The Impact of Construction on the Discharge of Sareen Spa Springs Using Numerical Analysis and Zoning Map

Document Type : Research paper

Authors

1 department of civil eng., Islamic azad university, tabriz branch

2 Department of Earth Sciences, Faculty of Natural Sciences, University of Tabriz, Tabriz, Iran

3 Department of civil engineering, Shabestar Branch, Islamic Azad University, Shabestar, Iran

4 MSc, Manager of Omran Takamol Kav Company

Abstract

The purpose of the present study was to identify the irrigation canals of the spring springs in the city of Sarein and the impact of construction on the hot springs. In this regard, field studies were carried out based on geophysical experiments in the area with geoelectric and ground-penetrating radar devices and hot water mapping was prepared. Based on the results of these experiments, the hot-water trajectory penetrates the ground surface through vertical disruptions at elevated depths through vertical aquifers at specific depths, causing source springs to form. To determine resistivity parameters, soil type and depth of soil, two log wells were drilled at 25 and 30 m depths and groundwater level at 1.5 m depth. For numerical modeling of three modes without building and land alone, the building is present in 5, 10, 15, 20 and 25 stories at 10 to 210 m intervals with 10 m incremental step in static and dynamic modes. The analysis was done. For dynamical analysis, the Turkmanchai earthquake mapping was used and the analysis was performed in Plexis software. The dead and live loads are based on hotel-use buildings. Based on the results above, up to 70 m in the zoned map of the report indicated in red, construction was not permitted and within 80 m of the red border edge, shown in brown Given, it was detected for buildings up to 5 floors and 50 meters later for 10 floors and 30 meters later for 15 floors and then up to 20 floors.

Keywords


عابدینی، م.، 1392. بررسی سازندهای مقر شهر توریستی سرعین با تأکید بر وضعیت توپوگرافی، تکتونیک و اقلیم جهت کاربری بهینه اراضی شهری با استفاده ازGIS، جغرافیــــا وبرنامــــه­ریــــزی محیطــــی ســال 24 ،پیــاپی 49 ، شــماره 1.
ویسی، ر.، حسینی، س.ع.، معصومی، د.، محمدی، م.، 1393. مکان‌یابی بهینه توسعه مجتمع‌های آب‌درمانی در شهر سرعین، فصلنامه پژوهش‌های بوم‌شناسی شهری، دوره پنجم، پیاپی 9، شماره 1.
Billi. A., 2005. Grain size distribution and thickness of breccia and gouge zones from thin less than 1m strike-slip fault cores in limestone. Journal of Structural Geology. 27: 1823–1837.
Caine, S. J., Coates, D. R., Timoffeef, N. P., Davis, W. D., 1991. Hydrogeology of the Northern Shawangunk Mountains: New York State Geological Survey Open-File Report. 72 : 782-795. Fabozi, S., Porchia, A.,Fierro, T., Edoardo A., Pagliaroli, A., Moscatellia, M. 2020. Seismic compression susceptibility in dry loose sandy and silty soil in a seismic microzonation perspective, Engineering  Geology. 264: 78-90.
Guo, Q. 2012. Hydrogeochemistry of high-temperature geothermal systems in China: A review. Applied Geochemistry. 27: 1887-1898.
 Chandrajith, R., Johannes, A.C., Barth, N.D., Subasinghe, M., Dirk Merten, C.B. 2013. Geochemical and isotope characterization of geothermal spring waters in Sri Lanka: Evidence for steeper than expected geothermal gradients. Journal of Hydrology. 476: 360-369.
Kazemi, G.A., Lehr, J.H., Perrochet, P. 2006. Groundwater Age. John Wiley & Sons, p. 125-164.
Margiotta, S., Mongelli, G., Summa, V. Paternoster, M., Fiore, S. 2012. Trace element distribution and Cr (VI) speciation in Ca-HCO3 and Mg-HCO3 spring waters from the northern sector of the Pollino massif, southern Italy. Journal of Geochemical Exploration. 115: 1-12.
Shakeri, A., Moore, F., Kompani-zare, M. 2008. Geochemistry of the thermal springs of Mount Taftan, southeastern Iran. Journal of Volcanology and Geothermal Research. 178: 829-836.
Shamsi. A., Kazemi, G.A. 2014.A review of research dealing with isotope hydrology in Iran and the first Iranian meteoric water line. Geopersia. 4:73-86.