4.7 Article

Comparison of transit time models for exploring seasonal variation of preferential flow in a Moso bamboo watershed

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JOURNAL OF HYDROLOGY
卷 626, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.jhydrol.2023.130308

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Preferential flow; Stable isotopes; SAS functions; Young water fraction; Moso bamboo watershed

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Understanding the seasonality of hydrological fluxes and preferential flow is crucial for studying the fate and transport of contaminants in a watershed. In this study, different StorAge Selection (SAS)-based rainfall-runoff models were compared for a Moso bamboo watershed in the East Asian monsoon climate. The results show that a two-parallel-reservoir flow module effectively captures the temporal variation in streamflow. The inclusion of SAS functions improves the performance of the models, especially when applied to both reservoir outflows. The addition of SAS functions for ET fluxes also leads to minor improvements in performance. The study highlights the seasonal variation of preferential flow for deep drainage and lower reservoir outflow, with more young water during the East Asian summer monsoon period.
Understanding seasonal variations of the hydrological fluxes and preferential flow is crucial in exploring contaminant fate and transport processes in a watershed of interest. Here, performance of different StorAge Selection (SAS)-based rainfall-runoff models was compared for a Moso bamboo watershed under the East Asian monsoon climate. Most of these models are composed of a two-parallel-reservoir flow module and a compan-ioned SAS module. The results show that the temporal variation in streamflow is well captured by a two-parallel-reservoir flow module. The tracer simulations from different models show that two-uniform-reservoir (SSU) model with no SAS function has the lowest NSE value (0.17), the model including an SAS in one of the two reservoir outflows (SSD(U) and SSD(L)) improves performance (NSE greater than 0.5). The performance in simulating streamflow delta 18O is further improved when SAS functions are applied for outflows from both reservoirs (SSD (U, L), NSE = 0.76). Additional inclusion an SAS function for ET fluxes in the model (SSD (U, ET, L)) results in a minor improvement from SSD (U, L). The results of SSD (U, ET, L) have achieved the best transport per-formance (NSE = 0.77), with implication for preferential flow in the watershed. The preferential flow for deep drainage and lower reservoir outflow shows seasonal variation, with more young water in the East Asian summer monsoon period than that in the East Asian winter monsoon period. The upper reservoir storage and deep drainage rates are the main factors determining the temporal variation of preferential flow for deep drainage and lower reservoir outflow, respectively.

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