A Method to Estimate the Hydraulic Conductivity of the Ground by TRT Analysis

被引:3
|
作者
Scorpo, Alberto Liuzzo [1 ,2 ]
Nordell, Bo [1 ]
Gehlin, Signhild [3 ]
机构
[1] Lulea Univ Technol, Div Architecture & Water, Dept Civil Min & Nat Resources Engn, SE-97187 Lulea, Sweden
[2] Univ Trieste, Dipartimento Ingn & Architettura, Via A Valerio 10, I-34127 Trieste, Italy
[3] Swedish Ctr Shallow Geothermal Energy, SE-22104 Lund, Sweden
关键词
THERMAL RESPONSE TEST; HEAT-EXCHANGERS; PERFORMANCE; ADVECTION; FLOW; BOREHOLES; SYSTEMS;
D O I
10.1111/gwat.12443
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The knowledge of hydraulic properties of aquifers is important in many engineering applications. Careful design of ground-coupled heat exchangers requires that the hydraulic characteristics and thermal properties of the aquifer must be well understood. Knowledge of groundwater flow rate and aquifer thermal properties is the basis for proper design of such plants. Different methods have been developed in order to estimate hydraulic conductivity by evaluating the transport of various tracers (chemical, heat etc.); thermal response testing (TRT) is a specific type of heat tracer that allows including the hydraulic properties in an effective thermal conductivity value. Starting from these considerations, an expeditious, graphical method was proposed to estimate the hydraulic conductivity of the aquifer, using TRT data and plausible assumption. Suggested method, which is not yet verified or proven to be reliable, should be encouraging further studies and development in this direction.
引用
收藏
页码:110 / 118
页数:9
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