Thiem Equation
The Thiem Equation is a steady-state groundwater flow model that describes the hydraulic head distribution in a confined aquifer under radial flow conditions, distinguished by its assumption of constant pumping rate and homogeneous, isotropic aquifer properties.
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1.7K
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70
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44
Institutions
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2017–2026
6
Variants
Thiem's Equation
Parents
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Controlled motion of skyrmions in a magnetic antidot lattice
J. Feilhauer, Susmita Saha, Jaroslav Tóbik et al. · Physical review. B./Physical review. B · 2020 · 50 citations · Full text
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Max Planck Society
Munich, Germany
2 h-index
3 publications
48 citations
The Ohio State University
Columbus, United States
2 h-index
3 publications
99 citations
Universität Hamburg
Hamburg, Germany
2 h-index
7 publications
122 citations

National Yang Ming Chiao Tung University
Hsinchu, Taiwan
2 h-index
5 publications
93 citations

University of Notre Dame
Notre Dame, United States
2 h-index
4 publications
120 citations
Advanced Light Source
Berkeley, United States
2 h-index
3 publications
54 citations
Paul Scherrer Institute
Villigen, Switzerland
1 h-index
2 publications
100 citations

Beijing Normal University
Beijing, China
1 h-index
8 publications
128 citations
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GW · 4 publications · 167 citations
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4 publications · 1.2K citations
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PRB · 3 publications · 49 citations
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3 publications · 48 citations
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1 publications · 13 citations
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