Relative Humidity Controls Ammonia Loss from Urea Applied to Loblolly Pine
In the United States, approximately 600,000 ha of pine trees are fertilized with urea each year, with NH3 volatilization losses ranging from 50% depending on environmental conditions. Previous work showed that the timing of rainfall after urea application plays a significant role in controlling NH3...
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description | In the United States, approximately 600,000 ha of pine trees are fertilized with urea each year, with NH3 volatilization losses ranging from 50% depending on environmental conditions. Previous work showed that the timing of rainfall after urea application plays a significant role in controlling NH3 loss, but the effect of other environmental variables is not well understood. We conducted 10 29-d studies under different environmental conditions during 2 yr to identify important variables controlling NH3 loss from urea applied to loblolly pine (Pinus taeda L.) at 200 kg N ha–1. Ammonia loss was measured with dynamic chambers that adjusted the rate of air flow through the system based on wind speed at 1 cm above the soil surface. Regression analysis indicated that a variable related to the initial water content of the forest floor and a variable related to the relative humidity (RH) during the study explained 85 to 94% of the observed variability in NH3 loss. Relatively high initial water content followed by consistently high RH led to large NH3 losses. In contrast, low initial water contents resulted in slow rates of NH3 loss, which increased when elevated RH led to an increase in the water content of the forest floor. These results indicate that RH can play a significant role in NH3 loss by accelerating urea dissolution and by increasing or decreasing the water content of the forest floor, which in turn can affect the rate of urea hydrolysis. |
doi_str_mv | 10.2136/sssaj2009.0220 |
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(PNNL), Richland, WA (United States)</creatorcontrib><description>In the United States, approximately 600,000 ha of pine trees are fertilized with urea each year, with NH3 volatilization losses ranging from <1% to >50% depending on environmental conditions. Previous work showed that the timing of rainfall after urea application plays a significant role in controlling NH3 loss, but the effect of other environmental variables is not well understood. We conducted 10 29-d studies under different environmental conditions during 2 yr to identify important variables controlling NH3 loss from urea applied to loblolly pine (Pinus taeda L.) at 200 kg N ha–1. Ammonia loss was measured with dynamic chambers that adjusted the rate of air flow through the system based on wind speed at 1 cm above the soil surface. Regression analysis indicated that a variable related to the initial water content of the forest floor and a variable related to the relative humidity (RH) during the study explained 85 to 94% of the observed variability in NH3 loss. Relatively high initial water content followed by consistently high RH led to large NH3 losses. In contrast, low initial water contents resulted in slow rates of NH3 loss, which increased when elevated RH led to an increase in the water content of the forest floor. These results indicate that RH can play a significant role in NH3 loss by accelerating urea dissolution and by increasing or decreasing the water content of the forest floor, which in turn can affect the rate of urea hydrolysis.</description><identifier>ISSN: 0361-5995</identifier><identifier>EISSN: 1435-0661</identifier><identifier>DOI: 10.2136/sssaj2009.0220</identifier><identifier>CODEN: SSSJD4</identifier><language>eng</language><publisher>Madison: Soil Science Society</publisher><subject>Agronomy. Soil science and plant productions ; AIR FLOW ; AMMONIA ; AUGMENTATION ; BASIC BIOLOGICAL SCIENCES ; Biological and medical sciences ; DISSOLUTION ; DYNAMICS ; Earth sciences ; Earth, ocean, space ; Environmental conditions ; environmental factors ; ENVIRONMENTAL SCIENCES ; EVAPORATION ; Evergreen trees ; Exact sciences and technology ; FLOORS ; Forest floor ; forest soils ; forest trees ; FORESTS ; Fundamental and applied biological sciences. Psychology ; GENERAL AND MISCELLANEOUS//MATHEMATICS, COMPUTING, AND INFORMATION SCIENCE ; HUMIDITY ; HUMIDITY CONTROL ; HYDROLYSIS ; LOSSES ; losses from soil ; nitrogen fertilizers ; Pine trees ; PINES ; Pinus taeda ; REGRESSION ANALYSIS ; Relative humidity ; Soil science ; Soil surfaces ; soil water content ; SOILS ; Surficial geology ; temperate forests ; Trees ; UREA ; VELOCITY ; volatilization ; Water content ; WELLS ; WIND ; Wind speed ; WORK</subject><ispartof>Soil Science Society of America journal, 2010-03, Vol.74 (2), p.543-549</ispartof><rights>Soil Science Society of America</rights><rights>2015 INIST-CNRS</rights><rights>Copyright American Society of Agronomy Mar/Apr 2010</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4970-6761aecc0005cb8487a4ee77542546733b68678a579ce68f0c5b81420be822e3</citedby><cites>FETCH-LOGICAL-c4970-6761aecc0005cb8487a4ee77542546733b68678a579ce68f0c5b81420be822e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.2136%2Fsssaj2009.0220$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.2136%2Fsssaj2009.0220$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=22487402$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/981996$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Cabrera, M.L</creatorcontrib><creatorcontrib>Kissel, D.E</creatorcontrib><creatorcontrib>Craig, J.R</creatorcontrib><creatorcontrib>Qafoku, N.P</creatorcontrib><creatorcontrib>Vaio, N</creatorcontrib><creatorcontrib>Rema, J.A</creatorcontrib><creatorcontrib>Morris, L.A</creatorcontrib><creatorcontrib>Pacific Northwest National Lab. (PNNL), Richland, WA (United States)</creatorcontrib><title>Relative Humidity Controls Ammonia Loss from Urea Applied to Loblolly Pine</title><title>Soil Science Society of America journal</title><description>In the United States, approximately 600,000 ha of pine trees are fertilized with urea each year, with NH3 volatilization losses ranging from <1% to >50% depending on environmental conditions. Previous work showed that the timing of rainfall after urea application plays a significant role in controlling NH3 loss, but the effect of other environmental variables is not well understood. We conducted 10 29-d studies under different environmental conditions during 2 yr to identify important variables controlling NH3 loss from urea applied to loblolly pine (Pinus taeda L.) at 200 kg N ha–1. Ammonia loss was measured with dynamic chambers that adjusted the rate of air flow through the system based on wind speed at 1 cm above the soil surface. Regression analysis indicated that a variable related to the initial water content of the forest floor and a variable related to the relative humidity (RH) during the study explained 85 to 94% of the observed variability in NH3 loss. Relatively high initial water content followed by consistently high RH led to large NH3 losses. In contrast, low initial water contents resulted in slow rates of NH3 loss, which increased when elevated RH led to an increase in the water content of the forest floor. These results indicate that RH can play a significant role in NH3 loss by accelerating urea dissolution and by increasing or decreasing the water content of the forest floor, which in turn can affect the rate of urea hydrolysis.</description><subject>Agronomy. Soil science and plant productions</subject><subject>AIR FLOW</subject><subject>AMMONIA</subject><subject>AUGMENTATION</subject><subject>BASIC BIOLOGICAL SCIENCES</subject><subject>Biological and medical sciences</subject><subject>DISSOLUTION</subject><subject>DYNAMICS</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Environmental conditions</subject><subject>environmental factors</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>EVAPORATION</subject><subject>Evergreen trees</subject><subject>Exact sciences and technology</subject><subject>FLOORS</subject><subject>Forest floor</subject><subject>forest soils</subject><subject>forest trees</subject><subject>FORESTS</subject><subject>Fundamental and applied biological sciences. 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(PNNL), Richland, WA (United States)</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relative Humidity Controls Ammonia Loss from Urea Applied to Loblolly Pine</atitle><jtitle>Soil Science Society of America journal</jtitle><date>2010-03</date><risdate>2010</risdate><volume>74</volume><issue>2</issue><spage>543</spage><epage>549</epage><pages>543-549</pages><issn>0361-5995</issn><eissn>1435-0661</eissn><coden>SSSJD4</coden><abstract>In the United States, approximately 600,000 ha of pine trees are fertilized with urea each year, with NH3 volatilization losses ranging from <1% to >50% depending on environmental conditions. Previous work showed that the timing of rainfall after urea application plays a significant role in controlling NH3 loss, but the effect of other environmental variables is not well understood. We conducted 10 29-d studies under different environmental conditions during 2 yr to identify important variables controlling NH3 loss from urea applied to loblolly pine (Pinus taeda L.) at 200 kg N ha–1. Ammonia loss was measured with dynamic chambers that adjusted the rate of air flow through the system based on wind speed at 1 cm above the soil surface. Regression analysis indicated that a variable related to the initial water content of the forest floor and a variable related to the relative humidity (RH) during the study explained 85 to 94% of the observed variability in NH3 loss. Relatively high initial water content followed by consistently high RH led to large NH3 losses. In contrast, low initial water contents resulted in slow rates of NH3 loss, which increased when elevated RH led to an increase in the water content of the forest floor. These results indicate that RH can play a significant role in NH3 loss by accelerating urea dissolution and by increasing or decreasing the water content of the forest floor, which in turn can affect the rate of urea hydrolysis.</abstract><cop>Madison</cop><pub>Soil Science Society</pub><doi>10.2136/sssaj2009.0220</doi><tpages>7</tpages></addata></record> |
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subjects | Agronomy. Soil science and plant productions AIR FLOW AMMONIA AUGMENTATION BASIC BIOLOGICAL SCIENCES Biological and medical sciences DISSOLUTION DYNAMICS Earth sciences Earth, ocean, space Environmental conditions environmental factors ENVIRONMENTAL SCIENCES EVAPORATION Evergreen trees Exact sciences and technology FLOORS Forest floor forest soils forest trees FORESTS Fundamental and applied biological sciences. Psychology GENERAL AND MISCELLANEOUS//MATHEMATICS, COMPUTING, AND INFORMATION SCIENCE HUMIDITY HUMIDITY CONTROL HYDROLYSIS LOSSES losses from soil nitrogen fertilizers Pine trees PINES Pinus taeda REGRESSION ANALYSIS Relative humidity Soil science Soil surfaces soil water content SOILS Surficial geology temperate forests Trees UREA VELOCITY volatilization Water content WELLS WIND Wind speed WORK |
title | Relative Humidity Controls Ammonia Loss from Urea Applied to Loblolly Pine |
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