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Livres sur le sujet « Partitioning of soil respiration »

Auteur : Grafiati

Publié le 9 mars 2023

Mis à jour le 10 mars 2023

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1

J, Pollock C., Farrar J. F et Gordon A. J, dir. Carbon partitioning, within and between organisms. Oxford : Bios Scientific, 1992.

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2

Naumov, A. V. Dykhanie pochvy : Sostavli︠a︡i︠u︡shchie, ėkologicheskie funkt︠s︡ii, geograficheskie zakonomernosti. Novosibirsk : Izd-vo Sibirskogo otd-nii︠a︡ Rossiĭskoĭ Akademii Nauk, 2009.

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3

Naumov, A. V. Dykhanie pochvy : Sostavli︠a︡i︠u︡shchie, ėkologicheskie funkt︠s︡ii, geograficheskie zakonomernosti. Novosibirsk : Izd-vo Sibirskogo otd-nii︠a︡ Rossiĭskoĭ Akademii Nauk, 2009.

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4

Gardea, Alfonso A. Water partitioning and respiration activity of dormant grape buds. 1992.

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5

Zhou, Xuhui, et Luo Yiqi. Soil Respiration and the Environment. Elsevier Science & Technology Books, 2010.

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6

Soil Respiration and the Environment. Academic Press, 2006.

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7

Soil Respiration and the Environment. Elsevier, 2006. http://dx.doi.org/10.1016/b978-0-12-088782-8.x5000-1.

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8

Luo, Yiqi, et Xuhui Zhou. Soil Respiration and the Environment. Academic Press, 2006.

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9

Forest Soil Respiration under Climate Changing. MDPI, 2018. http://dx.doi.org/10.3390/books978-3-03897-179-5.

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10

National Aeronautics and Space Administration (NASA) Staff. Boreas Te-5 Soil Respiration Data. Independently Published, 2018.

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11

Hung, Hayley Hing Ning. Partitioning and transport of organic compounds in air-plant-soil systems. 2000.

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12

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

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13

Taliaferro, Lindsay C. Seasonal changes in the partitioning of heavy metals in a southwestern Ohio soil. 1987.

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14

Wood, Brian David. Carbon dioxide as a measure of microbial activity in the unsaturated zone. 1991.

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15

Flint, Lorraine E. Effects of soil surface shading, mulching and vegetation control on Douglas-fir seedling growth and microsite water partitioning. 1985.

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16

Riggs, Dale Ila Miles. The effect of soil applied boron on fruit deformity, yield and boron partitioning in "Tristar" and "Benton" strawberries. 1987.

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17

Boening, Dean W. Evaluation of an automated respiration method used in assessing the toxicity of zinc on soil microorganisms. 1992.

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18

Brewer, J. Stephen, et Jan Schlauer. Biogeography and habitats of carnivorous plants. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198779841.003.0002.

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Understanding the processes involved in generating distribution patterns of carnivorous plants requires investigation at multiple scales. Carnivorous plants typically occur in warm or hot and humid or wet climates in subtropical to tropical regions of all continents. Carnivorous plants tend to grow in wet, open, and nutrient-poor habitats. Most carnivorous plants are less tolerant of dry soils than are non-carnivorous plants. The reasons why many carnivorous plants are absent from habitats with nutrient-rich soils remain unclear, but the roles of competition and soil anoxia warrant greater attention. Reduced competition from woody plants (e.g., following fires) contributes to neutral coexistence of carnivorous and noncarnivorous herbs, and there is no evidence to date in support of nutrient-niche partitioning. More studies of interspecific competition are needed to understand better the distribution patterns and drivers of species coexistence of carnivorous and noncarnivorous plants.

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19

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 habitats. In soils, both fungi and bacteria are important, with relative abundances and activity varying with soil type. In contrast, fungi are not common in the oceans and lakes, where they are out-competed by bacteria with their small cell size. Dead organic material, detritus, used by microbes, comes from dead plants and waste products from herbivores. It and associated microbes can be eaten by many eukaryotic organisms, forming a detritus food web. These large organisms also break up detritus into small pieces, creating more surface area on which microbes can act. Microbes in turn need to use extracellular enzymes to hydrolyze large molecular weight compounds, which releases small compounds that can be transported into cells. Fungi and bacteria use a different mechanism, “oxidative decomposition,” to degrade lignin. Organic compounds that are otherwise easily degraded (“labile”) may resist decomposition if absorbed to surfaces or surrounded by refractory organic material. Addition of labile compounds can stimulate or “prime” the degradation of other organic material. Microbes also produce organic compounds, some eventually resisting degradation for thousands of years, and contributing substantially to soil organic material in terrestrial environments and dissolved organic material in aquatic ones. The relationship between community diversity and a biochemical process depends on the metabolic redundancy among members of the microbial community. This redundancy may provide “ecological insurance” and ensure the continuation of key biogeochemical processes when environmental conditions change.

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20

Wilsey, Brian J. Nutrient Cycling and Energy Flow in Grasslands. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198744511.003.0004.

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Net primary productivity (NPP) is the amount of C or biomass that accumulates over time and is photosynthesis—autotroph respiration. Annual NPP is estimated by summing positive biomass increments across time periods during the growing season, including offtake to herbivores, which can be high in grasslands. Remote sensing techniques that are used to assess NPP are discussed by the author. Belowground productivity can be high in grasslands, and it is important to carbon storage. Across grasslands on a geographic scale, NPP, N mineralization, and soil organic C all increase with annual precipitation. Within regions, NPP can be strongly affected by the proportion of C4 plant species and animal species composition and diversity. Humans are adding more N to the environment than all the natural forms of addition (fixation and lightning) combined. Animals, especially herbivores, can have strong effects on how plants respond to changes in changes in resource availability.

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