Pregled bibliografske jedinice broj: 1206172
Characterization of soil drainage dynamics on karst terrains by developing a site-specific reservoir cascade scheme hydrological model with preferential flows
Characterization of soil drainage dynamics on karst terrains by developing a site-specific reservoir cascade scheme hydrological model with preferential flows // Journal of hydrology, 612 (2022), B; 128147, 13 doi:10.1016/j.jhydrol.2022.128147 (međunarodna recenzija, članak, znanstveni)
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Naslov
Characterization of soil drainage dynamics on karst terrains by developing a site-specific reservoir cascade scheme hydrological model with preferential flows
Autori
Švob, Mirna ; Domínguez-Villar, David ; Krklec, Kristina
Izvornik
Journal of hydrology (0022-1694) 612
(2022), B;
128147, 13
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
karst soil ; hydrological model ; reservoir cascade scheme ; recharge ; macroporosity ; preferential flows
Sažetak
Models provide quantitative solutions that enable better understanding of karst soils hydrology. A location in central Spain was selected to implement a 1-D hydrological model that uses a reservoir cascade scheme (RCS) approach to simulate soil water content (SWC) at daily resolution. The model simulates SWC for six soil layers and includes additional modules to reproduce preferential flow regime. The soil profile in the model is 0.5 m deep, developed in silt loam soil on top of dolomite marbles. Three different configurations of the model were considered. Configuration 1 considers a basic RCS module, whereas other configurations include preferential flows. Thus, Configuration 2 considers RCS module together with a continuous preferential flow module, where 1 to 5% of available SWC from each layer is drained every day along preferential pathways. Configuration 3 contains a discontinuous preferential flow module in addition to previous modules. The discontinuous preferential flow is only activated during rainfall events occurring after long dry periods. Simulated SWC values are compared with measured SWC values, so model parameters are iteratively adjusted to optimize the model results. The model produces the best simulations implementing the Configuration 3, when matrix flow and two preferential flow regimes are considered. The model shows that preferential flows significantly contribute to recharge and should not be neglected in soil hydrological models and recharge estimations in karst areas.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Biotehnologija
POVEZANOST RADA
Projekti:
IP-2018-01-7080 - Međuusporedba metoda mjerenja denudacije krša (KADEME) (Krklec, Kristina, HRZZ - 2018-01) ( CroRIS)
Ustanove:
Agronomski fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus