THE INVESTIGATION OF FLOODING BY PERMIBEABILITY & RUNOFF POTENTIAL DETERMINING OF GEOLOGY FORMATION IN DRAINAGE BASINS (A CASE STUDY IN KARDEH DRAINAGE AREA KHORASAN-E RAZAVI PROVINCE)

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NADERSEFAT M.H.; SAIDIYAN F.

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Journal: GEOGRAPHY Year:2010 | Volume:4 | Issue:12 Page(s): 163-198

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Title

THE INVESTIGATION OF FLOODING BY PERMIBEABILITY & RUNOFF POTENTIAL DETERMINING OF GEOLOGY FORMATION IN DRAINAGE BASINS (A CASE STUDY IN KARDEH DRAINAGE AREA KHORASAN-E RAZAVI PROVINCE)

Author(s)

NADERSEFAT M.H. | SAIDIYAN F. | Issue Writer Certificate

Keywords

FLOODINGQ2

PERMEABILITYQ3

LITHOLOGY UNITSQ3

GEOLOGICAL FORMATIONSQ2

SURFACE DETENTIONQ3

RUNOFF POTENTIALQ3

KARDEH BASINQ3

ARC-GIS SOFTWAREQ3

Abstract

The process of soil erosion and FLOODING are the main problems which permanently endangers a drainage area. The PERMEABILITY and RUNOFF POTENTIAL determining of geology formations is very important for estimating the danger of drainage areas FLOODING in order to establishing engineering structures for preventing flood and soil erosion. The purpose of this study is to prepare a map of FLOODING in Kardeh drainage area. This map would be main source for performing the executive operation, soil protection study and future plans in drainage areas. The Kardeh drainage area is located on the northeast of Iran and north of Khorasan Razavi province with 557, 9 squares kilometer extension. Since the FLOODING parameter is a great factor in soil protection process and prevention of erosion, its approximate control has a significant role in comprehensive management in drainage areas. Because of this the study of FLOODING in the mentioned area will perform through the PERMEABILITY and RUNOFF POTENTIAL determining of geologies formations. According to this approach the geological plan is prepared with ARC-GIS SOFTWARE in 1:20000 scales and there are formed varieties of rocks and type of identify fossils this basin. The then with using of geological map, PERMEABILITY map in the area and extents in 1:20000 scales has prepared. Firstly, the SURFACE DETENTION parameters and mean annual precipitation in the area estimated and according to that the S and P maps prepared in order to preparing the areas runoff map. According to the mentioned maps information the RUNOFF POTENTIAL map of the area prepared and then composed with the geological map to identify the runoff rate in any work unit. Finally, with comparison of PERMEABILITY map and RUNOFF POTENTIAL map, the FLOODING map in scale 1:20000 prepared. With regard to the genus of the formed rocks priority in FLOODING point of view. The Lithology the Nm, Ksh, Kshs, and Jka have low PERMEABILITY and are in the first PERMEABILITY and they locate in the second priority. At least the units of Jmz2, Jmz1, Q, Qa1, Qt2 and Qt1 Lithology have high PERMEABILITY and in FLOODING they are in the third priority.

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APA: Copy

NADERSEFAT, M.H., & SAIDIYAN, F.. (2010). THE INVESTIGATION OF FLOODING BY PERMIBEABILITY & RUNOFF POTENTIAL DETERMINING OF GEOLOGY FORMATION IN DRAINAGE BASINS (A CASE STUDY IN KARDEH DRAINAGE AREA KHORASAN-E RAZAVI PROVINCE). GEOGRAPHY, 4(12), 163-198. SID. https://sid.ir/paper/208000/en

Vancouver: Copy

NADERSEFAT M.H., SAIDIYAN F.. THE INVESTIGATION OF FLOODING BY PERMIBEABILITY & RUNOFF POTENTIAL DETERMINING OF GEOLOGY FORMATION IN DRAINAGE BASINS (A CASE STUDY IN KARDEH DRAINAGE AREA KHORASAN-E RAZAVI PROVINCE). GEOGRAPHY[Internet]. 2010;4(12):163-198. Available from: https://sid.ir/paper/208000/en

IEEE: Copy

M.H. NADERSEFAT, and F. SAIDIYAN, “THE INVESTIGATION OF FLOODING BY PERMIBEABILITY & RUNOFF POTENTIAL DETERMINING OF GEOLOGY FORMATION IN DRAINAGE BASINS (A CASE STUDY IN KARDEH DRAINAGE AREA KHORASAN-E RAZAVI PROVINCE),” GEOGRAPHY, vol. 4, no. 12, pp. 163–198, 2010, [Online]. Available: https://sid.ir/paper/208000/en

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