InTeGrate Modules and Courses >Water Science and Society > Student Materials > Section 3: Social Science of Water > Module 7: What is in your water? > Contaminant Example: Arsenic in Groundwater
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These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
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Contaminant Example: Arsenic in Groundwater

There are, of course, many possible contaminants in drinking water supplies—in part natural, but also induced by human activities. There are three main groups of contaminants with relation to anticipated health effects:

  1. Some contaminants produce no health effects until a threshold concentration is exceeded. Nitrate (NO3) is an example of this; OK at 50 mg/liter (50 ppm), but at higher levels it produces methaemoglobinaemia (e.g., "blue baby" syndrome).
  2. A second group of contaminants has no apparent threshold for health effects. These include genotoxic substances. These include some natural and synthetic organic compounds, microorganic compounds, some pesticides, and arsenic (see below) for example.
  3. A third group consists of elements essential to the human diet: fluoride, iodine, and selenium are good examples—their absence in diet causes problems, but an excess of intake can create problems.

Arsenic is a good example of both natural and human-induced contamination, and it is important as well because of its toxicity at higher concentrations (as are lead and fluoride). In recognition of the potential toxicity of arsenic (As), the US EPA lowered the MCL in drinking water from 50 ppb to 10 ppb in 2001. For example, check out this short video on possible health effects of arsenic and the need to have private wells tested.

In New England, groundwater As levels are particularly high (see Fig. 6) as a natural source. In this case, more alkaline (high pH), low dissolved oxygen groundwaters favor high solubility of arsenic in shallow aquifers of glacial origin. Other aquifers with high As concentrations originate because of the type of bed rock. Contamination of aquifers can also occur from agricultural runoff, runoff from arsenic-bearing wood preservatives, improper disposal of chemicals containing As, and/or mining activities. See this article in The New York Times, The Arsenic in Our Drinking Water, for a summary of possible health effects in the U.S. and Bangladesh.

Global maps of the probability of arsenic concentrations in groundwater greater than 10 ppb can be viewed at Global fluoride and arsenic contamination of water mapped, and is based on research by M Amini et al (Environ. Sci. Technol., 2008, DOI:10.1021/es702859e. A more generalized map of risk for As in drinking water can be seen in Figure 3.


These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
Explore the Collection »