Phthalates and Nonylphenols in Roskilde Fjord
Phthalates and Nonylphenols in Roskilde Fjord
Phthalates and Nonylphenols in Roskilde Fjord
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The diffusivity of a molecule depends on the r<strong>and</strong>om movements(Brownian motion) which aga<strong>in</strong> is dependant on the k<strong>in</strong>etic (or <strong>in</strong>ternal)energy. The k<strong>in</strong>etic energy is def<strong>in</strong>ed as ½ ⋅ m ⋅ v 2 stat<strong>in</strong>g that largermolecules have lower mean velocities than smaller molecules, givenequal energy levels. Furthermore the <strong>in</strong>creased cross sectional areas reducethe mean free path <strong>in</strong> the carrier medium result<strong>in</strong>g <strong>in</strong> a lower mobilityof larger molecules compared to smaller molecules.This relationship between molecular size <strong>and</strong> diffusivity can be used topredict diffusivities of compounds from known diffusivities of othercompounds based alone on the molecular masses, cf. Equation 7(Schwarzenbach et al., 1993)DDunknownknownmassknown≈ (7)massunknownThis requires that the carrier media are the same <strong>and</strong> that the chemicalstructures are related. Benzene can be used as a model compound forcalculat<strong>in</strong>g the diffusivity of DEHP that also conta<strong>in</strong> a benzene r<strong>in</strong>g <strong>in</strong>addition to the alkyl cha<strong>in</strong>s <strong>and</strong> ester groups. Schwarzenbach et al.(1993) have found a diffusion coefficient <strong>in</strong> water for benzene (M w = 78g ⋅ mol -1 ) of approximately 10 -9 m 2 ⋅ sec -1 .DDEHP= Dbenzene⋅mmbenzeneDEHP=1 ⋅ 10-92msec.⋅78391= 5 ⋅ 10-102msec.Fick’s 1st law can describe the vertical substance flux <strong>in</strong> the sedimentdCS⎡ mg ⎤sz= θ ⋅ Ddisp,sz ⋅dz ⎢⎣m⋅ sec. ⎥(8)⎦N2where θ is the porosity of the sediment <strong>and</strong> D disp,sz is the dispersion coefficient,def<strong>in</strong>ed as2⎡ m ⎤Ddisp, sz= α ⋅ vp+ Dsz⎢ ⎥(9)⎣sec.⎦where α is the longitud<strong>in</strong>al dispersivity, v p is the advective pore watervelocity (≈ 0) <strong>and</strong> D sz is the molecular diffusion coefficient.Schwarzenbach (1993) suggests the follow<strong>in</strong>g empirical relationshipD=D=5100.55=2102msec.1.5-101.5-10(10)disp, szszAdditionally, under favourable conditions, the redistribution of sedimentparticles by benthic macro fauna can occur by a variety of processes.This bioturbation can <strong>in</strong>fluence the transport <strong>and</strong> fate of hydrophobic xenobiotics<strong>in</strong> the surface layer. The particle rework<strong>in</strong>g <strong>and</strong> the pump<strong>in</strong>g ofpore water can create a mixed layer where the adsorbed <strong>and</strong> dissolved62