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Modeling 17α-ethinylestradiol removal in membrane bioreactors

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Poster Session<br />

WWTmod2012<br />

modification similar to the Hill k<strong>in</strong>etics, i.e. a power-law on the concentration. The parameter K EE2<br />

represents the maximum number of sorption sites that are available for sorption.<br />

Table 3. Gujer matrix of the add-<strong>in</strong> model describ<strong>in</strong>g EE2’s sorption and co-metabolic degradation<br />

Process S O S EE2 X EE2 X BA Process rate (g/m³.d)<br />

Sorption − 1 1<br />

Desorption 1 − 1<br />

Co-metabolic<br />

degradation<br />

by grow<strong>in</strong>g<br />

nitrifiers<br />

168<br />

− 1 1<br />

k<br />

⎛<br />

⎜<br />

EE 2<br />

EE2<br />

∗ X ∗S<br />

∗⎜<br />

⎟<br />

⎜<br />

EE 2<br />

n X<br />

EE 2 ⎛ ⎞ ⎟<br />

sor TSS EE2 n<br />

EE2<br />

⎜ KEE2<br />

+ ⎜ X ⎟<br />

TSS<br />

⎝<br />

k<br />

sor<br />

⋅ X<br />

K<br />

− ( )<br />

NH O EE2<br />

D<br />

EE2<br />

S S S<br />

η t ∗µ ∗ * ∗ ∗X<br />

EE2 A BA<br />

KNH + SNH KOA + SO KNEE2 + SEE2<br />

Biodegradation model<br />

The degradation of EE2 is assumed to be achieved by co-metabolism on soluble EE2 dur<strong>in</strong>g the<br />

aerobic growth of nitrify<strong>in</strong>g bacteria, X BA (mg/l) (Table 3). Hence, a new process rate similar to the<br />

one used for the aerobic growth of autotrophic biomass <strong>in</strong> ASM1 was created for co-metabolic<br />

degradation of EE2. The difference is an additional k<strong>in</strong>etic limitation term, i.e. it stops when no<br />

more EE2 is present. As the results below show, the biodegradation of EE2 is not <strong>in</strong>stantaneous,<br />

some adaptation seems required. To this end a Verhulst-type logistic function (η EE2 ) was added to<br />

the biodegradation k<strong>in</strong>etics (Verhulst, 1845). It is basically a differential equation describ<strong>in</strong>g how<br />

the fraction of the maximum rate that can be obta<strong>in</strong>ed, ƞ EE2 , evolves <strong>in</strong> function of time, t (d):<br />

dη<br />

⎛<br />

EE2<br />

η ⎞<br />

EE2<br />

= kACCηEE2<br />

1−<br />

dt<br />

⎜<br />

⎟ ; which solves <strong>in</strong>to:<br />

⎝ ηEE2,max<br />

⎠<br />

ηEE2,max<br />

* ηEE2,<strong>in</strong>i<br />

η t = ; where:<br />

η + η − η<br />

( )<br />

ACC<br />

( ) e −<br />

EE2 k *t<br />

EE2,<strong>in</strong>i EE2,max EE2,<strong>in</strong>i<br />

η EE2,max , can be viewed as the maximum susta<strong>in</strong>able fraction of the process rate;<br />

η EE2,<strong>in</strong>i , represents an <strong>in</strong>itial fraction of the process rate;<br />

k acc is the rate at which the fraction of the process rate evolves (d -1 ).<br />

Calibration<br />

A partition coefficient was calculated us<strong>in</strong>g the log(K OW ) values found <strong>in</strong> literature and the<br />

empirical formula (Karickhoff, 1981) shown below:<br />

KD = 0.41∗fOC ∗ KOW<br />

,<br />

where f OC is the fraction of organic carbon <strong>in</strong> the biomass. A f OC value of 0.41 was calculated<br />

accord<strong>in</strong>g to the ratio of VSS/TSS of 0.78 that was measured dur<strong>in</strong>g the experiment with a ratio of<br />

K<br />

⎝<br />

n<br />

⎠<br />

⎞<br />

⎟<br />

⎟<br />

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