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Journal articles on the topic 'Groundwater Interaction'

Author: Grafiati

Published: 6 September 2023

Last updated: 26 July 2025

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1

Guggenmos, M. R., B. M. Jackson, and C. J. Daughney. "Investigation of groundwater-surface water interaction using hydrochemical sampling with high temporal resolution, Mangatarere catchment, New Zealand." Hydrology and Earth System Sciences Discussions 8, no. 6 (2011): 10225–73. http://dx.doi.org/10.5194/hessd-8-10225-2011.

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Abstract. The interaction between groundwater and surface water is dynamic and is known to show considerable spatial and temporal variability. Generally hydrological studies that investigate this interaction are conducted at weekly to yearly timescales and inadvertently lose information contained at the neglected shorter timescales. This paper utilises high resolution physical and chemical measurements to investigate the groundwater and surface water interactions of the small temperate Mangatarere Stream in New Zealand. Continuous electrical conductivity, water temperature and stage measuremen

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2

Guggenmos, M. R., C. J. Daughney, B. M. Jackson, and U. Morgenstern. "Regional-scale identification of groundwater-surface water interaction using hydrochemistry and multivariate statistical methods, Wairarapa Valley, New Zealand." Hydrology and Earth System Sciences 15, no. 11 (2011): 3383–98. http://dx.doi.org/10.5194/hess-15-3383-2011.

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Abstract. Identifying areas of interaction between groundwater and surface water is crucial for effective environmental management, because this interaction is known to influence water quantity and quality. This paper applies hydrochemistry and multivariate statistics to identify locations and mechanisms of groundwater-surface water interaction in the pastorally dominated Wairarapa Valley, New Zealand. Hierarchical Cluster Analysis (HCA) and Principal Components Analysis (PCA) were conducted using site-specific median values of Ca, Mg, Na, K, HCO3, Cl, SO4 and electrical conductivity from 22 s

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Guggenmos, M. R., C. J. Daughney, B. M. Jackson, and U. Morgenstern. "Regional-scale identification of groundwater-surface water interaction using hydrochemistry and multivariate statistical methods, Wairarapa Valley, New Zealand." Hydrology and Earth System Sciences Discussions 8, no. 4 (2011): 6443–87. http://dx.doi.org/10.5194/hessd-8-6443-2011.

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Abstract. Identifying areas of interaction between groundwater and surface water is crucial for effective environmental management, because this interaction is known to influence water quantity and quality. This paper applies hydrochemistry and multivariate statistics to identify locations and mechanisms of groundwater-surface water interaction in the pastorally dominated Wairarapa Valley, New Zealand. Hierarchical Cluster Analysis (HCA) and Principal Components Analysis (PCA) were conducted using site-specific median values of Ca, Mg, Na, K, HCO3, Cl, SO4 and electrical conductivity from 22 s

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4

G, Ottos C., and Isaac E. O. "Modeling of Predictive interaction of Water Parameters in Groundwater." International Journal of Trend in Scientific Research and Development Volume-2, Issue-3 (2018): 1091–96. http://dx.doi.org/10.31142/ijtsrd11292.

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5

Ó Dochartaigh, Brighid É., Alan M. MacDonald, Andrew R. Black, et al. "Groundwater–glacier meltwater interaction in proglacial aquifers." Hydrology and Earth System Sciences 23, no. 11 (2019): 4527–39. http://dx.doi.org/10.5194/hess-23-4527-2019.

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Abstract. Groundwater plays a significant role in glacial hydrology and can buffer changes to the timing and magnitude of flows in meltwater rivers. However, proglacial aquifer characteristics or groundwater dynamics in glacial catchments are rarely studied directly. We provide direct evidence of proglacial groundwater storage, and quantify multi-year groundwater–meltwater dynamics, through detailed aquifer characterisation and intensive high-resolution monitoring of the proglacial system of a rapidly retreating glacier, Virkisjökull, in south-eastern Iceland. Proglacial unconsolidated glaciof

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Young, Steven C., Robert E. Mace, and Carlos Rubinstein. "Surface water-groundwater interaction issues in Texas." Texas Water Journal 9, no. 1 (2018): 129–49. http://dx.doi.org/10.21423/twj.v9i1.7084.

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In Texas, surface water is owned and regulated by the State of Texas, whereas groundwater is owned by respective property owners under the rule of capture. Owners of surface water rights, issued by the state, and groundwater may use and sell their water as a private property right. The Texas Commission on Environmental Quality administers surface water rights, while groundwater conservation districts (where they exist) are primarily responsible for permitting groundwater use. This paper focuses on the complexity of both systems that are designed to manage water resources differently with speci

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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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8

Novikov, Dmitry A. "Chemical equilibrium of groundwater with minerals of the host rocks in Upper Jurassic sediments (Arctic regions of Western Siberia)." E3S Web of Conferences 98 (2019): 01037. http://dx.doi.org/10.1051/e3sconf/20199801037.

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The results of thermodynamic calculations for a water-rock system in the Upper Jurassic deposits of the Arctic regions of Western Siberia are presented. In the area under investigation the groundwaters have been identified with mineralization up to 63.3 g/L and various chemical composition and genesis. Despite the long interaction with the rock (150-160 ma) equilibrium with endogenous minerals (albite, microcline and anorthite) is practically not observed. At the same time, groundwaters are in equilibrium with clay minerals and micas, such as: Caand Na-montmorillonites, kaolinite, paragonite,

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9

Shepelev, V. V., and M. N. Zhelezniak. "Main characteristics of the groundwater and permafrost interaction." Arctic and Subarctic Natural Resources 28, no. 4 (2024): 533–39. http://dx.doi.org/10.31242/2618-9712-2023-28-4-533-539.

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An analysis of the groundwater and permafrost interaction is presented in this study. The analysis is based on an extensive review of scientific literature and our own investigations. The article specifically examines the significant impact of phase changes between liquid and solid states in groundwater, including the freezing of aquifers and the thawing of ice-rich permafrost. The discussion highlights the essential characteristics of groundwater interactions with frozen ground in permafrost regions.

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10

Meng, Fanao, Changlai Xiao, Xiujuan Liang, Ge Wang, and Ying Sun. "Regularity and a statistical model of surface water and groundwater interaction in the Taoer River alluvial fan, China." Water Supply 19, no. 8 (2019): 2379–90. http://dx.doi.org/10.2166/ws.2019.118.

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Abstract The study of surface water and groundwater (SGW) interaction can be used to improve water resource management. Herein, annual and monthly interactions in the Taoer River alluvial fan were calculated for the 1956–2014 period using the surface water balance method and the groundwater balance method, and a statistical model of interaction was obtained. The SGW interaction is shown in terms of the recharge of groundwater by surface water. From 1956 to 2014, the amount of SGW interaction in the study area varied greatly, averaging 27,848.4 × 104m3 annually. SGW interaction decreased gradua

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11

Haque, Arefin, Amgad Salama, Kei Lo, and Peng Wu. "Surface and Groundwater Interactions: A Review of Coupling Strategies in Detailed Domain Models." Hydrology 8, no. 1 (2021): 35. http://dx.doi.org/10.3390/hydrology8010035.

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In groundwater numerical simulations, the interactions between surface and groundwater have received great attention due to difficulties related to their validation and calibration due to the dynamic exchange occurring at the soil–water interface. The interaction is complex at small scales. However, at larger scales, the interaction is even more complicated, and has never been fully addressed. A clear understanding of the coupling strategies between the surface and groundwater is essential in order to develop numerical models for successful simulations. In the present review, two of the most c

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Mnati, Maher, Ali Al-Aboodi, and Ayman Hassan. "Simulation of Interaction Between Groundwater and Surface Water in Safwan-Zubair Area, South of Iraq." Basrah journal for engineering science 23, no. 1 (2023): 50–55. http://dx.doi.org/10.33971/bjes.23.1.7.

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Groundwater in arid and semi-arid regions, such as the studied area (Safwan Al-Zubair area, south of Iraq), is of specific meaning as a major source for domestic use and irrigation demand. There is a need to better understand the interactions between groundwater and surface water (Shatt Al-Basrah Canal). These interactions can negatively affect the quality of groundwater in this area, especially that the water of Shatt Al-Basrah Canal contains highly concentrated pollutants. The aim of the study is to investigate the temporal disparity of river-aquifer interactions and count the amount of rive

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13

Bai, Zhanxue, Xinwei Hou, Xiangquan Li, et al. "Hydrogeochemical Characteristics and Sulfate Source of Groundwater in Sangu Spring Basin, China." Water 16, no. 20 (2024): 2884. http://dx.doi.org/10.3390/w16202884.

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The Sangu Spring Basin is located in an important economic area, and groundwater is the main source of water for local life and industry. Understanding the sources of chemical components in groundwater is important for the development and utilization of groundwater. In this paper, we analyzed the origin of the chemical components of groundwater and their evolution in the Sangu Spring Basin using statistical analysis, Piper diagrams, Gibbs diagrams, ion ratios, and combined hydrochemistry–isotope analyses. The results show that the groundwater in the Sangu Spring Basin is mainly derived from at

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14

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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15

Nefzaoui, Farah, Mohamed Fethi Ben Hamouda, Paula Maria Carreira, José Manuel Marques, and Hans G. M. Eggenkamp. "Evidence for Groundwater Salinity Origin Based on Hydrogeochemical and Isotopic (2H, 18O, 37Cl, 3H, 13C, 14C) Approaches: Sousse, Eastern Tunisia." Water 15, no. 6 (2023): 1242. http://dx.doi.org/10.3390/w15061242.

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The key processes responsible for the rise in groundwater salinization in the Mio–Pliocene aquifer system of Sousse (Tunisia, eastern coastline) were identified through a multidisciplinary approach based on the use of geochemical, stable (2H, 13C, 18O and 37Cl) and radioactive (3H and 14C) isotope methods. In the study region, the mineralization of groundwaters is related to water–rock interaction ascribed to the dissolution of minerals in evaporite rocks, as well as to saltwater intrusion. Both processes explain the development of groundwaters in which Cl and Na dominantly determine the groun

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16

Huerta, Pedro, Pedro Carrasco-García, Ildefonso Armenteros, Clemente Recio, Javier Carrasco-García, and Esther Rodríguez-Jiménez. "TDEM Soundings as a Tool to Determine Seasonal Variations of Groundwater Salinity (Villafáfila Lakes, Spain)." Water 14, no. 15 (2022): 2402. http://dx.doi.org/10.3390/w14152402.

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Interaction between groundwaters with different salinities and lakes show seasonal variations driven by changes in precipitation and evapotranspiration. In the vicinity of Villafáfila lakes, local fresh and brackish regional groundwaters feeds the lakes, forming a brine in the lake sediments aquitard. Two TDEM surveys (summer 2019 and winter 2020) were carried out. Five TDEM soundings were acquired at the same location for each survey, forming a profile from the hills to the lake-shore. Simultaneously to the TDEM surveys, electric conductivity of lake water and groundwater was measured. The re

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17

Sader, Jamil A., Anna L. Harrison, M. Beth McClenaghan, et al. "Generation of high-pH groundwaters and H2 gas by groundwater–kimberlite interaction, northeastern Ontario, Canada." Canadian Mineralogist 59, no. 5 (2021): 1261–76. http://dx.doi.org/10.3749/canmin.2000048.

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ABSTRACT We report new isotopic data for H2 and CH4 gases and Sr for groundwater collected from Jurassic Kirkland Lake kimberlites in northern Ontario, Canada. Groundwaters interacting with kimberlites have elevated pH (up to 12.4), are reducing (Eh as low as the H2-H2O couple), are dominated by OH− alkalinity, and have non-radiogenic (mantle) 87Sr/86Sr values (∼0.706–0.707). Most significantly, the highest pH groundwaters have low Mg, high K/Mg, and are associated with abundant reduced gases (H2 ± CH4). Open system conditions favor higher dissolved inorganic carbon and CH4 production, whereas

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18

Qian, Yong, Shijun Zhen, Chen Yue, and Xiangxiang Cui. "Distribution and Origins of Hardness in Shallow and Deep Groundwaters of the Hebei Plain, China." Water 16, no. 2 (2024): 310. http://dx.doi.org/10.3390/w16020310.

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Elevated hardness concentrations in groundwater have become a noteworthy concern in recent decades because long-term drinking of groundwater with high levels of hardness is an important factor resulting in chronic kidney diseases. In this study, the distribution and origins of groundwater total hardness (TH) in various sub-plains and different land-use areas of the Hebei Plain (HBP) were investigated. A total of 445 groundwater samples in the HBP were collected once in 2021, and twelve chemical parameters, including TH in groundwater, were analyzed. Results showed that TH-rich (>450 mg/L) s

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19

Shi, Jian-Xun, Zhao-Hui Li, Yong-Qiang He, Guo-Ming Zhang, and Ming-Qiang Wei. "The Influence of Physical and Chemical Reactions on Water Leakage in a Multiarch Tunnel." Advances in Civil Engineering 2020 (September 23, 2020): 1–8. http://dx.doi.org/10.1155/2020/8830739.

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In many tunnels in China, the groundwater is acidic and carbonated, causing in challenges in the prevention and control of leakages of the existing tunnels and tunnels under construction. Research on tunnel leakage and the physical and chemical effects of water due to water-rock interactions is a trending topic. In addition, there is a big difference between the waterproof and drainage of multiarch tunnels and separate tunnels. In this study, the mechanism of the interaction between the groundwater and the surrounding rock of a multiarch tunnel were analyzed. The relationship between the leaka

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20

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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21

KOBAYASHI, Masao. "Interaction between Lake Water and Groundwater." Journal of Groundwater Hydrology 43, no. 2 (2001): 101–12. http://dx.doi.org/10.5917/jagh1987.43.101.

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22

Nawalany, Marek, Grzegorz Sinicyn, Maria Grodzka-Łukaszewska, and Dorota Mirosław-Świątek. "Groundwater–Surface Water Interaction—Analytical Approach." Water 12, no. 6 (2020): 1792. http://dx.doi.org/10.3390/w12061792.

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Modelling of water flow in the hyporheic zone and calculations of water exchange between groundwater and surface waters are important issues in modern environmental research. The article presents the Analytical Hyporheic Flux approach (AHF) permitting calculation of the amount of water exchange in the hyporheic zone, including vertical water seepage through the streambed and horizontal seepage through river banks. The outcome of the model, namely water fluxes, is compared with the corresponding results from the numerical model SEEP2D and simple Darcy-type model. The errors of the AHF model, in

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23

Epting, Jannis, Peter Huggenberger, Dirk Radny, et al. "Spatiotemporal scales of river-groundwater interaction – The role of local interaction processes and regional groundwater regimes." Science of The Total Environment 618 (March 2018): 1224–43. http://dx.doi.org/10.1016/j.scitotenv.2017.09.219.

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24

Li, Zihan, Yongjun Fang, Bo Meng, Hui Guo, and Xinqiang Du. "Identification of Groundwater–Surface Water Interaction Using Combined Hydraulic and Hydrogeochemical Methods." Water 16, no. 19 (2024): 2777. http://dx.doi.org/10.3390/w16192777.

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Understanding groundwater–surface water interaction is essential for water resource management and watershed ecological protection. However, the existing studies often emphasize the tracer role of hydrogeochemical methods (including hydrochemistry and isotopes) while underestimating the importance of analyzing watershed hydraulic characteristics, thus neglecting the indications of the driving mechanisms (hydraulic head difference) for the water exchange. Taking the Songhua River in the Sanjiang Plain as an example, this study combines hydraulic, hydrochemical, and isotopic methods to clarify t

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25

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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Pang, Zhonghe, Jie Li, and Jiao Tian. "Noble gas geochemistry and chronology of groundwater in an active rift basin in central China." E3S Web of Conferences 98 (2019): 01040. http://dx.doi.org/10.1051/e3sconf/20199801040.

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Stable noble gas isotopes are excellent groundwater tracers. Radioactive noble gases are emerging new tools in the study of groundwater circulation dynamics. Among these, the 85Kr and 81Kr, and 39Ar have advanced very fast in recent years and exhibit strong potential in the reconstruction of the history of groundwater recharge and evolution in sedimentary basins at different scales. Here, we report the findings in groundwater circulation dynamics as relative to intensive water-rock interactions, heat transfer and He gas flux in Guanzhong Basin located in Xi’an, the geographical centre of China

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Shen, Shuai, Teng Ma, Yao Du, Kewen Luo, Yamin Deng, and Zongjie Lu. "Temporal variations in groundwater nitrogen under intensive groundwater/surface-water interaction." Hydrogeology Journal 27, no. 5 (2019): 1753–66. http://dx.doi.org/10.1007/s10040-019-01952-x.

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28

Mulyadi, A., M. Dede, and M. A. Widiawaty. "Spatial interaction of groundwater and surface topographic using geographically weighted regression in built-up area." IOP Conference Series: Earth and Environmental Science 477 (June 8, 2020): 012023. https://doi.org/10.1088/1755-1315/477/1/012023.

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Groundwater is a primary water resource for human living. In Indonesia, excessive exploitation of groundwater generally occurs in the built-up area due to over-discharge processes characterized by a cone of depression. This research revealed the spatial interaction between groundwater levels and surface topographic using geographically weighted regression in built-up area. Groundwater levels data are obtained from 72 wells in Cikembang, Bandung Regency, whereas surface topographic based on BIG's DEMNas data which has 8 meters spatial resolution. This study showed significant spatial intera

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29

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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30

Wu, Zihao, Yaolin Liu, Guie Li, Yiran Han, Xiaoshun Li, and Yiyun Chen. "Influences of Environmental Variables and Their Interactions on Chinese Farmland Soil Organic Carbon Density and Its Dynamics." Land 11, no. 2 (2022): 208. http://dx.doi.org/10.3390/land11020208.

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Farmland is one of the most important and active components of the soil carbon pool. Exploring the controlling factors of farmland soil organic carbon density (SOCD) and its sequestration rate (SOCDSR) is vital for improving carbon sequestration and addressing climate change. Present studies provide considerable attention to the impacts of natural factors and agricultural management on SOCD and SOCDSR. However, few of them focus on the interaction effects of environmental variables on SOCD and SOCDSR. Therefore, using 64 samples collected from 19 agricultural stations in China, this study expl

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31

Zhao, Zhen, Gongxi Liu, Guangxiong Qin, et al. "Exploring the Hydrochemical Characteristics and Controlling Processes of Groundwater in Agricultural Lower Reaches of a Typical Arid Watershed on Tibetan Plateau." Sustainability 17, no. 5 (2025): 2117. https://doi.org/10.3390/su17052117.

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Groundwater is crucial for domestic, agricultural, and ecological uses, particularly in the lower reaches of arid basins, where its quality often limits availability. A total of 26 phreatic groundwater samples were collected from a typical endorheic watershed on the Tibetan Plateau to assess the hydrochemical characteristics of phreatic groundwater in the lower reaches of arid inland watersheds. The hydrochemical characteristics, quality, and formation mechanisms of groundwater were analyzed using the Entropy-Weight Water Quality Index (EWQI), irrigation water quality indexes (such as sodium a

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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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Long, Tran Thanh, and Sucharit Koontanakulvong. "Groundwater and River Interaction Impact to Aquifer System in Saigon River Basin, Vietnam." Engineering Journal 24, no. 5 (2020): 15–24. http://dx.doi.org/10.4186/ej.2020.24.5.15.

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Since the 1990s, under the pressure of socio-economic growth in the Ho Chi Minh City and nearby provinces, the heavy-extraction of groundwater of this area has dramatically increased to meet high water demand for domestic and industrial purposes. Although the groundwater – Saigon River interaction significantly contributes to groundwater reserves, researchers have been less attentive to fully describe and understand the river recharge. This study attempts to explore the impact of groundwater-river interaction to aquifer system due to pumping increase via field seepage and (O18, H2) isotopic me

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Jing, Shao Dong, Shuai Ling Xu, and Chao Guo Wang. "Analysis of Water-Rock Interaction and Two-Dimensional Seepage Field of Tunnel." Advanced Materials Research 955-959 (June 2014): 3297–301. http://dx.doi.org/10.4028/www.scientific.net/amr.955-959.3297.

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Researches show that groundwater easily leads to tunnel disease. Groundwater seepage field is changed after the tunnel excavated. When crossing the fault fracture zone with groundwater, the tunnel will be cut into independent units with water. Along with the tensile stress on the tunnel invert and upper apex, it's prone to landslides and other damages. This paper analyzes the mechanism of interaction of water and rock, and describes the failure mechanism made by groundwater on the rock by RFPA2D, then analyzes the changes of groundwater seepage field before and after the tunnel excavation by u

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35

Zhu, Meijia, Shiqin Wang, Xiaole Kong, et al. "Interaction of Surface Water and Groundwater Influenced by Groundwater Over-Extraction, Waste Water Discharge and Water Transfer in Xiong’an New Area, China." Water 11, no. 3 (2019): 539. http://dx.doi.org/10.3390/w11030539.

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Understanding the interaction of surface water and groundwater affected by anthropogenic activities is of great importance for water resource and water quality management. The Xiong’an New Area, located in the North China Plain, has been designated a new building area by China’s government. Groundwater has been over pumped and artificial water was transferred to meet the water supply in this region. Therefore, the natural interaction of surface water and groundwater has been greatly changed and there has been a complex impact of the groundwater from anthropogenic activities. In this study, we

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Xie, Hong-Yu, Xiao-Wei Jiang, Shu-Cong Tan, et al. "Interaction of soil water and groundwater during the freezing–thawing cycle: field observations and numerical modeling." Hydrology and Earth System Sciences 25, no. 8 (2021): 4243–57. http://dx.doi.org/10.5194/hess-25-4243-2021.

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Abstract. Freezing-induced groundwater-level decline is widely observed in regions with a shallow water table, but many existing studies on freezing-induced groundwater migration do not account for freezing-induced water-level fluctuations. Here, by combining detailed field observations of liquid soil water content and groundwater-level fluctuations at a site in the Ordos Plateau, China, and numerical modeling, we showed that the interaction of soil water and groundwater dynamics was controlled by wintertime atmospheric conditions and topographically driven lateral groundwater inflow. With an

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Hidayat, Hadi, Boy Yoseph та Teuku Yan Waliana Muda Iskandarsyah. "Characteristics of Groundwater Hydrochemistry and Stable Isotopes (δ18O & δ2H) in Cadasari, Banten, Indonesia". Journal of Geoscience, Engineering, Environment, and Technology 10, № 02 (2025): 154–61. https://doi.org/10.25299/jgeet.2025.10.02.21531.

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Groundwater is an essential resource for drinking and domestic use, displaying significant diversity in volcanic regions.This study focuses on Cadasari, Banten, Indonesia, and aims to determine the hydrochemical characteristics of groundwater and the stable isotopes (δ18O & δ2H). Hydrogeological mapping was employed, and analytical data were collected from 20 groundwater sources, including springs, rivers, and wells, at elevations ranging from 167 to 928 meters above sea level. The hydrochemical analysis revealed various groundwater types, such as Ca-HCO3, Ca+Mg-HCO3, Na+K+Ca-HCO3, and Na+

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Olea-Olea, Selene, Raúl A. Silva-Aguilera, Javier Alcocer, et al. "Water–Rock Interaction Processes in Groundwater and Flows in a Maar Lake in Central Mexico." Water 16, no. 5 (2024): 715. http://dx.doi.org/10.3390/w16050715.

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Tropical maar lakes are distinct ecosystems with unique ecological features. To comprehend, manage, and conserve these lakes, it is essential to understand their water sources, particularly groundwater, and the hydrogeochemical processes shaping their water chemistry. This research focuses on the maar lake Alchichica in central Mexico, known for harboring 18 new and endemic species and a ring of stromatolites. With groundwater discharge as the primary source, concerns arise over anthropic extraction impacts on water levels and stromatolite survival. Sampling six wells and one piezometer reveal

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Zhao, Yawei, Chen Yang, and Sijia Xie. "Research Progress of Groundwater and Surface Water Interaction in Riparian Zone Based on Bibliometrics." International Journal of Natural Resources and Environmental Studies 5, no. 3 (2025): 129–46. https://doi.org/10.62051/ijnres.v5n3.15.

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The interaction between groundwater and surface water was a key link in the study of hydrological and ecological processes in riparian zones. Based on the literature of the SCI-E database of the core collection of Web of Science as the data source, the CiteSpace bibliometric tool was used to visualize the research literature on the interaction between groundwater and surface water in the riparian zone from the aspects of annual publication volume, research strength, subject distribution, and research hotspot frontier. The results showed that the number of research papers on the interaction bet

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Houria, Baazi, Kalla Mahdi, and Tebbi Fatima Zohra. "Hydrochemical Characterisation of Groundwater Quality: Merdja Plain (Tebessa Town, Algeria)." Civil Engineering Journal 6, no. 2 (2020): 318–25. http://dx.doi.org/10.28991/cej-2020-03091473.

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The objective of this work is to evaluate the physico-chemical quality of the groundwater of the Merdja plain and to determine the sources of mineralization. This quality is influenced by several environmental and anthropogenic factors such as geological context, climate, precipitation and interaction between groundwater and aquifers and human activities. A Principal Component Analysis (PCA) on samples taken from several wells spread over the entire Tebessa plain (Merdja) allowed us to detect two axes that explain 73.4% of the information. The first axis describes the variables related to mine

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Chapman, Steven W., Beth L. Parker, John A. Cherry, Ramon Aravena, and Daniel Hunkeler. "Groundwater–surface water interaction and its role on TCE groundwater plume attenuation." Journal of Contaminant Hydrology 91, no. 3-4 (2007): 203–32. http://dx.doi.org/10.1016/j.jconhyd.2006.10.006.

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Braaten, R., and G. Gates. "Groundwater–surface water interaction in inland New South Wales: a scoping study." Water Science and Technology 48, no. 7 (2003): 215–24. http://dx.doi.org/10.2166/wst.2003.0443.

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Groundwater and surface water have traditionally been managed separately in New South Wales (NSW). However, where rivers and aquifers are hydraulically connected, groundwater pumping has the potential to deplete streamflow. To highlight the major areas of connection in inland NSW, major streams were overlaid with groundwater depth data and the locations of irrigation bores. A consistent pattern was revealed related to basin geomorphology. The main areas of connection are the mid-sections of the major rivers where alluvial systems are well developed yet still narrow and constricted and groundwa

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Bhalaji C K, Deepasri R, Kavimalar K, and Eunice J. "Exploring Surface Water-Groundwater Interactions: A Multidisciplinary Approach." International Research Journal on Advanced Engineering Hub (IRJAEH) 2, no. 04 (2024): 944–51. http://dx.doi.org/10.47392/irjaeh.2024.0132.

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Surface water-ground water interaction plays a crucial role in hydrological systems, influencing water availability, quality and ecosystem sustainability. To maintain drinking water resources and ecosystem health, a mechanistic understanding of the underlying processes controlling the spatial patterns and temporal dynamics of groundwater–surface water interactions is crucial. Understanding these interactions requires a multidisciplinary approach that integrates insights from hydrology, geology, ecology, and geochemistry. Several software applications are available to model and analyze these in

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Qian, Yong, Qinxuan Hou, Chunxiao Wang, et al. "Hydrogeochemical Characteristics and Groundwater Quality in Phreatic and Confined Aquifers of the Hebei Plain, China." Water 15, no. 17 (2023): 3071. http://dx.doi.org/10.3390/w15173071.

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This study aims to investigate hydrogeochemical characteristics and groundwater quality in the Hebei Plain and to discuss factors controlling the groundwater quality. A total of 54 groundwater samples were collected and analyzed for 31 hydrogeochemical parameters, and a fuzzy synthetic evaluation (FSE) method was used for assessing groundwater quality. Results show groundwater total hardness, total dissolved solids (TDS), and major ions excluding K+ in phreatic aquifers higher than that in confined aquifers. From the Piedmont plain to the littoral plain, phreatic aquifers towards the reducing

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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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Li, Xiaomeng, Baizhong Yan, Yuqing Wang, Xinzhou Wang, Yao Li, and Junbai Gai. "Study of the Interaction between Yellow River Water and Groundwater in Henan Province, China." Sustainability 14, no. 14 (2022): 8301. http://dx.doi.org/10.3390/su14148301.

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Determining the interaction between surface water and groundwater is crucial for the protection of groundwater resources. Based on the data of natural geography, geological and hydrogeological conditions, environmental isotopes, and groundwater hydrochemical components, we investigated the interaction between Yellow River water and groundwater in Henan Province, China. The recharge range and interaction amount of the groundwater aquifer from the Yellow River lateral seepage were also analysed, and the influence of the lateral seepage of the Yellow River on groundwater hydrochemical type was st

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Soyaslan, I. I., A. Dogan, and R. Karaguzel. "Modelling of lake—groundwater interaction in Turkey." Proceedings of the Institution of Civil Engineers - Water Management 161, no. 5 (2008): 277–87. http://dx.doi.org/10.1680/wama.2008.161.5.277.

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Evans, Richard, Mike Dudding, and Greg Holland. "River-groundwater interaction: a practical management approach." Australasian Journal of Water Resources 10, no. 2 (2006): 171–78. http://dx.doi.org/10.1080/13241583.2006.11465290.

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Carabin, G., and A. Dassargues. "Modeling groundwater with ocean and river interaction." Water Resources Research 35, no. 8 (1999): 2347–58. http://dx.doi.org/10.1029/1999wr900127.

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Grischek, Thomas, and Chittaranjan Ray. "Bank filtration as managed surface-groundwater interaction." International Journal of Water 5, no. 2 (2009): 125. http://dx.doi.org/10.1504/ijw.2009.028722.

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