Les Henry: Sloughs and ‘bathtub’ salt rings

Some sloughs have rings, some do not — why?

Published: October 25, 2023

These sloughs with salt rings are near Conquest, Sask. Shallow (25 to 100 feet) glacial aquifers are the source of the pressure that prevents downward flow of water to drain the slough. The constant upward pressure maintains a high water table even in dry periods when evaporation is busy concentrating the salts.

Sloughs (polite name is potholes) are widespread on the Canadian Prairies and particularly in Saskatchewan, which has a great depth of glacial deposits. The sloughs catch much of the snowmelt and runoff from summer rains. If the water in the slough is the sole cause of salt rings, then all sloughs should have them.

Artesian pressure from beneath is the main cause of salt rings. Deep drainage by a deep aquifer that drains to a creek or river is why some very large sloughs have no salinity.

I checked out municipal assessment and they assess the land as normal and then take a 50 per cent deduction for poor drainage — assume crops will be five years out of 10.

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But what is the deep drain that allows all of this to happen? The deep drain is the pre-glacial (bedrock) Judith River aquifer. In that area, the wells completed in the Judith River Formation are 500-plus feet deep, and the static water level is 100-plus feet below ground surface. The Eagle Creek is about 12 miles north of Sovereign and the Judith River aquifer discharges to Eagle Creek.

In the decade or more of high profits on farms (approximately 2005 to 2019), there have been many Judith River wells completed in that area. With current drilling and well completion methods, yields of 20 gallons per minute or more are common. The water is mineralized but it is soft water (sodium dominated), which is great for domestic use.

This very large slough (about 1,500 acres) just west of Sovereign, Sask., has no evidence of a saline ring even though it can stay wet and can’t be farmed for several years. There are many such sloughs in this Heavy Clay belt near where I was raised. The approximately 20 to 30 feet of Heavy Clay soil will mean that downward drainage is slow. However, that slow drainage carries on 24 hours a day, every day of the year(s), until the slough drains and dries up. photo: Courtesy Les Henry

Testing Eagle Creek

Eagle Creek drains to the North Saskatchewan River about 15 miles west of the Ag in Motion site, west of Langham, Sask. Several years ago, I used my trusty water electrical conductivity meter and Hach Hardness Kit to test Eagle Creek water that was flowing despite a long, dry spell.

Creek water that has water from glacial deposits is hard. We checked several locations from Asquith to the point Eagle Creek discharges to the North Saskatchewan River. The water was too soft for glacial deposits and that indicated discharge from the Judith River Formation was occurring.

So, there you have it. To understand our soils, we must also understand the geology beneath our soils. Water is the elixir that ties the two together, so we must understand the groundwater also.

This is the slough all dried up and being farmed — now some of the best land — until the next wet spell. I quizzed a farmer who farms part of that slough to see how it all worked. Year one, he said, to plant the seed and stand back and watch until combine time and have a good trucker lined up. In year two, treat it like the rest of the land in the area. By year four, it is time for another three feet of water to fill up the slough and repeat the cycle. photo: Courtesy Les Henry

About the author

Les Henry

Les Henry

Columnist

J.L.(Les) Henry was a professor and extension specialist at the University of Saskatchewan and a longtime Grainews columnist who farmed at Dundurn, Sask. Les passed away in 2024.

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