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Problémy modelovania prúdenia podzemných vôd v územiach ovplyvnených banskou činnosťou.

Problémy modelovania prúdenia podzemných vôd v územiach ovplyvnených banskou činnosťou. Doc. RNDr. David Krčmář, PhD. Prírodovedecká fakulta UK, Bratislava Katedra Hydrogeológie.

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Problémy modelovania prúdenia podzemných vôd v územiach ovplyvnených banskou činnosťou.

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  1. Problémy modelovania prúdenia podzemných vôd v územiach ovplyvnených banskou činnosťou. Doc. RNDr. David Krčmář, PhD. Prírodovedecká fakulta UK, Bratislava Katedra Hydrogeológie

  2. MODFLOW USG UnStructured Grid,(Panday et al., 2013)control volume finite differences, or integrated finite differences The new Connected Linear Network (CLN) Package The CLN cells could represent wells, pipes, fractures, underground excavations, tunnels, rivers or other linear features and CLN cells could be vertical, horizontal or tilled.

  3. Riadiaca rovnica prítok - odtok = zmena množstva vody v zásobnosti

  4. 1 i,j+1 0 4 2 i-1,j i,j i+1,j 3 i,j-1 • Riešenie rovnice: • Analyticky Theis, 1935 2. Numericky Princíp: diskretizácia času a priestoru

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