Get Advances in the Research of Aquatic Environment: Volume 2 PDF

By M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)

ISBN-10: 3642240755

ISBN-13: 9783642240751

The booklet makes a speciality of the administration of the aquatic setting. it truly is aimed toward scientists, scholars, governmental officers and experts facing groundwater and surroundings. Its major aim is to notify the reader of principles, wisdom and event 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 floor waters; Karst Hydrogeology; non-stop Media Hydrogeology; Fissured Rocks Hydrogeology; Hydrochemistry; Geothermics and thermal waters; The position of water in development initiatives; Hydrology

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The petrophysical properties are close to the underlying Khusayyayn, so that these two units together form another combined reservoir (the upper sandstone sequence in the subsurface). The major difference to the subsurface is the absence of an effective aquiclude or aquitard, which in the subsurface is represented by thick shales of the Qusaiba. The lithology and the patchy distribution of the sediments, caused by cut-out of strata beneath the Khusayyayn unconformity; make the Qusaiba an ineffective aquitard.

1991) who report average porosities of 20% for the Dibsiyah, 21% - 25% for the Sanamah, 23% for the Khusayyayn, and locally 30% for the Juwayl. Similarly, Dirner (2007) and Filomena (2007) report porosities between 18% and 31% for the Wajid Sandstone. Together with high effective permeabilities of 1 to 8 darcies, this makes the Wajid Sandstone principally an important reservoir rock. A recent study (GTZ-DCo 2007) has shown that in the subsurface, the Wajid Sandstone succession represents two individual fractured bedrock aquifers separated by an aquitard.

B12 B11 I Borehole Topographic region Table 1. Boreholes description. Y. Chou et al. Rock samples were recovered and allowed for an initial on-site lithostratigraphic identification, as well as various laboratory analyses afterward. Fig. 1. Geological map of the study area. 3 Methodology In each borehole a series of borehole loggings were conducted in situ to identify the probable pathways of ground water. The electric log and the full waveform sonic log (from Robertson Geologging Ltd. UK) were adopted.

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Advances in the Research of Aquatic Environment: Volume 2 by M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)


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