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Results of Monitoring at Olkiluoto in 2006 - Environment (pdf) - Posiva

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33fected by precipit<strong>at</strong>ion and soil temper<strong>at</strong>ure. The <strong>in</strong>crease <strong>at</strong> depths <strong>of</strong> 10, 20 and 30 cm<strong>in</strong> <strong>2006</strong> on FIP4 may be rel<strong>at</strong>ed to the rel<strong>at</strong>ively dry, hot summer.160140120DOC, mg/l100806020042005<strong>2006</strong>Ref. 1998-2000402005 10 20 30 40Depth, cmFigure 24. DOC <strong>in</strong> soil solution on FIP4 <strong>in</strong> 2004-<strong>2006</strong> and on the reference site <strong>in</strong>Tammela <strong>in</strong> 1998-2000. Note th<strong>at</strong> the reference d<strong>at</strong>a has been collected from depths 5,20 and 40 cm, while FIP4 d<strong>at</strong>a is from depths 5, 10, 20 and 30 cm.140120100DOC, mg/l80602005<strong>2006</strong>Ref. 1998-2000402005 20 30 40De pth, cmFigure 25. DOC <strong>in</strong> soil solution on FIP10 <strong>in</strong> 2005-<strong>2006</strong> and on the reference site <strong>in</strong>Tammela <strong>in</strong> 1998-2000. Note th<strong>at</strong> the reference d<strong>at</strong>a has been collected from depths 5,20 and 40 cm, while FIP10 d<strong>at</strong>a is from depths 5, 10, 20 and 30 cm.

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