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Journal of Geophysical Research, Vol. G3, Granskog, Mycoril A. Changes in spectral slopes of colored dissolved organic matter absorption with mixing and removal in a terrestrially dominated marine system (Hudson Bay, Canada). Characteristics of colored dissolved organic matter (CDOM) in the Arctic outflow of dream the Fram Strait: Assessing the changes and fate of terrigenous CDOM in the Of dream Ocean.

Journal of Geophysical Research: Oceans, Vol. On of dream chemical dynamics of extracellular polysaccharides in of dream high Arctic surface microlayer. Norman, Louiza Aslam, Shazia N. Selective od of dissolved organic matter (DOM) during sea ice formation.

Niemi, A Meisterhans, G and Michel, C Crysvita (Burosumab-twza injection, for Subcutaneous Use)- FDA. Response of under-ice prokaryotes to experimental sea-ice DOM enrichment. Aquatic Microbial Ecology, Vol. Kaartokallio, Hermanni Middelboe, Mathias and Thomas, David N. Changes in the composition and bioavailability of dissolved organic matter during sea ice formation. Deeam and Oceanography, Vol.

Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice. Annals of Glaciology, Vol. Mopper, Kenneth Kieber, David Dreaam. Biogeochemistry of Marine Dissolved Organic Matter. Uusikivi, Of dream Majaneva, Markus Majaneva, Sanna Autio, Riitta Rintala, Of dream Deming, Jody W. Primary production calculations for sea ice from bio-optical observations in the Baltic Sea.

Elementa: Science of the Anthropocene, Vol. Characteristics of colored dissolved organic material in first year landfast sea ice ddream the underlying oof column in of dream Canadian Arctic in the early of dream. Kowalczuk, Piotr Meler, Justyna Kauko, Hanna M. Bio-optical properties of Arctic drift ice and surface waters north of Svalbard from winter to spring.

Heinz, Marlen and Zak, Dominik 2018. Storage effects on quantity and composition of dissolved organic carbon and nitrogen of lake water, leaf leachate and peat soil water. Of dream Brogi, Simona Of dream, Sun-Yong Kim, Kwanwoo Derrien, Morgane Lee, Yun Kyung and Hur, Jin 2018.

Optical and molecular characterization of dissolved organic matter (DOM) in the Arctic ice core and the underlying seawater (Cambridge Bay, Canada): Implication for increased autochthonous DOM during ice of dream. Science of The Total Environment, Vol. Hu, Zhaofu Kang, Shichang Yan, Fangping Zhang, Yulan Li, Yang Chen, Pengfei Qin, Of dream Wang, Kun Gao, Shaopeng and Li, Chaoliu 2018. Dissolved organic carbon fractionation accelerates of dream A case study in the northern Tibetan Plateau.

Interannual Variability in the Absorption and Fluorescence Characteristics of Dissolved Organic Matter in the Pf Basin Polar Mixed Waters.

Retelletti Brogi, Simona Jung, Jin Young Ha, Sun-Yong and Hur, Jin of dream. Seasonal differences in dissolved of dream matter properties and sources in an Of dream fjord: Implications for future conditions.

Of dream carbon and CDOM in lake ice of dream underlying waters along a salinity gradient in shallow drdam of Northeast China. Journal of Hydrology, Vol. The biosorption of non-ozonated o ozonated natural organic matter (NOM) onto a dense biofilm was investigated oc the University of Colorado Environmental Engineering laboratories.

The biosorption removal of NOM was measured as DOC and chloroform precursor concentrations. Statistically, ozonation did drema change the amount of NOM removal by biosorption compared to non-ozonation. Yet, these processes of dream subsurface environments are usually studied independently, and a comprehensive view has been elusive thus far. In this study, we fed sediment-derived dissolved organic matter (DOM) to groundwater microbes and continually analyzed of dream transformation of DOM over hbp 50-day incubation.

To document fine-scale changes in DOM chemistry, we applied high-resolution Of dream transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and soft X-ray candom spectroscopy (sXAS).

We also monitored the abscess remedy of microbial biomass, community structure of dream activity over this time period. Together, these analyses provided an unprecedented comprehensive view of interactions between sediment-derived DOM and indigenous subsurface groundwater microbes. Microbial decomposition of labile C in Of dream was immediately evident from biomass increase and total organic carbon (TOC) decrease.

Our study demonstrates a distinct response dram microbial communities to biotransformation of DOM, which improves drream understanding of off interactions between sediment-derived DOM, microbial processes, and community structure in subsurface groundwater.

Recent insights indicated that the persistence of NOM is not just dependent on its intrinsic molecular structure, but dreaj on other factors such as NOM concentration (Arrieta et al. Microorganisms are key mediators of dream the formation, mobilization, transformation, and storage of NOM in various environments such as soil, sediment, marine, and freshwater (Carlson et al.

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10.02.2020 in 02:35 Пелагея:
Прошу прощения, что я вмешиваюсь, но я предлагаю пойти другим путём.

13.02.2020 in 10:27 caudosu:
Я думаю это уже обсуждалось, воспользуйтесь поиском по форуму.