S
Stephen E. Silliman
Researcher at University of Notre Dame
Publications - 81
Citations - 3020
Stephen E. Silliman is an academic researcher from University of Notre Dame. The author has contributed to research in topics: Population & Engineering education. The author has an hindex of 25, co-authored 78 publications receiving 2845 citations. Previous affiliations of Stephen E. Silliman include National University of Benin & United States Geological Survey.
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A Transient Laboratory Method for Determining the Hydraulic Properties of "Tight"Rocks-I, Theory
TL;DR: In this paper, a general analytical solution for the transient pulse test is presented, graphically illustrated by plots of dimensionless variables for several cases of interest, as limiting cases, the more restrictive analytical solutions that the previous investigators have derived.
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Anomalous transport in laboratory-scale, heterogeneous porous media
TL;DR: In this paper, the first-passage time distribution (FPTD) of migrating contaminants in random media, developed with the use of a continuous time random walk (CTRW) formalism, is analyzed.
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Analysis of time-series measurements of sediment temperature for identification of gaining vs. losing portions of Juday Creek, Indiana
TL;DR: In this article, a method was proposed for the identification of the location of inflows-outflows in both creeks and streams, applied to a small creek in northern Indiana, involves measurement over time of both sediment temperature and the temperature at the base of the overlying water column.
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A transient laboratory method for determining the hydraulic properties of ‘tight’ rocks—II. Application
TL;DR: In this paper, a general analytical solution for the transient pulse test was presented and a graphical method for analyzing data from a test to obtain the hydraulic properties of the sample was presented.
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Quantifying downflow through creek sediments using temperature time series: one-dimensional solution incorporating measured surface temperature
TL;DR: In this article, the authors presented a more general solution to identify the location of and quantifying the volume of groundwater/surface water interaction by incorporating measured surface temperature (rather than an assumed surface temperature), which is targeted on quantification of flux across the sediment for conditions of one-dimensional downflow with a constant flux over periods of days to weeks.