Spatial variability of water chemistry in the Ayeyarwady River Basin, Myanmar
An V. Vu
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Abstract
Understanding chemical properties and biogeochemical changes can help us answer difficult ecological questions. Water chemistry is often dynamic in large tropical rivers, particularly in deltas where sea tides and river hydrological regimes are extremely influential.
This study assessed the spatial variability of water chemistry by measuring the elemental concentrations of seven trace elements and strontium isotopes (87Sr:86Sr) in the Ayeyarwady River Basin in Myanmar.
Inductively Coupled Plasma Optical Emission Spectroscopy and multi-collector inductively coupled plasma mass spectrometry were used to quantify concentrations of trace elements and strontium isotopes at 50 sampling sites, covering 1700 km of the Ayeyarwady River. Data was grouped into regions for statistical analyses.
Three elements (Sr, Ca, and Mg) showed distinct longitudinal concentration profiles, which were higher at the coast but consistently lower in freshwater. For example, elemental concentrations at coastal areas were 22-, 63-, and 150-times higher than in freshwater further upstream for Ca, Sr, and Mg, respectively. Although, longitudinal concentration profiles of 87Sr:86Sr ratios varied along the Ayeyarwady River, they were not significantly different among regions.
Longitudinal profiles of dissolved elements varied significantly. In particular, three elements (Sr, Ca, and Mg) are good indicators to differentiate between marine and freshwater in the Ayeyarwady River.
Our findings provide important baseline information on water chemistry for future fish otolith (inner ear of bony fish) chemistry studies to track fish migrations in the basin.
Keywords: Ayeyarwady River, chemistry, Chindwin River, fish migration, microchemistry, strontium isotopes, trace element, variation.
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