首页> 外文会议>The proceedings of the Ninth (2011) ISOPE ocean mining (amp; gas hydrates) symposium. >Entry Pressure Measurement of Unconsolidated Sediments, Sampled from Methane Hydrate-bearing Zones near NE-Nankai Trough, for Capillary Pressure Analysis
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Entry Pressure Measurement of Unconsolidated Sediments, Sampled from Methane Hydrate-bearing Zones near NE-Nankai Trough, for Capillary Pressure Analysis

机译:从NE-南开海槽附近的甲烷水合物含气区采样的未固结沉积物的入口压力测量,用于毛细管压力分析

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Natural gas hydrate is a potential future energy resource, and itsrndevelopment is now realistic; however, it is not clear how methanernhydrate reservoirs accumulate. Few data are available on capillaryrnpressure around gas hydrate reservoir, which is commonly used forrnreservoir characterization, because of the difficulty measuring it.rnWhereas conventional oil and gas reservoirs involve solid rocks, thernlayers containing concentrated gas hydrate consist of unconsolidatedrnsediments, which are easily deformed during measurements.rnThe pore-size distribution of Nankai Trough unconsolidated sedimentsrnwas measured using mercury injection, which is commonly used tornmeasure capillary pressure. After many measurements, the relationshiprnbetween the injection pressure and injected volume of mercury wasrndetermined. The pore size at the time of injection was calculated fromrnthe mercury injection curves. After the measurements, we observed thernmicrostructure of the sediments using field emission scanning electronrnmicroscopy (FE-SEM) and clarified the pore size. The pore sizes ofrnsediments were compared to eliminate inferior data caused by samplerndeformation. We ultimately measured 99 pieces of unconsolidated sand,rnsilt, and mud. The results of the entry pressure measurements of NankairnTrough sediments will help to determine the mechanism of methanernhydrate storage in sediments and will contribute to methane hydraternresearch and development. The entry pressure that is an indicator ofrncapillary pressure data will also be important reference data onrnunconsolidated sediments for assessing carbon dioxide capture andrnstorage (CCS).
机译:天然气水合物是一种潜在的未来能源,其发展已成为现实。然而,目前尚不清楚甲烷水合物的储集层如何堆积。天然气水合物储层周围的毛细压力的数据很少,由于测量困难,通常用于储层表征。常规油气储层涉及固体岩石,而含浓天然气水合物的储层则由未固结沉积物组成,在测量过程中很容易变形。用注入汞法测量南海槽未固结沉积物的孔径分布,这通常用于测量毛细管压力。经过多次测量,确定了注入压力与汞注入量之间的关系。根据汞注入曲线计算注入时的孔径。测量后,我们使用场发射扫描电子显微镜(FE-SEM)观察了沉积物的微观结构,并弄清了孔径。比较了沉积物的孔径,以消除由样品变形引起的劣质数据。我们最终测量了99块未固结的沙子,粉砂和泥土。 NankairnTrough沉积物入口压力测量结果将有助于确定沉积物中甲烷水合物的储存机理,并将有助于甲烷水合物的研究和开发。进入压力是毛细血管压力数据的指标,也将是未固结沉积物的重要参考数据,用于评估二氧化碳的捕获和储存(CCS)。

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