U.S. scientists working on a research vessel in the Gulf of Mexico have made the most promising discovery so far of
marine gas hydrate, a possible new energy source.
Our results stress the importance of external climatic forcing of the dynamics of the seafloor, and the role of the rapid warming following the Younger Dryas in pacing
the marine gas hydrate reservoir.
Knowledge of the timescales of gas hydrate dissociation and subsequent methane release are critical in understanding the impact of
marine gas hydrates on the ocean — atmosphere system, says Shyam Chand, researcher at NGU / CAGE.
Not exact matches
«You build up too much free
gas, and then you have an overpressured column,» says Gerald Dickens, a
marine geochemist at Rice University who went to
Hydrate Ridge on a drill ship in 2002.
Given the vastness of the world's
marine methane
hydrate deposits — more than twice the carbon reserves of all other fossil fuels combined — it's not surprising that government agencies and the petroleum and natural
gas industries have long been interested in harvesting this new energy supply.
He is
marine geologist at the Geological Survey of Norway (NGU) and Centre for Arctic
Gas Hydrate, Climate and Environment, UiT The Arctic Univeristy of Norway.
In the greater NZ region, we have undersea hot springs (hydrothermal vents of the Kermadecs),
marine hydrocarbon seeps and
gas hydrates (offshore eastern North Island — possible analogues for oceans on Icy Worlds), and terrestrial (on land) hot springs in the Taupo Volcanic Zone and elsewhere around the country.
# 33 — Gavin, one of the papers cited by Shakhova is
Gas and Possible
Gas Hydrates in the Permafrost of Bovanenkovo Gas Field, Yamal Peninsula, West Siberia by Evgeny M.Chuvilin, Vladimir S.Yakushev and Elena V.Perlova, Polarforschung 68: 215 — 219, 1998 (erschienen 2000) shows marine hydrates at depths of 60m
Hydrates in the Permafrost of Bovanenkovo
Gas Field, Yamal Peninsula, West Siberia by Evgeny M.Chuvilin, Vladimir S.Yakushev and Elena V.Perlova, Polarforschung 68: 215 — 219, 1998 (erschienen 2000) shows
marine hydrates at depths of 60m
hydrates at depths of 60m to 120m.
Warming destabilises permafrost and
marine sediments of methane
gas hydrates in some regions according to some model simulations (Denman et al., 2007 Section 7.4.1.2), as has been proposed as an explanation for the rapid warming that occurred during the Palaeocene / Eocene thermal maximum (Dickens, 2001; Archer and Buffett, 2005).
When
hydrates are present below permafrost, on land and beneath shallow
marine shelves, they are also thermally buffered by the latent heat energy needed to melt the permafrost and it could take thousands of years to destabilize the
gas hydrates (Taylor et al 2005).
The project at the University of Texas at Austin will develop conceptual and numerical models to analyze conditions under which
gas will be expelled from existing
marine accumulations of
gas hydrate into the ocean, which could potentially have a damaging effect to the ecosystem.