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Books on the topic 'Color dissolved organic matter'

Author: Grafiati

Published: 4 June 2021

Last updated: 5 February 2022

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1

Salonen, K., T. Kairesalo, and R. I. Jones, eds. Dissolved Organic Matter in Lacustrine Ecosystems: Energy Source and System Regulator. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2474-4.

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2

Caron, François. Dissolved organic matter in low-level waste leachates: First year of activities. AECL, Whiteshell Laboratories, 1994.

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3

Aluwihare, Lihini I. High molecular weight (HMW) dissolved organic matter (DOM) in seawater: Chemical structure, sources and cycling. Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, Joint Program in Oceanography/Applied Ocean Science and Engineering, 1999.

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4

Rosario-Ortiz, Fernando, ed. Advances in the Physicochemical Characterization of Dissolved Organic Matter: Impact on Natural and Engineered Systems. American Chemical Society, 2014. http://dx.doi.org/10.1021/bk-2014-1160.

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5

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

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6

Hansley, Paula L. Garnet dissolution in oxalic acid-- a possible analog for natural etching of garnet by dissolved organic matter. U.S. G.P.O, 1994.

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7

Simister, Claire. An analysis of the impact of "natural" dissolved organic matter on the aqueous speciation of 137Cs in contaminated groundwater. Laurentian University, School of Graduate Studies, 2005.

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8

Hansell, Dennis A., and Craig A. Carlson. Biogeochemistry of Marine Dissolved Organic Matter. Elsevier Science & Technology Books, 2014.

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9

(Editor), Dennis A. Hansell, and Craig A. Carlson (Editor), eds. Biogeochemistry of Marine Dissolved Organic Matter. Academic Press, 2002.

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10

(Editor), Dennis A. Hansell, and Craig A. Carlson (Editor), eds. Biogeochemistry of Marine Dissolved Organic Matter. Academic Press, 2002.

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11

Biogeochemistry of Marine Dissolved Organic Matter. Elsevier, 2002. http://dx.doi.org/10.1016/b978-0-12-323841-2.x5000-3.

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12

Biogeochemistry of Marine Dissolved Organic Matter. Elsevier, 2015. http://dx.doi.org/10.1016/c2012-0-02714-7.

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13

Pokrovsky, Oleg S., and Liudmila Shirokova. Dissolved Organic Matter: Properties, Applications and Behavior. Nova Science Publishers, Incorporated, 2017.

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14

(Editor), Stuart Findlay, and Robert L. Sinsabaugh (Editor), eds. Aquatic Ecosystems: Interactivity of Dissolved Organic Matter (Aquatic Ecology). Academic Press, 2002.

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15

Aquatic Ecosystems: Interactivity of Dissolved Organic Matter (Aquatic Ecology). Academic Press, 2002.

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16

Salonen, K., T. Kairesalo, and R. I. Jones. Dissolved Organic Matter in Lacustrine Ecosystems: Energy Source and System Regulator. Springer, 2012.

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17

K, Salonen, Kairesalo T, and Jones R. I, eds. Dissolved organic matter in lacustrine ecosystems: Energy source and system regulator. Kluwer Academic Publishers, 1992.

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18

Osburn, Christopher L., and Thomas S. Bianchi, eds. Linking Optical and Chemical Properties of Dissolved Organic Matter in Natural Waters. Frontiers Media SA, 2017. http://dx.doi.org/10.3389/978-2-88945-081-7.

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19

Jordan, Ryan Neil. Lead complexation and mobility in the presence of dissolved natural organic matter. 1995.

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20

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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21

Advances in the Physicochemical Characterization of Dissolved Organic Matter: Impact on Natural and Engineered Systems. Oxford University Press, Incorporated, 2015.

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22

Crum, Richard Harold. A non-adsorptive method for the isolation and fractionation of dissolved organic matter from aquatic systems. 1992.

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23

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

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24

W, Brown Christopher, and United States. National Aeronautics and Space Administration., eds. Impact of chromophoric dissolved organic matter on UV inhibition of primary productivity in the sea. National Aeronautics and Space Administration, 1996.

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25

Sjöstedt, Johanna, Jean-Francois Lapierre, Youhei Yamashita, and Federico Baltar, eds. Microbial Utilization and Transformation of Dissolved Organic Matter in Aquatic Environments - from Streams to the Deep Ocean. Frontiers Media SA, 2021. http://dx.doi.org/10.3389/978-2-88971-102-4.

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26

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 ox

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27

Jacobsen, Dean, and Olivier Dangles. Living conditions in high altitude waters. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0003.

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Chapter 3 deals with the abiotic environment in high altitude lakes and streams worldwide. It searches for general patterns in relation to altitude, without overlooking the enormous variability, both temporally as well as at small and large spatial scales. Overall, environmental conditions in high altitude waters may be regarded as harsh. Indeed, certain features such as low temperature, low oxygen pressure, and high ultraviolet radiation (all a direct result of high altitude) as well as transparent and ion-poor waters with low nutrient concentrations are typical of high altitude aquatic syste

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28

Patterson, DJ, and MA Burford. Guide to Protozoa of Marine Aquaculture Ponds. CSIRO Publishing, 2001. http://dx.doi.org/10.1071/9780643101081.

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As well as being a culture environment for fish and crustaceans, an aquaculture pond is a rich and complex ecosystem that is dominated by the microbial community. The community is nourished by food and sunlight, and is made up of algae, bacteria and, importantly, protozoa. Protozoa live by eating other organisms and detritus, or by absorbing soluble organic matter dissolved in the water. Ultimately they affect water quality in aquaculture ponds, including the stability of algal and bacterial communities, and nutrient concentrations. In addition, some protozoa can have adverse effects on the he

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