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Exact bounds for lift-to-drag ratios of profiles in the Helmholtz-Kirchhoff flow in the Helmholtz-Kirchhoff (infinite cavity) flow. The coefficients are based on the wetted arc length of profile
MANAGEMENT OF FINANCIAL FLOWS OF THE VERTICALLY INTEGRATED CORPORATE STRUCTURES on development of the concept of financial flows. To development of inter-economic communications and integral
Exact bounds for lift-to-drag ratios of profiles in the Helmholtz-Kirchhoff flow in the Helmholtz-Kirchhoff (infinite cavity) flow. The coefficients are based on the wetted arc length of profile
Aerosol aspiration into a cylindrical sampler from a low-velocity downward flow and from calm air-velocity downward flow and from calm air is solved. A simple analytical model for the velocity field of the carrier
Tension-saturated and unsaturated flows from line sources in subsurface irrigation: Riesenkampf's and Philip's solutions revisited to here as R-38), analytical solution for steady 2-D flow from a buried line source in a homogeneous Green
Construction of complex potentials for multiply connected domain to construction of a complex potential - an analytic function in an unbounded multiply connected domain with a
Aerosol aspiration into a cylindrical sampler from a low-velocity downward flow and from calm air-velocity downward flow and from calm air is solved. A simple analytical model for the velocity field of the carrier
INVESTIGATION OF THE STABILITY OF THE POTENTIAL FLUID FLOW IN A POROUS MEDIUM WITH VARIABLE TRANSVERSE DIFFUSION COEFFICIENTWe have considered the potential fluid flow in porous medium taking into account variable diffusion
Dipolic Flows Relevant to Aquifer Storage and Recovery: Strack’s Sink Solution Revisited© 2018, Springer Science+Business Media B.V., part of Springer Nature. Steady, 2-,3-D Darcian flows
Seepage to ditches and topographic depressions in saturated and unsaturated soils content, Kirchhoff potential). None of these singularities belongs to the real flow domain, evaporating
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