Geothermal Well Testing Consulting Services
Unlocking critical insights to reveal resource feasibility
Designing the right well test for your geothermal system.
Up to 330 degC [626 degF]
Conventional hydrothermal
EGS
Resman? geothermal tracers survive in the harshest environments. For conventional geothermal applications, their stability and dependability give operators the confidence to continuously measure the retention time and fine-tune water injection for maximum efficiency.
In the case of EGS, we also monitor fracture and circulation efficiency, building on our experience from the stimulation arena to optimize project economics.
Tracer signals are plotted against time, a dissimilar tracer, or both, for advanced analysis. The resulting curves are then interpreted, often together with other relevant data.
Appearance of tracers in a different place compared with where they were introduced provides proof of mass transport and connectivity. The value comes from interpreting the tracer journey, a task that we have simplified with advanced digital workflows that use the direct measurements as input.
For conventional hydrothermal applications, the Resman geothermal tracer is injected together with the return water and sampled at the surface extraction point. In the case of EGS, while stimulation or fracturing is in progress, unique tracers in liquid form are seamlessly blended into stage, stage cluster, or zonal treatments. The stimulation or fracturing process transports the tracer into the formation. During flowback and production, fluid samples are captured at surface at a frequency agreed with the operator and analyzed with a resolution of parts per trillion; proprietary interpretation methods are used to generate a quantitative production log (QPL) of stage, cluster, or zonal performance.
Results are subsequently presented via the Tracer Track? visualization solution, where applicable.
Scalable solutions for analysis