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Tracing sources and pathways of dissolved nitrate in forest and river ecosystems using high‐resolution isotopic techniques: a review
Author(s) -
Ohte Nobuhito
Publication year - 2013
Publication title -
ecological research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.628
H-Index - 68
eISSN - 1440-1703
pISSN - 0912-3814
DOI - 10.1007/s11284-012-0939-3
Subject(s) - biogeochemical cycle , environmental science , aquatic ecosystem , denitrification , nitrogen cycle , nitrate , environmental chemistry , nitrification , ecosystem , soil water , biogeochemistry , terrestrial ecosystem , isotope analysis , nitrogen , ecology , chemistry , soil science , biology , organic chemistry
Nitrogen inputs into stream and river ecosystems, and the factors influencing those inputs, are important for various ecological and environmental concerns. Reliable information on where and how nitrogen compounds flow into aquatic ecosystems is indispensable to understanding the nutrient status of these ecosystems. Such information should include the biogeochemical mechanisms and hydrological controls of nutrient leaching into rivers from terrestrial systems such as forests, agricultural fields, and urbanized areas. Advancements in stable isotopomer measurements over the past two decades have expanded the variety of target substances and the precision with which they can be investigated. The high‐throughput microbial denitrifier method allows for simultaneous measurement of nitrogen and oxygen isotope ratios and can provide high‐resolution spatiotemporal information on both nitrate sources and biogeochemical processes. Although advanced techniques of stable isotope analysis have been used extensively to detect sources and estimate the relative contributions of multi‐source systems in various rivers, there are still new horizons in investigating nitrogen transformations. For example, stable isotopes of oxygen ( 18 O and 17 O) occurring in nitrate due to atmospheric deposition can be used as natural tracers for evaluating internal nitrogen cycling; these isotopes are distinct from the oxygen within microbially generated nitrate in soils and water bodies. Another future challenge is improved use of nitrous oxide isotopomers in evaluating the relative contributions of nitrification and denitrification. Such analysis could provide insight into the nitrogen transformation that occurs under redox conditions at the boundary between terrestrial and aquatic systems, where nitrification and denitrification often occur simultaneously in soil and aquatic environments.