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Separation of surface flow from subsurface flow in catchments using runoff coefficient

Ardekani A. Afshar, Sabzevari T., Haghighi A. Torabi, Petroselli A.

Acta Geophysica

2021

Vol. 69, no. 6

2363--2376

Separating surface flow (SF) from subsurface flow (SSF) based on direct runoff measurements in river gauges is an important issue in hydrology. In this study, we developed a simple and practical method, based on runoff coefficient (RC), for separating SF from SSF. RC depends mainly on soil texture, land use and land cover, but we also considered the effect of slope and rainfall intensity. We assessed our RC-based method for three different soil types by comparing the value obtained with laboratory rainfall simulator data. The correlation coefficient between observed and calculated data exceeded 0.93 and 0.63 when estimating SF and SSF, respectively. The method was then used to separate SF and SSF in two catchments (Heng-Chi and San-Hsia) in Northern Taiwan, and the results were compared with those produced by the geomorphological instantaneous unit hydrograph (GIUH) model. Test revealed that, if RC is calculated accurately, the proposed method can satisfactorily separate SF from SSF at catchment scale.

Rozdział przepływu na przelewie gabionowym

Bajkowski S.

Przegląd Naukowy Inżynieria i Kształtowanie Środowiska

2006

Vol. 15, No. 2

113--120

The water level on the hydraulic structures is maintained by means of permanent or gated weirs. Conventional permanent dams are made with impermeable sills. Gated weirs are installed in rivers with low sills; the head of water on these objects is kept by movable closures. The constant concrete weirs’ role can be ful-filled also by the permeable rubble mound weirs. In the permeable stone weirs part of the water fl ows through the fill stone construction and the rest fl ows over the body. The analysis of the water discharge division into the overfl ow and the seepage flow gives the possibility of the infi ltration body and the shape of the weir profile. The geometry of the rubble sill, the grain size distribution of fill material and the localization of zones with velocity which can break stability stone elements of body, are important elements when determining the geometry of the gabion weir. Results of the laboratory on the gabion weir, including reconnaissance of the over and the trough-flow, are presented in the article. The discharge of the surface flow form was determined with the hydrometric method. The electromagnetic PEMS probe for measurement of velocity of water has been used. The degree of discharge distribution depends on hydraulic parameters of overflowing water stream.