Thermal-Plume fibre Optic Tracking (T-POT) test for flow velocity measurement in groundwater boreholes
|Resource type:||Composite Resource|
|Storage:||The size of this resource is 1.5 MB|
|Created:||Mar 31, 2018 at 9:46 p.m.|
|Last updated:|| Apr 09, 2018 at 8:22 p.m.
|Citation:||See how to cite this resource|
We develop an approach for measuring in-well fluid velocities using point electrical heating combined with spatially and temporally continuous temperature monitoring using Distributed Temperature Sensing (DTS). The method uses a point heater to warm a discrete volume of water. The rate of advection of this plume, once the heating is stopped, equates to the average flow velocity in the well. We conducted Thermal-Plume fibre Optic Tracking (T-POT) tests in a borehole in a fractured rock aquifer with the heater at the same depth and multiple pumping rates. Tracking of the thermal plume peak allowed the spatially varying velocity to be estimated up to 50 m downstream from the heating point, depending on the pumping rate. The T-POT technique can be used to estimate the velocity throughout long intervals provided that thermal dilution due to inflows, dispersion, or cooling by conduction do not render the thermal pulse unresolvable with DTS. A complete flow log may be obtained by deploying the heater at multiple depths, or with multiple point heaters.
Raw project data is available by contacting email@example.com
Duplicate. Keyword not added.
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/
Please wait for the process to complete.