首页> 外文期刊>Journal of Water Resource and Protection >Use of a Multiple Regression Model in the Estimation of Water Borehole Flows in the Middle of Cracked Basement in Côte d’Ivoire
【24h】

Use of a Multiple Regression Model in the Estimation of Water Borehole Flows in the Middle of Cracked Basement in Côte d’Ivoire

机译:在C&#244中的裂纹地下室中间使用多元回归模型在水钻孔中间流动。TE D'IVOIRE

获取原文
           

摘要

The objective of this study was to propose a mathematical regression model to estimate the exploitation flow rate of a water borehole from geophysical parameters in the midst of a fissured basement in the central-eastern part of C ? te d’Ivoire. The data of the study are both hydrogeological and geophysical parameters from one hundred and eleven (111) data sheets of (111) water and geophysical boreholes. Two methods were used. The Normal Principal Component Analysis (NPCA) method applied to the data made it possible to select the explanatory variables (geophysical parameters) for borehole productivity. The multiple linear regression method subsequently made it possible to propose a mathematical model capable of estimating the exploitation rate from the geophysical parameters. The results indicate a very strong correlation (0.87) between longitudinal conductivity and flow rate, with flow rate and apparent resistivity negatively correlated. The multiple linear regression method highlighted two relevant explanatory variables, longitudinal conductivity and apparent resistivity. These two geophysical parameters contributed to a mathematical model in the form Q = C _(1) X _(1) + C _(2) X _(2) + ... + C _(n) X _(n) + C _(0) . the real model obtained in this work is Q = 0.82 Cl - 0.12 Rho.app + 2.5 . The resulting model is efficient with a correlation of 86% in calibration and 95% in validation. A bias of 0.37 in calibration and 0.82 in validation is observed. Finally, the square root mean square error (RMSE) is 3.10 to 3.38 respectively in calibration and validation.
机译:本研究的目的是提出一种数学回归模型来估计C中央东部地区裂隙地下部地球物理参数的水钻孔的开发流速? te d'ivoire。该研究的数据是(111)水和地球物理钻孔的一百和十一(111)数据片的水文地质和地球物理参数。使用了两种方法。应用于数据的正常主成分分析(NPCA)方法使得可以选择用于钻孔生产率的解释性变量(地球物理参数)。随后使多个线性回归方法提出能够估计来自地球物理参数的利用率的数学模型。结果表明纵向导电性和流速之间的具有非常强的相关性(0.87),流速和表观电阻率负相关。多元线性回归方法强调了两个相关的解释变量,纵向导电性和表观电阻率。这两个地球物理参数有助于Q = C _(1)x _(1)x(1)+ c x(2)x _(2)+ ... + c _(n)x _(n)中的数学模型+ C _(0)。在此工作中获得的真实模型是Q = 0.82 CL - 0.12 rho.app + 2.5。结果模型有效,校准中的86%的相关性和95%的验证。观察到校准0.37的偏差和0.82在验证中。最后,在校准和验证中,平方根均方误差(RMSE)分别为3.10至3.38。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号