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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Two-dimensional unconfined seepage flow toward a highway cut slope</dc:title><dc:creator>Zerihun,	Yebegaeshet T.	(Avtor)
	</dc:creator><dc:subject>unconfined seepage flow</dc:subject><dc:subject>phreatic surface</dc:subject><dc:subject>artificial cut</dc:subject><dc:subject>seepage discharge</dc:subject><dc:subject>non-hydrostatic groundwater flow</dc:subject><dc:subject>seepage-face height</dc:subject><dc:description>The unconfined gravity-flow system near a free-outflow boundary such as a highway cut slope was
investigated by using a higher-order numerical model. Unlike the Dupuit–Forchheimer equation, which is
applicable mainly to a hydraulic flow problem, the proposed model accounts for the effects of the vertical
component of the flow for a full treatment of the problem of plane phreatic flow. The model equations were
numerically solved by means of a finite-difference scheme. Their accuracy was then verified using the
solutions of the full two-dimensional potential-flow method and rigorous mathematical approaches, revealing
that for a face slope flatter than 70º, the differences between the solutions of the model and the earlier
approaches for the relative seepage-face height were nearly negligible. The comparison results also
demonstrated the substantial effects of the slope of the downstream face on this height and the seepage
discharge. Furthermore, the accuracies of the model predictions for the phreatic-surface profile and the
distributions of the piezometric head at different vertical sections are much better than the earlier method,
which approximates the trapezoidal-shaped aquifer by its equivalent rectangular one. Such a satisfactory
performance may be attributed to the model’s higher-order correction factor for the effects of the phreaticsurface curvature and steep slope.</dc:description><dc:date>2023</dc:date><dc:date>2024-10-03 13:26:15</dc:date><dc:type>Članek v reviji</dc:type><dc:identifier>163182</dc:identifier><dc:identifier>UDK: 556.51</dc:identifier><dc:identifier>ISSN pri članku: 0352-3551</dc:identifier><dc:identifier>DOI: 10.15292/acta.hydro.2023.06</dc:identifier><dc:identifier>COBISS_ID: 209981187</dc:identifier><dc:language>sl</dc:language></metadata>
