Design of Flood Drainage in Golgohar Iron Ore Mine#3
Source: By:Saeid Maknouni Gilani
DOI: https://doi.org/10.30564/hsme.v1i1.1255
Abstract:The iron ore minerals reservoir of Golgohar Mine#3 is more than 660 million tons. It is the biggest in Iran and rate of ore extraction is more than 15 million tons per year. The pit takes place on the way of runoff pathway of this watershed and it needs an especial strategy for conserving the pit mine during next imminent floods. The area of Mine# 3 watershed is 20785700 square meters and its general slope in its topography map is 0.59 percent; then initial scheming indicates it can causes a great deal of problems for mining operation n the next floods; particularly, the pit is located into degree 4th sub branch of a main ephemeral river. For this purpose, the Soil Conservation Service Curve Number (SCS) method was employed to estimate intervals period of next floods based on the magnitude, the intensity and the duration of precipitation events data. Conceptual design of runoff drainage of the watershed was designed to lead the flood to a better pathway location. The Mine#3 overburden deposition occupies a huge area on the watershed; and it has been considered and redesigned in terms of size, form, dimensions and location to manage as a physical obstacle against next floods. Hydraulic calculations were applied for designing two essential open channels which can preserve the pit.
References:[1] Agard P, Omrani J, Jolivet L, Mouthereau F. Convergence history across Zagros (Iran): constraints from collisional and earlier deformation. International Journal of Earth Sciences, 2005, 94: 401-419. [2] Alric G, Virlogeux D. Pétrographie et géochimie des roches métamorphiques et magmatiques de la région de Deh Bid-Bavanat, Chaîne de Sanandaj–Sirjan, Iran. Thése 3éme cycle, Université Scientifique et Médicale de Grenoble. France, 1977: 316. [3] Azizi H, Jahangiri A. Cretaceous subduction-related volcanism in the northern Sanandaj-Sirjan Zone, Iran. Journal of Geodynamics, 2008, 45: 178-190. [4] Babaie HA, Ghazi AM, Babaei A, La Tour TE, Hasanipak AA. Geochemistry of arc volcanic rocks of the Zagros Crush Zone, Neyriz, Iran. Journal of Asian Earth Science, 2001, 19: 61-76. [5] Berberian F, Berberian M. Tectono-plutonic episodes in Iran. In: Gupta HK, Delany FM (eds.) Zagros, Hindukosh, Himalaya geodynamic evolution. American Geophysical Union Washington, 1981, 5-32. DOI: 10.1029/GD003p0005 [6] Berberian M, King GCP. Towards a paleogeography and tectonic evolution of Iran. Can. J. Earth Sciences, 1981, 18: 210-265 [7] Berberian M, Nogol M . Preliminary explanation text of the geology of Deh Sard and Khabr maps with some remarks on the metamorphic complexes and the tectonics of the area (two geological maps, 1/100000 from the Hajiabad quadrangle map). Geological Survey of Iran. internal report 1-60, 1974. [8] Braud J. Geological map of Kermanshah 1/250000 scale. Geological Survey of Iran, 1978. [9] Davoudzadeh M, Soffel HC, Schmidt K. On the rotation of the Central-East Iran microplate. N Jb Geol Palaont Mh, 1981, 3: 180-192. [10] Dewey JF, Pitman WC, Ryan WBF, Bonnin J. Plate tectonics and the evolution of the Alpine system. Geological Society of America Bulletin, 1973, 84: 3137-3180. [11] Dimitrijevic MD. Geology of Kerman Region. Geological Survey of Iran, 1973, 72: 52-334. [12] Forster H. Continental drift in Iran in relation to the Afar structures. In: Pilger A, Rosler A (eds), Afar between continental and oceanic rifting (VII). Schweizerbatsche Varlagsbuchhandlung, Stuttgart, 1976:182-190. [13] Omrani J, Agard P, Whitechurch H, Benoit M, Prouteau G, Jolivet L. Arc-magmatism and subduction history beneath the Zagros Mountains, Iran: A new report of adakites and geodynamic consequences. Lithos, 2008, 106: 380-98. [14] Sabzehei M. Les mélanges ophiolitiques de la région d’Esfandagheh (Iran meridonal) étude pétrologique et structural, interpré- tation dans le cadre iranien, Thèse d’État, Université de Grenoble, 1974. [15] Stocklin J. Possible ancient continental margins in Iran. In: Burk CA, Drake CL (Eds.), The geology of continental margins.Springer, Berlin, 1974: 873-887. [16] Taraz H. Geology of the Surmaq-Deh Bid area, Abadeh region, Central Iran, Geological Survey of Iran, Report , 1974, 37: 37: 148. [17] Maknouni Gilani S, Zare M and Raeisei E. Determining the hard rock groundwater pathway in Golgohar complex formation using hydrochemical data in AHP. Arabian Journal of Geosciences, 2018. DOI: org/10.1007/s12517-018-3472-z, 11:172 [18] Maknouni Gilani S, Zare M and Raeisei E. Locating a New Drainage Well by Optimization of a Back Propagation. Mine Water and the Environment, 2019. DOI: org/10.1007/s10230-019-00593-6