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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Veröffentlicht in:Soil Science Society of America journal 2004-07, Vol.68 (4), p.1386-1393
Hauptverfasser: Rachman, A, Anderson, S.H, Gantzer, C.J, Alberts, E.E
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Anderson, S.H
Gantzer, C.J
Alberts, E.E
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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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&amp;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 &lt; 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. 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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 &lt; 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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