Abstract

Abstract. Accurate reservoir budgets are important for understanding regional fluxes of sediment and nutrients. Here we present a comprehensive budget of sediment (based on total suspended solids, TSS), total nitrogen (TN) and total phosphorus (TP) for two subtropical reservoirs on rivers with highly intermittent flow regimes. The budget is completed from July 1997 to June 2011 on the Somerset and Wivenhoe reservoirs in southeast Queensland, Australia, using a combination of monitoring data and catchment model predictions. A major flood in January 2011 accounted for more than half of the water entering and leaving both reservoirs in that year, and approximately 30 % of water delivered to and released from Wivenhoe over the 14-year study period. The flood accounted for an even larger proportion of total TSS and nutrient loads: in Wivenhoe more than one-third of TSS inputs and two-thirds of TSS outputs between 1997 and 2011 occurred during January 2011. During non-flood years, mean historical concentrations provided reasonable estimates of TSS and nutrient loads leaving the reservoirs. Calculating loads from historical mean TSS and TP concentrations during January 2011, however, would have substantially underestimated outputs over the entire study period, by up to a factor of 10. The results have important implications for sediment and nutrient budgets in catchments with highly episodic flow. First, quantifying inputs and outputs during major floods is essential for producing reliable long-term budgets. Second, sediment and nutrient budgets are dynamic, not static. Characterizing uncertainty and variability is therefore just as important for meaningful reservoir budgets as accurate quantification of loads.

Highlights

  • Over the past century, human activities have caused unprecedented changes in water, sediment and nutrient movement between the atmosphere, lithosphere, hydrosphere and biosphere (Rockström et al, 2009)

  • The biggest effect of the flood year was on output of total suspended solids (TSS), which was 30–50 times higher in the flood year than on average during the non-flood years

  • Wivenhoe inflows were impacted: whereas the input of water, sediment and nutrient to both reservoirs was very similar during non-flood years, inputs to Wivenhoe were more than double those to Somerset during the flood year (Table 1)

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Summary

Introduction

Human activities have caused unprecedented changes in water, sediment and nutrient movement between the atmosphere, lithosphere, hydrosphere and biosphere (Rockström et al, 2009). Modification of these natural biogeochemical cycles on a range of scales has the potential to alter fundamental Earth system processes and undermine the ecosystem services on which human societies depend (Vörösmarty and Sahagian, 2000; Steffen et al, 2015). Artificial fixation of atmospheric nitrogen by humans exceeds fixation rates by all natural processes combined, contributing to a range of environmental problems including acidification, eutrophication and climate change (Gruber and Galloway, 2008; de Vries et al, 2013). Reservoirs have a major impact on nutrient and sediment budgets due to their high residence times and burial

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