Using geophysical log data to predict the fracture density in a claystone host rock for storing high-level nuclear waste

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Emese Tóth, Ervin Hrabovszki, Tivadar M. Tóth
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Abstract

Previously drilled boreholes of a host rock for a potential nuclear waste repository in Hungary revealed a highly fractured claystone rock body. A crucial step for characterizing the hydrodynamic behavior of such a fractured reservoir is fracture identification and accurate calculation of the fracture density. Although acoustic borehole televiewers provide a reliable base for determining the fracture density, older boreholes usually lack such data. However, conventional borehole geophysical measurements are often accessible in such cases. The aim of this study was to identify any correlations between well log data and fracture density. Multiple linear regression analysis was performed on data from two boreholes penetrating the Boda Claystone Formation in southwest Hungary. The upper section of the BAF-4 borehole was used for training, where the fracture density was estimated with a fit of R2 = 0.767. The computed regression function predicted the fracture density with high accuracy in both boreholes for all intervals with typical lithological features. However, in some sections where anomalous well log data indicated changes in the lithology, the prediction accuracy decreased. For example, the function underestimated the fracture density in sandy intervals.

Abstract Image

利用地球物理测井资料预测存放高放核废料的粘土岩宿主岩的裂缝密度
先前在匈牙利一个潜在的核废料储存库的宿主岩石上钻孔发现了一个高度断裂的粘土岩体。裂缝识别和裂缝密度的准确计算是表征此类裂缝性储层水动力特性的关键步骤。尽管声波井眼电视为确定裂缝密度提供了可靠的基础,但较老的井眼通常缺乏此类数据。然而,在这种情况下,通常可以使用常规的钻孔地球物理测量方法。这项研究的目的是确定测井数据与裂缝密度之间的相关性。对穿透匈牙利西南部Boda粘土岩组的两个钻孔数据进行了多元线性回归分析。BAF-4井眼上部用于训练,裂缝密度估计拟合R2 = 0.767。计算出的回归函数对具有典型岩性特征的所有井段的裂缝密度均有较高的预测精度。然而,在一些异常测井数据显示岩性变化的路段,预测精度下降。例如,该函数低估了砂质层段的裂缝密度。
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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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