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Journal articles on the topic 'Groundwater-river interactions'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 January 2023

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1

Cai, Yi, Wenrui Huang, Fei Teng, Beibei Wang, Ke Ni, and Chunmiao Zheng. "Spatial variations of river–groundwater interactions from upstream mountain to midstream oasis and downstream desert in Heihe River basin, China." Hydrology Research 47, no. 2 (2015): 501–20. http://dx.doi.org/10.2166/nh.2015.072.

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The Heihe River basin consists of three different characteristic regions: upstream mountain area, midstream oasis region, and downstream desert region. Understanding the river–groundwater interactions in different river reaches is important for sustainable water resources management. In this study, river–groundwater interactions in three different river regions are investigated by the analysis of geophysical characteristics, meteor-hydrological characteristics, agricultural irrigations, and channel water balance equation in the river reaches in different seasons. Results indicate that the rive

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2

Brunner, Philip, René Therrien, Philippe Renard, Craig T. Simmons, and Harrie-Jan Hendricks Franssen. "Advances in understanding river-groundwater interactions." Reviews of Geophysics 55, no. 3 (2017): 818–54. http://dx.doi.org/10.1002/2017rg000556.

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3

Wan, Yu Yu, Fu Tian Liu, and Guang Yu Lin. "Study on the Hydraulic Relationship between Molin River and Groundwater." Advanced Materials Research 490-495 (March 2012): 652–56. http://dx.doi.org/10.4028/www.scientific.net/amr.490-495.652.

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Molin River catchment is located in arid and semi-arid region in China. River water and groundwater are major water sources in this area. It is a key work to identify the interaction between river water and groundwater for not only water resources assessment and sustainable development, but residents living, industry and agriculture and environment protection. In this study, the interaction of Molin River water and groundwater has been analyzed systematically with hydrogeochemical and isotopic methods based on analyzing the characteristics of groundwater hydrodynamic field. The results show th

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4

Unland, N. P., I. Cartwright, M. S. Andersen, et al. "Investigating the spatio-temporal variability in groundwater and surface water interactions: a multi-technical approach." Hydrology and Earth System Sciences Discussions 10, no. 3 (2013): 3795–842. http://dx.doi.org/10.5194/hessd-10-3795-2013.

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Abstract. The interaction between groundwater and surface water along the Tambo and Nicholson Rivers, southeast Australia, was investigated using 222Rn, Cl, differential flow gauging, head gradients, electrical conductivity (EC) and temperature profiling. Head gradients, temperature profiles, Cl concentrations and 222Rn activities all indicate higher groundwater fluxes to the Tambo River in areas of increased topographic variation where the potential to form large groundwater–surface water gradients is greater. Groundwater discharge to the Tambo River calculated by Cl mass balance was signific

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5

Baskaran, S., T. Ransley, R. S. Brodie, and P. Baker. "Investigating groundwater–river interactions using environmental tracers." Australian Journal of Earth Sciences 56, no. 1 (2009): 13–19. http://dx.doi.org/10.1080/08120090802541887.

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6

Parlov, Jelena, Zoran Kovač, and Jadranka Barešić. "The study of the interactions between Sava River and Zagreb aquifer system (Croatia) using water stable isotopes." E3S Web of Conferences 98 (2019): 12017. http://dx.doi.org/10.1051/e3sconf/20199812017.

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Water stable isotopes were used to investigate hydrological pathways and interactions between surface water and groundwater in the Zagreb aquifer system (Croatia). δ2H and δ18O values indicate a spatial variability of the influence of individual groundwater sources inside the aquifer – local precipitation and the Sava River water. Fractions of surface water in groundwater strongly depend on fluctuations of the river water level and less on the distance from the Sava River. These data extend our understanding of groundwater flow in the Zagreb aquifer system, interactions between Sava River wate

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7

Hinzman, Larry D., Matthew Wegner, and Michael R. Lilly. "Hydrologic Investigations of Groundwater and Surface-water Interactions In Subarctic Alaska." Hydrology Research 31, no. 4-5 (2000): 339–56. http://dx.doi.org/10.2166/nh.2000.0020.

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Dynamic interactions between rivers and adjacent aquifers can significantly affect near-bank geochemistry and processes associated with natural attenuation of contaminants by mixing water or introducing oxygen or nutrients. During 1997 and 1998 in a study near Fairbanks, Alaska U.S.A, the hydrologic conditions in the Chena River and in the adjacent groundwater were monitored. The river stage, groundwater elevations, and the water chemistry and temperature in both river and groundwater were measured. In the spring of 1997, the groundwater gradient close to the Chena River reversed causing surfa

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8

Lee, Hyeonju, Min-Ho Koo, Juhyeon Lee, and Kangjoo Kim. "Changes in Stream–Aquifer Interactions Due to Gate Opening of the Juksan Weir in Korea." Water 13, no. 12 (2021): 1639. http://dx.doi.org/10.3390/w13121639.

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The Juksan weir, installed in the Yeongsan river in South Korea from 2010 to 2012, has secured sustainable water resources and helped control flooding. However, low river flow velocities due to the weir have deteriorated the quality of the river water. For natural river restoration, the water gate was opened in 2017. In this study, the three-dimensional finite difference model Visual MODFLOW was used to analyze the effects of gate opening on stream–aquifer interactions. A conceptual model was developed to simulate the stream–aquifer dynamics caused by the operation of the water gate at the Juk

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9

Brančić, Andjela, Anastasija Đordjević, and Dejan Nešković. "Characteristics of Groundwater–Surface Water Interaction in Areas with Scarce Input Data—Case Study of Banja River Catchment (Western Serbia)." Proceedings 2, no. 11 (2018): 625. http://dx.doi.org/10.3390/proceedings2110625.

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Water resources monitoring traditionally refers to the observation of surface or groundwater as separate entities. However, in one watershed, almost all characteristics of surface water interact with groundwater. This research was done in order to obtain more accurate assumptions about the interaction between groundwater and surface water and establish recharge zones on the example of Banja river catchment area. This research shows the possibility to have both quantitative and qualitative analyses of groundwater–surface water interactions of some river catchment with limited input data in shor

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10

Kurth, A. M., C. Weber, and M. Schirmer. "How effective is river restoration in re-establishing groundwater – surface water interactions? – A case study." Hydrology and Earth System Sciences Discussions 12, no. 1 (2015): 1093–118. http://dx.doi.org/10.5194/hessd-12-1093-2015.

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Abstract. In this study we investigated whether river restoration was successful in re-establishing vertical connectivity and, thereby, groundwater-surface water interactions, in a degraded urban stream. Well-tried passive Distributed Temperature Sensing (DTS) and novel active and passive DTS approaches were employed to study groundwater-surface water interactions in an experimental reach of an urban stream before and after its restoration and in two (near-) natural reference streams. Results were validated with Radon-222 analyses. Our results indicated that river restoration at the study site

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11

Liu, C., J. Liu, Y. Hu, and C. Zheng. "Studying groundwater and surface water interactions using airborne remote sensing in Heihe River basin, northwest China." Proceedings of the International Association of Hydrological Sciences 368 (May 7, 2015): 361–65. http://dx.doi.org/10.5194/piahs-368-361-2015.

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Abstract. Managing surface water and groundwater as a unified system is important for water resource exploitation and aquatic ecosystem conservation. The unified approach to water management needs accurate characterization of surface water and groundwater interactions. Temperature is a natural tracer for identifying surface water and groundwater interactions, and the use of remote sensing techniques facilitates basin-scale temperature measurement. This study focuses on the Heihe River basin, the second largest inland river basin in the arid and semi-arid northwest of China where surface water

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12

Unland, N. P., I. Cartwright, M. S. Andersen, et al. "Investigating the spatio-temporal variability in groundwater and surface water interactions: a multi-technique approach." Hydrology and Earth System Sciences 17, no. 9 (2013): 3437–53. http://dx.doi.org/10.5194/hess-17-3437-2013.

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Abstract. The interaction between groundwater and surface water along the Tambo and Nicholson rivers, southeast Australia, was investigated using 222Rn, Cl, differential flow gauging, head gradients, electrical conductivity (EC) and temperature profiles. Head gradients, temperature profiles, Cl concentrations and 222Rn activities all indicate higher groundwater fluxes to the Tambo River in areas of increased topographic variation where the potential to form large groundwater–surface water gradients is greater. Groundwater discharge to the Tambo River calculated by Cl mass balance was significa

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13

Racchetti, Salmaso, Pinardi, et al. "Is Flood Irrigation a Potential Driver of River-Groundwater Interactions and Diffuse Nitrate Pollution in Agricultural Watersheds?" Water 11, no. 11 (2019): 2304. http://dx.doi.org/10.3390/w11112304.

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In the Po plain, northern Italy, rivers within agricultural basins display steep summer increases in nitrate (NO3−) concentrations. Flood irrigation in overfertilized, permeable soils may drive such diffuse pollution, facilitating interactions between NO3−-rich groundwater and surface waters. We discuss multiple, indirect evidence of this mechanism in the Adda, Oglio, and Mincio rivers. These rivers drain agricultural soils with elevated nitrogen (N) surpluses, averaging 139, 193, and 136 kg ha−1 in the Adda, Oglio, and Mincio watersheds, respectively. The three rivers cross a transitional are

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14

Mastrocicco, M., N. Colombani, and A. Gargini. "Modelling present and future Po river interactions with alluvial aquifers (Low Po River Plain, Italy)." Journal of Water and Climate Change 5, no. 3 (2014): 457–71. http://dx.doi.org/10.2166/wcc.2014.058.

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A modelling study on a multi-layered confined/unconfined alluvial aquifer system was performed to quantify surface water/groundwater interactions. The calibrated groundwater flow model was used to forecast climate change impacts by implementing the results of a downscaled A1B model ensemble for the Po river valley. The modelled area is located in the north-western portion of the Ferrara Province (Northern Italy), along the eastern bank of the Po river. The modelling procedure started with a large scale steady state model followed by a transient flow model for the central portion of the domain,

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15

Yang, L., X. Song, Y. Zhang, D. Han, B. Zhang, and D. Long. "Characterizing interactions between surface water and groundwater in the Jialu River basin using major ion chemistry and stable isotopes." Hydrology and Earth System Sciences 16, no. 11 (2012): 4265–77. http://dx.doi.org/10.5194/hess-16-4265-2012.

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Abstract. The Jialu River, a secondary tributary of the Huaihe River, has been severely contaminated from major contaminant sources, such as a number of untreated or lightly treated sewage waste in some cities. Groundwater along the river is not an isolated component of the hydrologic system, but is instead connected with the surface water. This study aims to investigate temporal and spatial variations in water chemistry affected by humans and to characterize the relationships between surface water (e.g. reservoirs, lakes and rivers) and groundwater near the river in the shallow Quaternary aqu

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16

Ahring, T. S., and D. R. Steward. "Groundwater surface water interactions and the role of phreatophytes in identifying recharge zones." Hydrology and Earth System Sciences 16, no. 11 (2012): 4133–42. http://dx.doi.org/10.5194/hess-16-4133-2012.

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Abstract. Groundwater and surface water interactions within riparian corridors impact the distribution of phreatophytes that tap into groundwater stores. The changes in canopy area of phreatophytes over time is related to changes in depth to groundwater, distance from a stream or river, and hydrologic soil group. Remote sensing was used to determine the location of trees with pre-development and post-development aerial photography over the Ogallala Aquifer in the central plains of the United States. It was found that once the depth to groundwater becomes greater than about 3 m, tree population

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17

Kurth, A. M., C. Weber, and M. Schirmer. "How effective is river restoration in re-establishing groundwater–surface water interactions? – A case study." Hydrology and Earth System Sciences 19, no. 6 (2015): 2663–72. http://dx.doi.org/10.5194/hess-19-2663-2015.

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Abstract. In this study, we investigated whether river restoration was successful in re-establishing groundwater–surface water interactions in a degraded urban stream. Restoration measures included morphological changes to the river bed, such as the installation of gravel islands and spur dykes, as well as the planting of site-specific riparian vegetation. Standard distributed temperature sensing (DTS) and novel active and passive DTS approaches were employed to study groundwater–surface water interactions in two reference streams and an experimental reach of an urban stream before and after i

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18

Jing, Xiuyan, Hongbin Yang, and Na Wang. "Study on the hydro-chemistry process after mixing between water and rocks." Water Quality Research Journal 54, no. 2 (2018): 104–14. http://dx.doi.org/10.2166/wcc.2018.284.

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Abstract The chemical evolution of groundwater has received close attention from hydro-geologists. Northwest China largely consists of arid and semi-arid regions, where surface water and groundwater frequently exchange with each other, and where the mixing and water–rock interactions significantly affect the direction of water quality evolution. Based on experimental simulation, this paper investigates the interactions among the Yellow River water, groundwater and rocks in Yinchuan. The study found that when groundwater is mixed with the Yellow River water, the Yellow River water has a certain

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19

Yang, L., X. Song, Y. Zhang, D. Han, B. Zhang, and D. Long. "Characterizing interactions between surface water and groundwater in the Jialu River basin using major ion chemistry and stable isotopes." Hydrology and Earth System Sciences Discussions 9, no. 5 (2012): 5955–81. http://dx.doi.org/10.5194/hessd-9-5955-2012.

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Abstract. The Jialu River, a secondary tributary of the Huaihe River, has been severely contaminated for the major contaminant sources, such as a number of untreated or lightly treated sewage wastes in some cities. Groundwater along the river is not an isolated component of the hydrologic system, but instead connected with the surface water. This study aims to characterize the relationships between surface water (e.g. reservoirs, lakes and rivers) and groundwater near the river in the shallow Quaternary aquifer. The concentration of Cl− in North Zhengzhou City increased prominently due to the

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20

Vasilevskiy, Peter, Ping Wang, Sergey Pozdniakov, et al. "Simulating River/Lake–Groundwater Exchanges in Arid River Basins: An Improvement Constrained by Lake Surface Area Dynamics and Evapotranspiration." Remote Sensing 14, no. 7 (2022): 1657. http://dx.doi.org/10.3390/rs14071657.

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Surface water–groundwater interactions in arid zones are characterized by water exchange processes in a complex system comprising intermittent streams/terminal lakes, shallow aquifers, riparian zone evapotranspiration, and groundwater withdrawal. Notable challenges arise when simulating such hydrological systems; for example, field observations are scarce, and hydrogeological parameters exhibit considerable spatial heterogeneity. To reduce the simulation uncertainties, in addition to groundwater head and river discharge measurements, we adopted remote sensing-based evapotranspiration data and

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21

Krause, S., and A. Bronstert. "An advanced approach for catchment delineation and water balance modelling within wetlands and floodplains." Advances in Geosciences 5 (December 16, 2005): 1–5. http://dx.doi.org/10.5194/adgeo-5-1-2005.

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Abstract. Water balance of wetlands within lowland floodplains is strongly influenced by the temporally variable spatial extent of the interactions between groundwater and surface water. A robust algorithm will be introduced which makes it possible to delineate the interaction zone between the lowland river and the floodplain. This interaction zone is specified as the "Direct Catchment" which is defined by the part of the connected floodplain in which wetland water balance is mainly affected by the surface water dynamics of the adjacent river. The delineation algorithm is based on transfer fun

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22

Nie, Wen, Yong-chang Liang, Lin Chen, and Wei Shao. "Modelling of River-Groundwater Interactions under Rainfall Events Based on a Modified Tank Model." Geofluids 2017 (2017): 1–11. http://dx.doi.org/10.1155/2017/5192473.

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A multitank model experiment is employed to simulate the river-groundwater interaction under rainfall events. These experiments involve coarse and fine materials and rainfall events of 45 and 65 mm/hr. We developed a modified tank model for estimation of the groundwater table and river levels in these experiments. Parameter training of our tank model includes two algorithms: (i) the nonincremental learning algorithm-based model can predict the pore water pressure (PWP) in a slope and river under a 65 mm/hr rainfall event (coarse material) with Nash–Sutcliffe efficiency (NSE) = 0.427 and −0.909

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23

Ahring, T. S., and D. R. Steward. "Groundwater surface water interactions through streambeds and the role of phreatophytes in identifying important recharge zones." Hydrology and Earth System Sciences Discussions 9, no. 6 (2012): 7613–38. http://dx.doi.org/10.5194/hessd-9-7613-2012.

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Abstract. Groundwater and surface water interactions within riparian corridors impact the distribution of phreatophytes that tap into groundwater stores. The changes in canopy area of phreatophytes over time is related to changes in depth to groundwater, distance from a stream or river, and hydrologic soil group. Remote sensing was used to determine the location of trees with predevelopment and post-development aerial photography over the Ogallala Aquifer in the central plains of the United States. It was found that once the depth to groundwater becomes greater than about 3 m, tree populations

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Lee, Hyeonju, Min-Ho Koo, Byong Wook Cho, et al. "Effects of Baekje Weir Operation on the Stream–Aquifer Interaction in the Geum River Basin, South Korea." Water 12, no. 11 (2020): 2984. http://dx.doi.org/10.3390/w12112984.

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Hydraulic structures have a significant impact on riverine environment, leading to changes in stream–aquifer interactions. In South Korea, 16 weirs were constructed in four major rivers, in 2012, to secure sufficient water resources, and some weirs operated periodically for natural ecosystem recovery from 2017. The changed groundwater flow system due to weir operation affected the groundwater level and quality, which also affected groundwater use. In this study, we analyzed the changes in the groundwater flow system near the Geum River during the Baekje weir operation using Visual MODFLOW Clas

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25

Strauch, G., R. Oyarzún, F. Reinstorf, J. Oyarzún, M. Schirmer, and K. Knöller. "Interaction of water components in the semi-arid Huasco and Limarí river basins, North Central Chile." Advances in Geosciences 22 (October 13, 2009): 51–57. http://dx.doi.org/10.5194/adgeo-22-51-2009.

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Abstract. For sustainable water resource management in semi-arid regions, sound information is required about interactions between the different components of the water system: rain/snow precipitation, surface/subsurface run-off, groundwater recharge. Exemplarily, the Huasco and Limarí river basins as water stressed river catchments have been studied by isotope and hydrochemical methods for (i) the origin of water, (ii) water quality, (iii) relations of surface and groundwater. Applying the complex multi-isotopic and hydrochemical methodology to the water components of the Huasco and Limarí ba

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Koehn, Weston J., Stacey E. Tucker-Kulesza, and David R. Steward. "Conceptualizing Groundwater-Surface Water Interactions within the Ogallala Aquifer Region using Electrical Resistivity Imaging." Journal of Environmental and Engineering Geophysics 24, no. 2 (2019): 185–99. http://dx.doi.org/10.2113/jeeg24.2.185.

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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 underst

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McDonald, Alyson K., Zhuping Sheng, Charles R. Hart, and Bradford P. Wilcox. "Studies of a regulated dryland river: surface-groundwater interactions." Hydrological Processes 27, no. 12 (2012): 1819–28. http://dx.doi.org/10.1002/hyp.9340.

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Texier, Jérôme, Julio Gonçalvès, and Agnès Rivière. "Numerical Assessment of Groundwater Flowpaths below a Streambed in Alluvial Plains Impacted by a Pumping Field." Water 14, no. 7 (2022): 1100. http://dx.doi.org/10.3390/w14071100.

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The quality of the water from a riverbank well field is the result of the mixing ratios between the surface water and the local and regional groundwater. The mixing ratio is controlled by the complex processes involved in the surface water–groundwater interactions. In addition, the drawdown of the groundwater level greatly determines the water head differences between the river water and groundwater, as well as the field flowpath inside the alluvial plain, which subsequently impacts the water origin in the well. In common view, groundwater flows from both sides of the valley towards the river,

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Yu, M. C. L., I. Cartwright, J. L. Braden, and S. T. de Bree. "Examining the spatial and temporal variation of groundwater inflows to a valley-to-floodplain river using <sup>222</sup>Rn, geochemistry and river discharge: the Ovens River, southeast Australia." Hydrology and Earth System Sciences Discussions 10, no. 4 (2013): 5225–67. http://dx.doi.org/10.5194/hessd-10-5225-2013.

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Abstract. Radon (222Rn) and major ion geochemistry were used to define and quantify the catchment-scale river-aquifer interactions along the Ovens River in the southeast Murray-Darling Basin, Victoria, Australia, between September 2009 and October 2011. The Ovens River is characterized by the transition from a single channel river residing within a mountain valley in the upper catchment to a multi-channel meandering river on flat alluvial plains in the lower catchment. Overall, the river is dominated by gaining reaches, receiving groundwater from both alluvial and basement aquifers. The distri

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Chang, Sun Woo, and Il-Moon Chung. "Water Budget Analysis Considering Surface Water–Groundwater Interactions in the Exploitation of Seasonally Varying Agricultural Groundwater." Hydrology 8, no. 2 (2021): 60. http://dx.doi.org/10.3390/hydrology8020060.

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In South Korea, groundwater intended for use in greenhouse cultivation is collected from shallow riverside aquifers as part of agricultural activities during the winter season. This study quantified the effects of intensive groundwater intake on aquifers during the winter and examined the roles of nearby rivers in this process. Observation data were collected for approximately two years from six wells and two river-level observation points on the study site. Furthermore, the river water levels before and after the weir structures were examined in detail, because they are determined by artifici

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Tong, Xiaoxia, Hui Tang, Rong Gan, Zitao Li, Xinlin He, and Shuqian Gu. "Characteristics and Causes of Changing Groundwater Quality in the Boundary Line of the Middle and Lower Yellow River (Right Bank)." Water 14, no. 12 (2022): 1846. http://dx.doi.org/10.3390/w14121846.

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The alluvial plain in the middle and lower reaches of the Yellow River is an important agricultural production base that affects groundwater quality. Groundwater quality in the region is related to the residential and production uses of water by local residents. Samples of shallow groundwater and river water were collected from the right bank of the middle and lower reaches of the Yellow River to determine the evolution and causes of hydrochemical characteristics, and the relationship between the hydrochemical evolution of river water and groundwater was explored. The results showed that the s

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Yu, M. C. L., I. Cartwright, J. L. Braden, and S. T. de Bree. "Examining the spatial and temporal variation of groundwater inflows to a valley-to-floodplain river using <sup>222</sup>Rn, geochemistry and river discharge: the Ovens River, southeast Australia." Hydrology and Earth System Sciences 17, no. 12 (2013): 4907–24. http://dx.doi.org/10.5194/hess-17-4907-2013.

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Abstract. Radon (222Rn) and major ion geochemistry were used to define and quantify the catchment-scale groundwater-surface water interactions along the Ovens River in the southeast Murray–Darling Basin, Victoria, Australia, between September 2009 and October 2011. The Ovens River is characterized by the transition from a single channel within a mountain valley in the upper catchment to a multi-channel meandering river on flat alluvial plains in the lower catchment. Overall, the Ovens River is dominated by gaining reaches, receiving groundwater from both alluvial and basement aquifers. The dis

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Bisht, Gautam, Maoyi Huang, Tian Zhou, et al. "Coupling a three-dimensional subsurface flow and transport model with a land surface model to simulate stream–aquifer–land interactions (CP v1.0)." Geoscientific Model Development 10, no. 12 (2017): 4539–62. http://dx.doi.org/10.5194/gmd-10-4539-2017.

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Abstract. A fully coupled three-dimensional surface and subsurface land model is developed and applied to a site along the Columbia River to simulate three-way interactions among river water, groundwater, and land surface processes. The model features the coupling of the Community Land Model version 4.5 (CLM4.5) and a massively parallel multiphysics reactive transport model (PFLOTRAN). The coupled model, named CP v1.0, is applied to a 400 m × 400 m study domain instrumented with groundwater monitoring wells along the Columbia River shoreline. CP v1.0 simulations are performed at three spatial

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Négrel, P., E. Petelet-Giraud, and D. Widory. "Strontium isotope geochemistry of alluvial groundwater: a tracer for groundwater resources characterisation." Hydrology and Earth System Sciences 8, no. 5 (2004): 959–72. http://dx.doi.org/10.5194/hess-8-959-2004.

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Abstract. This study presents strontium isotope and major ion data of shallow groundwater and river water from the Ile du Chambon catchment, located on the Allier river in the Massif Central (France). There are large variations in the major-element contents in the surface- and groundwater. Plotting of Na vs. Cl contents and Ca, Mg, NO3, K, SO4, HCO3, Sr concentrations reflect water–rock interaction (carbonate dissolution for Ca, Mg, HCO3 and Sr because the bedrock contains marly limestones), agricultural input (farming and fertilising) and sewage effluents (for NO3, K, SO4), although some wate

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Alaghmand, S., S. Beecham, and A. Hassanli. "Fully integrated physically-based numerical modelling of impacts of groundwater extraction on surface and irrigation-induced groundwater interactions: case study Lower River Murray, Australia." Natural Hazards and Earth System Sciences Discussions 1, no. 4 (2013): 3577–624. http://dx.doi.org/10.5194/nhessd-1-3577-2013.

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Abstract. Combination of reduction in the frequency, duration and magnitude of natural floods, rising saline water-table in floodplains and excessive evapotranspiration have led to an irrigation-induced groundwater mound forced the naturally saline groundwater onto the floodplain in the Lower River Murray. It is during the attenuation phase of floods that these large salt accumulations are likely to be mobilised and will discharge into the river. The Independent Audit Group for Salinity highlighted this as the most significant risk in the Murray–Darling Basin. South Australian government and c

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Dong, Linyao, Yiwei Guo, Wenjian Tang, Wentao Xu, and Zhongjie Fan. "Statistical Evaluation of the Influences of Precipitation and River Level Fluctuations on Groundwater in Yoshino River Basin, Japan." Water 14, no. 4 (2022): 625. http://dx.doi.org/10.3390/w14040625.

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Precise evaluation of the correlations among precipitation, groundwater and river water enhance our understanding on regional hydrological circulation and water resource management. The innovative and efficient use of wavelet analysis has been able to identify significant interactions in the spatial and temporal domains and to estimate the recharge travel time. In this paper, a wavelet analysis was utilized to analyse 43 years of monthly, and 2 years of daily, precipitation, river level and groundwater level data in the Yoshino River Basin, Japan. There were two main results: (1) There was a s

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Schneider, P., T. Vogt, M. Schirmer, et al. "Towards improved instrumentation for assessing river-groundwater interactions in a restored river corridor." Hydrology and Earth System Sciences 15, no. 8 (2011): 2531–49. http://dx.doi.org/10.5194/hess-15-2531-2011.

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Abstract. River restoration projects have been launched over the last two decades to improve the ecological status and water quality of regulated rivers. As most restored rivers are not monitored at all, it is difficult to predict consequences of restoration projects or analyze why restorations fail or are successful. It is thus necessary to implement efficient field assessment strategies, for example by employing sensor networks that continuously measure physical parameters at high spatial and temporal resolution. This paper focuses on the design and implementation of an instrumentation strat

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Schneider, P., T. Vogt, M. Schirmer, et al. "Towards improved instrumentation for assessing river-groundwater interactions in a restored river corridor." Hydrology and Earth System Sciences Discussions 8, no. 2 (2011): 2503–53. http://dx.doi.org/10.5194/hessd-8-2503-2011.

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Abstract. River restoration projects have been launched over the last two decades to improve the ecological status and water quality of regulated rivers. As most restored rivers are not monitored at all, it is difficult to predict consequences of restoration projects or analyze why restorations fail or are successful. It is thus necessary to implement efficient field assessment strategies, for example by employing sensor networks that continuously measure physical parameters at high spatial and temporal resolution. This paper focuses on the design and implementation of an instrumentation strat

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Girard, Pierre, Carolina J. da Silva, and Mara Abdo. "River–groundwater interactions in the Brazilian Pantanal. The case of the Cuiabá River." Journal of Hydrology 283, no. 1-4 (2003): 57–66. http://dx.doi.org/10.1016/s0022-1694(03)00235-x.

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Unland, N. P., I. Cartwright, D. I. Cendón, and R. Chisari. "Residence times and mixing of water in river banks: implications for recharge and groundwater – surface water exchange." Hydrology and Earth System Sciences Discussions 11, no. 2 (2014): 1651–91. http://dx.doi.org/10.5194/hessd-11-1651-2014.

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Abstract. The residence time of groundwater within 50 m of the Tambo River, South East Australia, has been estimated through the combined use of 3H and 14C. Groundwater residence times increase towards the Tambo River which implies a gaining river system and not increasing bank storage with proximity to the Tambo River. Major ion concentrations and δ2H and δ18O values of bank water also indicate that bank infiltration does not significantly impact groundwater chemistry under baseflow and post-flood conditions, suggesting that the gaining nature of the river may be driving the return of bank st

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Calderon, H., and S. Uhlenbrook. "Investigation of seasonal river–aquifer interactions in a tropical coastal area controlled by tidal sand ridges." Hydrology and Earth System Sciences Discussions 11, no. 8 (2014): 9759–90. http://dx.doi.org/10.5194/hessd-11-9759-2014.

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Abstract. Water exchanges between streams and aquifers influence the quantity and quality of water in both domains. Seasonal river–aquifer interactions were investigated in a tropical coastal area where tidal sand ridges control river discharge to the sea. The study site is located in southwestern Nicaragua, dominated by humid tropical hydro-climatic conditions. The aquifer provides water to the rural town of Ostional. Connectivity between the river and the aquifer influences water quality and water availability for humans and for the downstream estuarine ecosystem. The effect of stream stage

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Fu, Yunmei, Yanhui Dong, Yueqing Xie, Zhifang Xu, and Liheng Wang. "Impacts of Regional Groundwater Flow and River Fluctuation on Floodplain Wetlands in the Middle Reach of the Yellow River." Water 12, no. 7 (2020): 1922. http://dx.doi.org/10.3390/w12071922.

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Floodplain wetlands are of great importance in the entire river and floodplain ecosystems. Understanding the hydrological processes of floodplain wetlands is fundamental to study the changes in wetlands caused by climate change and human activities. In this study, floodplain wetlands along the middle reach of the Yellow River were selected as a study area. The hydrological processes and the interactions between the river and the underlying aquifer were investigated by combining remote sensing, hydraulic monitoring, and numerical modeling. Wetland areas from 2014 to 2019 were extracted from Lan

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Korkka‐Niemi, Kirsti, Anna‐Liisa Kivimäki, and Maria Nygård. "Observations on groundwater‐surface water interactions at River Vantaa, Finland." Management of Environmental Quality: An International Journal 23, no. 2 (2012): 222–31. http://dx.doi.org/10.1108/14777831211204958.

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Islam, Md Shajedul, and M. G. Mostafa. "Evaluation of Hydrogeochemical Processes in Groundwater Using Geochemical and Geostatistical Approaches in the Upper Bengal Basin." Geofluids 2022 (April 6, 2022): 1–21. http://dx.doi.org/10.1155/2022/9591717.

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Overexploitation of groundwater for irrigation and radical changes of river morphology in the Bengal basin has posed difficulties to sustainable management of this resource. Forty groundwater samples were collected from tube wells of the pre-monsoon and postmonsoon seasons in 2020, and the water parameters were analyzed. The hydrogeochemical studies, bivariate plots, and multivariate techniques were used to evaluate the rock-water interactions, influencing factors, and contamination pathways. The principal component analysis (PCA) was used to extract several directions in the data space and un

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Unland, N. P., I. Cartwright, D. I. Cendón, and R. Chisari. "Residence times and mixing of water in river banks: implications for recharge and groundwater–surface water exchange." Hydrology and Earth System Sciences 18, no. 12 (2014): 5109–24. http://dx.doi.org/10.5194/hess-18-5109-2014.

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Abstract. Bank exchange processes within 50 m of the Tambo River, southeast Australia, have been investigated through the combined use of 3H and 14C. Groundwater residence times increase towards the Tambo River, which suggests the absence of significant bank storage. Major ion concentrations and δ2H and δ18O values of bank water also indicate that bank infiltration does not significantly impact groundwater chemistry under baseflow and post-flood conditions, suggesting that the gaining nature of the river may be driving the return of bank storage water back into the Tambo River within days of p

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Nainggolan, Lamtupa, Chuen-Fa Ni, Yahya Darmawan, I.-Hsien Lee, Chi-Ping Lin, and Wei-Ci Li. "Data-Driven Approach to Assess Spatial-Temporal Interactions of Groundwater and Precipitation in Choushui River Groundwater Basin, Taiwan." Water 12, no. 11 (2020): 3097. http://dx.doi.org/10.3390/w12113097.

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The scarcity of groundwater and precipitation stations has limited accurate assessments of basin-scale groundwater systems. This study proposes a workflow that integrates satellite and on-site observations to improve the spatial and temporal resolution of the groundwater level and enable recharge estimations for the Choushui River groundwater basin (CRGB) in Western Taiwan. The workflow involves multiple data processing steps, including analysis of correlation, evaluation of residuals, and geostatistical interpolation based on kriging methods. The observed groundwater levels and recharge are t

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Kasahara, Tamao, Thibault Datry, Michael Mutz, and Andrew J. Boulton. "Treating causes not symptoms: restoration of surface - groundwater interactions in rivers." Marine and Freshwater Research 60, no. 9 (2009): 976. http://dx.doi.org/10.1071/mf09047.

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Many river restoration projects seek to address issues associated with impaired hydrological and ecological connectivity in longitudinal (e.g. effects of dams, weirs) or lateral (e.g. alienated floodplain) dimensions. Efforts to restore the vertical dimension of impaired stream–groundwater exchange are rare, hampered by limited understanding of the factors controlling this linkage in natural alluvial rivers. We propose a simplified two-axis model of the ‘primary drivers’ (sediment structure and vertical hydraulic gradient) of stream–groundwater exchange that acknowledges their interaction and

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Deng, Chenda, and Ryan T. Bailey. "Assessing the Impact of Artificial Recharge Ponds on Hydrological Fluxes in an Irrigated Stream–Aquifer System." Hydrology 9, no. 5 (2022): 91. http://dx.doi.org/10.3390/hydrology9050091.

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Artificial recharge ponds have been used increasingly in recent years to store water in underlying aquifers and modify baseline groundwater gradients or alter natural hydrologic fluxes and state variables in an aquifer system. The number of constructed ponds, their geographic spacing, and the volume of water diverted to each pond can have a significant impact on baseline system hydrologic fluxes and state variables such as groundwater head, with the latter sometimes rising to cause waterlogging in cultivated areas. This study seeks to quantify the impact of recharge ponds on groundwater state

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Shi, Yu Qing, and Yue Long Zhu. "Application of Comprehensive Water Flow Numerical Solution at Yifeng River Basin." Advanced Materials Research 864-867 (December 2013): 2327–30. http://dx.doi.org/10.4028/www.scientific.net/amr.864-867.2327.

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Our article is studied with the improvement of a physically-based numerical model that uses for a new finite element solution to the transient or steady problems of the groundwater and surface water flows of a specific region with the help of a Geographic Information Systems (GIS) to store, manage, represent and take decides on all condition. Our article research subsurface and surface model proposes groundwater and surface water interact to be depth averaged through a new interpretation of a linear river flood calculus method. Overland flows and infiltration rates production processes are est

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Bourgault, M. A., M. Larocque, and M. Roy. "Simulation of aquifer-peatland-river interactions under climate change." Hydrology Research 45, no. 3 (2013): 425–40. http://dx.doi.org/10.2166/nh.2013.228.

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Wetlands play an important role in preventing extreme low flows in rivers and groundwater level drawdowns during drought periods. This hydrological function could become increasingly important under a warmer climate. Links between peatlands, aquifers, and rivers remain inadequately understood. The objective of this study was to evaluate the hydrologic functions of the Lanoraie peatland complex in southern Quebec, Canada, under different climate conditions. This peatland complex has developed in the beds of former fluvial channels during the final stages of the last deglaciation. The peatland c

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