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A hydrogeologic study to optimize steamflood performance in a giant oilfield: kern river field, california

机译:加利福尼亚州克恩河油田的水文地质研究,旨在优化大型油田的蒸汽驱性能

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The stratigraphic interval above the Round Mountain formation in the Kern River field contains four confined aquifers. Two of these confined aquifers are composed of sandstones in the main and transition zones of the Santa Margarita formation, and the remaining two are composed of sandstones in the lower and middle zones of the Chanc Formation. Above the confined aquifers is one regional, mainly unconfined aquifer in sandstones of the upper Chanac Formation and lower zones (U-lower K2) of the Kern River Formation. This unconfined aquifer is overlain by several perched aquifers in sandstones of the upper zones (upper K2-C) of the Kern River Formation. Oil production in the Kern River field is from sandstones comprising the unconfined and perched aquifers in the Kern River Formation and is greatly facilitated by steamflood operations. Flow between the various zones of the Kern River Formation and from underlying formations used for water disposal may provide unwanted pressure support for the steamed intervals, resulting in poor steamflood performance. Results of our study suggest that a water management program designed to remove and dispose of excess water from the producing zones will increase steamflood efficiency. The overall dip of the potentiaometric surface in the regional unconfined aquifer and the smaller perched aquifers is westward and parallels the structural dip of the beds. Widespread fluid depletion in zones along the updip edge of the field, and the absence of a potentiometric gradient showing flow outward from the Kern River, suggest minimal groundwater recharge from natural sources. These observations suggest that fluids move downdip by gravity drainage from a closed volume, with significant removal of fluids by producing operations causing an overall decline in pressure in the unconfined aquifer. These findings are highly favorable for the implementation of a water management program designed to pump out and dispose of water from the producing zones.
机译:在克恩河油田的朗德山地层上方的地层间隔包含四个承压含水层。这些受限含水层中的两个由圣玛格丽塔组主要和过渡带的砂岩组成,其余两个由尚克组的中下部带的砂岩组成。在承压含水层上方是一个区域性的,主要是无约束含水层,位于上查纳克组上部和克恩河组下部区域(U-下K2)的砂岩中。在克恩河组上部(K2-C上部)的砂岩中,数个栖息的含水层覆盖了这个无限制的含水层。克恩河油田的石油生产是由砂岩组成的,这些砂岩包括克恩河地层的无侧限和高位含水层,蒸汽驱作业极大地促进了开采。在克恩河地层的各个区域之间以及从用于水处理的下层地层之间的流动可能会为蒸腾的间隔提供不必要的压力支撑,从而导致蒸汽驱性能较差。我们的研究结果表明,旨在从生产区去除和处置多余水的水管理程序将提高蒸汽驱效率。区域性无限制含水层和较小的栖息含水层中电位计表面的总体倾角向西,与床层的结构倾角平行。沿油田上倾边缘区域广泛的流体枯竭,并且没有电位计梯度显示克恩河向外流动,这表明自然来源的地下水补给最少。这些观察结果表明,由于重力的作用,流体从封闭的空间中向下倾入,并且由于生产作业而大量去除流体,从而导致无限制含水层中的压力整体下降。这些发现对于实施旨在从生产区抽水和处理水的水管理计划的实施非常有利。

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