Using 3D geological modelling and geochemical mixing models to characterise alluvial aquifer recharge sources in the upper Condamine River catchment, Queensland, Australia

2017 ◽  
Vol 574 ◽  
pp. 1-18 ◽  
Author(s):  
Jorge L. Martinez ◽  
Matthias Raiber ◽  
Dioni I. Cendón
2019 ◽  
Vol 24 (2) ◽  
pp. 185-199
Author(s):  
Weston J. Koehn ◽  
Stacey E. Tucker-Kulesza ◽  
David R. Steward

Dynamic interactions between rivers and aquifers are controlled by the underlying hydrogeologic environment, as well as the type of hydrologic connection between the riverbed and saturated zone. The Arkansas River supplies groundwater to a heavily exploited region of the Ogallala Aquifer across Western Kansas. Site characterizations of this region using existing well and borehole data reveal large scale geologic features that significantly impact recharge processes, such as the Bear Creek fault. However, the existing hydrogeologic data do not provide the level of detail needed to fully understand the contribution of the losing river system to Arkansas Alluvial aquifer recharge. Knowledge about riverbed hydrogeology is acquirable using electrical resistivity imaging (ERI) surveys. ERI surveys and soil sample analysis were conducted at three sites along the Arkansas River to characterize the hydrogeologic environment within the Arkansas River Alluvial aquifer, which overlies the Ogallala aquifer. Temporal changes in electrical resistivity served as an indicator of the hydrologic response of the alluvial sediments to changes in river discharge as different patterns of water movement from the Arkansas River to Arkansas River Alluvial aquifer were observed. The ERI surveys revealed both fully connected and disconnected regions between the riverbed and groundwater table. The results supplement the existing geologic characterization of this region, and provide a more spatially detailed view of the hydrogeologic environment that has a direct causative effect on groundwater surface water interactions. Understanding the behavior of river-aquifer interactions is vital to the ability to predict the future holds of this important groundwater system.


2018 ◽  
Vol 559 ◽  
pp. 835-847 ◽  
Author(s):  
Suneel Kumar Joshi ◽  
Shive Prakash Rai ◽  
Rajiv Sinha ◽  
Sanjeev Gupta ◽  
Alexander Logan Densmore ◽  
...  

Soil Research ◽  
1978 ◽  
Vol 16 (3) ◽  
pp. 245 ◽  
Author(s):  
TS Longley ◽  
AK Turner ◽  
JD Lawson

Overpumping for irrigation has caused a general lowering of the piezometric surface in a multilayered aquifer in the Westernport Bay area of Victoria. This lowering effectively increases costs for agricultural production because of the higher pumping lifts now needed, and sets a limit to further development for irrigation in this vegetable-growing locality. In addition, there is now some seawater intrusion into the aquifer. A finite-difference model had been developed by the Department of Minerals and Energy of Victoria for the prediction of piezometric surfaces associated with steady-state pumping rates. This model was altered so that the influence of various possible recharge sources on the piezometric surface could be predicted. The recharge sources were infiltration from rainfall in localities where there are outcrops of the aquifer formation, beds of rivers passing over the general area, and rainfall infiltration in the surrounding hill country. Correspondence between the results of the model and the field behaviour as recorded in a dense grid of bores, was adequate in that it confirmed the existence and relative importance of the postulated recharge sources. Recommendations are made as to the limited advisability of artificial recharge of the aquifer from surface sources.


2002 ◽  
Vol 255 (1-4) ◽  
pp. 90-106 ◽  
Author(s):  
C. Joerin ◽  
K.J. Beven ◽  
I. Iorgulescu ◽  
A. Musy

Water ◽  
2020 ◽  
Vol 12 (3) ◽  
pp. 731 ◽  
Author(s):  
Arianna Renau-Pruñonosa ◽  
Olga García-Menéndez ◽  
María Ibáñez ◽  
Enric Vázquez-Suñé ◽  
Clara Boix ◽  
...  

In urban, industrial, and agricultural areas, a vast array of contaminants may be found because they are introduced into the aquifers by different recharge sources. The emerging contaminants (ECs) correspond to unregulated contaminants, which may be candidates for future regulation depending on the results of research into their potential effects on health and on monitoring data regarding their occurrence. ECs frequently found in wastewater, such as acetaminophen, carbamazepine, primidone, and sulfamethoxazole, may be good indicators of the introduction of the reclaimed water to the aquifers. The resistance of the ECs to removal in wastewater treatment plants (WWTPs) causes them to be appropriate sewage markers. Plana de Castellón (Spain) is a coastal area that has been characterized by intensive citrus agriculture since the 1970s. Traditionally, in the southern sector of Plana de Castellón, 100% of irrigation water comes from groundwater. In recent years, local farmers have been using a mixture of groundwater and reclaimed water from wastewater treatment plants (WWTPs) to irrigate the citrus. The aims of the present study were: (i) to assess the occurrences, spatial distributions, and concentrations of selected ECs, including 32 antibiotics, 8 UV filters, and 2 nonsteroidal anti-inflammatory drugs, in groundwater in a common agricultural context; (ii) to identify the recharge (pollution) sources acting as the origin of the ECs, and (iii) to suggest ECs as indicators of reclaimed water arrival in detrital heterogeneous aquifers. The obtained data provided relevant information for the management of water resources and elucidated the fate and behavior of emerging contaminants in similar contexts.


Water ◽  
2021 ◽  
Vol 13 (6) ◽  
pp. 871
Author(s):  
Connor P. Newman ◽  
Suzanne S. Paschke ◽  
Gabrielle Keith

A multi-component geochemical dataset was collected from groundwater and surface-water bodies associated with the urban Fountain Creek alluvial aquifer, Colorado, USA, to facilitate analysis of recharge sources, geochemical interactions, and groundwater-residence times. Results indicate that groundwater can be separated into three distinct geochemical zones based on location within the flow system and proximity to surface water, and these zones can be used to infer sources of recharge and groundwater movement through the aquifer. Rare-earth-element concentrations and detections of wastewater-indicator compounds indicate the presence of effluent from wastewater-treatment plants in both groundwater and surface water. Effluent presence in groundwater indicates that streams in the area lose to groundwater in some seasons and are a source of focused groundwater recharge. Distributions of pharmaceuticals and wastewater-indicator compounds also inform an understanding of groundwater–surface-water interactions. Noble-gas isotopes corroborate rare-earth-element data in indicating geochemical evolution within the aquifer from recharge area to discharge area and qualitatively indicate variable groundwater-residence times and mixing with pre-modern groundwater. Quantitative groundwater-residence times calculated from 3H/3He, SF6, and lumped-parameter modeling generally are less than 20 years, but the presence of mixing with older groundwater of an unknown age is also indicated at selected locations. Future investigations would benefit by including groundwater-age tracers suited to quantification of mixing for both young (years to decades) and old (centuries and millennia) groundwater. This multi-faceted analysis facilitated development of a conceptual model for the investigated groundwater-flow system and illustrates the application of an encompassing suite of analytes in exploring hydrologic and geochemical interactions in complex systems.


2021 ◽  
Author(s):  
YongFeng Gong ◽  
Xin Liu ◽  
Bin Ma ◽  
PengFei Qi ◽  
Yan Li

Abstract Irrigation water extracted from the Yellow River plays a key role in water resource management in the Yinchuan Plain (YCP), arid Northwest China. Investigating the soluble matters (ion and gas) of groundwater provides information to explain the unconfined shallow aquifer recharge and groundwater mineralization processes after long-term flood irrigation activity. Environmental tracing with the elements, 2H, 18O, 3H, and CFCs, combining geochemistry using major ions and selected trace elements, was conducted for 43 water samples from September to October 2019 in the YCP. Evaporite and silicate weathering dominate the shallow unconfined groundwater geochemical compositions. Water–rock interactions control the mineralization characteristics regularly along the groundwater flow paths from the southwest toward the northeast. Stable isotopes suggest that Yellow River water and precipitation in winder and/or from Helan Mountainous area are the main recharge sources. The shallow unconfined aquifer mixed young (post-1940) and old (pre-1940) water with young water ratios from 53.1 to 73.5% inferred from the CFC concentrations and 3H activities. Water reinfiltrations extracted from the Yellow River and from the old groundwater are confirmed. Lateral flow recharge for the shallow unconfined aquifer is less indistinctive than that from the water re-infiltration in the plain areas.


2006 ◽  
Vol 39 (3) ◽  
pp. 293-302 ◽  
Author(s):  
M.R. Lelliott ◽  
D. McC. Bridge ◽  
H. Kessler ◽  
S.J. Price ◽  
K.J. Seymour

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