
Explore groundwater hydrology concepts, including groundwater occurrence, aquifers, Darcy's law, groundwater flow, well design, pollution, saline water intrusion, and protection, within a four-section course structure.
Explore groundwater flow and hydrology, defining groundwater, its occurrence, distribution, and movement beneath the earth, and learn about aquifers, confined and unconfined, aquicludes, wells, artesian springs, and irrigation zones.
Explore groundwater aquifer characteristics, including porosity, specific yield, specific retention, specific storage, and storage coefficient, then analyze hydraulic conductivity and transitivity via Darcy's law.
Explore groundwater aquifer characteristics, focusing on specific storage and storage coefficient, their equations and relation to confined and unconfined aquifers, and practical examples for porosity and water volume calculations.
Examine differentiated aquifer properties, including homogeneous vs heterogeneous and isotropic vs anisotropic hydraulic conductivities, and compute horizontal, vertical, and beta directional equivalents (kh=7.25, kv=4.42, k45=5.49 m/day) from a three-layer example.
Apply groundwater movement principles using Darcy's law, hydraulic conductivity, and hydraulic gradient to calculate flow velocity, actual velocity with porosity, head losses, and determine movement direction from multiple wells.
Apply groundwater hydrology concepts to analyze steady unidirectional flow to wells in confined and unconfined aquifers using Darcy's law, calculating head differences, discharge, and equivalent hydraulic conductivity.
Apply flow-tool methods to compute the maximum groundwater rise, its location, travel times to rivers, and daily discharge per kilometer for an unconfined sand and gravel aquifer with recharge.
Explore steady radial flow to pumping wells in confined and unconfined aquifers, focusing on static and pumping water levels, drawdown, cone of depression, and radius of influence.
Explore steady-state radial flow in unconfined aquifers and compare with confined aquifers, deriving hydraulic conductivity from pumping tests and analyzing recharge and well design.
Apply unsteady radial flow analysis in a confined aquifer with the Jacob and Cooper method to relate drawdown, time, and distance, and compute transitivity and storage coefficient from pumping data.
Analyze three confined aquifers in series to compute flow rates and head losses using Darcy's law, and determine equivalent horizontal and vertical hydraulic conductivities, plus heads at specified distances.
Solve groundwater discharge and drawdown problems in unconfined and confined aquifers using hydraulic conductivity, recharge, and pumping calculations. Estimate greatest groundwater level rise and well drawdown from pumping.
Explore the construction and design of groundwater wells, including dug wells, driven wells, and jetted wells, with casing, screens, gravel covers, development, and key specifications shaping depth, diameter, and productivity.
Analyze groundwater problems and water supply wells, including pollution sources from surface waste, septic tanks, fertilizers, and leakage, and how drawdown and specific capacity affect well productivity.
Examine saline water intrusion in coastal aquifers, its sources and mechanisms, and apply control strategies such as pumping pattern modification, artificial recharge, and barrier methods.
This course is structured into four sections with 16 lectures, each covering a specific topic related to groundwater hydrology.
The sections are as follows:
Section 1: Introduction
In this section, you will identify the main objectives and the structure of “Apply Groundwater Hydrology Concepts” course.
Section 2: Groundwater Hydrology Concept
In this section, you will learn about groundwater hydrology definition, occurrence and properties. You will identify the difference between groundwater layers and the difference between confined and unconfined aquifers. You will also learn how to determine the equivalent hydraulic conductivity and groundwater investigation.
Section 3: Groundwater Movement
In this section, you will learn about Darcy’s Law and how to determine the actual groundwater discharge and flow velocity through confined and unconfined aquifers for steady state. You can also learn about flow to wells.
Section 4: Well Construction and Groundwater Problems
In this section, you will learn about the well functions, the methods of shallow and deep wells construction, the well's completion and the well development. You will identify the causes of groundwater pollution, supply well problems and how to protect them. You will learn how the saline water intrusion occurred and how to draw the shape of the surface separating fresh and salt water. You will also learn how to control of saline water intrusion.