Initial validation of a soil-based mass-balance approach for empirical monitoring of enhanced rock weathering rates
Tom Reershemius, Mike E. Kelland, Jacob S. Jordan, Isabelle R., Davis, Rocco D'Ascanio, Boriana Kalderon-Asael, Dan Asael, T. Jesper, Suhrhoff, Dimitar Z. Epihov, David J. Beerling, Christopher T. Reinhard, Noah, J. Planavsky

TL;DR
This paper presents a soil-based mass-balance method using isotope-dilution mass spectrometry to accurately monitor carbon removal in enhanced rock weathering, validated through controlled experiments with promising initial results.
Contribution
It introduces a novel, cost-effective soil analysis approach for MRV of ERW, improving accuracy and robustness over existing methods.
Findings
Method accurately estimates initial CDR within error margins.
Controlled mesocosm experiments demonstrate feasibility.
Provides a robust, time-integrated CDR measurement.
Abstract
Enhanced Rock Weathering (ERW) is a promising scalable and cost-effective Carbon Dioxide Removal (CDR) strategy with significant environmental and agronomic co-benefits. A major barrier to large-scale implementation of ERW is a robust Monitoring, Reporting, and Verification (MRV) framework. To successfully quantify the amount of carbon dioxide removed by ERW, MRV must be accurate, precise, and cost-effective. Here, we outline a mass-balance-based method where analysis of the chemical composition of soil samples is used to track in-situ silicate rock weathering. We show that signal-to-noise issues of in-situ soil analysis can be mitigated by using isotope-dilution mass spectrometry to reduce analytical error. We implement a proof-of-concept experiment demonstrating the method in controlled mesocosms. In our experiment, basalt rock feedstock is added to soil columns containing the cereal…
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Taxonomy
TopicsCO2 Sequestration and Geologic Interactions · Geological and Geophysical Studies Worldwide · Methane Hydrates and Related Phenomena
