by Grant Ferguson And Jennifer C. Mcintosh, The Conversation
Water is becoming a scarce resource in many parts of the world. Water tables have been falling in many regions for decades, particularly in areas with intensive agriculture. Wells are going dry and there are few long-term solutions available —a common stopgap has been to drill deeper wells.
This is exactly what happened in California’s Central Valley. The recent drought there prompted drilling of deeper and deeper water wells to support irrigated agriculture.
Arizona is also looking to drill additional wells to tackle water shortages to support agriculture. The flow of the Colorado River, which supplies water to more than 44 million people across seven states, including Arizona, has dropped by close to 20 per cent in the past 15 years, lowering water levels in Lake Mead, the river’s largest reservoir.
Under Arizona’s proposed Drought Contingency Plan, the state will have to reduce its use of Colorado River water by about 500 million cubic metres per year, an amount equal to three times Calgary’s annual water consumption.
Groundwater supplies around the world are being threatened by excessive pumping, but drilling deeper wells is not a long-term solution. There is a limit to the availability of fresh groundwater at depth. A better solution is to manage water use and avoid excessive declines in groundwater levels.
The water surface elevation of Lake Mead has dropped about 15 metres from its highest level, revealing a white ring of mineral deposits on its walls. Credit: Wayne Hsieh/flickr, CC BY-NC
Shifting corn belt, shifting water needs
Drilling deeper wells to support irrigated agriculture may not be possible everywhere. Recent research indicates the depths at which fresh groundwater resources occur is highly variable and not as extensive as previously thought.
Deep fresh groundwater can be found in parts of California and Arizona, but this is not the case beneath the High Plains in the western United States, the U.S. Midwest or the Canadian Prairies. Intensive irrigation in Kansas, Nebraska, Oklahoma and Texas has depleted the High Plains aquifer. Wells in this area now reach to the bottom of fresh groundwater resources.
Irrigation for agriculture is currently uncommon in the Canadian Prairies, but this could change over the coming decades. Water scarcity in the southern U.S. High Plains combined with climate change could lead to changes in agricultural practices in Canada. As the corn belt shifts north, the demand for water will increase.
Water in the Saskatchewan River watershed is already close to fully allocated in some areas. Steamflow in the headwaters of the Saskatchewan River has decreased during the growing season, as glaciers and snowpacks in the Rocky Mountains melt and shrink. Groundwater demand is likely to increase to address shortfalls in water from surface water sources.
The Saskatchewan River watershed extends over much of the agricultural land in the Canadian Prairies. Author provided
Widespread groundwater depletion has not been noted in Canada, in part because of low demand from groundwater to date. It is not clear what level of groundwater pumping would be sustainable.
Examining this issue ahead of widespread development of groundwater resources due to growing population and changes in agriculture is key to avoiding the widespread depletion problems seen in other regions.
Groundwater depletion by contamination
Canada has, however, seen issues with groundwater quality.
In the Canadian Prairies, these issues are often related to oil and gas development and agricultural practices. Saskatchewan has documented nearly 20,000 surface spills of hydrocarbons and waters from oil fields since 2005. Migration of these contaminants and others, notably nitrates from agriculture, to the water table decreases groundwater quality.
Groundwater resources are threatened from the bottom up by the oil and gas industry.
Another issue is the contamination of groundwater from the bottom up. There are more than 700,000 oil and gas wells, and more than 20,000 injection wells, mainly used for the disposal of saline waters produced during oil and gas extraction in Western Canada. More than 23 billion cubic metres of fluids, mainly saline waters produced during oil and gas extraction, have been injected into the subsurface —equivalent to one-fifth of all global oil production since 1850.
These activities could be creating conditions that would allow for migration of hydrocarbons, saline waters and other contaminants upwards into groundwater supplies that might otherwise be suitable for agriculture and drinking water supplies.
The impacts from the oil and gas industry on water chemistry have not been studied in detail at the regional scale. Most of THE studies that have been done relied on data submitted when wells were initially drilled, meaning that we’re unable to track changes in water chemistry over time.
Studies that do examine changes in water chemistry over time and the potential migration of contaminants into potable water supplies are rare, mainly due to a lack of reporting requirements for water chemistry and injected fluids, along with sparse monitoring networks.
Groundwater may play a large role in meeting the water needs of Western Canada over the coming century. Understanding how extensive this resource is and developing better management strategies is urgently needed.