The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources

Drought conditions are expected to increase in frequency and severity as the climate changes, representing a threat to carbon sequestered in peat soils. Downstream water treatment works are also at risk of regulatory compliance failures and higher treatment costs due to the increase in riverine...

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Main Authors: J. P. Ritson, R. E. Brazier, N. J. D. Graham, C. Freeman, M. R. Templeton, J. M. Clark
Format: Article
Language:English
Published: Copernicus Publications 2017-06-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/14/2891/2017/bg-14-2891-2017.pdf
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spelling doaj-786cc506e78c49fab167934c944420272020-11-24T20:50:17ZengCopernicus PublicationsBiogeosciences1726-41701726-41892017-06-01142891290210.5194/bg-14-2891-2017The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sourcesJ. P. Ritson0R. E. Brazier1N. J. D. Graham2C. Freeman3M. R. Templeton4J. M. Clark5Department of Civil and Environmental Engineering, Imperial College London, South Kensington, London, SW7 2AZ, UKGeography, College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, UKDepartment of Civil and Environmental Engineering, Imperial College London, South Kensington, London, SW7 2AZ, UKWolfson Carbon Capture Laboratory, School of Biological Sciences, Bangor University, Bangor, Gwynedd, LL57 2UW, UKDepartment of Civil and Environmental Engineering, Imperial College London, South Kensington, London, SW7 2AZ, UKDepartment of Geography and Environmental Science, School of Archaeology, Geography and Environmental Science, the University of Reading, Whiteknights campus, P.O. Box 227, Reading, RG6 6AB, UKDrought conditions are expected to increase in frequency and severity as the climate changes, representing a threat to carbon sequestered in peat soils. Downstream water treatment works are also at risk of regulatory compliance failures and higher treatment costs due to the increase in riverine dissolved organic carbon (DOC) often observed after droughts. More frequent droughts may also shift dominant vegetation in peatlands from <i>Sphagnum</i> moss to more drought-tolerant species. This paper examines the impact of drought on the production and treatability of DOC from four vegetation litters (<i>Calluna vulgaris</i>, <i>Juncus effusus</i>, <i>Molinia caerulea</i> and <i>Sphagnum</i> spp.) and a peat soil. We found that mild droughts caused a 39.6 % increase in DOC production from peat and that peat DOC that had been exposed to oxygen was harder to remove by conventional water treatment processes (coagulation/flocculation). Drought had no effect on the amount of DOC production from vegetation litters; however large variation was observed between typical peatland species (<i>Sphagnum</i> and <i>Calluna</i>) and drought-tolerant grassland species (<i>Juncus</i> and <i>Molinia</i>), with the latter producing more DOC per unit weight. This would therefore suggest the increase in riverine DOC often observed post-drought is due entirely to soil microbial processes and DOC solubility rather than litter layer effects. Long-term shifts in species diversity may, therefore, be the most important impact of drought on litter layer DOC flux, whereas pulses related to drought may be observed in peat soils and are likely to become more common in the future. These results provide evidence in support of catchment management which increases the resilience of peat soils to drought, such as ditch blocking to raise water tables.http://www.biogeosciences.net/14/2891/2017/bg-14-2891-2017.pdf
collection DOAJ
language English
format Article
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author J. P. Ritson
R. E. Brazier
N. J. D. Graham
C. Freeman
M. R. Templeton
J. M. Clark
spellingShingle J. P. Ritson
R. E. Brazier
N. J. D. Graham
C. Freeman
M. R. Templeton
J. M. Clark
The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources
Biogeosciences
author_facet J. P. Ritson
R. E. Brazier
N. J. D. Graham
C. Freeman
M. R. Templeton
J. M. Clark
author_sort J. P. Ritson
title The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources
title_short The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources
title_full The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources
title_fullStr The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources
title_full_unstemmed The effect of drought on dissolved organic carbon (DOC) release from peatland soil and vegetation sources
title_sort effect of drought on dissolved organic carbon (doc) release from peatland soil and vegetation sources
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2017-06-01
description Drought conditions are expected to increase in frequency and severity as the climate changes, representing a threat to carbon sequestered in peat soils. Downstream water treatment works are also at risk of regulatory compliance failures and higher treatment costs due to the increase in riverine dissolved organic carbon (DOC) often observed after droughts. More frequent droughts may also shift dominant vegetation in peatlands from <i>Sphagnum</i> moss to more drought-tolerant species. This paper examines the impact of drought on the production and treatability of DOC from four vegetation litters (<i>Calluna vulgaris</i>, <i>Juncus effusus</i>, <i>Molinia caerulea</i> and <i>Sphagnum</i> spp.) and a peat soil. We found that mild droughts caused a 39.6 % increase in DOC production from peat and that peat DOC that had been exposed to oxygen was harder to remove by conventional water treatment processes (coagulation/flocculation). Drought had no effect on the amount of DOC production from vegetation litters; however large variation was observed between typical peatland species (<i>Sphagnum</i> and <i>Calluna</i>) and drought-tolerant grassland species (<i>Juncus</i> and <i>Molinia</i>), with the latter producing more DOC per unit weight. This would therefore suggest the increase in riverine DOC often observed post-drought is due entirely to soil microbial processes and DOC solubility rather than litter layer effects. Long-term shifts in species diversity may, therefore, be the most important impact of drought on litter layer DOC flux, whereas pulses related to drought may be observed in peat soils and are likely to become more common in the future. These results provide evidence in support of catchment management which increases the resilience of peat soils to drought, such as ditch blocking to raise water tables.
url http://www.biogeosciences.net/14/2891/2017/bg-14-2891-2017.pdf
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