Phosphorus Losses in Furrow Irrigation Runoff
ABSTRACT Phosphorus (P) often limits the eutrophication of streams, rivers, and lakes receiving surface runoff. We evaluated the relationships among selected soil P availability indices and runoff P fractions where manure, whey, or commercial fertilizer applications had previously established a rang...
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| Veröffentlicht in: | Journal of environmental quality 2001-05, Vol.30 (3), p.1009-1015 |
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| creator | Westermann, D.T. Bjorneberg, D.L. Aase, J.K. Robbins, C.W. |
| description | ABSTRACT
Phosphorus (P) often limits the eutrophication of streams, rivers, and lakes receiving surface runoff. We evaluated the relationships among selected soil P availability indices and runoff P fractions where manure, whey, or commercial fertilizer applications had previously established a range of soil P availabilities on a Portneuf silt loam (coarse‐silty, mixed, superactive, mesic Durinodic Xeric Haplocalcid) surface‐irrigated with Snake River water. Water‐soluble P, Olsen P (inorganic and organic P), and iron‐oxide impregnated paper–extractable P (FeO‐Ps) were determined on a 0.03‐m soil sample taken from the bottom of each furrow before each irrigation in fall 1998 and spring 1999. Dissolved reactive phosphorus (DRP) in a 0.45‐μm filtered runoff sample, and iron‐oxide impregnated paper–extractable P (FeO‐Pw), total P, and sediment in an unfiltered runoff sample were determined at selected intervals during a 4‐h irrigation on 18.3‐m field plots. The 1998 and 1999 data sets were combined because there were no significant differences. Flow‐weighted average runoff DRP and FeO‐Pw concentrations increased linearly as all three soil P test concentrations increased. The average runoff total P concentration was not related to any soil P test but was linearly related to sediment concentration. Stepwise regression selected the independent variables of sediment, soil lime concentration, and soil organic P extracted by the Olsen method as related to average runoff total P concentration. The average runoff total P concentration was 1.08 mg L−1 at a soil Olsen P concentration of 10 mg kg−1 Soil erosion control will be necessary to reduce P losses in surface irrigation runoff. |
| doi_str_mv | 10.2134/jeq2001.3031009x |
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Phosphorus (P) often limits the eutrophication of streams, rivers, and lakes receiving surface runoff. We evaluated the relationships among selected soil P availability indices and runoff P fractions where manure, whey, or commercial fertilizer applications had previously established a range of soil P availabilities on a Portneuf silt loam (coarse‐silty, mixed, superactive, mesic Durinodic Xeric Haplocalcid) surface‐irrigated with Snake River water. Water‐soluble P, Olsen P (inorganic and organic P), and iron‐oxide impregnated paper–extractable P (FeO‐Ps) were determined on a 0.03‐m soil sample taken from the bottom of each furrow before each irrigation in fall 1998 and spring 1999. Dissolved reactive phosphorus (DRP) in a 0.45‐μm filtered runoff sample, and iron‐oxide impregnated paper–extractable P (FeO‐Pw), total P, and sediment in an unfiltered runoff sample were determined at selected intervals during a 4‐h irrigation on 18.3‐m field plots. The 1998 and 1999 data sets were combined because there were no significant differences. Flow‐weighted average runoff DRP and FeO‐Pw concentrations increased linearly as all three soil P test concentrations increased. The average runoff total P concentration was not related to any soil P test but was linearly related to sediment concentration. Stepwise regression selected the independent variables of sediment, soil lime concentration, and soil organic P extracted by the Olsen method as related to average runoff total P concentration. The average runoff total P concentration was 1.08 mg L−1 at a soil Olsen P concentration of 10 mg kg−1 Soil erosion control will be necessary to reduce P losses in surface irrigation runoff.</description><identifier>ISSN: 0047-2425</identifier><identifier>EISSN: 1537-2537</identifier><identifier>DOI: 10.2134/jeq2001.3031009x</identifier><identifier>PMID: 11401247</identifier><identifier>CODEN: JEVQAA</identifier><language>eng</language><publisher>Madison: American Society of Agronomy, Crop Science Society of America, Soil Science Society</publisher><subject>Agricultural and forest climatology and meteorology. Irrigation. Drainage ; Agriculture - methods ; Agronomy. Soil science and plant productions ; Biological and medical sciences ; Calcium Compounds ; Conservation of Natural Resources ; Erosion control ; Eutrophication ; Fertilizer application ; Fertilizers ; Freshwater ; Fundamental and applied biological sciences. Psychology ; Furrow irrigation ; General agronomy. Plant production ; Geologic Sediments ; Irrigation. Drainage ; Manure ; Nitrogen, phosphorus, potassium fertilizations ; Organic Chemicals ; Oxides ; Phosphorus ; Phosphorus - analysis ; Phosphorus fertilization ; Regression Analysis ; Rivers ; Sediment concentration ; Silt loam ; Soil and water pollution ; Soil erosion ; Soil Pollutants - analysis ; Soil science ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Streams ; Surface irrigation ; Surface runoff ; Water Movements ; Water Pollutants - analysis</subject><ispartof>Journal of environmental quality, 2001-05, Vol.30 (3), p.1009-1015</ispartof><rights>Published in J. Environ. Qual.30:1009–1015.</rights><rights>2001 INIST-CNRS</rights><rights>Copyright American Society of Agronomy, Inc. May/Jun 2001</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c546X-2d222bd4c993d15de127d04dd0eaf9eae41ad9f06290f8abc02f934657986cf93</citedby><cites>FETCH-LOGICAL-c546X-2d222bd4c993d15de127d04dd0eaf9eae41ad9f06290f8abc02f934657986cf93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.2134%2Fjeq2001.3031009x$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.2134%2Fjeq2001.3031009x$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1051908$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/11401247$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Westermann, D.T.</creatorcontrib><creatorcontrib>Bjorneberg, D.L.</creatorcontrib><creatorcontrib>Aase, J.K.</creatorcontrib><creatorcontrib>Robbins, C.W.</creatorcontrib><title>Phosphorus Losses in Furrow Irrigation Runoff</title><title>Journal of environmental quality</title><addtitle>J Environ Qual</addtitle><description>ABSTRACT
Phosphorus (P) often limits the eutrophication of streams, rivers, and lakes receiving surface runoff. We evaluated the relationships among selected soil P availability indices and runoff P fractions where manure, whey, or commercial fertilizer applications had previously established a range of soil P availabilities on a Portneuf silt loam (coarse‐silty, mixed, superactive, mesic Durinodic Xeric Haplocalcid) surface‐irrigated with Snake River water. Water‐soluble P, Olsen P (inorganic and organic P), and iron‐oxide impregnated paper–extractable P (FeO‐Ps) were determined on a 0.03‐m soil sample taken from the bottom of each furrow before each irrigation in fall 1998 and spring 1999. Dissolved reactive phosphorus (DRP) in a 0.45‐μm filtered runoff sample, and iron‐oxide impregnated paper–extractable P (FeO‐Pw), total P, and sediment in an unfiltered runoff sample were determined at selected intervals during a 4‐h irrigation on 18.3‐m field plots. The 1998 and 1999 data sets were combined because there were no significant differences. Flow‐weighted average runoff DRP and FeO‐Pw concentrations increased linearly as all three soil P test concentrations increased. The average runoff total P concentration was not related to any soil P test but was linearly related to sediment concentration. Stepwise regression selected the independent variables of sediment, soil lime concentration, and soil organic P extracted by the Olsen method as related to average runoff total P concentration. The average runoff total P concentration was 1.08 mg L−1 at a soil Olsen P concentration of 10 mg kg−1 Soil erosion control will be necessary to reduce P losses in surface irrigation runoff.</description><subject>Agricultural and forest climatology and meteorology. Irrigation. Drainage</subject><subject>Agriculture - methods</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>Calcium Compounds</subject><subject>Conservation of Natural Resources</subject><subject>Erosion control</subject><subject>Eutrophication</subject><subject>Fertilizer application</subject><subject>Fertilizers</subject><subject>Freshwater</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Furrow irrigation</subject><subject>General agronomy. Plant production</subject><subject>Geologic Sediments</subject><subject>Irrigation. Drainage</subject><subject>Manure</subject><subject>Nitrogen, phosphorus, potassium fertilizations</subject><subject>Organic Chemicals</subject><subject>Oxides</subject><subject>Phosphorus</subject><subject>Phosphorus - analysis</subject><subject>Phosphorus fertilization</subject><subject>Regression Analysis</subject><subject>Rivers</subject><subject>Sediment concentration</subject><subject>Silt loam</subject><subject>Soil and water pollution</subject><subject>Soil erosion</subject><subject>Soil Pollutants - analysis</subject><subject>Soil science</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. Amendments</subject><subject>Streams</subject><subject>Surface irrigation</subject><subject>Surface runoff</subject><subject>Water Movements</subject><subject>Water Pollutants - analysis</subject><issn>0047-2425</issn><issn>1537-2537</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkMtLAzEQxoMotj7unmQR8bY6ee7mKOKTgg8UvIV0k9gt202buKj_vSldUbz0MJmP4TffkA-hAwynBFN2NrULAoBPKVAMID830BBzWuQkPZtoCMCSZoQP0E6M00QSKMQ2GmDMkmbFEOUPEx_nEx-6mI18jDZmdZtddSH4j-w2hPpNv9e-zZ661ju3h7acbqLd7_suerm6fL64yUf317cX56O84ky85sQQQsaGVVJSg7mxmBQGmDFgtZNWW4a1kQ4EkeBKPa6AOEmZ4IUsRZXkLjpZ-c6DX3Q2vqtZHSvbNLq1vosKC0xEKYr1IOMF52LpePQPnPoutOkTCsuCypJKkSBYQVVIUQTr1DzUMx2-FAa1DFz1gaufwNPKYe_bjWfW_C70CSfguAd0rHTjgm6rOv4x5lhCmbDzFfZRN_Zr7V11d_lIlpWG_eyVfgNn6pnn</recordid><startdate>200105</startdate><enddate>200105</enddate><creator>Westermann, D.T.</creator><creator>Bjorneberg, D.L.</creator><creator>Aase, J.K.</creator><creator>Robbins, C.W.</creator><general>American Society of Agronomy, Crop Science Society of America, Soil Science Society</general><general>Crop Science Society of America</general><general>American Society of Agronomy</general><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7T7</scope><scope>7TG</scope><scope>7X2</scope><scope>7X7</scope><scope>7XB</scope><scope>88E</scope><scope>88I</scope><scope>8AF</scope><scope>8AO</scope><scope>8C1</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>KL.</scope><scope>L6V</scope><scope>M0K</scope><scope>M0S</scope><scope>M1P</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P64</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>S0X</scope><scope>SOI</scope><scope>7TV</scope><scope>7UA</scope><scope>F1W</scope><scope>H97</scope><scope>L.G</scope></search><sort><creationdate>200105</creationdate><title>Phosphorus Losses in Furrow Irrigation Runoff</title><author>Westermann, D.T. ; Bjorneberg, D.L. ; Aase, J.K. ; Robbins, C.W.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c546X-2d222bd4c993d15de127d04dd0eaf9eae41ad9f06290f8abc02f934657986cf93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Agricultural and forest climatology and meteorology. Irrigation. Drainage</topic><topic>Agriculture - methods</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>Calcium Compounds</topic><topic>Conservation of Natural Resources</topic><topic>Erosion control</topic><topic>Eutrophication</topic><topic>Fertilizer application</topic><topic>Fertilizers</topic><topic>Freshwater</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Furrow irrigation</topic><topic>General agronomy. Plant production</topic><topic>Geologic Sediments</topic><topic>Irrigation. 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Phosphorus (P) often limits the eutrophication of streams, rivers, and lakes receiving surface runoff. We evaluated the relationships among selected soil P availability indices and runoff P fractions where manure, whey, or commercial fertilizer applications had previously established a range of soil P availabilities on a Portneuf silt loam (coarse‐silty, mixed, superactive, mesic Durinodic Xeric Haplocalcid) surface‐irrigated with Snake River water. Water‐soluble P, Olsen P (inorganic and organic P), and iron‐oxide impregnated paper–extractable P (FeO‐Ps) were determined on a 0.03‐m soil sample taken from the bottom of each furrow before each irrigation in fall 1998 and spring 1999. Dissolved reactive phosphorus (DRP) in a 0.45‐μm filtered runoff sample, and iron‐oxide impregnated paper–extractable P (FeO‐Pw), total P, and sediment in an unfiltered runoff sample were determined at selected intervals during a 4‐h irrigation on 18.3‐m field plots. The 1998 and 1999 data sets were combined because there were no significant differences. Flow‐weighted average runoff DRP and FeO‐Pw concentrations increased linearly as all three soil P test concentrations increased. The average runoff total P concentration was not related to any soil P test but was linearly related to sediment concentration. Stepwise regression selected the independent variables of sediment, soil lime concentration, and soil organic P extracted by the Olsen method as related to average runoff total P concentration. The average runoff total P concentration was 1.08 mg L−1 at a soil Olsen P concentration of 10 mg kg−1 Soil erosion control will be necessary to reduce P losses in surface irrigation runoff.</abstract><cop>Madison</cop><pub>American Society of Agronomy, Crop Science Society of America, Soil Science Society</pub><pmid>11401247</pmid><doi>10.2134/jeq2001.3031009x</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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| ispartof | Journal of environmental quality, 2001-05, Vol.30 (3), p.1009-1015 |
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| subjects | Agricultural and forest climatology and meteorology. Irrigation. Drainage Agriculture - methods Agronomy. Soil science and plant productions Biological and medical sciences Calcium Compounds Conservation of Natural Resources Erosion control Eutrophication Fertilizer application Fertilizers Freshwater Fundamental and applied biological sciences. Psychology Furrow irrigation General agronomy. Plant production Geologic Sediments Irrigation. Drainage Manure Nitrogen, phosphorus, potassium fertilizations Organic Chemicals Oxides Phosphorus Phosphorus - analysis Phosphorus fertilization Regression Analysis Rivers Sediment concentration Silt loam Soil and water pollution Soil erosion Soil Pollutants - analysis Soil science Soil-plant relationships. Soil fertility. Fertilization. Amendments Streams Surface irrigation Surface runoff Water Movements Water Pollutants - analysis |
| title | Phosphorus Losses in Furrow Irrigation Runoff |
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