Summary
1. While much attention has been paid to the ecology of macro‐invertebrates in flowing water, the microbial ecology of such systems has been largely ignored and our knowledge of heterotrophic slimes in particular remains far from complete. Slime‐forming organisms are ubiquitous in their distribution and are part of the normal riverine flora. Slime outbreaks occur in all types of organically enriched flowing fresh waters, regardless of their chemical nature. Slimes are predominantly of heterotrophs which require a constant supply of (i) a suitable carbon source, (ii) inorganic nutrients and in particular nitrogen and phosphorous, and possibly (iii) growth factors such as vitamins. Phosphorous is not a limiting factor for growth, with slimes developing in rivers with < 0·02 mg P l‐1. Other inorganic nutrients such as nitrogen can be used in various forms and are usually present in adequate amounts, even in unpolluted streams. Therefore occurrence appears to be most closely correlated with the presence of a source of available carbon.
2. The severity of outbreaks are not closely associated with soluble organic carbon content although there is a tendency for heavy growths to occur more frequently in more severely polluted waters. Low‐molecular‐weight sugars are clearly the causative agents of Sphaerotilus natans dominated slimes with higher molecular weight material such as starches not immediately effective as growth promoters. Mono‐ to penta‐saccharides are mainly used by bacterial slimes while fungal components utilize fatty acids up to C8. It is not possible to adopt a nationwide BOD5 standards to control slime outbreaks as even small increases in river BOD5 (< 1·0 mg l‐1) can support slime growth. There is a need to develop new methods of assessing the slime‐promoting capability of effluents such as measuring the readily degradable low‐molecular‐weight carbon compounds, so that threshold concentrations of soluble organic carbon below which slime will not develop can be determined.
3. The effect of effluent enrichment on slime growth diminishes downstream as there is a tendency for the soluble carbohydrate to mix and dilute. The slime also metabolizes the carbohydrate, reducing the concentration by up to 60 % depending on the stage of slime development, thus limiting its own proliferation. This is the typical pattern of self‐purification in flowing waters.
4. The taxonomy of all the slime‐forming species are poorly understood as is the ecology of slimes. Species composition of slimes vary temporally and spatially within individual rivers. The primary factors affecting composition are nutrient type and water velocity, although pH determines whether a slime is either predominantly fungal or bacterial. The rate of transfer of oxygen and nutrients is dependent on water velocity with zoogloeal forms predominating as velocity falls to < 0·05 m s‐1. More details of the effects of water velocity and other environmental factors on all the slime‐forming organisms is required.
5. The effects of specific environmenta...