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mpmath: a Python library for arbitrary-precision floating-point arithmetic
- Fredrik Johansson, V. Steinberg, A. Brys
- Computer Science
- 27 September 2017
TLDR
Modeling slug tests in unconfined aquifers taking into account water table kinematics, wellbore skin and inertial effects
- B. Malama, Kristopher L. Kuhlman, W. Barrash, M. Cardiff, M. Thoma
- Environmental Science
- 30 September 2011
Review of inverse Laplace transform algorithms for Laplace-space numerical approaches
- Kristopher L. Kuhlman
- MathematicsNumerical Algorithms
- 20 April 2012
TLDR
Semi-analytical solution for flow in leaky unconfined aquifer–aquitard systems
- B. Malama, Kristopher L. Kuhlman, W. Barrash
- Engineering
- 15 November 2007
Brine flow in heated geologic salt.
- Kristopher L. Kuhlman, B. Malama
- Geology
- 1 March 2013
This report is a summary of the physical processes, primary governing equations, solution approaches, and historic testing related to brine migration in geologic salt. Although most information…
Nonlinear dynamics and instability of aqueous dissolution of silicate glasses and minerals
- Yifeng Wang, C. Jové-Colón, Kristopher L. Kuhlman
- Materials ScienceScientific reports
- 22 July 2016
TLDR
Semi-analytical solution for flow in a leaky unconfined aquifer toward a partially penetrating pumping well
- B. Malama, Kristopher L. Kuhlman, W. Barrash
- Engineering
- 1 July 2008
Basin‐Scale Transmissivity and Storativity Estimation Using Hydraulic Tomography
- Kristopher L. Kuhlman, A. Hinnell, P. Mishra, T. Yeh
- MathematicsGround water
- 1 September 2008
TLDR
Unconfined Aquifer Flow Theory: From Dupuit to Present
- P. Mishra, Kristopher L. Kuhlman
- Engineering
- 15 April 2013
Analytic and semi-analytic solution are often used by researchers and practitioners to estimate aquifer parameters from unconfined aquifer pumping tests. The nonlinearities associated with unconfined…
Multiporosity flow in fractured low‐permeability rocks
- Kristopher L. Kuhlman, B. Malama, J. Heath
- Geology
- 19 January 2015
A multiporosity extension of classical double and triple‐porosity fractured rock flow models for slightly compressible fluids is presented. The multiporosity model is an adaptation of the multirate…
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