Furrow irrigation erosion and management
Irrigation-induced furrow erosion reduces topsoil depth and pollutes surface waters. A variety of interacting factors, including inflow rate, slope and soil type, are known to affect furrow erosion. Data are inadequate to understand the furrow erosion process sufficiently well to recommend irrigatio...
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| Veröffentlicht in: | Irrigation science 2004-12, Vol.23 (3), p.123-131 |
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| creator | Fernandez-Gomez, R Mateos, L Giraldez, J.V |
| description | Irrigation-induced furrow erosion reduces topsoil depth and pollutes surface waters. A variety of interacting factors, including inflow rate, slope and soil type, are known to affect furrow erosion. Data are inadequate to understand the furrow erosion process sufficiently well to recommend irrigation practices that maintain high levels of water quality and conserve soil. We performed furrow erosion field studies on two soils (a loamy textured alluvial soil and a clay loam cracking soil) with slopes ranging from 0.3 to 0.8%. Three inflow rates per furrow were applied in each of three irrigations. We found net rates of soil loss in the upper part of the furrow that were up to six times higher than the average net rate for the whole furrow. The soil loss was related to the inflow rate by power functions. High inflow rates on furrows with slopes greater than 0.3% caused unsustainable soil losses. However, at least in the loamy textured soil, it is possible to maintain high irrigation uniformity and application efficiency (within the range 80-85%), while keeping soil losses within a sustainable limit. An analysis of the sediment load data made in the frame of a simple conceptual model helped to explain the dynamics of the furrow erosion process and to establish the basis for modeling furrow erosion. |
| doi_str_mv | 10.1007/s00271-004-0100-3 |
| format | Article |
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A variety of interacting factors, including inflow rate, slope and soil type, are known to affect furrow erosion. Data are inadequate to understand the furrow erosion process sufficiently well to recommend irrigation practices that maintain high levels of water quality and conserve soil. We performed furrow erosion field studies on two soils (a loamy textured alluvial soil and a clay loam cracking soil) with slopes ranging from 0.3 to 0.8%. Three inflow rates per furrow were applied in each of three irrigations. We found net rates of soil loss in the upper part of the furrow that were up to six times higher than the average net rate for the whole furrow. The soil loss was related to the inflow rate by power functions. High inflow rates on furrows with slopes greater than 0.3% caused unsustainable soil losses. However, at least in the loamy textured soil, it is possible to maintain high irrigation uniformity and application efficiency (within the range 80-85%), while keeping soil losses within a sustainable limit. 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A variety of interacting factors, including inflow rate, slope and soil type, are known to affect furrow erosion. Data are inadequate to understand the furrow erosion process sufficiently well to recommend irrigation practices that maintain high levels of water quality and conserve soil. We performed furrow erosion field studies on two soils (a loamy textured alluvial soil and a clay loam cracking soil) with slopes ranging from 0.3 to 0.8%. Three inflow rates per furrow were applied in each of three irrigations. We found net rates of soil loss in the upper part of the furrow that were up to six times higher than the average net rate for the whole furrow. The soil loss was related to the inflow rate by power functions. High inflow rates on furrows with slopes greater than 0.3% caused unsustainable soil losses. However, at least in the loamy textured soil, it is possible to maintain high irrigation uniformity and application efficiency (within the range 80-85%), while keeping soil losses within a sustainable limit. An analysis of the sediment load data made in the frame of a simple conceptual model helped to explain the dynamics of the furrow erosion process and to establish the basis for modeling furrow erosion.</description><subject>agricultural soils</subject><subject>Alluvial soils</subject><subject>Clay loam</subject><subject>clay loam soils</subject><subject>erosion control</subject><subject>Furrow irrigation</subject><subject>furrows</subject><subject>Irrigation practices</subject><subject>irrigation water</subject><subject>loam soils</subject><subject>Sediment load</subject><subject>sediment yield</subject><subject>Soil erosion</subject><subject>Soil texture</subject><subject>Soil types</subject><subject>spatial variation</subject><subject>Surface water</subject><subject>Topsoil</subject><subject>water erosion</subject><subject>water flow</subject><subject>Water quality</subject><issn>0342-7188</issn><issn>1432-1319</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpdkMFKxDAQhoMouK4-gCcXD-IlOpNpk_Qoi6vCggfdc0jbZOmybdekRXx7s9STp4Hh-4f5P8auER4QQD1GAKGQA2Qc0oLTCZthRoIjYXHKZkCZ4Aq1PmcXMe4AUEmdzdj9agyh_140ITRbOzR9t3Chj8dpu3rR2s5uXeu64ZKdebuP7upvztlm9fy5fOXr95e35dOaVyTUwH2dU60qVetMISpFnnytfSmczqlQWVlRZQunZFnIymdQF7lPiCpBelkLT3N2N909hP5rdHEwbRMrt9_bzvVjNKhymZMUCbz9B-76MXTpNyORNEopdIJwgqpUKgbnzSE0rQ0_BsEcxZlJnEnizFGcoZS5mTLe9sZuQxPN5kMAEkAqkFrRL5k8aMA</recordid><startdate>20041201</startdate><enddate>20041201</enddate><creator>Fernandez-Gomez, R</creator><creator>Mateos, L</creator><creator>Giraldez, J.V</creator><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7ST</scope><scope>7UA</scope><scope>7X2</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</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>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M0K</scope><scope>M2P</scope><scope>M7S</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>SOI</scope></search><sort><creationdate>20041201</creationdate><title>Furrow irrigation erosion and management</title><author>Fernandez-Gomez, R ; 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A variety of interacting factors, including inflow rate, slope and soil type, are known to affect furrow erosion. Data are inadequate to understand the furrow erosion process sufficiently well to recommend irrigation practices that maintain high levels of water quality and conserve soil. We performed furrow erosion field studies on two soils (a loamy textured alluvial soil and a clay loam cracking soil) with slopes ranging from 0.3 to 0.8%. Three inflow rates per furrow were applied in each of three irrigations. We found net rates of soil loss in the upper part of the furrow that were up to six times higher than the average net rate for the whole furrow. The soil loss was related to the inflow rate by power functions. High inflow rates on furrows with slopes greater than 0.3% caused unsustainable soil losses. However, at least in the loamy textured soil, it is possible to maintain high irrigation uniformity and application efficiency (within the range 80-85%), while keeping soil losses within a sustainable limit. An analysis of the sediment load data made in the frame of a simple conceptual model helped to explain the dynamics of the furrow erosion process and to establish the basis for modeling furrow erosion.</abstract><cop>Heidelberg</cop><pub>Springer Nature B.V</pub><doi>10.1007/s00271-004-0100-3</doi><tpages>9</tpages></addata></record> |
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| source | SpringerNature Journals |
| subjects | agricultural soils Alluvial soils Clay loam clay loam soils erosion control Furrow irrigation furrows Irrigation practices irrigation water loam soils Sediment load sediment yield Soil erosion Soil texture Soil types spatial variation Surface water Topsoil water erosion water flow Water quality |
| title | Furrow irrigation erosion and management |
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