Details
| Original language | English |
|---|---|
| Pages (from-to) | 71-84 |
| Number of pages | 14 |
| Journal | Soil Biology and Biochemistry |
| Volume | 135 |
| Early online date | 22 Apr 2019 |
| Publication status | Published - Aug 2019 |
Abstract
Drainage turns peatlands from natural carbon sinks into hotspots of greenhouse gas (GHG)emissions from soils due to alterations in hydrological and biogeochemical processes. As a consequence of drainage-induced mineralisation and anthropogenic sand addition, large areas of former peatlands under agricultural use have soil organic carbon (SOC)contents at the boundary between mineral and organic soils. Previous research has shown that the variability of GHG emissions increases with anthropogenic disturbance. However, how and whether sand addition affects GHG emissions remains a controversial issue. The aim of this long-term incubation experiment was to assess the influence of hydrological and biogeochemical soil properties on emissions of carbon dioxide (CO2), nitrous oxide (N2O)and methane (CH4). Strongly degraded peat with sand addition (peat-sand mixtures)and without sand addition (earthified peat)was systematically compared under different moisture conditions for fen and bog peat. Soil columns originating from both the topsoil and the subsoil of ten different peatlands under grassland use were investigated. Over a period of six months the almost saturated soil columns were drained stepwise via suction to −300 hPa. The CO2 fluxes were lowest at water-saturated and dry soil moisture conditions, resulting in a parabolic dependence of CO2 fluxes on the water-filled pore space (WFPS)peaking at 56–92% WFPS. The highest N2O fluxes were found at between 73 and 95% WFPS. Maximum CO2 fluxes were highest from topsoils, ranging from 21 to 77 mg C m−2 h−1, while the maximum CO2 fluxes from subsoils ranged from 3 to 14 mg C m−2 h−1. No systematic influence of peat type or sand addition on GHG emissions was found in topsoils, but CO2 fluxes from subsoils below peat-sand mixtures were higher than from subsoils below earthified peat. Maximum N2O fluxes were highly variable between sites and ranged from 18.5 to 234.9 and from 0.2 to 22.9 μg N m−2 h−1 for topsoils and subsoils, respectively. CH4 fluxes were negligible even under water-saturated conditions. The highest GHG emissions occurred at a WFPS that relates – under equilibrium conditions – to a water table of 20–60 cm below the surface in the field. High maximum CO2 and N2O fluxes were linked to high densities of plant-available phosphorus and potassium. The results of this study highlight that nutrient status plays a more important role in GHG emissions than peat type or sand addition, and do not support the idea of peat-sand mixtures as a mitigation option for GHG emissions.
Keywords
- Carbon dioxide, Microcosm incubation, Mitigation measures, Nitrous oxide, Peat-sand mixture, Peatland agriculture
ASJC Scopus subject areas
- Immunology and Microbiology(all)
- Microbiology
- Agricultural and Biological Sciences(all)
- Soil Science
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In: Soil Biology and Biochemistry, Vol. 135, 08.2019, p. 71-84.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - How do sand addition, soil moisture and nutrient status influence greenhouse gas fluxes from drained organic soils?
AU - Säurich, Annelie
AU - Tiemeyer, Bärbel
AU - Dettmann, Ullrich
AU - Don, Axel
N1 - Funding information: This work would not have been possible without the help of Frank Hegewald, Stefan Burkart, Thomas Viohl, Arndt Piayda, Mareille Wittnebel, Sebastian Willi Oehmke, Peter Braunisch, Viridiana Alcántara, Roland Prietz, Arne Heidkamp, Anna Jacobs, Angélica Jaconi, Ute Tambor, Nicole Altwein, Daniel Ziehe and Sabine Wathsack. The study was carried out as part of the German Agricultural Soil Inventory, which was funded by the German Federal Ministry of Food and Agriculture. This work would not have been possible without the help of Frank Hegewald, Stefan Burkart, Thomas Viohl, Arndt Piayda, Mareille Wittnebel, Sebastian Willi Oehmke, Peter Braunisch, Viridiana Alcántara, Roland Prietz, Arne Heidkamp, Anna Jacobs, Angélica Jaconi, Ute Tambor, Nicole Altwein, Daniel Ziehe and Sabine Wathsack. The study was carried out as part of the German Agricultural Soil Inventory, which was funded by the German Federal Ministry of Food and Agriculture .
PY - 2019/8
Y1 - 2019/8
N2 - Drainage turns peatlands from natural carbon sinks into hotspots of greenhouse gas (GHG)emissions from soils due to alterations in hydrological and biogeochemical processes. As a consequence of drainage-induced mineralisation and anthropogenic sand addition, large areas of former peatlands under agricultural use have soil organic carbon (SOC)contents at the boundary between mineral and organic soils. Previous research has shown that the variability of GHG emissions increases with anthropogenic disturbance. However, how and whether sand addition affects GHG emissions remains a controversial issue. The aim of this long-term incubation experiment was to assess the influence of hydrological and biogeochemical soil properties on emissions of carbon dioxide (CO2), nitrous oxide (N2O)and methane (CH4). Strongly degraded peat with sand addition (peat-sand mixtures)and without sand addition (earthified peat)was systematically compared under different moisture conditions for fen and bog peat. Soil columns originating from both the topsoil and the subsoil of ten different peatlands under grassland use were investigated. Over a period of six months the almost saturated soil columns were drained stepwise via suction to −300 hPa. The CO2 fluxes were lowest at water-saturated and dry soil moisture conditions, resulting in a parabolic dependence of CO2 fluxes on the water-filled pore space (WFPS)peaking at 56–92% WFPS. The highest N2O fluxes were found at between 73 and 95% WFPS. Maximum CO2 fluxes were highest from topsoils, ranging from 21 to 77 mg C m−2 h−1, while the maximum CO2 fluxes from subsoils ranged from 3 to 14 mg C m−2 h−1. No systematic influence of peat type or sand addition on GHG emissions was found in topsoils, but CO2 fluxes from subsoils below peat-sand mixtures were higher than from subsoils below earthified peat. Maximum N2O fluxes were highly variable between sites and ranged from 18.5 to 234.9 and from 0.2 to 22.9 μg N m−2 h−1 for topsoils and subsoils, respectively. CH4 fluxes were negligible even under water-saturated conditions. The highest GHG emissions occurred at a WFPS that relates – under equilibrium conditions – to a water table of 20–60 cm below the surface in the field. High maximum CO2 and N2O fluxes were linked to high densities of plant-available phosphorus and potassium. The results of this study highlight that nutrient status plays a more important role in GHG emissions than peat type or sand addition, and do not support the idea of peat-sand mixtures as a mitigation option for GHG emissions.
AB - Drainage turns peatlands from natural carbon sinks into hotspots of greenhouse gas (GHG)emissions from soils due to alterations in hydrological and biogeochemical processes. As a consequence of drainage-induced mineralisation and anthropogenic sand addition, large areas of former peatlands under agricultural use have soil organic carbon (SOC)contents at the boundary between mineral and organic soils. Previous research has shown that the variability of GHG emissions increases with anthropogenic disturbance. However, how and whether sand addition affects GHG emissions remains a controversial issue. The aim of this long-term incubation experiment was to assess the influence of hydrological and biogeochemical soil properties on emissions of carbon dioxide (CO2), nitrous oxide (N2O)and methane (CH4). Strongly degraded peat with sand addition (peat-sand mixtures)and without sand addition (earthified peat)was systematically compared under different moisture conditions for fen and bog peat. Soil columns originating from both the topsoil and the subsoil of ten different peatlands under grassland use were investigated. Over a period of six months the almost saturated soil columns were drained stepwise via suction to −300 hPa. The CO2 fluxes were lowest at water-saturated and dry soil moisture conditions, resulting in a parabolic dependence of CO2 fluxes on the water-filled pore space (WFPS)peaking at 56–92% WFPS. The highest N2O fluxes were found at between 73 and 95% WFPS. Maximum CO2 fluxes were highest from topsoils, ranging from 21 to 77 mg C m−2 h−1, while the maximum CO2 fluxes from subsoils ranged from 3 to 14 mg C m−2 h−1. No systematic influence of peat type or sand addition on GHG emissions was found in topsoils, but CO2 fluxes from subsoils below peat-sand mixtures were higher than from subsoils below earthified peat. Maximum N2O fluxes were highly variable between sites and ranged from 18.5 to 234.9 and from 0.2 to 22.9 μg N m−2 h−1 for topsoils and subsoils, respectively. CH4 fluxes were negligible even under water-saturated conditions. The highest GHG emissions occurred at a WFPS that relates – under equilibrium conditions – to a water table of 20–60 cm below the surface in the field. High maximum CO2 and N2O fluxes were linked to high densities of plant-available phosphorus and potassium. The results of this study highlight that nutrient status plays a more important role in GHG emissions than peat type or sand addition, and do not support the idea of peat-sand mixtures as a mitigation option for GHG emissions.
KW - Carbon dioxide
KW - Microcosm incubation
KW - Mitigation measures
KW - Nitrous oxide
KW - Peat-sand mixture
KW - Peatland agriculture
UR - http://www.scopus.com/inward/record.url?scp=85064838451&partnerID=8YFLogxK
U2 - 10.1016/j.soilbio.2019.04.013
DO - 10.1016/j.soilbio.2019.04.013
M3 - Article
AN - SCOPUS:85064838451
VL - 135
SP - 71
EP - 84
JO - Soil Biology and Biochemistry
JF - Soil Biology and Biochemistry
SN - 0038-0717
ER -