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Atmospheric wet sulphate deposition and lakewater chemistry

Abstract

Atmospheric sulphur deposition and its impacts on surface-water chemistry and biota have been extensively studied in several areas of the United States and elsewhere during the past two decades1,2. In the absence of regionally based statistical (probability) sampling, however, it has not been possible to extrapolate the results from intensive small-scale studies to a regional population. Here we present data from the first regional probability sampling of lakes in the United States3,4, indicating that median lake sulphate concentrations correlate highly with estimated wet sulphate deposition at lake sites. The data further suggest that acid deposition has depleted acid-neutralizing capacity (ANC) in low-base-cation lakes, and that some high-base-cation lakes receive substantial sulphate from internal watershed sources. Data suggest that acidic lakes greater than 4 hectares in surface area are generally not found in areas receiving low sulphate deposition, whereas most acidic lakes in the northeastern United States are currently acidic because of high sulphate relative to base cation concentrations.

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Sullivan, T., Eilers, J., Church, M. et al. Atmospheric wet sulphate deposition and lakewater chemistry. Nature 331, 607–609 (1988). https://doi.org/10.1038/331607a0

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