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Air quality expert group - Fine particulate matter (PM2.5) in ... - Defra

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<strong>PM2.5</strong> <strong>in</strong> the UK<br />

144<br />

53. Modell<strong>in</strong>g results have illustrated how primary <strong>PM2.5</strong> concentrations show<br />

localised peaks <strong>in</strong> urban areas ow<strong>in</strong>g to local sources, superimposed on a<br />

regional background. The sources which cause these peaks are potentially<br />

subject to abatement and the dispersion of these sources are generally well<br />

represented by models, except when close to roads with complex street<br />

geometries. An important limit<strong>in</strong>g factor <strong>in</strong> estimat<strong>in</strong>g concentrations and<br />

human exposure is likely to be uncerta<strong>in</strong>ty <strong>in</strong> the emissions, <strong>in</strong>clud<strong>in</strong>g miss<strong>in</strong>g<br />

sources.<br />

54. The largest contribution to <strong>PM2.5</strong> concentrations overall is secondary <strong>in</strong>organic<br />

aerosol (SIA). Secondary <strong>in</strong>organic aerosol contributions are more smoothly<br />

vary<strong>in</strong>g, result<strong>in</strong>g from advection on a range of scales up to cont<strong>in</strong>ental and<br />

illustrated by higher average concentrations <strong>in</strong> the south-east graduat<strong>in</strong>g to<br />

much lower values over Scotland. Nitrate is the largest component of SIA over<br />

the UK, and also the most spatially variable <strong>in</strong> space and time, depend<strong>in</strong>g as it<br />

does on the variability of ammonia emissions and concentrations. More detailed<br />

research is required to <strong>in</strong>vestigate the effect of temporal variations <strong>in</strong> emissions,<br />

especially of ammonia, and expla<strong>in</strong> the seasonal variation and the higher nitrate<br />

levels observed <strong>in</strong> w<strong>in</strong>ter. Sulphate now makes a smaller contribution to <strong>PM2.5</strong><br />

concentrations than nitrate ow<strong>in</strong>g to major reductions <strong>in</strong> sulphur emissions <strong>in</strong><br />

the UK and <strong>in</strong> other countries and from shipp<strong>in</strong>g.<br />

55. The ratio of urban <strong>in</strong>crement to regional background po<strong>in</strong>ts to future directions<br />

for <strong>PM2.5</strong> control. Control strategies should be considered for the regional<br />

background where secondary <strong>in</strong>organic aerosol is by far the largest component<br />

accord<strong>in</strong>g to models. It is also worth not<strong>in</strong>g that given the exposure reduction<br />

targets outl<strong>in</strong>ed <strong>in</strong> Chapter 1, the removal of the whole of the urban <strong>in</strong>crement<br />

would be required to satisfy them if noth<strong>in</strong>g is done to address the regional<br />

background.<br />

56. Source apportionment from modell<strong>in</strong>g shows how further reductions <strong>in</strong> SIA<br />

depend on the control of emissions of SO2, NOx and NH3 <strong>in</strong> other countries,<br />

and from shipp<strong>in</strong>g more generally, as well as <strong>in</strong> the UK. Scenario analysis<br />

shows dependence on future emission ceil<strong>in</strong>gs <strong>in</strong> the EU-27 countries and also<br />

the modelled reduction of sulphate result<strong>in</strong>g from the MARPOL agreement<br />

of the International Maritime Organization (IMO), counteracted by enhanced<br />

nitrate due to <strong>in</strong>creas<strong>in</strong>g shipp<strong>in</strong>g emissions of NOx. Modell<strong>in</strong>g <strong>in</strong>dicates a<br />

complex non-l<strong>in</strong>ear response of SIA concentrations to reductions <strong>in</strong> precursor<br />

emissions due to chemical <strong>in</strong>teractions between pollutants, <strong>in</strong> particular the<br />

high dependence on the availability of NH3 and the reversible and temperaturedependent<br />

formation of ammonium nitrate. This needs to be borne <strong>in</strong> m<strong>in</strong>d<br />

when consider<strong>in</strong>g the effectiveness of further SO2 and NOx reductions, whilst<br />

emissions of NH3 have rema<strong>in</strong>ed more constant.<br />

57. Modell<strong>in</strong>g of the smaller secondary organic aerosol (SOA) component is<br />

far more uncerta<strong>in</strong> and speculative than for SIA, both <strong>in</strong> terms of precursor<br />

emissions (see Chapter 4) and chemical processes, and further work is required<br />

<strong>in</strong> this area. However, it is more difficult to control SOA and its precursors, of<br />

which biogenic emissions are a large component. It is worth not<strong>in</strong>g that the<br />

oxidants for biogenic VOC precursors, namely hydroxyl ions (OH - ), ozone (O3)<br />

and NO3 - , are all controlled by atmospheric chemistry, and will respond to<br />

further reductions <strong>in</strong> carbon monoxide (CO), SO2, NOx and VOC emissions. It is

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