Groundwater flow in hillslopes

Analytical solutions by the theory of holomorphic functions and hydraulic theory

Anvar Kacimov, Yurii Obnosov, Osman Abdalla, Oscar Castro-Orgaz

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Three 2-D steady Darcian flows in an aquifer with a subjacent confining layer of a non-constant slope or a bedding inconformity are studied by two models: a potential theory (conformal mappings, the inverse boundary-value problem method, and the theory of R-linear conjugation) and hydraulic approximation. First, flow over a corner, whose vertex is either a stagnation point or point of infinite Darcian velocity, is analysed as a transition from one "normal" regime upstream to another downstream. The hodograph domain is a circular triangle, which is mapped onto a complex potential strip via an auxiliary half-plane. Parametric equations (backwater curves) for the phreatic surface are obtained. For the same flow problem, a depth-averaged 1-D nonlinear ODE for the thickness of the saturated zone (a generalized Dupuit-Fawer model) is numerically solved showing a perfect match with the potential (2-D) solution. Second, a non-planar aquifuge boundary is reconstructed as a streamline, along which an additional "control" boundary condition holds in the form of pore pressure as a function of an auxiliary variable (a relation between the hydraulic head and vertical Cartesian coordinate). The free surface is found in terms of Cauchy's integrals for the Zhukovskii function, with explicit integrations for selected "controls". Third, a confined flow in a two-layered aquifer having a lens-type semi-circular inclusion in the subjacent stratum and incident velocity parallel to the interface between two aquifers is examined. The conjugation conditions along all four boundaries, across which the hydraulic conductivity jumps, are exactly met. The three velocity fields are explicitly presented, with examination of the flow net, including separatrices ("capture zone" boundaries), demarcating suction/barriering of the lens, and evaluation of the lens-induced cross-flow (commingling) between the two strata.

Original languageEnglish
Pages (from-to)3380-3397
Number of pages18
JournalApplied Mathematical Modelling
Volume39
Issue number12
DOIs
Publication statusPublished - Jun 15 2015

Fingerprint

Groundwater Flow
Groundwater flow
Aquifers
Hydraulics
Lenses
Analytic function
Analytical Solution
Lens
Conjugation
Confined flow
Conformal mapping
Pore pressure
Hydraulic conductivity
Steady flow
Inverse Boundary Value Problem
Nonlinear ODE
Parametric equations
Hydraulic Conductivity
Stagnation Point
Cauchy Integral

Keywords

  • Hodograph
  • Hydraulic approximation
  • Hydrogeology of alluvium aquifers in Oman
  • Potential theory
  • Three-component heterogeneity
  • Unconfined seepage over corner

ASJC Scopus subject areas

  • Applied Mathematics
  • Modelling and Simulation

Cite this

Groundwater flow in hillslopes : Analytical solutions by the theory of holomorphic functions and hydraulic theory. / Kacimov, Anvar; Obnosov, Yurii; Abdalla, Osman; Castro-Orgaz, Oscar.

In: Applied Mathematical Modelling, Vol. 39, No. 12, 15.06.2015, p. 3380-3397.

Research output: Contribution to journalArticle

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