• Title/Summary/Keyword: Methane hydrate

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Phase Equilibria and Formation Behaviors of Methane Hydrate with Ethylene Glycol and Salts (에틸렌글리콜과 염이 포함된 메탄 하이드레이트의 상평형과 형성 거동)

  • Kim, Dong Hyun;Park, Ki Hun;Cha, Minjun
    • Korean Chemical Engineering Research
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    • v.58 no.4
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    • pp.635-641
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    • 2020
  • In this study, phase equilibria and formation behaviors of methane hydrate containing mono-ethylene glycol (MEG) and salts (sodium chloride, NaCl; sodium bromide, NaBr; sodium iodide, NaI) are investigated. Equilibrium conditions of methane hydrate containing MEG and salts are measured in a temperature range 272~283 K and a pressure range 3.5~11 MPa. Hydrate inhibition performance in the presence of additives can be summarized as follows: methane hydrate containing (5 wt% NaCl + 10 wt% MEG) > (5 wt% NaBr + 10 wt% MEG) > (5 wt% NaI + 10 wt% MEG). Formation behaviors of methane hydrate with MEG and salts are investigated for analyzing the induction time, gas consumption amount and growth rate of methane hydrates. There are no significant changes in the induction time during methane hydrate formation, but the addition of MEG and salts solution during hydrate formation can affect the gas consumption amount and growth rate.

Formation and Decomposition of Methane Hydrate Using Silica Sand (실리카샌드를 이용한 메탄하이드레이트 형성과 분해)

  • Nam, Sung-Chan;Linga, Praveen;Englezos, Peter
    • Applied Chemistry for Engineering
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    • v.19 no.6
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    • pp.680-684
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    • 2008
  • The formation of methane hydrate ($CH_4$ hydrate) in silica sand and decomposition experiments were performed at $7.0^{\circ}C$ using a newly designed reactor. Temperature profile within silica sand bed was measured by thermocouples installed at different height of reactor. Both temperature and pressure are the main parameters for the formation (measured by adsorption experiment) and decomposition (measured by desorption experiment) of methane hydrate. Experiment of methane hydrate formation at 8 MPa and $7.0^{\circ}C$ showed that 70% of methane was converted to hydrate and the recovery of methane by the decomposition of methane hydrate was 82%.

Nozzle effect on the formation of Methane hydrate

  • Seo, Hyang-Min;Park, Sung-Seek;Kim, Nam-Jin
    • 한국신재생에너지학회:학술대회논문집
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    • 2008.10a
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    • pp.226-229
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    • 2008
  • When methane hydrate is artificially formed to store and transport large quantity of natural gas, its reaction time may be too long and the gas consumption in water becomes relatively low, the reaction rate between water and methane gas is low. Therefore, the present investigation focuses on the rapid production of hydrates and increases the gas consumption by injecting water into methane gas utilizing nozzle. the hydrate in water injection using a nozzle formed rapidly more than that in gas injection, and the gas consumption of methane hydrate in water injection is about three to four times greater than that in gas injection according to subcooling.

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Nozzle Effect for the Formation Enhancement of Methane Hydrate (메탄 하이드레이트 생성촉진을 위한 노즐 분사효과 연구)

  • Kim, Nam-Jin;Chun, Won-Gee
    • Journal of the Korean Solar Energy Society
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    • v.28 no.6
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    • pp.8-14
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    • 2008
  • Methane hydrate is crystalline ice-like compounds which consist of methane gas of 99% and over, and the estimated amount of gas contained in hydrates is about 1 trillion carbon Ton. Therefore, they have the potential for being a significant source for natural gas, and 1$m^3$ solid hydrates contain up to 172N$m^3$ of methane gas, depending on the pressure and temperature of production. Such large volumes make natural gas hydrates can be used to store and transport natural gas. In this study, the tests were performed on the formation of methane hydrate by a nozzle. The result showed that utilizing nozzles dramatically reduces the time in hydrate formation, the pressure after the injection is decreased to be approximately 90% of experimental pressurethe, and gas consumption is higher about 3 times than that of subcooling test.

Experimental Investigation on the Enhancement of Methane Hydrate Formation in the Solid Transportation of Natural Gas (천연가스 고체화 수송을 위한 메탄 하이드레이트 충진율 증대에 대한 실험적 연구)

  • 김남진;정재성;김종보
    • Korean Journal of Air-Conditioning and Refrigeration Engineering
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    • v.14 no.10
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    • pp.863-870
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    • 2002
  • Fossil fuels have been depleted gradually and new energy resource which can solve this shortage is needed now. Methane hydrate, non-polluting new energy resource, satisfies this requirement and considered the precious resource prevent the global warming. Fortunately, there are abundant resources of methane hydrate distribute in the earth widely, so developing the techniques that can use these gases effectively is fully valuable. the work presented here is to develop the skill which can transport and store methane hydrate. As a first step, the equilibrium point experiment has been carried out by increasing temperatures in the cell at fixed pressures. The influence of gas consumption rates under variable degree of subcooling, stirring and water injection has been investigated formation to find out kinetic characteristics of the hydrate. The results of present investigation show that the enhancements of the hydrate formation in terms of the gas/water ratio are closely related to operational pressure, temperature, degrees of subcooling, stirring rate, and water injection.

Study of Producing Natural Gas From Gas Hydrate With Industrial Flue Gas (산업용 배기가스를 이용한 가스 하이드레이트로부터의 천연가스 생산 연구)

  • Seo, Yu-Taek;Kang, Seong-Pil;Lee, Jae-Goo;Cha, Min-Jun;Lee, Huen
    • 한국신재생에너지학회:학술대회논문집
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    • 2008.10a
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    • pp.188-191
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    • 2008
  • There have been many methods for producing natural gas from gas hydrate reservoirs in permafrost and sea floor sediments. It is well knownthat the depressurization should be a best option for Class 1 gas hydrate deposit, which is composed of tow layers: hydrate bearing layer and an underlying free gas. However many of gas hydrate reservoirs in sea floor sediments are classified as Class 2 that is composed of gas hydrate layer and mobile water, and Class 3 that is a single gas hydrate layer. The most appropriate production methods among the present methods such as thermal stimulation, inhibitor injection, and controlled oxidation are still under development with considering the gas hydrate reservoir characteristics. In East Sea of Korea, it is presumed that the thick fractured shale deposits could be Class 2 or 3, which is similar to the gas hydrate discovered offshore India. Therefore it is needed to evaluate the possible production methods for economic production of natural gas from gas hydrate reservoir. Here we would like to present the production of natural gas from gas hydrate deposit in East Sea with industrial flue gases from steel company, refineries, and other sources. The existing industrial complex in Gyeongbuk province is not far from gas hydrate reservoir of East Sea, thus the carbon dioxide in flue gas could be used to replace methane in gas hydrate. This approach is attractive due to the suggestion of natural gas productionby use of industrial flue gas, which contribute to the reduction of carbon dioxide emission in industrial complex. As a feasibility study, we did the NMR experiments to study the replacement reaction of carbon dioxide with methane in gas hydrate cages. The in-situ NMR measurement suggeststhat 42% of methane in hydrate cages have been replaced by carbon dioxide and nitrogen in preliminary test. Further studies are presented to evaluate the replacement ratio of methane hydrate at corresponding flue gas concentration.

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Estimating attenuation in methane hydrate bearing sediments from surface seismic data (메탄하이드레이트 부존층에서의 지진파 감쇠치 산출)

  • Lee, Kwang-Ho;Matsushima, Jun
    • 한국지구물리탐사학회:학술대회논문집
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    • 2009.10a
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    • pp.28-33
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    • 2009
  • Methane hydrates are considered important in terms of their effect on global warming and as potential energy resources. Now, mainly the presence of a BSR and seismic velocity are used for estimation of methane hydrate concentration in the seismic reflection survey. But recent studies on seismic attenuation show that it can be used also to estimate methane hydrates concentration. In this study, we tried to estimate attenuation from 2D seismic reflection data acquired at Nankai Trough in Japan and analyzed attenuation properties in methane hydrate bearing sediments. Seismic attenuation estimated by QVO method in an offset range $125{\sim}1,575m$. We observed high attenuation in methane hydrate bearing sediments over BSR in a frequency range of 30-70Hz. Thus, this result demonstrates that seismic reflection wave within this frequency range are affected significantly by the existence of methane hydrate concentration zone.

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Methane hydrate : The state of the art of Production technologies and environmental issues (메탄 하이드레이트의 생산 기술 현황과 환경에 미치는 영향)

  • Chang Seung yong
    • The Korean Journal of Petroleum Geology
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    • v.7 no.1_2 s.8
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    • pp.13-18
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    • 1999
  • Methane hydrate is an ice-like solid material and it has a structure which water molecules enclose gas molecules. For low temperature and high pressure, hydrocarbon gas forms hydrate and due to this condition, it is existed in the arctic region or deep sea. Presently, the amount of methane hydrate is unpredictable, but it is assumed that the amount will be enormous. For this reason, it is expected that it will play a major role as natural gas resources in the future. However, the production technologies are stayed on the low level and the economical technology was not developed yet. Also, emission of natural gas from methane hydrate will cause global warming and thus it is considered as a critical environmental problem. In this paper, the state of the art of the production technologies and environmental effects of methane hydrate were summarized.

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The Effect of DME on Phase Equilibria of Methane Hydrates (DME가 메탄하이드레이트 상평형에 미치는 영향)

  • Lim, Gyegyu;Lee, Gwanghee
    • Transactions of the Korean hydrogen and new energy society
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    • v.23 no.6
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    • pp.660-669
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    • 2012
  • Gas resources captured in the form of gas hydrates are an order of magnitude larger than the resources available from conventional resources. Focus of this research is to investigate the effect of DME on phase equilibria of methane hydrate, as well as the possibility of the use of the PRO/II computer simulation to estimate the phase equilibria. In systems containing water and a gaseous component like, for instance, methane, ethane, and propane, gas hydrates may occur, if conditions in terms of pressure and temperature are satisfied. Mixtures of gases, e.g. LPG or natural gas, are also able to form gas hydrates in the presence of water. The experiments presented here were performed at temperatures varying between 268.15K and 288.15K and at pressures varying between 1.88 MPa and 10.56 MPa. It was found that the phase equilibria of methane hydrate is influenced by the addition of DME to the system. The pressure for the equilibrium hydrate-liquid water-vapor (H - $L_w$ - V) in the system water + methane is reduced upon addition of DME. The phase equilibria of methane hydrate can be estimated by the PRO/II computer simulation, whereas those of methane hydrate containing DME or LPG can't be estimated properly.

Equilibrium Conditions of Methane Hydrate added Help Gases (보조가스가 첨가된 메탄 하이드레이트 상평형 조건에 대한 연구)

  • Kim, Nam-Jin;Lim, Sang-Hoon;Chun, Won-Gee
    • Journal of the Korean Solar Energy Society
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    • v.27 no.4
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    • pp.51-58
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    • 2007
  • Gas hydrate is a special kind of inclusion compound that can be formed by capturing gas molecules to water lattice in high pressure and low temperature conditions. When referred to standard conditions, $1m^3$ solid hydrates contain up to $172Nm^3$ of methane gas, depending on the pressure and temperature of production. Such large volumes make natural gas hydrates can be used to store and transport natural gas. In this study, three-phase equilibrium conditions for forming methane hydrate were theoretically obtained in aqueous single electrolyte solution containing 3wt% NaCl. The results show that the predictions match the previous experimental values very well, and it was found that NaCl acts as an inhibitor.