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Occurrence and distribution characteristics of fluids in tight sandstone reservoirs in the Shilijiahan zone, northern Ordos Basin

机译:鄂尔多斯盆地北部什里加汉地区致密砂岩储层流体成因与分布特征

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High-yield gas layers, low-yield gas layers and (gas bearing) water layers of Upper Paleozoic coexist in the Shilijiahan zone in the northern Ordos Basin, but gas–water distribution characteristics, laws and influence factors are not understood well, so the exploration and development of natural gas in this zone are restricted. In this paper, statistical analysis was carried out on the data of Upper Paleozoic formation water in this zone, e.g. salinity, pH value and ion concentration. It is shown that the formation water in this zone is of CaCl2type. Then, the origin, types, controlling factors and spatial distribution characteristics of formation water were figured out by using core, mud logging, well logging and testing data, combined with the classification and evaluation results of geochemical characteristics of formation water. Besides, the logging identification chart of gas, water and dry layers in this zone was established. Finally, the occurrence and distribution laws of reservoir fluids were defined. The formation water of CaCl2type indicates a good sealing capacity in this zone, which is favorable for natural gas accumulation. It is indicated that the reservoir fluids in this zone exist in the state of free water, capillary water and irreducible water. Free water is mainly distributed in the west of this zone, irreducible water in the east, and capillary water in the whole zone. The logging identification chart has been applied in many wells in this zone like Well Jin 86. The identification result is basically accordant with the gas testing result. It is verified that gas and water layers can be identified effectively based on this logging identification chart.
机译:鄂尔多斯盆地北部十里家涵地区上古生界高产气层,低产气层和(含气)水层共存,但对气水分布特征,规律和影响因素尚不了解。该区天然气勘探开发受到限制。本文对该区域上古生界地层水的数据进行了统计分析。盐度,pH值和离子浓度。结果表明,该区的地层水为CaCl2型。然后,利用岩心,录井,测井和测试数据,结合地层水地球化学特征的分类和评价结果,得出地层水的来源,类型,控制因素和空间分布特征。此外,还建立了该区天然气,水和干层的测井识别图。最后,定义了储层流体的发生和分布规律。 CaCl 2型地层水在该区具有良好的封闭能力,有利于天然气的聚集。结果表明,该区储层流体以游离水,毛细管水和不可还原水的状态存在。自由水主要分布在该区域的西部,东部是不可还原的水,而毛细管水则分布在整个区域。测井识别图已经在该地区的许多井中得到了应用,例如Jin 86井。识别结果与气体测试结果基本一致。根据该测井识别图,证实可以有效地识别气层和水层。

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