双透射率数学模型及其在解释beŁchatÓw褐煤矿测压试验中的应用实例

F. Wolny, M. Jamróz, J. Gasiński, M. Marciniak, M. Kaczmarek
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摘要

诸如段塞测试或paramx测试之类的压力测试通常会观察到水位的阻尼振荡或指数运动。然而,在一些试验中,记录了地下水位的双指数响应。双指数运动可能表明在压力表筛网周围存在双渗透性介质。该介质由两个子域组成,每个子域具有不同的水力特性(包括透过率,T)。本文旨在建立两个数学模型-分段指数模型和双指数模型-以解释在Bełchatów褐煤矿非均质沉积物中进行的段塞试验结果。介绍了几种压电计双透射率估计的理论背景、解释算法和实例。使用paramx 4和MATLAB软件进行所有必要的计算。此外,还讨论了解释算法的局限性。
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MATHEMATICAL MODELS OF DUAL TRANSMISSIVITY AND EXAMPLES OF THEIR APPLICATION IN INTERPRETING PIEZOMETRIC TESTS CONDUCTED IN THE BEŁCHATÓW LIGNITE MINE
Piezometric tests such as the slug test or PARAMEX test usually result in observing damped oscillations or exponential movement of the water level. However, during some tests, a bi-exponential response of the water table has been recorded. Bi-exponential movement may indicate the presence of a dual-permeability medium around the piezometer screen. Such medium is composed of two subdomains, each characterized by different hydraulic properties (including transmissivity, T). The paper aims to present two mathematical models – the piecewise exponential model and the bi-exponential model – which were applied in order to interpret the results of slug test conducted in heterogeneous sediments of the Bełchatów Lignite Mine. Theoretical background, interpretation algorithms and examples of dual transmissivity estimation for several chosen piezometers are presented. All necessary calculations were performed using Paramex 4 and MATLAB software. Furthermore, the limitations of the interpretation algorithms are discussed.
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ZŁOTO W POTOKACH I PEGMATYCIE Z REJONU STRZELINA ROZPOZNANIE LOKALIZACJI WYROBISK PIASKÓW I ŻWIRÓW WZGLĘDEM GRANIC GZWP ORAZ CIEKÓW POWIERZCHNIOWYCH NA OBSZARZE WOJEWÓDZTWA ŚLĄSKIEGO INTERPRETACJA ZMIENNOŚCI TEMPERATURY WODY W ŹRÓDLE NA WSCHODNIM STOKU ZAMECZKÓW (TATRY ZACHODNIE) NA PODSTAWIE CIĄGŁYCH OBSERWACJI MONITORINGOWYCH I NUMERYCZNEGO MODELU TRANSPORTU CIEPŁA PARAMETRY MIGRACJI ZANIECZYSZCZEŃ W ODPADACH FLOTACYJNYCH NA PODSTAWIE TERENOWEGO EKSPERYMENTU ZNACZNIKOWEGO NA PRZYKŁADZIE OBIEKTU UNIESZKODLIWIANIA ODPADÓW WYDOBYWCZYCH „GILÓW” ZRÓŻNICOWANIE TŁA HYDROGEOCHEMICZNEGO WÓD PODZIEMNYCH EKSPLOATOWANYCH W ZLEWNI BIEBRZY
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