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. 2021 Mar 24;11:6780. doi: 10.1038/s41598-021-86094-5

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© The Author(s) 2021

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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Energy partition in hydraulic-stimulation process. (a) True triaxial laboratory tests in Pocheon granite (CC = constant rate continuous, SC = stepwise rate continuous, CP = cyclic progressive); (b) underground test in naturally fractured granodiorite at Äspö HRL, Sweden (HF = hydraulic fracturing experiment); and (c) field stimulation at Pohang EGS site (PX1 = borehole PX1). All tests performed at all scales are flow-rate controlled.