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Wednesday, August 25, 2021 | History

2 edition of Hydrogeological investigation of Khor Arbaat basin found in the catalog.

Hydrogeological investigation of Khor Arbaat basin

Mohammed Tahir Hussein

Hydrogeological investigation of Khor Arbaat basin

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  • 31 Currently reading

Published by Democratic Republic of the Sudan, Geological & Mineral Resources Dept. in [Khartoum] .
Written in English

    Places:
  • Sudan.
    • Subjects:
    • Hydrology -- Sudan.

    • Edition Notes

      Bibliography: p. 160-161.

      Other titlesKhor Arbaat basin.
      Statementby Mohammed Tahir Hussein.
      SeriesBulletin - The Democratic Republic of the Sudan, Geological & Mineral Resources Department ;, no. 28
      Classifications
      LC ClassificationsGB806 .H88 1975
      The Physical Object
      Paginationii, 161 p., [7] fold. leaves of plates :
      Number of Pages161
      ID Numbers
      Open LibraryOL4533691M
      LC Control Number76980690

      As availability of hydrogeological data were limited for groundwater balance analysis, important data like annual and monthly groundwater recharges were estimated using (Thornthwaite-Mather, , ) study was conducted at fourteen sub basins of Upper Awash Basin which are located at the western escarpment of the Great East. The Rabigh basin was delineated and the drainage Marr and northern Hajer sub-basins. On the other hand, network has been extracted at selected grids of 2 km and the southern tributaries network of Hajer sub-basin,2 10 km. Subsequently, the basin has further been emerged from southeastern and southwestern boundaries,2.


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Hydrogeological investigation of Khor Arbaat basin by Mohammed Tahir Hussein Download PDF EPUB FB2

Hydrogeological investigation, were employed to characterize the hydrogeological setting and to determine the hydraulic properties of the aquifer system of Khor Adeit basin in the Red Sea State in eastern Sudan. Sixty five (VES) were conducted in the stream channels using.

Hussein MT () Hydrogeological investigation of Khor Arbaat Basin, Printed by Sudan Survey Department, Khartoum Kruseman GP, Ridder NA () Analysis and evaluation of pumping test data. International Institute for Land Reclamation and Improvement, Wageningen, The NetherlandsCited by: 6.

Hussein MT () Hydrogeological investigation of Khor Arbaat Basin, Printed by Sudan Survey Department, Khartoum Kruseman GP, Ridder NA () Analysis and evaluation of pumping test ted Reading Time: 9 mins.

Area of ground water basin is: Km 2, Km 2. inside the Jordan boarder and K. 2 in the Syrian par. Basin extend The basin extends from the southern part of Jebel El-Arab. The investigation also revealed the presence of a confined aquifer in the area, with resistivity values of Ωm, while the depth of the aquifer ranged between and m.

The average values of the groundwater characteristics obtained were mSm for electrical conductivity, mgm 3 for total dissolved solids, m Cited by: Hussein MT () Hydrogeological investigation of Khor Arbaat Basin, Printed by Sudan Survey Department, Khartoum Kruseman GP, Ridder NA () Analysis and evaluation of pumping test data.

The Great Artesian Basin (GAB) is one of Australia's most significant hydrogeological entities covering more than million square kilometres, underlying parts of Queensland, New South Wales. The investigations involved hydrogeological, geophysical field investigations and a detailed desk study in which the available relevant geological and hydrogeological data were collected, analyzed, collated and evaluated within the context of the Client's requirements.

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The high mean annual potential evapotranspiration which is higher than precipitation resulted in mean water loss of about 28 10 9 m.

requirements for hydrogeological investigations. The checklist (Table 1 in Section ) outlines specific study requirements depending on the type of development application. Section 3 provides a short description of report expectations, report components, as well as some of the resources available.

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The basin is characterized by different volcanic formations covered by thick alluvial and residual Quaternary sediments at the center of the basin around Lake Tana. In this study, an attempt was made to outline the hydrogeology of the basin based on limited information from well lithologic logs and previous relevant works.

hydrogeological massifs and artesian basins. They differ by physical, geographical, hydrogeological and geological structural conditions. The major part of geothermal resources is associated with sedimentary basins which cover nearly 60 of Kazakhstan territory. This paper seeks to review the current knowledge of the geology and hydrogeology of the Botany Basin, and focuses on how the latter impacts on its geomechanical behaviour.

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The quantity of the surface waters is very small compared with the surface area of the basin, however, due to the shortage of precipitation in. The Khor Arbaat basin is the main source of potable water supply for the more thaninhabitants of Port Sudan, eastern Sudan.

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A multi-criteria approach was used in the assessment of the basin granitoids including; electrical resistivity survey, pumping test and water quality analysis. A total of twenty-five (25) representative boreholes were drilled, developed and pumped; obtaining data for aquifer hydraulic.

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laneous Geologic Investigations Map A). As work on the quadrangles progressed, geologist, companies, and governments working in areas adjacent to the Kingdom of Saudi Arabia were consulted by Aramco and invited to participate in the mapping project.

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These investigations also included the. Upper Awash basin is located at the transient of the Main Ethiopian Rift (MER) and the central highlands. The study area is confined within the limits of 8°159°15N and 3839°15E. It occupies a total area of ab km 2. The basin has all the three major physiographic zones: rift, escarpment and highlands.

In basin-fill sediments, changing depositional environments over short distances may result in substantial facies changes that can affect transmissivity and hydraulic conductivity, particularly where silt and clay become intermixed or interbedded with sand and gravel (Plume, ). In volcanic rocks, a characteristic change from lava flows to.

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The upper Housatonic River basin covers an area of about square miles in western Connecticut and includes the towns of Bridgewater, Brookfield, Canaan, Cornwall, Kent, New Fairfield, New Hilford, North Canaan, Salisbury, Sharon, Sherman and Warren and parts of Bethel, Bethlehem, Danbury, Goshen, Litchfield, Morris, Newtown, Norfolk, Ridgefield, Roxbury, Southbury, Torrington and Washington.

Thus, part of the feeding water of the Kufra basin may flow away toward the Dakhla basin and the Mediterranean Sea across the Sarir basin. The observed groundwater depletion over zone 2 was estimated at ± mmyr ( ± km 3 yr), whereas the average groundwater extraction rate is ± mmyr ( ± km 3.

The basin area is consisted of different rock types of various geological ages, ranging from Proterozoic to Quaternary (Sen et al. ; Geological Survey of India, ). Most of the basin area is covered with granitic gneiss () followed by micha schist () and hornblende schist () of CGGC.

Distribution of clay with caliche. A detailed hydrocensus was conducted as part of the hydrogeological investigation whereby properties within a 2km radius of Alternative 2 were visited.

During the visit, details including water use type, volumes, water levels and coordinates were obtained. In total, 16 boreholes were identified surrounding Alternative 2 including the boreholes. The hydrogeology and water quality of the Chakari Basin, a square-kilometer (km2) watershed near Kabul, Afghanistan, was assessed by the U.

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