Tuesday, 8 November 2005
12

Accounting Method for Tracking Changes in Agricultural Phosphorus Entering theTar-Pamlico River Basin, North Carolina.

Amy Johnson1, Deanna Osmond1, R.W. Gannon2, David H. Hardy3, and L. Price4. (1) North Carolina State University, Department of Soil Science, College of Agriculture and Life Sciences, Campus Box 7619, Raleigh, NC 27695-7619, (2) North Carolina Dept. Environment & Natural Resources, 1617 Mail Service Center, Raleigh, NC 27699-1617, (3) NC Dept. of AG & Consumer Serv., 1040 MAIL SERVICE CENTER, Raleigh, NC 27699-1040, (4) USDA Natural Resources Conservation Service, 4405 Bland Street, Suite 205, Raleigh, NC 27609

An estimated 92% of water quality degradation in the Tar-Pamlico River Basin of North Carolina is attributed to nutrient-laden runoff, a large portion of which is contributed by agricultural activities. The Tar-Pamlico Agricultural Rule mandates that agricultural operations in the basin collectively achieve and maintain no net increase in total phosphorus (P) loading over 1991 P levels. In order to accomplish this, the development of a strategy that accounts for P losses and gains from agricultural activities in the basin was required. Quantitative accounting of P loading is not possible due to the complexity of P behavior and transport within a watershed and the lack of data quantifying the various mechanisms of P loss and retention. Therefore, we designed an approach which documents trends in land use and management related to agriculture in the basin. Relative changes in land-use practices that either increase or decrease the risk of P loss were tracked from 1991 to the present. Because of the reliance on historical county-level data, there are many sources of error involved with the data used, most notably the assumption that crops and livestock are uniformly distributed throughout each county. The use of soil test P data is also problematic due to the biased nature in which soil samples are collected by land owners as well as the temporal and spatial variability of soil test P. Relative changes from 1991 to the present were estimated for the following factors: cropland acreage, livestock numbers, manure P content, land uses that reduce the risk of P loss, BMP implementation, as well as soil test P. Results of our approach show either no change or only a slight increase in P inputs to the basin, while the use of conservation practices to prevent P loss greatly increased during the period of interest.

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