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Books on the topic 'Dissolved organic carbon'

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Author: Grafiati

Published: 4 June 2021

Last updated: 1 June 2024

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1

Cussion, Sylvia. Dissolved organic carbon and total organic carbon in reagent water and effluent: Report. [Toronto]: Quality Management Office, Laboratory Services Branch, Ontario Ministry of the Environment, 1992.

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2

Knocke, William R. Impacts of dissolved organic carbon on iron removal. Denver, CO: The Foundation and American Water Works Association, 1993.

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3

LaZerte, Bruce. Metal transport and retention: The role of dissolved organic carbon. [Toronto]: Queen's Printer for Ontario, 1991.

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4

Lazerte, Bruce D. Metal transport and retention: The role of dissolved organic carbon. Toronto, Ont: Ministry of the Environment, 1991.

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5

Reilly, Timothy J. Dissolved pesticides, dissolved organic carbon, and water-quality characteristics in selected Idaho streams, April-December 2010. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2012.

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6

Sturman, Paul John. Control of acid rock drainage from mine tailings through the addition of dissolved organic carbon. Bozeman, MT: Montana State University, 2004.

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7

Salley, Betty A. Comparison study of five instruments measuring dissolved organic carbon for the Chespeake [sic] Bay Monitoring Program. Gloucester Point, Va: Virginia Institute of Marine Science, School of Marine Science, College of William and Mary, 1995.

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8

McCall, Jackie Kendal. Relationships among yellow substance, dissolved organic carbon, pH, and transparency in acidic lakes near Sudbury, Ontario. Sudbury, Ont: Laurentian University, Department of Geography, 1994.

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9

Beauclerc, Kaela B. The influence of dissolved organic carbon on the absorbance of ultraviolet light in Northern Ontario lakes. Sudbury, Ont: Laurentian University, Department of Biology, 2000.

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10

Goldstone, Jared Verrill. Direct and indirect photoreactions of chromophoric dissolved organic matter: Roles of reactive oxygen species and iron. Cambridge, Mass: Massachusetts Institute of Technology, 2002.

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11

Wetz, Jennifer Jarrell. Particulate and dissolved organic carbon and nitrogen data from the GLOBEC long-term observation program, 1997-2004. Corvallis, Or: College of Oceanic and Atmospheric Sciences, Oregon State University, 2006.

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12

1946-, Richey Jeffrey Edward, and United States. National Aeronautics and Space Administration., eds. Oxidation and reduction rates for organic carbon in the Amazon mainstream tributary and floodplain, inferred from distributions of dissolved gases. [Washington, D.C: National Aeronautics and Space Administration, 1986.

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13

R, Garbarino J., and Geological Survey (U.S.), eds. Concentration and transport data for selected dissolved inorganic constituents and dissolved organic carbon in water collected from the Mississippi River and some of its tributaries, July 1991-May 1992. Denver, Colo: U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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14

Wetz, Jennifer Jarrell. Pump station data report for the May 2001, August 2001 and January 2003 COAST cruises: Nutrients, extracted chlorophyll, and dissolved and particulate organic carbon and nitrogen. Corvallis, Or: College of Oceanic and Atmospheric Sciences, Oregon State University, 2005.

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15

Speiran, Gary K. Dissolved organic carbon and disinfection by-product precursors in waters of the Chickahominy River basin, Virginia, and implications for public supply. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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16

Speiran, Gary K. Dissolved organic carbon and disinfection by-product precursors in waters of the Chickahominy River basin, Virginia, and implications for public supply. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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17

NSF/NOAA/DOE Workshop (1991 Seattle, U.S.). Measurement of dissolved organic carbon and nitrogen in natural waters: Proceedings of NSF/NOAA/DOE Workshop, Seattle, WA, USA, 15-19 July 1991. Amsterdam: Elsevier, 1993.

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18

Boerschke, Roy Carl. Quantitive isolation and characterization of freshwater dissolved organic carbon and the influence of pH and A1 on the absorption spectra of the isolated humic material. Sudbury, Ont: Laurentian University Press, 1996.

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19

Roger, Fujii, California. Dept. of Water Resources, and Geological Survey (U.S.), eds. Dissolved organic carbon concentrations and compositions, and trihalomethane formation potentials in waters from agricultural peat soils, Sacramento-San Joaquin Delta, California: Implications for drinking-water quality. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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20

Roger, Fujii, California. Dept. of Water Resources., and Geological Survey (U.S.), eds. Dissolved organic carbon concentrations and compositions, and trihalomethane formation potentials in waters from agricultural peat soils, Sacramento-San Joaquin Delta, California: Implications for drinking-water quality. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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21

Miller, Ronald L. Water quality in the southern Everglades and Big Cypress Swamp in the vicinity of the Tamiami Trail, 1996-97. [Reston, Va.?]: Dept. of the Interior, U.S. Geological Survey, 1999.

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22

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

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23

Brophy, Jennifer Elaine. Production of biologically-refractory dissolved organic carbon by natural seawater microbial populations. 1986.

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24

Kawasaki, Nobuyuki. The release of total and dissolved organic carbon from macroalgae and phytoplankton. 1999.

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25

Hill, Jon K. The distribution and partitioning of dissolved organic matter off the Oregon Coast: A first look. 1999.

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26

Evans, Hayla Ellen *. The effects of dissolved organic carbon on the behaviour of PCBs in fresh waters. 1991.

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27

Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory: Determination of dissolved organic carbon by UV-promoted persulfate oxidation and infrared spectrometry. Denver, Colo: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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28

Abd-Elrahman, Shaimaa Hassan. Remediation of some degraded soils using new techniques: Chemical remediation/Salt-affected soil/Heavy metals/Fractionation/Dissolved organic carbon/Wheat plants/Lettuce plants. Scholars' Press, 2013.

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29

Robinson, Carol. Phytoplankton Biogeochemical Cycles. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199233267.003.0005.

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This chapter describes how the activity of phytoplankton, bacteria, and Archaea drive the marine biogeochemical cycles of carbon, nitrogen, and phosphorus, and how climate driven changes in plankton abundance and community composition influence these biogeochemical cycles in the North Atlantic Ocean and adjacent seas. Carbon, nitrogen, and phosphorus are essential elements required for all life on Earth. In the marine environment, dissolved inorganic carbon, nitrogen, and phosphorus are utilized during phytoplankton growth to form organic material, which is respired and remineralized back to inorganic forms by the activity of bacteria, Archaea, and zooplankton. The net result of the photosynthesis, calcification, and respiration of marine plankton is the uptake of carbon dioxide from the atmosphere, its sequestration to the deep ocean as organic and inorganic carbon, and its availability to fuel all fish and shellfish production.

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30

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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31

Canfield, Donald Eugene. Earth’s Middle Ages: What Came after the GOE. Princeton University Press, 2017. http://dx.doi.org/10.23943/princeton/9780691145020.003.0009.

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This chapter considers the aftermath of the great oxidation event (GOE). It suggests that there was a substantial rise in oxygen defining the GOE, which may, in turn have led to the Lomagundi isotope excursion, which was associated with high rates of organic matter burial and perhaps even higher concentrations of oxygen. This excursion was soon followed by a crash in oxygen to very low levels and a return to banded iron formation deposition. When the massive amounts of organic carbon buried during the excursion were brought into the weathering environment, they would have represented a huge oxygen sink, drawing down levels of atmospheric oxygen. There appeared to be a veritable seesaw in oxygen concentrations, apparently triggered initially by the GOE. The GOE did not produce enough oxygen to oxygenate the oceans. Dissolved iron was removed from the oceans not by reaction with oxygen but rather by reaction with sulfide. Thus, the deep oceans remained anoxic and became rich in sulfide, instead of becoming well oxygenated.

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