Boulder, Colo., USA: Cretaceous climate warming led to a significant methane release from the seafloor, indicating potential for similar destabilization of
gas hydrates under modern global warming.
Gargantuan stores of
gas hydrates under the oceans and permafrost regions of the globe have many scientists wondering whether they can find an economically feasible way to unlock the methane, creating a natural gas supply that could last for centuries.
Not exact matches
Naturally - occurring methane
hydrates, hidden deep
under the sea floor or tucked
under Arctic permafrost, contain substantial natural
gas reserves locked up in a form that is difficult to extract.
The Arctic ocean floor hosts vast amounts of methane trapped as
hydrates, which are ice - like, solid mixtures of
gas and water.These
hydrates are stable
under high pressure and cold temperatures.
When methane
hydrates «melt,» they release the methane trapped inside the ice, but because the methane was first trapped
under pressure when the
hydrate was formed, one cubic metre of solid methane
hydrate will release 160 cubic metres of methane
gas.
Under most frozen
hydrate deposits is a layer of free methane
gas occupying the pore spaces in the sediment.
Under some parts of
Hydrate Ridge there is so much methane gas, says German geologist Gerhard Bohrman, that it is constantly bubbling up into the hydrat
Hydrate Ridge there is so much methane
gas, says German geologist Gerhard Bohrman, that it is constantly bubbling up into the
hydratehydrate zone.
Gas hydrates — a mixture of ice and methane — are found only
under high pressure and at cold temperatures, and they are expected to make up a significant portion of the energy mix once existing oil fields dwindle, says David Scott, manager of the Northern Resources Development Program for Natural Resources Canada.
methane
hydrate Molecules of methane
gas trapped — and compressed
under pressure — within a lattice of water ice.
Nor do we adequately understand the relative contributions of microbes (i.e., biogenic methanogenesis), fossil sources, and the dissociation of
gas hydrates (an ice - like substance formed by methane and water
under pressure).
Moreover, as if discovering methane emissions from the deep seas of the Arctic isn't already of major concern, a recent study discovered immense amounts of methane locked
under Antarctic ice: «They... calculated that the potential amount of methane
hydrate and free methane
gas beneath the Antarctic Ice Sheet could be up to 4 billion metric tons, a similar order of magnitude to some estimates made for Arctic permafrost.
But
under permafrost the
gas hydrate may stay stable even where the pressure is not that high, because of the constantly low temperatures.»
Methane release from stores of so - called
gas hydrates, that can form on land or
under the sea, is not new to researchers.
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.
The USGS, which announced the discovery, estimates there is about 700,000 tcf of
gas hydrate worldwide, most of it below the ocean floors, where
hydrates form
under high pressure and cold temperatures.
Methane
hydrates are 3D ice - lattice structures with natural
gas locked inside, and are found both onshore and offshore — including
under the Arctic permafrost and in ocean sediments along nearly every continental shelf in the world.