Assessment of aquifer recharge and groundwater availability in a semiarid region of Brazil in the context of an interbasin water transfer scheme

Particularly in arid and semiarid areas, more and more populations rely almost entirely on imported water. However, the extent to which intentional discharge into transiting river systems and unintentional leakage may be augmenting water resources for communities along and down gradient of the water...

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Published inHydrogeology journal Vol. 31; no. 3; pp. 751 - 769
Main Authors Costa, Alexandre C., Dupont, Fanny, Bier, George, van Oel, Pieter, Walker, David W., Martins, Eduardo S. P. R.
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer Berlin Heidelberg 01.05.2023
Springer Nature B.V
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Online AccessGet full text
ISSN1431-2174
1435-0157
1435-0157
DOI10.1007/s10040-023-02612-x

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Abstract Particularly in arid and semiarid areas, more and more populations rely almost entirely on imported water. However, the extent to which intentional discharge into transiting river systems and unintentional leakage may be augmenting water resources for communities along and down gradient of the water transfer scheme has not previously been subject to research. The objective of this study was to assess both the potential of a large-scale water transfer (WT) scheme to increase groundwater availability by channel transmission losses in a large dryland aquifer system (2,166 km²) in Brazil, and the capability of the receiving streams to transport water downstream under a prolonged drought. An integrated surface-water/groundwater model was developed to improve the estimation of the groundwater resources, considering the spatio-temporal variability of infiltrated rainfall for aquifer recharge. Aquifer recharge from the WT scheme was simulated under prolonged drought conditions, applying an uncertainty analysis of the most influential fluxes and parameters. The annual recharge (66 mm/year) was approximately twice the amount of water abstracted (1990–2016); however, the annual recharge dropped to 13.9 mm/year from 2012 to 2016, a drought period. Under similar drought conditions, the additional recharge (6.89 × 106 m³/year) from the WT scheme did not compensate for the decrease in groundwater head in areas that do not surround the receiving streams. Actually, the additional recharge is counteracted by a decrease of 25% of natural groundwater recharge or an increase of 50% in pumping rate; therefore, WT transmission losses alone would not solve the issue of the unsustainable management of groundwater resources.
AbstractList Particularly in arid and semiarid areas, more and more populations rely almost entirely on imported water. However, the extent to which intentional discharge into transiting river systems and unintentional leakage may be augmenting water resources for communities along and down gradient of the water transfer scheme has not previously been subject to research. The objective of this study was to assess both the potential of a large-scale water transfer (WT) scheme to increase groundwater availability by channel transmission losses in a large dryland aquifer system (2,166 km²) in Brazil, and the capability of the receiving streams to transport water downstream under a prolonged drought. An integrated surface-water/groundwater model was developed to improve the estimation of the groundwater resources, considering the spatio-temporal variability of infiltrated rainfall for aquifer recharge. Aquifer recharge from the WT scheme was simulated under prolonged drought conditions, applying an uncertainty analysis of the most influential fluxes and parameters. The annual recharge (66 mm/year) was approximately twice the amount of water abstracted (1990–2016); however, the annual recharge dropped to 13.9 mm/year from 2012 to 2016, a drought period. Under similar drought conditions, the additional recharge (6.89 × 106 m³/year) from the WT scheme did not compensate for the decrease in groundwater head in areas that do not surround the receiving streams. Actually, the additional recharge is counteracted by a decrease of 25% of natural groundwater recharge or an increase of 50% in pumping rate; therefore, WT transmission losses alone would not solve the issue of the unsustainable management of groundwater resources. En particulier dans les zones arides et semi-arides, de plus en plus de populations dépendent presque entièrement de l'eau importée. Cependant, l’ampleur des rejets intentionnels transitant dans les systèmes fluviaux et les fuites non intentionnelles qui peuvent augmenter les ressources en eau pour les communautés le long et en aval du système de transfert d'eau n'a pas encore fait l'objet de recherche. L'objectif de cette étude était d'évaluer à la fois le potentiel d'un système de transfert d'eau (WT) à grande échelle pour augmenter la disponibilité des eaux souterraines en canalisant les pertes de transmission dans un grand système aquifère en zone aride (2’166 km²), et la capacité des cours d'eau récepteurs à transporter l'eau en aval lors d’une sécheresse prolongée. Un modèle intégré d'eau de surface et d'eau souterraine a été développé pour améliorer l'estimation des ressources en eau souterraine, en considérant la variabilité spatio-temporelle des précipitations infiltrées pour la recharge des aquifères. La recharge de l'aquifère à partir du schéma WT a été simulée dans des conditions de sécheresse prolongée, en appliquant une analyse d'incertitude des flux et des paramètres les plus influents. La recharge annuelle (66 mm/an) était approximativement le double de la quantité d'eau prélevée (1990-2016). Cependant, la recharge annuelle a chuté à 13.9 mm/an de 2012 à 2016, une période de sécheresse. Dans des conditions de sécheresse similaires, la recharge supplémentaire (6.89×106 m³/an) du système WT n'a pas compensé la diminution de la charge hydraulique de l’aquifère dans les zones qui ne sont pas situées à proximité des cours d'eau récepteurs. En fait, la recharge supplémentaire est contrebalancée par une diminution de 25% de la recharge naturelle des eaux souterraines ou une augmentation de 50% du taux de pompage. Par conséquent, les pertes de transmission de WT ne résoudraient pas à elles seules le problème de la gestion non durable des ressources en eau souterraine. En particular en las zonas áridas y semiáridas, cada vez son más las poblaciones que dependen casi por completo del agua importada. Sin embargo, hasta ahora no se había investigado en qué medida los trasvases intencionales a los sistemas fluviales en circulación y las pérdidas no intencionales podían aumentar los recursos hídricos de las comunidades situadas a lo largo de los sistemas de trasvase y en su gradiente inferior. El objetivo de este estudio era evaluar tanto el potencial de un esquema de transferencia de agua (WT) a gran escala para aumentar la disponibilidad de agua subterránea mediante la canalización de las pérdidas de conducción en un sistema acuífero de tierras secas de gran tamaño (2,166 km²), como la capacidad de los arroyos receptores para transportar agua hacia aguas abajo bajo una sequía prolongada. Se desarrolló un modelo integrado de aguas superficiales y subterráneas para mejorar la estimación de los recursos hídricos subterráneos, teniendo en cuenta la variabilidad espaciotemporal de las precipitaciones infiltradas para la recarga de los acuíferos. Se simuló la recarga del acuífero a partir del esquema WT en condiciones de sequía prolongada, aplicando un análisis de incertidumbre de los flujos y parámetros más influyentes. La recarga anual (66 mm/año) fue aproximadamente el doble de la cantidad de agua extraída (1990-2016). Sin embargo, la recarga anual se redujo a 13.9 mm/año de 2012 a 2016, un período de sequía. En condiciones de sequía similares, la recarga adicional (6.89×106 m³/año) del esquema WT no compensó la disminución de la carga de agua subterránea en las zonas que no rodean los arroyos receptores. En realidad, la recarga adicional se contrarresta con una disminución del 25% de la recarga natural de las aguas subterráneas o un aumento del 50% de la tasa de bombeo. Por lo tanto, las pérdidas de transporte de agua por sí solas no resolverían el problema de la gestión no sostenible de los recursos hídricos subterráneos. 特别是在干旱和半干旱地区,越来越多的人口几乎完全依赖外来水。然而,蓄意排放到过境河流系统和意外渗漏可能在很大程度上增加了输水方案沿线和下游社区的水资源,此前尚未进行过研究。本研究目的是评估大规模调水(WT)方案通过大型旱区含水层系统(2,166 km²)的渠道传输损失增加地下水可利用性的潜力,以及在长期干旱情况下接收河流向下游输送水的能力。考虑到含水层补给接受降雨入渗的时空变化,开发了一个地表水-地下水联合模型以改进地下水资源的估计。应用最有影响的通量和参数不确定性分析,模拟了在长期干旱条件下基于WT方案的含水层补给。年补给量(66 mm/y)约为抽水量(1990-2016年)的两倍。然而,从2012年到2016年(干旱期),年补给量下降至13.9 mm/y。在类似干旱条件下,来自WT方案的额外补给(6.89×106 m³/y)没有补偿不在受纳河流周围地区的地下水水头下降。事实上,额外补给被天然地下水补给量减少25%或抽水率增加50%所抵消。因此,仅依靠WT传输损失无法解决地下水资源的不可持续管理问题。 Particularmente em áreas áridas e semiáridas, cada vez mais populações dependem quase inteiramente de água importada. No entanto, até que ponto a descarga intencional em sistemas fluviais em trânsito e o vazamento não intencional podem aumentar os recursos hídricos para as comunidades ao longo e a jusante do esquema de transferência de água não foi objeto de pesquisa anterior. O objetivo deste estudo foi avaliar o potencial de um esquema de transferência de água (TA) em larga escala para aumentar a disponibilidade de águas subterrâneas por perdas de transmissão de canal em um grande sistema aquífero seco (2,166 km²) e a capacidade dos fluxos receptores de transportar água a jusante durante uma seca prolongada. Um modelo integrado de águas superficiais/subterrâneas foi desenvolvido para melhorar a estimativa dos recursos hídricos subterrâneos, considerando a variabilidade espaço-temporal da precipitação infiltrada para a recarga do aquífero. A recarga do aquífero do esquema de TA foi simulada sob condições de seca prolongada, aplicando uma análise de incerteza dos fluxos e parâmetros mais influentes. A recarga anual (66 mm/ano) foi aproximadamente o dobro da quantidade de água captada (1990-2016). No entanto, a recarga anual caiu para 13.9 mm/ano de 2012 a 2016, um período de estiagem. Sob condições de seca semelhantes, a recarga adicional (6.89 × 106 m³/ano) do esquema de TA não compensou a diminuição da carga de água subterrânea em áreas que não circundam os córregos receptores. Na verdade, a recarga adicional é compensada por uma diminuição de 25% da recarga natural do lençol freático ou um aumento de 50% da taxa de bombeamento. Portanto, as perdas de transmissão da TA por si só não resolveriam o problema da gestão insustentável dos recursos hídricos subterrâneos.
Particularly in arid and semiarid areas, more and more populations rely almost entirely on imported water. However, the extent to which intentional discharge into transiting river systems and unintentional leakage may be augmenting water resources for communities along and down gradient of the water transfer scheme has not previously been subject to research. The objective of this study was to assess both the potential of a large-scale water transfer (WT) scheme to increase groundwater availability by channel transmission losses in a large dryland aquifer system (2,166 km²) in Brazil, and the capability of the receiving streams to transport water downstream under a prolonged drought. An integrated surface-water/groundwater model was developed to improve the estimation of the groundwater resources, considering the spatio-temporal variability of infiltrated rainfall for aquifer recharge. Aquifer recharge from the WT scheme was simulated under prolonged drought conditions, applying an uncertainty analysis of the most influential fluxes and parameters. The annual recharge (66 mm/year) was approximately twice the amount of water abstracted (1990–2016); however, the annual recharge dropped to 13.9 mm/year from 2012 to 2016, a drought period. Under similar drought conditions, the additional recharge (6.89 × 106 m³/year) from the WT scheme did not compensate for the decrease in groundwater head in areas that do not surround the receiving streams. Actually, the additional recharge is counteracted by a decrease of 25% of natural groundwater recharge or an increase of 50% in pumping rate; therefore, WT transmission losses alone would not solve the issue of the unsustainable management of groundwater resources.
Particularly in arid and semiarid areas, more and more populations rely almost entirely on imported water. However, the extent to which intentional discharge into transiting river systems and unintentional leakage may be augmenting water resources for communities along and down gradient of the water transfer scheme has not previously been subject to research. The objective of this study was to assess both the potential of a large-scale water transfer (WT) scheme to increase groundwater availability by channel transmission losses in a large dryland aquifer system (2,166 km²) in Brazil, and the capability of the receiving streams to transport water downstream under a prolonged drought. An integrated surface-water/groundwater model was developed to improve the estimation of the groundwater resources, considering the spatio-temporal variability of infiltrated rainfall for aquifer recharge. Aquifer recharge from the WT scheme was simulated under prolonged drought conditions, applying an uncertainty analysis of the most influential fluxes and parameters. The annual recharge (66 mm/year) was approximately twice the amount of water abstracted (1990–2016); however, the annual recharge dropped to 13.9 mm/year from 2012 to 2016, a drought period. Under similar drought conditions, the additional recharge (6.89 × 106 m³/year) from the WT scheme did not compensate for the decrease in groundwater head in areas that do not surround the receiving streams. Actually, the additional recharge is counteracted by a decrease of 25% of natural groundwater recharge or an increase of 50% in pumping rate; therefore, WT transmission losses alone would not solve the issue of the unsustainable management of groundwater resources.
Author Costa, Alexandre C.
Bier, George
van Oel, Pieter
Dupont, Fanny
Walker, David W.
Martins, Eduardo S. P. R.
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  organization: University of International Integration of the Afro-Brazilian Lusophony, Institute of Engineering and Sustainable Development, Water Resources Management Group, Wageningen University
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  organization: Water Resources Management Group, Wageningen University
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  organization: Research Institute of Meteorology and Water Resources
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crossref_primary_10_1016_j_eve_2025_100064
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DocumentTitle_FL Évaluation de la recharge des aquifères et de la disponibilité des eaux souterraines dans une région semi-aride du Brésil dans le contexte d'un système de transfert d'eau entre bassins
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  doi: 10.1002/aqc.3270020404
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Snippet Particularly in arid and semiarid areas, more and more populations rely almost entirely on imported water. However, the extent to which intentional discharge...
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SubjectTerms Aquatic Pollution
Aquifer recharge
Aquifer systems
Aquifers
Arid lands
Arid zones
Arroyos
Availability
Brazil
Drought
Drought conditions
Earth and Environmental Science
Earth Sciences
Geology
Geophysics/Geodesy
Groundwater
Groundwater availability
groundwater flow
Groundwater recharge
Groundwater resources
Hydrogeology
Hydrology/Water Resources
Imported water
Influents
Moisture content
Populations
Pumping rates
Rain
Rainfall
Receiving
Receiving waters
River systems
Rivers
Semi arid areas
Semiarid zones
Streams
Surface water
Temporal variability
Temporal variations
Transmission loss
Uncertainty analysis
Waste Water Technology
Water content
Water Management
Water Pollution Control
Water Quality/Water Pollution
Water resources
Water transfer
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Title Assessment of aquifer recharge and groundwater availability in a semiarid region of Brazil in the context of an interbasin water transfer scheme
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