Plant-mediated methane and nitrous oxide fluxes from a carex meadow in Poyang Lake during drawdown periods
AIMS: Plants have been suggested to have significant effects on methane (CH₄) and nitrous oxide (N₂O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. METHODS: We conducted in situ measurement of CH₄ and N₂O fluxes for two years. To distinguish between the effects of shoot...
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Published in | Plant and soil Vol. 400; no. 1-2; pp. 367 - 380 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
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Springer International Publishing
01.03.2016
Springer Springer Nature B.V |
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Abstract | AIMS: Plants have been suggested to have significant effects on methane (CH₄) and nitrous oxide (N₂O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. METHODS: We conducted in situ measurement of CH₄ and N₂O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH₄ and N₂O fluxes were analyzed. RESULTS: The mean ecosystem CH₄ emission rate was 36 μg CH₄ m⁻² h⁻¹ for drying periods, but 8219 μg CH₄ m⁻² h⁻¹ for drying-wetting transition periods. CH₄ fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH₄ flux rate, but root exclusion decreased the CH₄ flux by 116 % as compared to the control. N₂O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 μg N₂O m⁻² h⁻¹. Both clipping and root exclusion significantly increased N₂O fluxes as compared to the control. CONCLUSIONS: There was no significant correlation between CH₄ and N₂O fluxes. Roots dominated plant-mediated enhancement in CH₄ fluxes, but played almost an equal role as shoots in plant-regulated suppression on N₂O fluxes in this Carex meadow during drawdown periods. |
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AbstractList | Aims
Plants have been suggested to have significant effects on methane (CH
4
) and nitrous oxide (N
2
O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes.
Methods
We conducted
in situ
measurement of CH
4
and N
2
O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH
4
and N
2
O fluxes were analyzed.
Results
The mean ecosystem CH
4
emission rate was 36 μg CH
4
m
−2
h
−1
for drying periods, but 8219 μg CH
4
m
−2
h
−1
for drying-wetting transition periods. CH
4
fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH
4
flux rate, but root exclusion decreased the CH
4
flux by 116 % as compared to the control. N
2
O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 μg N
2
O m
−2
h
−1
. Both clipping and root exclusion significantly increased N
2
O fluxes as compared to the control.
Conclusions
There was no significant correlation between CH
4
and N
2
O fluxes. Roots dominated plant-mediated enhancement in CH
4
fluxes, but played almost an equal role as shoots in plant-regulated suppression on N
2
O fluxes in this
Carex
meadow during drawdown periods. AIMS: Plants have been suggested to have significant effects on methane (CH₄) and nitrous oxide (N₂O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. METHODS: We conducted in situ measurement of CH₄ and N₂O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH₄ and N₂O fluxes were analyzed. RESULTS: The mean ecosystem CH₄ emission rate was 36 μg CH₄ m⁻² h⁻¹ for drying periods, but 8219 μg CH₄ m⁻² h⁻¹ for drying-wetting transition periods. CH₄ fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH₄ flux rate, but root exclusion decreased the CH₄ flux by 116 % as compared to the control. N₂O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 μg N₂O m⁻² h⁻¹. Both clipping and root exclusion significantly increased N₂O fluxes as compared to the control. CONCLUSIONS: There was no significant correlation between CH₄ and N₂O fluxes. Roots dominated plant-mediated enhancement in CH₄ fluxes, but played almost an equal role as shoots in plant-regulated suppression on N₂O fluxes in this Carex meadow during drawdown periods. Plants have been suggested to have significant effects on methane (CH.sub.4) and nitrous oxide (N.sub.2O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. We conducted in situ measurement of CH.sub.4 and N.sub.2O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH.sub.4 and N.sub.2O fluxes were analyzed. The mean ecosystem CH.sub.4 emission rate was 36 [mu]g CH.sub.4 m.sup.-2 h.sup.-1 for drying periods, but 8219 [mu]g CH.sub.4 m.sup.-2 h.sup.-1 for drying-wetting transition periods. CH.sub.4 fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH.sub.4 flux rate, but root exclusion decreased the CH.sub.4 flux by 116 % as compared to the control. N.sub.2O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 [mu]g N.sub.2O m.sup.-2 h.sup.-1. Both clipping and root exclusion significantly increased N.sub.2O fluxes as compared to the control. There was no significant correlation between CH.sub.4 and N.sub.2O fluxes. Roots dominated plant-mediated enhancement in CH.sub.4 fluxes, but played almost an equal role as shoots in plant-regulated suppression on N.sub.2O fluxes in this Carex meadow during drawdown periods. Aims Plants have been suggested to have significant effects on methane (CH.sub.4) and nitrous oxide (N.sub.2O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. Methods We conducted in situ measurement of CH.sub.4 and N.sub.2O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH.sub.4 and N.sub.2O fluxes were analyzed. Results The mean ecosystem CH.sub.4 emission rate was 36 [mu]g CH.sub.4 m.sup.-2 h.sup.-1 for drying periods, but 8219 [mu]g CH.sub.4 m.sup.-2 h.sup.-1 for drying-wetting transition periods. CH.sub.4 fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH.sub.4 flux rate, but root exclusion decreased the CH.sub.4 flux by 116 % as compared to the control. N.sub.2O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 [mu]g N.sub.2O m.sup.-2 h.sup.-1. Both clipping and root exclusion significantly increased N.sub.2O fluxes as compared to the control. Conclusions There was no significant correlation between CH.sub.4 and N.sub.2O fluxes. Roots dominated plant-mediated enhancement in CH.sub.4 fluxes, but played almost an equal role as shoots in plant-regulated suppression on N.sub.2O fluxes in this Carex meadow during drawdown periods. Plants have been suggested to have significant effects on methane (CH sub(4)) and nitrous oxide (N sub(2)O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. We conducted in situ measurement of CH sub(4) and N sub(2)O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH sub(4) and N sub(2)O fluxes were analyzed. The mean ecosystem CH sub(4) emission rate was 36 mu g CH sub(4) m super(-2) h super(- 1) for drying periods, but 8219 mu g CH sub(4) m super(-2) h super(- 1) for drying-wetting transition periods. CH sub(4) fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH sub(4) flux rate, but root exclusion decreased the CH sub(4) flux by 116 % as compared to the control. N sub(2)O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 mu g N sub(2)O m super(-2) h super(- 1). Both clipping and root exclusion significantly increased N sub(2)O fluxes as compared to the control. There was no significant correlation between CH sub(4) and N sub(2)O fluxes. Roots dominated plant-mediated enhancement in CH sub(4) fluxes, but played almost an equal role as shoots in plant-regulated suppression on N sub(2)O fluxes in this Carex meadow during drawdown periods. Aims Plants have been suggested to have significant effects on methane (CH4) and nitrous oxide (N2O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. Methods We conducted in situ measurement of CH4 and N2O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH4 and N2O fluxes were analyzed. Results The mean ecosystem CH4 emission rate was 36 [mu]g CH4 m^sup -2^ h^sup -1^ for drying periods, but 8219 [mu]g CH4 m^sup -2^ h^sup -1^ for drying-wetting transition periods. CH4 fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter CH4 flux rate, but root exclusion decreased the CH4 flux by 116 % as compared to the control. N2O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 [mu]g N2O m^sup -2^ h^sup -1^. Both clipping and root exclusion significantly increased N2O fluxes as compared to the control. Conclusions There was no significant correlation between CH4 and N2O fluxes. Roots dominated plant-mediated enhancement in CH4 fluxes, but played almost an equal role as shoots in plant-regulated suppression on N2O fluxes in this Carex meadow during drawdown periods. Aims Plants have been suggested to have significant effects on methane (CH₄) and nitrous oxide (N₂O) fluxes from littoral wetlands, but it remains unclear in subtropical lakes. Methods We conducted in situ measurement of CH₄ and N₂O fluxes for two years. To distinguish between the effects of shoots and roots, three treatments (i.e., intact plants as control, shoot clipping, and root exclusion) were used. Effects of plant biomass, temperature, and soil moisture on CH₄ and N₂O fluxes were analyzed. Results The mean ecosystem CH₄ emission rate was 36 µg CH₄ m⁻² h⁻¹ for drying periods, but 8219 µg CH₄ m⁻² h⁻¹ for drying-wetting transition periods. CH₄ fluxes were positively correlated with below-ground and total biomass, but not with above-ground biomass. Clipping did not significantly alter flux rate, but root exclusion decreased the CH₄ flux by 116 % as compared to the control. N₂O emissions were similar for both the drying and drying-wetting transition periods, with a mean rate of 20 µg N₂O m⁻² h⁻¹. Both clipping and root exclusion significantly increased N₂O fluxes as compared to the control. Conclusions There was no significant correlation between CH₄ and N₂O fluxes. Roots dominated plantmediated enhancement in CH₄ fluxes, but played almost an equal role as shoots in plant-regulated suppression on N₂O fluxes in this Carex meadow during drawdown periods. |
Audience | Academic |
Author | Yao, Bo Hu, Qiwu Cai, Jiayan Wu, Qin Wang, Yeqiao Xu, Xingliang |
Author_xml | – sequence: 1 fullname: Hu, Qiwu – sequence: 2 fullname: Cai, Jiayan – sequence: 3 fullname: Yao, Bo – sequence: 4 fullname: Wu, Qin – sequence: 5 fullname: Wang, Yeqiao – sequence: 6 fullname: Xu, Xingliang |
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Snippet | AIMS: Plants have been suggested to have significant effects on methane (CH₄) and nitrous oxide (N₂O) fluxes from littoral wetlands, but it remains unclear in... Aims Plants have been suggested to have significant effects on methane (CH₄) and nitrous oxide (N₂O) fluxes from littoral wetlands, but it remains unclear in... Aims Plants have been suggested to have significant effects on methane (CH 4 ) and nitrous oxide (N 2 O) fluxes from littoral wetlands, but it remains unclear... Aims Plants have been suggested to have significant effects on methane (CH.sub.4) and nitrous oxide (N.sub.2O) fluxes from littoral wetlands, but it remains... Plants have been suggested to have significant effects on methane (CH.sub.4) and nitrous oxide (N.sub.2O) fluxes from littoral wetlands, but it remains unclear... Aims Plants have been suggested to have significant effects on methane (CH4) and nitrous oxide (N2O) fluxes from littoral wetlands, but it remains unclear in... Plants have been suggested to have significant effects on methane (CH sub(4)) and nitrous oxide (N sub(2)O) fluxes from littoral wetlands, but it remains... |
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SubjectTerms | aboveground biomass Biomass Biomedical and Life Sciences Carbon dioxide emissions Carex Drawdown Drying Ecology ecosystems Emissions Environmental aspects Grassland soils greenhouse gas emissions Greenhouse gases In situ measurement Lakes Lentic systems Life Sciences littoral zone Littoral zones Meadows Methane Nitrous oxide Plant biomass Plant Physiology Plant roots Plant Sciences Regular Article Roots Shoots Soil moisture Soil Science & Conservation soil water temperature Wetland soils Wetlands |
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Title | Plant-mediated methane and nitrous oxide fluxes from a carex meadow in Poyang Lake during drawdown periods |
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