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Libro de Resúmenes / Book of Abstracts (Español/English)

Libro de Resúmenes / Book of Abstracts (Español/English)

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Resumenes 126<br />

The lagoon <strong>of</strong> Chascomús is the largest one pertaining to the “Linked<br />

Lagoons” <strong>of</strong> the province <strong>of</strong> Buenos Aires (Argentina); it has a surface <strong>of</strong><br />

3044 ha, a length <strong>of</strong> 15 km and a wi<strong>de</strong> <strong>of</strong> 5 km; its average <strong>de</strong>pth is 1.52 m<br />

and its maximum <strong>de</strong>pht is 2.50 m. The lagoon bottom is composed <strong>of</strong><br />

muddy clay and muddy sand, and lodges a great variety <strong>of</strong> fish <strong>of</strong><br />

commercial interest. Many <strong>of</strong> these fish are affected by periodic anoxic<br />

crises that occur in association with high temperatures and low rain.<br />

Previous studies have <strong>de</strong>monstrated a strong association between dissolved<br />

oxygen (DO) concentration and the amount <strong>of</strong> suspen<strong>de</strong>d matter (seston).<br />

Seston inclu<strong>de</strong>s live organisms, <strong>de</strong>ad organic matter and inorganic matter.<br />

We present here a mathematical mo<strong>de</strong>l <strong>of</strong> the seston dynamics. The mo<strong>de</strong>l<br />

was parametrised with existing data and a DO prediction was ma<strong>de</strong> taking<br />

into account the negative correlation between seston and DO.<br />

We consi<strong>de</strong>r that seston dynamics can be represented by a<br />

differential equation including a growth rate (algae growth) related to light<br />

and temperature, and a mortality/<strong>de</strong>composition rate correlated with<br />

temperature only:<br />

dt<br />

−k1<br />

sin<br />

[ ( B sin t + k )( 1 − e ) − C sin t − q ] ⋅ s<br />

ds t<br />

=<br />

0<br />

Temperature and light are periodic variables throughout the year.<br />

The grow rate is consi<strong>de</strong>red asimptotic with light.<br />

The solution <strong>of</strong> the equation is:<br />

ln<br />

−k<br />

sin<br />

e<br />

cost<br />

⎛ B<br />

⎜<br />

⎝ k1<br />

1<br />

0<br />

() s = ( C − B)<br />

cost<br />

+ ( k − q ) ⋅ t + ⎜ sin t + ⎟ + E<br />

0<br />

The mo<strong>de</strong>l has an equilibrium point that fluctuates throughout the<br />

year following the forcing variables (temperature and light). The mo<strong>de</strong>l fits<br />

very well to experimental data <strong>of</strong> seston and DO. This mo<strong>de</strong>l can help us to<br />

predict anoxic crises and to predict them.<br />

0<br />

t<br />

0<br />

k<br />

k<br />

1<br />

⎞<br />

⎟<br />

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