(592f) Ecohydrological Management and Valuation Insights of Ecosystem Services in Salt Lakes through Advanced Dynamic Optimisation Strategies
AIChE Annual Meeting
2018
2018 AIChE Annual Meeting
Environmental Division
Rapid Fire Session: Environmental Division
Wednesday, October 31, 2018 - 5:10pm to 5:15pm
We formulate dynamic mass balances for water and salt; evaporation is calculated based on energy and momentum balances on a daily basis. The model has been validated with collected data for the period 2008-2016 (Siniscalchi et al., 2018a). Based on two bathymetric studies, we include rigorous calculations for lake volume, as composed of several geometric forms. We formulate an optimal control problem to manage the water resource during wet and dry periods. In wet periods the water body is managed to prevent flooding of the nearby fields. In dry periods, management actions are carried out to address an important ecological and economic issue, the maintenance of optimal environmental conditions for silverside.
The objective is to keep lake salinity around a desired value considered as optimal for silverside reproduction, while fulfilling the differential algebraic equations system describing the hydrological model. Therefore, the objective function is integral of the square difference between a set point value and current salinity value at each time instant. There are two control variables: the diverted flowrate to a nearby artificial reservoir in a wet scenario and the required inflow from the artificial reservoir in dry periods. We consider a four-year wet period (mean annual rainfall 800 mm), followed by a two-year dry period (annual rainfall 408 mm). Numerical results show diverted river flowrate profiles in the wet period, which are between 0 and 85% of the river discharge. During the four-year wet period, a new artificial reservoir of 80 hm3 volume (area: 11 km2) could be constructed fed with the diverted water flowrate. This reservoir, for which mass balances and evaporation calculation are performed, can later provide an input stream to Chasicó Lake throughout the two-year dry period. Stream profiles are obtained. In this way, salinity can be kept within desired values, as well as lake volume. The model is implemented within a control vector parameterization environment in gPROMS (PSEnterprise, 2017). The driving forces of the ecosystem services provided by the salt lake, identified through the proposed integrated model, represent useful tools towards their valuation.
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