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Climate Change and the European Water Dimension - Agri ...

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Figure VI.F.4. Maximum Reservoir Capacity (MRC) for PCB-28, January (A) <strong>and</strong> July (B).<br />

Different scales are used in <strong>the</strong> two predictions.<br />

⎡<br />

0.<br />

2RT<br />

⎤ d<br />

MRC =<br />

foc<br />

KOA<br />

⎢<br />

0. 246 × ρ × × + ×<br />

⎣<br />

H ⎥<br />

⎦ AML<br />

where R is <strong>the</strong> gas law constant, T is <strong>the</strong> absolute temperature, foc is <strong>the</strong> fraction of<br />

organic carbon in <strong>the</strong> soil, ρ is <strong>the</strong> soil density (kg/l), H is <strong>the</strong> dimensionless Henry’s<br />

law constant, d is <strong>the</strong> active soil depth (here 1 mm was considered), AML is <strong>the</strong> air<br />

mixing layer (1000 m).<br />

216

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