English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Tools annual

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Presents the access of premium content as premium feature

Premium Content

Global: Zendy Plus annual

Global: Zendy Free Plan

The groundwater recharge processes were investigated in the unsaturated zone of the Ljubljansko polje\udintergranular aquifer. The study based on application of environmental tracers. The monitoring of the drainage\udsystem was established at an urban lysimeter consisting of artifiial and autochthonous sediment layers.\udGroundwater was sampled with the suction cups instaled at depths of 0.3, 0.6, 1.2, 1.8, 3.0 and 4.0 m. The results\udpointed out the most important factors that control the hydrodynamic processes and solute transport in the\udstudy site where the soil cover and vegetation are missing. The physico–chemical and isotopic properties of\udsampled groundwater indicated that the clayey layers have an important role in the hydraulic behaviour of the\udunsaturated zone. As a consequence of a piston effect the event and pre-event water concentrate above these\udlayers causing lateral flw. A vertical breakthrough of this water into lower layers of the unsaturated zone could\udoccur through preferential paths during intensive precipitation events in dependence on pre-accumulated water\udvolumes. Under such conditions groundwater residence time is about 2 months in the unsaturated zone 3 m below\udthe surface

Application of environmental tracers to study the drainage system of the unsaturated zone of the Ljubljansko polje aquifer