• 제목/요약/키워드: Methane gas hydrate

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감압법을 이용한 메탄 하이드레이트 생산에 대한 연구 (Study on methane hydrate production using depressurization method)

  • 박성식;김남진
    • 한국태양에너지학회 논문집
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    • 제30권1호
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    • pp.34-41
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    • 2010
  • Gas hydrates are solid solutions when water molecules are linked through hydrogen bonding and create host lattice cavities that can enclose many kinds of guest(gas) molecules. There are plenty of methane(gas) hydrate in the earth and distributed widely at offshore and permafrost. Several schemes, to produce methane hydrates, have been studied. In this study, depressurization method has been utilized for the numerical model due to it's simplicity and effectiveness. IMPES method has been used for numerical analysis to get the saturation and velocity profile of each phase and pressure profile, velocity of dissociation front progress and the quantity of produced gas. The values calculated for the sample length of 10m, show that methane hydrates has been dissolved completely in approximately 223 minutes and the velocity of dissociation front progress is 3.95㎝ per minute. The volume ratio of the produced gas in the porous media is found to be about 50%. Analysing the saturation profile and the velocity profile from the numerical results, the permeability of each phase in porous media is considered to be the most important factor in the two phase flow propagation. Consequently, permeability strongly influences the productivity of gas in porous media for methane hydrates.

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

  • 김동현;박기훈;차민준
    • Korean Chemical Engineering Research
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    • 제58권4호
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    • pp.635-641
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    • 2020
  • 이 연구에서는 에틸렌글리콜과 염이 포함된 메탄 하이드레이트의 상평형과 형성 거동을 측정하였다. 염의 종류로는 염화나트륨(NaCl), 브롬화나트륨(NaBr), 아이오딘화나트륨(NaI)을 이용하였으며, 272~283 K의 온도 범위와 3.5~11 MPa의 압력범위에서 상평형 조건을 확인하였다. 5 wt% NaCl + 10 wt% MEG, 5 wt% NaBr + 10 wt% MEG, 5 wt% NaI + 10 wt% MEG의 순서로 메탄 하이드레이트의 억제 효과가 나타났음을 확인하였다. 에틸렌글리콜과 염이 포함된 메탄 하이드레이트의 형성 거동은 생성유도시간, 가스소모량과 성장 속도를 분석하여 확인하였다. 에틸렌글리콜과 염이 포함된 메탄 하이드레이트의 생성유도시간은 실험 조건에서 큰 차이를 보이지 않았지만, 에틸렌글리콜과 염의 첨가는 가스소모량과 성장 속도에 영향을 주었음을 확인할 수 있었다.

메탄 하이드레이트의 부존 가능성과 평형조건

  • 류병재;허대기;선우돈;정태진;김현태;김세준;이호섭
    • 한국석유지질학회:학술대회논문집
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    • 한국석유지질학회 1998년도 제5차 학술발표회 발표논문집
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    • pp.56-65
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    • 1998
  • Methane hydrate is ice-like solid compound consisting of mainly methane and water, and is stable under specific low temperature and high pressure conditions (HSZ : methane hydrate stability zone) that occurs in permafrost regions and in the ocean floor sediments. Geophysical survey was implemented in the southern area of the East Sea, and the HSZ of the study area is determined by the temperature, pressure and local heat flow obtained from the survey and well data. In the study area, methane hydrates could exist in the sediments below the water depths of about $300{\cal}m$, and the base of HSZ is about 600m beneath the seafloor. The acoustically blanking zones in the sediment and phenomena of gas seepage were detected from the seismic section. These sediments have the sufficient physical condition for the formation of methane hydrate. The temperature and pressure conditions were experimentally measured for the dissociation of methane and propane hydrates in Pure water. Equilibrium conditions of methane and propane hydrates were obtained in the pressure range up to 19050Kpa and 401.3Kpa. Under same temperature condition, propane hydrate was dissociated at lower pressure than that of methane hydrate.

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Gas trasport and Gas hydrate distribution characteristics of Southern Hydrate Ridge: Results from ODP Leg 204

  • 이영주;류병재;김지훈;이상일
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2006년도 춘계학술대회
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    • pp.407-409
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    • 2006
  • Geochemical analyses carried out on samples collected from cores on and near the southern smit of Hydrate Ridge have advanced understanding by providing a clear contrast of the two major modes of marine gas hydrate occurrence. High concentrations (15%-40% of pore space) of gas hydrate occurring at shallow depths (0-40 mbsf) on and near the southern summit are fed by gas migrating from depths of as much as 2km within the accretionary prism. This gas carries a characteristic minor component of C2-C5 thermogenic hydrocarbons that enable tracing of migration pathways and may stabilize the occurrence of some structure II gas hydrate. A structure II wet gas hydrate that is stable to greater depths and temperatures than structure I methane hydrate may account for the deeper, faint second bottom simulating reflection (BSR2) that occurs on the seaward side of the ridge. The wet gas is migrating In an ash/turbidite layer that intersects the base of gas hydrate stability on the seaward side of and directly beneath the southern summit of Hydrate Ridge. The high gas saturation (>65%) of the pore space within this layer could create a two-phase (gas + solid) system that would enable free gas to move vertically upward through the gas hydrate stability zone. Away from the summit of the ridge there is no apparent influx of the gas seeping from depth and sediments are characterized by the normal sequence of early diagenetic processes involving anaerobic oxidation of sedimentary organic matter, initially linked to the reduction of sulfate and later continued by means of carbonate reduction leading to the formation of microbial methane.

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감압법을 이용한 메탄하이드레이트 생산에 대한 수치적 연구 (Numerical Study on the Production of Methane Hydrate by Depressurization Method)

  • 김진홍;천원기;김남진
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2007년도 춘계학술대회
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    • pp.519-523
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    • 2007
  • Gas(or methane) hydrates are solid solutions when water molecules are linked through hydrogen bonding and create host lattice cavities that can enclose a large variety of guest gas molecules. The natural gas hydrate crystal may exist at low temperature above the normal freezing point of water and high pressure greater than about 30 bars. A lot of quantities of natural gas hydrates exists in the earth and many production schemes are being studied. In the present investigation, depressurization method was considered to predict the production of gas and the simulation of the two phase flow - gas and water - in porous media is being carried out. The simulation show about the fluid flow in porous media have a variety of applications in industry. Results provide the appearance of gas and water production, the pressure profile, the saturation of gas/ water/ hydrates profiles and the location of the pressure front.

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가스하이드레이트 구조 변형을 통한 메탄 저장에 관한 연구 (Study of Methane Storage through Structure Transition of Gas Hydrate)

  • 이주동;이만식;김영석
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2006년도 추계학술대회
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    • pp.54-57
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    • 2006
  • Structure H formation experiments were conducted in a semi-batch stirred vessel using methane as the small guest substance and neohexane(NH), tert-butylmethylether(TBME) and methylcyclohexane(MCH) as the large molecule guest substance (LMGS). The results indicate that the rates of gas uptake and induction times are generally dependent on the magnitude of the driving force. When tert-butyl methyl ether is used as the LMGS rapid hydrate formation, much smaller induct ion time and rapid decomposition can be achieved. Liquid-liquid equilibrium (LLE) data for the above LMGS with water have been measured under atmospheric pressure at 275.5, 283.15K, and 298.15K. It was found that TBME is the most water soluble followed by NM and MCH. The solubility of water in the non-aqueous liquid was found to increase in the following order: MCH

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메탄 하이드레이트 탐사를 위한 3 차원 탄성파 탐사와 해저면 지구화학탐사의 융합 기술 (Fusion of 3D seismic exploration and seafloor geochemical survey for methane hydrate exploration)

  • 장구보 정웅;소림 임명;등정 철재
    • 지구물리와물리탐사
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    • 제10권1호
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    • pp.37-43
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    • 2007
  • MH21 연구 컨소시엄에서는 일본 난카이 트러프 동부의 메탄 하이드레이트 탐사를 위해 고분해능 3 차원 탄성파 탐사와 해저면 지구화학탐사를 수행해 왔다. 메탄 하이트레이트가 존재하는 천부지층을 영상화 하기 위해 수행된 고분해능 3 차원 탄성파탐사 결과, 천부 지층에 대한 훌륭한 지질 정보를 획득할 수 있었다. 이러한 정보들은 지질학적, 지구화학적 모델을 구축하는데 유용하며, 특히 메탄가스 또는 메탄을 포함하는 유체의 이동통로, 지구화학적 메탄 하이드레이트 지시자등을 포함하는 복잡한 해저면 지질구조를 이해하는데 유용하다. 수중잠수정을 이용해 확인된 메탄 유출 지점과 탄성파 단면의 비교 결과, 해저면 하부의 메탄가스층 및 메탄 하이드레이트 저류층과 해저면 메탄 하이드레이트 지시자 사이의 특정적인 관계가 확인되었다. 해저지형도와 해저면 반사파로부터 영상화된 해저면 반사파진폭 영상 역시 넓은 지역에 대한 이들 관계를 이해하는 유용하며, 이러한 자료에 기반한 새로운 지구화학적 해저면 탐사도 요구된다. 메탄 하이드레이트 저류층과 해저면 메탄 하이드레이트 지시자 사이의 관계는 고분해능 3 차원 탄성파탐사 자료의 해석을 통해 점점 더 분명해지고 있다. MH21 연구 컨소시엄은 향후 고분해능 3 차원 탄성파탐사로부터 구축된 지질학적, 지구화학적 모델에 기반하여 해저면 지구화학탐사를 수행할 것이다. 이 논문에서는 3 차원 탄성파 탐사와 해저면 지구화학탐사기술의 융합에 의한 일본에서의 메탄 하이트레이트 탐사에 대해 소개한다.

CSMHYD를 이용한 혼합가스 하이드레이트의 상평형에 대한 연구 (A Study on the Phase Equilibrium Conditions of Mixture Gas Hydrates using CSMHYD)

  • 서향민;박윤범;천원기;김남진
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2007년도 추계학술대회 논문집
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    • pp.585-589
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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 Nacl acts as a inhibitor, but help gases such as ethan, propane, i-butane, and n-butane reduce the hydrate formation pressure at the same temperature.

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Natural gas hydrate occurrence and detection in the Sea of Okhotsk

  • 진영근
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2006년도 추계학술대회
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    • pp.47-49
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    • 2006
  • The Sea of Okhotsk is the unique area providing the highest methane production rate of the northern hemisphere. The area of focused fluid venting offshore the NE Sakhalin continental slope was investigated during the CHAOS (Hydro-Carbon Hydrate Accumulations in the Okhotsk Sea) expeditions onboard of RV "Akademik Lavrentyev" In 2003, 2005 and 2006. The International Research Project CHAOS (Russia-Korea-Japan) aimed at the study of gas hydrate formation processes associated with the fluid venting in the Sea of Okhotsk. Several new gas hydrate accumulations were discovered during the cruise. Hydrate-associated structures have been named as KOPRI, VNIIOKeangeologia, POI and KIT (the names of cruise participant institutes) Some of hydrate-bearing cores contain big amount of gas hydrates: massive gas hydrate layers (up to 35cm thick) were recovered. The shallowest submarine gas hydrate accumulations in the world (at the depth less then 400m) were discovered during the cruise.

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천연가스 하이드레이트의 자기보존 효과 연구 (Investigation on the Self-preservation Effect of Natural Gas Hydrates)

  • 이종원;이주동
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2011년도 추계학술대회 초록집
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    • pp.123.2-123.2
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    • 2011
  • Self-preservation effect was identified by means of macroscopic dissociation experiments after keeping natural gas hydrate samples at 258 K for 15 days. The hydrate samples were formed using synthetic natural gas hydrate whose compositions are 90% $CH_4$, 7% $C_2H_6$, and 3% $C_3H_8$. In addition, during the formation, heavy hydrocarbons of propane and ethane are found to occupy hydrate cages in a more favorable way than methane so as to change the gas composition after hydrate formation. Experimental results obtained in this study can provide useful information on applications of natural gas hydrate for storing or transporting natural gas in the form of solid hydrate.

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