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

*Tämän työn vastaava kirjoittaja

Tutkimustuotos: LehtiartikkeliComment/debateScientificvertaisarvioitu

Abstrakti

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.

AlkuperäiskieliEnglanti
Artikkeli123134
JulkaisuWater Research
Vuosikerta274
DOI - pysyväislinkit
TilaJulkaistu - 15 huhtik. 2025
OKM-julkaisutyyppiB1 Kirjoitus tieteellisessä aikakauslehdessä

Sormenjälki

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