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Preface to the Special Issue

The Waterloo Moraine: Water, science and policy

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Pages 85-87 | Received 22 Feb 2014, Accepted 17 Mar 2014, Published online: 10 Jul 2014

Growth is widely seen as the means to create employment and achieve economic prosperity. Growth also consumes natural resources. As a consequence, growth can create the potential for societal conflict where resources are limited. For example, urban development or aggregate extraction can conflict with ecosystem preservation and recharge zone protection.

In the Canadian context, Waterloo Region (the Region) is a classical case study for this potential conflict. Economically, the Region is changing rapidly. While much of the Region’s traditional manufacturing industry has been devastated by globalization, a new high-tech industry has emerged, resulting in considerable urban growth. The provincial government has supported this trend by designating Waterloo Region as one of a number of growth centres in the province, and as a result, the population is expected to increase by 50% over the next 30 years.

Growth increases the pressure on the community’s natural resources. In addition to land, the most critical natural resource for the Region is water. Although the Region is situated between two of North America’s Great Lakes, access to potable water from these lakes is complicated and expensive. Fortunately, the Region already has an excellent source of water beneath the urban landscape – the groundwater of the Waterloo Moraine. In addition to providing the Region’s drinking water, the Moraine also assures the ecological health of streams and wetlands, and it supports a healthy agricultural sector in the rural areas. The Moraine water resource is adequate for present use; however, it is also limited.

Growth not only increases the demand on water but can potentially diminish the resource itself. Sprawling subdivision developments over the aquifer recharge areas can affect the quantity of water available, urban contaminants such as road salt can impact the groundwater quality and aggregate pits can weaken the protection of the aquifers from contaminants. Consequently, conflict can potentially arise when the growing demand tests the limits of the resource.

Water managers at the Region of Waterloo have so far been successful in striking a balance between growth, water use and the protection of the water source, using a multi-faceted approach including demand management, delineating groundwater sensitivity zones and constraining the urbanized area by means of a “countryside line”. The sensitivity zone concept is science-based, while the countryside line has a political origin. The latter concept is being challenged by development interests, which seek to expand residential subdivisions across the countryside line into rural areas that also contain the main recharge areas of the Waterloo Moraine. Allowing urban sprawl into the main Moraine recharge areas has the associated risk of upsetting the recharge-withdrawal balance.

The considerable effort to preserve and protect the Region’s water source has produced a large amount of knowledge over the past 40 years, involving different branches of groundwater science. The idea for this Special Issue arose when researchers at the Geological Survey of Canada and the University of Waterloo decided to compile an authoritative source for this body of knowledge, to be readily available to others confronted with similar land-water conflicts. The result is a set of 11 research papers by authors from government, universities and private consultants, all with different backgrounds and expertise, but all with a passion for groundwater. These papers cover both science and societal aspects of groundwater, they are all interrelated, but each stands on its own merit.

Frind and Middleton (Citation2014, this issue) examine the Region’s overall strategy for managing the complex Moraine groundwater resource and providing a reliable water source for the growing community. This successful strategy integrates the principles of sustainable water governance with a science-based understanding of the complex Moraine system. Bajc et al. (Citation2014, this issue) lay the foundation for the science of the Waterloo Moraine by unravelling its depositional history during the Quaternary age. Understanding this history and applying a full range of exploratory tools including geophysical methods leads to insights into the complex three-dimensional architecture of the Moraine, which is then used as a basis for constructing a new three-dimensional geodata-based stratigraphic model of the Moraine. Blackport et al. (Citation2014, this issue) integrate the geodata-based model with the large base of hydrogeological data, including water level observations and borehole logs that have been collected over the years of hydrogeological investigations of the Moraine. The result is a refined hydrostratigraphic/hydrogeological conceptualization of the Moraine that shows the extent of the aquifers and aquitards, outlines the key recharge areas and defines the linkages between the municipal aquifers and sensitive environmental features. Stotler et al. (Citation2014, this issue) demonstrate the use of environmental tracers for estimating the age of the water in the Waterloo Moraine multi-aquifer system, thus giving insight from the geochemical point of view into aquifer connectivity and continuity. The geochemical characteristics of the groundwater in the Moraine aquifers clearly show an anthropogenic impact on the water resource from contaminants such as road salt in urban areas and fertilizers in rural areas. Frind et al. (Citation2014, this issue) review the historical role of modelling in the study of the Waterloo Moraine, and the evolution of numerical modelling tools, which have yielded valuable insight into the dynamics of the Waterloo Moraine. The focus changed over time from well interference to capture zone analysis, groundwater age and the prediction of impact due to various land uses. Attention is drawn to conceptual uncertainties that may affect model-based predictive assessments. Meyer et al. (Citation2014, this issue) build on the historic model development and on the new geodata-based hydrogeological conceptualization to develop and calibrate a three-dimensional state-of-the-science groundwater model of the Waterloo Moraine, which is intended for use in the Region’s groundwater program. The model was applied in a water budget and risk assessment study for a subwatershed within the Grand River watershed. Veale et al. (Citation2014, this issue) examine the role of the Waterloo Moraine from the perspective of the Grand River watershed as a whole, showing the importance of the Moraine to the watershed. The interdependence between groundwater and surface water, and the role of the Moraine’s groundwater in sustaining environmentally sensitive areas and aquatic and terrestrial ecosystems, is examined. Preserving the Moraine’s natural functions in the face of rapid growth is found to require adaptive management and coordinated multi-scale planning.

Sousa et al. (Citation2014, this issue) examine the threats to groundwater resources in terms of both quantity and quality. These threats differ for urban and rural areas; they depend on scale, and they can take on chronic as well as acute forms. The current framework for threat assessment is reviewed, and improvements are proposed as part of a comprehensive future framework of science-based groundwater governance for Canada. Blackport and Dorfman (Citation2014, this issue) outline how scientific insight is translated into a policy framework for regulating the management and protection of the water resource, and how groundwater protection has been enshrined as official policy by Waterloo Region by inclusion within environmental protection standards. Suggestions are made for developing a defensible policy framework for protecting groundwater sources throughout Ontario. Reconciling the uncertainty inherent in the science with the certainty expected within a policy framework remains a challenge. Simpson and de Loë (Citation2014, this issue) demonstrate a cooperative approach to groundwater management as an alternative to the regulatory approach based on wellhead protection planning. The collaborative approach involves diverse stakeholders in a decision-making process that integrates expert science, local knowledge, and community beliefs and values. This approach has been successfully applied in the rural areas of Waterloo Region. Finally, Holysh and Gerber (Citation2014, this issue) address the fundamental issue of knowledge management (which is different from database management), using the comprehensive Oak Ridges Moraine Hydrogeology Program as an example. The objective is to make the management of water resources more effective and efficient by providing a transparent knowledge base accessible to all users.

It is hoped that the insights offered in the papers of this Special Issue, focused on the unique challenges of managing the Waterloo Moraine water source, will be of benefit to scientists and water managers confronted with similar challenges.

Acknowledgements

This Special Issue has brought together an expert team of authors and reviewers with different backgrounds from research institutions, academe and private industry, who contributed many diverse and uniquely valuable viewpoints on the central theme of groundwater. All these contributors are sincerely thanked for their hard work. This project was supported by the Groundwater Geoscience Program, Geological Survey of Canada, Natural Resources Canada, and the Water Institute, University of Waterloo. The abstracts were translated by the Translation Bureau, Public Works and Government Services Canada. The expert technical review of the French abstracts by Nicolas Benoit is much appreciated.

References

  • Bajc¸ A. F., H. A. J. Russell, and D. R. Sharpe. 2014. A three-dimensional hydrostratigraphic model of the Waterloo Moraine area, southern Ontario, Canada. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914794.
  • Blackport, R. J., and M. L. Dorfman. 2014. Developing science-based policy for protecting the Waterloo Moraine groundwater resource. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914803.
  • Blackport, R. J., P. A. Meyer, and P. J. Martin. 2014. Toward an understanding of the Waterloo Moraine hydrogeology. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914795.
  • Frind. E. O., and T. A. Middleton. 2014. The Waterloo Moraine: A sustainable water source for Waterloo Region. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914791.
  • Frind, E. O., J. W. Molson, M. R. Sousa, and P. J. Martin. 2014. Insights from four decades of model development on the Waterloo Moraine: A review. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914799.
  • Holysh, S., and R. Gerber. 2014. Groundwater knowledge management for southern Ontario: An example from the Oak Ridges Moraine. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914788.
  • Meyer, P. A., M. Brouwers, and P. J. Martin. 2014. A three-dimensional groundwater flow model of the Waterloo Moraine for water resource management. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914800.
  • Simpson, H. C., and R. C. de Loë. 2014. A collaborative approach to groundwater protection: The Rural Water Quality Program for Waterloo Region. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914789.
  • Sousa, M. R., D. L. Rudolph, and E. O. Frind. 2014. Threats to groundwater resources in urbanizing watersheds: The Waterloo Moraine and beyond. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914801.
  • Stotler, R. L., S. K. Frape, and L. Labelle. 2014. Insights gained from geochemical studies in the Waterloo Moraine: Indications and implications for anthropogenic loading. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914796.
  • Veale, B., S. Cooke, G. Zwiers, and M. Neumann. 2014. The Waterloo Moraine: A watershed perspective. Canadian Water Resources Journal 39(2): doi: 10.1080/07011784.2014.914790.

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