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首页> 外文期刊>Journal of Hydrology >Depth-discrete specific storage in fractured sedimentary rock using steady-state and transient single-hole hydraulic tests
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Depth-discrete specific storage in fractured sedimentary rock using steady-state and transient single-hole hydraulic tests

机译:稳态和瞬态单孔水力试验在裂隙沉积岩中的深度离散比存储

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A method is presented for obtaining depth-discrete values of specific storage (Ss) from single-hole hydraulic tests in fractured rock boreholes using straddle packers (1.5-17 m test intervals). Low flow constant head (CH) step tests analyzed using the Thiem method provide transmissivity (T) values free from non-Darcian error. Short-term, constant-rate pumping tests (0.5-2 h) analyzed using the Cooper-Jacob approximation of the Theis method provide S from the hydraulic diffusivity using the Darcian T value from the CH step test. This synergistic use of two types of hydraulic tests avoids the common source of error when pumping tests (injection or withdrawal) are conducted at higher flow rates and thereby induce non-Darcian flow resulting in the underestimation of T. Other errors, such as well bore storage and leakage, can also substantially influence S by causing a shift in the time axis of the Cooper-Jacob semi-log plot. In this approach, the Darcian T values from the CH step tests are used in the analysis of the transient pumping test data for calculating S throughout the pumping test using the Cooper-Jacob approximation to minimize all of the aforementioned errors, resulting in more representative S values. The effect of these non-idealities on the measured drawdown is illustrated using the Theis equation with the Darcian T and S values to calculate drawdown for comparison to measured data. The Ss values for tests in sandstone obtained from this approach are more consistent with confined aquifer conditions than values derived from the traditional Cooper-Jacob method, and are within the range of field and lab values presented from a compilation of literature values for fractured sandstone. (10(-7)-10(-5) m(-1)) This method for obtaining Ss values from short-interval, straddle packer tests improves the estimation of both K and Ss and provides opportunity to study their spatial distribution in fractured rock. (C) 2016 Elsevier B.V. All rights reserved.
机译:提出了一种使用跨式封隔器(1.5-17 m测试间隔)从裂隙岩孔中的单孔水力测试中获得特定储量(Ss)的深度离散值的方法。使用Thiem方法分析的低流量恒压头(CH)阶跃测试可提供无非达西误差的透射率(T)值。使用Theis方法的Cooper-Jacob近似进行的短期恒速泵送测试(0.5-2 h),使用CH阶跃测试的Darcian T值,通过水力扩散率提供S。两种液压测试的这种协同使用避免了在较高流量下进行泵送测试(注入或抽出)时常见的误差源,从而导致非达西渗流,从而导致T的低估。其他误差,例如井筒存储和泄漏也会通过引起Cooper-Jacob半对数图的时间轴偏移而对S产生实质性影响。在这种方法中,将CH阶跃测试中的Darcian T值用于瞬态泵浦测试数据的分析,以便在整个泵浦测试中使用Cooper-Jacob逼近来计算S,以最大程度地减少上述所有误差,从而得到更具代表性的S价值观。这些非理想因素对测得的压降的影响通过使用Theis方程和Darcian T和S值来计算压降以与测得的数据进行比较来说明。与从传统的Cooper-Jacob方法获得的值相比,通过这种方法获得的砂岩测试的Ss值与受限的含水层条件更加一致,并且在裂隙砂岩文献值汇编中给出的田间和实验室值范围内。 (10(-7)-10(-5)m(-1))这种从短间隔跨装填机测试获得Ss值的方法改善了对K和Ss的估计,并提供了研究裂缝中它们的空间分布的机会岩。 (C)2016 Elsevier B.V.保留所有权利。

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