We analyze the TSS distribution over the whole Seine basin (67 500 km(2), s
tream order 8) from: 1. a set of 236 stations sampled quaterly to bimonthly
from the french national water quality monitoring network over the 1971-19
97 period, 2. four stations sampled daily over 3 and 4 years located on str
eam orders 1, 5, 6 and 8, 3. a weekly survey of the exceptional 1994/95 hig
h water stage at 4 stations upstream and downstream of Greater Paris (10 M.
people). Due to very low relief and even rainfall distribution over the ye
ar, the Seine and its river network from order 3 to 8, are characterized by
very low TSS: 79% of medians (C50%) are between 8 and 32 mg l(-1) and maxi
mum TSS barely reach 300 mg l(-1). Due to similar relief distributions, run
off patterns and geology in all sub-basins, major tributaries have near-ide
ntical long-term TSS regimes and seasonal variations during the 1994/95 flo
od stage. Second order TSS variations are linked to lithology: streams drai
ning argillaceous and marl terrains are up to 3 and 4 times more turbid tha
n those draining limestones and chalks. Basin size was also tested: the TSS
range (quantiles C1% to C99%) decreases from order 1 to 8, and quantiles l
evels C10% to C75% double from order 3 to 8. Human impacts on TSS levels ar
e quite limited: Greater Paris influence on longitudinal profiles is not ob
served; in periurban streams, where population density reach 1000 p km(-2),
TSS levels are twice those observed in rural conditions (40 p km(-2)): C75
% are 32 +/- 12 and 17.5 +/- 9 mg l(-1), respectively. In orders 6 to 8, th
e lower TSS quantiles (C10% and C25%) are higher than in orders 3 - 5, this
can be attributed to eutrophication and/or to an important fluvial traffic
. No significant trend was observed on the TSS distributions at the river m
outh from 1971 to 1997. Comparison with a previous daily survey in 1863-186
6 showed present marked decrease of average TSS and TSS yearly range attrib
uted mostly to locks.