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1

Lei, Kunchao, Fengshan Ma, Jiurong Liu, et al. "Leaking recharge mechanism in the multi-layer aquifer system of a typical land subsidence area in Beijing." Proceedings of the International Association of Hydrological Sciences 382 (April 22, 2020): 309–14. http://dx.doi.org/10.5194/piahs-382-309-2020.

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Abstract. It is of great significance to reveal the mechanism of land subsidence to further find out the mechanism of leakage flow in multi-layer aquifer systems and the water-release compression of weak aquifers. In this paper, conditions of groundwater leakage flow are expounded, and the initial hydraulic gradient calculation formula in the aquitards are deduced. The data of Tianzhu Land Subsidence Monitoring Station are selected to preliminarily discuss the leakage flow mechanism of the multi-layer groundwater system and water-release compression of weak aquifers. The results show that, fir
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2

Xu, Guigui, Xiaosi Su, Yiwu Zhang, and Bing You. "Identifying Potential Sites for Artificial Recharge in the Plain Area of the Daqing River Catchment Using GIS-Based Multi-Criteria Analysis." Sustainability 13, no. 7 (2021): 3978. http://dx.doi.org/10.3390/su13073978.

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As an essential component for the development of the Xiong’an New Area, China’s second capital, groundwater in the area has been overexploited, resulting in ecological and environmental geological problems. Therefore, artificial groundwater replenishment measures are urgently required, for which the evaluation of the recharge potential is an important prerequisite. In this study, a GIS (Geographic Information System)-based multi-criteria evaluation system was constructed, considering the source water conditions, recharge infiltration conditions, aquifer storage conditions, and environmental co
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3

Zhao, Jiang, Zhihua Chen, Tao Wang, Caijuan Xiang, Mingming Luo, and Hongxin Yuan. "Control of Contaminant Transport Caused by Open-Air Heavy Metal Slag in Zhehai, Southwest China." International Journal of Environmental Research and Public Health 16, no. 3 (2019): 443. http://dx.doi.org/10.3390/ijerph16030443.

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Slag heaps are formed by mining waste materials, and the improper treatment of leachate from such heaps can threaten nearby aquifers. The Zhehai slag heap in Yunnan Province, China, contains 2.7 million tons of zinc and cadmium slag, and is considered a heavy metal source threatening the local groundwater safety, however, the severity of contamination remains unknown. In this study, numerical modeling was used to predict the groundwater flow and contaminant transport in this area based on field data. The results show that the atmospheric precipitation infiltration recharge at the top of the he
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4

Ye, S., Y. Wang, J. Wu, et al. "Characterization of earth fissures in South Jiangsu, China." Proceedings of the International Association of Hydrological Sciences 372 (November 12, 2015): 249–53. http://dx.doi.org/10.5194/piahs-372-249-2015.

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Abstract. The Suzhou-Wuxi-Changzhou (known as "Su-Xi-Chang") area, located in the southern part of Jiangsu Province, China, experienced serious land subsidence caused by overly exploitation of groundwater. The largest cumulative land subsidence has reached 3 m. With the rapid progress of land subsidence since the late 1980s, more than 20 earth fissures developed in Su-Xi-Chang area, although no pre-existing faults have been detected in the surroundings. The mechanisms of earth fissure generation associated with excessive groundwater pumping are: (i) differential land subsidence, (ii) differenc
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5

Galego Fernandes, Paula, Paula Carreira, and Manuel Oliveira da Silva. "Anthropogenic sources of contamination recognition — Sines coastal aquifer (SW Portugal)." Journal of Geochemical Exploration 98, no. 1-2 (2008): 1–14. http://dx.doi.org/10.1016/j.gexplo.2007.10.003.

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6

De Carlo, Lorenzo, Maria Clementina Caputo, Rita Masciale, Michele Vurro, and Ivan Portoghese. "Monitoring the Drainage Efficiency of Infiltration Trenches in Fractured and Karstified Limestone via Time-Lapse Hydrogeophysical Approach." Water 12, no. 7 (2020): 2009. http://dx.doi.org/10.3390/w12072009.

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In the test site of Castellana Grotte (Southern Italy), since 2016, around 2300 m3d−1 of tertiary treated wastewater has been alternatively spread in nine infiltration trenches, dug into fractured and karstified limestone. In one of these trenches, located upstream, seasonal variations in the infiltration rate were observed, with a lower infiltration rate during summer than in winter. This effect could be due to the occurrence of a bioclogging phenomenon in the warm season. In addition, time-lapse electrical resistivity tomography (ERT) was carried out in two different periods, corresponding t
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7

Bilalov, Bilal, and Fatima Guliyeva. "On the Frame Properties of Degenerate System of Sines." Journal of Function Spaces and Applications 2012 (2012): 1–12. http://dx.doi.org/10.1155/2012/184186.

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8

Erebi, Jonathan Lisa, Samuel Oseji, and Eteh Desmond Rowland. "Investigation of groundwater flow direction using Geospatial technology: A case study in part of Port Harcourt, Rivers State, Nigeria." International Journal of Rural Development, Environment and Health Research 7, no. 2 (2023): 07–16. http://dx.doi.org/10.22161/ijreh.7.2.2.

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A geospatial technique was used in some parts of the Port Harcourt metropolis to establish the direction of groundwater movement. This method included the use of twelve carefully selected boreholes and a variety of cutting-edge tools, such as depth meters, handheld GPS, and measuring tape. The static water level in the boreholes and the ground surface elevation in relation to the average sea level of the region were two of the variables that were gathered. High-end software was used to analyze the data in order to create groundwater flow direction maps and 3D visualizations for displaying the
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9

Pinheiro, L. V., A. H. Gomes, N. Lopes, et al. "NEURAL NETWORKS FOR OPTIMIZATION OF AN EARLY WARNING SYSTEM FOR MOORED SHIPS IN HARBOURS." Coastal Engineering Proceedings, no. 37 (September 1, 2023): 60. http://dx.doi.org/10.9753/icce.v37.papers.60.

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Within the BlueSafePort project, an early warning system (EWS) for moored ships in the port of Sines was developed. In order to improve the reliability and accuracy of the system, two neural networks (NN) were trained, using wave buoys measured datasets. Numerical models results for the wave propagation are adjusted and forecasts are improved. The trained neural networks were able to produce more accurate estimates for the significant wave height and mean wave period, at the buoy location, deployed in front of the Sines Port. The use of the new NN led to an overall reduction of the root mean s
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10

Pinheiro, Liliana Vieira, Andreia H. Gomes, Conceição Juana Fortes, and João Alfredo Santos. "Implementation and Validation of SAFEPORT System at Sines Harbour." Defect and Diffusion Forum 427 (July 14, 2023): 215–26. http://dx.doi.org/10.4028/p-2sbfir.

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SAFEPORT safety system aims to daily reports to the Sines harbor administration, potential emergency situations regarding ships’ operation in port areas caused by extreme weather-oceanographic conditions, that may occur in the next three days. It consists of a set of numerical models and a qualitative risk assessment and forecasting. It uses forecasts provided offshore of the area under the study of sea agitation, wind and tide. The characterization of the response of the free and moored ships at a berth is performed using numerical models which deal with formulations in the frequency and time
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11

Purnama, Setyawan, Suyono Suyono, and Budi Sulaswono. "Sistem Akuifer dan Potensi Airtanah Daerah Aliran Sungai (DAS) Opak." Forum Geografi 21, no. 2 (2016): 111. http://dx.doi.org/10.23917/forgeo.v21i2.2356.

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Opak River Basin is an area with high concentration of settlement. Generally, the settlement use groundwater as a water source. Variation of groundwater condition cause differentiation of water usage in some regions. There are two objectives of this research. First, to determine aquifer system in the research area and second, to calculate the groundwater potential in each aquifer system. To achieve these objectives, aquifer system is determined base on its geology and geomorphology, whereas groundwater potency is calculated by static and dynamic approach. As a result, show that the aquifer sys
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12

Yizhi, Shen, Wei Minrui, and Hou Bowen. "Sustainability assessment and environmental impacts of water supply systems: a case study in Tampa Bay water supply system." E3S Web of Conferences 308 (2021): 01010. http://dx.doi.org/10.1051/e3sconf/202130801010.

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Due to the accelerated industrial and urbanization development, climate change, and increasing populations and life quality expectations, the issue of drinking water shortage has raised much public awareness. The desalination system has been widely applied to accommodate the growing demand for clean water resources despite the continuous concerns about its relatively higher energy consumption and environmental footprints. This research conducted a case study in the Tampa Bay Regional Surface Water Treatment Plant and Tampa Bay Seawater Desalination Plant in Florida, U.S. It analysed the perfor
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13

Shukurov, Aydin Sh. "Comment on “On the Frame Properties of Degenerate System of Sines”." Journal of Function Spaces 2017 (2017): 1–4. http://dx.doi.org/10.1155/2017/9257076.

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The proof of Theorem 3.1 of the paper “On the Frame Properties of Degenerate System of Sines” (see (Bilalov and Guliyeva, 2012)) published earlier in this journal contains a gap; the reasoning given there to prove this theorem is not enough to state the validity of the mentioned theorem. To overcome this shortage we state the most general fact on the completeness of sine system which implies in particular the validity of this fact. It is shown in this note that the system{ω(t)φn(t)}, where{φn(t)}is an exponential or trigonometric (cosine or sine) systems, becomes complete in the corresponding
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14

Kamel, Osman M., and Adel S. Soliman. "A Second Order Secular J–S Planetary Theory Part I : Lemma." Mechanics and Mechanical Engineering 22, no. 4 (2020): 871–74. http://dx.doi.org/10.2478/mme-2018-0067.

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AbstractA concise lemma is given for the construction of a semi – analytic Hamiltonian second order secular J–S planetary theory using the Jacobi – Radau system of origins and in terms of the non-singular variables of H. Poincaré. We truncate our expansions at the desired power in the eccentricities and the sines of the inclinations.
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15

Fernandes, Paula Galego, Paula Carreira, and Manuel Oliveira da Silva. "Identification of Anthropogenic Features Through Application of Principal Component Analysis to Hydrochemical Data from the Sines Coastal Aquifer, SW Portugal." Mathematical Geology 38, no. 6 (2006): 765–80. http://dx.doi.org/10.1007/s11004-006-9040-1.

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16

Sindico, Francesco. "The Guarani Aquifer System and the International Law of Transboundary Aquifers." International Community Law Review 13, no. 3 (2011): 255–72. http://dx.doi.org/10.1163/187197311x585338.

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AbstractArgentina, Brazil, Paraguay and Uruguay signed the Guarani Aquifer Agreement on 2 August 2010. This is the first international treaty regarding the management of a specific transboundary aquifer to have been adopted after the UN International Law Commission (UNILC) adopted the Draft Articles on the Law of Transboundary Aquifers, which have been annexed to UN General Assembly Resolution 63/124. The latter encourages States to take into account the Draft Articles when devising arrangements for the management of specific transboundary aquifers. The Guarani Aquifer Agreement, therefore, is
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17

Chuang, M. H., C. S. Huang, G. H. Li, and H. D. Yeh. "Groundwater fluctuations in heterogeneous coastal leaky aquifer systems." Hydrology and Earth System Sciences Discussions 7, no. 4 (2010): 4473–99. http://dx.doi.org/10.5194/hessd-7-4473-2010.

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Abstract. In the past, the coastal leaky aquifer system, including an unconfined aquifer on the top, a confined aquifer at the bottom, and an aquitard in between, was commonly assumed to be homogeneous and of an infinite extent in the horizontal direction. The leaky aquifer system may however be nonhomogeneous and of a finite extent due to variations in depositional and post depositional processes. Thus, in the paper, the leaky aquifer system is divided into several horizontal regions for simulating the heterogeneity involved in both the confined aquifer and aquitard. A one-dimensional analyti
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18

Udin, Yana, and Wiwit Suryanto. "Identification of Seismic Response to Aquifer System with A Synthetic Modelling Approach." IOP Conference Series: Earth and Environmental Science 1071, no. 1 (2022): 012019. http://dx.doi.org/10.1088/1755-1315/1071/1/012019.

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Abstract The microseismic method is relatively new in groundwater exploration, especially in Indonesia. This study will examine the response of microseismic to groundwater aquifer systems. This study aims to analyze the response of seismic waves and to interpret the seismic wave response characteristics to the aquifer system model. The modeling of the aquifer system was carried out using seismic stratigraphy data. This data was used as input data to model the exposed HVSR curve using the Microtrem program in MATLAB. The study of physical parameters and supporting parameters of the aquifer laye
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19

Karaszewski, Kajetan, and Wiesław Wiktor Jędrzejczak. "Selinexor and Other Selective Inhibitors of Nuclear Export (SINEs)—A Novel Approach to Target Hematologic Malignancies and Solid Tumors." Drugs and Drug Candidates 2, no. 2 (2023): 459–76. http://dx.doi.org/10.3390/ddc2020023.

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Exportin 1 (XPO1) is a crucial molecule of nucleocytoplasmic transport. Among others, it exports molecules important for oncogenesis from the nucleus to the cytoplasm. The expression of XPO1 is increased in numerous malignancies, which contributes to the abnormal localization of tumor suppressor proteins in the cytoplasm and subsequent cell cycle dysregulation. Selective inhibitors of nuclear export (SINEs) are novel anticancer agents that target XPO1, arrest tumor suppressor proteins in the nucleus, and induce apoptosis in cancer cells. Selinexor, a first-in-class SINE, has already been appro
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20

Gan, Yiqun, and Quanrong Wang. "Technical note: A model of chemical transport in a wellbore–aquifer system." Hydrology and Earth System Sciences 28, no. 6 (2024): 1317–23. http://dx.doi.org/10.5194/hess-28-1317-2024.

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Abstract. Wellbore is proven to be the only effective way of delivering chemicals to a target aquifer during a tracer test or aquifer remediation. The volume of original water in the operational well is a critical parameter affecting the concentration of injected tracers or chemicals in the wellbore in the early stages. We found that the calculation of the wellbore water volume by previous numerical methods was correct when the wellbore penetrates an unconfined aquifer but incorrect when the wellbore penetrates a confined aquifer, further resulting in errors in describing the solute transport
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21

Kang, D. H., and J. Li. "3-D land subsidence simulation using the NDIS package for MODFLOW." Proceedings of the International Association of Hydrological Sciences 372 (November 12, 2015): 437–42. http://dx.doi.org/10.5194/piahs-372-437-2015.

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Abstract. The standard subsidence package for MODFLOW, MODFLOW-SUB simulates aquifer-system compaction and subsidence assuming that only 1-D-vertical displacement of the aquifer system occurs in response to applied stresses such as drawdowns accompanying groundwater extraction. In the present paper, 3-D movement of an aquifer system in responses to one or more pumping wells is considered using the new aquifer-system deformation package for MODFLOW, NDIS. The simulation of aquifer- system 3-D movement using NDIS was conducted with a stress or hydraulic head dependent specific storage coefficien
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22

Koreny, John S., and Terry T. Fisk. "Hydraulic conductivity of the Portland Basin deep aquifer system." Environmental and Engineering Geoscience 6, no. 3 (2000): 279–92. http://dx.doi.org/10.2113/gseegeosci.6.3.279.

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Abstract The Portland Basin is 900 mi 2 in size and includes portions of Oregon and Washington. A deep aquifer system of the Troutdale Formation is used for municipal ground-water supply in both states over an area of approximately 300 mi 2 . Although lateral sedimentary facies variations are evident in the lithologic record, data from multi-well aquifer tests show that the aquifer forms a continuous hydrostratigraphic unit in both states. The aquifer is synclinal and in the center of the basin is well-confined by low-permeability layers. On the eastern and western margins of the basin, the aq
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23

Song, Zongzhong, Hailong Li, Qian Ma, Chunmiao Zheng, Jiu Jimmy Jiao, and Shaohong Li. "Analytical Solution of Tidal Loading Effect in a Submarine Leaky Confined Aquifer System." Geofluids 2019 (June 20, 2019): 1–15. http://dx.doi.org/10.1155/2019/8017164.

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Although there are many existing analytical studies of tidal groundwater level fluctuations in coastal aquifer systems, few of them focus on an offshore submarine aquifer. Here, we consider tidal groundwater head fluctuations in a submarine leaky confined aquifer overlain by a semipermeable seabed. Both the seabed and the confined aquifer are assumed to extend horizontally infinitely. A one-dimensional mathematical model is established to describe the problem, and the analytical solution is derived. The impacts of the tidal loading efficiency, hydraulic conductivity and elastic storage of the
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24

Suh, M., H. C. Leung, and R. E. Kettner. "Cerebellar Flocculus and Ventral Paraflocculus Purkinje Cell Activity During Predictive and Visually Driven Pursuit in Monkey." Journal of Neurophysiology 84, no. 4 (2000): 1835–50. http://dx.doi.org/10.1152/jn.2000.84.4.1835.

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Purkinje cells in the flocculus and ventral paraflocculus were studied in tasks designed to distinguish predictive versus visually guided mechanisms of smooth pursuit. A sum-of-sines task allowed studies of complex predictive pursuit. A perturbation task examined visually driven pursuit during unpredictable right-angle changes in target direction. A gap task examined pursuit that was maintained when the target was turned off. Neural activity patterns were quantified using multi-linear models with sensitivities to the position, velocity, and acceleration of both motor output (eye motion) and vi
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25

Zhang, Jun, Zhen Hong Zhao, Hong Yun Ma, Dong Wang, and Li Guo. "Comparison of Groundwater Flow Systems under the Control of Different Aquifer Structures." Advanced Materials Research 610-613 (December 2012): 2688–92. http://dx.doi.org/10.4028/www.scientific.net/amr.610-613.2688.

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The structure of groundwater flow system is the core of study of groundwater system and the base of evaluation of groundwater resources. The control role of aquifer system to groundwater flow system is a key of study of the structure of groundwater flow system. The groundwater systems of the Ordos basin are analyzed as a case study. The control role of aquifer system to groundwater flow system is studied by comparison of groundwater flow systems under the control of different aquifer structures in 2-D profile numerical model. The research shows that the groundwater flow systems of the Ordos ba
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26

Macfarlane, P. Allen. "Revisions to the Nomenclature for Kansas Aquifers." Bulletin (Kansas Geological Survey), no. 244 (December 6, 2000): 1–14. https://doi.org/10.17161/kgsbulletin.no.244.20397.

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The nomenclature for Kansas aquifers needs revision. Many of the names currently in use were derived in an ad hoc manner without the benefit of a consistent set of hydrogeologically based guidelines. Because nomenclature forms the basis of scientific discussion of hydrologic issues, names should be clearly defined and consistently applied in order to prevent erroneous or unintended hydrologic interpretations. The nomenclature revisions presented in this paper are based on the guidelines developed by the U.S. Geological Survey's Water Resources Division (Laney and Davidson, 1986). According to
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27

Ju, Qiding, Youbiao Hu, Kai Chen, and Qimeng Liu. "Hydrogeochemical Processes and Connection of Multi-Layer Groundwater System in Sunan Mining Area, Eastern China." International Journal of Environmental Research and Public Health 19, no. 19 (2022): 12392. http://dx.doi.org/10.3390/ijerph191912392.

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Groundwater is an important freshwater resource in the world and serves as the main source of water for mining areas in Northern China. Coal mining may cause changes in water quality. As such, to identify ways to prevent water contamination, this study investigates the hydrogeochemical processes and transport paths of a complex aquifer system in the Sunan mining area in Northern China. Using the APFS-MLR model, a geographic information system (GIS) spatial analysis, and a hydrochemical correlation analysis method, this study identifies the potential mineral phases in groundwater, the spatial d
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28

Chuang, M. H., C. S. Huang, G. H. Li, and H. D. Yeh. "Groundwater fluctuations in heterogeneous coastal leaky aquifer systems." Hydrology and Earth System Sciences 14, no. 10 (2010): 1819–26. http://dx.doi.org/10.5194/hess-14-1819-2010.

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Abstract. In the past, the coastal leaky aquifer system, including two aquifers and an aquitard between them, was commonly assumed to be homogeneous and of infinite extent in the horizontal direction. The leaky aquifer system may however be heterogeneous and of finite extent due to variations in depositional and post depositional processes. In this paper, the leaky aquifer system is divided into several horizontal regions for the heterogeneous aquitard and underlying aquifer. A one-dimensional analytical model is developed for describing the head fluctuation in such a heterogeneous leaky aquif
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29

Kronfeld, Joel, Israel Carmi, and Dror Avisar. "The Yarkon-Taninim Aquifer (Judea Group Israel): What Radiocarbon Can Tell." Radiocarbon 61, no. 5 (2019): 1377–85. http://dx.doi.org/10.1017/rdc.2019.51.

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ABSTRACTRadiocarbon (14C) conclusively demonstrates that the very important Yarkon-Tanininm aquifer, named after the two springs where the drainage presumably occurs, is in actuality two distinct aquifers—Upper and Lower. The springs have higher 14C activities than the exploitation wells that surround them (all drilled into the Upper aquifer). The springs are situated at faults that allow the Lower aquifer water to rise due to its higher pieziometric head and drain along with the Upper aquifer. The Lower aquifer water flows rapidly along a path that includes a karstic system. The Upper aquifer
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30

Sola, F., A. Vallejos, L. Daniele, and A. Pulido-Bosch. "Identification of a Holocene aquifer–lagoon system using hydrogeochemical data." Quaternary Research 82, no. 1 (2014): 121–31. http://dx.doi.org/10.1016/j.yqres.2014.04.012.

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AbstractThe hydrogeochemical characteristics of the Cabo de Gata coastal aquifer (southeastern Spain) were studied in an attempt to explain the anomalous salinity of its groundwater. This detritic aquifer is characterised by the presence of waters with highly contrasting salinities; in some cases the salinity exceeds that of seawater. Multivariate analysis of water samples indicates two groups of water (G1 and G2). Group G1 is represented in the upper part of the aquifer, where the proportion of seawater varies between 10 and 60%, whilst G2 waters, taken from the lower part of the aquifer, con
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31

Kemper, Karin E., Eduardo Mestre, and Luiz Amore. "Management of the Guarani Aquifer System." Water International 28, no. 2 (2003): 185–200. http://dx.doi.org/10.1080/02508060308691684.

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32

Rahmawati, Novi, Kisworo Rahayu, and Deasy Arisanty. "Potential Evapotranspiration in Merapi Aquifer System." Sustainability (STPP) Theory, Practice and Policy 3, no. 1 (2023): 1–10. http://dx.doi.org/10.30631/sdgs.v1i1.1758.

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Temperature variation due to climate change can give greatest impact on potential evapotranspiration. Increase of temperature in Yogyakarta Special Region can increase potential evapotranspiration. It is necessary to study potential evapotranspiration as one of indication impact of climate change to its potential evapotranspiration. Potential evapotranspiration (PET) can be estimated applying Hargreaves and Samani (1982) that requires limited meteorological parameter. Therefore, this research aims are: a) to analyze daily PET in 3 gauge station of Merapi Aquifer System, b) to analyze variation
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33

Nanni, Arthur Schmidt, Ari Roisenberg, Maria Helena Bezerra Maia de Hollanda, Maria Paula Casagrande Marimon, Antonio Pedro Viero, and Luiz Fernando Scheibe. "Fluoride in the Serra Geral Aquifer System: Source Evaluation Using Stable Isotopes and Principal Component Analysis." Journal of Geological Research 2013 (August 29, 2013): 1–9. http://dx.doi.org/10.1155/2013/309638.

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Groundwater with anomalous fluoride content and water mixture patterns were studied in the fractured Serra Geral Aquifer System, a basaltic to rhyolitic geological unit, using a principal component analysis interpretation of groundwater chemical data from 309 deep wells distributed in the Rio Grande do Sul State, Southern Brazil. A four-component model that explains 81% of the total variance in the Principal Component Analysis is suggested. Six hydrochemical groups were identified. δ18O and δ2H were analyzed in 28 Serra Geral Aquifer System samples in order to identify stable isotopes patterns
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34

Rodríguez, L., L. Vives, and A. Gomez. "Conceptual and numerical modeling of the Guaraní Aquifer System." Hydrology and Earth System Sciences Discussions 9, no. 8 (2012): 9885–930. http://dx.doi.org/10.5194/hessd-9-9885-2012.

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Abstract. In large aquifers relevant for their considerable size, regional groundwater modeling remains challenging given geologic complexity and data scarcity in space and time. The Guaraní Aquifer System is the largest transboundary aquifer in South America. It contains an enormous volume of water, however, it is not well known being difficult to assess the impact of exploitation currently used to supply over 25 million inhabitants. This is a sensitive issue because the aquifer is shared by four countries. Moreover, an integrated groundwater model, and therefore, a global water balance were
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35

Rodríguez, L., L. Vives, and A. Gomez. "Conceptual and numerical modeling approach of the Guarani Aquifer System." Hydrology and Earth System Sciences 17, no. 1 (2013): 295–314. http://dx.doi.org/10.5194/hess-17-295-2013.

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Abstract. In large aquifers, relevant for their considerable size, regional groundwater modeling remains challenging given geologic complexity and data scarcity in space and time. Yet, it may be conjectured that regional scale groundwater flow models can help in understanding the flow system functioning and the relative magnitude of water budget components, which are important for aquifer management. The Guaraní Aquifer System is the largest transboundary aquifer in South America. It contains an enormous volume of water; however, it is not well known, being difficult to assess the impact of ex
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36

Zhang, Baoyun, Junzhi Wang, Ruolin Zhang, Yasong Li, Xiangke Kong, and Yaci Liu. "Estimating Unconfined Aquifer Diffusivity Using 1D Phase Spectral Analysis: A Case Study in the Middle Reach of the Hutuo River, North China Plain." Water 15, no. 16 (2023): 3012. http://dx.doi.org/10.3390/w15163012.

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Aquifer diffusivity is a basic physical parameter used in hydrogeological calculations and is important for the evaluation and rational utilization of water resources, pollution prevention, and wetland protection. In this study, with the assumptions of aquifer isotropy, i.e., no vertical flow and constant saturated aquifer thickness, by using the Fourier transform and convolution theorem, a 1D analytical solution of the phase spectrum for an unconfined aquifer system was derived, which subsequently led to a phase spectrum solution for aquifer diffusivity. To test the efficacy, the proposed met
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37

Santosa, Langgeng Wahyu. "Hidrostratigrafi Akuifer sebagai Geoindikator Genesis Bentuk Lahan di Wilayah Kepesisiran Kabupaten Kulonprogo, Daerah Istimewa Yogyakarta." Forum Geografi 26, no. 2 (2012): 160. http://dx.doi.org/10.23917/forgeo.v26i2.5070.

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Purpose of this research is to study on aquifer hydrostratigraphy that can be a geo-indicator of geomorphological processes on the past, that describe of landform genetic in the research area. The research method is survey. The framework of analysis in this research is landform genetic. The results of the research indicate that: (1) "the forming of aquifer hydrostratigraphy in the research area is controlled by some of main processes in geomorphology, that show of landform genetic specifically". The research area consists of 3 aquifer hydrostratigraphy systems, each of the aquifer system has t
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SA, Sonloye. "Formulation of Generalized Hillslope Leakage-Dependent Model for Groundwater Flow in N-Aquifer System within a Sedimentary Basin." Arid-zone Journal of Basic and Applied Research 4, no. 1 (2024): 1–16. http://dx.doi.org/10.55639/607.494847.

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In this study, the recently derived Hillslope Leakage-dependent (HL-D) models for groundwater flow in leaky three-aquifer system have been generalized to obtain Generalized Hillslope Leakage-dependent, GHL-D equation that model groundwater flow in leaky n-aquifer system. This generalization extends the capability of Hillslope Leakage-dependent (HL-D) equations to modeling groundwater flow in any number of aquifers (n-aquifer system) of all configurations within a sedimentary basin. The formulated GHL-D Model was tested on some aquifer types and the results have shown that it can be used to obt
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Macumber, Phillip G., and Jennifer J. Macumber. "Groundwater flow in the Campaspe and Loddon Valleys of Northern Victoria: an enhanced role for the Shepparton Formation." Proceedings of the Royal Society of Victoria 122, no. 2 (2010): 43. http://dx.doi.org/10.1071/rs10015.

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Recent work on the fluvial aquifer systems of the Campaspe and Loddon Valleys in northern Victoria has shown that a two-aquifer conceptualisation and use of ‘typical’ hydraulic parameters for the Calivil Formation regional aquifer and its notional aquitard the Shepparton Formation, may mask the true nature of their interactions. In the highland tracts of the Loddon and Campaspe Valleys the regional aquifer system comprises the Calivil Formation and much of the Shepparton Formation. On the southern Loddon Plains, intensive groundwater development occurs from both the Calivil Formation and a She
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De Schepper, Guillaume, Pierre-Yves Bolly, Pietro Vizzotto, Hugo Wecxsteen, and Tanguy Robert. "Investigations into the First Operational Aquifer Thermal Energy Storage System in Wallonia (Belgium): What Can Potentially Be Expected?" Geosciences 10, no. 1 (2020): 33. http://dx.doi.org/10.3390/geosciences10010033.

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In the context of energy transition, new and renovated buildings often include heating and/or air conditioning energy-saving technologies based on sustainable energy sources, such as groundwater heat pumps with aquifer thermal energy storage. A new aquifer thermal energy storage system was designed and is under construction in the city of Liège, Belgium, along the Meuse River. This system will be the very first to operate in Wallonia (southern Belgium) and should serve as a reference for future shallow geothermal developments in the region. The targeted alluvial aquifer reservoir was thoroughl
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Maples, Stephen R., Graham E. Fogg, and Reed M. Maxwell. "Modeling managed aquifer recharge processes in a highly heterogeneous, semi-confined aquifer system." Hydrogeology Journal 27, no. 8 (2019): 2869–88. http://dx.doi.org/10.1007/s10040-019-02033-9.

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Abstract Widespread groundwater overdraft in alluvial aquifer systems like the Central Valley (CV) in California, USA, has increased interest in managed aquifer recharge (MAR). Like most clastic sedimentary basins, recharge to the productive semi-confined CV aquifer system remains a challenge due to the presence of nearly ubiquitous, multiple confining units (silt and clay) that limit recharge pathways. Previous studies suggest the presence of interconnected networks of coarse-texture sand and gravel deposits that bypass regional confining units over a small fraction of the CV near the America
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Höyng, Dominik, Fernando Mazo D’Affonseca, Peter Bayer, et al. "High-resolution aquifer analog of fluvial–aeolian sediments of the Guarani aquifer system." Environmental Earth Sciences 71, no. 7 (2013): 3081–94. http://dx.doi.org/10.1007/s12665-013-2684-5.

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Halford, Keith J. "Effects of Unsaturated Zone on Aquifer Test Analysis in a Shallow-Aquifer System." Ground Water 35, no. 3 (1997): 512–22. http://dx.doi.org/10.1111/j.1745-6584.1997.tb00112.x.

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Merzougui, Touhami, Abderezak Bouanani, Cherif Rezzoug, Abedrehmene Mekkaoui, Fadoua A. Hamzaoui, and Fatima Z. Merzougui. "Palm grove groundwater assessment and hydrodynamic modelling Case study: Beni Abbes, South-West of Algeria." Journal of Water and Land Development 43, no. 1 (2019): 133–43. http://dx.doi.org/10.2478/jwld-2019-0071.

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AbstractThis paper presents the groundwater modelling of Beni Abbes palm grove in Southwest Algeria. Beni Abbes oasis alluvial aquifer is part of the Saoura Valley aquifer system, including a loose slick contained in a Quaternary alluvial embankment that fills the Beni Abbes basin. To address local needs, industry and agriculture, groundwater has been intensively exploited in recent years. Groundwater of the Beni Abbes oasis in the Saoura Valley oasis chain, is composed of a complex system, whose layer of alluvial terraces ensures a vital role for a 40-hectare palm grove. Due to its architectu
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Lei, Jun Qin, Xiu Qing Zheng, and Hong Fei Zang. "The Effect of Coal Mining on the Multi-Aquifer System." Advanced Materials Research 919-921 (April 2014): 1252–56. http://dx.doi.org/10.4028/www.scientific.net/amr.919-921.1252.

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Based on the analysis of the regional geological and hydrogeologic conditions of a coal mine in Xishan Coalfield, Shanxi Province in China, the groundwater aquifer system is generalized as a three layers structure in vertical direction and a three-dimensional unsteady flow model in confined aquifer is established. The regime of karst groundwater levels under the coal mining conditions for both Carboniferous and Ordovician limestone aquifers are predicted by using Visual Modflow. The results show that the groundwater levels of the two aquifers are all in decline as a result of coal mining. Afte
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Islam, Md Tariqul, and ASM Woobaidullah. "Surface Resistivity Sounding and Borehole Data Analysis for the Evaluation of Aquifer Characteristics of Southern Districts Barguna and Patuakhali, Bangladesh." Dhaka University Journal of Earth and Environmental Sciences 8, no. 1 (2020): 11–18. http://dx.doi.org/10.3329/dujees.v8i1.50755.

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The study delineates the aquifer system of the study area and determines the extension of potential fresh water aquifer and suitable locations for groundwater development through geophysical electrical resistivity method. Vertical electrical sounding with Schlumberger electrode configuration, a method for surface resistivity measurement, has been used for data collection. Resistivity data along with borelog data analyses are used for this investigation. Lithological cross section analyses show that sand and clay dominated lithology with frequent facies changes occur throughout the area and als
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Ben Saad, Eya, Mohsen Ben Alaya, Jean-Denis Taupin, Nicolas Patris, Najet Chaabane, and Radhia Souissi. "A Hydrogeological Conceptual Model Refines the Behavior of a Mediterranean Coastal Aquifer System: A Key to Sustainable Groundwater Management (Grombalia, NE Tunisia)." Hydrology 10, no. 9 (2023): 180. http://dx.doi.org/10.3390/hydrology10090180.

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The Mediterranean coastal aquifer system of the Grombalia basin (NE Tunisia) offers immense potential as a source of fresh water for agriculture, industry, and drinking water supply. Nonetheless, due to its intricate hydrogeological characteristics and the prevailing issue of groundwater salinity, comprehending its groundwater system behavior becomes crucial for the effective and sustainable management of this aquifer system. Based on the hydrogeological characterization of the Grombalia basin, a novel 3D hydrogeological conceptual model was developed to enhance the understanding of its comple
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ALLIA, Zineb. "The Mio-pliocene aquifer system of the South Auresian Trough, Low Septentrional Sahara, Algeria: aquifer geometry and groundwater characterization." International Journal of Sciences and Natural Ressources 1, no. 2 (2022): 6–14. http://dx.doi.org/10.58205/ijsnr.v1i2.251.

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In the South auresian trough, Low Septentrional Sahara, Algeria, the sands aquifer is contained in the Mio-pliocene deposits in which several sedimentary sets have identified and contain two independent aquifer levels. Their relationship is determined by data correlation of several cross-sections surveyed on outcrops and boreholes that permit us a 2D construction of the multi-layer aquifer formations and to specify its geometry. The latter shows an asymmetrical synclinal structure with greater depth to the south and an unconformity of the upper unit (upper aquifer) on the base unit (lower aqui
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Saleena, N. Vahid, Kumar R.B. Binoj, E. Shaji, and Jacob Noble. "Hydrochemical characteristics and groundwater assessment of a multi-aquifer system in Alappuzha area, South India." Journal of Geointerface 4, no. 1 (2025): 104–24. https://doi.org/10.5281/zenodo.15586855.

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A hydrogeochemical investigation was carried out in a multi-aquifer in the Alappuzha area, Kerala, South India. Quality assessment of groundwater for both drinking and irrigation purposes was carried out to understand its hydrogeochemical evo-lution. Quaternary alluvium (phreatic aquifer) and Tertiary sediments (confined aquifer) forms the major aquifer system in this area. The topmost Tertiary aquifer namely, the Warkalli aquifer is extensively developed through tube wells. For the present study, 74 water samples were collected from dug wells, tube wells, and surface water bodies, during June
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Wilske, Cornelia, Axel Suckow, Ulf Mallast, et al. "A multi-environmental tracer study to determine groundwater residence times and recharge in a structurally complex multi-aquifer system." Hydrology and Earth System Sciences 24, no. 1 (2020): 249–67. http://dx.doi.org/10.5194/hess-24-249-2020.

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Abstract. Despite being the main drinking water resource for over 5 million people, the water balance of the Eastern Mountain Aquifer system on the western side of the Dead Sea is poorly understood. The regional aquifer consists of fractured and karstified limestone – aquifers of Cretaceous age, and it can be separated into a Cenomanian aquifer (upper aquifer) and Albian aquifer (lower aquifer). Both aquifers are exposed along the mountain ridge around Jerusalem, which is the main recharge area. From here, the recharged groundwater flows in a highly karstified aquifer system towards the east a
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