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Books on the topic 'Soil organic carbon. eng'

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Published: 4 June 2021
Last updated: 5 February 2022

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1

Smith, W. Soil degradation risk indicator: Organic carbon component. Ottawa: Agriculture and Agri-Food Canada, 1997.

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2

Leventhal, Joel S. Soil organic carbon content in rice soils of Arkansas and Louisiana and a comparison to non-agricultural soils, including a bibliography for agricultural soil carbon. [Denver, CO]: U.S. Geological Survey, 1997.

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3

Leventhal, Joel S. Soil organic carbon content in rice soils of Arkansas and Louisiana and a comparison to non-agricultural soils, including a bibliography for agricultural soil carbon. [Denver, CO]: U.S. Geological Survey, 1997.

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4

service), SpringerLink (Online, ed. Carbon Sequestration in Agricultural Soils: A Multidisciplinary Approach to Innovative Methods. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012.

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5

Nong tian tu rang you ji tan bian hua yan jiu: Nongtian turang youjitan bianhua yanjiu. Wuhu Shi: Anhui shi fan da xue chu ban she, 2011.

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6

Ryan, Miriam G. The influence of draught and rewetting on the dynamics of nitrogen, potassium and disolved organic carbon in a coniferous forest ecosystem. Dublin: University College Dublin, 1997.

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7

McInerney, M. The effect of earthworm activity, silt/clay content and climatic interactions on soil organic matter dynamics in forestry systems. Dublin: University College Dublin, 1998.

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8

Soil Organic Carbon: The Hidden Potential. Food & Agriculture Organization of the United Nations, 2017.

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9

J, Zinke Paul, Millemann Raymond E, Boden Thomas A, Carbon Dioxide Information Analysis Center (U.S.), Oak Ridge National Laboratory. Environmental Sciences Division, United States. Dept. of Energy. Office of Basic Energy Sciences. Carbon Dioxide Research Division, and United States. Dept. of Energy. Office of Energy Research, eds. Worldwide organic soil carbon and nitrogen data. Oak Ridge, Tenn: Oak Ridge National Laboratory, 1986.

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10

Ochs, Michael. Association of hydrophobic organic compounds with dissolved soil organic carbon. 1988.

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11

Global Soil Organic Carbon Map (GSOCmap) Version 1.5. FAO, 2020. http://dx.doi.org/10.4060/ca7597en.

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12

Soil carbon sequestration under organic farming in the mediterranean environment. Trivandrum: Transworld Research Signpost, 2008.

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13

Sara, Marinari, and Caporali Fabio, eds. Soil carbon sequestration under organic farming in the mediterranean environment. Trivandrum: Transworld Research Signpost, 2008.

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14

Soil organic carbon content in rice soils of Arkansas and Louisiana and a comparison to non-agricultural soils, including a bibliography for agricultural soil carbon. [Denver, CO]: U.S. Geological Survey, 1997.

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15

United States. Natural Resources Conservation Service., ed. Model simulation of soil loss, nutrient loss, and change in soil organic carbon associated with crop production. [Washington, D.C.]: U.S. Dept. of Agriculture, Natural Resources Conservation Service, 2006.

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16

United States. Natural Resources Conservation Service., ed. Model simulation of soil loss, nutrient loss, and change in soil organic carbon associated with crop production. [Washington, D.C.]: U.S. Dept. of Agriculture, Natural Resources Conservation Service, 2006.

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17

Rodman, Ann Winne. The effect of slope position, aspect, and cultivation on organic carbon distribution in the Palouse. 1988.

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18

United States. Natural Resources Conservation Service, ed. Model simulation of soil loss, nutrient loss, and change in soil organic carbon associated with crop production. [Washington, D.C.]: U.S. Dept. of Agriculture, Natural Resources Conservation Service, 2006.

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19

Superfund Innovative Technology Evaluation Program (U.S.), IT Corporation, and United States. Environmental Protection Agency, eds. Process for the treatment of volatile organic carbon and heavy metal contaminated soil. [Washington, D.C.]: U.S. Environmental Protection Agency, 1995.

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20

Monte, Francesca. NMR study of 1,4-phenilene-bis(dithiadiazolyl), soil organic matter and copper aluminum oxide. 2000.

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21

Monte, Francesca. NMR study of 1,4-phenilene-bis(dithiadiazolyl), soil organic matter and copper aluminum oxide. 2000.

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22

A soil profile and organic carbon data base for Canadian forest and tundra mineral soils. Edmonton: Northern Forestry Centre, 1997.

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23

A protocol for measurement, monitoring, reporting and verification of soil organic carbon in agricultural landscapes. FAO, 2020. http://dx.doi.org/10.4060/cb0509en.

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24

Chapin, Michele F. Effects of ryegrass residue management on Dayton soil organic carbon content, distribution and related properties. 1992.

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25

Piccolo, Alessandro. Carbon Sequestration in Agricultural Soils: A Multidisciplinary Approach to Innovative Methods. Springer, 2012.

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26

Piccolo, Alessandro. Carbon Sequestration in Agricultural Soils: A Multidisciplinary Approach to Innovative Methods. Springer, 2012.

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27

R, Carter Martin, and Stewart B. A. 1932-, eds. Structure and organic matter storage in agricultural soils. Boca Raton, FL: Lewis Publishers, 1996.

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28

Stewart, Bobby A., and Martin Roger Carter. Structure and Organic Matter Storage in Agricultural Soils (Advances in Soil Science). CRC, 1995.

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29

Literature review and research scoping study on the treatment of volatile organic carbon compounds in the off-gas from contaminated groundwater and soil remedial technologies. Burlington, ON: Burlington Environmental Technology Office, Canada Centre for Inland Waters, 1991.

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30

Hazelton, Pam, and Brian Murphy. Interpreting Soil Test Results. CSIRO Publishing, 2016. http://dx.doi.org/10.1071/9781486303977.

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Interpreting Soil Test Results is a practical reference enabling soil scientists, environmental scientists, environmental engineers, land holders and others involved in land management to better understand a range of soil test methods and interpret the results of these tests. It also contains a comprehensive description of the soil properties relevant to many environmental and natural land resource issues and investigations. This new edition has an additional chapter on soil organic carbon store estimation and an extension of the chapter on soil contamination. It also includes sampling guidelines for landscape design and a section on trace elements. The book updates and expands sections covering acid sulfate soil, procedures for sampling soils, levels of nutrients present in farm products, soil sodicity, salinity and rainfall erosivity. It includes updated interpretations for phosphorus in soils, soil pH and the cation exchange capacity of soils. Interpreting Soil Test Results is ideal reading for students of soil science and environmental science and environmental engineering; professional soil scientists, environmental scientists, engineers and consultants; and local government agencies and as a reference by solicitors and barristers for land and environment cases.
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31

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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32

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 quantity in an increasingly competitive world market. The promotion of organic and biodynamic practices has raised a general awareness of "soil health", which is often associated with a soil's biology, but which to be properly assessed must be focused on a soil's physical, chemical, and biological properties. This edition of White's influential book presents the latest updates on these and other developments in soil management in vineyards. With a minimum of scientific jargon, Understanding Vineyard Soils explains the interaction between soils on a variety of parent materials around the world and grapevine growth and wine typicity. The essential chemical and physical processes involving nutrients, water, oxygen and carbon dioxide, moderated by the activities of soil organisms, are discussed. Methods are proposed for alleviating adverse conditions such as soil acidity, sodicity, compaction, poor drainage, and salinity. The pros and cons of organic viticulture are debated, as are the possible effects of climate change. The author explains how sustainable wine production requires winegrowers to take care of the soil and minimize their impact on the environment. This book is a practical guide for winegrowers and the lay reader who is seeking general information about soils, but who may also wish to pursue in more depth the influence of different soil types on vine performance and wine character.
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33

Kirchman, David L. Elements, biochemicals, and structures of microbes. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0002.

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Microbiologists focus on the basic biochemical make-up of microbes, such as relative amounts of protein, RNA, and DNA in cells, while ecologists and biogeochemists use elemental ratios, most notably, the ratio of carbon to nitrogen (C:N), to explore biogeochemical processes and to connect up the carbon cycle with the cycle of other elements. Microbial ecologists make use of both types of data and approaches. This chapter combines both and reviews all things, from elements to macromolecular structures, that make up bacteria and other microbes. The most commonly used elemental ratio was discovered by Alfred Redfield who concluded that microbes have a huge impact on the chemistry of the oceans because of the similarity in nitrogen-to-phosphorus ratios for organisms and nitrate-to-phosphate ratios in the deep oceans. Although statistically different, the C:N ratios in soil microbes are remarkably similar to the ratios of aquatic microbes. The chapter moves on to discussing the macromolecular composition of bacteria and other microbes. This composition gives insights into the growth state of microbes in nature. Geochemists use specific compounds, “biomarkers”, to trace sources of organic material in ecosystems. The last section of the chapter is a review of extracellular polymers, pili, and flagella, which serve a variety of functions, from propelling microbes around to keeping them stuck in one place.
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34

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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