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[PDF] Top 20 Chemodiversity of dissolved organic matter in the Amazon Basin

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Chemodiversity of dissolved organic matter in the Amazon Basin

Chemodiversity of dissolved organic matter in the Amazon Basin

... the Amazon Basin have been asso- ciated with specific biogeochemical processes, but a de- tailed chemical classification of the abundant and ubiquitous dissolved organic matter (DOM), ... See full document

12

Chemodiversity of dissolved organic matter in the Amazon Basin

Chemodiversity of dissolved organic matter in the Amazon Basin

... the Amazon Basin have been asso- ciated with specific biogeochemical processes, but a de- tailed chemical classification of the abundant and ubiquitous dissolved organic matter (DOM), ... See full document

14

The chemodiversity of paddy soil dissolved organic matter correlates with microbial community at continental scales

The chemodiversity of paddy soil dissolved organic matter correlates with microbial community at continental scales

... DOM chemodiversity as it en- hances upward movement of ferrous ions and DOM mol- ecules from deep soils, and influences the influx of selective DOM from the surface ... See full document

16

The chemodiversity of paddy soil dissolved organic matter correlates with microbial community at continental scales.

The chemodiversity of paddy soil dissolved organic matter correlates with microbial community at continental scales.

... DOM chemodiversity as it en- hances upward movement of ferrous ions and DOM mol- ecules from deep soils, and influences the influx of selective DOM from the surface ... See full document

17

Organic carbon amendments affect the chemodiversity of soil dissolved organic matter and its associations with soil microbial communities

Organic carbon amendments affect the chemodiversity of soil dissolved organic matter and its associations with soil microbial communities

... 426 Previous research regarding linkages between DOM and BCC has only focused 427 on the effects of the content of soil carbon 12 , the appreciation of their relationships with 428 each other is strikingly limited on the ... See full document

39

Spatial and Seasonal Variability of Dissolved Organic Matter in the Cariaco Basin

Spatial and Seasonal Variability of Dissolved Organic Matter in the Cariaco Basin

... 4.1.2. DON and DOP [ 23 ] DON levels in the upper 250 m of the Cariaco Basin were similar to those measured in other marine settings [Carlson et al., 1994; Guo et al., 1994, 1995; Hansell et al., 1997; Hansell and ... See full document

14

Fluxes of dissolved organic matter from urban catchments in the Neuse River Basin

Fluxes of dissolved organic matter from urban catchments in the Neuse River Basin

... precursor material can help in establishment of effective monitoring programs. DOM sources and concentrations were evaluated in this study using optical analyses (absorbance and fluorescence) and biomarkers (lignin and ... See full document

67

Spatial and seasonal contrasts of sedimentary organic matter in floodplain lakes of the central Amazon basin

Spatial and seasonal contrasts of sedimentary organic matter in floodplain lakes of the central Amazon basin

... crenarchaeol (µg g −1 OC ) 7.8 ± 6.0 26.0 1.2 27 grasses/leaves) or wetland soils might explain the elevated S : V ratio of the SOM. Further information with respect to sources of SOM can be obtained from the GDGT ... See full document

16

Dissolved organic carbon and biodegradable dissolved organic carbon determination in river water of the Strug Basin

Dissolved organic carbon and biodegradable dissolved organic carbon determination in river water of the Strug Basin

... %BDOC recorded by Fellman et al. [19] in three watersheds in Alaska ranged between 7 and 38%. The present study demonstrated that DOC and BDOC concentrations varied depending on season. This was due to both accelerated ... See full document

9

Colored dissolved organic matter dynamics across the shelf-basin interface in the western Arctic Ocean

Colored dissolved organic matter dynamics across the shelf-basin interface in the western Arctic Ocean

... 457 nm) ranged from 0.5 to 3.1 Fl.U. (Figure 7) and showed a maximum between 40 and 200 m water depth (Figures 4 – 7). In transect C, the CDOM maximum was found on the shelf break, whereas in transects A and B in the ... See full document

11

CiteSeerX — inferred concentration of dissolved organic matter

CiteSeerX — inferred concentration of dissolved organic matter

... 3. Results 3.1. Seasonality of DOM, climate and hydrology DOM in the Malse River during 1969–2000 ˇ showed a distinct seasonal pattern with the lowest concentrations (COD ;4 mg l ) during winter y1 periods of freezing ... See full document

10

Iron and humic-type fluorescent dissolved organic matter in the Chukchi Sea and Canada Basin of the western Arctic Ocean

Iron and humic-type fluorescent dissolved organic matter in the Chukchi Sea and Canada Basin of the western Arctic Ocean

... Melling and Lewis, 1982] and interactions with bottom sediments on the shelves [Moore et al., 1983]. The lower halocline layer (lower HL) is found beneath the upper HL and mainly originates from the Atlantic. Mixtures ... See full document

17

FRACTIONATION OF DISSOLVED SOLUTES AND CHROMOPHORIC DISSOLVED ORGANIC MATTER DURING EXPERIMENTAL SEA ICE FORMATION

FRACTIONATION OF DISSOLVED SOLUTES AND CHROMOPHORIC DISSOLVED ORGANIC MATTER DURING EXPERIMENTAL SEA ICE FORMATION

... agree with the in situ fluorescence in Figure 2. Sea ice formation and DOM rejection on shelves is the most likely process explaining the differing estimates of the riverine contribution to freshwater in the Canada ... See full document

39

Shift in the chemical composition of dissolved organic matter in the Congo River network

Shift in the chemical composition of dissolved organic matter in the Congo River network

... River basin (n = 104), Lago Janauacá (a central Amazon floodplain lake, n = 17), the Niger River (n = 19) and the Okavango Delta (n = 17) were added to the dataset to increase the variability in DOM ... See full document

16

CiteSeerX — Dissolved Organic Matter and Sorption to Goethite

CiteSeerX — Dissolved Organic Matter and Sorption to Goethite

... study, organic acids with low pK a values would be expected to be primarily dissociated and therefore less available to protonate potential Lewis acid sites on the goethite sur- ... See full document

10

CiteSeerX — Dissolved organic matter in oceanic waters

CiteSeerX — Dissolved organic matter in oceanic waters

... Sedimentary organic matter is a possible source of the older component in the deep DOC. Bauer and Druffel (1998) found elevated DOC concentrations with a more 14 C-depleted, “older”, signature in the ... See full document

19

A molecular perspective on the ageing of marine dissolved organic matter

A molecular perspective on the ageing of marine dissolved organic matter

... represented by a single elemental formula in the FT-ICR mass spectra is probably not as high as expected for natural organic matter. 3.2 East Atlantic Ocean DOM degradation state The linear correlation ... See full document

21

Terrestrial dissolved organic matter distribution in the North Sea

Terrestrial dissolved organic matter distribution in the North Sea

... The organic frac- tion of this fl ux may be buried, remineralized or ultimately stored in the deep ...restrial organic carbon can pass through the coastal and estuarine filter, a process of unknown ... See full document

18

Decomposition of dissolved organic matter in Arctic and boreal streams

Decomposition of dissolved organic matter in Arctic and boreal streams

... 2012), and DOM in pore water from these soils is highly aromatic (Wickland et al. 2007). Further support for the contribution of DOM from a shallow flowpath during freshet comes from the greater proportion of Component 5 ... See full document

110

Production of chromophoric dissolved organic matter by marine phytoplankton

Production of chromophoric dissolved organic matter by marine phytoplankton

... In all cultures, humic-like and protein-like substances increased during the course of the incubations. Because bacteria were absent, it implies that the increases in DOC and FDOM were exclusively due to phytoplankton ... See full document

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