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Author |
Title |
Year |
Publication |
Volume |
Pages |
Links  |
|
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Leibundgut, C.; Maloszewski, P.; Külls, C. |
Tracers in Hydrology |
2009 |
|
|
|
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Külls, C. |
Groundwater of the North-Western Kalahari, Namibia: estimation of recharge and quantification of the flow system |
2001 |
Hydrogeologie und Umwelt |
|
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|
|
Aldawsari, S.; Kampmann, R.; Harnisch, J.; Rohde, C. |
Setting Time, Microstructure, and Durability Properties of Low Calcium Fly Ash/Slag Geopolymer: A Review |
2022 |
Materials |
15 |
|
|
|
|
Eliades, M.; Bruggeman, A.; Djuma, H.; Christofi, C.; Kuells, C. |
Quantifying Evapotranspiration and Drainage Losses in a Semi-Arid Nectarine (Prunus persica var. nucipersica) Field with a Dynamic Crop Coefficient (Kc) Derived from Leaf Area Index Measurements |
2022 |
Water |
14 |
|
|
|
|
Eliades, M.; Bruggeman, A.; Djuma, H.; Christofi, C.; Kuells, C. |
Quantifying Evapotranspiration and Drainage Losses in a Semi-Arid Nectarine (Prunus persica var. nucipersica) Field with a Dynamic Crop Coefficient (Kc) Derived from Leaf Area Index Measurements |
2022 |
Water |
14 |
|
|
|
|
Eliades, M.; Bruggeman, A.; Djuma, H.; Christofi, C.; Kuells, C. |
Quantifying Evapotranspiration and Drainage Losses in a Semi-Arid Nectarine (Prunus persica var. nucipersica) Field with a Dynamic Crop Coefficient (Kc) Derived from Leaf Area Index Measurements |
2022 |
Water |
14 |
|
|
|
|
Ardelt, G.; Külls, C.; Hellbrück, H. |
Towards intrinsic molecular communication using isotopic isomerism |
2018 |
Open Journal of Internet Of Things (OJIOT) |
4 |
135-143 |
|
|
|
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 |
|
|
|
Lightfoot, D.R. |
Moroccan khettara: Traditional irrigation and progressive desiccation |
1996 |
Geoforum |
27 |
261-273 |
|
|
|
Vogel, J.C.; Talma, A.S.; Heaton, T.H.E. |
Gaseous nitrogen as evidence for denitrification in groundwater |
1981 |
Journal of Hydrology |
50 |
191-200 |
|
