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Seepage under Static and Dynamic Conditions of Darbandikhan Dam in Iraq
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Abstract<p>Static and dynamic circumstances confirm that seepage is water movement through the earth dam’s embankment’s voids from upstream to downstream. Seepage is a quantity of fluid that has seeped through the permeable material or as the infiltration downward and lateral movement of water into soil or substrata from a source of supply such as a reservoir of a dam. In case of an earthquake strikes saturated soils, the water-filled pore spaces collapse, reducing the soil’s overall volume. The water pressure between individual soil grains is increased as a result of this action, and the grains can then move freely in the watery matrix. This reduces the soil’s resistance to shear stress and causes the mass of soil to take on liquid-like qualities. Soil deforms quickly in its liquefied state, and massive items such as structures can be destroyed by the rapid loss of support from below. This study employs finite element method (FEM) analysis to examine the seepage under static and dynamic condition and effect of earthquake on the Darbandikhan earth dam seepage. The study adopted the maximum head of water equal to 486 m.a.s.l. meter above sea level, the peak acceleration of earthquake was 0.15, 0.3 and 0.5 m2/s, time = 25s, and five history points in upstream and downstream were assessed. Geo-studio software represented by the programs like SEEP/W and quake/w that support the numerical analysis system under seismic influence were used. The results showed that the amount of seepage under seismic action was significantly influenced and increased as the peak acceleration of the earthquake increased. Therefore, the significance of the findings in terms of practical application for engineers and decision-makers involved in dam safety measures.</p>
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