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Page 1: THE IMPACT OF STANDING COLUMN WELL OPERATION ON … · 2020. 5. 1. · standing column well was monitored over a one-year period using a geothermal mobile laboratory located near

GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 1

Léo Cerclet, Philippe Pasquier, Benoît Courcelles

Department of Civil, Geological and Mining Engineering

Polytechnique Montréal

European Geosciences Union – General Assembly 2020

May 05, 2020

THE IMPACT OF STANDING COLUMN WELL OPERATION ON CARBONATE SCALING

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 2

STANDING COLUMN WELLS

Introduction Experimental Results Conclusions

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o Standing Column Wells (SCW) demonstrate high heatexchange capacity (Orio et al., 2005) and represent apromising solution to reduce the capital cost comparedto classic closed loop, by 49% to 78% (O’Neill et al.,2006).

o In a SCW, groundwater is continuously recirculated inan uncased well, bringing the water in direct contactwith the rock.

o During peak periods, the SCW can discharge a portionof the outlet water into an injection well. For a fractionof 10% of groundwater flow, it can improve heattransfers by about 2.5 times (Beaudry et al., 2019).

o This technology yields great results in igneous rock,which has limited geochemical reaction (Orio et al.,2005).

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 3

o The clogging of a geothermal system impacts groundwaterflow rate and heat transfer. Indeed, 0.8 mm of scale on theheat exchanger surface results in 19% higher consumptionfor the heat pump compared to a clean heat exchanger(Rafferty, 2004).

o Geothermal systems are particularly exposed to cloggingevents. The pumping rate, the variation of temperatureand the mixing of water promote several cloggingprocesses which can be physical (Burté, 2018),microbiological (Kim et al., 2017; Lerm et al., 2013) andchemical (Palmer and Cherry 1984; Possemiers et al.,2014).

o Precipitation of calcite is identified as a potential problemwhen groundwater temperature increases (i.e. when thegeothermal system is operated in cooling mode).

CLOGGING OF STANDING COLUMN WELL

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Introduction Experimental Results Conclusions

Source: Eppner, F., Pasquier, P. Baudron, P., 2015. Development of a Thermo-Hydro-Geochemical Model for Low Temperature Geoexchange Applications. COMSOL 2015-Boston.

Source : Bott, T. R. (1995). Fouling of heat exchangers. Elsevier.

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 4

PROBLEMATIC AND OBJECTIVE

Introduction Experimental Results Conclusions

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Objective :

To evaluate which operating condition creates theoptimal conditions for clogging in standing column wellconstructed in carbonate aquifer.

Problematic :

The risk of carbonate scaling is known in the literatureto be a hazard during the operation of open-loopsystems.

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 5

EXPERIMENTAL SCW AND PRESENCE OF CARBONATES

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Introduction Experimental Results Conclusions

Initial rock composition Initial Groundwater composition

Stratigraphy adapted form Beaudry et al, 2019

o For this study, a 215.8-m-deep experimentalstanding column well was monitored over a one-year period using a geothermal mobile laboratorylocated near Montreal.

o The aquifer is composed primarily of silicates, andits high concentrations in calcium and magnesiummake it reactive, since they are the more reactiveelements (Appelo and Postma., 2004).

o The initial groundwater composition is also abovethe recommendations made by Rafferty (2004) toavoid calcium precipitation. This limit is fixed at 80ppm CaCO3 for hardness.

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 6

EXPERIMENTAL SCW AND GEOTHERMAL LABORATORY

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Introduction Experimental Results Conclusions

Mobile geothermal laboratory

o In operation since 2016o This study takes place between January 2018

and October 2018 (1 year)o 51 groundwater sampleso 1 advanced monitoring system (flow,

temperature)o 4 sample pointso 1 solid deposit sample scheduled for the end

of this study

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 7

OPERATION – VARIABLES FOR STEPWISE REGRESSION

Introduction Experimental Results Conclusions

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o This figure presents the operating parameters and the calciumconcentrations of water. It presents the major variables used bythe stepwise regression performed between the operationalparameter and the groundwater calcium concentration (SP-1).

o The monitoring system logs the bleeding water flow (red line),the total flow (blue line) and the treated water flow (green line).

o The red boxes represent the periods where the geothermalsystem was offline. The downtime is used as a variable in thestepwise regression.

o The temperatures LWT and EWT are recorded for eachsampling.

o A new variable is created to represent the three modes linkedto temperature (the “heating mode”, the “recirculating mode”and the “cooling mode”).

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 8

o The regression found 10 operating variablesexplaining the calcium concentration, with acorrelation factor of 0.86.

The most significant operating variables :

o The pumping groundwater flow has the mostimpact on groundwater calcium concentration.

o The LWT also influences the calcium concentration.This result is in agreement with the simulationperformed by Eppner et al. (2016). Moreover, thetransition from recirculation to cooling leads toprecipitation of calcium.

o The downtime has a strong impact on the calciumconcentration.

STEPWISE REGRESSION

Introduction Experimental Results Conclusions

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𝐶𝑎𝐶𝑂3 Precipitation

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 9

RESULTS AND DISCUSSION

Introduction Experimental Results Conclusions

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o After two years of operation, twoflow sensors were cleaned. Thedeposit observed is black, solidand reacts with nitric acid.

o The results show that theconcentrations in calcium,oxygen and carbon are highest inthe deposit.

o This chemical composition andthe mineral structure indicate adeposit composed of calcite. TheX-ray had a score of 81 for thecalcite.

o Nevertheless, the effect of thescaling on the system’s operationwas limited to the flowmeters.

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 10

CONCLUSION

Introduction Experimental Results Conclusion

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o This study explored the impacts of standing column well operation on the stability ofcalcite. These impacts are limited to the precipitation of calcite in the flowmeters.

o Future works will focus on the impacts of these deposits on thermal exchanges, onfinding a way to avoid their formation through the use of a water treatment systemand on strategies to limit the impacts of system downtimes.

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 11

Léo Cerclet, Philippe Pasquier, Benoît Courcelles

Department of Civil, Geological and Mining Engineering

Polytechnique Montréal

European Geosciences Union – General Assembly 2020

May 05, 2020

THE IMPACT OF STANDING COLUMN WELL OPERATION ON CARBONATE SCALING

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 12

• Appelo, C. A. J., & Postma, D. (2004). Geochemistry, groundwater and pollution. CRC press.

• Bott, T. R. (1995). Fouling of heat exchangers. Elsevier.

• Burté, L., Baranger, C. C., Aquilina, L., Le Borgne, T., Frechin, N., & Gérard, M.-F. (2016). Clogging of shallowgeothermal doublets: Hydrologic, geochemical and microbiological observations in a pilot site. Conference:European Geothermal Congress 2016.

• Eppner, F., Pasquier, P., & Baudron, P. (2017). Investigation of thermo-hydro-geochemical processes in a standingcolumn well intersected by a fracture. https://doi.org/10.22488/okstate.17.000527

• Gabrielle Beaudry, Philippe Pasquier, & Denis Marcotte. (2019, November 21). FIELD TESTING OF A STANDINGCOLUMNWELL LOCATED IN THE NICOLET FORMATION. https://zenodo.org/record/3565977#.XjL4W2j0k2w

• Kim, H., Mok, J.-K., Park, Y., Kaown, D., & Lee, K.-K. (2017). Composition of groundwater bacterial communitiesbefore and after air surging in a groundwater heat pump system according to a pyrosequencing assay. Water,9(11), 891.

• Lerm, S., Westphal, A., Miethling-Graff, R., Alawi, M., Seibt, A., Wolfgramm, M., & Würdemann, H. (2013).Thermal effects on microbial composition and microbiologically induced corrosion and mineral precipitationaffecting operation of a geothermal plant in a deep saline aquifer. Extremophiles, 17(2), 311–327.

• O’Neill, Z. D., Spitler, J. D., & Rees, S. (2006, July 1). Performance analysis of standing column well ground heatexchanger systems. ASHRAE Transactions. https://link.galegroup.com/apps/doc/A156720180/AONE?sid=lms

BIBLIOGRAPHY

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GLQ2601 – Hydrogéologie Appliquée Chapitre 1 – page 13

• Orio, C. D., Chiasson, A., Johnson, C. N., Deng, Z., & others. (2005). A survey of standing column well installationsin North America. ASHRAE Transactions, 111, 109.

BIBLIOGRAPHY