pstarr wrote:Think of the worst tight-shale play and then multiply the costs by 100x and the payback by 1/100. It's underwater right?
Tanada notes that it is NOT underwater. I imagine the economics of that are quite a bit different.
pstarr wrote:Think of the worst tight-shale play and then multiply the costs by 100x and the payback by 1/100. It's underwater right?
seenmostofit wrote:pstarr wrote:Think of the worst tight-shale play and then multiply the costs by 100x and the payback by 1/100. It's underwater right?
Tanada notes that it is NOT underwater. I imagine the economics of that are quite a bit different.
wiki wrote:Originally thought to occur only in the outer regions of the Solar System where temperatures are low and water ice is common, significant deposits of methane clathrate have been found under sediments on the ocean floors of Earth.[3]


As Tanada mentioned, the Russians have done work with this as well. And not just a research well, Norilsk is producing commercial methane hydrate gas today. Other countries are getting into the game as well.Scottie wrote:Apparently not only is it possible, but it has been done. From the quoted article...pstarr wrote:This crap is no more possible than Saturian Space Methane.
Tundra Gas - MethaneDeep in the Arctic Circle, in the Messoyakha gas field of western Siberia, lies a pioneer in methane hydrate extraction. Back in 1967, Russian engineers began pumping natural gas from beneath the permafrost and piping it east across the tundra to the Norilsk metal smelter, the biggest industrial enterprise in the Arctic. In 1978 they decided to wind down the operation. According to their surveys, they had sapped nearly all the methane from the deposit. But despite their estimates, the gas just kept on coming. The gas field was re-opened and continues to power Norilsk today.
Where was this methane coming from? Russian geologists initially thought it was leaking from another deposit hidden beneath the first. But their experiments revealed the opposite -- the mystery methane was seeping into the well from the icy permafrost above. If unintentionally, what they had achieved was the first, and so far only, successful exploitation of methane hydrate.
China's largest coal producer to develop "combustible ice"China's largest coal producer, China Shenhua Group, has launched a project to research and develop combustible ice, a kind of natural gas hydrate, in the northwestern Qinghai province. Shenhua Group signed an agreement with the Qinghai provincial government on Monday evening to start the exploration of combustible ice in the province.
China announced the first discovery of the resource under the bed of the South China Sea in May 2007. After it was discovered in Muli prefecture in Qinghai province in 2009, the Ministry of Land Resources announced that China had found combustible ice in the land-based region as well.
Experts expect China to experience a period of peak energy demand from 2020 to 2025. With further exploration, the country's prospective volume of natural gas hydrate in frozen earth regions is estimated to reach an equivalent to 35 billion tonnes of oil.

Makes sense to me. Capture the methane before it leaks into the atmosphere, and at the same time you get another fossil fuel source.Scottie wrote:Seems like if it is going to end up in the atmosphere anyway, might as well burn it and get some work out of it before it does?dbruning wrote:While I bet the methane deposits hold a ton of energy, wouldn't mining this stuff and burning it have wicked environmental problems?
Methane Hydrates - More Energy than All Other Fossil Fuels CombinedThe most recent DoE experiment was innovative. They lowered well pressure to make the hydrate flow and get the gas out.
In other words, this method removed a greenhouse gas from the atmosphere and produced an energy source. Even my environmentally-conscious colleague Jeff Siegel of the Power Portfolio would give two thumbs up for that.
Tundra GasOne of the main arguments in favor of exploiting onshore methane hydrates deposits concerns climate change. With many parts of the world, especially the permafrost regions, experiencing increases in temperature, methane is slowly being released from these deposits into the atmosphere. The permafrost is melting at an accelerating pace and thus the release of methane is increasing exponentially. As methane is a "greenhouse" gas that has a much greater impact on global warming than carbon dioxide, it is imperative to prevent as much of this methane as possible from escaping into the atmospere. Extracting the methane hydrates for use as fuel serves a doubly important purpose: it provides a much needed fuel at a time when global oil supplies appear to be dwindling and it saves the world from possibly disastrous sudden rises in temperature. By coincidence, Qinghai has been identified in scientific studies as the place with the fastest rising temperatures in the world.




Piece of cake.vtsnowedin wrote:As difficult as both deep water and sub permafrost hydrate methane deposits are to access they are still a hell of a lot closer then Saturn or some asteroid. For one thing you don't have to bring it through the reentry process without burning it up. I expect they will keep working on ways to bring usable amounts to the surface and eventually find a way that is viable at the then prevailing price.
Imagine if you will a robot bulldozer pushing square miles of deep water hydrate beds to one central riser pipe where the slush is brought up out of the deep pressure and the methane is separated from the water. Might be able to get it to the surface as already compressed LNG. Working through just 500 meters of permafrost should be a piece of cake in comparison and would obviously become profitable well before any deep water process.



pstarr wrote:Piece of cake.vtsnowedin wrote:As difficult as both deep water and sub permafrost hydrate methane deposits are to access they are still a hell of a lot closer then Saturn or some asteroid. For one thing you don't have to bring it through the reentry process without burning it up. I expect they will keep working on ways to bring usable amounts to the surface and eventually find a way that is viable at the then prevailing price.
Imagine if you will a robot bulldozer pushing square miles of deep water hydrate beds to one central riser pipe where the slush is brought up out of the deep pressure and the methane is separated from the water. Might be able to get it to the surface as already compressed LNG. Working through just 500 meters of permafrost should be a piece of cake in comparison and would obviously become profitable well before any deep water process.
At this rate you might earn your stripes under VASSAL OF HIS LORD GINGRICH OF THE MOON COLONY

dissident wrote:There are no seabed clathrate extraction operations that would enable an assessment of commercial viability. If people can find any news on such operations being planned then that would be really useful information.

Timo wrote:If that's the case, what are the consequences/advantages to capturing the methane hyrdates underground, extracting them, using them for fuel, and ultimately releasing them into the atmospehere as exhaust, versus just letting them enter the atmosphere naturally. What's the better approach? Or worse approach?

Natural Gas and the EnvironmentEmissions from the Combustion of Natural Gas
Natural gas is the cleanest of all the fossil fuels, as evidenced in the Environmental Protection Agency’s data comparisons in the chart below, which is still current as of 2010. Composed primarily of methane, the main products of the combustion of natural gas are carbon dioxide and water vapor, the same compounds we exhale when we breathe. Coal and oil are composed of much more complex molecules, with a higher carbon ratio and higher nitrogen and sulfur contents. This means that when combusted, coal and oil release higher levels of harmful emissions, including a higher ratio of carbon emissions, nitrogen oxides (NOx), and sulfur dioxide (SO2). Coal and fuel oil also release ash particles into the environment, substances that do not burn but instead are carried into the atmosphere and contribute to pollution. The combustion of natural gas, on the other hand, releases very small amounts of sulfur dioxide and nitrogen oxides, virtually no ash or particulate matter, and lower levels of carbon dioxide, carbon monoxide, and other reactive hydrocarbons.
Greenhouse Gas Emissions
Because carbon dioxide makes up such a high proportion of U.S. greenhouse gas emissions, reducing carbon dioxide emissions can play a pivotal role in combating the greenhouse effect and global warming. The combustion of natural gas emits almost 30 percent less carbon dioxide than oil, and just under 45 percent less carbon dioxide than coal.

The study of natural gas hydrate systems in the field provides invaluable information on these widely variable and complex systems. Results from the field can be utilized for experimental and numerical studies which offer the potential to evaluate aspects of these systems on a variety of scales and through different methodologies. The research and technology requirements necessary to further advance the understanding of natural gas hydrate systems are significant. NETL Office of Research & Development’s (ORD) Natural Gas Hydrate Team conducts integrated research from the laboratory to the field, and from the molecular to the reservoir scale modeling, leveraging NETL-ORD’s strengths in geology, geochemistry, microbiology, and numerical simulation to improve understanding of these complex systems. The NETL-ORD’s field studies efforts are often aligned with other ORD R&D activities, key projects supported by the National Methane Hydrate R&D Program both domestically and internationally, and collaboration with external partners.
The primary goals of the DOE/NETL NGHFS project are:
Conduct field-based studies that advance our ability to predict, detect, characterize, and understand where, how, and what controls natural gas hydrate occurrences in relation to both resource and climate issues.
Analyze geologic, geochemical, and microbiologic data for indications of past and current changes to the stability of natural gas hydrate in marine settings;
Develop links between the U.S. Program and international R&D efforts through direct participation in international field programs & workshops;
Evaluate the potential role natural gas hydrates play in the global carbon cycle through analysis of modern and paleo-natural gas occurrences;
Provide expertise to domestic and international collaborators, focusing on activities such as pre-expedition/field site selection and evaluation, field analyses, and synthesis of samples and data collected in the field;
Supply geologic expertise to the efforts of DOE/NETL to advance numerical simulation and field-relevant experimental studies;
Work with the DOE’s domestic research partners, particularly those partners involved in major field operations in the Gulf of Mexico and Alaska, to ensure field test locations and plans are based on a full “gas hydrate systems” analyses.
Phase 1B Activities
With hydrate stability established in Phase 1A, Phase 1B will determine whether there is hydrate of sufficient thickness and reservoir quality updip of the free gas accumulations to support production. This will require an integrated review of all seismic, well, and production history data, building on previous studies of the field data. Of particular interest is
characterization of the updip pinchout of reservoir sands.
Assuming the results of the hydrate stability modeling and reservoir limits review are encouraging, a detailed reservoir characterization will be undertaken to support simulation of hydrate production methodologies and planning for a potential dedicated hydrate test well. A goal of reservoir simulation modeling will be to quantify the impact of hydrate dissociation
recharge of the producing gas fields. This work will aid in understanding
effectiveness of secondary production via depressurization of the associated free gas interval.
Based on the static and dynamic reservoir modeling, the optimum location of a dedicated hydrate well for sampling and production testing will be proposed. The well will be designed to fit the geologic, reservoir, and operational specifics required in the Barrow gas fields but will also leverage and expand on the findings of the Anadarko and Milne Point wells.


Many environmentalists are protesting the proposed Keystone XL Pipeline because it would help facilitate the delivery of oil from Canada’s oil sands and, they argue, increase carbon dioxide emissions. They may have more reason to worry about what’s happening in Alaska. The state’s Department of Natural Resources is teaming up with the U.S. Department of Energy to speed up production of natural gas from a resource—methane hydrate deposits–that’s far larger than the oil sands in Canada, and could in theory lead to far greater greenhouse gas emissions.
The only way to keep methane hydrates in the ground is for other sources of energy to make more economic sense. Doing that would require research to make sources like nuclear power cheaper, and likely taxing carbon emissions to make sources like methane more expensive.



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