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Redesigning Animal Agriculture

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Quarterly flow weighted mean<br />

nitrate concentration (NO3−N mg l−1 )<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

1930<br />

UK <strong>Agriculture</strong><br />

Act, 1947<br />

Second World<br />

War<br />

1940<br />

illustrated using three long-term data sets<br />

for water bodies in England and Wales in<br />

Figs 11.3 and 11.4. In Fig. 11.3, long-term<br />

trends in nitrate concentrations in the<br />

River Thames at Walton on Thames are<br />

summarized (after Onstad and Blake, 1980;<br />

supplemented with more recent monthly<br />

data from the Environment Agency routine<br />

water quality monitoring programme). Key<br />

change points in the nitrate concentration<br />

trend occurred in conjunction with major<br />

phases of change in the social, economic<br />

and political systems. The first change<br />

point occurred during the Second World<br />

War, when much of the traditional grazing<br />

land was ploughed up, and many marginal<br />

lands were drained and cultivated<br />

in response food shortages and the UK<br />

Government ‘Dig for Victory’ campaign. In<br />

the post-war period, the 1947 <strong>Agriculture</strong><br />

Act was enacted to support Government<br />

policy to develop self-sufficiency in food<br />

production at a time of severe food rationing<br />

following the collapse of food production<br />

and support in the post-war era.<br />

A third change point is apparent when<br />

the UK joined the EU in the early 1970s<br />

and benefited from the economic support<br />

structures introduced under the Common<br />

Agricultural Policy (CAP).<br />

Ecological Restoration Targets 191<br />

EU Common<br />

Agricultural Policy<br />

1950 1960 1970 1980 1990<br />

Data source: Onstad and Blake, 1980;<br />

Environment Agency Data Archive.<br />

Fig. 11.3. Long-term trends in nitrate enrichment in the River Thames, 1930–2000.<br />

2000<br />

In Fig. 11.4, two long-term data sets<br />

collected by the Freshwater Biological<br />

Association at Windermere (now the Centre<br />

for Ecology and Hydrology, Lancaster) are<br />

presented, along with the output from two<br />

models reconstructing the likely P enrichment<br />

history for Windermere and Esthwaite<br />

Water in the English Lake District (after<br />

Bennion et al., 2005). In these it is apparent<br />

that TP concentrations have more than<br />

doubled in both lakes since the mid-19th<br />

century, evident in both the observed P<br />

chemistry data, model simulations of nutrient<br />

export from catchment to lake, and in the<br />

response of the diatom communities in each<br />

lake. Key change points in both lakes can be<br />

tied to the opening of STWs on the shores of<br />

each lake, and the subsequent introduction<br />

of P stripping at these works in the late 20th<br />

century, but underlying these change points<br />

is a general trend of enrichment which is<br />

tied to increased diffuse P export from agricultural<br />

practices in the catchment of each<br />

lake (Bennion et al., 2005).<br />

The nature and extent of diffuse nutrient<br />

enrichment of waters is clearly a problem<br />

for the competent authorities charged<br />

with the implementation of the WFD in each<br />

member state, and will be a particular problem<br />

in those member states with intensive

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