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pro vyhledávání: '"Ana Gonzalez-Nicolas"'
Autor:
Ana Gonzalez-Nicolas, Deborah Bilgic, Ilja Kröker, Assem Mayar, Luca Trevisan, Holger Steeb, Silke Wieprecht, Wolfgang Nowak
Publikováno v:
Transport in Porous Media. 143:463-496
Several environmental phenomena require monitoring time-dependent densities in porous media, e.g., clogging of river sediments, mineral dissolution/precipitation, or variably-saturated multiphase flow. Gamma-ray attenuation (GRA) can monitor time-dep
Publikováno v:
Water
Volume 13
Issue 13
Water, Vol 13, Iss 1723, p 1723 (2021)
Volume 13
Issue 13
Water, Vol 13, Iss 1723, p 1723 (2021)
Currently, the export regime of a catchment is often characterized by the relationship between compound concentration and discharge in the catchment outlet or, more specifically, by the regression slope in log-concentrations versus log-discharge plot
The boundaries of surface-water catchments can be delineated by analyzing digital elevation models using geographic information systems. Surface-water divides and groundwater divides, however, might significantly differ from each other because the gr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f87c2603aabf4fafdf7678260b0ce920
https://doi.org/10.5194/egusphere-egu2020-6907
https://doi.org/10.5194/egusphere-egu2020-6907
Commonly, chemical catchment regimes are described by a simple regression slope of log-concentrations versus log-discharges measured in the catchment outlet river. The slope value of these plots defines the chemical regime of a catchment. A slope=-1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4013df4dc0998bddae96d2b7ae802f6a
https://doi.org/10.5194/egusphere-egu2020-4843
https://doi.org/10.5194/egusphere-egu2020-4843
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Surface-water divides can be delineated by analyzing digital elevation models. They might, however, significantly differ from groundwater divides because the groundwater surface does not necessarily follow the surface topography. Thus, in order to de
Externí odkaz:
https://doaj.org/article/b08ec1ac3c0c4deabec899dab0c79fec