Hydro-geophysical configuration for the quaternary aquifer of Nuweiba alluvial fan.

Nuweiba is one of Egypt’s strategic marine harbors and tourist sites located on the western coast of the Gulf of Aqaba. The absence of freshwater resources in Nuweiba necessitates investigations of local groundwater aquifers. Determination of the hydro-geophysical parameters of the Nuweiba alluvial fan constitutes the basic foundation for optimizing groundwater exploitation over time. Fifteen Schlumberger vertical electrical soundings (maximum AB∕2=1,001.5m), augmented by borehole stratigraphic data, aquifer tests, hydro-chemical analysis, and numbers of measured and/or calculated hydraulic parameters, were carried out in the study area. The fresh to brackish aquifer of Quaternary and pre-Quaternary alluvium sediments was effectively delineated with true resistivity and thickness ranges of 93–125ohm‐m and 0.5–4.5m, respectively. The western part of the aquifer has a large volume of fresh ground water for extraction and is characterized by a gradual increase in thickness (4.5m), grain size, transmissivity ...

[1]  M. Wyllie,et al.  Application of the Kozeny Equation to Consolidated Porous Media , 1950, Nature.

[2]  M. R. J. Wyllie,et al.  Application of Electrical Resistivity Measurements to Problem of Fluid Flow in Porous Media , 1952 .

[3]  Kym Anderson,et al.  Arab Republic of Egypt , 2000, Intellectual Property Laws of the Arab Countries.

[4]  A. Oteri Geoelectric investigation of saline contamination of a chalk aquifer by mine drainage water at Tilmanstone, England , 1981 .

[5]  C. V. Theis The relation between the lowering of the Piezometric surface and the rate and duration of discharge of a well using ground‐water storage , 1935 .

[6]  William E. Kelly,et al.  A hydrogeophysical model for relations between electrical and hydraulic properties of aquifers , 1985 .

[7]  P. K. Weyl,et al.  Influence of Texture on Porosity and Permeability of Unconsolidated Sand , 1973 .

[8]  F. Mostaghimi,et al.  ESSAIS DE DÉTERMINATION DU COEFFICIENT D'EMMAGASINEMENT EN NAPPE LIBRE APPLICATION A LA NAPPE ALLUVIALE DU RHIN , 1969 .

[9]  A. Zohdy The auxiliary point method of electrical sounding interpretation, and its relationship to the Dar Zarrouk parameters , 1965 .

[10]  W. Kelly,et al.  The relation between hydraulic transmissivity and transverse resistance in a complicated aquifer of glacial outwash deposits , 1985 .

[11]  D. C. Singhal,et al.  Estimation of aquifer transmissivity from Dar-Zarrouk parameters in porous media , 1981 .

[12]  C. Singh,et al.  Some geoelectrical investigations for potential groundwater zones in part of Azamgarh area of U.P. , 1970 .

[13]  P. Carman Fluid flow through granular beds , 1997 .

[14]  D. Urish,et al.  Electrical resistivity—hydraulic conductivity relationships in glacial outwash aquifers , 1981 .

[15]  A. R. Gregory,et al.  Formation Factors of Unconsolidated Porous Media: Influence of Particle Shape and Effect of Cementation , 1953 .

[16]  A. Zohdy Use of Dar Zarrouk curves in the interpretation of vertical electrical sounding data , 1974 .

[17]  H. Flathe,et al.  A PRACTICAL METHOD OF CALCULATING GEOELECTRICAL MODEL GRAPHS FOR HORIZONTALLY STRATIFIED MEDIA , 1955 .

[18]  G. Kruseman,et al.  Analysis and Evaluation of Pumping Test Data , 1983 .

[19]  F. M. Perkins,et al.  RESISTIVITY OF SANDSTONES AS RELATED TO THE GEOMETRY OF THEIR INTERSTITIAL WATER , 1956 .

[20]  D. T. Smith,et al.  Resistivity-porosity-particle shape relationships for marine sands , 1978 .

[21]  D. L. Campbell MODEL FOR ESTIMATING ELECTRIC MACROANISOTROPY COEFFICIENT OF AQUIFERS WITH HORIZONTAL AND VERTICAL FRACTURES , 1977 .

[22]  J. R. Schopper,et al.  A THEORETICAL INVESTIGATION ON THE FORMATION FACTOR/PERMEABILITY/POROSITY RELATIONSHIP USING A NETWORK MODEL* , 1966 .

[23]  K. Sundberg Effect Of Impregnating Waters On Electrical Conductivity Of Soils And Rocks , 1980 .

[24]  R. Maillet THE FUNDAMENTAL EQUATIONS OF ELECTRICAL PROSPECTING , 1947 .

[25]  R. Frohlich COMBINED GEOELECTRICAL AND DRILL‐HOLE INVESTIGATIONS FOR DETECTING FRESH‐WATER AQUIFERS IN NORTHWESTERN MISSOURI , 1974 .

[26]  A. Zohdy Automatic interpretation of Schlumberger sounding curves, using modified Dar Zarrouk functions , 1975 .

[27]  A. Corey,et al.  Mechanics of heterogeneous fluids in porous media. , 1977 .

[28]  Sri Niwas,et al.  Aquifer transmissivity of porous media from resistivity data , 1985 .

[29]  Empirical relation between electrical transverse resistance and hydraulic transmissivity , 1984 .

[30]  W. O. Winsauer,et al.  Resistivity of Brine-Saturated Sands in Relation to Pore Geometry , 1952 .

[31]  Ernesto Orellana Properties and drawing of the so-called Dar Zarrouk curves , 1963 .

[32]  P. Worthington Quantitative geophysical investigations of granular aquifers , 1975 .

[33]  H. Flathe POSSIBILITIES AND LIMITATIONS IN APPLYING GEOELECTRICAL METHODS TO HYDROGEOLOGICAL PROBLEMS IN THE COASTAL AREAS OF NORTH WEST GERMANY , 1955 .

[34]  D. A. Morris,et al.  Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60 , 1966 .

[35]  M. S. Paterson,et al.  The equivalent channel model for permeability and resistivity in fluid-saturated rock—A re-appraisal , 1983 .

[36]  D. Marsden THE AUTOMATIC FITTING OF A RESISTIVITY SOUNDING BY A GEOMETRICAL PROGRESSION OF DEPTHS , 1973 .

[37]  J. Maxwell A Treatise on Electricity and Magnetism , 1873, Nature.

[38]  G. E. Archie The electrical resistivity log as an aid in determining some reservoir characteristics , 1942 .

[39]  Harold M. Mooney,et al.  A RESISTIVITY COMPUTATION METHOD FOR LAYERED EARTH MODELS , 1966 .

[40]  Adel A.R. Zohdy,et al.  Application of surface geophysics to ground-water investigations , 1980 .

[41]  Á. Kézdi,et al.  Handbook of soil mechanics , 1982 .

[42]  Domenico Patella,et al.  A NUMERICAL COMPUTATION PROCEDURE FOR THE DIRECT INTERPRETATION OF GEOELECTRICAL SOUNDINGS , 1975 .