Abstract
This paper presents a systematic method for approximating hydraulic head gradients from randomly located hydraulic head values. The locations of these head values are connected by straight lines to form a network of triangles. Over each triangle, a plane surface is used to approximate the head values; the gradient of this plane is then taken as the hydraulic gradient. Given values of porosity and hydraulic conductivity, the fluid velocity can be calculated from Darcy's Law.
Original language | English (US) |
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Pages (from-to) | 262-264 |
Number of pages | 3 |
Journal | Groundwater |
Volume | 19 |
Issue number | 3 |
DOIs | |
State | Published - May 1981 |
All Science Journal Classification (ASJC) codes
- Water Science and Technology
- Computers in Earth Sciences