Spatial and temporal variability of ammonia and other inorganic aerosol species
Nitrogen deposition to the sensitive ecosystems in Rocky Mountain National Park (RMNP) has been increasing. Ammonia has been shown to be a large fraction of this nitrogen deposition, and sources in northeastern Colorado were found to be a significant contributor. In this work we report on the result...
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Veröffentlicht in: | Atmospheric environment (1994) 2012-12, Vol.61, p.490-498 |
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container_title | Atmospheric environment (1994) |
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creator | Day, D.E. Chen, X. Gebhart, K.A. Carrico, C.M. Schwandner, F.M. Benedict, K.B. Schichtel, B.A. Collett, J.L. |
description | Nitrogen deposition to the sensitive ecosystems in Rocky Mountain National Park (RMNP) has been increasing. Ammonia has been shown to be a large fraction of this nitrogen deposition, and sources in northeastern Colorado were found to be a significant contributor. In this work we report on the results from a small network of Radiello passive samplers to investigate the temporal and spatial variability of ammonia gas concentrations in northeastern Colorado. A URG denuder/filter-pack sampler was collocated with a Radiello passive sampler to provide a check on the accuracy of passive ammonia measurements and to provide information about complementary aerosol and trace gas species. These measurements showed seasonal variations in the concentrations of both particulate- and gas-phase aerosol components. The highest concentrations of ammonia occurred during summer months. These were almost twice the lowest concentrations, which occurred during spring and fall months. Ammonia also exhibited higher than expected concentrations during winter. There was considerable spatial variability in average ammonia concentrations, with May–August averages ranging from 3 μg m−3 in rural grasslands to 4–11 μg m−3 at suburban-urban sites to almost 30 μg m−3 in an area of intensive livestock feeding and farming operations. The large ammonia gradients near sources are expected for this primary pollutant with high deposition rates. The overall concentrations in this region are significantly larger than those measured in RMNP, which were around 0.5 μg m−3, and represent a large reservoir of ammonia that can be transported to RMNP with easterly winds.
► Ammonia from the plains of Colorado contributes to N deposition in RMNP. ► Ammonia and other inorganic aerosol species show seasonal variability. ► Ammonia concentrations exhibit large spatial variability. |
doi_str_mv | 10.1016/j.atmosenv.2012.06.045 |
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► Ammonia from the plains of Colorado contributes to N deposition in RMNP. ► Ammonia and other inorganic aerosol species show seasonal variability. ► Ammonia concentrations exhibit large spatial variability.</description><identifier>ISSN: 1352-2310</identifier><identifier>EISSN: 1873-2844</identifier><identifier>DOI: 10.1016/j.atmosenv.2012.06.045</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>aerosols ; Ammonia ; Applied sciences ; atmospheric chemistry ; Atmospheric pollution ; autumn ; Eastern plains of Colorado ; ecosystems ; Exact sciences and technology ; farming systems ; Front range ; grasslands ; livestock feeding ; national parks ; nitrogen ; Passive sampling ; pollutants ; Pollutants physicochemistry study: properties, effects, reactions, transport and distribution ; Pollution ; samplers ; seasonal variation ; Spatial variability ; spring ; summer ; Temporal concentrations ; wind direction ; winter</subject><ispartof>Atmospheric environment (1994), 2012-12, Vol.61, p.490-498</ispartof><rights>2012 Elsevier Ltd</rights><rights>2014 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c465t-3b2294ead4a69077f2d8bd1bf99bd332c7334503aefa57f90d8ad33f045adb0c3</citedby><cites>FETCH-LOGICAL-c465t-3b2294ead4a69077f2d8bd1bf99bd332c7334503aefa57f90d8ad33f045adb0c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S1352231012006085$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=26436755$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Day, D.E.</creatorcontrib><creatorcontrib>Chen, X.</creatorcontrib><creatorcontrib>Gebhart, K.A.</creatorcontrib><creatorcontrib>Carrico, C.M.</creatorcontrib><creatorcontrib>Schwandner, F.M.</creatorcontrib><creatorcontrib>Benedict, K.B.</creatorcontrib><creatorcontrib>Schichtel, B.A.</creatorcontrib><creatorcontrib>Collett, J.L.</creatorcontrib><title>Spatial and temporal variability of ammonia and other inorganic aerosol species</title><title>Atmospheric environment (1994)</title><description>Nitrogen deposition to the sensitive ecosystems in Rocky Mountain National Park (RMNP) has been increasing. Ammonia has been shown to be a large fraction of this nitrogen deposition, and sources in northeastern Colorado were found to be a significant contributor. In this work we report on the results from a small network of Radiello passive samplers to investigate the temporal and spatial variability of ammonia gas concentrations in northeastern Colorado. A URG denuder/filter-pack sampler was collocated with a Radiello passive sampler to provide a check on the accuracy of passive ammonia measurements and to provide information about complementary aerosol and trace gas species. These measurements showed seasonal variations in the concentrations of both particulate- and gas-phase aerosol components. The highest concentrations of ammonia occurred during summer months. These were almost twice the lowest concentrations, which occurred during spring and fall months. Ammonia also exhibited higher than expected concentrations during winter. There was considerable spatial variability in average ammonia concentrations, with May–August averages ranging from 3 μg m−3 in rural grasslands to 4–11 μg m−3 at suburban-urban sites to almost 30 μg m−3 in an area of intensive livestock feeding and farming operations. The large ammonia gradients near sources are expected for this primary pollutant with high deposition rates. The overall concentrations in this region are significantly larger than those measured in RMNP, which were around 0.5 μg m−3, and represent a large reservoir of ammonia that can be transported to RMNP with easterly winds.
► Ammonia from the plains of Colorado contributes to N deposition in RMNP. ► Ammonia and other inorganic aerosol species show seasonal variability. ► Ammonia concentrations exhibit large spatial variability.</description><subject>aerosols</subject><subject>Ammonia</subject><subject>Applied sciences</subject><subject>atmospheric chemistry</subject><subject>Atmospheric pollution</subject><subject>autumn</subject><subject>Eastern plains of Colorado</subject><subject>ecosystems</subject><subject>Exact sciences and technology</subject><subject>farming systems</subject><subject>Front range</subject><subject>grasslands</subject><subject>livestock feeding</subject><subject>national parks</subject><subject>nitrogen</subject><subject>Passive sampling</subject><subject>pollutants</subject><subject>Pollutants physicochemistry study: properties, effects, reactions, transport and distribution</subject><subject>Pollution</subject><subject>samplers</subject><subject>seasonal variation</subject><subject>Spatial variability</subject><subject>spring</subject><subject>summer</subject><subject>Temporal concentrations</subject><subject>wind direction</subject><subject>winter</subject><issn>1352-2310</issn><issn>1873-2844</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNqFkEtP3TAQRiPUSjzav9Bmg9RNwviRONlRIaBISCyAtTWxx-CrJE7tcCX-Pb5cyrYr26MzM59PUfxgUDNg7dmmxnUKieZtzYHxGtoaZHNQHLFOiYp3Un7Jd9HwigsGh8VxShsAEKpXR8Xd_YKrx7HE2ZYrTUuI-bHF6HHwo19fy-BKnKYwe3xnwvpMsfRziE84e1MixZDCWKaFjKf0rfjqcEz0_eM8KR6vLh8u_lS3d9c3F79vKyPbZq3EwHkvCa3EtgelHLfdYNng-n6wQnCjhJANCCSHjXI92A5z3eWPoR3AiJPi137uEsPfF0qrnnwyNI44U3hJmjEmOOsbJjPa7lGTk6ZITi_RTxhfNQO9M6g3-p9BvTOoodV5UW48_diByeDoIs7Gp89u3krRqmbH_dxzDoPGp5iZx_s8qAFgfae6XYTzPUFZydZT1CnLmg1ZH8ms2gb_vzBvyemUtg</recordid><startdate>20121201</startdate><enddate>20121201</enddate><creator>Day, D.E.</creator><creator>Chen, X.</creator><creator>Gebhart, K.A.</creator><creator>Carrico, C.M.</creator><creator>Schwandner, F.M.</creator><creator>Benedict, K.B.</creator><creator>Schichtel, B.A.</creator><creator>Collett, J.L.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7TV</scope><scope>7U6</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>20121201</creationdate><title>Spatial and temporal variability of ammonia and other inorganic aerosol species</title><author>Day, D.E. ; Chen, X. ; Gebhart, K.A. ; Carrico, C.M. ; Schwandner, F.M. ; Benedict, K.B. ; Schichtel, B.A. ; Collett, J.L.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c465t-3b2294ead4a69077f2d8bd1bf99bd332c7334503aefa57f90d8ad33f045adb0c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>aerosols</topic><topic>Ammonia</topic><topic>Applied sciences</topic><topic>atmospheric chemistry</topic><topic>Atmospheric pollution</topic><topic>autumn</topic><topic>Eastern plains of Colorado</topic><topic>ecosystems</topic><topic>Exact sciences and technology</topic><topic>farming systems</topic><topic>Front range</topic><topic>grasslands</topic><topic>livestock feeding</topic><topic>national parks</topic><topic>nitrogen</topic><topic>Passive sampling</topic><topic>pollutants</topic><topic>Pollutants physicochemistry study: properties, effects, reactions, transport and distribution</topic><topic>Pollution</topic><topic>samplers</topic><topic>seasonal variation</topic><topic>Spatial variability</topic><topic>spring</topic><topic>summer</topic><topic>Temporal concentrations</topic><topic>wind direction</topic><topic>winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Day, D.E.</creatorcontrib><creatorcontrib>Chen, X.</creatorcontrib><creatorcontrib>Gebhart, K.A.</creatorcontrib><creatorcontrib>Carrico, C.M.</creatorcontrib><creatorcontrib>Schwandner, F.M.</creatorcontrib><creatorcontrib>Benedict, K.B.</creatorcontrib><creatorcontrib>Schichtel, B.A.</creatorcontrib><creatorcontrib>Collett, J.L.</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Pollution Abstracts</collection><collection>Sustainability Science 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 & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Atmospheric environment (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Day, D.E.</au><au>Chen, X.</au><au>Gebhart, K.A.</au><au>Carrico, C.M.</au><au>Schwandner, F.M.</au><au>Benedict, K.B.</au><au>Schichtel, B.A.</au><au>Collett, J.L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial and temporal variability of ammonia and other inorganic aerosol species</atitle><jtitle>Atmospheric environment (1994)</jtitle><date>2012-12-01</date><risdate>2012</risdate><volume>61</volume><spage>490</spage><epage>498</epage><pages>490-498</pages><issn>1352-2310</issn><eissn>1873-2844</eissn><abstract>Nitrogen deposition to the sensitive ecosystems in Rocky Mountain National Park (RMNP) has been increasing. Ammonia has been shown to be a large fraction of this nitrogen deposition, and sources in northeastern Colorado were found to be a significant contributor. In this work we report on the results from a small network of Radiello passive samplers to investigate the temporal and spatial variability of ammonia gas concentrations in northeastern Colorado. A URG denuder/filter-pack sampler was collocated with a Radiello passive sampler to provide a check on the accuracy of passive ammonia measurements and to provide information about complementary aerosol and trace gas species. These measurements showed seasonal variations in the concentrations of both particulate- and gas-phase aerosol components. The highest concentrations of ammonia occurred during summer months. These were almost twice the lowest concentrations, which occurred during spring and fall months. Ammonia also exhibited higher than expected concentrations during winter. There was considerable spatial variability in average ammonia concentrations, with May–August averages ranging from 3 μg m−3 in rural grasslands to 4–11 μg m−3 at suburban-urban sites to almost 30 μg m−3 in an area of intensive livestock feeding and farming operations. The large ammonia gradients near sources are expected for this primary pollutant with high deposition rates. The overall concentrations in this region are significantly larger than those measured in RMNP, which were around 0.5 μg m−3, and represent a large reservoir of ammonia that can be transported to RMNP with easterly winds.
► Ammonia from the plains of Colorado contributes to N deposition in RMNP. ► Ammonia and other inorganic aerosol species show seasonal variability. ► Ammonia concentrations exhibit large spatial variability.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.atmosenv.2012.06.045</doi><tpages>9</tpages></addata></record> |
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subjects | aerosols Ammonia Applied sciences atmospheric chemistry Atmospheric pollution autumn Eastern plains of Colorado ecosystems Exact sciences and technology farming systems Front range grasslands livestock feeding national parks nitrogen Passive sampling pollutants Pollutants physicochemistry study: properties, effects, reactions, transport and distribution Pollution samplers seasonal variation Spatial variability spring summer Temporal concentrations wind direction winter |
title | Spatial and temporal variability of ammonia and other inorganic aerosol species |
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