USGS

 

U.S. GEOLOGICAL SURVEY

Water-Resources Investigations Report 03-4124


Development, Calibration, and Analysis of a Hydrologic and Water-Quality Model of the Delaware Inland Bays Watershed

By Angélica L. Gutiérrez-Magness and Jeff P. Raffensperger

 

This report is available as a pdf.

 

ABSTRACT

Excessive nutrients and sediment are among the most significant environmental stressors in the Delaware Inland Bays (Rehoboth, Indian River, and Little Assawoman Bays). Sources of nutrients, sediment, and other contaminants within the Inland Bays watershed include point-source discharges from industries and wastewater-treatment plants, runoff and infiltration to ground water from agricultural fields and poultry operations, effluent from on-site wastewater disposal systems, and atmospheric deposition. To determine the most effective restoration methods for the Inland Bays, it is necessary to understand the relative distribution and contribution of each of the possible sources of nutrients, sediment, and other contaminants.

A cooperative study involving the Delaware Department of Natural Resources and Environmental Control, the Delaware Geological Survey, and the U.S. Geological Survey was initiated in 2000 to develop a hydrologic and water-quality model of the Delaware Inland Bays watershed that can be used as a water-resources planning and management tool. The model code Hydrological Simulation Program - FORTRAN (HSPF) was used. The 719-square-kilometer watershed was divided into 45 model segments, and the model was calibrated using streamflow and water-quality data for January 1999 through April 2000 from six U.S. Geological Survey stream-gaging stations within the watershed. Calibration for some parameters was accomplished using PEST, a model-independent parameter estimator. Model parameters were adjusted systematically so that the discrepancies between the simulated values and the corresponding observations were minimized.

Modeling results indicate that soil and aquifer permeability, ditching, dominant land-use class, and land-use practices affect the amount of runoff, the mechanism or flow path (surface flow, interflow, or base flow), and the loads of sediment and nutrients. In general, the edge-of-stream total suspended solids yields in the Inland Bays watershed are low in comparison to yields reported for the Eastern Shore from the Chesapeake Bay watershed model. The flatness of the terrain and the low annual surface runoff are important factors in determining the amount of detached sediment from the land that is delivered to streams. The highest total suspended solids yields were found in the southern part of the watershed, associated with high total streamflow and a high surface runoff component, and related to soil and aquifer permeability and land use. Nutrient yields from watershed model segments in the southern part of the Inland Bays watershed were the highest of all calibrated segments, due to high runoff and the substantial amount of available organic fertilizer (animal waste), which results in over-application of organic fertilizer to crops.

Time series of simulated hourly total nitrogen concentrations and observed instantaneous values indicate a seasonal pattern, with the lowest values occurring during the summer and the highest during the winter months. Total phosphorus and total suspended solids concentrations are somewhat less seasonal. During storm events, total nitrogen concentrations tend to be diluted and total phosphorus concentrations tend to rise sharply. Nitrogen is transported mainly in the aqueous phase and primarily through ground water, whereas phosphorus is strongly associated with sediment, which washes off during precipitation events.

 

TABLE OF CONTENTS

Abstract

Introduction

Purpose and scope

Previous investigations

Acknowledgments

Description of the study area

Climate

Hydrology, soils, and topography

Water use

Model development

Overview of the hydrological simulation program - FORTRAN (HSPF)

Model assumptions

Watershed segmentation

Land use

Development of nutrient application rates

Animal counts, animal units, and the manure land-use category

Organic fertilizer calculations

Nutrient requirements and goal yields

Total nutrient applications

Method of fertilizer application

Schedule of organic fertilizer application

Schedule of mineral fertilizer application

Planting and harvesting dates

Atmospheric deposition

On-site wastewater disposal system information

Point sources

Meteorological data

Development of water-quality data base for model calibration

Model calibration approach

Calibration of hydrology

Parameter estimation

Objective function for parameter estimation

Calibration of total suspended solids and nutrients

Analysis of model calibration and results

Calibration of hydrology

Annual and monthly water balance

Mean daily streamflow time series

Calibration of total suspended solids

Annual edge-of-stream yields

Hourly concentration time series

Calibration of nutrients

Annual edge-of-stream yields

Hourly concentration time series

Summary and conclusions

References cited


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For more information about USGS activities in Maryland, Delaware and the District of Columbia contact:

 

Director
U.S. Geological Survey
Maryland, Delaware, D.C. Water Science Center
8987 Yellow Brick Road
Baltimore, MD 21237
Telephone: (410) 238-4200
Fax: (410) 238-4210

 

or access the USGS Water Resources of Maryland, Delaware, and District of Columbia home page at:  http://md.water.usgs.gov/.




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