Abstract

ABSTRACT Many inland waters are enriched with nutrients, causing deleterious effects to their ecology and the benefits they provide for society, but their effective management first requires identification of the nutrient(s) that limit algal production. Concentrations of nutrients and chlorophyll a (Chl-a) were used to assess nutrient limitation seasonally at 17 meres over 2 time periods: historic (2005–2009; 1995–1998 at one site) and contemporary (2014–2018). Different approaches were used to assess nutrient limitation because they reflect different aspects of nutrient availability and their conversion into biomass. In the historic period, 3 meres were phosphorus (P) limited, 3 nitrogen (N) limited, 5 co-limited; the remaining 6 meres were not nutrient limited. For this period, ecological status assessed using phytoplankton Chl-a was only at good or high ecological status (sensu the Water Framework Directive) at 2 sites. The contemporary period was slightly improved, with 4 sites at good status. At the sites that failed to meet good ecological status, the required reduction in P concentration was least in P-limited sites and, conversely, the reduction in N was least in N-limited sites, suggesting that remediation by nutrient reduction would be most efficient if it was targeted using site-specific information. Even in primarily P-limited sites, once input of P has been reduced, further ecological benefit of reducing N at targeted sites should be explored.

Highlights

  • Lakes are highly connected systems impacted by a range of anthropogenic pressures: locally from inputs of material from the catchment; regionally from atmospheric deposition of acids, nitrogen (N), and large-scale weather effects; and globally from climate change (Maberly and Elliott 2012, Richardson et al 2018)

  • Early large-scale comparisons across temperate lakes found broad relationships between phytoplankton biomass, commonly expressed as the concentration of the ubiquitous photosynthetic pigment chlorophyll a (Chl-a), and P expressed as total phosphorus (TP; e.g., Dillon and Rigler 1974, Vollenweider and Kerekes 1980, Vollenweider 1989, Phillips et al 2008)

  • Excluding Oak Mere where the alkalinity is 0.03 mequiv L−1 and Bomere Pool where it is 0.56 mequiv L−1, the water is hard with an overall median alkalinity of 2.45 mequiv L−1

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Summary

Introduction

Lakes are highly connected systems impacted by a range of anthropogenic pressures: locally from inputs of material from the catchment; regionally from atmospheric deposition of acids, nitrogen (N), and large-scale weather effects; and globally from climate change (Maberly and Elliott 2012, Richardson et al 2018). Nutrient enrichment, derived from local point sources and diffuse sources as well as regional atmospheric deposition, has had the longest and largest effect on the ecological structure and function of lakes (Moss et al 2011, Moss 2018, Le Moal et al 2019). The symptoms of this eutrophication include increased growth of planktonic and attached algae, blooms of cyanobacteria, a decline in macrophyte abundance, and deoxygenation at depth during stratification (Moss et al 2011).

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