Soil carbon loss from drained agricultural peatland after coverage with mineral soil
Creators
- 1. Environmental Geosciences, University of Basel, Bernoullistrasse 30, 4056 Basel (Switzerland)
- 2. Climate and Agriculture Group, Agroscope, Reckenholzstrasse 191, 8046 Zürich (Switzerland)
- 3. Oeschger Centre for Climate Change Research, University of Bern, Hochschulstrasse 4, 3012 Bern (Switzerland)
- 4. Department of Chemistry, Biochemistry and Pharmaceutical Sciences, University of Bern, Freiestrasse 3, 3012 Bern (Switzerland)
Description
Highlights: • Sustained use of drained peatland requires halting the decline of peatland carbon stocks. • Mineral soil coverage has become an increasingly used management in drained peatland. • Mineral soil coverage does not reduce heterotrophic respiration from drained peatland. • Decomposition of relatively old peat carbon is reduced after mineral soil coverage. Drainage for agriculture has turned peatlands from a net sink to a net source of carbon (C). In order to reduce the environmental footprint of agricultural peatland drainage, and to counteract soil subsidence, mineral soil coverage is becoming an increasingly used practice in Switzerland. To explore the effect of mineral soil coverage on soil C loss and the source of CO2 from peatland drained for agriculture, we utilized the radiocarbon signature (F14C) of soil C and emitted CO2 in the field. The experiment, located in the Swiss Rhine Valley, was carried out on two adjacent drained organic soils, either without mineral soil cover (reference 'Ref'), or covered with mineral soil (thickness ~ 40 cm) (coverage 'Cov') 13 years ago. Drainage already commenced 130 years ago and the site was managed as meadow since the 1970ies. Drainage induced 41–75 kg C m−2 loss, which is equivalent to annual C loss rates of 0.49–0.58 kg C m−2 yr−1 and 0.31–0.63 kg C m−2 yr−1 for Cov and Ref, respectively. Mineral soil coverage had no significant effect on the amount of heterotrophic respiration, however, at Cov, the radiocarbon signature of heterotrophic CO2 was significantly (p 0.01) younger than at Ref, indicating that mineral soil coverage moved the source of decomposition of soil organic carbon (SOC) from a higher share of old peat towards a higher share of relatively younger material. In summary, our study lends support to the hypothesis that mineral soil coverage might reduce the decomposition of old peat underneath, and may therefore be a promising peatland management technique for the future use of drained peatland for agriculture.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2021.149498Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2021.149498;
- PII
- S0048969721045721;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 800
- Journal Page Range
- vp.
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54061336
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AGRICULTURE; CARBON; CARBON DIOXIDE; EMISSION; GROUND SUBSIDENCE; PEAT; RHINE RIVER; SOILS; WETLANDS
- Descriptors DEC
- AQUATIC ECOSYSTEMS; CARBON COMPOUNDS; CARBON OXIDES; CHALCOGENIDES; ECOSYSTEMS; ELEMENTS; ENERGY SOURCES; FOSSIL FUELS; FUELS; MATTER; NONMETALS; ORGANIC MATTER; OXIDES; OXYGEN COMPOUNDS; RIVERS; SOLID FUELS; SURFACE WATERS
Optional Information
- Copyright
- Copyright (c) 2021 Published by Elsevier B.V.