Influence of soil bulk density and matric potential on microbial dynamics, inorganic N transformations, N2O and N2 fluxes following urea deposition

Transformation of ruminant urine-nitrogen (N) can contribute to negative environmental outcomes such as nitrate leaching which leads to eutrophication of waterways and production of nitrous oxide (N2O), a greenhouse gas. Although abiotic factors influencing urine-N processing have been well studied,...

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Veröffentlicht in:Soil biology & biochemistry 2013-10, Vol.65, p.1-11
Hauptverfasser: Hamonts, Kelly, Balaine, Nimlesh, Moltchanova, Elena, Beare, Mike, Thomas, Steve, Wakelin, Steven A., O'Callaghan, Maureen, Condron, Leo M., Clough, Tim J.
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container_title Soil biology & biochemistry
container_volume 65
creator Hamonts, Kelly
Balaine, Nimlesh
Moltchanova, Elena
Beare, Mike
Thomas, Steve
Wakelin, Steven A.
O'Callaghan, Maureen
Condron, Leo M.
Clough, Tim J.
description Transformation of ruminant urine-nitrogen (N) can contribute to negative environmental outcomes such as nitrate leaching which leads to eutrophication of waterways and production of nitrous oxide (N2O), a greenhouse gas. Although abiotic factors influencing urine-N processing have been well studied, detailed studies of the soil microbial community dynamics following urine application are required to improve mitigation strategies for reducing harmful N fluxes from urine deposition. A factorial laboratory experiment using packed silt-loam soil cores with two levels each of urea (±), soil matric potential (ψ −6.0 or −0.2 kPa) and soil bulk density (ρb 1.1 or 1.5 g cm−3) was performed to study the interaction of urea and soil physical conditions on both soil inorganic N transformations and the abundance of ammonia-oxidizers and denitrifiers. Soil ψ and ρb treatments had an immediate impact on soil pH, dissolved organic carbon, inorganic N pools and emissions of N2O and N2 following urea deposition, and microorganisms carrying the nosZ gene were present in lower numbers in the most aerobic soil (−6.0 kPa and 1.1 g cm−3) from day 7. In all treatments, both bacterial amoA and denitrifier nirS, nirK and nosZ gene copy numbers increased within 1 day following urea application. Dynamics in the NH4+ concentrations were significantly correlated with cumulative changes in the abundance of the ammonia-oxidizers, but no relation was found between cumulative changes in the denitrifier nirS, nirK and nosZ gene copy numbers and the dynamics in soil inorganic N, N2O or N2 emissions. Throughout most of the study period the specific soil conditions, induced by the ψ and ρb treatments, determined nitrifier and denitrifier activity rather than the size of the microbial communities involved. However, by day 35 soil ψ and ρb treatments exerted large treatment effects on bacterial amoA, nirS and nirK gene copy numbers. Thus, although nitrate concentrations and N2O emissions following urea deposition were determined by the soil ψ and ρb conditions in the short-term, our results indicate that changes in the population sizes of denitrifiers and AOB in ruminant urine patches may influence environmental N fluxes in the long-term. •Population size of ammonia-oxidizing bacteria and denitrifiers increased upon urea deposition.•Overall, soil bulk density and matric potential did not affect nitrifier and denitrifier abundance.•However, nosZ gene copy numbers were the lowest in the most aerob
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Although abiotic factors influencing urine-N processing have been well studied, detailed studies of the soil microbial community dynamics following urine application are required to improve mitigation strategies for reducing harmful N fluxes from urine deposition. A factorial laboratory experiment using packed silt-loam soil cores with two levels each of urea (±), soil matric potential (ψ −6.0 or −0.2 kPa) and soil bulk density (ρb 1.1 or 1.5 g cm−3) was performed to study the interaction of urea and soil physical conditions on both soil inorganic N transformations and the abundance of ammonia-oxidizers and denitrifiers. Soil ψ and ρb treatments had an immediate impact on soil pH, dissolved organic carbon, inorganic N pools and emissions of N2O and N2 following urea deposition, and microorganisms carrying the nosZ gene were present in lower numbers in the most aerobic soil (−6.0 kPa and 1.1 g cm−3) from day 7. In all treatments, both bacterial amoA and denitrifier nirS, nirK and nosZ gene copy numbers increased within 1 day following urea application. Dynamics in the NH4+ concentrations were significantly correlated with cumulative changes in the abundance of the ammonia-oxidizers, but no relation was found between cumulative changes in the denitrifier nirS, nirK and nosZ gene copy numbers and the dynamics in soil inorganic N, N2O or N2 emissions. Throughout most of the study period the specific soil conditions, induced by the ψ and ρb treatments, determined nitrifier and denitrifier activity rather than the size of the microbial communities involved. However, by day 35 soil ψ and ρb treatments exerted large treatment effects on bacterial amoA, nirS and nirK gene copy numbers. Thus, although nitrate concentrations and N2O emissions following urea deposition were determined by the soil ψ and ρb conditions in the short-term, our results indicate that changes in the population sizes of denitrifiers and AOB in ruminant urine patches may influence environmental N fluxes in the long-term. •Population size of ammonia-oxidizing bacteria and denitrifiers increased upon urea deposition.•Overall, soil bulk density and matric potential did not affect nitrifier and denitrifier abundance.•However, nosZ gene copy numbers were the lowest in the most aerobic soil from day 7.•Dynamics in soil NH4+-N correlated with cumulative changes in the abundance of ammonia-oxidizers.•Soil conditions rather than microbial abundance determined N2O and N2 emissions in the short-term.</description><identifier>ISSN: 0038-0717</identifier><identifier>EISSN: 1879-3428</identifier><identifier>DOI: 10.1016/j.soilbio.2013.05.006</identifier><identifier>CODEN: SBIOAH</identifier><language>eng</language><publisher>Amsterdam: Elsevier Ltd</publisher><subject>Agronomy. 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Although abiotic factors influencing urine-N processing have been well studied, detailed studies of the soil microbial community dynamics following urine application are required to improve mitigation strategies for reducing harmful N fluxes from urine deposition. A factorial laboratory experiment using packed silt-loam soil cores with two levels each of urea (±), soil matric potential (ψ −6.0 or −0.2 kPa) and soil bulk density (ρb 1.1 or 1.5 g cm−3) was performed to study the interaction of urea and soil physical conditions on both soil inorganic N transformations and the abundance of ammonia-oxidizers and denitrifiers. Soil ψ and ρb treatments had an immediate impact on soil pH, dissolved organic carbon, inorganic N pools and emissions of N2O and N2 following urea deposition, and microorganisms carrying the nosZ gene were present in lower numbers in the most aerobic soil (−6.0 kPa and 1.1 g cm−3) from day 7. In all treatments, both bacterial amoA and denitrifier nirS, nirK and nosZ gene copy numbers increased within 1 day following urea application. Dynamics in the NH4+ concentrations were significantly correlated with cumulative changes in the abundance of the ammonia-oxidizers, but no relation was found between cumulative changes in the denitrifier nirS, nirK and nosZ gene copy numbers and the dynamics in soil inorganic N, N2O or N2 emissions. Throughout most of the study period the specific soil conditions, induced by the ψ and ρb treatments, determined nitrifier and denitrifier activity rather than the size of the microbial communities involved. However, by day 35 soil ψ and ρb treatments exerted large treatment effects on bacterial amoA, nirS and nirK gene copy numbers. Thus, although nitrate concentrations and N2O emissions following urea deposition were determined by the soil ψ and ρb conditions in the short-term, our results indicate that changes in the population sizes of denitrifiers and AOB in ruminant urine patches may influence environmental N fluxes in the long-term. •Population size of ammonia-oxidizing bacteria and denitrifiers increased upon urea deposition.•Overall, soil bulk density and matric potential did not affect nitrifier and denitrifier abundance.•However, nosZ gene copy numbers were the lowest in the most aerobic soil from day 7.•Dynamics in soil NH4+-N correlated with cumulative changes in the abundance of ammonia-oxidizers.•Soil conditions rather than microbial abundance determined N2O and N2 emissions in the short-term.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Ammonia-oxidizing archaea</subject><subject>Ammonia-oxidizing bacteria</subject><subject>amoA</subject><subject>Biochemistry and biology</subject><subject>Biological and medical sciences</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>Denitrification</subject><subject>dissolved organic carbon</subject><subject>emissions</subject><subject>eutrophication</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>genes</subject><subject>greenhouse gases</subject><subject>leaching</subject><subject>microbial communities</subject><subject>Microbiology</subject><subject>nirK</subject><subject>nirS</subject><subject>nitrates</subject><subject>Nitrification</subject><subject>nitrogen</subject><subject>nitrous oxide</subject><subject>nosZ</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>population size</subject><subject>Ruminantia</subject><subject>ruminants</subject><subject>silt loam soils</subject><subject>soil density</subject><subject>soil matric potential</subject><subject>soil microorganisms</subject><subject>soil pH</subject><subject>Soil science</subject><subject>urea</subject><subject>Urine</subject><subject>waterways</subject><issn>0038-0717</issn><issn>1879-3428</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqFkc9u1DAQxiNEJZaWR0D4gsSBpGNnHScnhCr-VKq2B-jZGjv2yovXXuyksM_RF8ZhV1w5WSP_5vtm5quq1xQaCrS73jU5Oq9cbBjQtgHeAHTPqhXtxVC3a9Y_r1YAbV-DoOJF9TLnHQAwTttV9XQbrJ9N0IZESxYdomb_g4wmZDcdCYaR7HFKTpNDnEyYHHoSA9k7naJaivEYsFT5PXEhpi2Ggm7IlDBkG1PpdTGUzw27_yu2YaQY_jaZ2Oh9_OXClszJYHE8xGJZ6KvqwqLP5tX5vawePn_6fvO1vrv_cnvz8a7WrRBTbRQIZtWISgyUtxpHptUaupGp1oJG1GZUyHVvYeBWMT6UlXWvuNCDVh22l9W7k-4hxZ-zyZPcu6yN9xhMnLOkHEB0A19DQfkJLVvnnIyVh-T2mI6SglxCkDt5DkEuIUjgsoRQ-t6eLTBr9LZcRbv8r5mJbt3Tri_cmxNnMUrcpsI8fCtCZQKAHvii9OFEmHKRR2eSzNotuY0uGT3JMbr_zPIH5FGs-A</recordid><startdate>201310</startdate><enddate>201310</enddate><creator>Hamonts, Kelly</creator><creator>Balaine, Nimlesh</creator><creator>Moltchanova, Elena</creator><creator>Beare, Mike</creator><creator>Thomas, Steve</creator><creator>Wakelin, Steven A.</creator><creator>O'Callaghan, Maureen</creator><creator>Condron, Leo M.</creator><creator>Clough, Tim J.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7T7</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H95</scope><scope>L.G</scope><scope>P64</scope></search><sort><creationdate>201310</creationdate><title>Influence of soil bulk density and matric potential on microbial dynamics, inorganic N transformations, N2O and N2 fluxes following urea deposition</title><author>Hamonts, Kelly ; Balaine, Nimlesh ; Moltchanova, Elena ; Beare, Mike ; Thomas, Steve ; Wakelin, Steven A. ; O'Callaghan, Maureen ; Condron, Leo M. ; Clough, Tim J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c377t-eb072fbdab79153cad2cb406d2b3f0caacedba5c8f095fb259251c8b57c9cb6a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Ammonia-oxidizing archaea</topic><topic>Ammonia-oxidizing bacteria</topic><topic>amoA</topic><topic>Biochemistry and biology</topic><topic>Biological and medical sciences</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>Denitrification</topic><topic>dissolved organic carbon</topic><topic>emissions</topic><topic>eutrophication</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>genes</topic><topic>greenhouse gases</topic><topic>leaching</topic><topic>microbial communities</topic><topic>Microbiology</topic><topic>nirK</topic><topic>nirS</topic><topic>nitrates</topic><topic>Nitrification</topic><topic>nitrogen</topic><topic>nitrous oxide</topic><topic>nosZ</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>population size</topic><topic>Ruminantia</topic><topic>ruminants</topic><topic>silt loam soils</topic><topic>soil density</topic><topic>soil matric potential</topic><topic>soil microorganisms</topic><topic>soil pH</topic><topic>Soil science</topic><topic>urea</topic><topic>Urine</topic><topic>waterways</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hamonts, Kelly</creatorcontrib><creatorcontrib>Balaine, Nimlesh</creatorcontrib><creatorcontrib>Moltchanova, Elena</creatorcontrib><creatorcontrib>Beare, Mike</creatorcontrib><creatorcontrib>Thomas, Steve</creatorcontrib><creatorcontrib>Wakelin, Steven A.</creatorcontrib><creatorcontrib>O'Callaghan, Maureen</creatorcontrib><creatorcontrib>Condron, Leo M.</creatorcontrib><creatorcontrib>Clough, Tim J.</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 1: Biological Sciences &amp; Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>Soil biology &amp; biochemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hamonts, Kelly</au><au>Balaine, Nimlesh</au><au>Moltchanova, Elena</au><au>Beare, Mike</au><au>Thomas, Steve</au><au>Wakelin, Steven A.</au><au>O'Callaghan, Maureen</au><au>Condron, Leo M.</au><au>Clough, Tim J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of soil bulk density and matric potential on microbial dynamics, inorganic N transformations, N2O and N2 fluxes following urea deposition</atitle><jtitle>Soil biology &amp; biochemistry</jtitle><date>2013-10</date><risdate>2013</risdate><volume>65</volume><spage>1</spage><epage>11</epage><pages>1-11</pages><issn>0038-0717</issn><eissn>1879-3428</eissn><coden>SBIOAH</coden><abstract>Transformation of ruminant urine-nitrogen (N) can contribute to negative environmental outcomes such as nitrate leaching which leads to eutrophication of waterways and production of nitrous oxide (N2O), a greenhouse gas. Although abiotic factors influencing urine-N processing have been well studied, detailed studies of the soil microbial community dynamics following urine application are required to improve mitigation strategies for reducing harmful N fluxes from urine deposition. A factorial laboratory experiment using packed silt-loam soil cores with two levels each of urea (±), soil matric potential (ψ −6.0 or −0.2 kPa) and soil bulk density (ρb 1.1 or 1.5 g cm−3) was performed to study the interaction of urea and soil physical conditions on both soil inorganic N transformations and the abundance of ammonia-oxidizers and denitrifiers. Soil ψ and ρb treatments had an immediate impact on soil pH, dissolved organic carbon, inorganic N pools and emissions of N2O and N2 following urea deposition, and microorganisms carrying the nosZ gene were present in lower numbers in the most aerobic soil (−6.0 kPa and 1.1 g cm−3) from day 7. In all treatments, both bacterial amoA and denitrifier nirS, nirK and nosZ gene copy numbers increased within 1 day following urea application. Dynamics in the NH4+ concentrations were significantly correlated with cumulative changes in the abundance of the ammonia-oxidizers, but no relation was found between cumulative changes in the denitrifier nirS, nirK and nosZ gene copy numbers and the dynamics in soil inorganic N, N2O or N2 emissions. Throughout most of the study period the specific soil conditions, induced by the ψ and ρb treatments, determined nitrifier and denitrifier activity rather than the size of the microbial communities involved. However, by day 35 soil ψ and ρb treatments exerted large treatment effects on bacterial amoA, nirS and nirK gene copy numbers. Thus, although nitrate concentrations and N2O emissions following urea deposition were determined by the soil ψ and ρb conditions in the short-term, our results indicate that changes in the population sizes of denitrifiers and AOB in ruminant urine patches may influence environmental N fluxes in the long-term. •Population size of ammonia-oxidizing bacteria and denitrifiers increased upon urea deposition.•Overall, soil bulk density and matric potential did not affect nitrifier and denitrifier abundance.•However, nosZ gene copy numbers were the lowest in the most aerobic soil from day 7.•Dynamics in soil NH4+-N correlated with cumulative changes in the abundance of ammonia-oxidizers.•Soil conditions rather than microbial abundance determined N2O and N2 emissions in the short-term.</abstract><cop>Amsterdam</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.soilbio.2013.05.006</doi><tpages>11</tpages></addata></record>
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subjects Agronomy. Soil science and plant productions
Ammonia-oxidizing archaea
Ammonia-oxidizing bacteria
amoA
Biochemistry and biology
Biological and medical sciences
Chemical, physicochemical, biochemical and biological properties
Denitrification
dissolved organic carbon
emissions
eutrophication
Fundamental and applied biological sciences. Psychology
genes
greenhouse gases
leaching
microbial communities
Microbiology
nirK
nirS
nitrates
Nitrification
nitrogen
nitrous oxide
nosZ
Physics, chemistry, biochemistry and biology of agricultural and forest soils
population size
Ruminantia
ruminants
silt loam soils
soil density
soil matric potential
soil microorganisms
soil pH
Soil science
urea
Urine
waterways
title Influence of soil bulk density and matric potential on microbial dynamics, inorganic N transformations, N2O and N2 fluxes following urea deposition
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