Ammonium and nitrate in ice accretions and snow at two Central European montane locations: δ15N and δ18OH2O isotope ratios, fluxes and sources

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020699%3A_____%2F25%3AN0000089" target="_blank" >RIV/00020699:_____/25:N0000089 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11320/25:10507380

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S004896972408361X" target="_blank" >https://www.sciencedirect.com/science/article/pii/S004896972408361X</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.scitotenv.2024.178203" target="_blank" >10.1016/j.scitotenv.2024.178203</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Ammonium and nitrate in ice accretions and snow at two Central European montane locations: δ15N and δ18OH2O isotope ratios, fluxes and sources

Popis výsledku v původním jazyce

In many countries worldwide, NOx emissions currently decrease as a result of pollution control, while NH3 emissions stagnate or continue to increase. Little is known about horizontal deposition of NO3− and NH4+, the oxidation/neutralization products of these primary pollutants. To close the knowledge gap, we studied atmospheric inputs of NO3− and NH4+ at two mountain-top sites near the Czech–German–Polish borders during winter. Horizontal deposition via ice accretions (rime) made up 26–30 % of total atmospheric input of reactive nitrogen (Nr). Such high horizontal depositions should not be neglected in ecosystem N studies which currently often consider only vertical deposition via snow. Snow nitrate N was the largest type of Nr deposition (40–52 %), with snow ammonium N being the second largest (20–30 %). Rime ammonium N contributed a similar amount to total Nr input as rime nitrate N (12–16 %). The total inorganic Nr deposition was 4–6 kg ha−1 winter−1. Across the sites, the mean δ15 and δ15 values fell in a relatively narrow range from −3.1 to −7.3 ‰. Three systematic isotope patterns were observed: (i) NH4+-N was always heavier in rime than in snow, (ii) NO3−-N was always heavier in rime than in snow, and (iii) NO3−-N was always heavier than NH4+-N. For source apportionment, the Bayesian isotope mixing model SIMMR was used. Counter-intuitively, vehicles were larger sources of NH3 in rime than volatilation from animal waste plus fertilizers (46 vs. 19 %). The largest NO3− contributions to rime were derived from vehicles and biomass burning, followed by natural gas combustion and coal burning in power plants and households. Natural gas represented the largest source of nitrate in snow. Nitrate sources appeared to be better-mixed than ammonium sources. Our isotope-based source apportionment differed from national emission inventories, offering original insights into local atmospheric Nr inputs.

Název v anglickém jazyce

Ammonium and nitrate in ice accretions and snow at two Central European montane locations: δ15N and δ18OH2O isotope ratios, fluxes and sources

Popis výsledku anglicky

In many countries worldwide, NOx emissions currently decrease as a result of pollution control, while NH3 emissions stagnate or continue to increase. Little is known about horizontal deposition of NO3− and NH4+, the oxidation/neutralization products of these primary pollutants. To close the knowledge gap, we studied atmospheric inputs of NO3− and NH4+ at two mountain-top sites near the Czech–German–Polish borders during winter. Horizontal deposition via ice accretions (rime) made up 26–30 % of total atmospheric input of reactive nitrogen (Nr). Such high horizontal depositions should not be neglected in ecosystem N studies which currently often consider only vertical deposition via snow. Snow nitrate N was the largest type of Nr deposition (40–52 %), with snow ammonium N being the second largest (20–30 %). Rime ammonium N contributed a similar amount to total Nr input as rime nitrate N (12–16 %). The total inorganic Nr deposition was 4–6 kg ha−1 winter−1. Across the sites, the mean δ15 and δ15 values fell in a relatively narrow range from −3.1 to −7.3 ‰. Three systematic isotope patterns were observed: (i) NH4+-N was always heavier in rime than in snow, (ii) NO3−-N was always heavier in rime than in snow, and (iii) NO3−-N was always heavier than NH4+-N. For source apportionment, the Bayesian isotope mixing model SIMMR was used. Counter-intuitively, vehicles were larger sources of NH3 in rime than volatilation from animal waste plus fertilizers (46 vs. 19 %). The largest NO3− contributions to rime were derived from vehicles and biomass burning, followed by natural gas combustion and coal burning in power plants and households. Natural gas represented the largest source of nitrate in snow. Nitrate sources appeared to be better-mixed than ammonium sources. Our isotope-based source apportionment differed from national emission inventories, offering original insights into local atmospheric Nr inputs.

Druh

J_SC - Článek v periodiku v databázi SCOPUS

CEP obor

—

OECD FORD obor

10511 - Environmental sciences (social aspects to be 5.7)

Projekt

<a href="/cs/project/SS02030031" target="_blank" >SS02030031: Integrovaný systém výzkumu, hodnocení a kontroly kvality ovzduší</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Science of The Total Environment

ISSN

0048-9697

e-ISSN

1879-1026

Svazek periodika

959

Číslo periodika v rámci svazku

178203

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

14

Strana od-do

nestrankovano

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-85212830063