By G. Stournaras (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)
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 rules, wisdom and event when it comes to a sustainable aquatic setting. the most issues are as follows: Water our bodies and Ecosystems; weather switch 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 initiatives; Hydrology
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Example text
Regarding the consideration of the aquatic exchanges between the different water bodies, an extended range of exchanging procedures can be recognized. Exchanges between surface runoff and groundwater aquifers The main procedures in this subject are the development of the hydrologic circle by secondary, tertiary etc. phenomena as they are the secondary runoff by the groundwater coming out from a spring, the secondary infiltration during the runoff, etc. Exchanges between lakes and groundwater aquifers The regime of these exchanges is settled by the hydraulic charges of the lake and the surrounded aquifer in the different points of the lake’s perimeter.
Biologists describe the characters and the evolution of species without any reference to geophysics. Economists analyze the monetary exchanges without any connection with biology etc. Later, is quite possible that these references will be considered as necessary, but the symbiosis of the two worlds is to be described and analyzed in their real dimensions now. It is cited that, in many sciences, the use of a narrative account is not enough, since the outcome of actions and conditions can be a result of different experiments.
The initial shape concerning the water distribution on and I the earth is the hydrologic water circle P (Precipitation) = R (Runoff) + E (Evapotranspiration) + I (Infiltration) RV (Reserves Variations). The hydrologic water circle has a meaning only considered in certain period and in certain area. The above general distribution is modified because of secondary, tertiary etc. phenomena as they are the secondary runoff of the springs water the secondary infiltration during the runoff and so on.