Evaluating regional patterns in nitrate sources to watersheds in national parks of the Rocky Mountains using nitrate isotopes

Abstract

In the Rocky Mountains, there is uncertainty about the source areas and emission types that contribute to nitrate (NO 3 ) deposition, which can adversely affect sensitive aquatic habitats of high-elevation watersheds. Regional patterns in NO 3 deposition sources were evaluated using NO 3 isotopes in five National Parks, including 37 lakes and 7 precipitation sites. Results indicate that lake NO 3 ranged from detection limit to 38 μeq/L, δ 18 O (NO 3 ) ranged from −5.7 to +21.3‰, and δ 15 N (NO 3 ) ranged from −6.6 to +4.6‰. δ 18 O (NO 3 ) in precipitation ranged from +71 to +78‰. δ 15 N (NO 3 ) in precipitation and lakes overlap; however, δ 15 N (NO 3 ) in precipitation is more depleted than δ 15 N (NO 3 ) in lakes, ranging from −5.5 to −2.0‰. δ 15 N (NO 3 ) values are significantly related ( p < 0.05) to wet deposition of inorganic N, sulfate, and acidity, suggesting that spatial variability of δ 15 N (NO 3 ) over the Rocky Mountains may be related to source areas of these solutes. Regional patterns show that NO 3 and δ 15 N (NO 3 ) are more enriched in lakes and precipitation from the southern Rockies and at higher elevations compared to the northern Rockies. The correspondence of high NO 3 and enriched δ 15 N (NO 3 ) in precipitation with high NO 3 and enriched δ 15 N (NO 3 ) in lakes, suggests that deposition of inorganic N in wetfall may affect the amount of NO 3 in lakes through a combination of direct and indirect processes such as enhanced nitrification.