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biogas    
相关语句
  生物气
    CARBON ISOTOPE CHARACTERISTICS OF HCO_3 ̄-IN FORMATION WATER OF NANBA SAG AND BIOGAS IDENTIFICATION, NGI
    南堡凹陷地层水中HCO_3~-的碳同位素特征与生物气的识别
短句来源
    ADVANCES IN SIMULATED TEST OF BIOGAS
    生物气模拟试验的进展
短句来源
    THE FORMING AND MODE OF QUATERNARY BIOGAS RESERVOIRS IN CHAIDAMU BASIN
    柴达木盆地第四系生物气藏的形成与模式
短句来源
    FUNDAMENTAL GEOLOGIC FACTORS CONTROLLING BIOGAS ACCUMULATION
    控制生物气富集成藏的基本地质因素
短句来源
    ③the petrophysical property and scale of reservoir bed are the key factors restricting the size of the biogas reservoir;
    ③生物气的储集层物性、储集层规模是制约气藏大小的关键;
短句来源
更多       
  生物气
    CARBON ISOTOPE CHARACTERISTICS OF HCO_3 ̄-IN FORMATION WATER OF NANBA SAG AND BIOGAS IDENTIFICATION, NGI
    南堡凹陷地层水中HCO_3~-的碳同位素特征与生物气的识别
短句来源
    ADVANCES IN SIMULATED TEST OF BIOGAS
    生物气模拟试验的进展
短句来源
    THE FORMING AND MODE OF QUATERNARY BIOGAS RESERVOIRS IN CHAIDAMU BASIN
    柴达木盆地第四系生物气藏的形成与模式
短句来源
    FUNDAMENTAL GEOLOGIC FACTORS CONTROLLING BIOGAS ACCUMULATION
    控制生物气富集成藏的基本地质因素
短句来源
    ③the petrophysical property and scale of reservoir bed are the key factors restricting the size of the biogas reservoir;
    ③生物气的储集层物性、储集层规模是制约气藏大小的关键;
短句来源
更多       
  生物气
    CARBON ISOTOPE CHARACTERISTICS OF HCO_3 ̄-IN FORMATION WATER OF NANBA SAG AND BIOGAS IDENTIFICATION, NGI
    南堡凹陷地层水中HCO_3~-的碳同位素特征与生物气的识别
短句来源
    ADVANCES IN SIMULATED TEST OF BIOGAS
    生物气模拟试验的进展
短句来源
    THE FORMING AND MODE OF QUATERNARY BIOGAS RESERVOIRS IN CHAIDAMU BASIN
    柴达木盆地第四系生物气藏的形成与模式
短句来源
    FUNDAMENTAL GEOLOGIC FACTORS CONTROLLING BIOGAS ACCUMULATION
    控制生物气富集成藏的基本地质因素
短句来源
    ③the petrophysical property and scale of reservoir bed are the key factors restricting the size of the biogas reservoir;
    ③生物气的储集层物性、储集层规模是制约气藏大小的关键;
短句来源
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  biogas
Methane production rates were 0.039, 0.047, 0.064, and 0.069 ml/g OM per 1 h, with the mean relative amounts of methane in the biogas being equal to 25, 41, 55, and 62%, respectively.
      
Gas discharge effect on heat loss compensation in a biogas unit
      
Structural features of biogas units and their effect on technical and technological parameters of the system are considered.
      
Estimates of the biogas discharge part on the methane tank heat loss compensation are presented.
      
Results of theoretical and experimental studies are presented on liquid waste processing in a biogas unit by differentiated renewal of brewed mass in the reactor relative levels.
      
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Water-soluble gas is a kind of conventional energy resources widely distributing in the world. The water-soluble gas in China is classified according to present data, closed degree. genesis, stratum pressure and buried depth. The water-soluble gas of Quaternary is biogas only containing methane,but that of Tertiary is mostly secondery. The characteristics and distributions of shallow biogas, normal pressure water-soluble gas, the water-soluble gas of middle-depth strata. the water-soluble gas of...

Water-soluble gas is a kind of conventional energy resources widely distributing in the world. The water-soluble gas in China is classified according to present data, closed degree. genesis, stratum pressure and buried depth. The water-soluble gas of Quaternary is biogas only containing methane,but that of Tertiary is mostly secondery. The characteristics and distributions of shallow biogas, normal pressure water-soluble gas, the water-soluble gas of middle-depth strata. the water-soluble gas of abnormaly high pressure are expounded. The resources of water-Soluble gas in China is estimated 12×1012~65×1012m3 by respectively using volumetric method and analogy method.

水溶性天然气属非常规能源,在全世界广泛分布。据现有资料,按封闭程度、成因、地层压力和埋藏深度对我国水溶性天然气进行了分类,第四系水溶性天然气是仅含甲烷的生物成因气,而第三系多为次生的。论述了浅层生物成因气、正常压力下的水溶性天然气、中深层水溶性天然气和异常高压下水溶性天然气的特征与分布。分别采用容积法和类比法,估算出我国水溶性天然气资源潜量为12×1012~65×1012m3。

The Shallow gas reservoirs in Songliao Basin are the gas-bearing formations of K1n2,K1n3,K1n4, and K2m1. Commercial gas flows are found by drilling. They are distributed over the Shallow formations of Saertu, Xinbei, Putaohua, Longhupao, Mutou and Honggang oil fields and the upper parts of Aonan nose structure.Gas soruces mainly are from the combination of central oil-gas-bearing and oil-bearing formations of K1n1 and K1n2,including a few of infiltrated biogas. The sandstone formations of K1n2,K1n3,K1n4...

The Shallow gas reservoirs in Songliao Basin are the gas-bearing formations of K1n2,K1n3,K1n4, and K2m1. Commercial gas flows are found by drilling. They are distributed over the Shallow formations of Saertu, Xinbei, Putaohua, Longhupao, Mutou and Honggang oil fields and the upper parts of Aonan nose structure.Gas soruces mainly are from the combination of central oil-gas-bearing and oil-bearing formations of K1n1 and K1n2,including a few of infiltrated biogas. The sandstone formations of K1n2,K1n3,K1n4 and K2m1 are po reservoirs with loose lithnology and over 25 % porosity. The black Shale of K2n3 stably distributed in the Basin is the good regional caprock of K1n2 gas reservoir. Purer Shale with 25-30 m thickness is on the top of K1n3 gas reservoir. Black Shale with 20-30m thickness is on the top of K2m1 gas reservoir. The shales are stably distributed in the Basin. The most perts of shallow gas reserviors controlled by ruptures are distributed in fracture belt and the upper and lower walls of fault(mostly in the lower walls). Shallow gas reservoirs are associated with the known oil fields. If the measures of gas testing are improved,the exploration of shallow gas will have a vast prospect.

松辽盆地浅层气藏是指下白垩统嫩江组二、三、四段和上白垩统明水组一段含气层。钻探证实,具工业气流,且多数分布在盆地中央拗陷区的萨尔图、新北、葡萄花、龙虎泡、木头、红岗油田和敖南鼻状构造等之上的浅部地层。气源主要来自中部含油气组合和嫩一、二段生油层,不排除少量生物气的混入。嫩二、三、四段及明一段的砂岩组为气藏储集空间,粉-细砂岩为主,岩性疏松,孔隙度在25%以上。嫩三段黑色泥岩在盆地内稳定分布,为嫩二段气藏的良好区域盖层;嫩三段气藏之上有厚25~30m的较纯泥岩,明水组一段气藏上部也有厚20~25m的黑色泥岩,均在盆地内稳定分布。浅层气藏受断裂控制,大多数气藏分布在断裂带上和断层的两盘(多数在下盘)。浅层气藏和已知油田相伴生,若改进试气工艺及方法,有针对性地进行浅层天然气勘探,其前景将十分广阔。

Mudstone andcoal seam of coal measure strata possess better hydrocarbongeneration potential in Middle and Lower Jurassic of Junggar basin; hydrocarbon in Juras-sic reservoir is relatedwith mudy source rock of coal measure strata,From onsource,Jurassic reservoir can be divided into”old-genetic and new-reserve" type and authigenictype.The former mainly distributes in north part of Junggar basin,the latter in southpart,biogas and pyrolysis gas to form gas reservoir are all in piedmont structural zone insouth...

Mudstone andcoal seam of coal measure strata possess better hydrocarbongeneration potential in Middle and Lower Jurassic of Junggar basin; hydrocarbon in Juras-sic reservoir is relatedwith mudy source rock of coal measure strata,From onsource,Jurassic reservoir can be divided into”old-genetic and new-reserve" type and authigenictype.The former mainly distributes in north part of Junggar basin,the latter in southpart,biogas and pyrolysis gas to form gas reservoir are all in piedmont structural zone insouth margin of Junggar basin.

准噶尔盆地中、下侏罗统煤系地层中的泥岩和煤岩均具有良好的生烃潜力;已发现的侏罗系油气藏中的烃类可能主要与煤系地层中泥质烃源岩有关。从油源角度分析,侏罗系油藏可分为下源型和自源型,前者主要分布在盆地北部,后者主要分布在盆地南部。形成纯气藏的生物气、过熟裂解气均分布在盆地南缘山前构造带。

 
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