In this video clip, a scientific expert tells us about the ocean acidification. Catherine Jeandel, oceanographer, is a CNRS researcher (French National Centre for Scientific Research) and researcher director at LEGOS (Laboratoire d'Etudes en Géophysique et Océanographie Spatiales), Toulouse, France. CLIM is a series of videos created by the OCE, Dorothée Adam-Mazard, Claire Adam-Mazard and the production company WATTSON. The first serie of videos as part of the OCE educational project dedicated to the theme Ocean & Cryosphere, in the context of climate change.

In this video clip, a scientific expert tells us about Sea ice melt.

In this video clip, a scientific expert tells us about the Sea level rise.

In this video clip, a scientific expert tells us about the Thermohaline circulation.

This is a field based exercise that exposes students to streams as a major agent of erosion and to methods of quantifying stream discharge by collecting data in the field. Students also apply basic navigation skills by using hand-held GPS devices and plotting longitude and latitude of the field sites under investigation.

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Students construct three-dimensional models of water catchment basins using everyday objects to form hills, mountains, valleys and water sources. They experiment to see where rain travels and collects, and survey water pathways to see how they can be altered by natural and human activities. Students discuss how engineers design structures that impact water collection, as well as systems that clean and distribute water.

Students learn about power generation using river currents. A white paper is a focused analysis often used to describe how a technology solves a problem. In this literacy activity, students write a simplified version of a white paper on an alternative electrical power generation technology. In the process, they develop their critical thinking skills and become aware of the challenge and promise of technological innovation that engineers help to make possible. This activity is geared towards fifth grade and older students and computer capabilities are required. Some portions of the activity may be appropriate with younger students. CAPTION: Upper Left: Trey Taylor, President of Verdant Power, talks about green power with a New York City sixth-grade class. Lower Left: Verdant Power logo. Center: Verdant Power's turbine evaluation vessel in New York's East River. In the background is a conventional power plant. Upper Right: The propeller-like turbine can be raised and lowered from the platform of the turbine evaluation vessel. Lower Right: Near the East River, Mr. Taylor explains to the class how water currents can generate electric power.

In an upper-level seminar course, students bear significant responsibility for their learning. This activity provides the framework to help them identify the exact topics that they will discuss throughout a course in Environmental Analysis. The students are given constraints so that they don't either wander completely aimlessly through the environmental literature or pick only papers on their favorite topic. They are instead asked to dip into the literature to find papers that deal with analysis of pollutants in air, water, and solid matrices, and to have at least one that is relevant to climate change.

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This unit consists of seven distinct activities that teach climate change, the water cycle, and the effects of the changing climate on water resources through the use of games, science experiments, investigations, role-playing, research, and creating a final project to showcase learning.

When water utility personnel recognized their groundwater withdrawals were damaging ecosystems in the Tampa Bay area, they found new ways to reduce their dependence on it.

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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Most students understand that water quality is an important issue, however many do not understand the complexity associated with the processes involved, the complex nature of estuarine systems, or the fact that management decisions are made based on available data sets that can be difficult at best to interpret. Students will be provided nutrient data in Excel for two Texas estuaries which they will supplement with additional information that they have compiled on these two estuaries during the duration of the course through a GIS database available to the entire class. Furthermore, students will retrieve information from the WWW to learn more about the specific estuaries and the nutrients of interest and their impacts on the environment.

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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 demonstration uses sulfuric acid and crushed copper ore (malachite) to produce a solution of copper sulfate and carbonic acid in a beaker. When a freshly sanded nail is dropped into the copper sulfate solution, native copper precipitates onto the nail. The process is similar to that of heap leaching at a copper mine. The entire set-up can be placed on a wheeled cart and completed in less than 15 minutes in class. Students enjoy seeing the copper crystals form on the nail, and the experiment provides the basis for many avenues of discussion, from chemical reactions and mineral formation to problems with mine tailings and acid mine drainage.

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Because many students are familiar with contouring methods, they can mechanically construct water table maps from canned data sets with ease. However, their contouring abilities may mask their level of understanding. This field exercise aims to instill a deeper understanding of the nature of a water table surface as students also learn fundamental hydrogeological field techniques.

The exercise is based at Newark Road Prairie, which is owned and managed by Beloit College and located approximately five miles from campus. The property contains native prairie, wetlands, and a small stream. Although many schools may not own similar types of properties, land managers are often willing to allow the installation of shallow wells on public lands (e.g., county parks, state wildlife areas). Seven shallow monitoring wells and four staff gages are currently installed at Newark Road Prairie.

When we arrive at the field site, we begin by making observations on the subtle changes in topography and the direction of stream flow. Although we have just carried in all of the field equipment, I ask what type of information we will need to create a water table map. Handouts for the exercise are distributed after this discussion (see Supplementary Materials below).

Students are divided into groups of three for the field portion of the exercise, although each student ultimately drafts their own map using group and class data. Each group gets an electronic water level meter, a GPS unit, and a measuring tape, and we discuss the magnitude of error incorporated into the measurements taken by each of the instruments. We then review basic operation procedures for the water level meters and the GPS units, and students confirm that their GPS units are using the correct coordinate system and datum (UTM, NAD83).

We discuss surveying techniques as a class, and supplemental instructions are also provided in the handout (see Supplementary Materials below). We establish a centrally-located, bench mark (usually one of the staff gages) from which the students survey the wells and other staff gages. Each group is responsible for surveying at least two wells or staff gages. Groups distribute their surveying results to the rest of the class when we return to campus. Each group checks their results in the field, which reduces the chance of propagating surveying errors throughout the class.

Groups need to take water level measurements, survey wells, and record GPS coordinates for each well and staff gage. Additionally, because Newark Road Prairie has an established grid system with posts and markers at ten meter intervals, students measure the distance of each well/staff gage from at least three markers in order to evaluate the accuracy of their GPS measurements. Groups rotate the surveying equipment and are responsible for collecting all of the necessary data within the two lab periods. Two three-hour lab periods provide ample time for each group to collect the necessary data sets, including the time required to load/unload equipment and drive to/from the site. One 50-minute class period is provided for distributing survey results, compiling and printing base maps using ArcGIS, and contouring the water table maps.

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