Constraints and Drivers of Dissolved Fluxes of Pyrogenic Carbon in Soil and Freshwater Systems: A Global Review and Meta‐Analysis

Abney, R. B.; Barnes, M. E.; Moss, A.; Santos, F.

doi:10.1029/2023GB008092

Title: Constraints and Drivers of Dissolved Fluxes of Pyrogenic Carbon in Soil and Freshwater Systems: A Global Review and Meta‐Analysis

Journal Article · 22 June 2024 · Global Biogeochemical Cycles

DOI: https://doi.org/10.1029/2023GB008092 · OSTI ID:2377835

^[1];

^[2]; Moss, A. ^[1];

^[3]

Warnell School of Forestry and Natural Resources University of Georgia Athens GA USA
Biological Sciences Division Pacific Northwest National Laboratory Richland WA USA
Environmental Sciences Division Oak Ridge National Laboratory Oak Ridge TN USA

Abstract Pyrogenic carbon (PyC) is a significant component of the global soil carbon pool due to its longer environmental persistence than other soil organic matter components. Despite PyC's persistence in soil, recent work has indicated that it is susceptible to loss processes such as mineralization and leaching, with the significance and magnitude of these largely unknown at the hillslope and watershed scales. We present a review of the work concerning dissolved PyC transport in soil and freshwater. Our analysis found that the primary environmental controls on dissolved PyC (dPyC) transport are the formation conditions and quality of the PyC itself, with longer and higher temperature charring conditions leading to less transport of dPyC. While correlations between dPyC and dissolved organic carbon in rivers and other pools are frequently reported, the slope of these correlations was pool‐dependent (i.e., soil‐water, precipitation, lakes, streams, rivers), suggesting site‐specific environmental controls. However, the lack of consistency in analytical techniques and sample preparation remains a major challenge to quantifying environmental controls on dPyC fluxes. We propose that future research should focus on the following: (a) consistency in methodological approaches, (b) more quantitative measures of dPyC in pools and fluxes from soils to streams, (c) turnover times of dPyC in soils and aquatic systems, and (d) improved understanding of how mechanisms controlling the fate of dPyC in dynamic post‐fire landscapes interact. With more refined quantitative information about the controls on dPyC transport at the hillslope and landscape scale, we can increase the accuracy and utility of global carbon models.

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Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States); Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)

Sponsoring Organization:: USDOE; USDOE Laboratory Directed Research and Development (LDRD) Program; USDOE Office of Science (SC), Biological and Environmental Research (BER). Earth & Environmental Systems Science (EESS)

Grant/Contract Number:: AC05-00OR22725; AC05-76RL01830

OSTI ID:: 2377835

Report Number(s):: PNNL-SA--199875; e2023GB008092

Journal Information:: Global Biogeochemical Cycles, Journal Name: Global Biogeochemical Cycles Journal Issue: 6 Vol. 38; ISSN 0886-6236

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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Fire Reduces Fungal Species Richness and In Situ Mycorrhizal Colonization: A Meta-Analysis Dove, Nicholas C.; Hart, Stephen C. Fire Ecology, Vol. 13, Issue 2 https://doi.org/10.4996/fireecology.130237746	journal	August 2017

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