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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 ( IF 11.4 ) Pub Date : 2025-01-22 , DOI: 10.1016/j.watres.2025.123134
Axumawit Tequam Tesfamariam, Elisangela Heiderscheidt, Markus Sunela, Arttu Pitkänen, Lauri Rantala, Pekka M. Rossi
Water Research ( IF 11.4 ) Pub Date : 2025-01-22 , DOI: 10.1016/j.watres.2025.123134
Axumawit Tequam Tesfamariam, Elisangela Heiderscheidt, Markus Sunela, Arttu Pitkänen, Lauri Rantala, Pekka M. Rossi
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. >.
中文翻译:
“通过将水文参数、流量和温度的连续监测与氧和氢的稳定同位素相结合来估计污水管网中的渗透和流入”的勘误 [Water Research 255 (2024) 121505]
作者遗憾 < 3 月,地下水δ 18O 同位素信号的平均值为 -13.16 ‰,而 5 月为 -13.10 ‰。另一方面,饮用水的枯竭信号更多,3 月份为 -11.53 ‰,5 月份为 -12.26 ‰。
更新日期:2025-01-22
中文翻译:
“通过将水文参数、流量和温度的连续监测与氧和氢的稳定同位素相结合来估计污水管网中的渗透和流入”的勘误 [Water Research 255 (2024) 121505]
作者遗憾 < 3 月,地下水δ 18O 同位素信号的平均值为 -13.16 ‰,而 5 月为 -13.10 ‰。另一方面,饮用水的枯竭信号更多,3 月份为 -11.53 ‰,5 月份为 -12.26 ‰。