δ15N (delta-15 N) refers to the ratio of two stable nitrogen isotopes: 15N:14N. Each contains seven protons with the former containing eight neutrons and the latter, seven neutrons. δ15N analysis, also referred to as isotopic signature, can be used to illuminate past and present climatic conditions and to provide further information for source attribution efforts. It plays an important role in agriculture and soil science, hydrology, ocean science, and paleoclimatology research applications.
For example, with climate as a primary driver of the nitrogen cycle, δ15N levels in foliage have been directly correlated to mean annual temperature and show an inverse relationship with mean annual precipitation. δ15N soil values have also been positively correlated with aridity. Other studies have explored the use of δ15N values for source attribution in agriculture, for example, to identify the type and amount of fertilizer used or to examine nitrogen sources of groundwater contamination.
Picarro has designed and produced two isotope analyzers that precisely measure δ15N in nitrous oxide for laboratory and field studies.
The Picarro G5102-i isotopic and gas concentration analyzer enables measurements of site specific and bulk δ15N in N2O. It is an ideal solution for discerning and measuring the source of N2O emissions real-time in the field or through grab-sample measurements in the lab. The isotopomers of N2O can be used to probe sources and sinks in the global nitrogen cycle by identifying nitrification and denitrification processes in soils and water.
The Picarro G5131-i isotopic and gas concentration analyzer enables simultaneous measurements of site specific and bulk δ15N and δ18O in N2O. It is an ideal solution for discerning and measuring the source of N2O emissions real-time in the field or through grab-sample measurements in the lab.