ena-STUDY-HELMHOLTZ CENTRE FOR ENVIRONMENTAL RESEARCH - UFZ.-20-11-2020-14:11:01:281-681
Monitoring of the effects of a temporally limited heat stress on microbial communities in a shallow aquifer
Aquifer thermal energy storage (ATES) is a key concept for the use of renewable energy resources. Interest in the biogeochemical effects of ATES performed at high temperature (HT-ATES; > 60 °C) is increasing due to higher energetic efficiencies. However, HT-ATES induces temperature fluctuations that exceed the natural variability in shallow aquifers, which could lead to adverse effects in subsurface ecosystems by altering the groundwater chemistry, biodiversity, and microbial metabolic activity, resulting in changes of the groundwater quality, biogeochemical processes, and ecosystem functions. The aim of this study was to emulate the initial operating phase of a HT-ATES system with a short-term infiltration of warm water into a typical porous middle European aquifer and to monitor the effects on the microbial communities inhabiting the aquifer. Therefore, local groundwater was withdrawn, heated up to 75 °C, and re-infiltrated into a shallow aquifer located near Wittstock/Dosse (Brandenburg, Germany) for around five days. Groundwater samples were taken regularly before and after the infiltration and analyzed by conducting 16S rRNA gene amplicon sequencing for microbial diversity analyses as well as total cell counting. During the infiltration, a thermal plume with groundwater temperatures increasing from 9 ± 2 to up to ~ 65 °C was recorded. The highest temperature at which samples were taken was 34.9 °C. The microbial communities in the groundwater were mainly composed of Gammaproteobacteria, Alphaproteobacteria, Bacteroidia, and Actinobacteria, and the total cell numbers ranged from 3.2 * 104 to 3.1 * 106 cells ml-1. Samples from monitoring wells with up to moderately increased groundwater temperatures (< 35 °C) showed that neither the compositions of the microbial communities nor the total number of cells in groundwater were significantly influenced, indicating that the diverse groundwater microbiome was resilient to the temporally limited heat stress.
Aquifer thermal energy storage (ATES) is a key concept for the use of renewable energy resources. Interest in the biogeochemical effects of ATES performed at high temperature (HT-ATES; > 60 °C) is increasing due to higher energetic efficiencies. However, HT-ATES induces temperature fluctuations that exceed the natural variability in shallow aquifers, which could lead to adverse effects in subsurface ecosystems by altering the groundwater chemistry, biodiversity, and microbial metabolic activity, resulting in changes of the groundwater quality, biogeochemical processes, and ecosystem functions. The aim of this study was to emulate the initial operating phase of a HT-ATES system with a short-term infiltration of warm water into a typical porous middle European aquifer and to monitor the effects on the microbial communities inhabiting the aquifer. Therefore, local groundwater was withdrawn, heated up to 75 °C, and re-infiltrated into a shallow aquifer located near Wittstock/Dosse (Brandenburg, Germany) for around five days. Groundwater samples were taken regularly before and after the infiltration and analyzed by conducting 16S rRNA gene amplicon sequencing for microbial diversity analyses as well as total cell counting. During the infiltration, a thermal plume with groundwater temperatures increasing from 9 ± 2 to up to ~ 65 °C was recorded. The highest temperature at which samples were taken was 34.9 °C. The microbial communities in the groundwater were mainly composed of Gammaproteobacteria, Alphaproteobacteria, Bacteroidia, and Actinobacteria, and the total cell numbers ranged from 3.2 * 104 to 3.1 * 106 cells ml-1. Samples from monitoring wells with up to moderately increased groundwater temperatures (< 35 °C) showed that neither the compositions of the microbial communities nor the total number of cells in groundwater were significantly influenced, indicating that the diverse groundwater microbiome was resilient to the temporally limited heat stress.