Integrated Watershed Management

Integrated Watershed Management

Application of digital filtering methods for assessing base flow and groundwater recharge in the Kashkan Watershed

Document Type : Original Article

Authors
Department of Range and Watershed Management Engineering, Faculty of Natural Resources, Lorestan University, Khorramabad, Iran
Abstract
Extended Abstract
 Introduction: Natural resource management is considered the foundation of sustainable development. Therefore, in a country like Iran, located in the water-stressed and tense region of the Middle East, water resource management is of paramount importance. Knowledge of temporal changes in baseflow is crucial for effective water resources management. Identifying the most suitable and optimal method for hydrograph separation and baseflow estimation enables the accurate calculation of the baseflow index.
 Materials and methods: In this study, nine recession filter algorithms were used to estimate baseflow. These algorithms include Local Minimum, Sliding Interval, Fixed Interval, Eckhardt, Chapman, Chapman & Maxwell, Lyne & Hollick, Furey & Gupta, and Boughton. Using these algorithms, daily baseflow was calculated for the Kashkan watershed using daily discharge and rainfall data from 1999 to 2020. The Kakareza, Sarab Seid Ali, Cham Anjir, Afrineh, and Pol-e-Dokhtar stations were investigated to separate baseflow in the Kashkan watershed. The performance of the methods for separating baseflow in the hydrograph of the Kashkan watershed was assessed using the Nash-Sutcliffe efficiency (NSE) coefficient and the R² coefficient to select the most suitable filtering method.
 Results: Among the recession algorithms examined, the Furey & Gupta method estimated the lowest baseflow for all five sub-watersheds. In the Afrineh sub-watershed, the Lyne and Hollick, Fixed Interval, and Sliding Interval methods estimated baseflow as 36.41, 30.11, and 29.7 m3/s, respectively. These methods attributed 85%, 82%, and 81% of the total flow to groundwater contributions. In the Cham Anjir sub-watershed, the highest annual average baseflow values were obtained using the Lyne & Hollick, and Local Minimum methods, with values of 7.22, and 6.24 m3/s, respectively. The variation in mean baseflow among different methods in the Cham Anjir sub-watershed ranged from 17% to 94%. For the Kakareza sub-watershed, the highest annual average baseflow values were observed using the Lyne & Hollick, and Sliding Interval methods, with values of 9.70, and 9.72 m3/s, respectively. The variation in mean baseflow among different methods in the Kakareza sub-watershed ranged from 17% to 95%. Similarly, in  the Pol-e-Dokhtar sub-watershed, the highest values were obtained using the Lyne & Hollick, Fixed Interval, and Sliding Interval methods, with values of 36.10, 34.40, and 34.40 m3/s, respectively, and variations ranging from 17% to 99%. In the Sarab Seid Ali sub-watershed, the Lyne & Hollick, Fixed Interval, and Sliding Interval methods yielded the highest annual average baseflow values of 5.97, 5.95, and 5.94 m³/s, respectively, with variations ranging from 17% to 92%. Based on the findings and evaluation criteria, the Local Minimum, Lyne & Hollick, Sliding Interval, and Fixed Interval methods were identified as suitable for baseflow separation in the studied sub-watersheds.
 Discussion: Baseflow in the Kashkan watershed of Lorestan constitutes a significant portion of the flow. In the majority of the methods examined in this study, it was also shown that baseflow accounts for more than 50% of the streamflow throughout the year. In all studied sub-watersheds, the Lyne and Holick algorithm showed suitable values for the NSE coefficient and R². Therefore, this algorithm can be considered an appropriate method for estimating baseflow in the Kashkan watershed. Considering the hydrological characteristics of the watershed, this method can better simulate the natural fluctuations of baseflow.
Conclusion: The results of this study can inform baseflow contribution estimates and help in selecting appropriate methods for flow separation in the hydrological modeling of rivers with varying discharge ranges in the Kashkan watershed. The present research focused on differentiating water sources in the Kashkan watershed using digital filtering methods. Future studies are recommended to explore other approaches, such as chemical methods and tracers, for water source differentiation in the Kashkan watershed, and to compare the accuracy of these methods with digital filtering techniques.
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  • Receive Date 06 October 2024
  • Revise Date 27 December 2024
  • Accept Date 17 January 2025