Index Catalog // ScholarsArchive@OSU

Solute and sediment transport at laboratory and field scale: Contributions of J.-Y. Parlange

Creator:: Barry, D. A., Sander, G. C., Jomaa, S., Yeghiazarian, L., Steenhuis, T. S., and Selker, J. S.
Abstract:: We explore selected aspects of J.-Y. Parlange’s contributions to hydrological transport of solutes and sediments, including both the laboratory and field scales. At the laboratory scale, he provided numerous approximations for solute transport accounting for effects of boundary conditions, linear and nonlinear reactions, and means to determine relevant parameters. Theory...
Resource Type:: Article
Full Text:: J.-Y. Parlange D. A. Barry,1 G. C. Sander,2 S. Jomaa,3 L. Yeghiazarian,4 T. S. Steenhuis,5 and J. S

A simple accurate method to predict time of ponding under variable intensity rainfall

Creator:: Assouline, S., Selker, J. S., and Parlange, J.-Y.
Abstract:: The prediction of the time to ponding following commencement of rainfall is fundamental to hydrologic prediction of flood, erosion, and infiltration. Most of the studies to date have focused on prediction of ponding resulting from simple rainfall patterns. This approach was suitable to rainfall reported as average values over intervals...
Resource Type:: Article
Full Text:: . Parlange, J.-Y., W. L. Hogarth, D. A. Barry, M. B. Parlange, R. Haverkamp, P. J. Ross, T. S. Steenhuis, D

The importance of hydraulic groundwater theory in catchment hydrology: The legacy of Wilfried Brutsaert and Jean-Yves Parlange

Creator:: Troch, Peter A., Berne, Alexis, Bogaart, Patrick, Harman, Ciaran, Hilberts, Arno G. J., Lyon, Steve W., Paniconi, Claudio, Pauwels, Valentijn R. N., Rupp, David E., Selker, John S., Teuling, Adriaan J., Uijlenhoet, Remko, and Verhoest, Niko E. C.
Abstract:: Based on a literature overview, this paper summarizes the impact and legacy of the contributions of Wilfried Brutsaert and Jean-Yves Parlange (Cornell University) with respect to the current state-of-the-art understanding in hydraulic groundwater theory. Forming the basis of many applications in catchment hydrology, ranging from drought flow analysis to surface...
Resource Type:: Article
Full Text:: . Troch,1 Alexis Berne,2 Patrick Bogaart,3 Ciaran Harman,4 Arno G. J. Hilberts,5 Steve W. Lyon,6 Claudio

What controls the apparent timescale of solute mass transfer in aquifers and soils? A comparison of experimental results

Creator:: Haggerty, Roy, Harvey, Charles F., von Schwerin, Claudius Freiherr, and Meigs, Lucy C.
Abstract:: Estimates of mass transfer timescales from 316 solute transport experiments reported in 35 publications are compared to the pore-water velocities and residence times, as well as the experimental durations. New tracer experiments were also conducted in columns of different lengths so that the velocity and the advective residence time could...
Resource Type:: Article
Full Text:: process or aver- aging of multiple rates. Bajracharya and Barry [1997] report that a changes approximately

Drainage of a horizontal Boussinesq aquifer with a power law hydraulic conductivity profile

Creator:: Rupp, David E. and Selker, John S.
Abstract:: Solutions to the Boussinesq equation describing drainage into a fully penetrating channel have been used for aquifer characterization. Two analytical solutions exist for early- and late-time drainage from a saturated, homogeneous, and horizontal aquifer following instantaneous drawdown. The solutions for discharge Q can be expressed as dQ/dt = −aQ [superscript...
Resource Type:: Article
Full Text:: , D. A. Barry, L. Li, F. Stagnitti, A. Heilig, and J. Szilagyi (2001), Sudden drawdown and drainage of

Late-time drainage from a sloping Boussinesq aquifer

Creator:: Bogaart, Patrick W., Rupp, David E., Selker, John S., and van der Velde, Ype
Abstract:: Numerical solutions to the nonlinear Boussinesq equation, applied to a steeply sloping aquifer and assuming uniform hydraulic conductivity, indicate that late-time recession discharge decreases nearly linearly in time. When recession discharge is characterized by -dQ/dt=aQ[superscript b], this is equivalent to constant dQ/dt or b=0. This result suggests that a previously...
Resource Type:: Article
Full Text:: consistent with that of the linearized Boussinesq equation. Citation: Bogaart, P. W., D. E. Rupp, J. S

Transient groundwater chemistry near a river: Effects on U(VI) transport in laboratory column experiments

Creator:: Yin, Jun, Haggerty, Roy, Stoliker, Deborah L., Kent, Douglas B., Istok, Jonathan D., Greskowiak, Janek, and Zachara, John M.
Abstract:: In the 300 Area of a U(VI)-contaminated aquifer at Hanford, Washington, USA, inorganic carbon and major cations, which have large impacts on U(VI) transport, change on an hourly and seasonal basis near the Columbia River. Batch and column experiments were conducted to investigate the factors controlling U(VI) adsorption/desorption by changing...
Resource Type:: Article
Full Text:: the knowledge of real-time change of local groundwater chemistry. Citation: Yin, J., R. Haggerty, D

Infrared thermography of evaporative fluxes and dynamics of salt deposition on heterogeneous porous surfaces

Creator:: Nachshon, Uri, Shahraeeni, Ebrahim, Or, Dani, Dragila, Maria, and Weisbrod, Noam
Abstract:: Evaporation of saline solutions from porous media, common in arid areas, involves complex interactions between mass transport, energy exchange and phase transitions. We quantified evaporation of saline solutions from heterogeneous sand columns under constant hydraulic boundary conditions to focus on effects of salt precipitation on evaporation dynamics. Mass loss measurements...
Resource Type:: Article
Full Text:: for flow and potential decrease in unsaturated hydraulic conductiv- ity [Wissmeier and Barry, 2008

On the use of the Boussinesq equation for interpreting recession hydrographs from sloping aquifers

Creator:: Rupp, David E. and Selker, John S.
Abstract:: The method of recession analysis proposed by Brutsaert and Nieber (1977) remains one of the few analytical tools for estimating aquifer hydraulic parameters at the field scale and beyond. In the method, the recession hydrograph is examined as −dQ/dt = f(Q), where Q is aquifer discharge and f is an...
Resource Type:: Article
Full Text:: of the aquifer. Citation: Rupp, D. E., and J. S. Selker (2006), On the use of the Boussinesq

Present-day and future contributions of glacier runoff to summertime flows in a Pacific Northwest watershed: Implications for water resources

Creator:: Nolin, Anne W., Phillippe, Jeff, Jefferson, Anne, and Lewis, Sarah L.
Abstract:: While the impacts of long-term climate change trends on glacier hydrology have received much attention, little has been done to quantify direct glacier runoff contributions to streamflow. This paper presents an approach for determining glacier runoff contributions to streamflow and estimating the effects of increased temperature and decreased glacier area...
Resource Type:: Article
Full Text:: to be substantial. Citation: Nolin, A. W., J. Phillippe, A. Jefferson, and S. L. Lewis (2010

ScholarsArchive@OSU

Solute and sediment transport at laboratory and field scale: Contributions of J.-Y. Parlange

A simple accurate method to predict time of ponding under variable intensity rainfall

The importance of hydraulic groundwater theory in catchment hydrology: The legacy of Wilfried Brutsaert and Jean-Yves Parlange

What controls the apparent timescale of solute mass transfer in aquifers and soils? A comparison of experimental results

Drainage of a horizontal Boussinesq aquifer with a power law hydraulic conductivity profile

Late-time drainage from a sloping Boussinesq aquifer

Transient groundwater chemistry near a river: Effects on U(VI) transport in laboratory column experiments

Infrared thermography of evaporative fluxes and dynamics of salt deposition on heterogeneous porous surfaces

On the use of the Boussinesq equation for interpreting recession hydrographs from sloping aquifers

Present-day and future contributions of glacier runoff to summertime flows in a Pacific Northwest watershed: Implications for water resources

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