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Journal articles on the topic 'Causeway Lake'

Author: Grafiati

Published: 4 June 2021

Last updated: 7 February 2022

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

Shamshiri, R., M. Motagh, M. Baes, and M. A. Sharifi. "INSAR AND FINITE ELEMENT ANALYSIS OF GROUND DEFORMATION AT LAKE URMIA CAUSEWAY (LUC), NORTHWEST IRAN." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XL-1/W3 (September 25, 2013): 389–91. http://dx.doi.org/10.5194/isprsarchives-xl-1-w3-389-2013.

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12

Sabbagh-Yazdi, S. R., L. GhelichKhany, and K. Kalhor. "Numerical investigation of the effects of causeway opening configurations on horizontal currents of Lake Urmia." International Journal of Environmental Science and Technology 17, no. 4 (2019): 1885–98. http://dx.doi.org/10.1007/s13762-019-02599-7.

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13

Eslami, A., E. Aflaki, and B. Hosseini. "Evaluating CPT and CPTu based pile bearing capacity estimation methods using Urmiyeh Lake Causeway piling records." Scientia Iranica 18, no. 5 (2011): 1009–19. http://dx.doi.org/10.1016/j.scient.2011.09.003.

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14

Zeinoddini, Mostafa, Mohammad Ali Tofighi, and Fereydun Vafaee. "Evaluation of dike-type causeway impacts on the flow and salinity regimes in Urmia Lake, Iran." Journal of Great Lakes Research 35, no. 1 (2009): 13–22. http://dx.doi.org/10.1016/j.jglr.2008.08.001.

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15

White, James S., Sarah E. Null, and David G. Tarboton. "How Do Changes to the Railroad Causeway in Utah’s Great Salt Lake Affect Water and Salt Flow?" PLOS ONE 10, no. 12 (2015): e0144111. http://dx.doi.org/10.1371/journal.pone.0144111.

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16

Tilton, James C., Robert E. Wolfe, and Guoqing Lin. "On-Orbit Line Spread Function Estimation of the SNPP VIIRS Imaging System From Lake Pontchartrain Causeway Bridge Images." IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing 10, no. 11 (2017): 5056–72. http://dx.doi.org/10.1109/jstars.2017.2729879.

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17

Dadashzadeh, Mehran, Javad Parsa, and Alireza Mojtahedi. "Investigation over the Interaction of Lake Urmia Wave Pattern and Causeway Using Meteorological Models and Computational Fluid Dynamics." Journal of Oceanography 11, no. 41 (2020): 49–61. http://dx.doi.org/10.52547/joc.11.41.49.

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18

Whitby, Michael. "Justinian's bridge over the Sangarius and the date of Procopius' de Aedificiis." Journal of Hellenic Studies 105 (November 1985): 129–48. http://dx.doi.org/10.2307/631526.

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In the village of Beşköprü, about five kilometres to the south-west of the town of Adapazari in western Turkey, and just to the north of the main Istanbul–Ankara highway, there stands a large well-constructed bridge; its fabric is generally in good condition apart from the destruction of a short section of the causeway near its eastern end to permit the passage of the branch railway line to Adapazan. Although the bridge now only spans two minor side channels of the small stream called the Çark Deresi, which drains Lake Sophon (modern Sapanca), there is no doubt that the bridge was originally d

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19

Gavel, Melody J., R. Timothy Patterson, Nawaf A. Nasser, et al. "What killed Frame Lake? A precautionary tale for urban planners." PeerJ 6 (June 14, 2018): e4850. http://dx.doi.org/10.7717/peerj.4850.

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Frame Lake, located within the city of Yellowknife, Northwest Territories, Canada, has been identified as requiring significant remediation due to its steadily declining water quality and inability to support fish by the 1970s. Former gold mining operations and urbanization around the lake have been suspected as probable causes for the decline in water quality. While these land-use activities are well documented, little information is available regarding their impact on the lake itself. For this reason, Arcellinida, a group of shelled protozoans known to be reliable bioindicators of land-use c

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20

German, J., K. Jansons, G. Svensson, D. Karlsson, and L. G. Gustafsson. "Modelling of different measures for improving removal in a stormwater pond." Water Science and Technology 52, no. 5 (2005): 105–12. http://dx.doi.org/10.2166/wst.2005.0120.

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The effect of retrofitting an existing pond on removal efficiency and hydraulic performance was modelled using the commercial software Mike21 and compartmental modelling. The Mike21 model had previously been calibrated on the studied pond. Installation of baffles, the addition of culverts under a causeway and removal of an existing island were all studied as possible improvement measures in the pond. The subsequent effect on hydraulic performance and removal of suspended solids was then evaluated. Copper, cadmium, BOD, nitrogen and phosphorus removal were also investigated for that specific im

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21

Shamshiri, Roghayeh, Mahdi Motagh, Marzieh Baes, and Mohammad Ali Sharifi. "Deformation analysis of the Lake Urmia causeway (LUC) embankments in northwest Iran: insights from multi-sensor interferometry synthetic aperture radar (InSAR) data and finite element modeling (FEM)." Journal of Geodesy 88, no. 12 (2014): 1171–85. http://dx.doi.org/10.1007/s00190-014-0752-6.

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22

Neumann, Klaus, W. Berry Lyons, and David J. Des Marais. "Inorganic carbon-isotope distribution and budget in the Lake Hoare and Lake Fryxell basins, Taylor Valley, Antarctica." Annals of Glaciology 27 (1998): 685–89. http://dx.doi.org/10.3189/1998aog27-1-685-689.

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One of the unusual features of Lakes Fryxell and Hnare in Taylor Valley, southern Victoria Land, Antarctica, is their perennial ice cover. This ice cover limits gas exchange between the atmosphere and the lake water, and causesa very stable stratification of the lakes. We analyzed a series of water samples from profiles of these lakes and their tributaries for δ13C of the dissolved inorganic carbon (DIC) in order to qualify the carbon flux from the streams into the lakes, and to investigate the carbon cycling with in the lakes. Isotopic values in the uppermost waters (δ13C = +l.3‰ to 5.3‰ in L

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23

Cooper, A. H., and S. G. Molyneux. "The age and correlation of Skiddaw Group (early Ordovician) sediments in the Cross Fell inlier (northern England)." Geological Magazine 127, no. 2 (1990): 147–57. http://dx.doi.org/10.1017/s0016756800013832.

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AbstractThe Skiddaw Group in the Cross Fell inlier comprises the Catterpallot Formation of latest Tremadoc or earliest Arenig age, the Murton Formation of Arenig age, and the Kirkland Formation of early Llanvirn age. Each of these formations can be correlated with formations in the Skiddaw Group of the Lake District. The faulted contact of the Catterpallot and Kirkland formations is the probable extension of the Causey Pike Fault (CPF), which separates two distinct sequences in the Skiddaw inlier of the northern Lake District. Contrasts across the CPF in the Cross Fell inlier reflect those see

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24

Whitney, Bronwen S., Ruth Dickau, Francis E. Mayle, J. Daniel Soto, and José Iriarte. "Pre-Columbian landscape impact and agriculture in the Monumental Mound region of the Llanos de Moxos, lowland Bolivia." Quaternary Research 80, no. 2 (2013): 207–17. http://dx.doi.org/10.1016/j.yqres.2013.06.005.

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We present a multiproxy study of land use by a pre-Columbian earth mounds culture in the Bolivian Amazon. The Monumental Mounds Region (MMR) is an archaeological sub-region characterized by hundreds of pre-Columbian habitation mounds associated with a complex network of canals and causeways, and situated in the forest–savanna mosaic of the Llanos de Moxos. Pollen, phytolith, and charcoal analyses were performed on a sediment core from a large lake (14 km2), Laguna San José (14°56.97′S, 64°29.70′W). We found evidence of high levels of anthropogenic burning from AD 400 to AD 1280, corroborating

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25

Fortey, N. J., B. Roberts, and S. R. Hirons. "Relationship between metamorphism and structure in the Skiddaw Group, English Lake District." Geological Magazine 130, no. 5 (1993): 631–38. http://dx.doi.org/10.1017/s0016756800020938.

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AbstractRegional variation of white mica (illite) crystallinity in the Skiddaw Group is set against the structural interpretation of Hughes, Cooper & Stone (1993, this issue) in which early- or pre-Ludlow deformation and slaty cleavage development (S1) were succeeded by southward thrusting and an associated development of S1 and S1 crenulation cleavages, possibly during early Devonian times. Kubier index (KI) values are plotted in relation to geological structure for a major part of the Skiddaw Group, and cross-sections constructed. The pattern is interpreted in terms of three processes: (

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26

Jewell, Paul W. "Historic low stand of Great Salt Lake, Utah: I." SN Applied Sciences 3, no. 8 (2021). http://dx.doi.org/10.1007/s42452-021-04691-5.

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AbstractGreat Salt Lake of Utah is among the largest and most ecologically important water bodies in North America. Since the late 1950s, the lake has been divided into two hydrologically distinct water bodies by a rock-fill railroad causeway. Flux through the causeway is driven by two forces: differential surface elevation and differential density between the north and south arms. The south arm features episodic vertical stratification due to the influx of deep, dense brine from the north arm. The source of this brine (a breach, two culverts, or subsurface flow) has been investigated over the

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27

"Postfailure analysis: Tramping Lake causeway, Saskatchewan, Canada." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 27, no. 5 (1990): 299. http://dx.doi.org/10.1016/0148-9062(90)93081-v.

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28

Karimzadeh, Sadra, Masashi Matsuoka, and Fumitaka Ogushi. "Spatiotemporal deformation patterns of the Lake Urmia Causeway as characterized by multisensor InSAR analysis." Scientific Reports 8, no. 1 (2018). http://dx.doi.org/10.1038/s41598-018-23650-6.

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29

Shacker, Andrew, Nick Scrivens, Jason Tupper, and Katherine Witherspoon. "Assessment of Road Mortality in the Spotted Turtle (Clemmys guttata)." Inquiry@Queen's Undergraduate Research Conference Proceedings, February 20, 2018. http://dx.doi.org/10.24908/iqurcp.9357.

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The Spotted Turtle (Clemmy guttata), a small freshwater turtle species, prefer shallow wetland habitats, and are restricted to eastern North America, predominantly in southern Ontario along the southern shores of the Great Lakes. However, the Spotted Turtle has been classified as ‘vulnerable’ (a species of special concern) by COSEWIC since 1991, owing to the 35% decline of the population throughout the past century. This is primarily of concern regarding reductions of ecosystem biodiversity, and further anthropogenic pressures will drive the species towards further endangerment. High rates of

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30

Ryan, John C., Danielle Brady, and Christopher Kueh. "Where Fanny Balbuk Walked: Re-imagining Perth’s Wetlands." M/C Journal 18, no. 6 (2016). http://dx.doi.org/10.5204/mcj.1038.

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Special Care Notice This article contains images of deceased people that might cause sadness or distress to Aboriginal and Torres Strait Islander readers. Introduction Like many cities, Perth was founded on wetlands that have been integral to its history and culture (Seddon 226–32). However, in order to promote a settlement agenda, early mapmakers sought to erase the city’s wetlands from cartographic depictions (Giblett, Cities). Since the colonial era, inner-Perth’s swamps and lakes have been drained, filled, significantly reduced in size, or otherwise reclaimed for urban expansion (Bekle). N

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31

Pontonuwu, James. "Gambaran Status Karies Anak Sekolah Dasar di Kelurahan Kinilow 1 Kecamatan Tomohon Utara." e-GIGI 1, no. 2 (2013). http://dx.doi.org/10.35790/eg.1.2.2013.3145.

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Karies gigi adalah penyakit jaringan gigi yang ditandai dengan kerusakan jaringan, dimulai dari permukaan gigi meluas ke arah pulpa. Karies gigi dapat terjadi pada setiap orang yang dapat timbul pada suatu permukaan gigi dan dapat meluas kebagian yang lebih dalam dari gigi. Masalah utama dalam rongga mulut anak sampai saat ini yaitu penyakit karies gigi, sehingga masalah kesehatan gigi dan mulut menjadi perhatian yang sangat penting dalam pembangunan kesehatan yang salah satunya disebabkan oleh rentannya kelompok anak usia sekolah dari gangguan kesehatan gigi. Tujuan penelitian ini untuk menge

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