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In this study, modeling of mineral resources of underground water in karst mountain area of Maros-Pangkep, Indonesia was made by the Boltzmann lattice-gas automata method. The simulation results showed that the greater the time duration, the mor e different fluid motion pattern. For the state of the karst region, this means that the heterogeneous medium karst very unstable and affect the movement of the particles. In addition, karstification process takes place in a relatively long time with adequate rainfall.

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In this study, modeling of mineral resources of underground water in karst mountain area of Maros-Pangkep, Indonesia was made by the Boltzmann lattice-gas automata method. The simulation results showed that the greater the time duration, the mor e different fluid motion pattern. For the state of the karst region, this means that the heterogeneous medium karst very unstable and affect the movement of the particles. In addition, karstification process takes place in a relatively long time with adequate rainfall.

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In this study, modeling of mineral resources of underground water in karst mountain area of Maros-Pangkep, Indonesia was made by the Boltzmann lattice-gas automata method. The simulation results showed that the greater the time duration, the mor e different fluid motion pattern. For the state of the karst region, this means that the heterogeneous medium karst very unstable and affect the movement of the particles. In addition, karstification process takes place in a relatively long time with adequate rainfall.

Mr Ansari Saleh Ahmar
Universitas Negeri Makassar

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This page is a summary of: Model of Groundwater Flow Using Boltzmann Lattice-Gas Automation Method In Maros Karst Region, Indonesia, Drinking Water Engineering and Science Discussions, February 2017, Copernicus GmbH,
DOI: 10.5194/dwes-2016-9.
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