Long-term assessment of floodplain reconnection as a stream restoration approach for managing nitrogen in ground and surface waters.

Trends in NO 3 − and TN fluxes from bi-weekly monitoring at Minebank Run Monthly NO 3 − flux estimates showed an increasing trend pre-restoration ( R 2 = 0.2, p = 0.01), and a decreasing trend post-restoration from 2005–2008 ( R 2 = 0.13, p = 0.01; Fig. 13a ), but there was no change in flux post-restoration from 2005–2012 ( R 2 = 0.003, p = 0.26; Fig. 13b ).

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