Modelling the impacts of climate change on agrochemical fate and transport by water on a catchment scale.


Journal

Heliyon
ISSN: 2405-8440
Titre abrégé: Heliyon
Pays: England
ID NLM: 101672560

Informations de publication

Date de publication:
15 Aug 2024
Historique:
received: 06 03 2024
revised: 31 07 2024
accepted: 01 08 2024
medline: 22 8 2024
pubmed: 22 8 2024
entrez: 22 8 2024
Statut: epublish

Résumé

The export of agrochemicals and their transformation products (TPs) following their application in the agricultural fields poses a threat to water quality. Future changes in climatic conditions (e.g. extreme weather events such as heavy rainfall or extended dry periods) could alter the degradation and mobility of agrochemicals. In this research, we use an integrated modelling framework to understand the impact of extreme climate events on the fate and transport of the agrochemical S-Metolachlor and two of its TPs (M-OXA, Metolachlor Oxanilic Acid and M-ESA, Metolachlor Ethyl Sulfonic Acid). This is done by coupling climate model outputs to the Zin-AgriTra agrochemical reactive transport model in four simulation scenarios. 1) Reference (2015-2018), 2) Very dry (2038-2041), 3) Very wet (2054-2057) and 4) High temperature (2096-2099) conditions of a selected RCP8.5 based regional climate scenario. The modelling framework is tested on an agricultural catchment, Wulka, in Burgenland, Austria. The model results indicate that 13-14 % of applied S-Metolachlor is retained in the soil, and around 85 % is degraded into TPs in the different scenarios. In very dry and high-temperature scenarios, degradation is higher, and hence, there is less S-Metolachlor in the soil. However, a large share of formed M-OXA and M-ESA are retained in the soil, which is transported via overland and groundwater flow, leading to a build-up effect in M-OXA and M-ESA river concentrations over the years. Though a small share of S-Metolachlor and TPs are transported to rivers, their river export is affected by the intensity and amount of rainfall. The very wet and high-temperature scenarios show higher S-Metolachlor and TP concentrations at the catchment outlet due to higher river discharge. The reference scenario shows higher river peak concentrations associated with higher overland flow caused by measured hourly rainfall compared to disaggregated daily precipitation data in the other scenarios.

Identifiants

pubmed: 39170220
doi: 10.1016/j.heliyon.2024.e35669
pii: S2405-8440(24)11700-8
pmc: PMC11336872
doi:

Types de publication

Journal Article

Langues

eng

Pagination

e35669

Informations de copyright

© 2024 The Authors.

Déclaration de conflit d'intérêts

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Poornima Nagesh (P)

Copernicus Institute of Sustainable Development, Utrecht University, Utrecht, the Netherlands.

Matthias Gassmann (M)

Department of Hydrology and Substance Balance, University of Kassel, Kassel, Germany.

Josef Eitzinger (J)

Institute of Meteorology and Climatology, University of Natural Resources and Life Sciences, Vienna, BOKU, Austria.

Hugo J de Boer (HJ)

Copernicus Institute of Sustainable Development, Utrecht University, Utrecht, the Netherlands.

Oreane Y Edelenbosch (OY)

Copernicus Institute of Sustainable Development, Utrecht University, Utrecht, the Netherlands.

Detlef P van Vuuren (DP)

Copernicus Institute of Sustainable Development, Utrecht University, Utrecht, the Netherlands.
PBL Netherlands Environmental Assessment Agency, the Netherlands.

Stefan C Dekker (SC)

Copernicus Institute of Sustainable Development, Utrecht University, Utrecht, the Netherlands.

Classifications MeSH