Temporal changes in photoreactivity of dissolved organic carbon and implications for aquatic carbon fluxes from peatlands

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Temporal changes in photoreactivity of dissolved organic carbon and implications for aquatic carbon fluxes from peatlands

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wetenschappelijk artikel

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наукова стаття, опублікована у квітні 2017

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Temporal changes in photoreact ...... c carbon fluxes from peatlands

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Temporal changes in photoreact ...... c carbon fluxes from peatlands

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Temporal changes in photoreact ...... c carbon fluxes from peatlands

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Temporal changes in photoreact ...... c carbon fluxes from peatlands

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Temporal changes in photoreact ...... c carbon fluxes from peatlands

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Temporal changes in photoreact ...... c carbon fluxes from peatlands

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P1476

Temporal changes in photoreact ...... c carbon fluxes from peatlands

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P2093

Amy E. Pickard

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Andrew R. McLeod

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Kate V. Heal

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Kerry J. Dinsmore

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P2860

Temperature and precipitation drive temporal variability in aquatic carbon and GHG concentrations and fluxes in a peatland catchment.

Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon.

Annual patterns in bacterioplankton community variability in a humic lake.

Ultraviolet radiation drives methane emissions from terrestrial plant pectins.

The wavelengths in sunlight effective in producing skin cancer: a theoretical analysis.

Carbon cycle. Sunlight controls water column processing of carbon in arctic fresh waters.

Spatial variability overwhelms seasonal patterns in bacterioplankton communities across a river to ocean gradient.

Increases in terrestrially derived carbon stimulate organic carbon processing and CO₂ emissions in boreal aquatic ecosystems.

Fluorescence spectroscopy reveals ubiquitous presence of oxidized and reduced quinones in dissolved organic matter.

Link between DOC in near surface peat and stream water in an upland catchment.

P304

1793-1809

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P31

scholarly article

P356

10.5194/BG-14-1793-2017

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P433

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P478

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P577

2017-04-04T00:00:00Z

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