Nitrogen transport and retention in an arid land watershed: influence of storm characteristics on terrestrial-aquatic linkages

• Published in: Biogeochemistry 2005-12, Vol.76 (3), p.421-440
• Main Authors: Welter, J.R, Fisher, S.G, Grimm, N.B
• Format: Article
• Language: English
• Subjects: Ammonium; ammonium nitrogen; Animal and plant ecology; Animal, plant and microbial ecology; arid soils; Arid zones; biogeochemical cycles; biological activity in soil; Biological and medical sciences; Desert soils; Drought; Earth sciences; Earth, ocean, space; Exact sciences and technology; Fundamental and applied biological sciences. Psychology; Hydrology; Hydrology. Hydrogeology; losses from soil; Marine and continental quaternary; nitrate nitrogen; Nitrification; Nitrogen; overland flow; Rain; Retention; Runoff; Soil ecology; Soil microorganisms; Storm seasons; Storms; Stormwater; Summer; Surficial geology; Synecology; Terrestrial ecosystems; Watersheds; Winter
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1007/s10533-005-6997-7

Arid ecosystems experience prolonged dry periods, as well as storms that vary in size, intensity and frequency. As a result, nitrogen (N) retention and export patterns may be a function of individual storm characteristics. Our objective was to determine how seasonal patterns in rainfall as well as individual storm characteristics influence N transport and retention on terrestrial hill slopes in a Sonoran Desert watershed. Regression models indicated that variation in runoff ammonium (NH₄⁺) was best explained by antecedent conditions (cumulative seasonal rainfall, days since last storm) while variation in runoff nitrate (NO₃⁻) was best explained by single storm characteristics, primarily rain NO₃⁻. Increases in runoff NO₃⁻ along overland surface flowpaths were balanced by decreases in NH₄⁺ during summer, with no change in dissolved inorganic nitrogen (DIN) concentration; a pattern consistent with nitrification. Nitrate increases along flowpaths were not as strong during winter storms. Results indicate that NH₄⁺ is transported from hillslopes to other parts of the catchment, including streams, and that nitrification occurs along surface flowpaths, particularly during summer storms. These findings suggest that the extent to which a receiving patch is supplied with NH₄⁺ or NO₃⁻ depends on the distance runoff has traveled (flowpath length) and the length of the antecedent dry period. The extent and configuration of fluvial reconnection amongst patches in the landscape following long drought periods likely determines the fate of available N, whether N is processed and retained in the terrestrial or in the aquatic component of the watershed, and the mechanisms involved. The nature of this fluvial reconnection is driven by the size, intensity and sequence of storms in space and time.