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).
Not exact matches
It is entirely possible that a random triggering event or series of events (lightning or some
form of electricity charging a primordial soup of
methane, ammonia, etc.; bombardment
by cosmic radiation and other hypothetically random occurrences) was the occasion through which a whole new dimension, that of the biosphere, flooded onto the terrestrial scene.
Before the
methane storage project was approved
by the Federal Energy Regulatory Commission in October 2014, hundreds of citizens tried every possible legal means to prevent the expansion of fracked gas storage at Seneca Lake, a source of drinking water for 100,000 people and to object to a
form of industrialization that places us in harm's way.
The Methods: Photochemical modeling
by a Caltech team indicates that ethane, a hydrocarbon detected on Titan
by both of the Voyager spacecraft and the European Infrared Space Observatory, is created when solar ultraviolet light breaks down
methane, a minor component of Titan's nitrogen - rich atmosphere, into a stew of organic molecules that
form a dense orange - brown smog.
Most carbon emissions linked to human activity are in the
form of carbon dioxide gas (CO2), but other
forms of carbon include the
methane gas (CH4) and the particles generated
by such fires — the tiny bits of soot, called black carbon, and motes of associated substances known as brown carbon.
Because they
form by leakage of
methane into seawater it implies that something at that time caused a large release of
methane into the ocean.
Chemical analyses revealed that this was a carbonate rock
formed by the oxidation of
methane, and the spaghetti texture was
formed by fossil tube worms.
Scientists can determine ancient atmospheric concentrations
by measuring CO2 and
methane levels in tiny air bubbles trapped in such ice,
formed when the ice fell to the earth as snow.
Natural
methane hydrates were first discovered
by Russian scientists in the late 1960s in Siberian permafrost — where the ground is so cold that hydrates can
form at shallower depths and at lower pressures than under the sea — and then, in the 1970s, at the bottom of the Black Sea.
Ozone, the triplet
form of oxygen, indicates that life - giving oxygen is also in abundance, and
methane, a complex hydrocarbon, is a
by - product of life processes.
«It is true that they do warm climate
by strong
methane emissions when they first
form, but on a longer - term scale, they switch to become climate coolers because they ultimately soak up more carbon from the atmosphere than they ever release.»
However, Sagan and Christopher Chyba believe organic compounds,
formed at high altitudes
by the action of solar ultraviolet radiation on
methane and ammonia can provide an ultraviolet «shield» to protect the
methane and ammonia in the lower atmosphere.
For example, it might be converted decentrally with the carbon dioxide produced
by the about 800,000 biogas facilities and stored in the
form of
methane.
Now a research team led
by scientists at MIT and including colleagues from the Woods Hole Oceanographic Institution, the University of Toronto, and elsewhere has developed an instrument that can rapidly and precisely analyze samples of environmental
methane to determine how the gas was
formed.
The researchers applied this new interpretation to
methane formed by microbes in the lab, and found good agreement between the isotopes detected and the rates at which the gas
formed.
The researchers estimate that cutting those 14 together could avoid between 700,000 and 4.7 million premature deaths (largely from smoky, unhealthy air) and increase crop yields
by between 30 million and 135 million metric tons (due to concomitant reductions in ground - level ozone, otherwise known as smog, which
forms from fugitive
methane and blights crops in Brazil, China, India, the U.S. and elsewhere).
When ruminants digest their feed,
methane is
formed as a natural
by - product of the microbial process in the rumen, and since
methane is a 25 times more powerful greenhouse gas than carbon dioxide, there is a need to devise methods to reduce such emissions from cattle.
(
Methane forms as a
by - product of anaerobic bacterial decomposition of organic matter in the soil and reaches the atmosphere through the roots and stems of the rice plants.)
However, many of the sources along the continental slope lie at cold depths in which ices have
formed at high pressures within sea - floor sediments, which once trapped
methane produced
by microbes living there.
Once
formed by either serpentinization or microbes,
methane could be stored as a stable clathrate hydrate — a chemical structure that traps
methane molecules like animals in a cage — for later release to the atmosphere, perhaps
by gradual outgassing through cracks and fissures or
by episodic bursts triggered
by volcanism.
Lower in the atmosphere, oxygen atoms and hydroxyl radicals (OH), which
form when water molecules are broken apart
by ultraviolet photons, oxidize
methane.
In the above citied letter to Nature the authors concluded out of their experiments: «Here we demonstrate using stable carbon isotopes that
methane is readily
formed in situ in terrestrial plants under oxic conditions
by a hitherto unrecognized process.»
On December 16, NASA announced another potential whiff of Martian life in the
form of
methane sniffed
by the rover Curiosity.
Methane hydrates are
formed by bonding with water to make an ice - like substance in certain temperature / pressure conditions that can be found at shallow water depths in
On the dwarf planet, the reddish color is likely caused
by tholins, which are
formed when cosmic rays and solar ultraviolet light interact with
methane in Pluto's atmosphere and on its surface.
The findings were headed
by Bruce Macintosh, a professor of physics at Stanford University, and show the new planet, 51 Eridani b, is one million times fainter than its parent star and shows the strongest
methane signature ever detected on an alien planet, which should yield additional clues as to how the planet
formed.
Scientists can hunt for extraterrestrial cellular life
forms, such as bacteria or more complex life,
by looking for certain chemicals on a planet or in its atmosphere, but virions do not create
by - products like
methane or oxygen.
• Significantly, the East Siberian Arctic Shelf, ESAS, has up to 1000 Gt of
methane reserves, and it is highly believable that 1 % of this (or up to 10 Gt) is in the
form of free gas trapped underneath the currently degrading subsea permafrost cap, which could be released within the next few decades
by a combination of increasing Arctic Ocean water temperatures, increased storm activity, and possible increases in seismic activity.
Methane production is accelerated even more in areas dominated
by sedges, grasslike plants that exude more easily altered
forms of dissolved organic carbon from their roots.
Because the carbon that stimulates
methane production is primarily dissolved organic carbon carried downward through the peat
by rainwater rather than the solid - phase carbon that
forms peat, this change in transport depth doubled the peak production zones for
methane.
Finally, they tracked radiocarbon, which is also carried downward
by precipitation, as a representative of young, easily altered, and mobile
forms of carbon that stimulate
methane production.
Unlike biomethane produced
by anaerobic digestion, Bio-SNG is
formed by the conversion of thermally - derived syngas — i.e., via the gasification of biomass waste — into
methane.
«When
methane makes its way into the upper atmosphere, it is oxidized
by a complex series of reactions to
form water vapor,» Russell added.
Our significant
methane reduction achievement on the Norwegian Continental Shelf will
form the basis for our contribution to this joint effort
by partners from industry, government and civil society.
Fortunately, as depicted in Figure 2 (orange «thermal down surface» arrow), some of this energy does stay in the atmosphere, where it is sent back toward Earth
by clouds, released
by clouds as they condense to
form rain or snow, or absorbed
by atmospheric gases composed of three or more atoms, such as water vapor (H2O), carbon dioxide (CO2), nitrous oxide (N2O), and
methane (CH4).
«As
methane has been permanently originating in the seabed since it was
formed, these deposits are huge and emissions of this ready - to - go
methane to the water column only depend on occurence of migration pathways (provided or not provided
by permafrost),» she said.
Unlike other terrestrial and marine sources, which gradually release
methane as it
forms, the shelf is emitting
methane that has accumulated in seabed deposits for hundreds of thousands of years and until now was restricted
by permafrost, says Shakhova.
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.
Around half of our grid - based electricity could be supplied
by means of a few very large power systems burning
methane, either in the
form of natural gas or the effluvium from underground coal gasification [the only way to employ coal cleanly, he argues], and burying the carbon dioxide they produce.
Converting Hydrogen to
Methane I first became of aware of the Sabatier reaction
form reading a book «The Case For Mars»
by Robert Zubrin.
One consideration might be the fact that some / much of the exiting
methane may be
forming clathrates as it hits the cold water as demonstrated
by the [foolishly unanticipated?]
Simply speaking, volcanoes helped
form the atmosphere while living organisms have helped shape the atmosphere to their liking in two ways: firstly
by warming the planet to a liveable temperature
by producing
methane and carbon dioxide during the process of decay of dead matter, and secondly
by creating oxygen through the process of photosynthesis
by our green friends in the plant kingdom.