up to 1,100 m below the ground surface. Assessment of groundwater behavior at such depths is important in geoscience since depth of well screens for water abstraction is typically < 100 m below ground level
Vandebohede A, Lebbe L (2011) Heat transport in a coastal groundwater flow system near De Panne Belgium. J Hydrogeol 19:1225–1238 Article Google Scholar Vogelmann JE, Howard SM, Yang L, Larson CR, Wylie BK, Van Driel JN (2001) Completion of the 1990’s national land cover data se...
Iron is present in wells that are not near permeable soils or wells that are greater than 40 feet deep. Calcium, bicarbonate and total dissolved solids concentrations increase with well depth.University of Arkansas.Clayton, William Roane.
Deep groundwater is an important source of drinking water, and can be preferable to shallower groundwaters where they are polluted by surface-borne contaminants. Surface-borne contaminants are disproportionately common in ‘modern’ groundwaters that are
Near-surface water balance modeling is often used to evaluate land-atmosphere interactions, deep drainage, and groundwater recharge. The purpose of this st... BR Scanlon,M Christman,RC Reedy,... - 《Water Resources Research》 被引量: 249发表: 2002年 Hydraulic Characteristics and Nutrient Transp...
This trend, together with the increasing water demand for agricultural and urban development, as well as the growing tourism industry, is worsening water stress in the region and will increase further in the near future. In addition, the total population of this region is expected to increase ...
The quality of the aquifer water is represented by the resistivity values below the earth’s surface. Therefore, to depict a complete aquifer system including quality and quantity, respective resistivity prediction maps (Fig. 4a–c) were generated. The sigma values obtained are quite significant, ...
a[3] Capilla JE, Pulido-Velazquez D, Sahuquillo A, Andreu J. Solving the steady state groundwater flow equation for finite linear aquifer using a generalized Fourier series approach in two dimensional domains. Int J Numer Methods Eng [3) 教堂JE,波兰语Vela'zquez D, Sahuquillo对, Andreu...
In year 2010, the static level elevation configuration shows that the three possible water inlets to the aquifer mentioned in the dry season continue to be present, the first coming from the north of the aquifer, near Apaseo el Grande, where the flow continues until it reaches the municipality...
Five major groups of springs (Kalamionas, Kolymba, Vrysidia, Platanos, Varypetro) near the Agyia’s settlement (Figure 1) comprise the main discharge outlets for the karst aquifer [21,22]. They constitute a front of springs with a total water flow that ranges from 1.7 to 3.4 m3/s, ...