2006
DOI: 10.1016/j.jhydrol.2005.11.033
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Interpretation of transient borehole flow metering data in a fissured granite formation

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Cited by 9 publications
(9 citation statements)
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“…The flow rate occurring in the probe is calculated from the travel time of the heat impulse from the emitter to the sensors; the water flow outside the flowmeter is excluded by deformable rubber disks used as packers. To ensure high accuracy in the measurement, we applied the repeated point‐by‐point method with a resolution of 1 m (Sze´kely and Galsa ).…”
Section: Methodsmentioning
confidence: 99%
“…The flow rate occurring in the probe is calculated from the travel time of the heat impulse from the emitter to the sensors; the water flow outside the flowmeter is excluded by deformable rubber disks used as packers. To ensure high accuracy in the measurement, we applied the repeated point‐by‐point method with a resolution of 1 m (Sze´kely and Galsa ).…”
Section: Methodsmentioning
confidence: 99%
“…To ensure high accuracy in the measurement, the repeated point-by-point method has been applied with a vertical resolution of 1 m (Székely and Galsa 2006).…”
Section: Flow Meter Testsmentioning
confidence: 99%
“…The WT is able to use an analytical technique based on the numerical Laplace inversion (Hemker 1999) and also a numerical technique which is a finite difference method improved by Székely and Galsa (2006). The wellbore simulator of the WT software includes the evaluation of the following effects: laminar and/or turbulent well-loss with depth and/or time variant parameters of the well screen; turbulent axial friction loss; a non-uniform static level in the screened model layers; induced flow-controlled drawdown in observation wells; and wellbore storage.…”
Section: Analytical and Numerical Wt Softwarementioning
confidence: 99%
“…Automatic parameter calibration may be carried out by fitting the simulated drawdown, recovery, flow metering and overflow data to the measured ones. The software has been successfully applied to the evaluation of field tests conducted in sedimentary aquifers (Székely 1992(Székely , 2012Mukhopadhyay et al 1994), fissured granite (Székely 2013;Székely and Galsa 2006) and in volcanic aquifers (Székely et al 2015), as well. Table 2 shows the comparison of the VTZ and the WT models.…”
Section: Analytical and Numerical Wt Softwarementioning
confidence: 99%