Algal bloom at the loch - a thing of the past.
Kinghorn Loch was polluted with a highly alkaline liquor that was leaching from Whinnyhall Landfill Site. This occurred from 1950s to 1983, by which time the loch was dead, except for midge larvae and blue-green algal blooms.
After 1983 the loch was effectively cleaned up and now has a healthy ecosystem and excellent water quality.
1981: foam around the loch and a young Marilyn
-Thick layer of iron rich sediments. Hydrated iron oxide solids from the Red Mud leachate.
-Soaking up (adsorbing) arsenic and phosphate into the sediments
-Local waters are nitrate rich, being Coalfield-derived groundwater, naturally rich in nitrate.
-Phosphorus is the limiting nutrient, because nitrate is high.
1985: Photographing a core taken at the head of the loch. Formed primarily of Red Mud material over natural peat.
In 1983, once the pH of the water dropped the "sludgy" sediment collapsed to a thicker consistency, the water became clear and rare plants, such as Water Hyacinth, arrived.
However, by 1990, algal blooms once again became rife, lasting all year on occasions, and stifling other plants.
Nutrients (nitrate and phosphate) in the water encouraged the blooms.
The picture shows Mediterranean green, algae-rich water and the barley straw rafts built to treat the problem.
Straw has been donated by Banchory Farm every year for 22 years.
As algal blooms have been controlled and eliminated, rooted plants have more sunlight and have thrived. Rooted plants are now dominant, aerating the water and giving refuge to nesting mallard, coots, and others, feeding the fish and protecting frog and toad tadpoles from the pike.
Otters are often seen at the loch, and the remains of carp are often found on the banks.
The raft in the middle of the picture shows the scale of the loch.
1990
Whinnyhall Landfill Site - remediated - green and pleasant view.
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Correspondence address: Craigencalt Cottage, Kinghorn,
KY3 9YG, Scotland, UK
Marilyn. Tel: 07740 999 514