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8
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Introduction
Dave is a soil scientist and carbon modeler born and raised in British Columbia, Canada. He earned his Bachelor's Degree from The University of British Columbia Okanagan Campus (UBCO) studying Biology and Computer Science. He then went on to earn his Master's of Biology with the Jones Soil Lab at UBCO and collaborators at Agriculture and Agri-food Canada. Dave now studies in Braunschweig, Germany where he is pursuing his PhD at the Thünen-Institut für Agrarklimaschutz.
Current institution
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December 2020 - March 2022
May 2019 - May 2021
Publications
Publications (8)
Converting natural vegetation for agriculture has resulted in the loss of approximately 5% of the current global terrestrial soil organic carbon (SOC) stock to the atmosphere. Increasing the agricultural area under grassland may reverse some of these losses, but the effectiveness of such a strategy is limited by how quickly SOC recovers after conve...
Munoz et al. (2024) raised concerns regarding our recent contribution and the definition of the term C sequestration in soils (Don et al., 2024). We performed a review and therefore based our analysis on existing definitions of C sequestrations, mainly by the IPCC. We recommend sticking with terminologies around C sequestration and climate mitigati...
The term carbon (C) sequestration has not just become a buzzword but is something of a siren's call to scientific communicators and media outlets. Carbon sequestration is the removal of C from the atmosphere and the storage, for example, in soil. It has the potential to partially compensate for anthropogenic greenhouse gas emissions and is, therefo...
To successfully reduce atmospheric CO 2 by sequestering additional soil carbon, it is essential to understand the potential of a given soil to store carbon in a stable form. Carbon that has formed organo-mineral complexes with silt and clay particles is believed to be less susceptible to decay than non-complexed, or particulate, organic carbon. Usi...
Over the last 200 years, conversion of non‐cultivated land for agriculture has substantially reduced global soil organic carbon (SOC) stocks in upper soil layers. Nevertheless, practices such as no‐ or reduced tillage, application of organic soil amendments, and maintenance of continuous cover can increase SOC in agricultural fields. While these ma...
Agricultural practices such as annual crop production, land use change and grazing on marginal lands lead to a loss of soil carbon (C) stock. But soil C losses are not universal in agricultural systems and modest soil C gains can occur when constraints such as a lack of water are removed. To characterize this we used a meta-analysis of published da...
Increasing the carbon (C) content of agricultural soils can help mitigate rising atmospheric CO2 concentrations, improve soil health and increase crop yield. Unlike annual cropping systems, soils planted to perennial woody crops, such as vineyards and orchards, are left undisturbed for many years making them particularly amenable to soil C storage....
