Jupyter Notebook for Computing the Well Function Using the Theis Equation

The Theis equation models the drawdown in an unconfined aquifer based on a given pumping rate, transmissivity, and storativity. A classic equation in hydrogeology, this example has been programmed into a Jupyter notebook. This educational resources is targeted at upper-level undergraduate students and is intended to supplement lectures or homework assignments on well hydraulics. The primary learning objectives are to identify the purpose of the equation, determine appropriate inputs and outputs, and predict the extent of drawdown around a well. Secondary objectives are to refresh skills associated with scientific and programming and learn to use a Jupyter notebook. A companion notebook to be used for pump test analysis is also available (see related resources).

**Open in native Jupyter Notebook format by clicking the blue "open with" button in the top right corner on Hydroshare. Requires numypy, matplotlib, and math libraries; Python 3 Scientific environment recommended.**

Theis 方程式基于给定的抽水速率、透水率和储水率，对无界含水层中的降深进行建模。作为水文地质学中的经典方程，此例已编程至 Jupyter 笔记本中。该教育资源旨在面向高年级本科生，旨在补充井水力学课程的教学或作业。主要学习目标在于识别方程式的作用、确定适当的输入和输出以及预测井周降深范围。次要目标包括复习与科学和编程相关的技能，并学习使用 Jupyter 笔记本。此外，还提供了一本用于泵测试分析的配套笔记本（参见相关资源）。通过在 Hydroshare 顶部右侧点击蓝色“以原格式打开”按钮，可在原生 Jupyter 笔记本格式中打开。需使用 numypy、matplotlib 和 math 库；建议使用 Python 3 科学环境。