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Research ArticleResearch Section

Riparian buffer width and nitrate removal in a lagoon-effluent irrigated agricultural area

T. A. Smith, D. L. Osmond and J. W. Gilliam
Journal of Soil and Water Conservation September 2006, 61 (5) 273-281;
T. A. Smith
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D. L. Osmond
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J. W. Gilliam
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ABSTRACT:

The ideal buffer width required to maximize water quality benefits while minimizing unnecessary land utilization is difficult to determine. This study examined the effect of increasing buffer width on nitrate (NO3-N) reduction in shallow groundwater in the middle Coastal Plain of North Carolina. The study site was a streamside buffer zone where previous research determined the buffer did not sufficiently reduce NO3-N discharge to stream water. Buffer width was increased from 9 to 30 m (30 to 98 ft) by fencing out cattle and allowing volunteer vegetation to emerge, thus forming a grass and shrub buffer along the newly widened area. Buffer functions were assessed by comparing groundwater NO3-N concentrations from this new system with the same area prior to widening. A significant increase in percent NO3-N reduction was observed in shallow (0.8 to 1.2 m; 2.6 to 4.0 ft) groundwater on the east (34.7 percent to 95.0 percent; p = 0.02) side of stream, most likely due to an increase (p = 0.01) in dissolved organic carbon (C) at this depth. Reduction at the 30-m (98-ft) width in shallow groundwater at the west side of stream was measured at 93.3 percent, although this was not a statistically significant increase from the 9-m (30-ft) width (53.1 percent; p = 0.2). Percent NO3-N reduction was less efficient in deep (2.4 to 4.5 m; 7.9 to 14.5 ft) groundwater, although a significant increase (-37.8 percent to 39.2 percent; p = 0.003) at the east side of stream was observed. Reduction on the west side at this depth significantly decreased (19.5 percent to -5.1 percent; p = 0.05) suggesting that the deeper confining layer along this side of stream allowed groundwater to bypass the zone of high dissolved organic C enhanced by riparian vegetation, thus minimizing the effects of buffer widening in this area. Stream sampling indicated no significant difference in upstream and downstream NO3-N between the two buffer widths (p = 0.61). Although increasing the buffer width did improve reduction in some areas, the severity of the groundwater NO3-N situation at this site was not completely resolved by increasing the buffer width to 30 m (98 ft).

Footnotes

  • Tim A. Smith is a former graduate student in the Department of Soil Science at North Carolina State University in Raleigh, North Carolina. Deanna L. Osmond is a professor and extension leader in the Soil Science Department at North Carolina State University in Raleigh, North Carolina. J. Wendell Gilliam is a William Neal Reynolds emeritus professor at North Carolina State University in Raleigh, North Carolina.

  • Copyright 2006 by the Soil and Water Conservation Society

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Journal of Soil and Water Conservation: 61 (5)
Journal of Soil and Water Conservation
Vol. 61, Issue 5
September/October 2006
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Riparian buffer width and nitrate removal in a lagoon-effluent irrigated agricultural area
T. A. Smith, D. L. Osmond, J. W. Gilliam
Journal of Soil and Water Conservation Sep 2006, 61 (5) 273-281;

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Riparian buffer width and nitrate removal in a lagoon-effluent irrigated agricultural area
T. A. Smith, D. L. Osmond, J. W. Gilliam
Journal of Soil and Water Conservation Sep 2006, 61 (5) 273-281;
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