1. Advective transport in heterogeneous aquifers: Are proxy models predictive?. Issue 12 (13th December 2015) Authors: Fiori, A.; Zarlenga, A.; Gotovac, H.; Jankovic, I.; Volpi, E.; Cvetkovic, V.; Dagan, G. Journal: Water resources research Issue: Volume 51:Issue 12(2015:Dec.) Page Start: 9577 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
2. Aquifer heterogeneity controls on adverse human health effects and the concept of the hazard attenuation factor. Issue 8 (6th August 2016) Authors: de Barros, F. P. J.; Bellin, A.; Cvetkovic, V.; Dagan, G.; Fiori, A. Journal: Water resources research Issue: Volume 52:Issue 8(2016:Aug.) Page Start: 5911 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
3. Debates—Stochastic subsurface hydrology from theory to practice: The relevance of stochastic subsurface hydrology to practical problems of contaminant transport and remediation. What is characterization and stochastic theory good for?. Issue 12 (21st December 2016) Authors: Fiori, A.; Cvetkovic, V.; Dagan, G.; Attinger, S.; Bellin, A.; Dietrich, P.; Zech, A.; Teutsch, G. Journal: Water resources research Issue: Volume 52:Issue 12(2016:Dec.) Page Start: 9228 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
4. Dynamic effective properties of heterogeneous geological formations with spherical inclusions under periodic time variations. Issue 7 (13th April 2013) Authors: Rabinovich, A.; Dagan, G.; Miloh, T. Journal: Geophysical research letters Issue: Volume 40:Issue 7(2013:Apr.) Page Start: 1345 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
5. Effective Hydraulic Conductivity of Three‐Dimensional Heterogeneous Formations of Lognormal Permeability Distribution: The Impact of Connectivity. Issue 3 (8th March 2018) Authors: Zarlenga, A.; Janković, I.; Fiori, A.; Dagan, G. Journal: Water resources research Issue: Volume 54:Issue 3(2018) Page Start: 2480 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
6. Groundwater Development in Israel. Issue 1 (8th December 2015) Authors: Schwarz, J.; Bear, J.; Dagan, G. Journal: Ground water Issue: Volume 54:Issue 1(2016:Jan./Feb.) Page Start: 143 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
7. Is unique scaling of aquifer macrodispersivity supported by field data?. Issue 9 (20th September 2015) Authors: Zech, A.; Attinger, S.; Cvetkovic, V.; Dagan, G.; Dietrich, P.; Fiori, A.; Rubin, Y.; Teutsch, G. Journal: Water resources research Issue: Volume 51:Issue 9(2015:Sep.) Page Start: 7662 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
8. Oscillatory pumping wells in phreatic, compressible, and homogeneous aquifers. Issue 8 (22nd August 2014) Authors: Dagan, G.; Rabinovich, A. Journal: Water resources research Issue: Volume 50:Issue 8(2014:Aug.) Page Start: 7058 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
9. Reply to comment by S. Neuman on "Is unique scaling of aquifer macrodispersivity supported by field data?". Issue 5 (22nd May 2016) Authors: Zech, A.; Attinger, S.; Cvetkovic, V.; Dagan, G.; Dietrich, P.; Fiori, A.; Rubin, Y.; Teutsch, G. Journal: Water resources research Issue: Volume 52:Issue 5(2016:May) Page Start: 4203 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
10. Solute transport in aquifers: The comeback of the advection dispersion equation and the First Order Approximation. (December 2017) Authors: Fiori, A.; Zarlenga, A.; Jankovic, I.; Dagan, G. Journal: Advances in water resources Issue: Volume 110(2017) Page Start: 349 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗