A general framework of stream–aquifer interaction caused by variable stream stages

A general analytical solution for flow to a single horizontal well by Fourier and Laplace transforms

“…(3) The stream bed has the same hydraulic conductivity as aquifers. Note that Intaraprasong and Zhan [7] had addressed the effects of variable stream stage and low-permeable stream bed on the stream depletion rate.…”

“…Many analytical models treat the stream as a constant-head boundary to estimate stream depletion rate [e.g., [1][2][3]6,17,21]. Some researchers proposed to treat the stream as a variable stream stage represented by a periodic function for seasonal variations or a function changed in space and time for flood wave [7]. The articles mentioned above investigated the behavior of stream depletion rate induced from a vertical well.…”

Twenty years of global groundwater research: A Science Citation Index Expanded-based bibliometric survey (1993–2012)

“…The study of water in aquifers and the characterization of aquifers are key topics of Hydrogeology, a discipline concerned with groundwater research. Stream/ tide-aquifer interaction, ''groundwater flow'' in aquifers, aquifer overexploitation, and climate change impacts on aquifers have remained hot research fields (Loáiciga et al, 2000;Custodio, 2002;Nastev et al, 2005;Intaraprasong and Zhan, 2009;Singh and Jha, 2011). Numerical simulation of ''groundwater flow'' and related contaminants and heat transport have attracted increasing attention during the past two decades.…”

An analytical approach to capture zone delineation for a well near a stream with a leaky layer

“…Anderson (2000) obtained an analytical solution to the problem in a complex domain by dropping Hantush's assumption. Recent researchers who have investigated the interaction between groundwater and streams through assumption of a leaky layer between them include Hantush (2005), Intaraprasong and Zhan (2007), Ha et al (2007), Rushton (2007), and Intaraprasong and Zhan (2009).…”