Monday, May 27, 2019
Solving Vertical and Horizontal Well Hydraulics Problems
A new generalized three-dimensional analytical solution is developed for a partially-penetrating vertical rectangular parallelopipedon well dissemble in a confined aquifer by solving the three-dimensional transient ground water flow differential equation in x-y-z Cartesian coordinates system for drawdown by taking into account the three principal hydraulic conductivities (K _x, K _y, and K _z) along the x-y-z coordinate directions. The fully penetrating screen case becomes equivalent to the single vertical fracture case of Gringarten and Ramey (1973).It is shown that the new solution and Gringarten and Ramey solution (1973) match very well. Similarly, it is shown that this new solution for a horizontally tiny fully penetrating parallelopipedon rectangular parallelopiped screen case match very well with Theis (1935) solution. Moreover, it is also shown that the horizontally tiny partially-penetrating parallelepiped rectangular well screen case of this new solution match very well w ith Hantush (1964) solution.This new analytical solution can also covert a partially-penetrating horizontal well by representing its screen interval with vertically tiny rectangular parallelepiped. Also the solution takes into account both the vertical anisotropy (a _(zx)=K _z/K _x) as well as the horizontal anisotropy (a _(yx)=K _y/K _x) and has potential application areas to analyze pumping test drawdown data from partially-penetrating vertical and horizontal well by representing them as tiny rectangular parallelepiped as well as line sources.The solution has also potential application areas for a partially-penetrating parallelepiped rectangular vertical fracture. With this new solution, the horizontal anisotropy (a _(yx)=K _y/K _x) in addition to the vertical anisotropy (a _(zx)=K _z/K _x) can also be opinionated using observed drawdown data. Most importantly, with this solution, to the knowledge of the author, it has been shown the first time in the literature that some well-k nown well hydra
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