“…Water velocities (e.g., Biggs, 1995) and suspended sediment loads (Hicks & Griffiths, 1992;Hicks et al, 2000) were within the wide ranges observed during floods in New Zealand rivers. Our suspended sediment loads were similar to those observed during a managed reservoir release ($4000 mg l )1 , Robinson et al, 2004) and after low impact timber harvesting ($800 mg l )1 , Stott et al, 2001), but were considerably less than suspended sediment loads associated with use of earth moving equipment for timber harvest or heavy construction (up to 30,000 mg L )1 , Hicks & Griffiths, 1992). Our experimental sediments were New Zealand river sands (84% between 63 and 500 lm).…”