In this activity students examine groundwater flow path based on hydraulic head data/ potentiometric surface and spatial variation of groundwater chemistry. Students analyze the data using AquaChem and Phreeqc which is integrated with AquaChem

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Well Field Practice: aquifer characterization through conducting and interpreting of aquifer pump tests.

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First assignment of the course

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This assignment reviews basic of chemistry for students who should have had 2 introductory semesters of basic chemistry prior to enrolling in the Fundamental of Water Quality course for which the assignment is used. Assignment reviews basic equation balancing and questions about valence and concentration conversion that students will confront regularly in any geochemistry course.

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Introduction:
Groundwater is key to Texas future and economy. The resource has long been a focus of legislative and economic interest. In the earliest days, the resource was viewed as 'occult and hidden.' That sense of mystery remains even as groundwater becomes more critical to the water resource picture for the state.
Since 1951, the state conducts regional water planning with the involvement of citizen stakeholders. Let's use your science-based knowledge of groundwater flow to see if you can find the right balance for both protecting and planning for groundwater use.
Our Case:
This week we will evaluate a historic court case from June 13, 1904. The case of East versus Texas Central Railroad Company is the Texas Supreme Ruling that provides the foundation for Texas groundwater law -- Rule of Capture.
In the appendix, you will find the following figures to help you determine whether or not Mr. East's well was impacted by the railroad company's pumping:

Platt map showing well locations and possible distances
Schematics of the well dimensions, along with simplified subsurface geology in the area.

In addition, you will be interested in knowing that the Geologic Atlas of Texas shows that the wells were likely completed in the Pawpaw Formation, which is a thick calcareous clay unit in the lower sections and cemented sand in the upper part. Lithologies in the area are reported to yield limited to moderate amounts of water in shallow wells. You can expect that the formation was an unconfined unit and assume that the East well is down-gradient from the Railroad well.
Assignment Part One:

1. Using the information from our last lecture, what do you think a reasonable transmissivity rate might be for the Pawpaw formation?

a. Estimate a transmissvity for a cemented sand unit.
b. Use this value as your first estimate in calculations to calculate the potential drawdown with Jacob's equation. This calculates the drawdown in an nonleaky artesian aquifer, sa, given the observed water table drawdowns.

sa = swt -- (s2st/2m)

c. Calculate swt using a correction equation.

Swt = m-(m2-2msa)1/2

Where m is the initial saturated thickness, which you may estimate at 30 ft.

2. How much water do you estimate that the railroad can extract before the well is impacted? Complete a diagram showing estimated drawdown (ft) on the y-axis and distances from the Railroad well (ft) using different transmissivity values and different distances. What do you discover about the case?
3. With your hydrogeologic analysis, do you believe that the East well was impacted by the railroad well? Can you explain how significant the impact may or may not have been?

Climate Considerations:
Is it possible that climate conditions could have impacted conditions in the well? Visit the Greenleaf website ([greenleaf.unl.edu/downloads/scPDSI.zip]) and access data for Palmer Drought Severity Indices. Looking at this data, complete the next questions.
Assignment Part 2:

4. Looking at the drought severity index maps of Texas from October 1900 to September 1902. What kind of implications might climate conditions have had on the groundwater conditions?
5. If climate conditions worsened, what do you think would happen to the wells?

Reference:
Mace, R.E., Ridgeway, C., and Sharp, J.M., 2004, Groundwater is no longer secret and occult - A historical and hydrogeologic analysis of the East case, 100 Years of Rule of Capture: From East to Groundwater Management, ed. Mullican, W.F. and Schwarz, S., Report 361, Texas Water Development Board, 63-86 pp.
Appendix -- support documents:
Figure 1 shows that Mr. East lived in Denison County, TX. The inset is a plan view map showing the potential locations of the wells in the town.
(in supporting documents)
Figure 2: Schematic of well dimensions and simplified geology.
(In supporting documents)

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This assignment is meant to illustrate how the advection of heat by groundwater leads to the elevated temperatures at shallow sedimentary basin margins at which Mississippi Valley-type Zn-Pb hydrothermal ore deposits are formed. The assignment is based on analytical solutions for groundwater flow and heat transport published by Domenico & Palciauskas (1973). Students use a spreadsheet to calculate and plot the flow field and temperature in a sedimentary basin, and to investigate the conditions needed to produce ore-forming temperatures. These results have further implications for the length of time available for ore formation and the concentration of metals and pH of the groundwater, which are also explored in the assignment. The assignment provides an example of how groundwater plays a fundamental role in an important geologic process in the Earth's crust. The activity also shows the linkages of hydrology to other disciplines such as heat transport, geochemistry, and economic geology.

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This homework assignment is designed to give the students practice in developing a simple conceptual model using reservoirs, fluxes, and simple calculations of sediment, carbon and nutrient accumulation in a typical reservoir/river system. This assignment is typically used after an introductory lecture to biogeochemical cycles and gives the students a concrete example of nutrient and sediment issues in surface water systems.

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This site teaches kids about the importance of safe drinking water through teaching and learning resources such as an activity on how to build your own aquifer, experiments on the water treatment process, and the drinking water art project.

This is an in-class activity analyzing our drinking water reservoir, but would apply to any reservoir for which there are basic crest/elevation data and maps available.

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This is a inquiry-driven class research project on a local environmental geochemistry question that is accomplished during three-hour laboratory sessions each week. Students are divided into groups that will share the responsibilities of collecting samples and data. Once the data is collected, it is shared among the entire class so that all students have the same data set. The class works on data presentation, preliminary analysis, and statistics together Then each student writes his/her own report separately.

Outcomes:

Laboratory skills -- Students have basic laboratory skills necessary to carry out a supervised geochemical study (e.g. can perform Gram titration of waters in field, can collect water samples using clean methods).

Quantitative methods -- Students can manipulate, sort, and transfer data in Excel and can create simple x-y plots and histograms to bring out trends in data.

Critical thinking -- Students can develop multiple hypotheses to explain trends in data and can design tests of these hypotheses.

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This is an independent case study project completed in pairs. The students should investigate an example of natural geochemistry and then use a poster format to share their findings with the class.

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Course combines the fields of ecology and conservation with planning for the efficient use and preservation of land, water, wildlife, and forests. Within this course may be topics covering environmental factors affecting water, water pollution, water and land use management, alternative energy resources, metals and minerals.
** References to Common Core Standards are included as the first slide in each lesson's PowerPoint**

Students make measurements of dam dimensions and water levels above and below a small, accessible earthen dam. They assess the soil texture in the field. They follow up by developing a simple flow net and estimating seepage rate as part of a problem set. They discuss their assumptions and the likely sources and magnitude of error.

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In this activity students use published data from the Massachusetts Military Reservation to observe and predict mass transport parameters.

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Between 70 and 75% of the Earth's surface is covered with water and there exists still more water in the atmosphere and underground in aquifers. In this lesson, students learn about water bodies on the planet Earth and their various uses and qualities. They will learn about several ways that engineers are working to maintain and conserve water sources. They will also think about their role in water conservation.

This project is used instead of a final exam in an upper level undergraduate course in Applied GIS. A student may propose their own project, or choose one from a list from the instructor. A brief proposal must be approved by the instructor before the project can begin. Students will construct a working, query-able database, use appropriate imagery, and use it to analyze a problem, understand cause and effect, and show changes with time. A final report must be submitted with all supporting documentation in digital form. Students also give a PP presentation in one of the last class meetings.

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Students work with data bases and GIS to develop saturated thickness maps. Each data base consists of observations made by drillers where they have encountered the High Plains aquifer base and the annual water-level measurements taken in wells screened in the High Plains aquifer by field technicians.

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As global population grows, so does the demand for water. Yet less than one percent of the planet’s supply is potable, and estimates suggest that 40% of humanity will not have access to clean water by 2025. Explore the complex issues surrounding this precious resource in this episode of America Abroad.

America Abroad is an award-winning documentary radio program distributed by Public Radio International (PRI) and broadcast on public radio stations nationwide. Each month, we take an in-depth look at a critical issue in international affairs and U.S. foreign policy.

To learn more visit http://www.americaabroad.org

This activity allows students to understand the groundwater flow. Using a groundwater map, they will draw flow lines and determine the discharge and rate of flow.

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The simulation has several conditions in which students are able to collect and analyze data. The first of these scenarios models the water table in an area where there has been no human development. Students observe the annual, cyclical pattern of the water table over a five-year time period, and then use this as the control for comparison to other scenarios. Students then investigate scenarios in which a city, or a city plus a farm, are added. Students can choose to add wells to the city and the farm and select well pumping rates to meet human consumption needs in the city. Wells that are added in the farm scenario have predetermined pumping rates and are active during the growing season only.

As students add wells and gather data, they observe the effects on the wetlands, outflow of the river, and changes to the water table. When a single cell on the map is selected, a graph is generated showing water table data over a five year period for that cell. Using the graphs, students can quantitatively make observations and use data in order to create computational models. They can analyze and interpret the results of pumping over time and the effect on the water table and river outflow. Students can calculate the area of the wetland using the graphs generated by the simulation for each scenario. Examining cross-sections of the map also encourages students to make qualitative observations.

Students can further investigate the relationship between surface and groundwater by adding a drought option to each scenario. Students will collect and analyze data as before, and draw conclusions across the investigated scenarios to understand the effects of drought. After examining current data and news articles from California, students are asked to construct explanations based on evidence collected in the simulation for how the availability of fresh water, in addition to natural hazards such as drought, and climate change, influence human activity.

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