity" of wines. All this is embodied in an increased focus on the terroir or "sense of place" of vineyard sites, with greater emphasis being placed on wine quality relative to quanti

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21

Kirchman, David L. The physical-chemical environment of microbes. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0003.

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Many physical-chemical properties affecting microbes are familiar to ecologists examining large organisms in our visible world. This chapter starts by reviewing the basics of these properties, such as the importance of water for microbes in soils and temperature in all environments. Another important property, pH, has direct effects on organisms and indirect effects via how hydrogen ions determine the chemical form of key molecules and compounds in nature. Oxygen content is also critical, as it is essential to the survival of all but a few eukaryotes. Light is used as an energy source by photo

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22

Kirchman, David L. Degradation of organic matter. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0007.

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The aerobic oxidation of organic material by microbes is the focus of this chapter. Microbes account for about 50% of primary production in the biosphere, but they probably account for more than 50% of organic material oxidization and respiration (oxygen use). The traditional role of microbes is to degrade organic material and to release plant nutrients such as phosphate and ammonium as well as carbon dioxide. Microbes are responsible for more than half of soil respiration, while size fractionation experiments show that bacteria are also responsible for about half of respiration in aquatic hab

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