Document Type

Article

Department/Program

Virginia Institute of Marine Science

Publication Date

1-2002

Journal

Aquatic Microbial Ecology

Volume

26

Issue

3

First Page

295

Last Page

304

Abstract

Recent studies have shown that in a number of humic-rich surface waters in North America, NH4+ is released when dissolved organic matter (DOM) is exposed to sunlight. However, photochemical NH4+ production has not been observed in all surface waters, and factors that contribute to it are not well understood. We hypothesized that the presence or absence of NH4+ photoproduction may be affected by the light exposure history of DOM, The present study was undertaken to determine whether DOM from surficial groundwaters, with minimal light exposure history, would produce labile nitrogen (N) photoproducts more consistently, In this study, estuarine surface waters and surficial groundwaters, collected just adjacent to estuaries in Georgia and South Carolina, USA, were exposed to sunlight to quantify the photochemical production of NH4+, dissolved primary amines (DPA), and NO2-. The photoproduction of NH4+ was observed in 4 of 5 irradiated estuarine surface water samples but in only 2 of 13 groundwater samples. In contrast, NH4+ concentrations decreased in 5 of 13 groundwater samples when exposed to sunlight. The results indicate that a small amount of NH4+ may be lost from waters in which groundwater-derived DOM is first exposed to sunlight. No consistent trends were observed in the photoproduction or loss of DPA and NO2-.

DOI

10.3354/ame026295

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