Abstract
Baseflow recession analysis is widely used in hydrological research, water resource planning and management, and watershed hydrogeological research. The first step of baseflow recession analysis is to extract the baseflow recession segments from the hydrograph. Different extraction results lead to different analysis results. At present, the four major recession segment extraction methods applied by hydrologists are mostly based on experience, and there is no clear theoretical basis. Therefore, this study derives a second-order derivation (Sec-D) recession segment extraction method based on the power law relationship between storage and discharge. Moreover, by applying the Sec-D method and the four conventional extraction methods to four hydrological stations in the Tao’er River basin in northeastern China, the differences in the recession segment extraction, determination of basin-wide hydrogeological parameters, and groundwater balance estimation are compared. The results demonstrate that, contrary to the four conventional methods, the Sec-D method can effectively eliminate the early recession stage affected by the surface runoff or rainfall and some streamflow data with more than 1% non-sequential error. The hydraulic conductivity of the four basins estimated by the Sec-D method is between 2.3 × 10−5–4.9 × 10−5 m/s, and the aquifer thickness is between 131.2 and 202.5 m. However, the four conventional extraction methods may underestimate (by about 2.5 times) the basin-wide hydraulic conductivity and overestimate (by about 3 times) the aquifer thickness. The groundwater balance elements calculated by the Sec-D method and the four conventional methods present similar intra-annual fluctuation characteristics; the correlation coefficients of daily evapotranspiration calculated by the five methods ranged from 0.7 to 0.95, and those of daily effective groundwater recharge ranged from 0.95 to 0.99. The use of the Sec-D method in baseflow recession analyses is significant for future studies and can be combined with conventional methods.
Highlights
Baseflow, known as low flow or drought flow, represents the streamflow formed mainly by discharge of stored water in a basin during the dry season [1,2,3,4]
The results demonstrate that there is no significant difference in the distribution characteristics of the extracted segments of the Kir, Vog, Bru, and Aks methods, while the segments extracted by the second-order derivative (Sec-D) method are concentrated in the stage of low streamflow
The Sec-D method developed in this paper is highly dependent on the calculation results of the second-order derivative of the streamflow
Summary
Based on Second-Order Derivative of Streamflow and Comparison with Four Conventional Methods. Jilin Provincial Key Laboratory of Water Resources and Environment, Jilin University, Changchun 130021, China. National-Local Joint Engineering Laboratory of In-Situ Conversion, Drilling and Exploitation Technology for. College of New Energy and Environment, Jilin University, Changchun 130021, China
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