EGU21-4512
https://doi.org/10.5194/egusphere-egu21-4512
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Can we improve soil properties and plant biomass using rock powder as soil amendment?

Lena Reifschneider1, Vinzenz Franz Eichinger2, Evelin Pihlap1,3, Noelia Garcia-Franco1, Anna Kühnel4, Franziska Bucka1, Ingrid Kögel-Knabner1, and Alix Vidal1
Lena Reifschneider et al.
  • 1Chair of Soil Science, Research Department Ecology and Ecosystem Management, Technical University of Munich, 85354 Freising, Germany (bodenkunde@wzw.tum.de)
  • 2Extraordinariat für Geomorphologie und Bodenkunde, Technical University of Munich, 85354 Freising, Germany
  • 3Soil Monitoring and Research Bureau, Agricultural Research Centre, 51010 Tartu, Estonia
  • 4Institute for Organic Farming, Soil and Resource Management, Bavarian State Research Center for Agriculture, 85354 Freising, Germany

The application of rock powder is an option to improve soil fertility while valorising the overburden material produced by industries. The “enhanced weathering” of silicate rock has also gained recent interest in the scientific community for its potential to mitigate climate change. However, the effect of rock powder on the soil physical properties remains unclear, especially under climate change (e.g., increasing drought events). Prior to any large scale application of rock powder, it is crucial to disentangle the potential effects of rock powder application on its environment. In a mesocosm experiment, we explored the effect of three rock powders on plant biomass, soil aggregation and organic carbon (OC) allocation within aggregates, in two soils with clayey and sandy textures, under regular watering or severe drought conditions. We demonstrate that the rock powder was the third factor after drought and soil texture significantly affecting the plant growth, resulting in a significant plant biomass decrease ranging from - 13 % to - 42 % compared with the control. We mainly attribute this effect to the increase of the already neutral soil pH, along with the release of excessive heavy metal amounts at a toxic range for the plant. Yet, we found that adding rock powder to the soil resulted in an increase of the relative amount of microaggregates in the soil by up to + 70 %, along with a re-distribution of OC within the fine fractions of the soil (up to + 32 % of OC in < 250 µm fractions). The new mineral-mineral and organo-mineral interactions promoted by the rock powder addition could potentially favour OC persistence in soil on the long term. With our results, we insist on the potential risks for plant growth associated to the application of rock powder when not handled properly. In addition to the current enthusiasm around the capacity of rock powder to enhance carbon sequestration in the inorganic form, we also encourage scientists to focus their research on its effect on soil structure properties and OC storage.

How to cite: Reifschneider, L., Eichinger, V. F., Pihlap, E., Garcia-Franco, N., Kühnel, A., Bucka, F., Kögel-Knabner, I., and Vidal, A.: Can we improve soil properties and plant biomass using rock powder as soil amendment?, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-4512, https://doi.org/10.5194/egusphere-egu21-4512, 2021.

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