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Статті в журналах з теми "Groundwater contribution"
Lam, A., D. Karssenberg, B. J. J. M. van den Hurk, and M. F. P. Bierkens. "Spatial and temporal connections in groundwater contribution to evaporation." Hydrology and Earth System Sciences Discussions 8, no. 1 (February 1, 2011): 1541–68. http://dx.doi.org/10.5194/hessd-8-1541-2011.
Повний текст джерелаBidwell, V. J., R. Stenger, and G. F. Barkle. "Dynamic analysis of groundwater discharge and partial-area contribution to Pukemanga Stream, New Zealand." Hydrology and Earth System Sciences Discussions 4, no. 4 (July 30, 2007): 2461–96. http://dx.doi.org/10.5194/hessd-4-2461-2007.
Повний текст джерелаBidwell, V. J., R. Stenger, and G. F. Barkle. "Dynamic analysis of groundwater discharge and partial-area contribution to Pukemanga Stream, New Zealand." Hydrology and Earth System Sciences 12, no. 4 (July 28, 2008): 975–87. http://dx.doi.org/10.5194/hess-12-975-2008.
Повний текст джерелаZhu, Yonghua, Liliang Ren, Robert Horton, Haishen Lü, Xi Chen, Yangwen Jia, Zhenlong Wang, and E. A. Sudicky. "Estimating the contribution of groundwater to rootzone soil moisture." Hydrology Research 44, no. 6 (January 16, 2013): 1102–13. http://dx.doi.org/10.2166/nh.2013.071.
Повний текст джерелаLam, A., D. Karssenberg, B. J. J. M. van den Hurk, and M. F. P. Bierkens. "Spatial and temporal connections in groundwater contribution to evaporation." Hydrology and Earth System Sciences 15, no. 8 (August 24, 2011): 2621–30. http://dx.doi.org/10.5194/hess-15-2621-2011.
Повний текст джерелаAbbas, Haider, and Ramanathan Sri Ranjan. "Groundwater contribution to irrigated potato production in the Canadian Prairies." Canadian Biosystems Engineering 57, no. 1 (August 10, 2015): 1.13–1.24. http://dx.doi.org/10.7451/cbe.2015.57.1.13.
Повний текст джерелаFan, Y., and G. Miguez-Macho. "Potential groundwater contribution to Amazon evapotranspiration." Hydrology and Earth System Sciences Discussions 7, no. 4 (July 30, 2010): 5131–70. http://dx.doi.org/10.5194/hessd-7-5131-2010.
Повний текст джерелаFan, Y., and G. Miguez-Macho. "Potential groundwater contribution to Amazon evapotranspiration." Hydrology and Earth System Sciences 14, no. 10 (October 25, 2010): 2039–56. http://dx.doi.org/10.5194/hess-14-2039-2010.
Повний текст джерелаMustafa, Syed M. Touhidul, M. Moudud Hasan, Ajoy Kumar Saha, Rahena Parvin Rannu, Els Van Uytven, Patrick Willems, and Marijke Huysmans. "Multi-model approach to quantify groundwater-level prediction uncertainty using an ensemble of global climate models and multiple abstraction scenarios." Hydrology and Earth System Sciences 23, no. 5 (May 13, 2019): 2279–303. http://dx.doi.org/10.5194/hess-23-2279-2019.
Повний текст джерелаListyani, T., and I. A. Prabowo. "Groundwater in Bener area, its quality and contribution for agriculture." IOP Conference Series: Earth and Environmental Science 985, no. 1 (February 1, 2022): 012028. http://dx.doi.org/10.1088/1755-1315/985/1/012028.
Повний текст джерелаДисертації з теми "Groundwater contribution"
Pacheco, Adriana. "Contribution of methanotrophic groundwater and rhizosphere bacteria to phytoremediation." [Gainesville, Fla.] : University of Florida, 2006. http://purl.fcla.edu/fcla/etd/UFE0013836.
Повний текст джерелаBurkett, Danny, and danny burkett@deakin edu au. "Nutrient contribution to hyper-eutrophic wetlands in Perth, Western Australia." Deakin University. School of Life and Environmental Sciences, 2005. http://tux.lib.deakin.edu.au./adt-VDU/public/adt-VDU20071115.082506.
Повний текст джерелаChatton, Eliot. "Contribution of dissolved gases to the understanding of groundwater hydrobiogeochemical dynamics." Thesis, Rennes 1, 2017. http://www.theses.fr/2017REN1S131/document.
Повний текст джерелаFor more than a century, global change has led to a profound modification of our societies, our lifestyles and, of course, our environment. This trajectory followed willy-nilly by all mankind has consequences for natural systems and already seems to lead the future generations ahead of serious challenges. In order not to compromise our ability to meet these future ordeals, and because of the urgent need for action, part of the scientific community has chosen to concentrate on the near-surface environment that supports terrestrial life: the Critical Zone. The emergence of this concept underlines the need to develop multidisciplinary scientific approaches integrating a wide variety of temporal and spatial scales. As the link between the different compartments of the Critical Zone (Atmosphere, Biosphere, Hydrosphere, Lithosphere and Pedosphere), water is an essential molecule controlling the exchanges of energy and matter whose dynamics require special attention. In view of the diversity and spatiotemporal variability of water and matter transfers arising in aquatic environments, new methods of investigation are needed. The general objective of this thesis is to describe the interest and the potential lying in the use of dissolved gases, especially when they are measured at high frequency in the field, in order to characterise the hydrobiogeochemical dynamics of the natural waters of the Critical Zone at different spatial and temporal scales. To perfect this ambition, this work focused first on the development of an innovative instrumentation, then, on the implementation of novel tracers integrated into original experimental setups and finally, on the acquisition, processing and analysis of different dissolved gas datasets focusing on groundwater
Liuzzo, Scorpo Alberto. "Heat transfer in borehole heat exchangers and the contribution of groundwater flow." Doctoral thesis, Università degli studi di Trieste, 2014. http://hdl.handle.net/10077/10123.
Повний текст джерелаThe exploitation of geothermal heat by ground source heat pumps is presently growing throughout Europe and the world. In Italy, at the end of 2010, borehole heat exchangers covered most of the 30% of the total energy used for space conditioning, showing an increase of 50%compared to 2005. The forecasts for 2015 suggest a further increase in the direct uses of the geothermal heat exceeding 50% compared to 2010 and a corresponding increase in the geothermal energy consumption. The possibility to design plants with higher efficiency and lower costs of installation and operation is required, to support the growth of the ground source heat pump systems and the consequent diffusion of the exploitation of the geothermal resources. Research and better knowledge of the processes involved in the heat transfer between the borehole heat exchanger and the surrounding ground is crucial to predict the behavior of the plant-geothermal source interaction in any possible operational condition. The knowledge of the hydrogeological characteristics of the specific site where the plant has to be installed is also essential to prevent over- or under-sizing of the heat exchanger(s) due to a rough design. Over the years, several analytical solutions have been proposed to calculate the temperature distribution around a borehole heat exchanger during operation. The infinite line source analytical model considers an infinite linear heat source which exchanges heat with the surrounding ground by conduction only. Other models, based on the infinite linear heat source, have been later developed, considering also the contribution to the conductive heat transfer due to groundwater flow. The presence of flowing water around a borehole heat exchanger implies forced convection, resulting in an increased efficiency of the heat transfer between the ground and the borehole heat exchanger. Studying this process may suggest new ways to improve the efficiency and to reduce the cost of ground source heat pump systems. In this thesis, the contribution of groundwater flow in the heat transfer process between borehole heat exchangers and surrounding ground has been investigated, in order to increase the theoretical knowledge as well as to improve the existing design tools. Two-dimensional models have been considered, taking into account the actual cylindrical geometry of the borehole. The groundwater flow has been modeled as steady, horizontal and with variable flow rates, in order to encompass most of the real ground source heat pump applications. Gravitational effects, i.e. the effects of a possible natural convection, have been neglected. The results suggest that in the considered range of Darcy number, the calculation of the heat transfer efficiency is not affected if Darcynian model is used to describe the velocity field, although the viscous effects, and consequently the formation of the hydraulic boundary layer, are neglected. Calculations made using numerical simulations are compared with an analytical solution which takes into account forced convection due to groundwater flow and based on the linear heat source model. The regions of space and time where this analytical solution is affected by the effects of the line source assumption, in both cases of single- and multiple-borehole(s) systems, have been defined. The potential of the thermal response test analysis as a tool to predict the spacing between boreholes when groundwater flow occurs has been investigated, defining and studying the Influence Length as function of groundwater flow rate. The results suggest that even relatively low flow rates allow to reduce significantly the spacing between boreholes in the perpendicular direction with respect to groundwater flow. The distance from the borehole where the temperature disturbance becomes not-significant (Influence Length) is roughly predictable by thermal response test analysis. The study of the Influence Length may be a useful tool in the design of dissipative multiple-boreholes systems, as well as in areas with a high density of single-borehole plants, to reduce the spacing avoiding thermal interferences. Moreover, an expeditious, graphical method to estimate the hydraulic conductivity of the ground by thermal response test analysis has been proposed. An example of application of the methodology is presented, taking into account experimental data as well as plausible hydrological and petrological assumptions when the data are unavailable. The obtained result is in agreement with the hydraulic conductivity range reported in literature for the type of substrate considered in the example. In order to verify this method, further inv1estigations and developments are required. In fact, the graphs used in the procedure presented in this work are referred to specific borehole conditions (borehole filled by groundwater) and are based on two-dimensional models (i.e. end-effects and natural convection are neglected). Besides, the assumptions required to compensate the unavailable data imply that the method cannot be considered verified. Finally, further studies are suggested in order to improve and develop the proposed methods.
Negli ultimi anni, l’utilizzo del calore geotermico tramite pompe di calore accoppiate al terreno sta aumentando significativamente in tutta Europa e in generale nel mondo. In Italia, alla fine del 2010, le sonde geotermiche coprivano più del 30% dell’energia totale utilizzata per riscaldamento e raffrescamento degli edifici, mostrando un aumento del 50% rispetto al 2005. Le previsioni per il 2015 suggeriscono un ulteriore aumento degli utilizzi diretti del calore geotermico maggiore del 50% rispetto al 2010 e un analogo incremento del consumo di energia geotermica in generale. Con l’aumento della diffusione di questa tecnologia, e quindi un maggior sfruttamento di tale risorsa, aumenta anche la necessità di progettare impianti con la massima efficienza possibile e con bassi costi di installazione ed esercizio. La comprensione dei processi coinvolti nel trasferimento di calore tra sonda geotermica e terreno circostante è fondamentale per prevedere il comportamento degli impianti. Anche la conoscenza delle caratteristiche idrogeologiche del sito specifico nel quale l’impianto deve essere installato è essenziale al fine di evitare un’errata progettazione che può causare sovra- o sotto-dimensionamento della sonda. Nel corso degli anni, diverse soluzioni analitiche sono state proposte per calcolare la distribuzione di temperatura attorno alla sonda geotermica durante il suo utilizzo. Il modello analitico della sorgente di calore lineare e infinita considera lo scambio di calore che avviene per sola conduzione attorno ad una sorgente di raggio infinitesimo e di lunghezza infinita. Altri modelli successivi a questo e anch’essi basati sulla sorgente di calore lineare ed infinita, tengono conto anche del contributo convettivo dovuto al flusso dell’acqua di falda. La presenza di un flusso di acqua attorno ad una sonda geotermica, infatti, comporta convezione forzata e, di conseguenza, un aumento dello scambio di calore tra sonda e terreno. Per questo motivo, lo studio degli effetti di tale processo è un fattore chiave per riuscire a migliorare l’efficienza degli scambiatori di calore accoppiati al terreno. Questa tesi presenta lo studio del contributo del flusso delle acque di falda sul processodi scambio termico tra sonde geotermiche e terreno circostante, al fine di incrementare la conoscenza teorica e migliorare gli strumenti di progettazione già esistenti. Per raggiungere questo scopo ci si è serviti di modelli numerici bi-dimensionali che tengono conto della reale geometria cilindrica della sonda. Il fusso delle acque di falda è stato assunto come stazionale e orizzontale. Al fine di includere la maggior parte delle applicazioni geotermiche reali, un vasto range di portate è stato preso in considerazione. Gli effetti gravitativi, e quindi i possibili effetti di convezione naturale, sono stati invece trascurati. Sono stati confrontati i risultati del calcolo del trasferimento di calore ottenuti utilizzando rispettivamente l’equazione di Darcy e l’equazione di Darcy-Brinkman per descrivere il campo di velocità dell’acqua di falda attorno alla sonda. Le conclusioni raggiunte suggeriscono che utilizzando il modello di Darcy, il risultato risulta comunque sufficientemente accurato per i numeri di Darcy considerati, nonostante gli effetti viscosi, e quindi la formazione dello strato-limite fluidodinamico, vengano trascurati. I risultati delle simulazioni numeriche sono stati comparati con un modello analitico che prevede convezione forzata, dovuta al flusso di falda, attorno ad una sorgente di calore lineare ed infinita. Sono quindi state definite le regioni dello spazio e del tempo dove tale soluzione analitica è soggetta agli effetti della linearit`a della sorgente, sia nel caso di sonda singola, sia nel caso di campo-sonde. Sono inoltre state studiate le potenzialità dell’analisi del test di risposta termica come strumento per prevedere la spaziatura tra le sonde in funzione della portata del flusso dell’acqua di falda. I risultati suggeriscono che portate relativamente modeste, permettono una riduzione significativa della spazitura tra le sonde in direzione perpendicolare rispetto a quella di scorrimento dell’acqua di falda. Sfruttando l’analisi del test di risposta termica, è possibile stimare approssimativamente la distanza dalla sonda alla quale il disturbo di temperatura diventa trascurabile (distanza di influenza). Lo studio di questa distanza di influenza pu`o essere un utile strumento per la progettazione di sistemi dissipativi composti da sonde multiple, così come nelle aree con un’alta densità di impianti a sonda singola, al fine di ridurre la spaziatura tra le sonde, evitando allo stesso tempo l’insorgere di interferenze termiche tra sonde adiacenti. Inoltre è stato proposto un metodo grafico e speditivo per la stima della conducibilità idraulica del substrato tramite l’analisi del test di risposta termica. È stato presentato un esempio dell’applicazione di questa metodologia utilizzando sia dati sperimentali sia assunzioni plausibili di carattere idrologico e petrologico, quando non è stato possibile avvalersi di dati sperimentali. I risultati ottenuti sono in accordo con i valori di conducibilità idraulica proposti in letteratura per il tipo di substrato dell’esempio. Per poter verificare l’affidabilità di questo metodo, ulteriori studi e sviluppi sono sono necessari. Infatti, i grafici utilizzati nella procedura presentata in questa tesi, si riferiscono a specifiche condizioni della sonda (acqua di falda come materiale di riempimento) e sono inoltre basati su modelli bi-dimensionali (trascurando quindi gli effetti di fine-pozzo e il contributo della convezione naturale). Infine vengono forniti suggerimenti riguardo ulteriori studi che consentirebbero di migliorare e sviluppare ulteriormente le metodologie proposte.
XXVI Ciclo
1985
Lapp, Anthony. "Seasonal Variability of Groundwater Contribution to Watershed Discharge in Discontinuous Permafrost in the North Klondike River Valley, Yukon." Thesis, Université d'Ottawa / University of Ottawa, 2015. http://hdl.handle.net/10393/32298.
Повний текст джерелаBushman, Michelle. "Contribution of Recharge Along Regional Flow Paths to Discharge at Ash Meadows, Nevada." Diss., CLICK HERE for online access, 2008. http://contentdm.lib.byu.edu/ETD/image/etd2386.pdf.
Повний текст джерелаBarquin, Valle Luis Pablo. "Modeling shallow groundwater table contribution to soil water retention in the unsaturated zone of a calcareous soil of south Florida." [Gainesville, Fla.] : University of Florida, 2009. http://purl.fcla.edu/fcla/etd/UFE0025060.
Повний текст джерелаSmidt, Geerd Ahlrich [Verfasser]. "Mobility of fertiliser-derived uranium in arable soils and its contribution to uranium concentrations in groundwater and tap water / Geerd Ahlrich Smidt." Bremen : IRC-Library, Information Resource Center der Jacobs University Bremen, 2013. http://d-nb.info/1035267578/34.
Повний текст джерелаGarnier, Frédéric. "Contribution à l’évaluation biogéochimique des impacts liés à l’exploitation géothermique des aquifères superficiels : expérimentations et simulations à l’échelle d’un pilote et d’installations réelles." Thesis, Orléans, 2012. http://www.theses.fr/2012ORLE2079/document.
Повний текст джерелаThe use of shallow groundwater as heat source for heat pump is very coveted for air-conditioning of building or industrial facilities. Their intensive use during many years combined with the redeployment of the geothermal industry these last years, raise concerns about the safeguarding of the water resources. In such a context, the present study aims to evaluate the impact of local variations of temperature on the physicochemical and microbiological quality of groundwater systems on the basis of (I) field investigation and, (II) experiments on a pilot (named BIOTHERMEX) making it possible to reproduce, in perfectly supervised conditions, the effect of the propagation of a thermal plume in a reduced aquifer model. Within the temperature recorded on site, principal outcomes showed that thermal impacts are confined in the immediate vicinity of the installation, and were able to deteriorate, up to about ten degrees, the stenothermy of the groundwater systems. The evolution of the physicochemical parameters did not reveal any significant disturbances over the monitoring period, this being also predicted by hydrogeochemical modeling. On the other hand, a significant influence was raised about some microbiological indicators-descriptors (namely activity, diversity of the total microflora). Lastly, the experiments undertaken on the laboratory scale made it possible to finely apprehend the reactional behavior of the system and to define a critical temperature of re-injection beyond which, potential disorders are expected
Satchithanantham, Sanjayan. "Water management effects on potato production and the environment." American Society of Agricultural and Biological Engineers (ASABE), 2012. http://hdl.handle.net/1993/22279.
Повний текст джерелаКниги з теми "Groundwater contribution"
Gingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 1999.
Знайти повний текст джерелаGingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.
Знайти повний текст джерелаGingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.
Знайти повний текст джерелаGingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 1999.
Знайти повний текст джерелаGingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.
Знайти повний текст джерелаGingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 1999.
Знайти повний текст джерелаGingerich, Stephen B. Ground-water occurrence and contribution to streamflow, northeast Maui, Hawaii. Honolulu, Hawaii: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.
Знайти повний текст джерелаWarner, James W. Ground-water contribution to the salinity of the Upper Colorado River Basin. Lakewood, Colo: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаWarner, James W. Ground-water contribution to the salinity of the Upper Colorado River Basin. Lakewood, Colo: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаWarner, James W. Ground-water contribution to the salinity of the Upper Colorado River Basin. Lakewood, Colo: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаЧастини книг з теми "Groundwater contribution"
Seward, P., Y. Xu, and A. Turton. "Using backcasting to explore ways to improve the national water department's contribution to good groundwater governance in South Africa." In Groundwater, 42–58. London: Routledge, 2023. http://dx.doi.org/10.4324/9781003345862-5.
Повний текст джерелаMujere, N. "Contribution of groundwater towards urban household water security." In Groundwater for Sustainable Livelihoods and Equitable Growth, 95–99. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003024101-5.
Повний текст джерелаSherif, Mohsen, Abdel Azim Ebraheem, Ampar Shetty, Ahmed Sefelnasr, Khaled Alghafli, and Mohamed Al Asam. "Evaluation of the Effect of the Wadi Bih Dam on Groundwater Recharge, UAE." In Natural Disaster Science and Mitigation Engineering: DPRI reports, 509–27. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-2904-4_21.
Повний текст джерелаChandrakanth, M. G. "Supply-Side Economic Contribution of Watershed Programme to Groundwater Recharge." In Water Resource Economics, 139–48. New Delhi: Springer India, 2015. http://dx.doi.org/10.1007/978-81-322-2479-2_10.
Повний текст джерелаYamada, Chusei. "Comment: The ILC’s Contribution to the Peaceful Sharing of Transboundary Groundwater." In Peace through International Law, 173–75. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03380-3_15.
Повний текст джерелаBourhane, Anli, Jean-Christophe Comte, Jean-Lambert Join, and Kassim Ibrahim. "Groundwater Prospection in Grande Comore Island—Joint Contribution of Geophysical Methods, Hydrogeological Time-Series Analysis and Groundwater Modelling." In Active Volcanoes of the Southwest Indian Ocean, 385–401. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-31395-0_24.
Повний текст джерелаAlmeida, Alexandre M., Paula M. Carreira, José Manuel Marques, Jorge Espinha Marques, Marina Paiva, Alexandra Carvalho, and Catarina Mansilha. "Groundwater Contribution to Alpine Ponds Recharge in Serra Da Estrela Natural Park, Portugal." In Advances in Geoethics and Groundwater Management : Theory and Practice for a Sustainable Development, 157–61. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-59320-9_34.
Повний текст джерелаMatz-Lück, Nele. "The Benefits of Positivism: The ILC’s Contribution to the Peaceful Sharing of Transboundary Groundwater." In Peace through International Law, 125–50. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03380-3_12.
Повний текст джерелаAbiy, Anteneh Z., Solomon S. Demissie, Charlotte MacAlister, Shimelis B. Dessu, and Assefa M. Melesse. "Groundwater Recharge and Contribution to the Tana Sub-basin, Upper Blue Nile Basin, Ethiopia." In Springer Geography, 463–81. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-18787-7_22.
Повний текст джерелаAsfaw, Daniel, Getachew Workineh Gella, and Mulualem Asfaw. "Modeling Landscape Dynamics, Erosion Risk, and Annual Sediment Yield in Guna-tana Watershed: A Contribution for Microwatershed Level Conservation Priority Area Identification." In Groundwater Resources Development and Planning in the Semi-Arid Region, 73–91. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-68124-1_4.
Повний текст джерелаТези доповідей конференцій з теми "Groundwater contribution"
Ramdhan, A., A. Arifin, and R. Suwarman. "Assessing Groundwater-Citarum River Interaction and Groundwater Contribution to Flooding." In NSG2021 27th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202120067.
Повний текст джерелаM. Gabr, A. "Non Seismic - Contribution to Groundwater Investigation, Case Studies, UAE and Egypt." In EAGE Workshop on Non-Seismic Methods. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609.201402599.
Повний текст джерелаRusso, Aeon, Jordan Jenckes, David Boutt, and LeeAnn Munk. "CONTRIBUTION OF FRESH SUBMARINE GROUNDWATER DISCHARGE TO THE GULF OF ALASKA." In Northeastern Section-56th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021ne-361932.
Повний текст джерелаIgel, J., T. Gunther, H. Sulzbacher, H. Wiederhold, and M. Kuntzer. "GPR investigations of an island aquifer as a contribution to groundwater modelling." In 2012 14th International Conference on Ground Penetrating Radar (GPR). IEEE, 2012. http://dx.doi.org/10.1109/icgpr.2012.6254960.
Повний текст джерелаWelch, Eric M. "GROUNDWATER CONTRIBUTION TO GLYPHOSATE CONCENTRATIONS IN THE FAGA`ALU STREAM, AMERICAN SAMOA." In 113th Annual GSA Cordilleran Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017cd-292458.
Повний текст джерелаYamamoto, Yuhei, Daisuke Aosai, and Takashi Mizuno. "Evaluation of Behavior of Rare Earth Elements Based on Determination of Chemical State in Groundwater in Granite." In ASME 2010 13th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2010. http://dx.doi.org/10.1115/icem2010-40072.
Повний текст джерелаBarnes, Austin, Shellie Habel, Kian Bagheri, Yousef Sangsefidi, Hassan Tavakol-Davani, and Mark Merrifield. "INVESTIGATING CONTRIBUTION OF SEA LEVEL INDUCED GROUNDWATER SHOALING TO URBAN FLOODING IN IMPERIAL BEACH, CALIFORNIA." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383928.
Повний текст джерелаMaillol, J. M., J. Ortega‐Ramírez, W. L. Bandy, and A. Valiente‐Banuet. "Contribution of Electrical Resistivity Methods to Paleoenvironmental Reconstruction and Groundwater Exploration in the Chihuahua Desert, Mexico." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2000. Environment and Engineering Geophysical Society, 2000. http://dx.doi.org/10.4133/1.2922710.
Повний текст джерелаRoy, J., M. W. Lubczynski, R. J. Sporry, and W. A. Hugens. "Contribution from EM surveys to a regional groundwater resource quantification project in a hard rock area." In 3rd EEGS Meeting. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609.201407314.
Повний текст джерелаMaillol, J. M., J. Ortega-Ramirez, W. L. Bandy, and A. Valiente-Banuet. "Contribution Of Electrical Resistivity Methods To Paleoenvironmental Reconstruction And Groundwater Exploration In The Chihuahua Desert, Mexico." In 13th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609-pdb.200.2000_121.
Повний текст джерелаЗвіти організацій з теми "Groundwater contribution"
Bunce, Lauren, Tim Lowenstein, and Elliot Jagniecki. Spring, River, and Lake Water Analyses from the Great Salt Lake Basin, Northern Utah. Utah Geological Survey, September 2022. http://dx.doi.org/10.34191/ofr-745.
Повний текст джерелаChefetz, Benny, and Jon Chorover. Sorption and Mobility of Pharmaceutical Compounds in Soils Irrigated with Treated Wastewater. United States Department of Agriculture, 2006. http://dx.doi.org/10.32747/2006.7592117.bard.
Повний текст джерелаChefetz, Benny, and Jon Chorover. Sorption and Mobility of Pharmaceutical Compounds in Soils Irrigated with Treated Wastewater. United States Department of Agriculture, 2006. http://dx.doi.org/10.32747/2006.7709883.bard.
Повний текст джерелаBécu, V., A.-A. Sappin, and S. Larmagnat. User-friendly toolkits for geoscientists: how to bring geology experts to the public. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331220.
Повний текст джерелаLacerda Silva, P., G. R. Chalmers, A. M. M. Bustin, and R. M. Bustin. Gas geochemistry and the origins of H2S in the Montney Formation. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329794.
Повний текст джерелаLooney, B., C. Eddy-Dilek, M. Amidon, J. Rossabi, and L. Stewart. INDEPENDENT TECHNICAL REVIEW OF THE FOCUSED FEASIBILITY STUDY AND PROPOSED PLAN FOR DESIGNATED SOLID WASTE MANAGEMENT UNITS CONTRIBUTING TO THE SOUTHWEST GROUNDWATER PLUME AT THE PADUCAH GASEOUS DIFFUSION PLANT. Office of Scientific and Technical Information (OSTI), May 2011. http://dx.doi.org/10.2172/1017433.
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