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      Potential accumulation of toxic trace elements in soils during enhanced rock weathering

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          Abstract

          Terrestrial enhanced rock weathering (ERW) is a carbon dioxide removal technology that aims at accelerating one of the most powerful negative feedbacks on Earth's climate, the chemical weathering of silicates. To achieve this, ERW proposes to spread ground silicate rock on agricultural soils. According to many models, global application rates of 40 tonnes of ground basaltic rock per hectare and per year would be necessary to sequester a significant amount of CO 2, representing up to 24% of the current net annual increase in atmospheric CO 2. When assessing the viability of ERW as a global geo‐engineering strategy, a pivotal but overlooked question to address is whether ERW may lead to toxic trace element accumulation in soils at unauthorized and potentially harmful levels. This study evaluates the legal sustainability of ERW with regard to trace element contents in soils. We compare different trace element accumulation scenarios considering a range of rock sources, application rates and national regulatory limits. The results indicate that, at the suggested annual application rate of 40 tonnes per hectare, the first regulatory limits would be exceeded after 6 and 10 years for copper and nickel, respectively. This study argues in favour of close tailoring of ERW deployment to local conditions in order to tap into its climate mitigation potential while preserving long‐term soil uses.

          Highlights

          • Terrestrial enhanced rock weathering (ERW) is a carbon sequestration technology that consists in applying rock powder to soils.

          • This study evaluates whether rock powder application can lead to trace metals accumulation in soils beyond regulatory limits.

          • ERW can lead to the overrun of some environmental regulatory limits within less than a decade.

          • Specific site and rock selection will be necessary for this method to preserve long‐term soil uses.

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          Most cited references67

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          Distribution of the Elements in Some Major Units of the Earth's Crust

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            Negative emissions—Part 2: Costs, potentials and side effects

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              Mechanisms of silicon-mediated alleviation of heavy metal toxicity in plants: A review.

              In present era, heavy metal pollution is rapidly increasing which present many environmental problems. These heavy metals are mainly accumulated in soil and are transferred to food chain through plants grown on these soils. Silicon (Si) is the second most abundant element in the soil. It has been widely reported that Si can stimulate plant growth and alleviate various biotic and abiotic stresses, including heavy metal stress. Research to date has explored a number of mechanisms through which Si can alleviate heavy metal toxicity in plants at both plant and soil levels. Here we reviewed the mechanisms through which Si can alleviate heavy metal toxicity in plants. The key mechanisms evoked include reducing active heavy metal ions in growth media, reduced metal uptake and root-to-shoot translocation, chelation and stimulation of antioxidant systems in plants, complexation and co-precipitation of toxic metals with Si in different plant parts, compartmentation and structural alterations in plants and regulation of the expression of metal transport genes. However, these mechanisms might be associated with plant species, genotypes, metal elements, growth conditions, duration of the stress imposed and so on. Further research orientation is also discussed.
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                Author and article information

                Contributors
                (View ORCID Profile)
                (View ORCID Profile)
                Journal
                European Journal of Soil Science
                European J Soil Science
                1351-0754
                1365-2389
                January 2023
                February 07 2023
                January 2023
                : 74
                : 1
                Affiliations
                [1 ] Institute of Earth Surface Dynamics University of Lausanne Lausanne Switzerland
                [2 ] University of Bayreuth Bayreuth Germany
                [3 ] Saint Loup Research Institute Saint Loup Lamairé France
                Article
                10.1111/ejss.13343
                b3e87e6a-abe1-4be7-be42-adf4f6a85c82
                © 2023

                http://creativecommons.org/licenses/by-nc-nd/4.0/

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