I agree with Francesca conceptually. If the whole run of 1000 feet is 10:1 there's not much you can claim there. However, it really varies by what state you're in as far as what you can claim.
In Georgia for instance, you can get credits for sheet flow through a stream buffer, which can counterbalance the water quality requirement, so it's effectively treated as a TSS reduction in the calculation. How much you can claim is set rather arbitrarily in the Georgia Stormwater Management Manual. You can also claim "overland flow filtration" credits if the overland flow is flat enough. From memory I think the limit is down around 2%, not 10%, and I think you have to be discharging as sheet flow.
I don't know that those credits are based on any real science, they're just set out there as an encouragement for "better site design practice," and that's just Georgia. In North Carolina, for instance, you could put a level spreader and filter strip somewhere between you and the creek and gain credits, and you could utilize some of the stream buffer as credits as well if you design it properly. They're all different.
Of course, the truth of the matter is that TSS doesn't come from pavement anyway, it comes from stream morphology changes due to the urbanization of the watershed, but state EPDs jumped the shark a long time ago on that one. It's much easier to plug your fingers in your ears and pretend correlation = causality when the EPA is breathing down your neck, than it is to try and model increases in sediment transport due to stream morphology in your TMDLs.
Hydrology, Drainage Analysis, Flood Studies, and Complex Stormwater Litigation for Atlanta and the South East -