Australian science has made rapid advances in the last decade in understanding eutrophication processes in inland waters and estuaries. The freshwater research on which these advances are based was triggered by well-publicised blooms of cyanobacteria during the 1980s and early 1990s, particularly a 1000 km long bloom on the Darling River. In estuaries the study which greatly enhanced our understanding but simultaneously served to stimulate further research into estuarine eutrophication, the Port Phillip Bay Study, was initially designed to address perceived problems of toxicants in the Bay but provided profound insights into drivers for, and ecosystem responses to, eutrophication. Subsequent estuarine research has largely been stimulated by management questions arising from Australia’s increasing coastal development for residential purposes. The research has shown that some of the beliefs extant at the time of the blooms were incorrect. For example, it is now clear that stratification and light penetration, not nutrient availability, are the triggers for blooms in the impounded rivers of southeastern Australia, although nutrient exhaustion limits the biomass of blooms. Again, nitrogen seems to play as important a role as phosphorus does in controlling the biomass of these freshwater blooms. The research has also shown that aspects of eutrophication, such as nutrient transport, are dominated by different processes in different parts of Australia. Many of the biophysical processes involved in eutrophication have now been quantified sufficiently for models to be developed of such processes as sediment-nutrient release, stratification, turbidity and algal growth in both freshwater and estuarine systems. In some cases the models are reliable enough for the knowledge gained in particular waterbodies to be applied elsewhere. Thus, there is now a firm scientific foundation for managers to rely upon when managing algal blooms. Whilst these findings have already been presented to managers and communities throughout Australia, there is still a considerable way to go before they are absorbed into their modus operandi.

Eutrophication in Australian rivers, reservoirs and estuaries - a southern hemisphere perspective on the science and its implications

The loss of phosphorous (P) from the landscape is commonly viewed as deleterious for surface water quality. However, the quantities lost and the impact this can have on surface waters depends on numerous mechanisms that occur whilst en route. The aim of this review is to give an outline of these mechanisms and thus how sources of P in the agricultural landscape are connected to the impairment of surface water quality. Processes are dealt with by examining the potential for P loss from the landscape and its availability to aquatic plants during flow overland and subsurface flow and once in streamflow or a lake or reservoir. By examining the connectivity between P loss and the impact on surface water quality, potential mitigation and management of P losses are discussed for various aquatic systems.

Connecting phosphorus loss from agricultural landscapes to surface water quality

Wetlands in many inland catchments are being subjected to increasing salinity. To expand our limited understanding of how increasing salinity will alter carbon and nutrient dynamics in freshwater sediments, we carried out microcosm experiments to examine the acute effects of increasing salinity on the anaerobic cycling of carbon, nutrients (N, P, and S), metals (Fe and Mn), and microbial community structure in sediments from a non-salt-impacted freshwater wetland. Sediments were collected from a wetland on the River Murray floodplain, south eastern Australia and incubated with NaCl concentrations ranging from 0 to 100 mmol L−1. Increasing NaCl concentration led to the immediate release of between about 80 and 190 μmol L−1 ammonium and 235 to 3300 μmol L−1 Fe(II) from the sediments, the amount released ‘increasing with NaCl concentration. Conversely, net phosphate release decreased with increasing NaCl concentration. The overall microbial community structure, determined from phospholipid fatty acid profiles, changed only at the highest NaCl loadings, with evidence of a decrease in microbial diversity. Bacterial community structure, determined by examining terminal restriction fragment length polymorphism (T-RFLP) of the bacterial 16S rRNA gene, showed little response to increasing NaCl concentration. Conversely, the archaeal (methanogen) population, determined by examining T-RFLP of the archaeal 16S rRNA gene, showed significant changes with increasing NaCl loading. This shift corresponded with a significant decrease in methane production from salt-impacted sediments and therefore shows a linkage between microbial community structure and an ecosystem process.

The short-term effects of salinization on anaerobic nutrient cycling and microbial community structure in sediment from a freshwater wetland

This systematic review considers how water quality and aquatic ecology models represent the phosphorus cycle. Although the focus is on phosphorus, many of the observations and discussion points here relate to aquatic ecosystem models in general. The review considers how models compare across domains of application, the degree to which current models are fit for purpose, how to choose between multiple alternative formulations, and how models might be improved. Lake and marine models have been gradually increasing in complexity, with increasing emphasis on inorganic processes and ecosystems. River models have remained simpler, but have been more rigorously assessed. Processes important in less eutrophic systems have often been neglected: these include the biogeochemistry of organic phosphorus, transformations associated with fluxes through soils and sediments, transfer rate-limited phosphorus uptake, and responses of plants to pulsed nutrient inputs. Arguments for and against increasing model complexity, physical and physiological realism are reviewed. Display Omitted The treatment of phosphorus in aquatic models is systematically reviewed.The complexity of lake, river and marine models is increasing over time.Catchment-river models tend to be simpler than lake and marine models.Performance assessment of lake and marine models is generally inadequate.Processes not included in models are discussed.

J. M. Olley

Papers

Pollutant-sediment interactions: sorption, reactivity and transport of phosphorus.