EGU26-11419, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-11419
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 11:45–11:55 (CEST)
 
Room 0.11/12
An Integrated Modelling Framework to Determine Terrestrial Carbon Dioxide Removal via Enhanced Rock Weathering
Ziyan Zhang1, Gregory Jones2, Salvatore Calabrese3, Matteo Bertagni4, Simone Fatichi5, Bonnie Waring2, and Athanasios Paschalis6
Ziyan Zhang et al.
  • 1Imperial College London, Imperial College London, Department of Civil and Environmental Engineering, London, United Kingdom of Great Britain – England, Scotland, Wales (ziyan.zhang14@imperial.ac.uk)
  • 2Department of Life Sciences, Imperial College London, London, UK
  • 3Biological and Agricultural Engineering, Texas A&M University, College Station, USA
  • 4Department of Environment, Land and Infrastructure Engineering, Polytechnic University of Turin, Italy
  • 5Department of Civil and Environmental Engineering, National University of Singapore, Singapore
  • 6Department of Civil and Environmental Engineering, University of Cyprus, Nicosia, Cyprus

Enhanced rock weathering (ERW) is an emerging carbon dioxide removal (CDR) strategy that can support net-zero emission targets. However, current ERW modelling efforts rely on assumptions that introduce substantial variation in CDR estimates across varying ecosystems and hydroclimatic conditions. They typically ignore or oversimplify plant–soil interactions and high-frequency hydrological dynamics, obscuring short-term weathering responses and biotic feedbacks to soil moisture dynamics. Here, we introduce an integrated, process-based modelling framework, T&C-SMEW, which represents ecohydrological and ERW dynamics, along with microbially explicit biogeochemical processes. We compared framework simulations against a controlled mesocosm experiment and long-term field observations, demonstrating its ability to reproduce feedstock cation release, soil pH dynamics, gross primary production, and CO2 fluxes. T&C-SMEW reveals hydrological constraints and vegetation effects on ERW-mediated CDR by quantifying impacts on ecosystem respiration, net ecosystem exchange, and alkalinity export, emphasising the importance of ecohydrological modelling for ecosystem-level CDR estimation. These advances provide a modelling framework for identifying optimal deployment scenarios to establish ERW as a viable and operationally feasible CDR approach.

How to cite: Zhang, Z., Jones, G., Calabrese, S., Bertagni, M., Fatichi, S., Waring, B., and Paschalis, A.: An Integrated Modelling Framework to Determine Terrestrial Carbon Dioxide Removal via Enhanced Rock Weathering, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-11419, https://doi.org/10.5194/egusphere-egu26-11419, 2026.