Not exact matches
Gas hydrates naturally form along the coasts of continents and in Arctic permafrost, places where water and gas mix at relatively high pressure and low temperatu
Gas hydrates naturally
form along the coasts of continents and in Arctic permafrost, places where water and
gas mix at relatively high pressure and low temperatu
gas mix at relatively high pressure and low temperature.
«If the decomposition of the methane
hydrate phase is fast enough, which depends on temperature, the methane
gas in the aqueous phase
forms nanobubbles,» said Saman Alavi, one of the lead researchers on the project.
«The
gas hydrate pingos in permafrost are
formed because of the low temperatures.
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.
A crew of a dozen sailors, a geophysics professor, and two graduate students, we were combing the ocean floor for buried methane
hydrate, an ice - like
form of natural
gas estimated to be more abundant than fossil fuels.
The key ingredient is
gas hydrate, a substance that
forms when hydrocarbon
gases like methane and ethane come into contact with water at the right temperature and pressure.
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.
Permafrost was known to contain
gas hydrates — icelike mixtures of water and organic
gases first identified in deep - sea sediments which
form only at very high pressures and low temperatures.
The
gas - phase results are consistent with the spontaneous hydrolysis of PaO2 + in aqueous solution, this in contrast to heavier actinide dioxides of uranium, neptunium, and plutonium; the heavier actinide dioxides
form stable
hydrates in both solution and
gas phase.
However, if the seafloor is already saturated with
gas and the process takes place very quickly, the released
gases make their way to the seafloor, without
forming new
hydrates,» says Dr. Karstens.
«You release a
hydrate and then
form a
hydrate, which is pretty cool,» he says, especially given that methane
gas hydrates represent the most abundant global natural carbon resource.
Gas clathrate hydrates are ice - like solids, in which gas molecules or atoms are trapped inside crystalline frameworks formed by water molecul
Gas clathrate
hydrates are ice - like solids, in which
gas molecules or atoms are trapped inside crystalline frameworks formed by water molecul
gas molecules or atoms are trapped inside crystalline frameworks
formed by water molecules.
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).
The most likely explanation is the mass release of methane from sediments on the sea floor, where the
gas was sequestered, as it is now, in a solid
form as methane
hydrate.
In one study, Mao and colleagues subjected a mixture of hydrogen and water to a pressure of about 220 megapascals (2,000 times atmospheric pressure) at room temperature (300 K or 80 °F), which
formed a clathrate
hydrate — a cage - like framework of water molecules enclosing molecules of
gas.
Basically, free
gas co-exists with
gas hydrate and a brine, and no additional
gas hydrate can
form, because the pore water is too salty.
In Siberian permafrost, large deposits of methane
gas are trapped in ice,
forming what is called a
gas hydrate.
The lakes may also be storing large volumes of the potent greenhouse
gas methane, frozen in a
form called methane
hydrates.
Ice sheets are heavy and cold, providing pressure and temperatures that contain methane in
form of ice - like substance called
gas hydrate.
Methane release from stores of so - called
gas hydrates, that can
form on land or under the sea, is not new to researchers.
Researchers at Southern Methodist University will conduct numerical modeling, field data collection, and extensive laboratory analyses to characterize the state of the upper boundary of pressures and temperatures where
gas hydrates are in a stable
form on the Alaskan Beaufort continental slope.
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.
Globally,
gas hydrate — an icelike substance
formed mainly of methane and water — is thought to be more abundant than oil, coal and conventional natural
gas combined.
R&D ers have been talking up natural
gas extraction from methane
hydrates — a solid
form of the greenhouse
gas, found tucked away beneath the sea floor where low temperature and high pressure keep it stable.
Scientists from the Center for Arctic
Gas Hydrate (CAGE), Environment and Climate at the Arctic University of Norway, published a study in June 2017, describing over a hundred ocean sediment craters, some 3,000 meters wide and up to 300 meters deep,
formed due to explosive eruptions, attributed to destabilizing methane
hydrates, following ice - sheet retreat during the last glacial period, around 12,000 years ago, a few centuries after the Bølling - Allerød warming.
[9] However, it is also thought that fresh water used in the pressurization of oil and
gas wells in permafrost and along the continental shelves worldwide combines with natural methane to
form clathrate at depth and pressure, since methane
hydrates are more stable in fresh water than in salt water.
Improvements in our understanding of clathrate chemistry and sedimentology have revealed that
hydrates form in only a narrow range of depths (continental shelves), at only some locations in the range of depths where they could occur (10 - 30 % of the
Gas hydrate stability zone), and typically are found at low concentrations (0.9 — 1.5 % by volume) at sites where they do occur.
Methane
hydrates are believed to
form by migration of
gas from deep along geological faults, followed by precipitation or crystallization, on contact of the rising
gas stream with cold sea water.
Hydrates normally exclude the salt in the pore fluid from which it forms, thus they exhibit high electric resistivity just like ice, and sediments containing hydrates have a higher resistivity compared to sediments without gas hydrates (Judge [6
Hydrates normally exclude the salt in the pore fluid from which it
forms, thus they exhibit high electric resistivity just like ice, and sediments containing
hydrates have a higher resistivity compared to sediments without gas hydrates (Judge [6
hydrates have a higher resistivity compared to sediments without
gas hydrates (Judge [6
hydrates (Judge [67]-RRB-.
The extra pressure from the glacier could have allowed a regional layer of
gas hydrate to
form at about 100 meters depth.
Government support will prioritize research into five types of renewables and energy
forms: biomass fuels and biomass power, wind power, solar power, hydrogen energy and fuel cells, and natural
gas hydrates, of which there is a large reserve in the South China Sea and which China recently succeeded in tapping.
Hydrates can
form with almost any
gas and consist of a «cage» of water molecules surrounding the
gas.