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    John Wiley & Sons
    In:  In: Gas Hydrates 2: Geoscience Issues and Potential Industrial Applications. , ed. by Ruffine, L., Broseta, D. and Desmedt, A. John Wiley & Sons, Newark, pp. 121-164.
    Publication Date: 2018-05-04
    Description: This chapter talks about physicochemical properties of gas hydrate‐bearing sediments. Lab‐based experiments are the most cost‐effective and systematic approach to evaluate physicochemical properties and behavior of gas hydrate‐bearing sediments in a systematic way. Physicochemical property studies were largely focused on measurements with respect to homogeneous and reproducible gas hydrate distributions. The chapter includes overviews of thermodynamic and kinetic constraints of relevant processes of gas hydrate formation, dissociation and conversion, fluid transport in gas hydrate‐bearing sediments, thermal and electrical properties and distribution of gas hydrates. It reviews some flow‐through experimental systems and procedures for studying the behavior of gas hydrate‐bearing sediments with different research objectives. The chapter provides a brief overview on available systems for high‐resolution online fluid monitoring, as well as tools for a destruction‐free analysis of the multiphase sample with emphasis on tomographic techniques.
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 2
    Publication Date: 2023-02-08
    Description: The fate of plastic debris entering the oceans is largely unconstrained. Currently, intensified research is devoted to the abiotic and microbial degradation of plastic floating near the ocean surface for an extended period of time. In contrast, the impacts of environmental conditions in the deep sea on polymer properties and rigidity are virtually unknown. Here, we present unique results of plastic items identified to have been introduced into deep-sea sediments at a water depth of 4150 m in the eastern equatorial Pacific Ocean more than two decades ago. The results, including optical, spectroscopic, physical and microbial analyses, clearly demonstrate that the bulk polymer materials show no apparent sign of physical or chemical degradation. Solely the polymer surface layers showed reduced hydrophobicity, presumably caused by microbial colonization. The bacterial community present on the plastic items differed significantly (p 〈 0.1%) from those of the adjacent natural environment by a dominant presence of groups requiring steep redox gradients (Mesorhizobium, Sulfurimonas) and a remarkable decrease in diversity. The establishment of chemical gradients across the polymer surfaces presumably caused these conditions. Our findings suggest that plastic is stable over extended times under deep-sea conditions and that prolonged deposition of polymer items at the seafloor may induce local oxygen depletion at the sediment-water interface.
    Type: Article , PeerReviewed
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