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Fluid flow monitoring in oilfields using downhole measurements of electrokinetic potential

机译:使用井下电动势测量来监测油田的流体流量

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Downhole measurements of electrokinetic potential are a promising new technology for hydrocarbon reservoir monitoring. Using a 3D finite-element model combining both multiphase flow and electrokinetic components, we investigated the behavior of electrokinetic (streaming) potential during oil production in a range of reservoir environments. We found that streaming-potential signals originate at fluid fronts and at geologic boundaries where fluid saturation changes. As water encroaches on an oil production well, the streaming-potential signal associated with the water front encompasses the well even when the front is up to 100 m away, so the potential measured at the well starts to change significantly relative to a distant reference electrode. Variations in the geometry of the encroaching water front can becharacterized using an array of electrodes positioned along the well, but a good understanding of the local reservoir geology is required to identify signals caused by the front. The streaming potential measured at a well is maximized in low-permeability reservoirs produced at a high rate and in thick reservoirs with low shale content. However, considerable uncertainties remain, particularly relating to the nature of electrokinetic coupling at high salinity and during multiphase flow. Our results suggest that the streaming potential at low salinity (10(-3)-10(-4) mol/L) is large (100-1000 mV) but might become too small to resolve (< 0.1mV) at high salinity (0.5-2 mol/L), depending on how the available data for the electrokinetic coupling at low salinity are extrapolated into the high-salinity domain. More work remains to determine the behavior of electrokinetic coupling and therefore the utility of this technique at high salinity.
机译:电动势的井下测量是用于油气藏监测的有前途的新技术。使用结合了多相流和电动成分的3D有限元模型,我们研究了在一系列油藏环境中采油过程中电动(流动)电势的行为。我们发现,流势信号起源于流体饱和度变化的流体前沿和地质边界。当水侵蚀采油井时,与水前沿相关的流电势信号即使在最远100 m处仍会包围该井,因此,相对于远处的参比电极,该井处测得的电势开始显着变化。可以使用沿井定位的电极阵列来表征侵蚀性水锋的几何形状的变化,但是需要对当地的储层地质有很好的了解才能识别由水锋引起的信号。在高速率生产的低渗透油藏和低页岩含量的厚油藏中,井中测得的流动潜力最大。然而,仍然存在相当大的不确定性,特别是与高盐度和多相流期间的电动耦合的性质有关。我们的结果表明,在低盐度(10(-3)-10(-4)mol / L)下的流电势很大(100-1000 mV),但在高盐度下可能变得太小而无法分辨(<0.1mV)( 0.5-2 mol / L),取决于如何将低盐度电动耦合的可用数据外推到高盐度域中。要确定电动耦合的行为以及因此在高盐度下该技术的实用性,还有更多工作要做。

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