Relevant bibliographies by topics / Aggradation

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Aggradation'

Author: Grafiati
Published: 4 June 2021
Last updated: 10 March 2023

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Journal articles on the topic "Aggradation"

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Nikic, Zoran, Ratko Ristic, Nenad Maric, Vukasin Milcanovic, Sinisa Polovina, and Ivan Malusevic. "Function of check dam aggradation in local water supply of mountainous areas." Bulletin of the Faculty of Forestry, no. 120 (2019): 117–30. http://dx.doi.org/10.2298/gsf1920117n.

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Check dams are built to control erosion processes and torrential floods. In Serbia, legally binding documents, VOS (2002) and PPRS (2010), provide the concept for the water supply of the population and industry by regional systems for which water is provided by building high dams and formation of reservoirs. With this concept, it is often not possible to meet the needs of local communities in mountainous areas. In order to contribute to solving the water supply problems of these mostly poor villages, research was conducted on the possibility of using check dam aggradation groundwater for this
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Johnson, Peggy A., Richard D. Hey, Michael W. Horst, and Amanda J. Hess. "Aggradation at Bridges." Journal of Hydraulic Engineering 127, no. 2 (February 2001): 154–57. http://dx.doi.org/10.1061/(asce)0733-9429(2001)127:2(154).

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Alappat, Linto, Palaniandy Seralathan, Anil Shukla, Kyth Thrivikramji, and Ashok Singhvi. "Chronology of red dune aggradations of South India and its Palaeo-environmental significance." Geochronometria 40, no. 4 (December 1, 2013): 274–82. http://dx.doi.org/10.2478/s13386-013-0118-5.

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Abstract Red sand dunes occur in the coastal plains of south east and west of Tamil Nadu, India between the coordinates of 8°00′ to 9°30′ N; 77°18′ to 79° 00′ E. OSL dating of these sands indicated aggradations between ∼16-9 ka and ∼9-3 ka in the west and east coasts respectively. Dating results from inland red dunes at the foothills of Western Ghats show a break in deposition at ∼6 ka and aggradation since ∼2 ka. The sand aggradations in the west coast occurred during the transition period when SW monsoon in the area was reestablishing. The dunes attained their stability by 9 ka. In the coast
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Treat, Claire C., and Miriam C. Jones. "Near-surface permafrost aggradation in Northern Hemisphere peatlands shows regional and global trends during the past 6000 years." Holocene 28, no. 6 (January 19, 2018): 998–1010. http://dx.doi.org/10.1177/0959683617752858.

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The history of permafrost aggradation and thaw in northern peatlands can serve as an indicator of regional climatic history in regions where records are sparse. We infer regional trends in the timing of permafrost aggradation and thaw in North American and Eurasian peatland ecosystems based on plant macrofossils and peat properties using existing peat core records from more than 250 cores. Results indicate that permafrost was continuously present in peatlands during the last 6000 years in some present-day continuous permafrost zones and formed after 6000 BP in peatlands in the isolated to disc
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Humlum, Ole. "Holocene permafrost aggradation in Svalbard." Geological Society, London, Special Publications 242, no. 1 (2005): 119–29. http://dx.doi.org/10.1144/gsl.sp.2005.242.01.11.

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Vandermaelen, Nathan, Koen Beerten, François Clapuyt, Marcus Christl, and Veerle Vanacker. "Constraining the aggradation mode of Pleistocene river deposits based on cosmogenic radionuclide depth profiling and numerical modelling." Geochronology 4, no. 2 (December 15, 2022): 713–30. http://dx.doi.org/10.5194/gchron-4-713-2022.

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Abstract. Pleistocene braided-river deposits commonly represent long periods of non-deposition or erosion that are interrupted by rapid and short aggradation phases. When dating these sedimentary sequences with in situ-produced cosmic radionuclides (CRNs), simple concentration depth profiling approaches often fall short, as they assume that the alluvial sedimentary sequence has been deposited with a constant and rapid aggradation rate and been exposed to cosmic radiations afterwards. Numerical modelling of the evolution of CRNs in alluvial sequences permits one to account for aggradation, non-
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Pelletier, J. D. "The linkage between hillslope vegetation changes and late-Quaternary fluvial-system aggradation in the Mojave Desert revisited." Earth Surface Dynamics Discussions 2, no. 1 (March 24, 2014): 181–213. http://dx.doi.org/10.5194/esurfd-2-181-2014.

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Abstract. Valley-floor-channel and alluvial-fan deposits and terraces in the southwestern US record multiple episodes of late Quaternary fluvial aggradation and incision. Perhaps the most well constrained of these episodes took place from the latest Pleistocene to the present in the Mojave Desert. One hypothesis for this episode, i.e. the paleo-vegetation change hypothesis (PVCH), posits that a reduction in hillslope vegetation cover associated with the transition from Pleistocene woodlands to Holocene desert scrub generated a pulse of sediment that triggered a primary phase of aggradation dow
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Pelletier, J. D. "The linkages among hillslope-vegetation changes, elevation, and the timing of late-Quaternary fluvial-system aggradation in the Mojave Desert revisited." Earth Surface Dynamics 2, no. 2 (August 21, 2014): 455–68. http://dx.doi.org/10.5194/esurf-2-455-2014.

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Abstract. Valley-floor-channel and alluvial-fan deposits and terraces in the southwestern US record multiple episodes of late-Quaternary fluvial-system aggradation and incision. Perhaps the most well-constrained of these episodes took place from the latest Pleistocene to the present in the Mojave Desert. One hypothesis for this episode – i.e., the paleovegetation-change hypothesis (PVCH) – posits that a reduction in hillslope vegetation cover associated with the transition from Pleistocene woodlands to Holocene desert scrub generated a pulse of sediment that triggered a primary phase of aggrad
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Tamang, Sagar Kumar, Wenjun Song, Xing Fang, Jose Vasconcelos, and J. Brian Anderson. "Framework for quantifying flow and sediment yield to diagnose and solve the aggradation problem of an ungauged catchment." Proceedings of the International Association of Hydrological Sciences 379 (June 5, 2018): 131–38. http://dx.doi.org/10.5194/piahs-379-131-2018.

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Abstract. Estimating sediment deposition in a stream, a standard procedure for dealing with aggradation problem is complicated in an ungauged catchment due to the absence of necessary flow data. A serious aggradation problem within an ungauged catchment in Alabama, USA, blocked the conveyance of a bridge, reducing the clearance under the bridge from several feet to a couple of inches. A study of historical aerial imageries showed deforestation in the catchment by a significant amount over a period consistent with the first identification of the problem. To further diagnose the aggradation prob
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Hereford, Richard. "Modern Alluvial History of the Paria Rver Drainage Basin, Southern Utah." Quaternary Research 25, no. 3 (May 1986): 293–311. http://dx.doi.org/10.1016/0033-5894(86)90003-7.

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Stream channels in the Paria River basin were eroded and partially refilled between 1883 and 1980. Basin-wide erosion began in 1883; channels were fully entrenched and widened by 1890. This erosion occurred during the well-documented period of arroyo cutting in the Southwest. Photographs of the Paria River channel taken between 1918 and 1940 show that the channel did not have a floodplain and remained wide and deep until the early 1940s. A thin bar (<50 cm), now reworked and locally preserved, was deposited at that time. Basin-wide aggradation, which began in the early 1940s, developed floo
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Dissertations / Theses on the topic "Aggradation"

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Townsend, Kirk F. "A Chronostratigraphic Record of Arroyo Entrenchment and Aggradation in Kanab Creek, Southern Utah." DigitalCommons@USU, 2015. https://digitalcommons.usu.edu/etd/4492.

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Arroyos are entrenched channels characterized by near-vertical walls of alluvium and flat channel bottoms. Historic channel entrenchment in the southwest United States during the late AD 1800s and early 1900s has stimulated extensive research on these dynamic fluvial systems. The near-synchronous episodes of arroyo entrenchment and aggradation in Kanab Creek and other drainages in southern Utah during the last ~1 Ka has led many researches to argue that hydroclimatic forcings drive arroyo processes. These hypotheses remain largely untested, and there remains considerable uncertainty regardi
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Shaffner, Adam Levis. "SPECIFIC GAGE ANALYSIS ON THE LOWER WHITE RIVER, ARKANSAS." OpenSIUC, 2012. https://opensiuc.lib.siu.edu/theses/1009.

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This study documents the stage adjustments in the Lower White River between 1931 and 2012 at four rated gaging stations along the trunk stem of the river. The study reach extends from Calico Rock, Arkansas, to the confluence of the White River with the Mississippi River north of Arkansas City, a distance of about 509 km. The specific gage approach was used to track hydrological response in the study reach. In order to approach spatial homogeneity across the four gaging locations along the study reach, input discharges were normalized to multiples of mean daily flow (MDF). Specific gage analysi
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Vecsei, Adam Vecsei Adam Vecsei Adam. "Aggradation und Progradation eines Karbonaplattform-Randes : Kreide bis Mittleres Tertiär der Montagna della Maiella, Abruzzen /." Zürich : [s.n.], 1991. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=9550.

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Clauson, Karen D. "Measuring Trends In Riverbed Gradation: A Lower Mississippi River Case Study." OpenSIUC, 2009. https://opensiuc.lib.siu.edu/theses/75.

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The trends of degradation and aggradation are measured in this study for the Lower Mississippi River. Historical riverbed elevation and stage data from the past hundred years were used from six gages in order to measure changes in riverbed gradation. It was found that using stage data to measure gradation changes is a superior method to using riverbed elevations, due to stage data’s reliability, length of record and daily measurements. Degradation in the Lower Mississippi River was seen during the
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Summa, Michelle Carlene. "Geologic Mapping, Alluvial Stratigraphy, and Optically Stimulated Luminescence Dating of the Kanab Creek Area, Southern Utah." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/506.

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At the turn of the century, Kanab Creek incised 30-meters into its alluvium, leaving behind fluvial terraces and thick basin fill sediments exposed along arroyo walls. Research objectives were to determine the timing and causes of past valley-filling and arroyo-cutting episodes along a 20 km-long reach of Kanab Creek in southern Utah. Fluvial deposits were mapped at the 1:12,000 scale and sediments were described and dated using Optically Stimulated Luminescence (OSL) and radiocarbon dating. The Kanab Creek valley can be divided into a narrow, upper terraced reach and a broad lower basin f
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Hodge, Joshua B. "Hurricane Storm Surge Sedimentation on the McFaddin National Wildlife Refuge, Texas: Implications for Coastal Marsh Aggradation." Thesis, University of North Texas, 2016. https://digital.library.unt.edu/ark:/67531/metadc849751/.

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This study uses the storm surge sediment beds deposited by Hurricanes Audrey (1957), Carla (1961), Rita (2005) and Ike (2008) to investigate spatial and temporal changes in sedimentation rates on the McFaddin National Wildlife Refuge in Southeast Texas. Fourteen sediment cores were collected along a transect extending from 90 to 1230 meters inland from the Gulf Coast. Storm-surge-deposited sediment beds were identified by texture, organic content, carbonate content, the presence of marine microfossils, and Cesium-137 dating. The hurricane-derived sediment beds are marker horizons that facilita
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Zuniga, David. "Flood dynamics, hazard and risks in an active alluvial fan system threatening Ciudad Juàrez Chihuahua Mexico." Thesis, Brunel University, 2012. http://bura.brunel.ac.uk/handle/2438/13049.

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The aim of this research is to assess hazards and risks associated with flooding in the city of Juárez, northern México, where there is a flood threat from active alluvial fans from mountains to the southwest and from the Rio Grande (Bravo River) to the northwest forming the northeast border of the city. Aims of this Ph.D. were addressed processing a digital elevation model (DEM) of the study area in a GIS platform to define the several alluvial fans, and thus to examine their history and palaeohydrology. Three OSL dates in the youngest parts of the fans show ages ranging from 74 - 31 ka. Howe
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Sheridan, Mattilda. "The effects of an Alpine Fault earthquake on the Taramakau River, South Island New Zealand." Thesis, University of Canterbury. Geology, 2014. http://hdl.handle.net/10092/10253.

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An Alpine Fault Earthquake has the potential to cause significant disruption across the Southern Alps of the South Island New Zealand. In particular, South Island river systems may be chronically disturbed by the addition of large volumes of sediment sourced from coseismic landsliding. The Taramakau River is no exception to this; located north of Otira, in the South Island of New Zealand, it is exposed to natural hazards resulting from an earthquake on the Alpine Fault, the trace of which crosses the river within the study reach. The effects of an Alpine Fault Earthquake (AFE) have been extens
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Fitzgibbon, Holly Ann. "Interpretation of Whether Incision Rates in Appalachian Karst Reflect Long-term Downcutting toward a Surface Versus Subsurface Base Level." Ohio University / OhioLINK, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1289851338.

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Denlinger, Emily E. "Contribution of Hurricane Ike Storm Surge Sedimentation to Long-term Aggradation of Coastal Marshes in Southeastern Texas and Southwestern Louisiana." Thesis, University of North Texas, 2013. https://digital.library.unt.edu/ark:/67531/metadc500114/.

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Coastal marshes and wetlands are vital natural resources that offer habitats for plants and animals, serve as ecological filtration for soil and water pollutants, and act as protection for coastlines. Fishing, both commercial and sport, has a large economic impact in the study area – the Gulf Coast between Galveston Bay, TX and Oak Grove, LA. The objective of this research was to determine the contribution of Hurricane Ike storm surge sedimentation to long-term marsh aggradation in Texas and Louisiana coastal marshes. The research hypothesized that Hurricane Ike’s storm surge deposit would
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Books on the topic "Aggradation"

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Jackson, M. P. A. Centrifuge modeling of the effects of aggradation and progradation on syndepositional salt structures. Austin, Tex: Bureau of Economic Geology, University of Texas at Austin, 1988.

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Jackson, M. P. A. Centrifuge modeling of the effects of aggradation and progradation on syndepositional salt structures. Austin, TX: University of Texas at Austin, 1988.

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Conference on Missouri River Streambed Degradation, Aggradation, and Bank Erosion (1986 Omaha, Neb.). Summary proceedings, Conference on Missouri River Streambed Degradation, Aggradation, and Bank Erosion, April 2-3, 1986. Omaha, Neb. (10834 Old Mill Rd., Suite 1, Omaha 68154): MBSA, 1986.

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Eash, David A. Flood-plain and channel aggradation at selected bridge sites in the Iowa and Skunk River Basins, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Eash, David A. Flood-plain and channel aggradation at selected bridge sites in the Iowa and Skunk River Basins, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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C, Schmidt John. Aggradation and degradation of alluvial sand deposits, 1965 to 1986, Colorado River, Grand Canyon National Park, Arizona. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1988.

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Eash, David A. Flood-plain and channel aggradation at selected bridge sites in the Iowa and Skunk River Basins, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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C, Schmidt John. Aggradation and degradation of alluvial sand deposits, 1965 to 1986, Colorado River, Grand Canyon National Park, Arizona. Washington: U.S. G.P.O., 1990.

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Eash, David A. Flood-plain and channel aggradation at selected bridge sites in the Iowa and Skunk River Basins, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Eash, David A. Flood-plain and channel aggradation at selected bridge sites in the Iowa and Skunk River Basins, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Book chapters on the topic "Aggradation"

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Bowman, Dan. "Aggradation." In Principles of Alluvial Fan Morphology, 57–60. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-024-1558-2_7.

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Bull, William B. "Correlation of Fluvial Aggradation Events to Times of Global Climate Change." In AGU Reference Shelf, 456–64. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/rf004p0456.

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Elston, Donald P. "Pre-Pleistocene(?) deposits of aggradation, Lees Ferry to Western Grand Canyon, Arizona." In Geology of Grand Canyon, Northern Arizona (with Colorado River Guides): Lee Ferry to Pierce Ferry, Arizona, 175–85. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft115p0175.

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Robinson, Ruth A. J., Rudy L. Slingerland, and Jeremy M. Walsh. "Predicting Fluvial-Deltaic Aggradation in Lake Roxburgh, New Zealand: Test of a Water and Sediment Routing Model." In Geologic Modeling and Simulation, 119–32. Boston, MA: Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-1359-9_7.

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Jianheng, Xie. "Tentative Ideas for Controlling the Aggradation of the Lower Yellow River in the Near and Remote Future." In The GeoJournal Library, 339–54. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2450-5_23.

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Grötsch, J. "Guilds, Cycles and Episodic Vertical Aggradation of a Reef (Late Barremian to Early Aptian, Dinaric Carbonate Platform, Slovenia)." In Orbital Forcing and Cyclic Sequences, 227–42. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304039.ch17.

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Krautblatter, Michael. "Patterns of Multiannual Aggradation of Permafrost in Rock Walls with and Without Hydraulic Interconnectivity (Steintälli, Valley of Zermatt, Swiss Alps)." In Landform - Structure, Evolution, Process Control, 199–219. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-75761-0_13.

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Wadhawan, Sudesh Kumar. "Palaeogene–Neogene Tectonics and Continental Aggradational Basins in North-Western India: Implications for Geological Evolution of Thar Desert." In Society of Earth Scientists Series, 151–66. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-77443-5_5.

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"aggradation." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 28. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_10972.

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"aggradation…" In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 28. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_10973.

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Conference papers on the topic "Aggradation"

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Dulovicova, Renata. "CURRENT STATE OF AGGRADATION AT KOMARNANSKY CHANNEL." In 15th International Multidisciplinary Scientific GeoConference SGEM2015. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2015/b31/s12.026.

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Radice, Alessio, Barbara Zanchi, and Ehsan Heydari. "Laboratory experiments for channel aggradation in supercritical flow." In Proceedings of the 39th IAHR World Congress From Snow to Sea. Spain: International Association for Hydro-Environment Engineering and Research (IAHR), 2022. http://dx.doi.org/10.3850/iahr-39wc252171192022467.

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Jakob, Matthias, Michael Porter, K. Wayne Savigny, and Eugene Yaremko. "A Geomorphic Approach to the Design of Pipeline Crossings of Mountain Streams." In 2004 International Pipeline Conference. ASMEDC, 2004. http://dx.doi.org/10.1115/ipc2004-0239.

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Several hydrological methods are available to determine flood discharge and scour of streams at pipeline crossings. These methods are appropriate for streams dominated by purely hydrological processes, but fail where other, more hazardous processes occur within the design recurrence interval. Several investigations have shown that scour, impact and aggradation associated with debris flows, outburst floods or related phenomena may fundamentally change the parameters needed for proper pipeline crossing design. Depending on the process type, the peak discharge of the hazardous process can exceed
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Ghaly, Ashraf. "Variation of flow pattern in waterways due to degradation and aggradation." In the 3rd International Conference. New York, New York, USA: ACM Press, 2012. http://dx.doi.org/10.1145/2345316.2345356.

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Neagu, Nathalie, Ari Matmon, Yehouda Enzel, and Naomi Porat. "CONTROLS ON QUATERNARY AGGRADATION-INCISION CYCLES IN A HYPERARID WATERSHED, NORTHEASTERN NEGEV, ISRAEL." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-295906.

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Ahmed, Joshua, Jeff Peakall, Dan Parsons, and Matt Balme. "EXCEPTIONAL CHANNEL AGGRADATION ON MARS AND WHAT IT MEANS FOR WATER LEVEL RISE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358815.

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Wong, Annie, Darrell S. Kaufman, R. Scott Anderson, Nicholas P. McKay, Erik Schiefer, and Al Werner. "TIMING AND RATE OF GLACIALLY DRIVEN OUTWASH PLAIN AGGRADATION: POTHOLE LAKE, SOUTH-CENTRAL ALASKA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318986.

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Carson, Eric C., Stefanie E. Dodge, John W. Attig, and J. Elmo Rawling. "LATE MIS 3 ONSET TO LARGE-SCALE AGGRADATION ON THE UPPER MISSISSIPPI RIVER VALLEY, USA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334287.

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Sutfin, Nicholas, Ellen Wohl, Tim Fegel, and Laurel Lynch. "HOW MIGHT LOGJAMS REDUCE FLOODPLAIN FINE SEDIMENT AGGRADATION AND ORGANIC CARBON STORAGE IN MOUNTAIN STREAMS?" In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359381.

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Massey, Matthew A. "PLEISTOCENE FLUVIAL INCISION, AGGRADATION, AND SLACKWATER DEPOSITION ASSOCIATED WITH THE LICKING RIVER IN NORTHERN KENTUCKY." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-301603.

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Reports on the topic "Aggradation"

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Pollard, W. H. Ground-ice aggradation on Fosheim Peninsula, Ellesmere Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211971.

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Weissinger, Rebecca, and Dana Witwicki. Riparian monitoring of wadeable streams at Courthouse Wash, Arches National Park: Summary report, 2010–2019. Edited by Alice Wondrak Biel. National Park Service, November 2021. http://dx.doi.org/10.36967/nrr-2287907.

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The goal of Northern Colorado Plateau Network (NCPN) riparian monitoring is to determine long-term trends in hydrologic, geomorphic, and vegetative properties of wadeable streams in the context of changes in other ecological drivers, stressors, and processes. This information is intended to provide early warning of resource degradation and determine natural variability of wadeable streams. This report summarizes NCPN monitoring of Courthouse Wash in Arches National Park (NP) from 2010 to 2019. The focus of this report is to (1) present geomorphology and vegetation data from five reaches monito
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Dechert, T. V., P. A. McDaniel, and A. L. Falen. Aggradational and erosional history of the Radioactive Waste Management Complex at the Idaho National Engineering Laboratory. Office of Scientific and Technical Information (OSTI), September 1994. http://dx.doi.org/10.2172/10191420.

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Flood-plain and channel aggradation of selected bridge sites in the Iowa and Skunk River basins, Iowa. US Geological Survey, 1996. http://dx.doi.org/10.3133/wri954290.

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