Potential canopy influences on the isotopic composition of nitrogen and sulphur in atmospheric deposition

@article{Heaton1997PotentialCI,
  title={Potential canopy influences on the isotopic composition of nitrogen and sulphur in atmospheric deposition},
  author={Tim H. E. Heaton and Baruch Spiro and S. M. Robertson},
  journal={Oecologia},
  year={1997},
  volume={109},
  pages={600-607}
}
Abstract Isotopic studies of nitrogen and sulphur inputs to plant/soil systems commonly rely on limited published data for the 15N/14N and 34S/32S ratios of nitrate, ammonium and sulphate in rainfall. For systems with well-developed plant canopies, however, inputs of these ions from dry deposition or particulates may be more important than rainfall. The manner in which isotopic fractionation between ions and gases may lead to dry deposition and particulates having 15N/14N or 34S/32S ratios… 

Stable N isotope composition of nitrate reflects N transformations during the passage of water through a montane rain forest in Ecuador

Knowledge of the fate of deposited N in the possibly N-limited, highly biodiverse north Andean forests is important because of the possible effects of N inputs on plant performance and species

Dominance of biologically produced nitrate in upland waters of Great Britain indicated by stable isotopes

Atmospheric deposition of nitrogen (N) compounds is the major source of anthropogenic N to most upland ecosystems, where leaching of nitrate (NO3−) into surface waters contributes to eutrophication

Partitioning between atmospheric deposition and canopy microbial nitrification into throughfall nitrate fluxes in a Mediterranean forest

Microbial activity plays a central role in nitrogen (N) cycling, with effects on forest productivity. Although N biotransformations, such as nitrification, are known to occur in the soil, here we

Isotopic composition of nitrate in wet and dry atmospheric deposition on Crete in the eastern Mediterranean Sea

The eastern Mediterranean Sea (EMS) is a nutrient‐poor ocean with unusually high nitrate‐phosphate ratios (up to 28:1) and relatively depleted 15N/14N ratios (expressed as δ15N) in deepwater nitrate

Great Britain indicated by stable isotopes

14 Atmospheric deposition of nitrogen (N) compounds is the major source of anthropogenic N to most 15 upland ecosystems, where leaching of nitrate (NO3) into surface waters contributes to

Isotopic constraints on the atmospheric sources and formation of nitrogenous species in clouds influenced by biomass burning

Abstract. Predicting tropospheric cloud formation and subsequent nutrient deposition relies on understanding the sources and processes affecting aerosol constituents of the atmosphere that are

Natural 15N abundance of epiphytes depends on the position within the forest canopy: source signals and isotope fractionation

The natural (15)N abundance (delta(15)N) of epiphytes and its N sources were studied in the canopy of a lowland rainforest in Costa Rica. Vascular and non-vascular epiphytes and canopy soils were
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