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Aquatic sources

Fatty acid esters. Fatty acid esters (FESs) are readily degraded in aerobic environments [120], by co- and (3-oxidation steps, followed by desulfonation [122], such that extensive mineralisation has been described. Persistence from aquatic sources can only be envisaged in cases where adsorption leads to removal of the surfactant from the aerobic conditions, with anaerobic degradation not observed in any studies described to date [122]. Aerobic degradation in sludge-amended soils has, however, been described as rapid [122]. [Pg.585]

At present, soil derived humic matter and fulvic acids extracted from freshwater are available commercially and are commonly used to test techniques for DOM detection and also used as model compounds for trace metal chelation studies. The results obtained using these model compounds are frequently extrapolated to the natural environment and measurements on "real" samples provide evidence that this DOM is a good model compound. In the past, some investigators also made available organic matter isolated from marine environments using C18 resins. While these compounds come from aquatic sources, this isolation technique is chemically selective and isolates only a small percentage of oceanic DOM. Reference materials are not currently available for these compounds, which inhibits study of the role they play in a variety of oceanographic processes. [Pg.60]

Canuel et al., 1997). This recurring theme of overlapping sterol markers in different organic matter sources indicates that caution should be advised when using sterols solely to distinguish between land and aquatic sources (Volkman, 1986 Jaffe et al., 2001). Instead, biomarker source identifications should be corroborated across lipid compound classes and using bulk and compound-specific isotope analysis. [Pg.250]

Short-chain fatty acids fatty acids thought to be derived from aquatic sources (C12-C18) to others (C44-C18) from multi-sources (zooplankton, bacteria, and benthic animal and marsh plants). [Pg.530]

Cholestane (66a) In aquatic sources probably almost exclusively derived from diverse eukaryotes in organic matter from terrestrial sources (e.g., paleosols) input from soil bacteria of the order Myxococcales conceivable. Volkman (2003), Bode et al. (2003), Kohl et al. (1983)... [Pg.3956]

Aquatic Sources of Halocarbons. One of the main pathways for ie natural formation of halocarbons involves peroxidase enzymes (8, 68-70). hloroperoxidases can catalyze the formation of chlorinated, brominated, and dinated organic compounds bromoperoxidases can produce only the latter co types of halocarbons (8, 69). The Fe-heme peroxidase enzymes, which e activated by hydrogen peroxide and organic peroxides, produce methyl Aides as well as polyhalogenated compounds (Scheme II). [Pg.273]

Compared to the isolation of humic substances from soil or peat, the extraction of reasonable quantities of humic substances from aquatic sources poses severe difficulties due to their very low concentrations in natural waters. However, in recent years significant advances have been made in the technology of isolating humic substances from aquatic environments as discussed by Aiken in Chapter 14. [Pg.4]

These problems were addressed in a paper published by MacCarthy (1976) wherein it was proposed that an international reference collection of humic substances be established. The potential benefits that would result from such a collection were outlined in the paper. That proposal was further promoted by MacCarthy and Malcolm (MacCarthy and Malcolm, 1979 Malcolm and MacCarthy, 1979), and at the Congress of the International Society of Soil Science in 1978 (MacCarthy and Malcolm, 1978) a special working group was formed to examine the possibility of establishing an international standard collection of humic substances. In 1981, an international group of scientists met in Denver, Colorado and formulated a plan for generating a suite of standard humic substances which would be available to researchers worldwide. It was decided to extract and purify humic and fulvic acids from the soil, peat, leonardite, and aquatic sources by a carefully... [Pg.10]

Aquatic humic substances have also been isolated from aquatic sources by DEAE-cellulose chromatography (Miles et al., 1983). [Pg.470]

FIGURE 14. Excitation and emission fluorescence spectra of humic and fulvic acids from various soil and aquatic sources (Plechanov et al., 1983). [Pg.554]

I. 0). The isotopic composition of alkanes and of other classes of compounds can also be used as a general source input indicator. Isotopic fractionation resulting from the metabolic pathways involved in the synthesis of biologically produced compounds, when preserved in a dlagenetlc product, is frequently used to differentiate between terrestrial and aquatic sources. Hydrogen and carbon isotopic compositions of biogenic methanes from shallow aquatic environments is discussed in a later chapter of this volume (R. A. Burke and W. M. Sackett). The applicability of carbon isotopic data to tracing the source of deep-sea Mesozoic sediments is discussed by R.M. Joyce and E. S. Van Vleet. [Pg.3]

Natural products are an indispensable source for novel structures and chemical diversity for drag discovery. Aquatic sources and plant sources are an underutilized source of active principles or lead compounds. [Pg.135]

Elkins JW, Wofsy SC, McElroy MB, Kolb CE, and Kaplan WA (1978) Aquatic sources and sinks for nitrous oxide. Nature 275 602-606. [Pg.481]

Branched-chain acids [in addition to phytol-based acids (this section) and furanoid acids (Section 1.10)] have been identified in a number of aquatic sources. These include monoene acids such as 7-methylhexadec-6 and 7-enoic acids and 5-methyl-tetradec-4-enoic add. Some marine animals have a deposit of lipid in the head (melon), an organ which has been implicated in the echo-locating abilities of these animals. These lipids are rich in isovaleric acid (3-methylbutanoic) and iso acids of more conventional chain length but there is no evidence that... [Pg.16]

A difference between seawater and most other natural aquatic sources is its high ionic strength. This often complicates direct CE analysis. Another serious problem is due to large differences in concentrations between matrix components, such as sodium or chloride, and minor cationic and anionic constituents. One way to solve seawater matrix effects on separation and detection is sample dilution, but compounds present at lower concentrations can be diluted below the detection limits. [Pg.379]

A field quality assurance/quality control (QA/QC) program must ensure the integrity and representativeness of the samples taken from aquatic sources such as surface waters, groundwater, and marine environments. [Pg.4088]

If nonrepresentative samples are collected, and sampling preservation techniques are inadequate, the quantitative results will be invalid. Emphasis must not be placed only on the collection of samples that are appropriately representative of the aquatic source from which they are taken, but also on the... [Pg.4088]

Apart from using objectives to allocate sampling stations, other factors such as size of aquatic source and available resources must enter the selection scheme so that a reasonable degree of optimization can be achieved. Resources may be allocated on the... [Pg.4091]

The appropriate size of samples to be collected for any given parameter will depend on the estimated natural concentration level of that parameter within the aquatic source. The smaller the existing analyte concentration, the larger the volume necessary for obtaining a reasonable measurement (a measurement equal to or greater than the limit of quantification after volume reduction). [Pg.4092]

The fortification of food groups or food products with n-3 PUFA can be accomplished in two ways (1) by feeding animals used in food production with n-3 PUFA from vegetable or aquatic sources to generate eggs, meat, and milk enriched in n-3 PUFA or (2) by adding highly refined odorless fish oils or n-3 plant oils directly, or in a protected microencapsulated form, to the food product. [Pg.249]

Again, ISO 14851 had some predecessors, namely OECD 301C [15] and ISO 9408 [16]. Differences between the latter two procedures and ISO 14851 lie in flexibility of test conditions, source of inoculum and possibility for biomass determination. The test is often named after MITI (the Japanese Ministry of Trade and Environment) because they proposed the test to OECD. The OECD procedure prescribes the need to take inoculum from at least 10 (mostly aquatic) sources and make a mixed inoculum. [Pg.153]


See other pages where Aquatic sources is mentioned: [Pg.333]    [Pg.315]    [Pg.316]    [Pg.45]    [Pg.87]    [Pg.673]    [Pg.10]    [Pg.129]    [Pg.55]    [Pg.653]    [Pg.384]    [Pg.289]    [Pg.385]    [Pg.393]    [Pg.395]    [Pg.4092]    [Pg.1105]    [Pg.218]    [Pg.232]   
See also in sourсe #XX -- [ Pg.273 ]

See also in sourсe #XX -- [ Pg.273 ]




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