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The determination of aquifer recharge zones is necessary for optimal and sustainable management of water resources. Stable isotopes (δ18O and δ2H) are an effective tool to better understand the relationship between precipitation and groundwater. Ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bae3d2f2b6b13d5fa9f3cdc297221fe6
https://doi.org/10.5194/egusphere-egu22-9346
https://doi.org/10.5194/egusphere-egu22-9346
