By M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)
The publication makes a speciality of the administration of the aquatic surroundings. it really is aimed toward scientists, scholars, governmental officers and experts facing groundwater and atmosphere. Its major objective is to notify the reader of rules, wisdom and adventure when it comes to a sustainable aquatic atmosphere. the most themes are as follows: Water our bodies and Ecosystems; weather swap and Water our bodies; Water caliber and agriculture; interplay of floor and flooring waters; Karst Hydrogeology; non-stop Media Hydrogeology; Fissured Rocks Hydrogeology; Hydrochemistry; Geothermics and thermal waters; The function of water in development tasks; Hydrology
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Additional info for Advances in the Research of Aquatic Environment: Volume 2
This unit in turn is followed by some 10 meters of fine to coarse-grained sandstones in small-scale bed forms with abundant channels. The uppermost unit again is dominated by large-scale bed forms and coarse-grained, often pebbly sandstones. We interpret the Khusayyayn to have been deposited on a high-energy open shelf. This is indicated by the lateral continuity of the large cross-bedded units. They represent submarine megaripples or dunes and testify to strong unidirectional currents of tidal origin.
C. in volcanites. Hydrogeological properties of fractured rocks under the climate of West Africa 9 Below this highest density level, the density of WPZ decreases with depth for each of the profiles. However, a significant increase of the density of WPZ occurs around 80 m depth in metasediments; this level is associated to fractured fresh sandstone layer. The same phenomenon is also observed in granites and volcanites around 75 and 100 m respectively, but in a slightly less significant manner. In hard rocks, this decrease of fracturing density with depth was described by the works of Wyns et al.
Earth Planet. Sci. 13, 315-344 Williams JH, Johnson CD (2004) Acoustic and optical borehole-wall imaging for fractured-rock aquifer studies. J. Appl. Geophys. 55, 151-159 Advances in understanding the relation between reservoir properties and facies distribution in the Paleozoic Wajid Sandstone, Saudi Arabia H. Al Ajmi1, M. Keller2,4, M. Hinderer3, R. com 2 Geozentrum Nordbayern, Abteilung Krustendynamik, Schlossgarten 5, 91054 Erlangen, Germany 3 Institut für Angewandte Geowissenschaften, TU Darmstadt, Schnittspahnstrasse 9, 64287 Darmstadt, Germany 4 Gesellschaft für Technische Zusammenarbeit International Services (GTZ-IS), Riyadh, Saudi Arabia Abstract The Wajid Sandstone is one of the most important groundwater reservoirs in the Kingdom of Saudi Arabia.
Advances in the Research of Aquatic Environment: Volume 2 by M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)