By M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)
The booklet 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 target is to notify the reader of rules, wisdom and adventure by way of a sustainable aquatic setting. the most issues 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 function of water in development tasks; Hydrology
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Additional resources for Advances in the Research of Aquatic Environment: Volume 2
In the light of this, the groundwater is the source to the rescue. Attempts to exploit groundwater resources have made groundwater search an all comer’s affairs. This has lead to indiscriminate exploitation of groundwater resources and the attendant poor results. The purpose of electrical surveys is to determine the subsurface resistivity distribution by making measurements on the ground surface as these measurements help to estimate the electrical resistivity of the subsurface. The subsurface electrical resistivity is associated with various geological factors such as the mineral and fluid content, porosity and degree of water saturation in the rock, ionic concentration of the pore fluid and composition of the N.
Y. C. T. H. M. T. C. , No. tw Abstract The movement and storage of ground water in the mountainous region has a significant impact on the dynamics of surface water flow. An adequate identification of the conductible fracture in the aquifer has thus received growing interest over the past decades. This paper summarizes the major findings from the first year of a hydrogeological investigation program initiated by the Central Geological Survey, Ministry of Economic Affairs (MOEA) of Taiwan since 2010, with a special focus on exploring in detail the fracture permeability.
75 m3/h. Beyond 100 m this discharge decreases with the depth. Compared to metasediments, granites show lower flows. 8 m3/h between 40 and 60 m (in fractured fresh granites layer). In metasediments and volcanites, WPZ are undifferentially localized in isalterite layer, fissured layer and fractured fresh basement layer while in granites, they are only localized in fissured layer and fractured fresh basement. In each of the profiles, the frequency of WPZ (all layers of the profile having been taken into account) is distributed in a log-normal way.
Advances in the Research of Aquatic Environment: Volume 2 by M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)