2019
DOI: 10.15244/pjoes/97395
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Ecological Flow Regime and its Satisfactory Degree Assessment Based on an Integrated Method

Abstract: Ecological flow regime (EFR) evaluation is essential in river ecosystem protection. To evaluate and maintain EFR under a changing environment reasonably, an integrated method based on both the monthly 7Q10 method and biological analysis method was put forward for its simple modelling and small data requirement, and then reasonable EFR was obtained after a reasonable check by the Tennant method. Meanwhile, the concept and quantitative formula of the ecological flow regime satisfactory degree (EFRSD) were recomm… Show more

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Cited by 7 publications
(2 citation statements)
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“…The flow regime coefficient is the ratio between the maximum discharge (Q max ) and minimum discharge (Q min ) of a river in the watershed (Asdak, 2014). The flow regime coefficient is one of the most decisive parameters in monitoring and knowing the flow capacity of a river from time to time (Xu et al, 2019), especially the highest discharge during the rainy season and the lowest discharge during the dry season (Berhanu et al, 2015;Handayani et al, 2019). The results of the analysis of river regime coefficients in the Wanggu watershed are presented in Figures 2 and 3.…”
Section: Flow Regime Coefficientmentioning
confidence: 99%
“…The flow regime coefficient is the ratio between the maximum discharge (Q max ) and minimum discharge (Q min ) of a river in the watershed (Asdak, 2014). The flow regime coefficient is one of the most decisive parameters in monitoring and knowing the flow capacity of a river from time to time (Xu et al, 2019), especially the highest discharge during the rainy season and the lowest discharge during the dry season (Berhanu et al, 2015;Handayani et al, 2019). The results of the analysis of river regime coefficients in the Wanggu watershed are presented in Figures 2 and 3.…”
Section: Flow Regime Coefficientmentioning
confidence: 99%
“…At present, the ecological flow calculation includes four methods, as shown in Table 1: hydrological methods, hydraulic methods, habitat simulation methods, and holistic methods [15]. Among them, hydrological methods are based on a long series of historical run-off data, and take a fixed flow percentage as the required flow process of the river; these are generally used for reference or method comparison, including the Tennant method [16][17][18], Texas method [19,20], flow duration curve (FDC) method [21,22], range of variability approach (RVA) [23][24][25], minimum average 7 day (consecutive) flow expected to occur once every 10 years (7Q10) method [26,27], annual distribution method [28,29], monthly frequency calculation method [30,31], monthly guarantee rate method [32,33], minimum monthly average flow method [34,35], and the Northern Great Plains Resources Program (NGPRP) method [36,37]. The hydrological methods are simple and convenient, and do not require on-site monitoring, but the accuracy is low, due to single factor.…”
Section: Introductionmentioning
confidence: 99%