This activity provides an approach to teach field methods that is programmed to avoid common pitfalls in teaching field methods to students. The two common problems that are avoided is familiarity with equipment and improved group function.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

This project is designed to introduce students to a local hydrogeologic problem or issue of interest to the community. The project requires the students to learn about their local groundwater environment and apply principles and concepts that they learn in the classroom to an issue that is of concern to the public. This project provides a good introduction to "real world" problems that the students are likely to encounter as professionals. Students are required to synthesize information from a variety of sources and develop their own assessment of the problem and also to make recommendations based on their professional opinions.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

This is an assignment I worked on with Dr. Brusseau (University of Arizona) for his Contaminant Transport class. In this problem solving exercise, students are provided data sets that could be obtained by monitoring flow and transport of a tracer or contaminant in the field or in a soil column experiment in the laboratory. They will need to input the equations into a spreadsheet to complete the assignment.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

This unit provides students with experience analyzing traditional (depth to water table measured in a well) and geodetic: GRACE (Gravity Recovery and Climate Experiment) data for monitoring changes in groundwater storage in the High Plains Aquifer. Variations across timescales are compared, from seasonal to interannual to decadal. This comparison highlights some of the challenges associated with quantifying changes in groundwater storage at the regional scale. Aquifer properties are used to consider changes in terms of both "depth to water table" and water storage. Students are asked to formulate explanations for the observed variations in the context of the water balance equation. Students compare their results to a multidecadal trend reported in the literature (Konikow, 2011).

Show more about Online Teaching suggestions
Hide
Online-ready: The exercise is electronic and could be done individually or in small online groups. Lecture is best done synchronously due to the technical nature. Discussion would be better that way too.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

In an out-of-class assignment, students receive background information for the site and the pump test performed, including the aquifer properties determined. Through a series of questions, students are asked to evaluate the pump test method, results, interpretations made by the consultant that performed the test, and the significance of a rain event that occurred during the test.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

This module looks at the feasibility of using deeper wells as a source of low As water. The data sets are described in detail by van Geen et al. (van Geen et al., 2003; van Geen et al., 2002).

Students are being introduced to background information about the Arsenic problem in Bangladesh in lecture format. This includes health aspects and the history of the issue. They also have been using the sand tank groundwater model distributed by the University of Wisconsin Stevens Point (https://www.uwsp.edu/cnr-ap/watershed/Pages/GroundwaterModelWorkshop.aspx) to develop an intuitive understanding of groundwater flow and transport and are familiar with basic hydrogeological concepts. They inject a dye into the shallow aquifer of the model and study how pumping effects the migration of the Arsenic plume (Fig 1).

Students get an Excel spreadsheet that contains the longitude, latitude, and depth of 6000 wells and a satellite image that shows the area of investigation. They use Arc GIS software to plot data on the satellite image (Fig. 2), or alternatively plot the data as a function of longitude and latitude as a bubble plot in Excel. They find that the distribution of As in many regions is very heterogeneous. They then select sub-regions and look at the depth distribution and find that often there is a gap in the depth population of wells which turns out to be due to a clay layer varying in thickness that separates the shallow aquifer from the deep aquifer. The depth distribution (Fig. 3) of As also shows a characteristic pattern with most of the elevated As concentrated in the top 30 meters.
Students then discuss remediation options, in particular the possibility of switching to neighboring wells and using deeper groundwater as an alternative source of drinking water. They find that in many regions there are safe wells within a few hundred m of the high As well. However, it is not clear how long these wells will remain low in dissolved As and there are social barriers as well to use the neighbors well. They then determine a depth below which As concentrations are low in their region and elevate the risk of using deeper groundwater for drinking water and irrigation. They find that personal use is resulting in only ~1cm year-1 of water use, while irrigation (~1 m year-1) would considerably lower the water table and potentially could contaminate the deeper aquifer as well. The conclusion is that if deeper groundwater is utilized its use should be limited to personal use.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

The assignment will begin with teaching proper water collection and use of equipment for hydrochemical field work. Once the class is familiar with sample collecting technques, the class takes a field trip to several springs within the Madera Limestone, Sandia Mountains New Mexico. Collecting waters and obtaining hydrochemical field parameters for each spring location as well as collecting groundwater from one well in the same aquifer. Returning to the lab and preparing and running samples for ion analysis.

Spring waters will then be compared to well water and average precipitation data available from the USGS. Geochemical modeling will then be completed to understand the proportion of aquifer, precipitation and possible deeply sourced waters found in the spring waters.

The outcomes include 1) teaching proper sampling techniques 2) proper preparation of samples for ion analysis 3) Geochemical modeling to understand mixing

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

To prepare for this project / assignment, students could view the 'A Civil Action' movie, the instructor could read to them excerpts from the book and/or the trial testimony, and show them images from Woburn, wells G and H, the subsurface geologic materials, geologic cross sections, the trial participants, and the federal courtroom in Boston (see below). The materials in Bair (2001) about scientists in the courtroom, specific (excerpted) testimony presented by the three expert witnesses in the 'A Civil Action' trial, a chart summarizing the differences in their testimony, and the views of a federal judge on the goal of science versus the goal of a civil trial may also be worthwhile reading by the class prior to the assignment.

The instructor could show students the large plates included in the USGS report by Myette and others (1987) that display potentiometric data and contours before and after the critically important aquifer test performed in December 1985 and January 1986, just before the trial, and discuss the significance of the stream discharge measurement made by the USGS upstream and downstream of municipal wells G and H to the experts' testimony and the outcome of the trial.

The instructor could also show the animations of TCE movement from 1960 to 1986 from the five known sources of TCE contamination at the Woburn Wells G & H Superfund Site (W.R. Grace, UniFirst dry cleaners, Olympia Trucking, Beatrice Foods, and New England Plastics) and the animation showing temporal changes in induced infiltration from the Aberjona River to wells G and H that were created by Martin van Oort (M.S., 2005) based on the research of Maura Metheny (M.S., 1998; Ph.D., 2004) at Ohio State University.

The article by Bair and Metheny (2002) concerning the remediation activities subsequent to the famous trial at the Wells G & H Superfund Site could be used to show how groundwater contamination is cleaned up, why different remediation schemes needed to be used in different hydrogeologic settings, and why cleanup to U.S. EPA standards can take decades.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

In this exercise, students predict changes in the movement of a dissolved plume in response to remedial pumping in an unconfined aquifer. The underlying conceptual model for the distribution of aquifer and aquitard materials is not known with certainty. Consequently, two alternative end-member conceptualizations are presented to students who are then asked to hypothesize differences in predicted responses at the pumping wells and nearby monitoring wells for each conceptual model. Predictions are compared to actual field data, and students discover that contaminant concentration measurements depend not only on the location of the observation point (in three dimensions), but also on the length of the screened interval through which water samples are collected. The activity is divided into three parts: (1) site/problem description, (2) formulation and testing of hypotheses for pumping wells, and (3) formulation and testing of hypotheses for monitoring wells. The activity gives students practice in three dimensional thinking and reinforces their intuitive understanding of contaminant plume migration in response to natural gradients and engineered stresses.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)

This exercise uses an analytical method (Grubb, 1993) and Excel to calculate the capture zone shape for a TCE remediation well in Wooster, Ohio. The case study description given in an extensive PowerPoint presentation. The capture-zone equations are programmed by the student into an Excel worksheet and used to delineate the contributing area of a contaminant recovery well. Students can then experiment with by varying the pumping rate, hydraulic conductivity, and hydraulic gradient to better understand the sensitivity of these parameters on capture-zone shape.

(Note: this resource was added to OER Commons as part of a batch upload of over 2,200 records. If you notice an issue with the quality of the metadata, please let us know by using the 'report' button and we will flag it for consideration.)