Best practices for characterization of High Temperature-Aquifer Thermal Energy Storage (HT-ATES) potential using well tests in Berlin (Germany) as an example

被引:6
|
作者
Bloecher, Guido [1 ]
Regenspurg, Simona [1 ]
Kranz, Stefan [1 ]
Lipus, Martin [1 ]
Pei, Liang [1 ]
Norden, Ben [1 ]
Reinsch, Thomas [2 ]
Henninges, Jan [3 ]
Siemon, Romy [4 ]
Orenczuk, Dominika [5 ]
Zeilfelder, Sarah [6 ]
Scheytt, Traugott [7 ]
Saadat, Ali [1 ]
机构
[1] GFZ German Res Ctr Geosci, Telegrafenberg, D-14473 Potsdam, Germany
[2] Fraunhofer Einrichtung Energieinfrastrukturen & Ge, Bochum, Germany
[3] Off Safety Nucl Waste Management BASE, Berlin, Germany
[4] Kummer Erd & Tiefbau GmbH, D-12249 Berlin, Germany
[5] ISAC GmbH, Lutzowstr, D-10785 Berlin, Germany
[6] Senatsverwaltung Umwelt Mobil Verbraucher & Klimas, D-10179 Berlin, Germany
[7] Tech Univ Bergakademie Freiberg, Gustav Zeuner Str, D-09599 Freiberg, Germany
关键词
Aquifer Thermal Energy Storage (ATES); Push-pull test; Step-rate test; Tracer test; Well test analysis; PUSH-PULL TESTS; TRACER TESTS; SINGLE-WELL;
D O I
10.1016/j.geothermics.2023.102830
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Application of Aquifer Thermal Energy Storage with High Temperatures (HT-ATES) ranging from 60-90 degrees C is a promising technique to store large amounts of energy in urban areas. However, these areas typically lack information on hydrogeological and thermal parameters of the subsurface to determine the potential for energy storage. Moreover, conventional exploration methods as pumping tests do not account for the variation in density caused by the high temperature gradients or changes in salinity as encountered in HT-ATES operation. The objective of this study is therefore to develop best practices for characterizing the hydrogeological and thermal properties of groundwater wells and their surrounding formation that determine the potential performance of HT-ATES-systems. In addition to conventional pumping tests, a set of Push-Pull tracer Tests (PPTs) with cold and hot water are proposed and scrutinized using Berlin as case study. There, the research well Gt BChb 1/2015, which is characterized by a reservoir temperature of 17 degrees C at a depth between 220 und 230 m below ground surface was tested. In 2017, seven Slug-Withdrawal Tests (SWTs), a Step-Rate-Test (SRT), a production tests, and two Push-Pull tracer Tests (PPTs) with hot and cold water were performed during a period of 40 days. These tests were accompanied by Distributed-Temperature-Sensing (DTS) monitoring. The temperature measurements provide indications of injection areas based on the warmback period during a PPT with 81 degrees C hot water. The determined aquifer transmissibility tau = 3.2 x 10(-5) m(2)/s, the related Productivity Index (PI = 2.0 m(3)/(h bar)), and maximum flow rates of about 5 m(3)/h indicate that the aquifer has potential for HT-ATES. However, the PPT and the DTS monitoring revealed cross flow between the target aquifer and an overlying aquifer. Thus, a new well with a design avoiding cross flow is required to utilize the aquifer's energy storage potential. A set of best practices for characterizing HT-ATES potential was derived from the experiences in this study.
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页数:18
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