Wilpattu National Park Villu hydrochemistry: dissolved calcium carbonate buffering and salinity?

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Arjun Karst930 rep

Why do water chemistry parameters differ between fresh villus like Kumbuk Wila and saline basins like Kokkare Villu within the same sand plain?

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5 Answers from travellers

Accepted Answer

The diverse water chemistry across Wilpattu’s villu basins is governed by subterranean karst hydrogeology and marine evaporation. Freshwater villus (such as Kumbuk Wila and Mahapatana) rest on thick, unconfined sand aquifers that store seasonal monsoon rainfall, maintaining low total dissolved solids (TDS < 300 mg/L) and neutral pH (6.8-7.4) buffered by dissolved calcium bicarbonate from underlying Miocene limestone. Conversely, hypersaline basins (like Kokkare Villu) have shallow impervious clay sub-layers that cut off freshwater aquifer recharge; centuries of high evaporation have concentrated sodium, chloride, and sulfate ions, creating saline lakes.

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D
Dr Bandara DWC1890 rep

The high salinity in Kokkare Villu supports distinct benthic halophytic algae that turn the lake margins white with salt crusts during dry August droughts.

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A
Arjun Karst930 rep

Migratory shorebirds, including Black-winged Stilts and Little Stints, congregate at saline villus to feed on abundant brine flies and larval crustaceans.

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Prof Gamhewage Bio1950 rep

Mammals (leopards, elephants, and deer) drink exclusively at freshwater villus, avoiding saline basins during the dry season.

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Ranger Upul Yala1750 rep

Kumbuk Wila features an elevated wooden picnic pavilion where safari visitors can disembark to observe waterbirds under giant Kumbuk trees.

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Sarah Field Scout1720 rep

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