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Surface water and groundwater interactions between the stream and the hyporheic zone profoundly affect river intermittency and biogeochemical processes, yet they are rarely quantified. As an excellent natural tracer, temperature was used to quantify
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb5dcae511f9ea9a7a5a39cddb5ec825
https://doi.org/10.5194/egusphere-egu23-2177
https://doi.org/10.5194/egusphere-egu23-2177
