Effects of Changes in Nitrogen Availability on Nitrogen Gas Emissions in a Tropical Forest During a Drought

Atmospheric nitrogen (N) deposition in tropical forests may increase substantially in coming decades, stimulating a concomitant increase of soil N gas emissions. At the same time, climate change may increase the prevalence of drought, altering the processes that produce these gases (dominantly aerob...

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Veröffentlicht in:Journal of geophysical research. Biogeosciences 2019-09, Vol.124 (9), p.2917-2926
Hauptverfasser: Almaraz, Maya, Groffman, Peter M., Porder, Stephen
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creator Almaraz, Maya
Groffman, Peter M.
Porder, Stephen
description Atmospheric nitrogen (N) deposition in tropical forests may increase substantially in coming decades, stimulating a concomitant increase of soil N gas emissions. At the same time, climate change may increase the prevalence of drought, altering the processes that produce these gases (dominantly aerobic nitrification and anaerobic denitrification). This alteration is of particular concern if global changes increase the fraction of N gas released as nitrous oxide (N2O; a greenhouse gas) relative to dinitrogen (N2). To simulate the effects of atmospheric N deposition on the amount and species of soil N gas emissions, we installed fertilized ion exchange resin bags across a hillslope in the Luquillo Experimental Forest of Puerto Rico. Our experiment took place during a severe drought, providing opportunities to consider how N addition and dry soil conditions interact. After 2 months of fertilization, we measured denitrification potential using a denitrification enzyme assay, which utilizes anoxic incubations where N and carbon limitation are relieved and nitrification is inhibited. We also measured N2 and N2O emissions using a Nitrogen Free Air Recirculation Method (NFARM), which quantifies emissions from both nitrification and denitrification. Data from these two methods suggest that N inputs stimulated N2O emissions associated with aerobic nitrification. Our data suggest that soil drying during the drought decreased N2 emissions associated with anaerobic denitrification and changed the spatial patterns of emissions in the landscape. Together these results suggest that, at least during a drought, N inputs increase N2O emissions associated with nitrification, which may represent a positive feedback to climate change. Key Points Nitrogen addition to tropical forest soils during a drought increased nitrogen gas fluxes by 450% Data from two different methods suggest that nitrogen inputs stimulated nitrous oxide emissions associated with aerobic nitrification Valleys were hot spots of nitrogen gas emissions in the landscape, and the only locations with substantial production of dinitrogen
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At the same time, climate change may increase the prevalence of drought, altering the processes that produce these gases (dominantly aerobic nitrification and anaerobic denitrification). This alteration is of particular concern if global changes increase the fraction of N gas released as nitrous oxide (N2O; a greenhouse gas) relative to dinitrogen (N2). To simulate the effects of atmospheric N deposition on the amount and species of soil N gas emissions, we installed fertilized ion exchange resin bags across a hillslope in the Luquillo Experimental Forest of Puerto Rico. Our experiment took place during a severe drought, providing opportunities to consider how N addition and dry soil conditions interact. After 2 months of fertilization, we measured denitrification potential using a denitrification enzyme assay, which utilizes anoxic incubations where N and carbon limitation are relieved and nitrification is inhibited. We also measured N2 and N2O emissions using a Nitrogen Free Air Recirculation Method (NFARM), which quantifies emissions from both nitrification and denitrification. Data from these two methods suggest that N inputs stimulated N2O emissions associated with aerobic nitrification. Our data suggest that soil drying during the drought decreased N2 emissions associated with anaerobic denitrification and changed the spatial patterns of emissions in the landscape. Together these results suggest that, at least during a drought, N inputs increase N2O emissions associated with nitrification, which may represent a positive feedback to climate change. Key Points Nitrogen addition to tropical forest soils during a drought increased nitrogen gas fluxes by 450% Data from two different methods suggest that nitrogen inputs stimulated nitrous oxide emissions associated with aerobic nitrification Valleys were hot spots of nitrogen gas emissions in the landscape, and the only locations with substantial production of dinitrogen</description><identifier>ISSN: 2169-8953</identifier><identifier>EISSN: 2169-8961</identifier><identifier>DOI: 10.1029/2018JG004851</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Air recirculation ; Anaerobic processes ; Anoxia ; Biological fertilization ; Climate change ; Denitrification ; denitrification potential ; Deposition ; Drought ; Drying ; Emission measurements ; Emissions ; Fertilization ; Forests ; Gases ; Greenhouse effect ; Greenhouse gases ; Ion exchange ; Ion exchange resins ; Nitrification ; Nitrogen ; nitrogen deposition ; nitrogen gas emissions ; Nitrous oxide ; Positive feedback ; Soil ; Soil conditions ; Soils ; topography ; Tropical climate ; tropical forest soil ; Tropical forests</subject><ispartof>Journal of geophysical research. 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Biogeosciences</title><description>Atmospheric nitrogen (N) deposition in tropical forests may increase substantially in coming decades, stimulating a concomitant increase of soil N gas emissions. At the same time, climate change may increase the prevalence of drought, altering the processes that produce these gases (dominantly aerobic nitrification and anaerobic denitrification). This alteration is of particular concern if global changes increase the fraction of N gas released as nitrous oxide (N2O; a greenhouse gas) relative to dinitrogen (N2). To simulate the effects of atmospheric N deposition on the amount and species of soil N gas emissions, we installed fertilized ion exchange resin bags across a hillslope in the Luquillo Experimental Forest of Puerto Rico. Our experiment took place during a severe drought, providing opportunities to consider how N addition and dry soil conditions interact. After 2 months of fertilization, we measured denitrification potential using a denitrification enzyme assay, which utilizes anoxic incubations where N and carbon limitation are relieved and nitrification is inhibited. We also measured N2 and N2O emissions using a Nitrogen Free Air Recirculation Method (NFARM), which quantifies emissions from both nitrification and denitrification. Data from these two methods suggest that N inputs stimulated N2O emissions associated with aerobic nitrification. Our data suggest that soil drying during the drought decreased N2 emissions associated with anaerobic denitrification and changed the spatial patterns of emissions in the landscape. Together these results suggest that, at least during a drought, N inputs increase N2O emissions associated with nitrification, which may represent a positive feedback to climate change. Key Points Nitrogen addition to tropical forest soils during a drought increased nitrogen gas fluxes by 450% Data from two different methods suggest that nitrogen inputs stimulated nitrous oxide emissions associated with aerobic nitrification Valleys were hot spots of nitrogen gas emissions in the landscape, and the only locations with substantial production of dinitrogen</description><subject>Air recirculation</subject><subject>Anaerobic processes</subject><subject>Anoxia</subject><subject>Biological fertilization</subject><subject>Climate change</subject><subject>Denitrification</subject><subject>denitrification potential</subject><subject>Deposition</subject><subject>Drought</subject><subject>Drying</subject><subject>Emission measurements</subject><subject>Emissions</subject><subject>Fertilization</subject><subject>Forests</subject><subject>Gases</subject><subject>Greenhouse effect</subject><subject>Greenhouse gases</subject><subject>Ion exchange</subject><subject>Ion exchange resins</subject><subject>Nitrification</subject><subject>Nitrogen</subject><subject>nitrogen deposition</subject><subject>nitrogen gas emissions</subject><subject>Nitrous oxide</subject><subject>Positive feedback</subject><subject>Soil</subject><subject>Soil conditions</subject><subject>Soils</subject><subject>topography</subject><subject>Tropical climate</subject><subject>tropical forest soil</subject><subject>Tropical forests</subject><issn>2169-8953</issn><issn>2169-8961</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9kMtOwzAQRS0EElXpjg-wxJaAX0mcZdVHoKpAQmVtOa6duqRxsRNQ_x5DEeqK2cxo7pmHLgDXGN1hRIp7gjBflAgxnuIzMCA4KxJeZPj8r07pJRiFsEUxeGxhPABvM2O06gJ0Bk42sq11gLaFT7bzrtYtHH9I28jKNrY7QHcilDLA2c6GYF37MyLhyru9VbKBc-d16OC097atozD1rq833RW4MLIJevSbh-B1PltNHpLlc_k4GS8TRVGOE0mMQWstWUFZWjGVI6IMZ3m1xryquMozyXWO6LrgKdUok0ZRLSnHBc0rlTE6BDfHvXvv3vv4idi63rfxpCAU8TRPoyGRuj1SyrsQvDZi7-1O-oPASHw7Kk4djTg94p-20Yd_WbEoX0qCGcf0C7e8dq4</recordid><startdate>201909</startdate><enddate>201909</enddate><creator>Almaraz, Maya</creator><creator>Groffman, Peter M.</creator><creator>Porder, Stephen</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-0556-633X</orcidid><orcidid>https://orcid.org/0000-0001-8371-6255</orcidid></search><sort><creationdate>201909</creationdate><title>Effects of Changes in Nitrogen Availability on Nitrogen Gas Emissions in a Tropical Forest During a Drought</title><author>Almaraz, Maya ; Groffman, Peter M. ; Porder, Stephen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3071-a2ff0dea49345b4c702cf847bd18bb8c76a8e703d9853e06afc3ea381937bc643</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Air recirculation</topic><topic>Anaerobic processes</topic><topic>Anoxia</topic><topic>Biological fertilization</topic><topic>Climate change</topic><topic>Denitrification</topic><topic>denitrification potential</topic><topic>Deposition</topic><topic>Drought</topic><topic>Drying</topic><topic>Emission measurements</topic><topic>Emissions</topic><topic>Fertilization</topic><topic>Forests</topic><topic>Gases</topic><topic>Greenhouse effect</topic><topic>Greenhouse gases</topic><topic>Ion exchange</topic><topic>Ion exchange resins</topic><topic>Nitrification</topic><topic>Nitrogen</topic><topic>nitrogen deposition</topic><topic>nitrogen gas emissions</topic><topic>Nitrous oxide</topic><topic>Positive feedback</topic><topic>Soil</topic><topic>Soil conditions</topic><topic>Soils</topic><topic>topography</topic><topic>Tropical climate</topic><topic>tropical forest soil</topic><topic>Tropical forests</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Almaraz, Maya</creatorcontrib><creatorcontrib>Groffman, Peter M.</creatorcontrib><creatorcontrib>Porder, Stephen</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of geophysical research. 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We also measured N2 and N2O emissions using a Nitrogen Free Air Recirculation Method (NFARM), which quantifies emissions from both nitrification and denitrification. Data from these two methods suggest that N inputs stimulated N2O emissions associated with aerobic nitrification. Our data suggest that soil drying during the drought decreased N2 emissions associated with anaerobic denitrification and changed the spatial patterns of emissions in the landscape. Together these results suggest that, at least during a drought, N inputs increase N2O emissions associated with nitrification, which may represent a positive feedback to climate change. 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subjects Air recirculation
Anaerobic processes
Anoxia
Biological fertilization
Climate change
Denitrification
denitrification potential
Deposition
Drought
Drying
Emission measurements
Emissions
Fertilization
Forests
Gases
Greenhouse effect
Greenhouse gases
Ion exchange
Ion exchange resins
Nitrification
Nitrogen
nitrogen deposition
nitrogen gas emissions
Nitrous oxide
Positive feedback
Soil
Soil conditions
Soils
topography
Tropical climate
tropical forest soil
Tropical forests
title Effects of Changes in Nitrogen Availability on Nitrogen Gas Emissions in a Tropical Forest During a Drought
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