USGS North Carolina Water Science Center

Map of North Carolina highlighting the project study area

Map of study area and data collection sites

Project Summary

Full Title
Artificial Drainage

Location
Middle Swamp watershed of the Little Contentnea Creek subbasin

Cooperating Agencies
NCDENR, Division of Water Quality, Groundwater Section

Project Chief
Stephen Harden

Period of Project
2000 - 2001

Photo Index

Team Members

Tim Spruill

Artificial Drainage

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photo of drainage ditch in an agricultural field
Agricultural field with drainage improvement

Background

In North Carolina, about 40 percent of the cropland requires drainage improvements to increase agricultural production in poorly drained soils. A common practice for improving drainage is to install ditches (Pictures 1, 2) and subsurface tile drains (Pictures 3, 4) to lower the water table beneath agricultural fields. These drainage improvements increase the amount of land available for cultivation; however, the process of redirecting shallow ground water beneath agricultural fields through tile drains to ditches can alter the quality of drainage water exiting the fields to receiving streams. Nitrate-nitrogen (NO3) concentrations ranging from about 5 to 50 milligrams per liter (mg/L) in tile drainage water have been noted in various studies.

In eastern North Carolina, excessive nutrient loadings have contributed to the degradation of surface-water quality in the Neuse River basin. The North Carolina Environmental Management Commission adopted rules in 1997 to reduce nitrogen loads in the Neuse River by 30 percent to support the Neuse River Nutrient Sensitive Waters Management Strategy. For agricultural land, several combinations of best management practices (BMPs), including nutrient management, controlled drainage, forested riparian buffers, and vegetative filter strips, were proposed for reducing nutrient loads. Because tile drains and ditches are constructed channels that artificially intercept the water table, they can allow ground water containing agricultural chemicals beneath cultivated fields to bypass natural streamside buffers and organic carbon-rich streambeds that normally would reduce NO3 in the ground water before it discharges to streams. Subsurface tile drains are considered a major pathway for NO3 transport to surface water in some agricultural watersheds.

photo, agricultural drainage ditch
Picture 1
photo, agricultural drainage ditch
Picture 2
photo, tile drain
Picture 3
photo, tile drain
Picture 4
Ditches Tile Drains
Click on photo for an larger image
Additional photos available in the Photo Index

Objectives

This study was conducted to characterize the quality of drainage water in tile drains and ditches with respect to different agricultural settings in a low-gradient, organic rich, coastal plain watershed. Information obtained from this study is intended to provide a better understanding of the effects of land-management practices on nutrient loadings associated with artificially drained farmland and to assist water-resource managers in determining priorities for effective management of nutrient-reduction strategies.

Approach

The study area is in the Middle Swamp watershed of the Neuse River basin in the North Carolina Coastal Plain (fig. 1). Discharge measurements and water-quality samples were collected at study sites (table 1) from August 2000 to August 2001 to evaluate water-quality conditions in relation to different nitrogen fertilization practices used in the study area. Agricultural fields with existing ditches and(or) tile drains and in which different sources of nitrogen fertilizer were applied to row crops were selected for study. The three types of fertilizer applied to study sites include commercial inorganic fertilizer, sprayed swine-lagoon effluent, and wastewater-treatment plant sludge.

Discharge measurements at tile-drain outlets were determined primarily by using volumetric methods (Pictures 5, 6). In some cases, the tile pipes were modified to permit the use of velocity meters to obtain discharge data (Picture 7). Discharge measurements at ditch sites also were determined by using a velocity meter. Water-quality samples were collected from ditches and tile drains (Pictures 8, 9) and analyzed for nutrients, anions, and cations.

photo, volumetric technique
Picture 5
photo, volumetric technique
Picture 6
photo, velocity technique
Picture 7
photo, water quality sampling
Picture 8
photo, water quality sampling
Picture 9
Volumetric methods Velocity meter Water quality
Click on photo for an larger image

Progress (January 2004)

The final report for this investigation has been completed and submitted to a journal for peer review.

Map showing location of Middle Swamp watershed in North Carolina
Figure 1. Location of Middle Swamp watershed in the Neuse River basin, North Carolina.

Table 1. Tile and ditch sampling sites in streams of the Middle Swamp watershed.
Sample Site USGS Station Number Site Type Fertilizer Source
Sandy Run
SR1-T1 353408077410601 Tile Swine-lagoon effluent
SR1-D1 0209171725 Ditch Swine-lagoon effluent
SR2-T1 353407077411801 Tile Commercial
SR2-D1 02091717 Ditch Commercial
SR3-T1 353220077392401 Tile Commercial
SR3-D1 353212077392801 Ditch Commercial
SR4-T1 353107077383001 Tile Swine-lagoon effluent
SR5-T1 353111077334901 Tile Swine-lagoon effluent
Middle Swamp
MS1-T1 353343077354901 Tile Commercial
MS1-D1 0209171225 Ditch Commercial
MS2-T1 353351077342001 Tile Commercial
MS2-D1 353356077342901 Ditch Commercial
MS2-T2 353354077343401 Tile Commercial
MS3-T1 353308077340301 Tile Treatment plant sludge
MS4-T1 353110077330901 Tile Commercial
MS4-D1 353111077330501 Ditch Commercial
MS4-T2 353125077332501 Tile Swine-lagoon effluent
MS4-D2 02091734 Ditch Swine-lagoon effluent

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SR1-T1 SR1-D1 SR2-T1 SR2-D1 SR3-T1 SR3-D1 SR4-T1 SR5-T1 MS1-T1 MS1-D1 MS2-T1 MS2-T2 MS2-D1 MS3-T1 MS4-T1 MS4-T2 MS4-D1 MS4-D2 02191736