Modeling Runoff and Sediment Yield from a Terraced Watershed Using WEPP

Modeling Runoff and Sediment Yield from a Terraced Watershed Using WEPP
Author: Mary Carla McCullough
Publisher:
Total Pages: 12
Release: 2008
Genre:
ISBN:

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The watershed version of WEPP (Water Erosion Prediction Project) was used to estimate 50-year runoff and sediment yields for a 291 ha watershed in eastern Nebraska that is 90% terraced and which has no historical gage data. The watershed has a complex matrix of elements, including terraced and non-terraced subwatersheds, multiple combinations of soils and land management, a grassed-waterway network, and natural stream channels leading to the outlet. The objectives of this study were to model the study watershed using WEPP and to evaluate model results compared to literature values. WEPP estimated the sediment yield to be 1.9 T/ha/yr, the sediment delivery ratio to be 0.22 and the percent of sediment contribution from the main channel to be 31% of the total sediment yield. These results are consistent with values reported in the literature.

Study of Sediment Transport Mechanisms in Agricultural Watersheds

Study of Sediment Transport Mechanisms in Agricultural Watersheds
Author:
Publisher:
Total Pages: 0
Release: 2015
Genre:
ISBN:

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This study was conducted to improve understanding and prediction of sediment delivery through agricultural watersheds, with emphasis on the pathways from edge-of-field to receiving waters. The study was focused on agricultural watersheds within the University of Wisconsin (UW) - Platteville Pioneer Farm and one of the UW Discovery Farms located in southwestern Wisconsin. Artificial neural network (ANN) models were developed to predict runoff and sediment yield from agricultural watersheds that employ best management practices (BMPs). Results showed that input parameters representing BMPs were important for accurately simulating runoff and sediment yield from these watersheds. The study also showed that ANN models were able to successfully simulate runoff and sediment yield during training, validation and testing phases. Sediment eroded from upland source areas is often carried to the watershed outlet via grassed waterways. Critical shear stress of the soil is often estimated to determine the potential for soil to be detached. Previous studies suggest that critical shear stress may vary with antecedent moisture content. The dynamic nature of critical shear stress in an upland agricultural field and grassed waterway of a nested watershed was investigated at Pioneer Farm by measuring critical shear stress over a range of antecedent soil moisture conditions. Results showed that critical shear stress in both the grassed waterway and the agricultural field increased as soil moisture increased until the soil moisture content reached the plastic limit. Above the plastic limit, critical shear stress of the soil decreased significantly and was relatively constant, ultimately rendering the soil more susceptible to erosion. Finally, the process-based Water Erosion Prediction Project (WEPP) model was used to develop regressions equations that use channel, watershed and storm characteristics to estimate sediment delivery ratios (SDRs) for grassed waterways draining upland agricultural fields. Upland agricultural management scenarios considered included: (i) corn-oat-alfalfa crop rotation, chisel plow tillage, and terraces, and (ii) corn-oat-alfalfa crop rotation, chisel plow tillage, and no-terraces. Better R2 values resulted from equations developed for non-terraced fields compared to terraced fields suggested that channel and storm parameters were better able to explain the variation in SDR for grassed waterways draining from non-terraced fields.

Modeling Best Management Practices in a Small Watershed Using Process Based Modeling Approaches and GIS

Modeling Best Management Practices in a Small Watershed Using Process Based Modeling Approaches and GIS
Author: Taesoo Lee
Publisher:
Total Pages: 186
Release: 2008
Genre:
ISBN:

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Soil erosion is a problem that causes both the loss of valuable soil and water quality degradation by sediment and attached nutrients and pollutants. Soil loss and sediment discharge to waterbodies can be prevented and mitigated by best management practices (BMPs). The USDA-NRCS reported that BMPs such as filter strips and grassed waterways can reduce up to 50 to 70% of the runoff and sediment leaving agricultural land. This study includes measured data analyses and representation of BMPs such as row cropping, filter strips and grassed waterways in a small experimental watershed (2.09 ha) at Nelson Farm, MS. Row cropping was conducted throughout a study period from 1990 to 1995 (6 years). Filter strips and grassed waterways were implemented in October 1991 and August 1994, respectively. A total of three phases were established according to the BMP implementation schedule. Phase 1 started from December 1990 to October 1991 with row cropping only, phase 2 started from October 1991 to August 1994 with row cropping and filter strips, and phase 3 started from September 1994 to December 1995 with row cropping, filter strips, and grassed waterway. The WEPP (Water Erosion Prediction Project) model and its parameters including physically based parameters are used and adjusted for the representation of BMPs. Input data includes weather data measured by the National Sedimentation Laboratory researchers and staff in Oxford, Mississippi. Management, crop yield, and BMP information in previous studies by Dabney and Meyer were used. Watershed characteristics were derived from a 2 foot contour map using GIS. These watershed characteristics were also found in previous studies. The parameter setting for the vegetative practices were calibrated and validated to agree with observed data at the location of the practices in each phase. There are two WEPP projects depending on two different flow paths, one is based on flow along the cropping row and the other is based on flow over the crop rows when the rows are collapsed by large runoff events after tillage. The Soil and Water Assessment Tool (SWAT) was run with the same watershed properties and parameter settings although there were some parameters not available in SWAT. In general, SWAT estimated larger runoff and sediment yields although the difference was small. A possible explanation is that SWAT uses one representative slope, which is a linear slope, while WEPP uses dynamic slope steepness, which includes convex and concave slope shapes. Another reason is that there is no spatial location for filter strips and no representation for the multiple filter strips is possible in SWAT. The BMP impact analyses (using WEPP) estimate the reduction of runoff and sediment yield by each BMP in each phase. The results of these analyses show that row cropping reduced 11.1% of runoff and 15.8% of sediment yield in phase (1) Row cropping and filter strips reduced 14.6% of runoff and 41.9% of sediment yield in phase (2) Row cropping, filter strips, and grassed waterway reduced 20.5% of runoff and 65.7% of sediment yield in phase (3) Total reduction by all BMPs installed according to their schedule during the study period was 14.3% of runoff and 38.5% of sediment yield. Various scenario analyses have been conducted. These include the failure of BMPs, the effectiveness of a combination of BMPs, the long-term impacts of BMPs, and the spatially distributed estimation of the effectiveness of filter strips. BMP failure analysis was conducted for filter strips and grassed waterway in each phase based on the parameter value adjustment by 25%, 50%, 75%, and 100% from the range of possible parameter values. In phase 2, with filter strips, the results of filter strips failure analysis show the reduction of runoff ranges from -4.2% (best) to +0.6% (no function) and that of sediment yield ranges from -29.6% (best) to +14.0% (no function). There would be more runoff and sediment yield generated than observed when the filter strips are not maintained because there is no vegetation on filter strips. In phase 3, with filter strips and a grassed waterway, the results of failure analysis show the reduction of runoff ranges from -2.1% (best) to +12.1% (no function) and that of sediment yield ranges from -14.3% (best) to +138.1% (no function). For the same reason, the runoff and sediment yield were larger in the 'no function' scenario than observed. (Abstract shortened by UMI.).

Predicting Rainfall Erosion Losses

Predicting Rainfall Erosion Losses
Author: Walter H. Wischmeier
Publisher:
Total Pages: 70
Release: 1978
Genre: Agricultural conservation
ISBN:

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The Universal Soil Loss Equation (USLE) enables planners to predict the average rate of soil erosion for each feasible alternative combination of crop system and management practices in association with a specified soil type, rainfall pattern, and topography. When these predicted losses are compared with given soil loss tolerances, they provide specific guidelines for effecting erosion control within specified limits. The equation groups the numerous interrelated physical and management parameters that influence erosion rate under six major factors whose site-specific values can be expressed numerically. A half century of erosion research in many States has supplied information from which at least approximate values of the USLE factors can be obtained for specified farm fields or other small erosion prone areas throughout the United States. Tables and charts presented in this handbook make this information readily available for field use. Significant limitations in the available data are identified.

Watershed Hydrology

Watershed Hydrology
Author: Vijay P. Singh
Publisher: Allied Publishers
Total Pages: 588
Release: 2003
Genre: Groundwater
ISBN: 9788177645477

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Modelling Soil Erosion by Water

Modelling Soil Erosion by Water
Author: John Boardman
Publisher: Springer Science & Business Media
Total Pages: 552
Release: 2013-06-29
Genre: Science
ISBN: 3642589138

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TO THE MODEL EVALUATION 1. MODELLING SOIL EROSION BY WATER l 2 John Boardman and David Favis-Mortlock 1 School of Geography and Environmental Change Unit Mansfield Road University of Oxford Oxford OX1 3TB UK 2 Environmental Change Unit University of Oxford 5 South Parks Road Oxford OX1 3UB UK Introduction This volume is the Proceedings of the NATO Advanced Research Workshop 'Global Change: Modelling Soil Erosion by Water', which was held on II-14th September 1995, at the University of Oxford, UK. The meeting was also one of a series organised by the IGBP 1 GCTE Soil Erosion Network, which is a component of GCTE's Land Degradation Task (3.3.2) (Ingram et aI., 1996; Valentin, this volume). One aim of the GCTE Soil Erosion Network is to evaluate the suitability of existing soil erosion models for predicting the possible impacts of global change upon soil erosion. Due to the wide range of erosion models currently, in use or under development, it was decided to evaluate models in the following sequence Favis-Mortlock et al., 1996): • field-scale water erosion models • catchmenr-scale water erosion models • wind erosion models • models with a landscape-scale and larger focus. As part of this strategy, the first stage of the GCTE validation of field-scale erosion models was carried out at the Oxford NATO-ARW. I A list of Acronyms fonns Appendix A.

Estimating Runoff and Sediment Yield Using Kw-Giuh and Musle Models

Estimating Runoff and Sediment Yield Using Kw-Giuh and Musle Models
Author: Saleh Arekhi
Publisher: LAP Lambert Academic Publishing
Total Pages: 100
Release: 2010-10
Genre:
ISBN: 9783838394411

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In the present study, efforts were made to develop one Kinematic Wave and Geomorphic Instantaneous Unit hydrograph theory based and MUSLE model based rainfall-runoff and sediment yield estimating model for un-gauged/in-adequately gauged micro watersheds. The developed model was tested for its application potential on 3-ecologically diverse micro watersheds in Almora district of Uttaranchal. Proposed model simulated total runoff volumes for three micro watersheds were found to be associated with mean relative errors ranging between 16% to 38%. The developed KW-GIUH-MUSLE model was also tested for its potential to give realistic sediment yield estimates for 11 storms/events in a test micro- watershed. It was observed that these sediment yield estimates were associated with about 6% mean relative error and 0.94 mean DV value. The above analysis could thus clearly show that the developed KW-GIUH-MUSLE model can indeed be utilized for obtaining reasonable surface runoff and sediment yield estimates.