Temperature is one major physical quantity of the subsurface and therefore, heat can be used as a tracer. This thesis further promotes heat as a tracer by evaluating a thermal tracer test and comparing the obtained results to previous studies. Additionally, a new thermal field test for the hydraulic characterization of the subsurface is developed. This new development transfers the thermal response test, to a powerful hydrogeological field test, by introducing a new evaluation approach
Thermal response test (TRT) is a common procedure for characterization of ground and borehole therma...
Regular thermal response tests (TRT) are routinely performed to get data for sizing larger installat...
A large tank (4 × 8 × 1.4 m) filled with loamy sediments and equipped with 26 standard piezometers a...
Using heat as an active tracer for aquifer characterization is a topic of increasing interest. In th...
Using heat as a tracer together with a solute tracer is interesting for characterizing hydrogeotherm...
Simultaneous solute and heat tracer test provides essential information for a reliable assessment of...
Current thermal response tests, used to estimate the subsurface thermal conductivity in the geotherm...
In this paper for the first time the Moving Line Source (MLS) model is combined with a depth-resolve...
Thermal response tests (TRTs), used to evaluate the subsurface thermal conductivity when designing g...
Using heat as an active tracer in different types of aquifers is a topic of increasing interest. In ...
Using heat as an active tracer in different types of aquifers is a topic of increasing interest [e.g...
Innovative and efficient strategies for energy utilization become a priority, especially in the civi...
In the shallow geothermal sector, the main thermal properties of a reservoir are usually deduced by ...
Groundwater resources are increasingly used around the world as geothermal systems. Understanding ph...
The Thermal Response Test (TRT) is the most versatile tool to determine the thermal propriety of the...
Thermal response test (TRT) is a common procedure for characterization of ground and borehole therma...
Regular thermal response tests (TRT) are routinely performed to get data for sizing larger installat...
A large tank (4 × 8 × 1.4 m) filled with loamy sediments and equipped with 26 standard piezometers a...
Using heat as an active tracer for aquifer characterization is a topic of increasing interest. In th...
Using heat as a tracer together with a solute tracer is interesting for characterizing hydrogeotherm...
Simultaneous solute and heat tracer test provides essential information for a reliable assessment of...
Current thermal response tests, used to estimate the subsurface thermal conductivity in the geotherm...
In this paper for the first time the Moving Line Source (MLS) model is combined with a depth-resolve...
Thermal response tests (TRTs), used to evaluate the subsurface thermal conductivity when designing g...
Using heat as an active tracer in different types of aquifers is a topic of increasing interest. In ...
Using heat as an active tracer in different types of aquifers is a topic of increasing interest [e.g...
Innovative and efficient strategies for energy utilization become a priority, especially in the civi...
In the shallow geothermal sector, the main thermal properties of a reservoir are usually deduced by ...
Groundwater resources are increasingly used around the world as geothermal systems. Understanding ph...
The Thermal Response Test (TRT) is the most versatile tool to determine the thermal propriety of the...
Thermal response test (TRT) is a common procedure for characterization of ground and borehole therma...
Regular thermal response tests (TRT) are routinely performed to get data for sizing larger installat...
A large tank (4 × 8 × 1.4 m) filled with loamy sediments and equipped with 26 standard piezometers a...