Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes

Y. A. Teh*, T. Diem, S. Jones, L. P. Huaraca Quispe, E. Baggs, N. Morley, M. Richards, P. Smith, P. Meir

*Corresponding author for this work

Research output: Contribution to journalArticle

18 Citations (Scopus)
3 Downloads (Pure)

Abstract

Remote sensing and inverse modelling studies indicate that the tropics emit more CH4 and N2O than predicted by bottom-up emissions inventories, suggesting that terrestrial sources are stronger or more numerous than previously thought. Tropical uplands are a potentially large and important source of CH4 and N2O often overlooked by past empirical and modelling studies. To address this knowledge gap, we investigated spatial, temporal and environmental trends in soil CH4 and N2O fluxes across a long elevation gradient (600-3700 ma.s.l.) in the Kosnipata Valley, in the southern Peruvian Andes, that experiences seasonal fluctuations in rainfall. The aim of this work was to produce preliminary estimates of soil CH4 and N2O fluxes from representative habitats within this region, and to identify the proximate controls on soil CH4 and N2O dynamics. Area-weighted flux calculations indicated that ecosystems across this altitudinal gradient were both atmospheric sources and sinks of CH4 on an annual basis. Montane grasslands (3200-3700 ma.s.l.) were strong atmospheric sources, emitting 56.94 +/- 7.81 kg CH4-C ha(-1) yr(-1). Upper montane forest (2200-3200 ma.s.l.) and lower montane forest (1200-2200 ma.s.l.) were net atmospheric sinks (-2.99 +/- 0.29 and -2.34 +/- 0.29 kg CH4-C ha(-1) yr(-1), respectively); while premontane forests (600-1200 ma.s.l.) fluctuated between source or sink depending on the season (wet season: 1.86 +/- 1.50 kg CH4-C ha(-1) yr(-1); dry season: -1.17 +/- 0.40 kg CH4-C ha(-1) yr(-1)). Analysis of spatial, temporal and environmental trends in soil CH4 flux across the study site suggest that soil redox was a dominant control on net soil CH4 flux. Soil CH4 emissions were greatest from habitats, landforms and during times of year when soils were suboxic, and soil CH4 efflux was inversely correlated with soil O-2 concentration (Spearman's rho = -0.45, P <0.0001) and positively correlated with water-filled pore space (Spearman's rho = 0.63, P <0.0001). Ecosystems across the region were net atmospheric N2O sources. Soil N2O fluxes declined with increasing elevation; area-weighted flux calculations indicated that N2O emissions from premontane forest, lower montane forest, upper montane forest and montane grasslands averaged 2.23 +/- 1.31, 1.68 +/- 0.44, 0.44 +/- 0.47 and 0.15 +/- 1.10 kg N2O-N ha(-1) yr(-1), respectively. Soil N2O fluxes from premontane and lower montane forests exceeded prior model predictions for the region. Comprehensive investigation of field and laboratory data collected in this study suggest that soil N2O fluxes from this region were primarily driven by denitrification; that nitrate (NO3-) availability was the principal constraint on soil N2O fluxes; and that soil moisture and water-filled porosity played a secondary role in modulating N2O emissions. Any current and future changes in N management or anthropogenic N deposition may cause shifts in net soil N2O fluxes from these tropical montane ecosystems, further enhancing this emission source.

Original languageEnglish
Pages (from-to)2325-2339
Number of pages15
JournalBiogeosciences
Volume11
Issue number8
DOIs
Publication statusPublished - 25 Apr 2014

Keywords

  • forest soils
  • biogeochemical controls
  • atmospheric methane
  • Eastern Amazonia
  • nitric-oxide
  • Costa-Rica
  • land-use
  • emissions
  • N2O
  • carbon

Cite this

Teh, Y. A., Diem, T., Jones, S., Huaraca Quispe, L. P., Baggs, E., Morley, N., ... Meir, P. (2014). Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes. Biogeosciences, 11(8), 2325-2339. https://doi.org/10.5194/bg-11-2325-2014

Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes. / Teh, Y. A.; Diem, T.; Jones, S.; Huaraca Quispe, L. P.; Baggs, E.; Morley, N.; Richards, M.; Smith, P.; Meir, P.

In: Biogeosciences, Vol. 11, No. 8, 25.04.2014, p. 2325-2339.

Research output: Contribution to journalArticle

Teh, YA, Diem, T, Jones, S, Huaraca Quispe, LP, Baggs, E, Morley, N, Richards, M, Smith, P & Meir, P 2014, 'Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes', Biogeosciences, vol. 11, no. 8, pp. 2325-2339. https://doi.org/10.5194/bg-11-2325-2014
Teh YA, Diem T, Jones S, Huaraca Quispe LP, Baggs E, Morley N et al. Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes. Biogeosciences. 2014 Apr 25;11(8):2325-2339. https://doi.org/10.5194/bg-11-2325-2014
Teh, Y. A. ; Diem, T. ; Jones, S. ; Huaraca Quispe, L. P. ; Baggs, E. ; Morley, N. ; Richards, M. ; Smith, P. ; Meir, P. / Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes. In: Biogeosciences. 2014 ; Vol. 11, No. 8. pp. 2325-2339.
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title = "Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes",
abstract = "Remote sensing and inverse modelling studies indicate that the tropics emit more CH4 and N2O than predicted by bottom-up emissions inventories, suggesting that terrestrial sources are stronger or more numerous than previously thought. Tropical uplands are a potentially large and important source of CH4 and N2O often overlooked by past empirical and modelling studies. To address this knowledge gap, we investigated spatial, temporal and environmental trends in soil CH4 and N2O fluxes across a long elevation gradient (600-3700 ma.s.l.) in the Kosnipata Valley, in the southern Peruvian Andes, that experiences seasonal fluctuations in rainfall. The aim of this work was to produce preliminary estimates of soil CH4 and N2O fluxes from representative habitats within this region, and to identify the proximate controls on soil CH4 and N2O dynamics. Area-weighted flux calculations indicated that ecosystems across this altitudinal gradient were both atmospheric sources and sinks of CH4 on an annual basis. Montane grasslands (3200-3700 ma.s.l.) were strong atmospheric sources, emitting 56.94 +/- 7.81 kg CH4-C ha(-1) yr(-1). Upper montane forest (2200-3200 ma.s.l.) and lower montane forest (1200-2200 ma.s.l.) were net atmospheric sinks (-2.99 +/- 0.29 and -2.34 +/- 0.29 kg CH4-C ha(-1) yr(-1), respectively); while premontane forests (600-1200 ma.s.l.) fluctuated between source or sink depending on the season (wet season: 1.86 +/- 1.50 kg CH4-C ha(-1) yr(-1); dry season: -1.17 +/- 0.40 kg CH4-C ha(-1) yr(-1)). Analysis of spatial, temporal and environmental trends in soil CH4 flux across the study site suggest that soil redox was a dominant control on net soil CH4 flux. Soil CH4 emissions were greatest from habitats, landforms and during times of year when soils were suboxic, and soil CH4 efflux was inversely correlated with soil O-2 concentration (Spearman's rho = -0.45, P <0.0001) and positively correlated with water-filled pore space (Spearman's rho = 0.63, P <0.0001). Ecosystems across the region were net atmospheric N2O sources. Soil N2O fluxes declined with increasing elevation; area-weighted flux calculations indicated that N2O emissions from premontane forest, lower montane forest, upper montane forest and montane grasslands averaged 2.23 +/- 1.31, 1.68 +/- 0.44, 0.44 +/- 0.47 and 0.15 +/- 1.10 kg N2O-N ha(-1) yr(-1), respectively. Soil N2O fluxes from premontane and lower montane forests exceeded prior model predictions for the region. Comprehensive investigation of field and laboratory data collected in this study suggest that soil N2O fluxes from this region were primarily driven by denitrification; that nitrate (NO3-) availability was the principal constraint on soil N2O fluxes; and that soil moisture and water-filled porosity played a secondary role in modulating N2O emissions. Any current and future changes in N management or anthropogenic N deposition may cause shifts in net soil N2O fluxes from these tropical montane ecosystems, further enhancing this emission source.",
keywords = "forest soils, biogeochemical controls, atmospheric methane, Eastern Amazonia, nitric-oxide, Costa-Rica, land-use, emissions, N2O, carbon",
author = "Teh, {Y. A.} and T. Diem and S. Jones and {Huaraca Quispe}, {L. P.} and E. Baggs and N. Morley and M. Richards and P. Smith and P. Meir",
note = "The authors would like to acknowledge the agencies that funded this research; the UK Natural Environment Research Council (NERC; joint grant references NE/H006583, NE/H007849 and NE/H006753) and the Norwegian Agency for Development Cooperation (Norad; via a sub-contract to Yit Arn Teh managed by the Amazon Conservation Association). Pete Smith is a Royal Society Wolfson Research Merit Award holder and Patrick Meir is supported by an Australian Research Council Fellowship (FT110100457). Javier Eduardo Silva Espejo, Walter Huaraca Huasco, Adan Julian Ccahuana and the ABIDA NGO provided critical fieldwork and logistical support. Angus Calder and Vicky Munro provided invaluable laboratory support. Viktoria Oliver provided data on soil characteristics for Hacienda Villa Carmen. Thanks to Adrian Tejedor from the Amazon Conservation Association, who provided assistance with site access and selection at Hacienda Villa Carmen. Thanks are also owed to TCH for providing comments on an earlier draft of this manuscript. This publication is a contribution from the Scottish Alliance for Geoscience, Environment and Society (http://www.sages.ac.uk)",
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TY - JOUR

T1 - Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes

AU - Teh, Y. A.

AU - Diem, T.

AU - Jones, S.

AU - Huaraca Quispe, L. P.

AU - Baggs, E.

AU - Morley, N.

AU - Richards, M.

AU - Smith, P.

AU - Meir, P.

N1 - The authors would like to acknowledge the agencies that funded this research; the UK Natural Environment Research Council (NERC; joint grant references NE/H006583, NE/H007849 and NE/H006753) and the Norwegian Agency for Development Cooperation (Norad; via a sub-contract to Yit Arn Teh managed by the Amazon Conservation Association). Pete Smith is a Royal Society Wolfson Research Merit Award holder and Patrick Meir is supported by an Australian Research Council Fellowship (FT110100457). Javier Eduardo Silva Espejo, Walter Huaraca Huasco, Adan Julian Ccahuana and the ABIDA NGO provided critical fieldwork and logistical support. Angus Calder and Vicky Munro provided invaluable laboratory support. Viktoria Oliver provided data on soil characteristics for Hacienda Villa Carmen. Thanks to Adrian Tejedor from the Amazon Conservation Association, who provided assistance with site access and selection at Hacienda Villa Carmen. Thanks are also owed to TCH for providing comments on an earlier draft of this manuscript. This publication is a contribution from the Scottish Alliance for Geoscience, Environment and Society (http://www.sages.ac.uk)

PY - 2014/4/25

Y1 - 2014/4/25

N2 - Remote sensing and inverse modelling studies indicate that the tropics emit more CH4 and N2O than predicted by bottom-up emissions inventories, suggesting that terrestrial sources are stronger or more numerous than previously thought. Tropical uplands are a potentially large and important source of CH4 and N2O often overlooked by past empirical and modelling studies. To address this knowledge gap, we investigated spatial, temporal and environmental trends in soil CH4 and N2O fluxes across a long elevation gradient (600-3700 ma.s.l.) in the Kosnipata Valley, in the southern Peruvian Andes, that experiences seasonal fluctuations in rainfall. The aim of this work was to produce preliminary estimates of soil CH4 and N2O fluxes from representative habitats within this region, and to identify the proximate controls on soil CH4 and N2O dynamics. Area-weighted flux calculations indicated that ecosystems across this altitudinal gradient were both atmospheric sources and sinks of CH4 on an annual basis. Montane grasslands (3200-3700 ma.s.l.) were strong atmospheric sources, emitting 56.94 +/- 7.81 kg CH4-C ha(-1) yr(-1). Upper montane forest (2200-3200 ma.s.l.) and lower montane forest (1200-2200 ma.s.l.) were net atmospheric sinks (-2.99 +/- 0.29 and -2.34 +/- 0.29 kg CH4-C ha(-1) yr(-1), respectively); while premontane forests (600-1200 ma.s.l.) fluctuated between source or sink depending on the season (wet season: 1.86 +/- 1.50 kg CH4-C ha(-1) yr(-1); dry season: -1.17 +/- 0.40 kg CH4-C ha(-1) yr(-1)). Analysis of spatial, temporal and environmental trends in soil CH4 flux across the study site suggest that soil redox was a dominant control on net soil CH4 flux. Soil CH4 emissions were greatest from habitats, landforms and during times of year when soils were suboxic, and soil CH4 efflux was inversely correlated with soil O-2 concentration (Spearman's rho = -0.45, P <0.0001) and positively correlated with water-filled pore space (Spearman's rho = 0.63, P <0.0001). Ecosystems across the region were net atmospheric N2O sources. Soil N2O fluxes declined with increasing elevation; area-weighted flux calculations indicated that N2O emissions from premontane forest, lower montane forest, upper montane forest and montane grasslands averaged 2.23 +/- 1.31, 1.68 +/- 0.44, 0.44 +/- 0.47 and 0.15 +/- 1.10 kg N2O-N ha(-1) yr(-1), respectively. Soil N2O fluxes from premontane and lower montane forests exceeded prior model predictions for the region. Comprehensive investigation of field and laboratory data collected in this study suggest that soil N2O fluxes from this region were primarily driven by denitrification; that nitrate (NO3-) availability was the principal constraint on soil N2O fluxes; and that soil moisture and water-filled porosity played a secondary role in modulating N2O emissions. Any current and future changes in N management or anthropogenic N deposition may cause shifts in net soil N2O fluxes from these tropical montane ecosystems, further enhancing this emission source.

AB - Remote sensing and inverse modelling studies indicate that the tropics emit more CH4 and N2O than predicted by bottom-up emissions inventories, suggesting that terrestrial sources are stronger or more numerous than previously thought. Tropical uplands are a potentially large and important source of CH4 and N2O often overlooked by past empirical and modelling studies. To address this knowledge gap, we investigated spatial, temporal and environmental trends in soil CH4 and N2O fluxes across a long elevation gradient (600-3700 ma.s.l.) in the Kosnipata Valley, in the southern Peruvian Andes, that experiences seasonal fluctuations in rainfall. The aim of this work was to produce preliminary estimates of soil CH4 and N2O fluxes from representative habitats within this region, and to identify the proximate controls on soil CH4 and N2O dynamics. Area-weighted flux calculations indicated that ecosystems across this altitudinal gradient were both atmospheric sources and sinks of CH4 on an annual basis. Montane grasslands (3200-3700 ma.s.l.) were strong atmospheric sources, emitting 56.94 +/- 7.81 kg CH4-C ha(-1) yr(-1). Upper montane forest (2200-3200 ma.s.l.) and lower montane forest (1200-2200 ma.s.l.) were net atmospheric sinks (-2.99 +/- 0.29 and -2.34 +/- 0.29 kg CH4-C ha(-1) yr(-1), respectively); while premontane forests (600-1200 ma.s.l.) fluctuated between source or sink depending on the season (wet season: 1.86 +/- 1.50 kg CH4-C ha(-1) yr(-1); dry season: -1.17 +/- 0.40 kg CH4-C ha(-1) yr(-1)). Analysis of spatial, temporal and environmental trends in soil CH4 flux across the study site suggest that soil redox was a dominant control on net soil CH4 flux. Soil CH4 emissions were greatest from habitats, landforms and during times of year when soils were suboxic, and soil CH4 efflux was inversely correlated with soil O-2 concentration (Spearman's rho = -0.45, P <0.0001) and positively correlated with water-filled pore space (Spearman's rho = 0.63, P <0.0001). Ecosystems across the region were net atmospheric N2O sources. Soil N2O fluxes declined with increasing elevation; area-weighted flux calculations indicated that N2O emissions from premontane forest, lower montane forest, upper montane forest and montane grasslands averaged 2.23 +/- 1.31, 1.68 +/- 0.44, 0.44 +/- 0.47 and 0.15 +/- 1.10 kg N2O-N ha(-1) yr(-1), respectively. Soil N2O fluxes from premontane and lower montane forests exceeded prior model predictions for the region. Comprehensive investigation of field and laboratory data collected in this study suggest that soil N2O fluxes from this region were primarily driven by denitrification; that nitrate (NO3-) availability was the principal constraint on soil N2O fluxes; and that soil moisture and water-filled porosity played a secondary role in modulating N2O emissions. Any current and future changes in N management or anthropogenic N deposition may cause shifts in net soil N2O fluxes from these tropical montane ecosystems, further enhancing this emission source.

KW - forest soils

KW - biogeochemical controls

KW - atmospheric methane

KW - Eastern Amazonia

KW - nitric-oxide

KW - Costa-Rica

KW - land-use

KW - emissions

KW - N2O

KW - carbon

U2 - 10.5194/bg-11-2325-2014

DO - 10.5194/bg-11-2325-2014

M3 - Article

VL - 11

SP - 2325

EP - 2339

JO - Biogeosciences

JF - Biogeosciences

SN - 1726-4170

IS - 8

ER -