Corrigendum to “The estimation of infiltration and inflow in a sewage network by combining continuous monitoring of hydrological parameters, flow and temperature with stable isotopes of oxygen and hydrogen” [Water Research 255 (2024) 121505] (Water Research (2024) 255, (S004313542400407X), (10.1016/j.watres.2024.121505))

Axumawit Tequam Tesfamariam*, Elisangela Heiderscheidt, Markus Sunela, Arttu Pitkänen, Lauri Rantala, Pekka M. Rossi

*Corresponding author for this work

Research output: Contribution to journalComment/debateScientificpeer-review

Abstract

The authors regret < In March, the mean δ18O isotopic signal of groundwater was -13.16 ‰, while in May it was -13.10 ‰. The drinking water, on the other hand, had more depleted signals of -11.53 ‰ in March and -12.26 ‰ in May. >. The authors would like to apologise for any inconvenience caused. We would like the word depleted to be changed to enriched.

Original languageEnglish
Article number123134
JournalWater Research
Volume274
DOIs
Publication statusPublished - 15 Apr 2025
MoE publication typeB1 Non-refereed journal articles

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