Water Flow and Solute Transport In Porous Fractured Chalk

Ronit Nativ, Eilon Adar, Ofer Dahan, Noam Weisbrod, Brian Berkowitz, Daniel Ronen

Research output: Contribution to journalArticlepeer-review


The unique features of flow and transport in the chalk aquitard in the Negev desert were first
documented on a regional scale by the monitoring of 23 wells which penetrate the chalk
across the central and northern Negev. We suggested that water and solutes shortcut
through the low-permeability matrix of the vadose chalk via hctures and joints, escaping
much of the land surface exposure to evapotranspiration. This conclusion was based on
observed seasonal fluctuations of water level in these wells and the chemical and isotopic
Original languageEnglish
Pages (from-to)76-78
StatePublished - 1999


Dive into the research topics of 'Water Flow and Solute Transport In Porous Fractured Chalk'. Together they form a unique fingerprint.

Cite this