Abstract

A national river water quality database of total reactive phosphorus (TRP) and total phosphorus (TP) and flow was used, together with catchment characteristic datasets (soils, land use and hydroclimatic properties), to derive national fluvial phosphorus (P) flux estimates for Great Britain (England, Wales and Scotland) from 1974 to 2012. These fluvial P fluxes were compared with P imports and exports, in fertilizer, food, feedstuffs, and industrial products, along with coastal direct discharge of wastes, at the British national boundary from 1990 to 2012. The results showed that: (i) Average annual river TP concentrations in Great Britain have declined from a peak of 0.27–0.1 mg P/l and annual river TP flux has declined from 120 to 16 ktonnes P/year (0.49–0.06 tonnes P/km2/year); (ii) Average river TRP concentration has declined from a peak of 0.19–0.05 mg P/l and annual river TRP flux has declined from 71 to 10 ktonnes P/year (0.29–0.05 tonnes P/km2); (iii) Over the period 2003–2012, even after the introduction of the Urban Waste Water Directive, 60 % of UK’s TP flux was still from urban areas; and (iv) In 1990, the fluvial flux of TP from the UK was equivalent to 41 % of imports; by 2012 this had decreased to 15 %. The UK (relative to its boundary) continues to accumulate P and, over the last 15 years, this accumulation has increased at an average rate of 0.6 ktonnes P/year2. Enhanced removal of P in waste water treatment has shifted the environmental pathway of sewage P from discharge to rivers to accumulation in sewage sludge, which is largely disposed of on agricultural land, and which could eventually provide a sustained legacy source of P to rivers for decades. However, a substantial proportion of P accumulation is via food waste into landfills.

Highlights

  • Phosphorus (P) is an essential element for food and biofuel production, which cannot be substituted by any other chemical element, and is a non-renewable geological resource (Elser and Bennett 2011)

  • It was possible to assess the ratio of TRP to TP in 40,880 cases; the median value of this ratio was 0.73 with the 5th to 95th percentile as 0.17 to 1; these results show that a median of 73 % of total phosphorus was reactive phosphorus

  • Time series of fluvial P fluxes to the national coastal boundary of the UK were calculated for 38 years (1974–2012)

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Summary

Introduction

Phosphorus (P) is an essential element for food and biofuel production, which cannot be substituted by any other chemical element, and is a non-renewable geological resource (Elser and Bennett 2011). As a result of the availability of cheap P fertilisers, P usage along food production, consumption and waste management chains have become increasingly inefficient and dissipative (Jarvie et al 2013a, b). Reliance on imports of vital P resources risks exposure to commodity market volatilities (Elser et al 2014), and the UK’s national food and water security will become increasingly dependent on its ability to manage P more sustainably (Jarvie et al 2015). Haygarth et al (2014) proposed that the only way to understand whether P legacy was and would alter P concentrations and fluxes in surface waters a full P budget would be required. Powers et al (2016) demonstrated that for two large river basins (Thames, UK, and Maumee, USA) that during the 1990s the net exports from the catchments exceeded the inputs suggesting that both basins were relying on legacy stores of P

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