Author  |
Title |
Year |
Publication |
Volume |
Pages |
| Davila, P.; Külls, C. |
Reliability of current CFC data for age dating of water |
2010 |
EGU Geophysical Abstracts |
|
536 |
| Davila, P.; Külls, C. |
Combined application of 85-Kr, 39-Ar with CFCs in contaminated aquifers |
2009 |
EGU Geophysical Abstracts |
|
1074 |
| Dahan, O.; Tatarsky, B.; Enzel, Y.; Külls, C.; Seely, M.; Benito, G. |
Dynamics of flood water infiltration and ground water recharge in hyperarid desert |
2008 |
Groundwater |
46 |
450-461 |
| Christofi, C.; Bruggeman, A.; Külls, C.; Constantinou, C. |
Hydrochemical evolution of groundwater in gabbro of the Troodos Fractured Aquifer. A comprehensive approach |
2020 |
Applied Geochemistry |
114 |
104524 |
| Christofi, C.; Bruggeman, A.; Külls, C.; Constantinou, C. |
Isotope hydrology and hydrogeochemical modeling of Troodos Fractured Aquifer, Cyprus: The development of hydrogeological descriptions of observed water types |
2020 |
Applied Geochemistry |
123 |
104780 |
| Benito, G.; Rohde, R.; Seely, M.; Külls, C.; Dahan, O.; Enzel, Y.; Todd, S.; Botero, B.; Morin, E.; Grodek, T. |
Management of alluvial aquifers in two southern African ephemeral rivers: implications for IWRM |
2010 |
Water Resources Management |
24 |
641-667 |
| Baram, S.; Ronen, Z.; Kurtzman, D.; Külls, C.; Dahan, O. |
Desiccation-crack-induced salinization in deep clay sediment |
2013 |
Hydrology and Earth System Sciences |
17 |
1533 |
| Ardelt, G.; Külls, C.; Hellbrück, H. |
Towards intrinsic molecular communication using isotopic isomerism |
2018 |
Open Journal of Internet Of Things (OJIOT) |
4 |
135-143 |
| Androvitsanea, A.; Fawzy, M.; Fuchs, J.; Külls, C.; Fahlbusch, H.; Heiden, J. |
Hydrologische Bedingungen im Heraion von Samos vom 12. bis 8. Jh. v. Chr. und ihre Bedeutung für die wasserbauliche Infrastruktur |
2018 |
Environmental Water Engineering |
1 |
1-21 |
| Adolph, G.; Römer, T.; Külls, C. |
Deriving complex groundwater age structure by combining age dating and analytic element modelling |
|
G-DAT 2008-Leipzig |
|
12 |
