Duofu Chen

ORCID: 0000-0001-9519-5311
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About
Contact & Profiles
Research Areas
  • Methane Hydrates and Related Phenomena
  • Hydrocarbon exploration and reservoir analysis
  • Geology and Paleoclimatology Research
  • Atmospheric and Environmental Gas Dynamics
  • Geological and Geophysical Studies
  • Geochemistry and Elemental Analysis
  • Paleontology and Stratigraphy of Fossils
  • CO2 Sequestration and Geologic Interactions
  • Geological and Geochemical Analysis
  • Microbial Community Ecology and Physiology
  • Marine and coastal ecosystems
  • Marine Biology and Ecology Research
  • Geological formations and processes
  • earthquake and tectonic studies
  • Mercury impact and mitigation studies
  • Geological Studies and Exploration
  • Arctic and Antarctic ice dynamics
  • Geochemistry and Geologic Mapping
  • Spacecraft and Cryogenic Technologies
  • Isotope Analysis in Ecology
  • Offshore Engineering and Technologies
  • Toxic Organic Pollutants Impact
  • Underwater Vehicles and Communication Systems
  • Heavy metals in environment
  • Oil Spill Detection and Mitigation

Shanghai Ocean University
2016-2025

Qingdao National Laboratory for Marine Science and Technology
2017-2025

College of Marin
2023

University of Chinese Academy of Sciences
2008-2022

Chinese Academy of Sciences
2011-2021

Guangzhou Institute of Geochemistry
2011-2021

Institute of Oceanology
2004-2017

South China Sea Institute Of Oceanology
2004-2017

Second Institute of Oceanography
2017

Institute of Deep-Sea Science and Engineering
2014

Abstract Sulfate-driven anaerobic oxidation of methane (SD-AOM) supports chemosynthesis-based communities and limits the release from marine sediments. Formation authigenic carbonates at active seeps is promoted by SD-AOM stoichiometry. While distinctively small δ18O/δ34S slopes pore fluid sulfate have been shown to typify modern methane-rich environments, identification such environments has difficult for geological past due lack sedimentary fluids. However, if isotopic composition were...

10.1130/g38233.1 article EN cc-by Geology 2016-10-08

Abstract Marine hydrocarbon seeps are dynamic systems, which typically reflected in complex lithologies of limestones forming at these sites. In order to test if seep with their multiple generations carbonate phases reflect variable redox conditions, the rare earth element (REE) patterns from five ancient hydrocarbon‐seep localities, Hollard Mound (Middle Devonian), Iberg (Mississippian), Beauvoisin (Oxfordian), Canyon and Satsop River (Oligocene), Marmorito (Miocene) have been investigated....

10.1111/j.1365-3121.2008.00855.x article EN Terra Nova 2008-12-19

Abstract Hadal trenches have been proposed as depocenters of organic material and hot spots for matter mineralization. In this study, we the first time quantified total benthic O 2 uptake in hadal using situ chamber incubations. Three tropical Pacific were targeted exhibited relatively high diagenetic activity given great water depths, that is, Mariana Trench (2.0 × 10 μmol m −2 d −1 , 10,853 m), Mussau (2.7 ± 0.1 7,011 New Britain (6.0 8,225 m). Combined with analyses carbon δ 13 C...

10.1002/2017gl076232 article EN Geophysical Research Letters 2018-03-15

Abstract Gas hydrates represent a huge reservoir of methane in marine sediments, prone to dissociation response environmental changes. There is consensus that past events gas hydrate the environment mainly occurred during periods low sea level. Here, we report geochemical data for 2‐m‐thick layers seep carbonate collected from hydrate‐bearing drill core ~800‐m water depth northern South China Sea. The aragonite‐rich carbonates reveal positive δ 18 O values, confirming genetic link with...

10.1029/2019gl085643 article EN Geophysical Research Letters 2019-11-26

By employing a specific particle interaction theory and high-precision equation of states for the liquid vapor phases H2, respectively, new H2 solubility model in pure water aqueous NaCl solutions is proposed this study. The established by fitting experimental data can be used to estimate at temperatures pressures 273.15–423.15 K 0–1100 bar, salt (NaCl concentration = 0–5 mol/kg) 273.15–373.15 0–230 respectively. adopting electrolyte solutions, also predict seawater without system. Within or...

10.3390/en15145021 article EN cc-by Energies 2022-07-09

After nearly 20 years of exploration, various areas the seafloor with hydrocarbon seepage have been discovered in South China Sea (SCS). Through linking subsurface and biospheres, seeps become natural laboratories to enhance our knowledge on processes migration associated hydrocarbon-based ecosystems marine environment. This review summarizes distribution macrofauna active seep SCS describes physiological characteristics three groups representative (bathymodioline mussels, pliocardiine...

10.1016/j.geogeo.2022.100081 article EN cc-by Geosystems and Geoenvironment 2022-05-19
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