Pumped flowing fluid electrical conductivity (FFEC) logs, also known as pumped borehole dilution testing, is an experimentally easy‐to‐perform approach to evaluating vertical variations in the hydraulic conductivity of an aquifer. In contrast to the simplicity of the logging equipment, analysis of the data is complex and laborious. Current methods typically require repeated solution of the advection‐dispersion equation (ADE) for describing the flow in the borehole and comparison with the experimental results. In this paper, we describe a direct solution for determining borehole fluid velocity that bypasses the need for complex numerical computation and repetitive optimization. The method rests on the observation that, while solving the ADE ...
Single borehole dilution tests (SBDTs) are an inexpensive but effective technique for hydrogeologica...
Hydraulic conductivities of volcanic and carbonate lithologic units at the Nevada Test Site were est...
An understanding of both the hydraulic properties of the aquifer and the depth distribution of salts...
Recent numerical studies have demonstrated that the conventional interpretation of the borehole flo...
The flowing fluid electric conductivity (FFEC) loggingmethod is an efficient way to provide informat...
Identifying flows into, out of, and across boreholes is important for characterizing aquifers, deter...
Three single-borehole hydraulic techniques for estimation of hydraulic conductivity, the dipole-flow...
Identifying flows into, out of, and across boreholes is important for characterizing aquifers, deter...
A radially convergent tracer test was carried out in an unconfined Chalk aquifer of Berkshire, Unite...
A rigorous and practical approach for interpretation of impeller flow log data to determine vertical...
The flowing fluid electric conductivity (FFEC) logging method is an efficient way to provide inform...
Flowing fluid electrical conductivity (FFEC) logging is a hydrogeologic testing method that is usual...
A Bayesian inverse method is applied to two electromagnetic flowmeter tests conducted in fractured w...
Borehole measurements of spontaneous electrical potential (SP) are routinely acquired in wells drill...
Single-borehole dilution tests (SBDTs) are a method for characterizing groundwater monitoring wells ...
Single borehole dilution tests (SBDTs) are an inexpensive but effective technique for hydrogeologica...
Hydraulic conductivities of volcanic and carbonate lithologic units at the Nevada Test Site were est...
An understanding of both the hydraulic properties of the aquifer and the depth distribution of salts...
Recent numerical studies have demonstrated that the conventional interpretation of the borehole flo...
The flowing fluid electric conductivity (FFEC) loggingmethod is an efficient way to provide informat...
Identifying flows into, out of, and across boreholes is important for characterizing aquifers, deter...
Three single-borehole hydraulic techniques for estimation of hydraulic conductivity, the dipole-flow...
Identifying flows into, out of, and across boreholes is important for characterizing aquifers, deter...
A radially convergent tracer test was carried out in an unconfined Chalk aquifer of Berkshire, Unite...
A rigorous and practical approach for interpretation of impeller flow log data to determine vertical...
The flowing fluid electric conductivity (FFEC) logging method is an efficient way to provide inform...
Flowing fluid electrical conductivity (FFEC) logging is a hydrogeologic testing method that is usual...
A Bayesian inverse method is applied to two electromagnetic flowmeter tests conducted in fractured w...
Borehole measurements of spontaneous electrical potential (SP) are routinely acquired in wells drill...
Single-borehole dilution tests (SBDTs) are a method for characterizing groundwater monitoring wells ...
Single borehole dilution tests (SBDTs) are an inexpensive but effective technique for hydrogeologica...
Hydraulic conductivities of volcanic and carbonate lithologic units at the Nevada Test Site were est...
An understanding of both the hydraulic properties of the aquifer and the depth distribution of salts...