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Identifying Riparian Sinks for Watershed Nitrate using Soil Surveys

A. E. Rosenblatta, A. J. Gold*,a, M. H. Stolta, P. M. Groffmanb and D. Q. Kellogga

a Dep. of Natural Resources Science, 210B Woodward Hall, Univ. of Rhode Island, Kingston, RI 02881
b Institute of Ecosystem Studies, Box AB, Millbrook, NY 12545



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  		Fig. 1. Plan view of a site layout. Each site consisted of a left and right bank, determined from the direction of stream flow. Each bank contained three transects, 7.5 m apart and 30 m long. The three transects extended parallel to one another and perpendicular to the stream, beginning at the top of the stream bank.

 


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  		Fig. 2. Average width of very poorly drained (VPD) and poorly drained (PD) soils along lower-order streams in different hydrogeomorphic classes at 100 randomly selected sites in the Pawcatuck River Watershed, Rhode Island.

 


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  		Fig. 3. Comparison of riparian areas with high ground water nitrate removal capacity using different spatial databases on an identical fourth-order stream network within the Pawcatuck Watershed of Rhode Island. High ground water nitrate removal capacity riparian areas consist of soil map units classified as either outwash–hydric or organic/alluvium.

 




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The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education		 Soil Science Society of America Journal
Copyright © 2001 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.