Article - Where does my tap water come from?

by Steve Shikaze

In the year 2000, the town of Walkerton in southwestern Ontario had E.coli bacteria in one of their drinking supply wells that resulted in the death of six people and over 2,000 residents becoming sick. The water supply became contaminated at a pumping well that was close to a farm where cattle manure (which contains E.coli) was used to fertilize crops. Heavy rains in May 2000 carried the bacteria into the ground and towards the nearby supply well. Inadequate chlorination led to the distribution of contaminated water to residents and within days, residents began getting sick, with outbreaks of gastroenteritis occurring in the community. The public inquiry that followed concluded that negligence (including falsification of reports, failure to report) as well as inadequate chlorination and the shallow depth of the water supply well (combined with its proximity to cattle manure) led to this tragedy.

As a result of the Walkerton tragedy. the provincial government in Ontario developed a framework to protect drinking water. This framework includes laws and regulations, drinking water standards, regular testing, licensing and training of operators, transparency and a focus on source-to-tap. Locally, source water protection plans include understanding the sources of drinking water and implementing plans for the protection of these and future sources of drinking water.

That’s a lot of preamble for this article but I want to stress the importance of understanding where our water comes from. I live in Kitchener-Waterloo (KW) where about 75% of the water supply comes from groundwater (the remaining 25% comes from the nearby Grand River). The Region of Waterloo, the local government in charge of water distribution, has over 100 water supply wells spread throughout the KW area.

Through some online digging, I learned that near me, the tap water is coming from the William Street pumping wells in uptown Waterloo. The William Street well field has been in operation since 1899 and is the first site of public groundwater use in the area.

When we talk about protection of our water resources, we need to consider two things: (1) water quality, and (2) water quantity. For groundwater resources, protecting water quality means identifying potential sources of contamination (gas stations, agricultural fertilizers, road salt, for example) that might get to the water supply. To aid in understanding this, computer models can be used to estimate from where water wells are getting water. Recent reports from consultants and the Region of Waterloo show that the William Street wells pump groundwater from an area that extends from the pumping wells towards the west. The figure below (reference here, page 94) shows a map that requires more explanation.

Towards the right (east) of the map, there are small green dots labelled W1C, W1B and W2. These are three pumping wells at the William Street well field. The coloured polygons around this well field represent well head protection areas (WHPAs) of different water travel times to the wells. The largest yellow area indicates the 25-year WHPA. In other words, all groundwater within this yellow zone is predicted to reach the William Street pumping wells within 25 years. The darker colours represent shorter groundwater travel times to the pumping wells (5, and 2 years). Urban planners make use of maps like this to help in decision making (e.g., what can be built where). The 2, 5, and 25 year zones are estimated to aid in protecting the water quality at the water wells.