2020
DOI: 10.1007/s10040-020-02259-y
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Recharge and baseflow constrained by surface-water and groundwater chemistry: case study of the Chari River, Chad basin

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Cited by 4 publications
(1 citation statement)
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“…Given that base ow is released slowly when it ows through the soil matrix and maintains a relatively stable ow volume for a long time (Beck et al 2013), it has important ecological functions, such as regulating the seasonal distribution of river ow (Gan et al 2015), maintaining the aquatic habitat under extreme weather conditions (Fan et al 2013), and transferring physical and chemical substances (Bosch et al 2017). Su cient river discharge must be ensured based on the e cient quanti cation or prediction of base ow source (Goncalves et al 2020). However, the spatial variation and generation of base ow remain unclear due to the small number of gauging stations and the complex aquifer condition.…”
Section: Introductionmentioning
confidence: 99%
“…Given that base ow is released slowly when it ows through the soil matrix and maintains a relatively stable ow volume for a long time (Beck et al 2013), it has important ecological functions, such as regulating the seasonal distribution of river ow (Gan et al 2015), maintaining the aquatic habitat under extreme weather conditions (Fan et al 2013), and transferring physical and chemical substances (Bosch et al 2017). Su cient river discharge must be ensured based on the e cient quanti cation or prediction of base ow source (Goncalves et al 2020). However, the spatial variation and generation of base ow remain unclear due to the small number of gauging stations and the complex aquifer condition.…”
Section: Introductionmentioning
confidence: 99%