Effect of land use changes on sediment transport in Goodwin Creek

The Goodwin Creek Research Watershed (21.3 km2) is located in the north central part of Mississippi in the bluff hills just east of the Mississippi River floodplain. Land use on the watershed has been surveyed annually and the percentage of cultivated land has decreased from 26% in 1982 to 12% in 19...

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Published in:Water resources research 1996-10, Vol.32 (10), p.3189-3196
Main Authors: Kuhnle, R.A. (National Sedimentation Laboratory, USDA, ARS, Oxford, MS.), Bingner, R.L, Foster, G.R, Grissinger, E.H
Format: Article
Language:English
Subjects:
ARENA
BASSIN VERSANT
BOSQUES
CUENCAS HIDROGRAFICAS
DEBIT
EROSION
ESCORRENTIA
FARMLAND
FINE SEDIMENT
FLOW RATE
FORESTED WATERSHEDS
FORESTS
FORET
GASTO
GEOLOGIA
GEOLOGICAL SEDIMENTATION
GEOLOGIE
GEOLOGY
GOODWIN CREEK EXPERIMENTAL WATERSHED
GRAVA
GRAVEL
GRAVIER
LAND USE
LLUVIA
MISSISSIPPI
MODELE DE SIMULATION
MODELOS DE SIMULACION
PASTIZALES
PASTURE WATERSHEDS
PASTURES
PATURAGES
PLUIE
RAIN
RENDEMENT
RENDIMIENTO
RUISSELLEMENT
RUNOFF
SABLE
SAND
SEDIMENT
SEDIMENTO
SIMULATION MODELS
STREAM FLOW
TERRE AGRICOLE
TIERRAS AGRICOLAS
UTILISATION DES TERRES
UTILIZACION DE LA TIERRA
WATERSHEDS
YIELDS
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cited_by cdi_FETCH-LOGICAL-a3812-b4734712759d89f9577b34693d25082963570f6d9f1da56b877d07f10d009be53
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creator Kuhnle, R.A. (National Sedimentation Laboratory, USDA, ARS, Oxford, MS.)
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description The Goodwin Creek Research Watershed (21.3 km2) is located in the north central part of Mississippi in the bluff hills just east of the Mississippi River floodplain. Land use on the watershed has been surveyed annually and the percentage of cultivated land has decreased from 26% in 1982 to 12% in 1990. During this 9-year period the concentration of fines (0.062 mm) in Goodwin Creek have decreased by 62%, concentrations of sand (0.062-2.0 mm) have decreased by 66%, and concentrations of gravel (2.0 mm) have decreased by 39%. The decrease in the percentage of cultivated land affects the sediment budget of the watershed in two ways. A source of readily eroded sediment is removed, and the energy of the flowing water available to erode and transport sediment is reduced. The reduced flow in the channels from the decrease in cultivated land in the watershed was probably the main cause for the lower transport rates of sand and gravel
doi_str_mv 10.1029/96WR02104
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The reduced flow in the channels from the decrease in cultivated land in the watershed was probably the main cause for the lower transport rates of sand and gravel</description><subject>ARENA</subject><subject>BASSIN VERSANT</subject><subject>BOSQUES</subject><subject>CUENCAS HIDROGRAFICAS</subject><subject>DEBIT</subject><subject>EROSION</subject><subject>ESCORRENTIA</subject><subject>FARMLAND</subject><subject>FINE SEDIMENT</subject><subject>FLOW RATE</subject><subject>FORESTED WATERSHEDS</subject><subject>FORESTS</subject><subject>FORET</subject><subject>GASTO</subject><subject>GEOLOGIA</subject><subject>GEOLOGICAL SEDIMENTATION</subject><subject>GEOLOGIE</subject><subject>GEOLOGY</subject><subject>GOODWIN CREEK EXPERIMENTAL WATERSHED</subject><subject>GRAVA</subject><subject>GRAVEL</subject><subject>GRAVIER</subject><subject>LAND USE</subject><subject>LLUVIA</subject><subject>MISSISSIPPI</subject><subject>MODELE DE SIMULATION</subject><subject>MODELOS DE SIMULACION</subject><subject>PASTIZALES</subject><subject>PASTURE WATERSHEDS</subject><subject>PASTURES</subject><subject>PATURAGES</subject><subject>PLUIE</subject><subject>RAIN</subject><subject>RENDEMENT</subject><subject>RENDIMIENTO</subject><subject>RUISSELLEMENT</subject><subject>RUNOFF</subject><subject>SABLE</subject><subject>SAND</subject><subject>SEDIMENT</subject><subject>SEDIMENTO</subject><subject>SIMULATION MODELS</subject><subject>STREAM FLOW</subject><subject>TERRE AGRICOLE</subject><subject>TIERRAS AGRICOLAS</subject><subject>UTILISATION DES TERRES</subject><subject>UTILIZACION DE LA TIERRA</subject><subject>WATERSHEDS</subject><subject>YIELDS</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1996</creationdate><recordtype>article</recordtype><recordid>eNp10EFLAzEQBeAgCtbqwR8g5CR4WJ1sspnmKIutYlWoSsFLSJukrm03Ndmi_fe2rHjz9C7fG4ZHyCmDSwa5ulJyPIKcgdgjHaaEyFAh3ycdAMEzxhUekqOUPgCYKCR2yPWN927a0ODpwtSWrpOj03dTz1yioabJ2Wrp6oY20dRpFWJDq5oOQrBf2yyjc_NjcuDNIrmT3-yS1_7NS3mbDZ8Gd-X1MDO8x_JsIpALZDkWyvaUVwXihAupuM0L6OVK8gLBS6s8s6aQkx6iBfQMLICauIJ3yXl7dxXD59qlRi-rNHWL7dsurJNmXHImxQ5etHAaQ0rReb2K1dLEjWagdyPpv5G29qq1X9XCbf6HejwqR8jzfNvI2kaVGvf91zBxriVyLPT4caDv-6J8exg-650_a703QZtZrJJ-fWZKIQgFSvAfuXV9CQ</recordid><startdate>199610</startdate><enddate>199610</enddate><creator>Kuhnle, R.A. 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The reduced flow in the channels from the decrease in cultivated land in the watershed was probably the main cause for the lower transport rates of sand and gravel</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/96WR02104</doi><tpages>8</tpages></addata></record>
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identifier ISSN: 0043-1397
ispartof Water resources research, 1996-10, Vol.32 (10), p.3189-3196
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language eng
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source Wiley-Blackwell Journals (Backfile Content)
subjects ARENA
BASSIN VERSANT
BOSQUES
CUENCAS HIDROGRAFICAS
DEBIT
EROSION
ESCORRENTIA
FARMLAND
FINE SEDIMENT
FLOW RATE
FORESTED WATERSHEDS
FORESTS
FORET
GASTO
GEOLOGIA
GEOLOGICAL SEDIMENTATION
GEOLOGIE
GEOLOGY
GOODWIN CREEK EXPERIMENTAL WATERSHED
GRAVA
GRAVEL
GRAVIER
LAND USE
LLUVIA
MISSISSIPPI
MODELE DE SIMULATION
MODELOS DE SIMULACION
PASTIZALES
PASTURE WATERSHEDS
PASTURES
PATURAGES
PLUIE
RAIN
RENDEMENT
RENDIMIENTO
RUISSELLEMENT
RUNOFF
SABLE
SAND
SEDIMENT
SEDIMENTO
SIMULATION MODELS
STREAM FLOW
TERRE AGRICOLE
TIERRAS AGRICOLAS
UTILISATION DES TERRES
UTILIZACION DE LA TIERRA
WATERSHEDS
YIELDS
title Effect of land use changes on sediment transport in Goodwin Creek
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