I'm looking for information on how feasible it is for a large, freshwater lake to become salty, at least to a level where the people, animals and plants that live around and rely on it can no longer drink or make use of it in their every day lives. My idea is that the lake in question (the Lake of Kurn) is a natural saltwater lake, and there exists a supernatural artifact within it that, when activated, purges the waters of salt and other contaminants. The process of doing so would have been occurring for many centuries.
The Lake of Kurn is located in a tropical savannah climate in the southern hemisphere (hot, semi-arid at its southern tip) and is roughly 58,000km² with an average depth of ~30m and a maximum depth ~78m; just smaller and shallower than the real-life Lake Victoria. The region it resides in, like most equatorial regions, has wet and dry seasons.
As I understand it, salt builds up naturally in any lake that does not have an outlet, and the process to change from fresh water to brackish/saline water can take years to decades to happen. What I am not sure of is how my particular lake could come about that change, or what conditions need to be met so that the lake requires maintenance. I'm not looking for the lake to become like the Great Salt Lake or Caspian Sea, I just want it to become salty or contaminated enough to no longer be healthy to drink, use for crops, etc. And I am looking for it to get to that point regularly, so that the ritual to purify the lake needs to occur every few years to prevent ecological and societal catastrophe.
In my search for information, the closest things I could find on the matter were Lake Bonneville, Lake Peigneur and the Salton Sea. None of which feel a fit for what I need, for one reason or another.
- Lake Bonneville became salinized by the slow degradation of its outlets through the changing climate. In the case of the Lake of Kurn, it would be a freshwater lake with no outlets from the start, thereby being much more rapid in its salt accumulation. But I'm unsure how rapid.
- Lake Peigneur became the way it is because of seawater flowing into it. The Lake of Kurn is over 100 miles from the ocean, so I cannot see a similar event occurring here.
- Salton Sea almost matches what I am looking for, down to how rapid its contamination was. My major concerns for using the Salton Sea as a model are 1) the time period the story takes place in and 2) its geographical location. The story I am planning has a medieval-like setting. As such, the modern agricultural techniques that resulted in the Salton Sea's decline would not be present, or at least not to the scale needed for it. The Salton Sink was also located in a much more arid locale than the Lake of Kurn is, so the pre-existing conditions that created the saline lake would not be present to re-salinize a body of freshwater like the one I described, I wouldn't think.
My asks are:
- What conditions would need to be present for the lake to shift from fresh water to more brackish waters, to the point it becomes noticeable?
- How long would/could it take for this shift occur?
- Would there be any additional ramifications from continually turning the lake fresh?
Any information on the viability of this would be appreciated. Whether it be deposits from tributary rivers, erosion from the soil, natural salt deposits in the lake bed, and so on.
Thanks!