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Application of the error propagation theory in estimates of static formation temperatures in geothermal and petroleum boreholes

机译:误差传播理论在地热和石油井筒静态地层温度估算中的应用

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We used the error propagation theory to calculate uncertainties in static formation temperature estimates in geothermal and petroleum wells from three widely used methods (line-source or Horner method; spherical and radial heat flow method; and cylindrical heat source method). Although these methods commonly use an ordinary least-squares linear regression model considered in this study, we also evaluated two variants of a weighted least-squares linear regression model for the actual relationship between the bottom-hole temperature and the corresponding time functions. Equations based on the error propagation theory were derived for estimating uncertainties in the time function of each analytical method. These uncertainties in conjunction with those on bottom-hole temperatures were used to estimate individual weighting factors required for applying the two variants of the weighted least-squares regression model. Standard deviations and 95% confidence limits of intercept were calculated for both types of linear regressions. Applications showed that static formation temperatures computed with the spherical and radial heat flow method were generally greater (at the 95% confidence level) than those from the other two methods under study. When typical measurement errors of 0.25 h in time and 5℃ in bottom-hole temperature, were assumed for the weighted least-squares model, the uncertainties in the estimated static formation temperatures were greater than those for the ordinary least-squares model. However, if these errors were smaller (about 1% in time and 0.5% in temperature measurements), the weighted least-squares linear regression model would generally provide smaller uncertainties for the estimated temperatures than the ordinary least-squares linear regression model. Therefore, the weighted model would be statistically correct and more appropriate for such applications. We also suggest that at least 30 precise and accurate BHT and time measurements along with the respective errors should be obtained for a reliable application of the proposed regression procedure.
机译:我们使用误差传播理论从三种广泛使用的方法(线源或霍纳法;球形和径向热流法;以及圆柱热源法)计算地热井和石油井中静态地层温度估算的不确定性。尽管这些方法通常使用本研究中考虑的普通最小二乘线性回归模型,但我们还评估了加权最小二乘线性回归模型的两种变型,以了解井底温度与相应时间函数之间的实际关系。推导了基于误差传播理论的方程,用于估计每种分析方法的时间函数中的不确定性。这些不确定性与井底温度的不确定性一起用于估算应用加权最小二乘回归模型的两个变体所需的各个加权因子。两种线性回归类型均计算了标准差和截距的95%置信限。应用表明,用球形和径向热流方法计算的静态地层温度通常要高(在95%的置信水平下),高于其他两种正在研究的方法。假设加权最小二乘模型的典型测量误差为时间0.25 h,井底温度为5℃,则估计的静态地层温度的不确定性要大于普通最小二乘模型的不确定性。但是,如果这些误差较小(时间上的误差约为1%,温度测量值的误差约为0.5%),则与常规最小二乘线性回归模型相比,加权最小二乘线性回归模型通常会为估计的温度提供较小的不确定性。因此,加权模型在统计上将是正确的,并且更适合此类应用。我们还建议,为了可靠地应用所提出的回归程序,至少应获得30次精确且准确的BHT和时间测量值以及相应的误差。

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