Cited by 14Soil erosion and sediment transportSoil Carbon and Nitrogen DynamicsHydrology and Sediment Transport Processes

Fluvial sedimentary deposits as carbon sinks: organic carbon pools and stabilization mechanisms across a Mediterranean catchment

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Martínez-Mena, María, Almagro, María, García-Franco, Noelia, de Vente, Joris, García, Eloisa, Boix-Fayos, Carolina·2019·Biogeosciences

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Abstract

Abstract. The role of fluvial sedimentary areas as organic carbon sinks remains largely unquantified. Little is known about mechanisms of organic carbon (OC) stabilization in alluvial sediments in semiarid and sub-humid catchments where those mechanisms are quite complex because sediments are often redistributed and exposed to a range of environmental conditions in intermittent and perennial fluvial courses within the same catchment. The main goal of this study was to evaluate the contribution of transport and depositional areas as sources or sinks of CO2 at the catchment scale. We used physical and chemical organic matter fractionation techniques and basal respiration rates in samples representative of the three phases of the erosion process within the catchment: (i) detachment, representing the main sediment sources from forests and agricultural upland soils, as well as fluvial lateral banks; (ii) transport, representing the main channel as suspended load and bedload; and (iii) depositional areas along the channel, downstream in alluvial wedges and in the reservoir at the outlet of the catchment, representative of medium and long-term residence deposits, respectively. Our results show that most of the sediments transported and deposited downstream come from agricultural upland soils and fluvial lateral bank sources, where the physico-chemical protection of OC is much lower than that of the forest soils, which are less sensitive to erosion. The protection of OC in forest soils and medium-term depositional areas (alluvial wedges) was mainly driven by physical stabilization mechanisms, while chemical protection of OC was observed in the fluvial lateral banks. However, in the remaining sediment sources, in sediments during transport, and after deposition in long-term deposits (the reservoir), both mechanisms are equally relevant. Mineralization of the most labile OC, intra-aggregate particulate organic matter (MPOM), was predominant during transport. Aggregate formation and OC accumulation, mainly associated with macroaggregates and occluded microaggregates within macroaggregates, were predominant in depositional areas, being more protected than the OC from the most eroding sources (agricultural soils and fluvial lateral banks). Both temporary and permanent sediment deposits in the catchment have an important role in erosive areas, compensating OC losses from the eroded sources and functioning as C sinks.

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Crossref · 10.5194/bg-16-1035-2019

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  • Vegetation covers in almond crops reduce soil erosion by 51-95%.

    “and reduce soil erosion by 51-95% (Durán Zuazo and Rodríguez Pleguezuelo, 2008;Martínez-Mena et al., 2019).”

    From Almond farm profitability under agroecological management in south-eastern Spain: Accounting for externalities and opportunity costs (2020) · cites this paper as Martínez-Mena et al., 2019

    The field sampling section (2.2; page unavailable) describes forest and agricultural soils, while section 3.4 discusses water erosion and organic-carbon stabilization. Searches for almond crops, vegetation cover, and a 51–95% erosion reduction found no passage addressing that claim. (LLM, conf=0.76)

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1 of the 65 references couldn’t be matched to a known paper.

Research works printed but not linked: 1

  1. Paul, E. A., Morris, S. J., and Boehm, S.: The determination of soil C pool sizes and turnover rates: biophysical fractionation and tracers, in: Assessment Methods for Soil Carbon (Advances in Soil Science),edited by: Lal, R., Kimble, J. M., Follett, R. F., and Stewart, B. A., CRC Press LLC, Boca Raton, FL, USA, 193-206, 2001.

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Authors
Martínez-Mena, M., Almagro, M., García-Franco, N., de Vente, J., García, E., & Boix-Fayos, C.
Affiliations
  • University of the Basque Country (ES)
  • Technical University of Munich (DE)
  • Consejo Superior de Investigaciones Científicas (ES)
Corresponding author
  • Almagro, María
  • García-Franco, Noelia
  • García, Eloisa
Venue
Biogeosciences
Published
2019-03-15
Volume
16
Issue
5
Pages
1035-1051
ISSN
  • 1726-4170 (ISSN-L)
  • 1726-4189
OpenAlex
W2894875741
Cited by
14
References
65
Citations by year
2025: 1 · 2024: 1 · 2023: 3 · 2022: 1 · 2021: 2 · 2020: 4 · 2019: 2
FWCI
1.79
Type
journal article
Language
en
Open access
Locations
  • Biogeosciences (publishedVersion, cc-by)
  • Communities in ADDI (Universidad del Pais Vasco) (submittedVersion, other-oa)
  • LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas) (submittedVersion, cc-by-nc-sa)
  • DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
  • Hispana (submittedVersion, cc-by-nc-sa)
  • mediaTUM (Technical University of Munich) (submittedVersion, other-oa)
  • Biogeosciences (European Geosciences Union) (submittedVersion, cc-by)
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil erosion and sediment transport
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
  • Physical Sciences › Environmental Science › Ecology › Hydrology and Sediment Transport Processes
Keywords
organic carbon stabilization, carbon sink, alluvial deposits, soil organic carbon, sediment transport, organic matter fractionation, basal respiration, soil aggregates, mineral-associated organic carbon, forest soils, reservoir sediments, Mediterranean catchments

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