Agricultural practices influence flow regimes of headwater streams in western Iowa

Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971-1995) hydrologic records from four first-order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two...

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Published inJournal of environmental quality Vol. 34; no. 5; pp. 1547 - 1558
Main Authors Tomer, M.D, Meek, D.W, Kramer, L.A
Format Journal Article
LanguageEnglish
Published Madison American Society of Agronomy, Crop Science Society of America, Soil Science Society 01.09.2005
Crop Science Society of America
American Society of Agronomy
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Abstract Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971-1995) hydrologic records from four first-order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two were under conservation (ridge) tillage, one of which was terraced. All four watersheds grew corn (Zea mays L.) every year. Flow-frequency statistics and autoregressive modeling were used to determine how conservation treatments influenced stream hydrology. The autoregressive modeling characterized variations in discharge, baseflow, and runoff at multi-year, annual, and shorter time scales. The ridge-tilled watershed (nonterraced) had 47% less runoff and 36% more baseflow than the conventional watershed of similar landform and slope. Recovery of baseflow after drought was quicker in the conservation watersheds, as evidenced by 365-d moving average plots, and 67% greater baseflow during the driest 2 yr. The two conventional watersheds were similar, except the steeper watershed discharged more runoff and baseflow during short (<30 d), wet periods. Significant multi-year and annual cycles occurred in all variables. Under ridge-till, seasonal (annual-cycle) variations in baseflow had greater amplitude, showing the seasonality of subsurface contaminant movement could increase under conservation practices. However, deviations from the modeled cycles of baseflow were also more persistent under conservation practices, indicating baseflow was more stable. Indeed, flow-frequency curves showed wet-weather discharge decreased and dry-weather discharge increased under conservation practices. Although mean discharge increased in the conservation watersheds, variance and skewness of daily values were smaller. Ridge tillage with or without terraces increased stream discharge but reduced its variability.
AbstractList ABSTRACT Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971–1995) hydrologic records from four first‐order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two were under conservation (ridge) tillage, one of which was terraced. All four watersheds grew corn (Zea mays L.) every year. Flow‐frequency statistics and autoregressive modeling were used to determine how conservation treatments influenced stream hydrology. The autoregressive modeling characterized variations in discharge, baseflow, and runoff at multi‐year, annual, and shorter time scales. The ridge‐tilled watershed (nonterraced) had 47% less runoff and 36% more baseflow than the conventional watershed of similar landform and slope. Recovery of baseflow after drought was quicker in the conservation watersheds, as evidenced by 365‐d moving average plots, and 67% greater baseflow during the driest 2 yr. The two conventional watersheds were similar, except the steeper watershed discharged more runoff and baseflow during short (<30 d), wet periods. Significant multi‐year and annual cycles occurred in all variables. Under ridge‐till, seasonal (annual‐cycle) variations in baseflow had greater amplitude, showing the seasonality of subsurface contaminant movement could increase under conservation practices. However, deviations from the modeled cycles of baseflow were also more persistent under conservation practices, indicating baseflow was more stable. Indeed, flow‐frequency curves showed wet‐weather discharge decreased and dry‐weather discharge increased under conservation practices. Although mean discharge increased in the conservation watersheds, variance and skewness of daily values were smaller. Ridge tillage with or without terraces increased stream discharge but reduced its variability.
Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971-1995) hydrologic records from four first-order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two were under conservation (ridge) tillage, one of which was terraced. All four watersheds grew corn (Zea mays L.) every year. Flow-frequency statistics and autoregressive modeling were used to determine how conservation treatments influenced stream hydrology. The autoregressive modeling characterized variations in discharge, baseflow, and runoff at multi-year, annual, and shorter time scales. The ridge-tilled watershed (nonterraced) had 47% less runoff and 36% more baseflow than the conventional watershed of similar landform and slope. Recovery of baseflow after drought was quicker in the conservation watersheds, as evidenced by 365-d moving average plots, and 67% greater baseflow during the driest 2 yr. The two conventional watersheds were similar, except the steeper watershed discharged more runoff and baseflow during short (<30 d), wet periods. Significant multi-year and annual cycles occurred in all variables. Under ridge-till, seasonal (annual-cycle) variations in baseflow had greater amplitude, showing the seasonality of subsurface contaminant movement could increase under conservation practices. However, deviations from the modeled cycles of baseflow were also more persistent under conservation practices, indicating baseflow was more stable. Indeed, flow-frequency curves showed wet-weather discharge decreased and dry-weather discharge increased under conservation practices. Although mean discharge increased in the conservation watersheds, variance and skewness of daily values were smaller. Ridge tillage with or without terraces increased stream discharge but reduced its variability.
ABSTRACT Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971–1995) hydrologic records from four first‐order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two were under conservation (ridge) tillage, one of which was terraced. All four watersheds grew corn ( Zea mays L.) every year. Flow‐frequency statistics and autoregressive modeling were used to determine how conservation treatments influenced stream hydrology. The autoregressive modeling characterized variations in discharge, baseflow, and runoff at multi‐year, annual, and shorter time scales. The ridge‐tilled watershed (nonterraced) had 47% less runoff and 36% more baseflow than the conventional watershed of similar landform and slope. Recovery of baseflow after drought was quicker in the conservation watersheds, as evidenced by 365‐d moving average plots, and 67% greater baseflow during the driest 2 yr. The two conventional watersheds were similar, except the steeper watershed discharged more runoff and baseflow during short (<30 d), wet periods. Significant multi‐year and annual cycles occurred in all variables. Under ridge‐till, seasonal (annual‐cycle) variations in baseflow had greater amplitude, showing the seasonality of subsurface contaminant movement could increase under conservation practices. However, deviations from the modeled cycles of baseflow were also more persistent under conservation practices, indicating baseflow was more stable. Indeed, flow‐frequency curves showed wet‐weather discharge decreased and dry‐weather discharge increased under conservation practices. Although mean discharge increased in the conservation watersheds, variance and skewness of daily values were smaller. Ridge tillage with or without terraces increased stream discharge but reduced its variability.
Data from four small watersheds near Treynor, IA, were used to explore the influence of agricultural practices on flow regimes of headwater streams. Between 1971 and 1995, the respective watersheds had been managed consistently under a single experimental design, with two watersheds under a conventional tillage system and the other two under a ridge-till system. Daily data collected during the study period included precipitation, runoff, baseflow, and total discharge, and pan evaporation data were collected at an adjacent weather station. Results indicated that conservation tillage increased baseflow and total discharge, but decreased runoff compared to conventional tillage, which resulted in greater stream discharge from the conservation watersheds, especially during wet periods. Under conservation tillage, less discharge occurred during wet weather and greater discharge occurred during dry weather, and baseflow recovery after drought occurred more rapidly in the conservation watersheds.
Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971-1995) hydrologic records from four first-order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two were under conservation (ridge) tillage, one of which was terraced. All four watersheds grew corn (Zea mays L.) every year. Flow-frequency statistics and autoregressive modeling were used to determine how conservation treatments influenced stream hydrology. The autoregressive modeling characterized variations in discharge, baseflow, and runoff at multi-year, annual, and shorter time scales. The ridge-tilled watershed (nonterraced) had 47% less runoff and 36% more baseflow than the conventional watershed of similar landform and slope. Recovery of baseflow after drought was quicker in the conservation watersheds, as evidenced by 365-d moving average plots, and 67% greater baseflow during the driest 2 yr. The two conventional watersheds were similar, except the steeper watershed discharged more runoff and baseflow during short (&lt;30 d), wet periods. Significant multi-year and annual cycles occurred in all variables. Under ridge-till, seasonal (annual-cycle) variations in baseflow had greater amplitude, showing the seasonality of subsurface contaminant movement could increase under conservation practices. However, deviations from the modeled cycles of baseflow were also more persistent under conservation practices, indicating baseflow was more stable. Indeed, flow-frequency curves showed wet-weather discharge decreased and dry-weather discharge increased under conservation practices. Although mean discharge increased in the conservation watersheds, variance and skewness of daily values were smaller. Ridge tillage with or without terraces increased stream discharge but reduced its variability.
Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr (1971-1995) hydrologic records from four first-order watersheds in Iowa's loess hills. Two watersheds were under conventional tillage and two were under conservation (ridge) tillage, one of which was terraced. All four watersheds grew corn (Zea mays L.) every year. Flow-frequency statistics and autoregressive modeling were used to determine how conservation treatments influenced stream hydrology. The autoregressive modeling characterized variations in discharge, baseflow, and runoff at multi-year, annual, and shorter time scales. The ridge-tilled watershed (nonterraced) had 47% less runoff and 36% more baseflow than the conventional watershed of similar landform and slope. Recovery of baseflow after drought was quicker in the conservation watersheds, as evidenced by 365-d moving average plots, and 67% greater baseflow during the driest 2 yr. The two conventional watersheds were similar, except the steeper watershed discharged more runoff and baseflow during short (<30 d), wet periods. Significant multi-year and annual cycles occurred in all variables. Under ridge-till, seasonal (annual-cycle) variations in baseflow had greater amplitude, showing the seasonality of subsurface contaminant movement could increase under conservation practices. However, deviations from the modeled cycles of baseflow were also more persistent under conservation practices, indicating baseflow was more stable. Indeed, flow-frequency curves showed wet-weather discharge decreased and dry-weather discharge increased under conservation practices. Although mean discharge increased in the conservation watersheds, variance and skewness of daily values were smaller. Ridge tillage with or without terraces increased stream discharge but reduced its variability. [PUBLICATION ABSTRACT]
Author Meek, D.W
Tomer, M.D
Kramer, L.A
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Issue 5
Keywords Monocotyledones
First record
Modeling
Slope
Pollution
Flow regime
Gramineae
Seasonal variation
Ridge tillage
Conventional tillage
Angiospermae
Watershed
Motion study
Agriculture
Drought
Subsurface
Loess
Cultural practice
Soil tillage
Zea mays
Annual variation
Pollutant behavior
Stream discharge
Runoff water
Topographic form
Persistence
Weather
Hydrology
Terrace
First order
Conservation tillage
Spermatophyta
Infiltration
Contaminant
Language English
License CC BY 4.0
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PublicationTitle Journal of environmental quality
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American Society of Agronomy
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SAS Institute (e_1_2_10_27_1) 1999
e_1_2_10_18_1
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Logsdon S.D. (e_1_2_10_16_1) 1999; 54
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Prior J.C. (e_1_2_10_22_1) 1991
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SSID ssj0012076
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Snippet Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25 yr...
ABSTRACT Agricultural tillage influences runoff and infiltration, but consequent effects on watershed hydrology are poorly documented. This study evaluated 25...
Data from four small watersheds near Treynor, IA, were used to explore the influence of agricultural practices on flow regimes of headwater streams. Between...
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wiley
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StartPage 1547
SubjectTerms Agricultural management
Agricultural practices
Agricultural runoff
Agriculture - methods
Agronomy. Soil science and plant productions
Applied sciences
Base flow
Biological and medical sciences
Biotechnology
Chemical Precipitation
Conservation
Conservation of Natural Resources - methods
Conservation practices
conservation tillage
Contaminants
Cropping systems. Cultivation. Soil tillage
Drought
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Environment and pollution
Environmental impact
evapotranspiration
Exact sciences and technology
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Hydrology
Industrial applications and implications. Economical aspects
Iowa
Longitudinal Studies
Models, Theoretical
Pollution
Pollution, environment geology
precipitation
regression analysis
Rivers
Runoff
Seasonal variations
Seasons
Soil tillage
statistical models
Stream discharge
stream flow
Streams
temporal variation
Terraces
Tillage
Tillage. Tending. Growth control
Water conservation
Water Movements
Watersheds
Title Agricultural practices influence flow regimes of headwater streams in western Iowa
URI https://onlinelibrary.wiley.com/doi/abs/10.2134%2Fjeq2004.0199
https://www.ncbi.nlm.nih.gov/pubmed/16091607
https://www.proquest.com/docview/197372811
https://search.proquest.com/docview/14750254
https://search.proquest.com/docview/68463523
Volume 34
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