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 Plus annual

Presents the access of premium content as premium feature

Premium Content

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 annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The study was carried out within 4,000 km2 segment of Sassandra watershed located in Soubre, south-west of Cote d’Ivoire where coffee and cocoa production are preponderant. This work aimed to provide a general methodology in order to draw the flow directions and map the potential productive aquifer in hard-rocks. Drilling data, remote sensing, and geomorphic data in a context of weathered plutonic and metamorphic Precambrian were used. The regional water table was modeled through a linear relationship between the topographic surface of the digital elevation model and the base surface of the perennial streams thalwegs. As result, a map of regolith thickness obtained has been compared with the geology to emphasize their relationship. Furthermore, other correlations have been found between the hydraulic data and geomorphological features to get more precise stratification model. Concealed by the regolith, the hard-rock aquifer is made up of three layers. From top to bottom we have the saprolite (

Discontinuous Nature of Phreatic Aquifers in Granitic Rocks at Watershed Scale: A Stratiform Model from Perennial Streams and Well Data