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Information Journal Paper

Title

PHYSICAL MODELING OF SUBSURFACE FLOW SYSTEM OF COLLECTION RIVER BED

Pages

  294-306

Abstract

 The type of rivers are dry or seasonal in arid or semiarid zone and current flowing through them is short or if there is no flow. One of the best methods to divert the flow in the river basin system is implementation with subsurface DRAINAGE network in the river bed A laboratory model for study the effects of hydraulic and geometric characteristics of the intake flow rate diversion was designed, Which the possibility measuring the inflow and outflow of diversion was considered.in this study were evaluated the effect of bed slope intake and diameter size of particle on diversion flow in two condition, water level constant and without control input discharge. The results showed that the slope of the porous medium tangible impact on current of deviation is in a state of constant water level. But the steep increase in input mode increases the deviation is negligible in Dubai. The 20% increase in diameter drains, in case the input of 9% and 20% in fixed alignment surface water DRAINAGE flow improves.The SPSS were using to obtain an equations that by them can estimate the diversion flow base of head flow hydraulic conductivity in POROUS MEDIA.

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  • Cite

    APA: Copy

    GHAVAMI, E., ESMAILI, K., & BEHSHTI, A.. (2016). PHYSICAL MODELING OF SUBSURFACE FLOW SYSTEM OF COLLECTION RIVER BED. IRANIAN JOURNAL OF IRRIGATION AND DRAINAGE, 10(3 ), 294-306. SID. https://sid.ir/paper/131681/en

    Vancouver: Copy

    GHAVAMI E., ESMAILI K., BEHSHTI A.. PHYSICAL MODELING OF SUBSURFACE FLOW SYSTEM OF COLLECTION RIVER BED. IRANIAN JOURNAL OF IRRIGATION AND DRAINAGE[Internet]. 2016;10(3 ):294-306. Available from: https://sid.ir/paper/131681/en

    IEEE: Copy

    E. GHAVAMI, K. ESMAILI, and A. BEHSHTI, “PHYSICAL MODELING OF SUBSURFACE FLOW SYSTEM OF COLLECTION RIVER BED,” IRANIAN JOURNAL OF IRRIGATION AND DRAINAGE, vol. 10, no. 3 , pp. 294–306, 2016, [Online]. Available: https://sid.ir/paper/131681/en

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