The distribution of treated water of good quality can generate in many case
s the formation of unwanted loose deposits in the reservoirs and pipework o
f distribution systems. The approach used in this study seeks to characteri
ze the organic component of deposits in a large distribution system, since
organic matter is a key factor in controlling the biostability of water and
has not previously been described with relation to these deposits. Deposit
s were found to contain a variable, but minority fraction of organic matter
: less than 11% as organic carbon, 1.1% as nitrogen, or 28% as volatile sol
ids, but the corresponding concentrations were much higher (g l(-1)) than t
hose found in circulating water (mg l(-1)). The same ratio applies to bacte
rial counts. Proportions of C-organic and N were linked through a linear re
lationship, which results in a consistent C/N ratio close to 7 irrespective
of the quantity of or ganic matter in the sediment. This low C/N value sug
gests that the in situ biological activity has a strong influence on the C
and N fractions. This is confirmed by (i) the high heterotrophic plate coun
ts (HPC) in the deposits (up to 5.8 x 10(8) CFU 14 d g(-1) of dry matter);
(ii) the observation of a mature trophic chain in most samples resulting in
the presence of macro-organisms (Asellus, Gasteropodae), in some cases, an
d (iii) positive correlations between the organic matter fractions (as C-or
ganic and N) and the HPC. No relationship was found between the organic cha
racteristics of deposits and upstream/downstream locations in the system. T
he deposits appear to contain a reserve of organic matter capable of suppor
ting the development of bacteria as well as bacterial predators, which is l
ikely to provide favourable conditions for the contamination of water carri
ed by the distribution system. Chlorine demand of loose deposits was high a
nd would be predicted from nitrogen content, but inactivation of bacteria a
ssociated with resuspended deposits appears unfeasible with current disinfe
ction practices due to oxidant reduction resulting from deposit resuspensio
n. (C) 1999 Elsevier Science Ltd. All rights reserved.