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Статті в журналах з теми "Hydrological tracing"
K�ss, W. A. "Hydrological tracing practice on underground contaminations." Environmental Geology 23, no. 1 (February 1994): 23–29. http://dx.doi.org/10.1007/bf00773135.
Повний текст джерелаKAGABU, Makoto. "Tracing the Hydrological Cycle Using Environmental Isotopes." Journal of Japanese Association of Hydrological Sciences 51, no. 2 (August 25, 2021): 45–46. http://dx.doi.org/10.4145/jahs.51.45.
Повний текст джерелаFlorent, Perrine, Henry-Michel Cauchie, and Leslie Ogorzaly. "A Virological Perspective on the Use of Bacteriophages as Hydrological Tracers." Water 14, no. 24 (December 7, 2022): 3991. http://dx.doi.org/10.3390/w14243991.
Повний текст джерелаDai, Liyi, Yinghu Zhang, Ying Liu, Lumeng Xie, Shiqiang Zhao, Zhenming Zhang, and Lv Xizhi. "Assessing hydrological connectivity of wetlands by dye-tracing experiment." Ecological Indicators 119 (December 2020): 106840. http://dx.doi.org/10.1016/j.ecolind.2020.106840.
Повний текст джерелаBenischke, Ralf. "Review: Advances in the methodology and application of tracing in karst aquifers." Hydrogeology Journal 29, no. 1 (January 20, 2021): 67–88. http://dx.doi.org/10.1007/s10040-020-02278-9.
Повний текст джерелаClason, C. C., C. Coch, J. Jarsjö, K. Brugger, P. Jansson, and G. Rosqvist. "Dye tracing to determine flow properties of hydrocarbon-polluted Rabots glaciär, Kebnekaise, Sweden." Hydrology and Earth System Sciences 19, no. 6 (June 15, 2015): 2701–15. http://dx.doi.org/10.5194/hess-19-2701-2015.
Повний текст джерелаClason, C. C., C. Coch, J. Jarsjö, K. Brugger, P. Jansson, and G. Rosqvist. "Dye tracing for investigating flow and transport properties of hydrocarbon-polluted Rabots glaciär, Kebnekaise, Sweden." Hydrology and Earth System Sciences Discussions 11, no. 12 (December 15, 2014): 13711–44. http://dx.doi.org/10.5194/hessd-11-13711-2014.
Повний текст джерелаZhang, Wenqi, Lu Wang, Zhiying Tang, and Yinghu Zhang. "Effects of the Root System Architecture of Pinus taeda and Phyllostachys edulis on the Index of Hydrological Connectivity in Subtropical Forest Ecosystems." Forests 13, no. 12 (November 27, 2022): 2008. http://dx.doi.org/10.3390/f13122008.
Повний текст джерелаFoets, Jasper, Carlos E. Wetzel, Núria Martínez-Carreras, Adriaan J. Teuling, Jean-François Iffly, and Laurent Pfister. "Technical note: A time-integrated sediment trap to sample diatoms for hydrological tracing." Hydrology and Earth System Sciences 24, no. 10 (October 5, 2020): 4709–25. http://dx.doi.org/10.5194/hess-24-4709-2020.
Повний текст джерелаZhang, Yijie, Shugang Wang, Jing Wang, Bo Zhang, Haiyan Li, Liping Li, Chunjin Lin, Zhenhao Xu, Guodong Zhao, and Junfei Han. "A Targeted Grouting and Water Blocking Method Based on Hydrological Tracer Testing and Its Engineering Applications." Water 11, no. 5 (May 13, 2019): 1000. http://dx.doi.org/10.3390/w11051000.
Повний текст джерелаДисертації з теми "Hydrological tracing"
Otz, Martin H. "Using spectro-fluorometry and fluorescent dye-tracing to investigate hydrologic processes in organic-rich environments." Related electronic resource: Current Research at SU : database of SU dissertations, recent titles available full text, 2005. http://wwwlib.umi.com/cr/syr/main.
Повний текст джерелаBishop, Melisa R. "A Detailed Hydrologic Study of the Scott Hollow Groundwater Basin, Greenbrier and Monroe Counties, West Virginia." University of Akron / OhioLINK, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=akron1279892824.
Повний текст джерелаLiu, Zhuhuan, and Chen Zhou. "Hydrological and chloride transport processes in a small catchment of the Norrström Basin : a MIKE SHE modelling approach." Thesis, KTH, Hållbar utveckling, miljövetenskap och teknik, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-250030.
Повний текст джерелаVatten ersätter en viktig del av ekosystemet men det framkallar vattenrelaterade problem som vattenbrist och vattenförorening samtidigt. Emellertid finns det fortfarande ett gap mellan nuvarande vattenhanteringssituationer och våra hållbara mål. Modellering baserad på meteorologiska data erbjuder en möjlighet att förstå regionala hydrologiska processer och övervaka förändringar av miljömässiga kemikalier, särskilt för antropogena föroreningar. Dessutom finns det en hög potential för att förutse förändringar i vattenmängd och kvalitet med hydrologiska modeller, i samband med klimatförändringar. Studieområdet ligger i Kringlans upptagningsområde som ett av Norrström basins, med en yta på 54,5 km2. De lokala utsläppen sammanfogas i Rastälven och strömmar österut, så småningom mynnar i Östersjön. Detta projekt bygger upp en vattenbalansmodell baserad på meteorologiska data inom tidsramen från 2011 till 2012. Vattenbalansmodellen är kalibrerad för att exakt simulera realistiska hydrologiska komponentinteraktioner. För att förbättra modellens robusthet har olika parametrar testats och anpassats under varje process. Samtidigt försöker projektet att hitta en balans mellan modellens komplexitet och hur lång tid det tar att driva modellen. En partikelspårningsmodell för den mättade zonen har utvecklats med utgångspunkt i vattenbalansmodellen. Klorid används som spårämne eftersom det är inert i ekologiska system. Modellsresultaten kan också ge ett värde för grundvattenberäkningen. Tidigare undersökningar inriktade på området föreslår att läckage från vegetation och skogsmark i detta avrinningsområde har bidragit till obalanser i lokala Cl- budgetar. Med hjälp av MIKE SHE modellen har vi undersökt dynamisk process för hydrologisk modellering och kloridpartikelspårning i Kringlan avrinningsområde. Vad som kan gör i framtiden är att förlänga den nuvarande modellgränsen till ett större område med mer referensdata. Det är också möjligt att upprätta en fullständigt integrerad lösningsmodell för att undersöka kloridtransporter i ett avrinningsområde.
Pazol, Jordan Samuel. "Effects of Floodplain Reconnection on Storm Response of Restored River Ecosystems." Ohio University Honors Tutorial College / OhioLINK, 2021. http://rave.ohiolink.edu/etdc/view?acc_num=ouhonors1618926160551753.
Повний текст джерелаHarland, A. N. "Tracing local hydrology and water source use of Eucalyptus largiflorens on the Calperum Floodplain using strontium, oxygen and deuterium isotopes." Thesis, 2018. http://hdl.handle.net/2440/130626.
Повний текст джерелаBlack Box trees (Eucalyptus largiflorens) across the Murray-Darling Basin are in critical condition due to high groundwater salinity and infrequent natural flooding. Geochemical tracers such as radiogenic strontium (87Sr/86Sr), oxygen-18 (𝛿𝛿18O) and deuterium (𝛿𝛿D) are considered useful in the understanding of catchment hydrology and plant water use, and in this study, 87Sr/86Sr, 𝛿𝛿18O and 𝛿𝛿D isotopes were used accordingly to better comprehend local hydrology and water use behaviour patterns of Black Box trees on the Calperum Floodplain, South Australia. Investigations were achieved by sampling and analysing local surface waters (Lake Merreti, Lake Clover, and River Murray), groundwater, soils (1.5 m depth) and plant material (stem water, and leaves) from two separate sites, north (Site 1) and south (Site 4). Considering the local hydrology, Lake Clover was composed of evaporated rainwater, while Lake Merreti was a relative mix of both evaporated rainwater and river water. Additionally, local rainfall sources appeared to vary overtime. Furthermore, groundwater showed no close relationship with rain water suggesting an alternative recharge source such as river water or remnant paleo-water. In terms of water use, linear mixing models using soil 87Sr/86Sr, leaf 87Sr/86Sr and stem water 𝛿𝛿18O inputs showed that Site 1 trees, on average, were predominately using rainwater (77%, 77% & 67%), while Site 4 trees used both rainwater (16%, 32% & 42%) and saline groundwater (70%, 62% & 58%), regardless of nearby lakes and streams. These findings have implications for future monitoring, and the management of outer floodplain Black Box populations that are unable to receive natural flooding inundation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2018
Liou-HaoChen and 陳柳豪. "Analysis of Environmental Parameters and Hydrological Influence on eDNA Tracking Technology." Thesis, 2016. http://ndltd.ncl.edu.tw/handle/ygg54r.
Повний текст джерела國立成功大學
水利及海洋工程學系
104
In order to understand environmental parameters and hydrological influence on eDNA concentration, this study conducted eDNA technology to investigate Channa micropeltes, an invasive species, eDNA concentration. Our study areas include TsengWen Reservoir, NanHua Reservoir and HouJue River. We sampled Channa micropeltes eDNA concentration in all study areas besides TsengWen Reservoir where we investigated different water depth based on two different hydrological conditions. We discovered eDNA concentration in TsengWen Reservoir demonstrated the higest value in 10 m water depth, and lowest value in surface water. The eDNA concentration decreased and distribution was uniformed after rainfall caused runoff disturbing water in the reservoir. In addition, the eDNA concentration distributed higher value at middle section in NanHua Reservoir and downstream of HouJue River.
Mujtaba, Babar. "Rock fragments and surface-subsurface hydrological processes at plot and hillslope scales: Laboratory and numerical simulations." Doctoral thesis, 2021. http://hdl.handle.net/10316/98617.
Повний текст джерелаRainfall-induced surface runoff combined with soil erosion is one of the most important surface hydrological processes and its harmful impact on the environment and communities has been studied for decades. Understanding and modelling surface hydrological processes is vital for engineers, scientists, and policymakers to be able to develop water management and soil conservation strategies. Therefore, mathematical models that can predict the impact of surface hydrological processes on the environment require good quality measured hydrological data. Cost-effective innovative techniques are needed to obtain the good quality hydrological data from field and laboratory experiments. Furthermore, the presence of rock fragments in soils is a major soil property. Identifying the relationship between the rock fragments and surface-subsurface hydrological processes is a major challenge but one that is essential for the development of soil water conservation measures for the rock-fragment abundant soils. The present thesis focuses on two main objectives. The first is to improve understanding of the impact rock fragments have on surface-subsurface hydrological processes at plot and hillslope catchment scale. The second is concerned with the development of innovative measuring techniques and mathematical models related to surface hydrological processes. The research for the first objective started by comparing the influence of soil surface geometry and different distributions of surface rock fragment cover on runoff and soil loss under controlled laboratory conditions. Three different patterns of a constant surface rock fragment cover were tested for a single rainfall intensity event on converging and diverging plane soil surfaces at constant hillslope gradient. The study suggested that the understudied soil surface geometries had more influence on soil erosion than different distribution patterns of a specific percentage of rock fragment surface cover. The next study compared the simulated soil water response of stony soils with measured catchment runoff at hillslope scale. Rainfall-induced soil water response was simulated at three mountain catchment sites using the Hydrus-2D single porosity model. The soils at these sites had 10-65% stoniness. Soil hydraulic parameters employed in the numerical simulations, i.e. the saturated hydraulic conductivity and parameters of the soil water retention curves, were obtained by the Representative Elementary Volume approach (REVa) and by the inverse modelling with Hydrus-1D model (IMa). Shapes of the simulated soil water outflow hydrographs were similar to the measured catchment runoff ones for about a half of rainfall events. Furthermore, soil hydraulic parameters derived by REVa produced more realistic shapes of soil water hydrographs than the IMa ones. The research for the second objective started by testing the capability of a new thermal tracer (cold oil droplets) to measure the velocities of shallow overland flows (<2 mm depth) using the infrared-based particle tracking velocimetry (PTV) technique under controlled laboratory conditions without rainfall. This new approach was compared with dye tracing and the conventional PTV technique (polystyrene beads as tracer and optical video camera) in a quasi-laminar flow regime. The results showed that the infrared-based and conventional PTV techniques estimated velocities were closer to mean velocities measured through volumetric discharge method than were those given by the dye tracing method. This research stressed the potential of the infrared-based PTV technique to estimate the velocities of shallow water bodies due to its tracer's prominent visibility and independence from lighting conditions. Lastly, a 1D physically-based overland flow model that uses cascade plane theory for the estimation of rainfall-induced surface runoff, infiltration and soil erosion on converging and diverging plane surfaces was developed. The model’s simulations were evaluated by the measured data collected under controlled laboratory conditions. Satisfactory results indicated that the model could help to improve the modelling techniques for overland flow and soil erosion on convergent and divergent plane surfaces.
O escoamento superficial e o transporte sólido, induzidos pela precipitação, são importantes processos hidrológicos estudados há décadas, sendo o seu impacto muitas vezes prejudicial no meio ambiente e nos aglomerados populacionais. Compreender e modelar os processos hidrológicos de superfície é vital para que engenheiros, cientistas e decisores políticos possam desenvolver estratégias de gestão de água e conservação do solo. É por isso que os modelos matemáticos que podem prever o impacto dos processos hidrológicos de superfície no meio ambiente requerem dados hidrológicos de qualidade. São necessárias técnicas inovadoras e económicas para obter dados hidrológicos de boa qualidade em experiências de campo e de laboratório. A presença de pedras é uma propriedade importante do solo. Identificar a relação entre as pedras e fragmentos de rocha e os processos hidrológicos subsuperficiais é um grande desafio, mas é essencial para o desenvolvimento de medidas de conservação da água do solo para esses solos pedregosos. A presente tese concentra-se em dois objetivos principais. O primeiro é melhorar a compreensão do impacto que as pedras têm nos processos hidrológicos de superfície e subsuperficiais à escala de parcela e da bacia de drenagem. O segundo está relacionado ao desenvolvimento de técnicas inovadoras de medição e ao desenvolvimento de modelos matemáticos relacionados aos processos hidrológicos de superfície. A pesquisa relativamente ao primeiro objetivo começou por comparar a influência da geometria da superfície do solo e diferentes distribuições da cobertura de fragmentos de rocha no escoamento superficial e perda de solo, em condições controladas de laboratório. Três padrões diferentes de cobertura de pedras em superfícies planas, convergentes e divergentes, foram testados para uma chuvada tipo. Esse estudo concluiu que a geometria da superfície do solo tinha mais influência que os padrões de distribuição das pedras na severidade do processo de erosão. O estudo seguinte comparou a resposta da água no solo de solos pedregosos com o escoamento medido de bacia de drenagem, à escala da encosta. A resposta da água no solo induzida pela chuva foi simulada em três locais da bacia hidrográfica usando o modelo Hydrus-2D. Os solos nesses locais tinham pedregosidade entre 10-65%. Os parâmetros hidráulicos do solo usados nas simulações numéricas, ou seja, a condutividade hidráulica saturada e os parâmetros das curvas de retenção de água no solo, foram obtidos pela abordagem do Volume Elementar Representativo (REVa) e pela Modelagem Inversa com o modelo Hydrus-1D (IMa). As formas dos hidrogramas de água do solo simulados foram semelhantes às medidas formas dos hidrogramas de escoamento superficial das bacias para cerca de metade dos eventos de chuva. Além disso, os parâmetros hidráulicos do solo derivados do REVa produziram formas mais realistas de hidrogramas da água do solo do que os do IMa. A pesquisa para o segundo objetivo começou por testar a capacidade de um novo traçador térmico (gotas de óleo arrefecidas) para estimar as velocidades de escoamentos superficiais pouco profundos (<2 mm de profundidade) usando a técnica de velocimetria de rastreamento de partículas (PTV), baseada em infravermelho, sob condições controladas de laboratório. Esta nova abordagem foi comparada com o método do traçado colorido e a técnica PTV convencional (usando grânulos de poliestireno como traçador e uma câmara de vídeo) num regime de escoamento quase laminar. Os resultados mostraram que as velocidades estimadas das técnicas PTV convencionais e as baseadas no infravermelho estavam mais próximas das velocidades médias obtidas pelo método de volumétrico do que as velocidades do método de traçado colorido. Esta pesquisa enfatizou o potencial da técnica PTV baseada no infravermelho para estimativa das velocidades de escoamentos pouco profundos devido à alta visibilidade do traçador e independência das condições de iluminação. Por último, foi desenvolvido um modelo de escoamento superficial 1D, fisicamente baseado, que usa a teoria da cascata de planos para a estimativa do escoamento superficial, infiltração e erosão hídrica do solo em superfícies convergentes e divergentes. As simulações do modelo foram avaliadas comparando os resultados numéricos com dados medidos em laboratório. Os resultados indicaram que o modelo podia ajudar a aprimorar a modelação do escoamento superficial pouco profundo e a erosão do solo em superfícies planas convergentes e divergentes.
Книги з теми "Hydrological tracing"
Code of practice for hydrologic tracing analysis studies. Edmonton: Queen's Printer, 1997.
Знайти повний текст джерелаTillery, Anne. Survey of hydrologic models and hydrologic data needs for tracking flow in the Rio Grande, North-Central New Mexico, 2010. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2012.
Знайти повний текст джерелаInternational Symposium on Water Tracing (7th 1997 Portorož, Slovenia). Tracer hydrology 97: Proceedings of the 7th International Symposium on Water Tracing, Portorož, Slovenia, 26-31 May 1997. Rotterdam: A.A. Balkema, 1997.
Знайти повний текст джерелаMoyer, Douglas L. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Accotink Creek, Fairfax County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаMoyer, Douglas L. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Christians Creek, Augusta County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаMoyer, Douglas L. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Christians Creek, Augusta County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаL, Moyer Douglas. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Blacks Run, Rockingham County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаMoyer, Douglas L. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Blacks Run, Rockingham County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаMoyer, Douglas L. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Christians Creek, Augusta County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаMoyer, Douglas L. Use of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Blacks Run, Rockingham County, Virginia. Richmond, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.
Знайти повний текст джерелаЧастини книг з теми "Hydrological tracing"
Kalma, S. J., P. J. Thorburn, and G. M. Dunn. "Using Heat Pulse and Deuterium Tracing Techniques to Estimate Tree Water Use." In Subsurface Hydrological Responses to Land Cover and Land Use Changes, 47–60. Boston, MA: Springer US, 1997. http://dx.doi.org/10.1007/978-1-4615-6141-5_4.
Повний текст джерелаThatcher, L. L. "Water Tracing in the Hydrologic Cycle." In Isotope Techniques in the Hydrologic Cycle, 97–108. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm011p0097.
Повний текст джерелаMerritt, W. F. "Techniques of Groundwater Tracing Using Radionuclides." In Isotope Techniques in the Hydrologic Cycle, 169–70. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm011p0169.
Повний текст джерелаWarburton, Joseph A. "The Tracing of Radioisotopes Released Into the Lower Troposphere." In Isotope Techniques in the Hydrologic Cycle, 61. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm011p0061.
Повний текст джерелаPeters, Norman E., and Elizabeth B. Ratcliffe. "Tracing Hydrologic Pathways Using Chloride at the Panola Mountain Research Watershed, Georgia, USA." In Biogeochemical Investigations at Watershed, Landscape, and Regional Scales, 263–75. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-017-0906-4_25.
Повний текст джерелаCreed, Irena F., and Gabor Z. Sass. "Digital Terrain Analysis Approaches for Tracking Hydrological and Biogeochemical Pathways and Processes in Forested Landscapes." In Forest Hydrology and Biogeochemistry, 69–100. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1363-5_4.
Повний текст джерелаVallette, Anne, Quentin Gunti, Fatimatou Coulibaly, and Anne-Laure Beck. "Implementation of a Hydrologic Model as an Element of the Litter-TEP Service—Marine Litter Tracking and Stranding Forecast—Or for the Understanding of the Coastal Patterns Change." In Advances in Hydroinformatics, 921–36. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-1600-7_57.
Повний текст джерела"TRACING THE HYDROLOGICAL CYCLE." In Environmental Isotopes in Hydrogeology, 49–76. CRC Press, 2013. http://dx.doi.org/10.1201/9781482242911-9.
Повний текст джерелаLu, Jia-Ju, Quan-Jiu Wang, Jing-Jie Yu, Xian-Fang Song, Jun Xia, Wei-Zu Gu, and Chang-Ming Liu. "Hydrological experimental system and environmental isotope tracing." In Research Basins and Hydrological Planning, 11–18. Taylor & Francis, 2004. http://dx.doi.org/10.1201/9781439833858.ch2.
Повний текст джерела"Hydrologic Tracing." In Modern Hydrology and Sustainable Water Development, 181–216. Chichester, UK: John Wiley & Sons, Ltd, 2010. http://dx.doi.org/10.1002/9781444323962.ch7.
Повний текст джерелаТези доповідей конференцій з теми "Hydrological tracing"
Hernandez, Fernando, Jason S. Polk, Patricia N. Kambesis, James Smith, and Fredrick D. Siewers. "CHARACTERIZING HYDROLOGIC CONNECTIONS AND KARSTIFICATION IN SISTEMA HUAUTLA FROM EXPLORATION AND DYE TRACING." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324018.
Повний текст джерелаPajak, Katarzyna. "Seasonal Baltic Sea level change from altimetry data." In Environmental Engineering. VGTU Technika, 2017. http://dx.doi.org/10.3846/enviro.2017.223.
Повний текст джерелаParlanti, E., M. Sourzac, F. Baratelli, G. Varrault, and N. Flipo. "TRACKING SOURCES AND DYNAMICS OF DISSOLVED ORGANIC MATTER (DOM) IN AN ALLUVIAL PLAIN IN CONTRASTED HYDROLOGICAL SITUATIONS." In 30th International Meeting on Organic Geochemistry (IMOG 2021). European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202134119.
Повний текст джерелаWerner, Kent, Emma Bosson, and Sten Berglund. "Flow and Radionuclide Transport From Rock to Surface Systems: Characterization and Modelling of Potential Repository Sites in Sweden." In The 11th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2007. http://dx.doi.org/10.1115/icem2007-7300.
Повний текст джерелаЗвіти організацій з теми "Hydrological tracing"
Use of the Hydrological Simulation Program-FORTRAN and Bacterial Source Tracking for Development of the fecal coliform Total Maximum Daily Load (TMDL) for Accotink Creek, Fairfax County, Virginia. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034160.
Повний текст джерелаUse of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Blacks Run, Rockingham County, Virginia. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034161.
Повний текст джерелаUse of the Hydrological Simulation Program-FORTRAN and bacterial source tracking for development of the fecal coliform total maximum daily load (TMDL) for Christians Creek, Augusta County, Virginia. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034162.
Повний текст джерела