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首页> 外文期刊>Exploration Geophysics >Estimation of CO_2 saturation from time-lapse CO_2 well logging in an onshore aquifer, Nagaoka, Japan
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Estimation of CO_2 saturation from time-lapse CO_2 well logging in an onshore aquifer, Nagaoka, Japan

机译:日本长冈陆上含水层中延时CO_2测井的CO_2饱和度估算

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The first Japanese pilot-scale CO_2 sequestration project has been undertaken in an onshore saline aquifer, near Nagaoka in Niigata prefecture, and time-lapse well logs were carried out in observation wells to detect the arrival of injected CO_2 and to evaluate CO_2 saturation in the reservoir. CO_2 was injected into a thin permeable zone at the depth of 1110m at a rate of 20-40 tonnes per day. The total amount of injected CO_2 was 10 400 tonnes, during the injection period from July 2003 to January 2005. The pilot-scale demonstration allowed an improved understanding of the CO_2 movement in a porous sandstone reservoir, by conducting time-lapse geophysical well logs at three observation wells. Comparison between neutron well logging before and after the insertion of fibreglass casing in observation well OB-2 showed good agreement within the target formation, and the higher concentration of shale volume in the reservoir results in a bigger difference between the two well logging results. CO_2 breakthrough was identified by induction, sonic, and neutron logs. By sonic logging, we confirmed P-wave velocity reduction that agreed fairly well with a laboratory measurement on drilled core samples from the Nagaoka site. We successfully matched the history changes of sonic P-wave velocity and estimated CO_2 saturation after breakthrough in two observation wells out of three. The sonic-velocity history matching result suggested that the sweep efficiency was about 40%. Small effects of CO_2 saturation on resistivity resulted in small changes in induction logs when the reservoir was partially saturated. We also found that CO_2 saturation in the CO_2-bearing zone responded to suspension of CO_2 injection.
机译:日本的第一个中试规模的CO_2封存项目是在新泻县长冈附近的一个陆上盐水层中进行的,并在观测井中进行了随时间推移的测井,以检测注入的CO_2的到来并评估CO_2饱和度。水库。每天以20-40吨的速度将CO_2注入1110m深度的薄渗透区。在2003年7月至2005年1月的注入期间,注入的CO_2总量为10400吨。试点规模的演示使人们能够通过时移地球物理测井记录来更好地了解多孔砂岩储层中的CO_2运移。三个观察井。在OB-2观察井中插入玻璃纤维套管前后中子测井的比较表明,在目标地层内吻合良好,并且储层中较高的页岩体积浓度导致两次测井结果之间的差异更大。通过感应,声波和中子测井确定了CO_2的突破。通过声波测井,我们确认了P波速度的降低与实验室对长冈工厂的岩心样品进行的测量非常吻合。我们成功地将声波P波速度的历史变化和估计的CO_2饱和度在三个观测井中的两个突破后进行了匹配。声速历史匹配结果表明扫频效率约为40%。当储层部分饱和时,CO_2饱和度对电阻率的影响很小,导致感应测井的变化很小。我们还发现,含CO_2区域中的CO_2饱和度对CO_2注入的中止有响应。

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