Geophysical Results of Main Barton Springs and their implications on the groundwater flow pattern into Barton Springs Pool, Austin, Texas

2015 ◽  
Author(s):  
Mustafa Saribudak* ◽  
Nico Hauwert
Keyword(s):  
Groundwater Flow ◽  
Flow Pattern ◽  
Barton Springs

Determination of Landslide Potential in Trangkil Gunung Pati Based on Groundwater Flow Pattern

2017 ◽  
Vol 23 (7) ◽  
pp. 6635-6637 ◽  
Author(s):  
Tony Yulianto ◽  
Rahmat Gernowo ◽  
Sugeng Widada
Keyword(s):  
Groundwater Flow ◽  
Flow Pattern

scholarly journals UNCONFINED GROUNDWATER FLOW PATTERN AND FACIES CHANGES AT WAY HUWI VILLAGE, SOUTH LAMPUNG

2020 ◽  
Vol 30 (1) ◽  
pp. 109
Author(s):  
Luhut Pardamean Siringoringo ◽  
Sandi Maulana
Keyword(s):  
Groundwater Flow ◽  
Flow Pattern ◽  
Water Table ◽  
Flow Patterns ◽  
Research Area ◽  
Piper Diagram ◽  
Change Pattern ◽  
Lower Elevation ◽  
Facies Change

Way Huwi Village is located in South Lampung, near the Institut Teknologi Sumatera (ITERA). The purposes of this research is to know the unconfined groundwater flow pattern and groundwater facies changes. We measured the depth of water table at nine dig wells, analyzed piper diagram for groundwater facies identification. Then, we integrated groundwater flow patterns and groundwater facies from each well to analyze groundwater facies change pattern in research area. The result indicated that the unconfined groundwater flows from SW to NE of research area, following higher (SW) to lower elevation (NE). There are six patterns of unconfined groundwater facies changes: from Facies Na-Cl to Facies Na-HCO3-Cl, Facies Na-HCO3-Cl to Facies Ca-Mg-HCO3, Facies Na-HCO3-Cl to Facies Na-Cl, Facies Na-HCO3-Cl to Facies Na-SO4-Cl, Facies Ca-Mg-HCO3 to Facies Na-SO4-Cl, and Facies Ca-Mg-HCO3 to Facies Na-HCO3-Cl. ABSTRAK - Pola aliran airtanah tidak tertekan dan perubahan fasiesnya di Desa Way Huwi, Lampung Selatan. Desa Way Huwi terletak di Lampung Selatan, di dekat Institut Teknologi Sumatera (ITERA). Tujuan dari penelitian ini adalah untuk mengetahui perubahan pola aliran airtanah dan fasies airtanah yang terjadi. Kami mengukur kedalaman muka airtanah pada sembilan sumur gali, menganalisis Diagram Piper untuk mengetahui fasies airtanah. Kemudian kami mengintegrasikan pola aliran airtanah dan fasies airtanah setiap sumur untuk mengetahui pola perubahan fasies air tanah. Hasil analisa menunjukkan bahwa airtanah tidak tertekan mengalir dari Barat Daya ke Timur Laut mengikuti ketinggian yang lebih tinggi (SW) ke ketinggian yang lebih rendah (NE). Ada enam pola perubahan fasies airtanah tidak tertekan: dari Facies Na-Cl ke Facies Na-HCO3-Cl, Facies Na-HCO3-Cl ke Facies Ca-Mg-HCO3, Facies Na-HCO3-Cl ke Facies Na-Cl, Facies Na -HCO3-Cl ke Facies Na-SO4-Cl, Facies Ca-Mg-HCO3 ke Facies Na-SO4-Cl, dan Facies Ca-Mg-HCO3 ke Facies Na-HCO3-Cl

The Use of Environmental Isotope Techniques together with Conventional Methods in Regional Groundwater Studies

1976 ◽  
Vol 7 (2) ◽  
pp. 81-94
Author(s):  
Guttormur Sigbjarnarson ◽  
Pall Theodorsson ◽  
Bragi Arnason
Keyword(s):  
Groundwater Flow ◽  
Flow Pattern ◽  
Environmental Isotopes ◽  
Geological Exploration ◽  
Environmental Isotope ◽  
Mountain Ranges ◽  
Geological Conditions ◽  
Groundwater Systems ◽  
Regional Groundwater ◽  
Perched Aquifers

Regional hydrological investigations of the subsurface drainage in the neovolcanic area around lake Thorisvatn on the central Icelandic plateau have been carried out as well as geological exploration. Environmental isotopes, deuterium and tritium, proved decisive in finding the groundwater flow pattern and in separating the different groundwater systems and explaining local deviations as barriers and perched aquifers. The regional groundwater flow is only slightly dependent on the. topography but highly on the geological conditions, as it virtually flows under mountain ranges as well as under the river Tungnaa.

scholarly journals Evaluation of Topsoil Competence, Aquifer Types, Groundwater Prospect and Flow Pattern using Geoelectric Characterization for Part of Ogbomoso, Nigeria

2021 ◽  
Vol 7 (2) ◽  
Author(s):  
O. G. Bayowa
Keyword(s):  
Groundwater Flow ◽  
Flow Pattern ◽  
Flow Direction ◽  
Groundwater Potential ◽  
Water Levels ◽  
Groundwater Prospect ◽  
Southwestern Nigeria ◽  
Fractured Bedrock ◽  
Resistivity Method ◽  
Weathered Layer

Part of Ogbomoso Southwestern Nigeria was assessed using electrical resistivity method with a view to obtaining the subsurface geoelectric parameters (resistivities and thicknesses), categorizes the topsoil into different competence zones and evaluates the aquifer types, groundwater prospect and flow pattern. Fifty-four Vertical Electrical Sounding (VES) data were quantitatively interpreted using the partial curve matching technique to obtain the preliminary layer parameters which were further refined through 1-D forward modelling WinResist software package. The resulting final layer parameters were used to generate 2D geoelectric sections, isopach and isoresistivity maps and subsequently used to categorize the study area into different topsoil Competence, Aquifer types and Groundwater Potential zones. Static water levels of hand-dug wells in the area were used to generate the groundwater flow pattern. Four subsurface geoelectric layers were delineated. These were the topsoil, laterite, weathered/partly weathered layer (main aquifer) and fractured/fresh bedrock. The resistivities and thicknesses of the layers were 76-1858, 649-2021, 17-880 and 260-33385 Ωm and 0.4-4, 0.7-1.9 and 1.9-25.2 m respectively. The groundwater flow pattern in the area was NE-SW. The study concluded that incompetent to highly competent topsoil, weathered bedrock (main) aquifer unit/partly weathered/fractured bedrock aquifer and generally low groundwater potential with NE-SW flow direction underlay the study area.

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