Soil hydraulic properties influenced by stiff-stemmed grass hedge systems
The effectiveness of stiff-stemmed grass hedge systems in controlling runoff and soil erosion is influenced by the water transport properties of the soil under grass hedge management. This study evaluated soil hydraulic properties within a grass hedge system 10 yr after establishment. The study was...
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description | The effectiveness of stiff-stemmed grass hedge systems in controlling runoff and soil erosion is influenced by the water transport properties of the soil under grass hedge management. This study evaluated soil hydraulic properties within a grass hedge system 10 yr after establishment. The study was conducted at the USDA-ARS research station near Treynor, IA in a field managed with switchgrass (Panicum virgatum) hedges. The soil was classified as Monona silt loam (fine-silty, mixed, superactive, mesic Typic Hapludolls). Three positions were sampled: within the grass hedges, within the deposition zone 0.5 m upslope from the grass hedges, and within the row crop area 7 m upslope from the hedges. Intact soil samples (76 by 76 mm) were taken from the three positions at four depths (100-mm increments) to determine saturated soil hydraulic conductivity (K(sat)), bulk density (rho(b)), and soil water retention. The grass hedge position had significantly greater (P < 0.05) macroporosity than the row crop and deposition positions in the first two depths and greater than the deposition position in the last two depths. The K(sat) within the grass hedge (668 mm h(-1)) was six times greater than in the row crop position (115 mm h(-1)) and 18 times greater than in the deposition position (37 mm h(-1)) for the surface 10 cm. Bulk density and macroporosity were found to provide the best two-parameter regression model for predicting the log-transformed K(sat) (R2 = 0.68). These results indicate that grass hedges significantly affected soil hydraulic properties for this loess soil. |
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This study evaluated soil hydraulic properties within a grass hedge system 10 yr after establishment. The study was conducted at the USDA-ARS research station near Treynor, IA in a field managed with switchgrass (Panicum virgatum) hedges. The soil was classified as Monona silt loam (fine-silty, mixed, superactive, mesic Typic Hapludolls). Three positions were sampled: within the grass hedges, within the deposition zone 0.5 m upslope from the grass hedges, and within the row crop area 7 m upslope from the hedges. Intact soil samples (76 by 76 mm) were taken from the three positions at four depths (100-mm increments) to determine saturated soil hydraulic conductivity (K(sat)), bulk density (rho(b)), and soil water retention. The grass hedge position had significantly greater (P < 0.05) macroporosity than the row crop and deposition positions in the first two depths and greater than the deposition position in the last two depths. The K(sat) within the grass hedge (668 mm h(-1)) was six times greater than in the row crop position (115 mm h(-1)) and 18 times greater than in the deposition position (37 mm h(-1)) for the surface 10 cm. Bulk density and macroporosity were found to provide the best two-parameter regression model for predicting the log-transformed K(sat) (R2 = 0.68). These results indicate that grass hedges significantly affected soil hydraulic properties for this loess soil.</description><identifier>ISSN: 0361-5995</identifier><identifier>EISSN: 1435-0661</identifier><identifier>DOI: 10.2136/sssaj2004.1386</identifier><identifier>CODEN: SSSJD4</identifier><language>eng</language><publisher>Madison: Soil Science Society</publisher><subject>agricultural runoff ; agricultural watersheds ; Agronomy. Soil science and plant productions ; Biological and medical sciences ; bulk density ; conservation buffers ; Crops ; Fundamental and applied biological sciences. Psychology ; Grasses ; Hydraulic properties ; Hydraulics ; loess soils ; Moisture content ; Panicum virgatum ; Physical properties ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; pore-size distribution ; porosity ; Runoff ; saturated hydraulic conductivity ; Saturated soils ; sediment deposition ; Silt loam ; silt loam soils ; slope ; Soil conductivity ; Soil erosion ; Soil erosion control ; Soil erosion, conservation, land management and development ; soil organic matter ; soil pore system ; Soil properties ; Soil science ; Soil sciences ; soil texture ; Soil water ; soil water content ; Tripsacum dactyloides ; Water and solute dynamics ; Water transport</subject><ispartof>Soil Science Society of America journal, 2004-07, Vol.68 (4), p.1386-1393</ispartof><rights>Soil Science Society of America</rights><rights>2004 INIST-CNRS</rights><rights>Copyright American Society of Agronomy Jul/Aug 2004</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4346-8cb0b4292805afe61d7c431da87f22477a91a830a0f4f2d71bfa48c8d9b8bb6b3</citedby><cites>FETCH-LOGICAL-c4346-8cb0b4292805afe61d7c431da87f22477a91a830a0f4f2d71bfa48c8d9b8bb6b3</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%2Fsssaj2004.1386$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.2136%2Fsssaj2004.1386$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,27923,27924,45573,45574</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16143925$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Rachman, A</creatorcontrib><creatorcontrib>Anderson, S.H</creatorcontrib><creatorcontrib>Gantzer, C.J</creatorcontrib><creatorcontrib>Alberts, E.E</creatorcontrib><title>Soil hydraulic properties influenced by stiff-stemmed grass hedge systems</title><title>Soil Science Society of America journal</title><description>The effectiveness of stiff-stemmed grass hedge systems in controlling runoff and soil erosion is influenced by the water transport properties of the soil under grass hedge management. This study evaluated soil hydraulic properties within a grass hedge system 10 yr after establishment. The study was conducted at the USDA-ARS research station near Treynor, IA in a field managed with switchgrass (Panicum virgatum) hedges. The soil was classified as Monona silt loam (fine-silty, mixed, superactive, mesic Typic Hapludolls). Three positions were sampled: within the grass hedges, within the deposition zone 0.5 m upslope from the grass hedges, and within the row crop area 7 m upslope from the hedges. Intact soil samples (76 by 76 mm) were taken from the three positions at four depths (100-mm increments) to determine saturated soil hydraulic conductivity (K(sat)), bulk density (rho(b)), and soil water retention. The grass hedge position had significantly greater (P < 0.05) macroporosity than the row crop and deposition positions in the first two depths and greater than the deposition position in the last two depths. The K(sat) within the grass hedge (668 mm h(-1)) was six times greater than in the row crop position (115 mm h(-1)) and 18 times greater than in the deposition position (37 mm h(-1)) for the surface 10 cm. Bulk density and macroporosity were found to provide the best two-parameter regression model for predicting the log-transformed K(sat) (R2 = 0.68). These results indicate that grass hedges significantly affected soil hydraulic properties for this loess soil.</description><subject>agricultural runoff</subject><subject>agricultural watersheds</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>bulk density</subject><subject>conservation buffers</subject><subject>Crops</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Grasses</subject><subject>Hydraulic properties</subject><subject>Hydraulics</subject><subject>loess soils</subject><subject>Moisture content</subject><subject>Panicum virgatum</subject><subject>Physical properties</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>pore-size distribution</subject><subject>porosity</subject><subject>Runoff</subject><subject>saturated hydraulic conductivity</subject><subject>Saturated soils</subject><subject>sediment deposition</subject><subject>Silt loam</subject><subject>silt loam soils</subject><subject>slope</subject><subject>Soil conductivity</subject><subject>Soil erosion</subject><subject>Soil erosion control</subject><subject>Soil erosion, conservation, land management and development</subject><subject>soil organic matter</subject><subject>soil pore system</subject><subject>Soil properties</subject><subject>Soil science</subject><subject>Soil sciences</subject><subject>soil texture</subject><subject>Soil water</subject><subject>soil water content</subject><subject>Tripsacum dactyloides</subject><subject>Water and solute dynamics</subject><subject>Water transport</subject><issn>0361-5995</issn><issn>1435-0661</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkc1v1DAQxS0EEkvhypUICW5Zxh9x4gOHquKjqBKH0LM1ceytV9lk8WxU5b_H0a5A4tKLLb35zZvxM2NvOWwFl_oTEeFeAKgtl41-xjZcyaoErflztgGpeVkZU71kr4j2ALwyABt2205xKB6WPuE8RFcc03T06RQ9FXEMw-xH5_uiWwo6xRBKOvnDIQu7hETFg-93vqBlVek1exFwIP_mcl-x-69fft18L-9-fru9ub4rnZJKl43roFPCiAYqDF7zvs4F3mNTByFUXaPh2EhACCqIvuZdQNW4pjdd03W6k1fs49k3r_p79nSyh0jODwOOfprJSi240Vo-CXJV81obk8H3_4H7aU5jfoQVXIOWSqxu2zPk0kSUfLDHFA-YFsvBrvnbv_nbNf_c8OHiiuRwCAlHF-lfl87fY0SVuc9n7jEOfnnC1bbXP0TbrmeWLnPenfsDThZ3Kc-4bwVwCWCMUHn3P5qhoco</recordid><startdate>200407</startdate><enddate>200407</enddate><creator>Rachman, A</creator><creator>Anderson, S.H</creator><creator>Gantzer, C.J</creator><creator>Alberts, E.E</creator><general>Soil Science Society</general><general>Soil Science Society of America</general><general>American Society of Agronomy</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>7XB</scope><scope>88I</scope><scope>8AF</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</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>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>HCIFZ</scope><scope>L6V</scope><scope>M0K</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope><scope>SOI</scope><scope>KR7</scope></search><sort><creationdate>200407</creationdate><title>Soil hydraulic properties influenced by stiff-stemmed grass hedge systems</title><author>Rachman, A ; Anderson, S.H ; Gantzer, C.J ; Alberts, E.E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4346-8cb0b4292805afe61d7c431da87f22477a91a830a0f4f2d71bfa48c8d9b8bb6b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>agricultural runoff</topic><topic>agricultural watersheds</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>bulk density</topic><topic>conservation buffers</topic><topic>Crops</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Grasses</topic><topic>Hydraulic properties</topic><topic>Hydraulics</topic><topic>loess soils</topic><topic>Moisture content</topic><topic>Panicum virgatum</topic><topic>Physical properties</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>pore-size distribution</topic><topic>porosity</topic><topic>Runoff</topic><topic>saturated hydraulic conductivity</topic><topic>Saturated soils</topic><topic>sediment deposition</topic><topic>Silt loam</topic><topic>silt loam soils</topic><topic>slope</topic><topic>Soil conductivity</topic><topic>Soil erosion</topic><topic>Soil erosion control</topic><topic>Soil erosion, conservation, land management and development</topic><topic>soil organic matter</topic><topic>soil pore system</topic><topic>Soil properties</topic><topic>Soil science</topic><topic>Soil sciences</topic><topic>soil texture</topic><topic>Soil water</topic><topic>soil water content</topic><topic>Tripsacum dactyloides</topic><topic>Water and solute dynamics</topic><topic>Water transport</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rachman, A</creatorcontrib><creatorcontrib>Anderson, S.H</creatorcontrib><creatorcontrib>Gantzer, C.J</creatorcontrib><creatorcontrib>Alberts, E.E</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology 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Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><collection>Environment Abstracts</collection><collection>Civil Engineering Abstracts</collection><jtitle>Soil Science Society of America journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rachman, A</au><au>Anderson, S.H</au><au>Gantzer, C.J</au><au>Alberts, E.E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil hydraulic properties influenced by stiff-stemmed grass hedge systems</atitle><jtitle>Soil Science Society of America journal</jtitle><date>2004-07</date><risdate>2004</risdate><volume>68</volume><issue>4</issue><spage>1386</spage><epage>1393</epage><pages>1386-1393</pages><issn>0361-5995</issn><eissn>1435-0661</eissn><coden>SSSJD4</coden><abstract>The effectiveness of stiff-stemmed grass hedge systems in controlling runoff and soil erosion is influenced by the water transport properties of the soil under grass hedge management. This study evaluated soil hydraulic properties within a grass hedge system 10 yr after establishment. The study was conducted at the USDA-ARS research station near Treynor, IA in a field managed with switchgrass (Panicum virgatum) hedges. The soil was classified as Monona silt loam (fine-silty, mixed, superactive, mesic Typic Hapludolls). Three positions were sampled: within the grass hedges, within the deposition zone 0.5 m upslope from the grass hedges, and within the row crop area 7 m upslope from the hedges. Intact soil samples (76 by 76 mm) were taken from the three positions at four depths (100-mm increments) to determine saturated soil hydraulic conductivity (K(sat)), bulk density (rho(b)), and soil water retention. The grass hedge position had significantly greater (P < 0.05) macroporosity than the row crop and deposition positions in the first two depths and greater than the deposition position in the last two depths. The K(sat) within the grass hedge (668 mm h(-1)) was six times greater than in the row crop position (115 mm h(-1)) and 18 times greater than in the deposition position (37 mm h(-1)) for the surface 10 cm. Bulk density and macroporosity were found to provide the best two-parameter regression model for predicting the log-transformed K(sat) (R2 = 0.68). These results indicate that grass hedges significantly affected soil hydraulic properties for this loess soil.</abstract><cop>Madison</cop><pub>Soil Science Society</pub><doi>10.2136/sssaj2004.1386</doi><tpages>8</tpages></addata></record> |
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subjects | agricultural runoff agricultural watersheds Agronomy. Soil science and plant productions Biological and medical sciences bulk density conservation buffers Crops Fundamental and applied biological sciences. Psychology Grasses Hydraulic properties Hydraulics loess soils Moisture content Panicum virgatum Physical properties Physics, chemistry, biochemistry and biology of agricultural and forest soils pore-size distribution porosity Runoff saturated hydraulic conductivity Saturated soils sediment deposition Silt loam silt loam soils slope Soil conductivity Soil erosion Soil erosion control Soil erosion, conservation, land management and development soil organic matter soil pore system Soil properties Soil science Soil sciences soil texture Soil water soil water content Tripsacum dactyloides Water and solute dynamics Water transport |
title | Soil hydraulic properties influenced by stiff-stemmed grass hedge systems |
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