Academic literature on the topic 'Causeway Lake'

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Journal articles on the topic "Causeway Lake"

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Witcher, T. R. "Lake Pontchartrain Causeway." Civil Engineering Magazine Archive 87, no. 5 (2017): 42–45. http://dx.doi.org/10.1061/ciegag.0001196.

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He, Cheng, and Quintin Rochfort. "Numerical Modelling Approaches for Assessing Improvements to the Flow Circulation in a Small Lake." Modelling and Simulation in Engineering 2011 (2011): 1–21. http://dx.doi.org/10.1155/2011/897618.

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Kamaniskeg Lake is a long, narrow, and deep small lake located in the northern part of Ontario, Canada. The goals of this paper were to examine various options to improve the water quality in the northern part of the lake by altering the local hydraulic flow conditions. Towards this end, a preliminary screening suggested that the flow circulation could be increased around a central island (Mask Island) in the northern part of the lake by opening up an existing causeway connecting the mainland and central island. Three-dimensional (3D) hydraulic and transport models were adopted in this paper t
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Labossiere, J. L., E. K. Sauer, and E. A. Christiansen. "Postfailure analysis: Tramping Lake causeway, Saskatchewan, Canada." Canadian Geotechnical Journal 26, no. 4 (1989): 687–704. http://dx.doi.org/10.1139/t89-080.

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A traffic causeway placed on the sediments of saline Tramping Lake failed during construction in the summer of 1982. Vertical subsidence has continued until present (1988). The failure mechanism was controlled by sedimentary structure and artesian groundwater conditions. The shear zone is in a soft, near normally consolidated lacustrine sandy silt unit 22 m thick. The lake basin contains lacustrine, deltaic, and fluvial deposits of postglacial origin. Artesian conditions in the Upper Cretaceous Judith River Formation and postglacial fluvial sand and gravel dominate the hydrogeology at the site
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Rasmussen, Michael, Som Dutta, Bethany T. Neilson, and Brian Mark Crookston. "CFD Model of the Density-Driven Bidirectional Flows through the West Crack Breach in the Great Salt Lake Causeway." Water 13, no. 17 (2021): 2423. http://dx.doi.org/10.3390/w13172423.

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Stratified flows and the resulting density-driven currents occur in the natural environment and commonly in saline lakes. In the Great Salt Lake, Utah, USA, the northern and southern portions of the lake are divided by an east-to-west railroad causeway that disrupts natural lake currents and significantly increases salt concentrations in the northern section. To support management efforts focused on addressing rising environmental and economic concerns associated with varied saltwater densities throughout the lake, the causeway was recently modified to include a new breach. The purpose of this
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Chesteen, Susan A., and Bruce F. Baird. "Breaching the Great Salt Lake Causeway: An Addendum." Interfaces 15, no. 4 (1985): 48–51. http://dx.doi.org/10.1287/inte.15.4.48.

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Mohammadi, Ali, Razyeh Lak, Georg Schwamborn, Amaneh Kaveh Firouz, Attila Çiner, and Javad Darvishi Khatouni. "Depositional environments and salt-thickness variations in Urmia Lake (NW Iran): Insight from sediment-core studies." Journal of Sedimentary Research 91, no. 3 (2021): 296–316. http://dx.doi.org/10.2110/jsr.2020.078.

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ABSTRACT Urmia Lake is a large-scale hypersaline lake that experienced a drastic water-level fall due to natural and anthropogenic forces during the last two decades. Construction of a causeway in the central part of the lake after 1989 has divided the lake into northern and southern parts and caused an extreme change of the lake hydrochemical system. Precipitation of evaporite minerals as crust on the lake floor was caused by the combination of lake level fall and increasing water salinity. However, some parameters controlling rates of salt deposition and dissolution and temporal and spatial
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Ghadimi, M., and M. A. Nezammahalleh. "CONSTRUCTION OF A CAUSEWAY BRIDGE ACROSS THE LAKE URMIA AND ITS INFLUENCE ON DRYING TREND OF THE LAKE." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XL-1-W5 (December 11, 2015): 211–13. http://dx.doi.org/10.5194/isprsarchives-xl-1-w5-211-2015.

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Construction of a causeway bridge on the Lake Urmia accelerated the drying trend of the largest hyper-saline lake of the world. The objective of the research is to investigate the differences of precipitation and river discharge before and after initiation of the construction of the bridge in 2000. The study area was the watershed of the lake. The averages of the precipitation data in the two periods before and after the project have been interpolated by IDW based on GIS Geostatistical Analyst. The two interpolated precipitation layers were used to be plugged into Student T-test equation in GI
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Naftz, D. "Inputs and Internal Cycling of Nitrogen to a Causeway Influenced, Hypersaline Lake, Great Salt Lake, Utah, USA." Aquatic Geochemistry 23, no. 3 (2017): 199–216. http://dx.doi.org/10.1007/s10498-017-9318-6.

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Hemmati, Mohammad, Hojjat Ahmadi, Sajad Ahmad Hamidi, and Vahid Naderkhanloo. "Environmental effects of the causeway on water and salinity balance in Lake Urmia." Regional Studies in Marine Science 44 (May 2021): 101756. http://dx.doi.org/10.1016/j.rsma.2021.101756.

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Safavi, Salman, Abolfazl Shamsai, Bahram Saghafian, and Sayed Bateni. "Modeling Spatial Pattern of Salinity using MIKE21 and Principal Component Analysis Technique in Urmia Lake." Current World Environment 10, no. 2 (2015): 626–33. http://dx.doi.org/10.12944/cwe.10.2.28.

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Urmia Lake in the northwestern of Iran is a hypersaline water body and has become an environmentally important issue especially due to the presence of an infrequent aquatic species, Artemia Urmiana. During the last three decades, several considerable man-made changes including river damming and construction of a causeway across the lake affected the lake salinity. This article aims to propose a new approach of salinity modeling using a reduced-order model based on MIKE21 simulation model, in conjunction with principal component analysis (PCA) technique. At first, spatial variation of salinity
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Dissertations / Theses on the topic "Causeway Lake"

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Soetanto, Budi, and soetanto@gmail com. "EVALUATION OF SEDIMENTATION PROCESSES IN A COASTAL LAKE: CAUSEWAY LAKE, THE CAPRICORN COAST CASE STUDY." Central Queensland University. Engineering, 2007. http://library-resources.cqu.edu.au./thesis/adt-QCQU/public/adt-QCQU20070622.122252.

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This thesis presents analysis of the hydrodynamic and sedimentation changes of the Causeway Lake, Queensland. It was created in 1939 when a causeway and bridge construction was built across the estuary entrance. Since the construction, significant sediment retention has occurred in the lake. The sediment study presented in this thesis was undertaken based on historical data, field data measurement and numerical modelling, supported by theoretical analysis. Based on bathymetry data for the period from 1986 and 2003, an average of 2500 m3/year of sediment has settled in the estuary. To verify th
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White, James S. "Great Salt Lake Past and Present: Elevation and Salinity Changes to Utah's Great Salt Lake from Railroad Causeway Alterations." DigitalCommons@USU, 2015. https://digitalcommons.usu.edu/etd/4588.

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In 1959, Union Pacific Railroad constructed a rock-filled causeway bisecting Utah’s Great Salt Lake, separating the lake into a north and south arm. Flow between the two arms was limited to two 4.6 meter wide culverts installed during original construction, an 88 meter breach opening installed in 1984, and the semi porous boulder and gravel causeway material. The south arm receives nearly all streamflows entering Great Salt Lake and a salinity gradient between the two arms developed over time. North arm salinity is often at or near saturation, averaging 317 g\L since 1966, while the south is c
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Euclide, Peter T. "Genetic And Demographic Consequences Of Lake And River Habitat Fragmentation On Fishes In Vermont." ScholarWorks @ UVM, 2018. https://scholarworks.uvm.edu/graddis/887.

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Globally, habitat fragmentation has had a major impact on the conservation and management of many species and is one of the primary causes of species extinction. Habitat fragmentation is loosely defined as a process in which a continuous habitat is reduced to smaller, disconnected patches as the result of habitat loss, restriction of migration or the construction of barriers to movement. Aquatic systems are particularly vulnerable to habitat fragmentation, and today an estimated 48% of rivers are fragmented worldwide. My dissertation evaluates how habitat fragmentation has influenced the popul
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Gunnell, Nathan Vaun. "A Study of the Anthropogenic Impact in Farmington Bay through Isotopic and Elemental Analysis." BYU ScholarsArchive, 2020. https://scholarsarchive.byu.edu/etd/9208.

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The influence of human activity on surrounding environments is an important field of research. With respect to aquatic settings, lacustrine deposits provide excellent proxies of environmental change since the sediment accumulates at a relatively constant rate, recording environmental change. This study employs isotopic, mineral, and chemical records from Farmington Bay freeze cores, in particular δ13C, δ15N, and 210Pb isotopes as well as phosphorus level fluctuation and trace metal analysis. In particular, 210Pb isotopes permit estimation of the age of sediment with depth and δ15N, δ13C, and c
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Lai, Pei Ling, and 賴佩鈴. "The Study on the Effect of Somatic Movement Education in Cases of Pain Causedby Late Stage Breast Cancer." Thesis, 2012. http://ndltd.ncl.edu.tw/handle/y9mu4e.

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碩士<br>國立臺東大學<br>身心整合與運動休閒產業學系<br>100<br>The purpose of this study was to help a patient at late stage breast cancer after twenty years to relief pain through somatic movement education. It aimed to help patient to increase body observation sensitivity, enhance sleeping quality, self-relaxation through the practice of somatic movement and to formulate a set of somatic movement education and learning activities to help the course to be continual.Research method adopted the qualitative case study method by observing the case practicing somatic movement for four weeks, eighty minutes each session,
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Books on the topic "Causeway Lake"

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McCulloch, Urban F. Preliminary hydraulic study for improving the tidal flushing action in Graham Rogers Lake, North River causeway and sluice, Queens County. Urban F. McCulloch, 1987.

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2

Wold, Steven R. Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway. U.S. G.P.O., 1997.

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Loving, Brian L. Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway, 1987-98. U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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Connor, Aileen. Roman and Medieval occupation in Causeway Lane, Leicester: Excavations 1980 and 1991. School of Archaeological Studies, University of Leicester, 1999.

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5

Effects of breaching the Southern Pacific Railroad causeway, Great Salt Lake, Utah -- physical and chemical changes, August 1, 1984 - July, 1986. Utah Geological Survey, 1987. http://dx.doi.org/10.34191/wrb-25.

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Book chapters on the topic "Causeway Lake"

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Houk, Brett A., and Ashley Booher. "All the World’s a Stage." In Approaches to Monumental Landscapes of the Ancient Maya. University Press of Florida, 2020. http://dx.doi.org/10.5744/florida/9780813066226.003.0008.

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Approaching monumentality and politics at an epicentral-scale, Houk and Ashley Booher use a site-planning approach in chapter 8 to argue that the Late Classic rulers of Chan Chich, Belize designed major architectural components of the site to function as the theater for public spectacles and processions. The authors are able to demonstrate evidence for rituals’ having taken place along the two causeways and at their termini structures, as well as an apparent functional relationship between one causeway and an associated courtyard. Ritual, in this case, was actually the means to a political end. As Houk and Booher show, converting the monumental landscape of Chan Chich into a vast stage for public spectacle and ritual processions required considerable planning, labor, and resources. The Late Classic rulers at Chan Chich and other sites spent vast resources on the architecture of political theater as an exercise in community building and regional competition for labor, loyalty, and prestige.
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Doyle, Arthur Conan. "The Third Generation." In Gothic Tales. Oxford University Press, 2018. http://dx.doi.org/10.1093/owc/9780198734307.003.0016.

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Scudamore Lane, sloping down riverwards from just behind the Monument,* lies, at night, in the shadow of two black and monstrous walls which loom high above the glimmer of the scattered gas-lamps. The footpaths are narrow, and the causeway is paved...
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Chase, Diane Z., Arlen F. Chase, and Adrian S. Z. Chase. "Caracol’s Impact on the Landscape of the Classic Period Maya." In Approaches to Monumental Landscapes of the Ancient Maya. University Press of Florida, 2020. http://dx.doi.org/10.5744/florida/9780813066226.003.0006.

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Diane Chase and colleagues discuss one of the largest Classic-period Maya sites that ever existed, Caracol, Belize, in Chapter 6. Using over 30 years of data from the site, the authors examine four components of Caracol’s monumental landscape: the site’s plazuela groups, its causeway system, its reservoir system, and its agricultural terraces. Extensive excavation, mapping, and LiDAR data demonstrate that Caracol’s expansive territory was a heavily modified landscape, with considerable evidence for centralized planning. Mapped onto this planned landscape at Caracol is evidence for economic integration and centrally directed social engineering in the form of “symbolic egalitarianism.” As large and populous as Caracol was, it is not surprising that the city’s rulers extended their influence beyond the kingdom’s immediate territory and onto the larger geopolitical landscape of the Late Classic period. Chase and colleagues broaden the concept of monumentality to consider strategic political nodes on the landscape and inter-polity interactions on a truly regional scale. The authors close their chapter with a consideration of the roles of human decision making and climate change in the final abandonment of the kingdom.
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Harding, Dennis. "Hillforts in the Landscape." In Iron Age Hillforts in Britain and Beyond. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199695249.003.0009.

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Landscape in common usage refers to the physical landforms of hills, valleys, rivers, and lakes, together with vegetational cover that may have changed significantly over the centuries depending upon environmental factors as well as the impact of human settlement. It may also refer to the man-made landscape of buildings and settlements, roads and boundaries made by human occupation over the centuries. Although field archaeologists tend to focus their attention upon ‘sites’, it has long been recognized that individual settlements cannot have functioned in isolation from their environment, nor from their neighbours in the landscape. Equally important, although at the limits of archaeological inference, is how later prehistoric people viewed their own environment, which can hardly have been a matter of ignorance or indifference. The fact that a Neolithic long barrow extends down the spine of the hillfort at Hambledon Hill, or that a causewayed enclosure lies concentrically within the circuit at the Trundle in Sussex, may not have determined the hillfort's location, but it is hardly likely that Iron Age builders were unaware of their antiquity and significance. Landscape archaeology is often wrongly regarded as a recent contribution to field archaeology. Following the long-term excavations at Danebury of the 1970s and 1980s, the Danebury Environs Project still stands as one of the most significant advances in hillfort studies, together with landscape surveys around Maiden Castle, Dorset, and Cadbury Castle among others. A pioneer in this field was Christopher Hawkes, encouraged from the 1920s by O. G. S. Crawford. In the St Catharine's Hill report, Hawkes had stated explicitly that his purpose was to show &amp;lsquo;the place occupied by the hill settlement in the life of the contemporary countryside’ (Hawkes et al. 1930: 6), and in his Hampshire hillfort excavations of the 1930s he demonstrated this principle, notably at Quarley Hill (Hawkes 1939), where his excavation was designed to elucidate the relationship between hillfort and those linear features that physically linked it to its surrounding landscape. The Danebury excavation was the ultimate sequel to Hawkes’ Hampshire hillfort campaign, and with its Environs Programme, extended the study of the hillfort in its landscape context on a scale never previously practicable. This entailed a study of documentary sources and air photographs as well as field survey with selective excavation.
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Conference papers on the topic "Causeway Lake"

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Salvati, Lynn A., Stephen J. Guarente, and S. Caleb Douglas. "The Great Salt Lake Causeway—A Calculated Risk 50 Years Later." In IFCEE 2015. American Society of Civil Engineers, 2015. http://dx.doi.org/10.1061/9780784479087.061.

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Reports on the topic "Causeway Lake"

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Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway. US Geological Survey, 1997. http://dx.doi.org/10.3133/wsp2450.

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Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway, 1987-98. US Geological Survey, 2000. http://dx.doi.org/10.3133/wri004221.

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