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Phosphorus leaching in relation to soil type and soil phosphorus content
Phosphorus losses from arable soils contribute to eutrophication of freshwater systems. In addition to losses through surface runoff, leaching has lately gained increased attention as an important P transport pathway. Increased P levels in arable soils have highlighted the necessity of establishing...
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Published in: | Journal of environmental quality 2004-03, Vol.33 (2), p.678-684 |
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description | Phosphorus losses from arable soils contribute to eutrophication of freshwater systems. In addition to losses through surface runoff, leaching has lately gained increased attention as an important P transport pathway. Increased P levels in arable soils have highlighted the necessity of establishing a relationship between actual P leaching and soil P levels. In this study, we measured leaching of total phosphorus (TP) and dissolved reactive phosphorus (DRP) during three years in undisturbed soil columns of five soils. The soils were collected at sites, established between 1957 and 1966, included in a long-term Swedish fertility experiment with four P fertilization levels at each site. Total P losses varied between 0.03 and 1.09 kg ha(-1) yr(-1), but no general correlation could be found between P concentrations and soil test P (Olsen P and phosphorus content in ammonium lactate extract [P-AL]) or P sorption indices (single-point phosphorus sorption index [PSI] and P sorption saturation) of the topsoil. Instead, water transport mechanism through the soil and subsoil properties seemed to be more important for P leaching than soil test P value in the topsoil. In one soil, where preferential flow was the dominant water transport pathway, water and P bypassed the high sorption capacity of the subsoil, resulting in high losses. On the other hand, P leaching from some soils was low in spite of high P applications due to high P sorption capacity in the subsoil. Therefore, site-specific factors may serve as indicators for P leaching losses, but a single, general indicator for all soil types was not found in this study. |
doi_str_mv | 10.2134/jeq2004.0678 |
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In addition to losses through surface runoff, leaching has lately gained increased attention as an important P transport pathway. Increased P levels in arable soils have highlighted the necessity of establishing a relationship between actual P leaching and soil P levels. In this study, we measured leaching of total phosphorus (TP) and dissolved reactive phosphorus (DRP) during three years in undisturbed soil columns of five soils. The soils were collected at sites, established between 1957 and 1966, included in a long-term Swedish fertility experiment with four P fertilization levels at each site. Total P losses varied between 0.03 and 1.09 kg ha(-1) yr(-1), but no general correlation could be found between P concentrations and soil test P (Olsen P and phosphorus content in ammonium lactate extract [P-AL]) or P sorption indices (single-point phosphorus sorption index [PSI] and P sorption saturation) of the topsoil. Instead, water transport mechanism through the soil and subsoil properties seemed to be more important for P leaching than soil test P value in the topsoil. In one soil, where preferential flow was the dominant water transport pathway, water and P bypassed the high sorption capacity of the subsoil, resulting in high losses. On the other hand, P leaching from some soils was low in spite of high P applications due to high P sorption capacity in the subsoil. Therefore, site-specific factors may serve as indicators for P leaching losses, but a single, general indicator for all soil types was not found in this study.</description><identifier>ISSN: 0047-2425</identifier><identifier>EISSN: 1537-2537</identifier><identifier>DOI: 10.2134/jeq2004.0678</identifier><identifier>PMID: 15074820</identifier><identifier>CODEN: JEVQAA</identifier><language>eng</language><publisher>Madison, WI: Crop Science Society of America</publisher><subject>Adsorption ; Agronomy ; Agronomy. Soil science and plant productions ; Ammonium ; Applied sciences ; Arable land ; Biological and medical sciences ; Bypasses ; Copyrights ; Correlation ; Dissolution ; Earth sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Environmental monitoring ; Environmental quality ; Eutrophication ; Exact sciences and technology ; Fertility ; Fundamental and applied biological sciences. Psychology ; Indicators ; Leaching ; losses from soil ; Pathways ; Phosphorus ; Phosphorus - analysis ; Phosphorus - chemistry ; Phosphorus content ; phosphorus fertilizers ; Pollution ; Pollution, environment geology ; Preferential flow ; Runoff ; Saturation ; Soil (material) ; Soil columns ; Soil contaminants ; soil nutrient balance ; Soil Pollutants - analysis ; soil test values ; Soil testing ; soil transport processes ; Soil types ; Solubility ; Sorption ; Subsoils ; subsurface flow ; Surface runoff ; Topsoil ; Transport ; Water Movements ; Water Pollutants - analysis ; water pollution ; Water transport</subject><ispartof>Journal of environmental quality, 2004-03, Vol.33 (2), p.678-684</ispartof><rights>2004 INIST-CNRS</rights><rights>Copyright American Society of Agronomy Mar/Apr 2004</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c455t-48f36983ed72fd36d9212954a0c48fa37021d3fe6d06e1d952f0c1b9c9ca1a143</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=15587849$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/15074820$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Djodjic, F</creatorcontrib><creatorcontrib>Borling, K</creatorcontrib><creatorcontrib>Bergstrom, L</creatorcontrib><title>Phosphorus leaching in relation to soil type and soil phosphorus content</title><title>Journal of environmental quality</title><addtitle>J Environ Qual</addtitle><description>Phosphorus losses from arable soils contribute to eutrophication of freshwater systems. In addition to losses through surface runoff, leaching has lately gained increased attention as an important P transport pathway. Increased P levels in arable soils have highlighted the necessity of establishing a relationship between actual P leaching and soil P levels. In this study, we measured leaching of total phosphorus (TP) and dissolved reactive phosphorus (DRP) during three years in undisturbed soil columns of five soils. The soils were collected at sites, established between 1957 and 1966, included in a long-term Swedish fertility experiment with four P fertilization levels at each site. Total P losses varied between 0.03 and 1.09 kg ha(-1) yr(-1), but no general correlation could be found between P concentrations and soil test P (Olsen P and phosphorus content in ammonium lactate extract [P-AL]) or P sorption indices (single-point phosphorus sorption index [PSI] and P sorption saturation) of the topsoil. Instead, water transport mechanism through the soil and subsoil properties seemed to be more important for P leaching than soil test P value in the topsoil. In one soil, where preferential flow was the dominant water transport pathway, water and P bypassed the high sorption capacity of the subsoil, resulting in high losses. On the other hand, P leaching from some soils was low in spite of high P applications due to high P sorption capacity in the subsoil. Therefore, site-specific factors may serve as indicators for P leaching losses, but a single, general indicator for all soil types was not found in this study.</description><subject>Adsorption</subject><subject>Agronomy</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Ammonium</subject><subject>Applied sciences</subject><subject>Arable land</subject><subject>Biological and medical sciences</subject><subject>Bypasses</subject><subject>Copyrights</subject><subject>Correlation</subject><subject>Dissolution</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Environmental monitoring</subject><subject>Environmental quality</subject><subject>Eutrophication</subject><subject>Exact sciences and technology</subject><subject>Fertility</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Indicators</subject><subject>Leaching</subject><subject>losses from soil</subject><subject>Pathways</subject><subject>Phosphorus</subject><subject>Phosphorus - analysis</subject><subject>Phosphorus - chemistry</subject><subject>Phosphorus content</subject><subject>phosphorus fertilizers</subject><subject>Pollution</subject><subject>Pollution, environment geology</subject><subject>Preferential flow</subject><subject>Runoff</subject><subject>Saturation</subject><subject>Soil (material)</subject><subject>Soil columns</subject><subject>Soil contaminants</subject><subject>soil nutrient balance</subject><subject>Soil Pollutants - analysis</subject><subject>soil test values</subject><subject>Soil testing</subject><subject>soil transport processes</subject><subject>Soil types</subject><subject>Solubility</subject><subject>Sorption</subject><subject>Subsoils</subject><subject>subsurface flow</subject><subject>Surface runoff</subject><subject>Topsoil</subject><subject>Transport</subject><subject>Water Movements</subject><subject>Water Pollutants - analysis</subject><subject>water pollution</subject><subject>Water transport</subject><issn>0047-2425</issn><issn>1537-2537</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNqN0EtLxDAQAOAgiq6Pm2ctgnradSbP5ijiCxYU1HOJaep26Sa1aQ_7743siuJBvGTy-CaZCSGHCBOKjF_M3TsF4BOQKt8gIxRMjWkaNskobac5p2KH7MY4B0AKSm6THRSgeE5hRO4eZyG2s9ANMWucsbPav2W1zzrXmL4OPutDFkPdZP2ydZnx5WrVfmfZ4Hvn-32yVZkmuoN13CMvN9fPV3fj6cPt_dXldGy5EP2Y5xWTOmeuVLQqmSw1RaoFN2DTkWEKKJascrIE6bDUglZg8VVbbQ0a5GyPnK_ubbvwPrjYF4s6Wtc0xrswxEJxlh5QVCd59qdEiUqC_gfkMs-FwARPfsF5GDqf2i1QKw5a6M8Cj9ZoeF24smi7emG6ZfH15wmcroGJ1jRVZ7yt4w8ncpXzz7KOV64yoTBvXTIvTxSQAWgluEL2Ab1Wl3s</recordid><startdate>20040301</startdate><enddate>20040301</enddate><creator>Djodjic, F</creator><creator>Borling, K</creator><creator>Bergstrom, L</creator><general>Crop Science Society of America</general><general>American Society of Agronomy</general><scope>FBQ</scope><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</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>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>7QH</scope><scope>7TV</scope><scope>7UA</scope><scope>7SU</scope><scope>KR7</scope></search><sort><creationdate>20040301</creationdate><title>Phosphorus leaching in relation to soil type and soil phosphorus content</title><author>Djodjic, F ; Borling, K ; Bergstrom, L</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c455t-48f36983ed72fd36d9212954a0c48fa37021d3fe6d06e1d952f0c1b9c9ca1a143</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Adsorption</topic><topic>Agronomy</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Ammonium</topic><topic>Applied sciences</topic><topic>Arable land</topic><topic>Biological and medical sciences</topic><topic>Bypasses</topic><topic>Copyrights</topic><topic>Correlation</topic><topic>Dissolution</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Environmental monitoring</topic><topic>Environmental quality</topic><topic>Eutrophication</topic><topic>Exact sciences and technology</topic><topic>Fertility</topic><topic>Fundamental and applied biological sciences. 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In addition to losses through surface runoff, leaching has lately gained increased attention as an important P transport pathway. Increased P levels in arable soils have highlighted the necessity of establishing a relationship between actual P leaching and soil P levels. In this study, we measured leaching of total phosphorus (TP) and dissolved reactive phosphorus (DRP) during three years in undisturbed soil columns of five soils. The soils were collected at sites, established between 1957 and 1966, included in a long-term Swedish fertility experiment with four P fertilization levels at each site. Total P losses varied between 0.03 and 1.09 kg ha(-1) yr(-1), but no general correlation could be found between P concentrations and soil test P (Olsen P and phosphorus content in ammonium lactate extract [P-AL]) or P sorption indices (single-point phosphorus sorption index [PSI] and P sorption saturation) of the topsoil. Instead, water transport mechanism through the soil and subsoil properties seemed to be more important for P leaching than soil test P value in the topsoil. In one soil, where preferential flow was the dominant water transport pathway, water and P bypassed the high sorption capacity of the subsoil, resulting in high losses. On the other hand, P leaching from some soils was low in spite of high P applications due to high P sorption capacity in the subsoil. Therefore, site-specific factors may serve as indicators for P leaching losses, but a single, general indicator for all soil types was not found in this study.</abstract><cop>Madison, WI</cop><pub>Crop Science Society of America</pub><pmid>15074820</pmid><doi>10.2134/jeq2004.0678</doi><tpages>7</tpages></addata></record> |
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subjects | Adsorption Agronomy Agronomy. Soil science and plant productions Ammonium Applied sciences Arable land Biological and medical sciences Bypasses Copyrights Correlation Dissolution Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Environmental monitoring Environmental quality Eutrophication Exact sciences and technology Fertility Fundamental and applied biological sciences. Psychology Indicators Leaching losses from soil Pathways Phosphorus Phosphorus - analysis Phosphorus - chemistry Phosphorus content phosphorus fertilizers Pollution Pollution, environment geology Preferential flow Runoff Saturation Soil (material) Soil columns Soil contaminants soil nutrient balance Soil Pollutants - analysis soil test values Soil testing soil transport processes Soil types Solubility Sorption Subsoils subsurface flow Surface runoff Topsoil Transport Water Movements Water Pollutants - analysis water pollution Water transport |
title | Phosphorus leaching in relation to soil type and soil phosphorus content |
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