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| Content Provider | Springer Nature Link |
|---|---|
| Author | Edwards, David A. |
| Copyright Year | 2010 |
| Abstract | Parameters employed in the Cooper-Jacob equation to describe drawdown are transmissivity, storativity, radial distance, time and pumping rate. An approach is described for quantifying how error or uncertainty in any one of the parameters used causes error in estimated drawdown. Dimensionless fractional error in estimated drawdown is expressed quantitatively as a function of (1) dimensionless fractional error of a given parameter, and (2) dimensionless argument of the well function, u. Fractional error in estimated drawdown is a linear function of fractional error in pumping rate and, for any given value of u, a nonlinear function of fractional error in transmissivity, storativity, radial distance or time. Fractional error in estimated drawdown for a given fractional parameter error varies considerably between parameters. The greatest sensitivity is for transmissivity and flow rate. Sensitivity is less for radial distance and time, and even less for storativity. The magnitude of the fractional error in drawdown may be affected by the sign of the fractional parameter error.Les paramètres utilisés dans l’équation de Cooper-Jacob pour décrire le rabattement sont la transmissivité, l’emmagasinement, la distance radiale, la durée et le régime de pompage. Une approche est décrite pour quantifier comment une erreur ou une incertitude sur un quelconque des paramètres utilisés entraîne des erreurs dans l’évaluation du rabattement. Une erreur relative sans dimension dans l’évaluation du rabattement est exprimée quantitativement comme une fonction (1) de l’erreur relative sans dimension d’un paramètre donné, et (2) de la raison sans dimension de la fonction de puits, u. Une erreur relative dans l’évaluation du rabattement est une fonction linéaire de l’erreur relative sur le régime de pompage et, pour n’importe quelle valeur de u, une fonction non linéaire de l’erreur relative sur la transmissivité, l’emmagasinement, la distance radiale ou la durée. L’erreur relative dans l’estimation du rabattement pour une erreur relative donnée sur un paramètre varie considérablement d’un paramètre à l’autre. La sensibilité la plus grande est pour la transmissivité et le régime d’écoulement. La sensibilité est moindre pour la distance radiale et la durée, et même moins pour l’emmagasinement. L’amplitude de l’erreur relative pour le rabattement peut être affectée par le signe de l’erreur relative sur le paramètre.Los parámetros empleados en la ecuación de Cooper-Jacob para describir la depresión son la transmisividad, el almacenamiento, la distancia radial, el tiempo y el ritmo de bombeo. Se describe una aproximación para cuantificar como el error o incerteza en cualquiera de los parámetros usados provoca un error en la depresión estimada. El error fraccional adimensional en la depresión estimada está expresado cuantitativamente como una función de (1) error fraccional adimensional de un parámetro determinado, y (2) el argumento adimensional de la función de pozo, u. El error fraccional en la depresión estimada es una función lineal del error fraccional del ritmo de bombeo y, para cualquier valor dado de u, una función no lineal del error fraccional de la transmisivad, almacenamiento, distancia radial o tiempo. El error fraccional en la depresión estimada para un dado error fraccional de un parámetro varía considerablemente entre los parámetros. La mayor sensibilidad es para la transmisividad y el ritmo de flujo. La sensibilidad es menor para la distancia radial y el tiempo, y aún menor para el almacenamiento. La magnitud del error fraccional en la depresión puede ser afectada por el signo del error fraccional del parámetro.库珀雅各布方程中用于估算降深的参数为导水系数, 贮水系数, 径向距离, 时间和抽水量。本文介绍的一种方法可以用于估算其中任一参数对降深估算精度的影响。降深估算中的无量纲的相对误差被表示为以下值的定量函数: (1)给定参数的无量纲相对误差 (2) 井函数的无量纲自变量u。降深中的相对误差是抽水量相对误差的线性函数。对于任何给定的u值, 降深相对误差是导水系数, 贮水系数, 径向距离和时间相对误差的非线性函数。对于一个给定的相对参数误差, 降深的相对误差在参数之间有很大不同。最敏感的是导水系数和流量。径向距离和时间敏感度较Os parâmetros utilizados na equação de Cooper-Jacob para descrever o rebaixamento são a transmissividade, o coeficiente de armazenamento, a distância radial, o tempo e o caudal de bombagem. Descreve-se uma abordagem para quantificar como o erro ou a incerteza em qualquer um dos parâmetros utilizados provoca erros na estimativa do rebaixamento. O erro relativo adimensional na estimativa do rebaixamento expressa-se quantitativamente em função do (1) erro relativo adimensional de um dado parâmetro, e (2) argumento adimensional da função do poço, u. O erro relativo no rebaixamento estimado é uma função linear do erro na taxa de bombeamento, e, para cada valor de u, uma função não linear do erro relativo na transmissividade, coeficiente de armazenamento, distância radial ou tempo. O erro relativo no rebaixamento estimado para o erro relativo de um dado parâmetro varia consideravelmente entre parâmetros. A maior sensibilidade é para a transmissividade e para o caudal. A sensibilidade é menor para a distância radial e o tempo, e ainda menor para o coeficiente de armazenamento. A magnitude do erro relativo no rebaixamento pode ser afectada pelo sinal do erro relativo do parâmetro. |
| Starting Page | 1069 |
| Ending Page | 1076 |
| Page Count | 8 |
| File Format | |
| ISSN | 14312174 |
| Journal | Hydrogeology Journal |
| Volume Number | 18 |
| Issue Number | 5 |
| e-ISSN | 14350157 |
| Language | Portuguese |
| Publisher | Springer-Verlag |
| Publisher Date | 2010-03-05 |
| Publisher Institution | International Association of Hydrogeologists |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Analytical solutions Groundwater hydraulics Fractional error Uncertainty Analysis Waste Water Technology Water Pollution Control Water Management Aquatic Pollution Geology Hydrogeology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences Water Science and Technology |
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