Recovery of Soils From Acidic Deposition May Exacerbate Nitrogen Export From Forested Watersheds. Issue 1 (15th January 2020)

• Record Type: Journal Article
• Authors: Lawrence, Gregory B.; Scanga, Sara E.; Sabo, Robert D.
• Is Part Of: Journal of geophysical research. Volume 125:Issue 1(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-01-15
• Subjects: Forest nitrogen cycling -- acidic deposition recovery -- soil carbon -- forest floor decomposition -- stream nitrate -- soil calcium depletion; Geobiology -- Periodicals; Biogeochemistry -- Periodicals; Biotic communities -- Periodicals; Geophysics -- Periodicals; 577.14
• DOI: 10.1029/2019JG005036
• Languages: English
• ISSNs: 2169-8953

Abstract

Abstract: Effects of ambient decreases in N deposition on forest N cycling remain unclear as soils recover from acidic deposition. To investigate, repeated soil sampling data were related to deposition, vegetation, and stream data, for 2000–2015 in North and South Buck Creek watersheds, in the Adirondack region of New York, USA. In 63 other Adirondack streams, NO3 − concentrations were also compared between 2004–2005 and 2014–2015, and a link between soil calcium and stream NO3 − was investigated using data from 387 Adirondack streams that were sampled in either 2003–2005 or 2010–2011. No trends in N export or NO3 − concentrations were observed in either Buck watershed despite a 45% decrease in N deposition, although South Buck N export was 2 to 3 times higher than in North Buck, where 48% of deposited N was accounted for by accumulation in the upper soil. In marked contrast, the upper profile in South Buck showed a net loss of N. Increased decomposition appeared likely in South Buck as those soils are adjusted to lower levels of acidifying S deposition, whereas decomposition increases in North Buck were likely suppressed by high levels of natural organic acidity. Stream NO3 − concentrations in Buck watersheds bracketed regional results and were consistent with the regional streams that showed no overall change in NO3 − concentrations between 2004 and 2014. A negative correlation observed between NO3 − concentration and watershed buffering capacity expressed as the ratio of Ca 2+ to SO4 2− also suggested that stream NO3 − concentrations were elevated where soil Ca depletion had occurred. Key Points: Decreasing atmospheric deposition of nitrogen has not lowered watershed export of nitrogen by Adirondack streams Long‐term decreases in acidifying sulfur deposition are stimulating decomposition and nitrogen mineralization in the forest floor Movement of harmful nitric acid and aluminum from soils to streams continues despite lower deposition of sulfur and nitrogen