By G. Stournaras (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)
The publication makes a speciality of the administration of the aquatic surroundings. it's aimed toward scientists, scholars, governmental officers and experts facing groundwater and surroundings. Its major objective is to notify the reader of rules, wisdom and adventure when it comes to a sustainable aquatic atmosphere. the most subject matters are as follows: Water our bodies and Ecosystems; weather switch 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 building tasks; Hydrology
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Additional info for Advances in the Research of Aquatic Environment: Volume 1
2006). The GIS program proposed for the data manipulation and mapping is MapInfo professional. (d) Creation of thematic maps As a result, instant thematic maps can be derived using the thematic map capability of the GIS system according to custom needs. This final step gives the visual image of the expected impacts on different species due to the construction of a specific technical project. GIS combined with the assessment procedure can now present the degree of impact on different species according to their habitats taking into account the characteristics of their living environment, the distance from the construction site, the degree of their susceptibility to changes etc.
In Spain, many of Sites of Community Important (SCI) as part of the Natura 2000 network are surface water bodies such as lakes or Protected Areas as results of the implementation of the WFD, identified and subject to protection as stated in the Basin Water Plans. Therefore, protection elements are common in both directives. The purpose of this paper is directed to conduct a conceptual analysis to define the similarities and differences, and determine the scope of the meaning of both concepts. A superficial analysis might point that the two concepts are equivalent; however, a more detailed analysis reveals significant differences that must be taken into account to avoid misunderstandings from scientists and technicians.
Stream leakage rate is not a function of the location of the water table. Groundwater in integrated environmental consideration 17 Mechanisms of interactions Hydrologic interactions between surface and subsurface waters occur by subsurface lateral flow through the unsaturated soil and by infiltration into or exfiltration from the saturated zones. In the case of karst or fractured terrain, interactions occur through flow in fracture/solution channels. Water that enters a surface-water body promptly, in response to such individual water input events as rain or snowmelt, is known as event flow, direct flow, storm flow, or quick flow.
Advances in the Research of Aquatic Environment: Volume 1 by G. Stournaras (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)