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

Publication date

2024-08-15

Authors

Nagesh, PoornimaISNI 0000000506846143
Gassmann, Matthias
Eitzinger, Josef
de Boer, H.J.ORCID 0000-0002-6933-344XISNI 0000000391556946
Edelenbosch, OreaneISNI 0000000493300992
van Vuuren, DetlefORCID 0000-0003-0398-2831ISNI 0000000040910093
Dekker, StefanORCID 0000-0001-7764-2464ISNI 0000000397042727

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Abstract

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.

Keywords

General, SDG 13 - Climate Action, SDG 6 - Clean Water and Sanitation

Citation

Nagesh, P, Gassmann, M, Eitzinger, J, de Boer, H J, Edelenbosch, O Y, van Vuuren, D P & Dekker, S C 2024, 'Modelling the impacts of climate change on agrochemical fate and transport by water on a catchment scale', Heliyon, vol. 10, no. 15, e35669, pp. 1-15. https://doi.org/10.1016/j.heliyon.2024.e35669