Professor of aerospace engineering and Francis Chair of Excellence Joe Majdalani serves as the GHS director of honors and awards. “We are delighted to see the recognition and support provided by the AIAA Greater Huntsville Section to our alumni, who are clearly developing into leaders in the area, as well as our students who we expect to be leaders in the future.” Tracie Prater of the AIAA's Greater Huntsville Section, with Joe Majdalani. “At Auburn University, we work hard to deliver a world-class education in aerospace engineering and take great pride in Auburn’s significant contributions to the aerospace profession, particularly in the Huntsville region,” said Brian Thurow, aerospace engineering department chair and the W. Jayme Allgood, who earned a bachelor’s degree in aerospace engineering in 2009, was named the Earl Pearce Professional of the Year. Kevin Albarado, who earned bachelor’s and master’s degrees in aerospace engineering in 20, is the Ed Pruett Young Professional of the Year. Jordan Holland, a recent graduate at Sparkman High School in Harvest, Alabama, will begin her pursuit of an aerospace engineering degree this fall and was named the 2023 Robert L. Charles Smith, a rising sophomore in aerospace engineering, earned the 2022 Robert L. Cody Shelton, who is pursuing a PhD in aerospace engineering, was named Graduate Student of the Year. Yadav GS, Abolfazil (1998) Geoelectrical soundings and their relationship to hydraulic parameters in semi-arid regions of Jalore, north-western India.Three Auburn Engineering students, two alumni, a faculty member and a future student earned key honors by the American Institute of Aeronautics and Astronautics Greater Huntsville Section (GHS) at its annual awards dinner on May 20.Ĭolin Bamford, who earned a degree in aerospace engineering this spring, was named Undergraduate Student of the Year. Shahid S, Nath SK, Sircar A, Patra HP (1999) Estimation of model parameters from one-dimensional vertical electrical sounding data using evolutionary programming technique. Department of Geology & Geophysics, Indian Institute of Technology, Kharagpur, India, 62 pp Roy A, Niyogi D (1961) Geological and geophysical investigation for ground water around Hijli, Dt. Raghunath HM (1987) Groundwater, 2nd edn. Niwas S, Singhal DC (1981b) Aquifer transmissivity of porous media from resistivity data. Niwas S, Singhal DC (1981a) Estimation of aquifer transmissivity from Dar-Zarrouk parameters in porous media. Kosinski WK, Kelly EW (1981) Geoelectrical sounding for predicting aquifer properties. Kelly WE (1977) Gcoelcctric sounding for estimating aquifer hydraulic conductivity. Heigold PC, Gilkeson RH, Cartwright K, Reed PC (1979) Aquifer transmissivity from surficial electrical methods. Hantush MS, Jacob CE (1955) Nonsteady radial flow in an infinite leaky aquifer. Hantush MS (1956) Analysis of data from pumping tests in leaky aquifer. Consultancy Project Report, I.I.T., Kharagpur, 63 ppĭomenico PA, Schwartz FW (1990) Physical and chemical hydrogeology. Keywordsīandopadhyay M, Dikshit AK, Patra HP (2000) The geophysical and hydrological studies on River beds of Ajoy and Damodar (Bardhaman District) for the design of collector well. A contour can also be drawn for hydraulic conductivity and transmissibility for the area. Now, if the entire area is surveyed by VES and the T′ and F are calculated for each point, the hydraulic conductivity ( K) and transmissibility ( T) can be found out using the relations for the entire area of investigation. Then, a straight-line relation between transmissibility and transverse resistance and hydraulic conductivity and formation factor is brought out. Transverse resistance ( T′) and formation factors ( F) are calculated from all the VES results. Vertical electrical sounding (VES) is carried out near the boreholes. The T and K are calculated in these boreholes with the help of pump test. In this process, a few drillings are carried out in the area of investigation. As the drilling and pumping tests are expensive, time-taking and laborious geoelectrical measurements are used for alternate approach to estimate the aquifer characteristics. From this curve, T and S values are calculated by different methods. During pumping test, a time–drawdown curve is generated. The transmitting capacity for the entire thickness is known as transmissibility ( T), and storage coefficient ( S) of an aquifer is the volume of water discharged through unit prismatic volume. The hydraulic conductivity of an aquifer is its capacity to transmit and to yield it. The terms hydraulic conductivity ( K), transmissibility ( T) and storage coefficient ( S) are useful for computation of yield.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |