Littérature scientifique sur le sujet « Erosion-sedimentation Balance »
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Articles de revues sur le sujet "Erosion-sedimentation Balance"
Nada, I. Made, I. Wayan Redana, I. G. B. Sila Dharma et A. A. Gde Agung Yana. « Model Penataan Lahan Penanggulangan Erosi Berbasis Masyarakat Di Kawasan Danau Batur ». Bumi Lestari Journal of Environment 18, no 1 (1 février 2018) : 1. http://dx.doi.org/10.24843/blje.2018.v18.i01.p01.
Texte intégralNada, I. Made, I. Wayan Redana, I. G. B. Sila Dharma et A. A. Gde Agung Yana. « Terasering Mekar Erosion Control Model in Batur Lake Zone ». International Journal of Contemporary Research and Review 10, no 01 (16 janvier 2019) : 20254–59. http://dx.doi.org/10.15520/ijcrr.v10i01.642.
Texte intégralNada, I. Made, I. Wayan Redana, IG B. Sila Dharma et A. A. Gde Agung Yana. « Community-based erosion control model in Batur Lake zone ». MATEC Web of Conferences 276 (2019) : 04008. http://dx.doi.org/10.1051/matecconf/201927604008.
Texte intégralNada, I. Made, Ida Bagus Suryatmaja et I. Gusti Ngurah Alit Wiswasta. « MODEL PENANGGULANGAN SEDIMENTASI DANAU BERBASIS MASYARAKAT DI PULAU BALI ». Bumi Lestari Journal of Environment 17, no 2 (1 août 2017) : 100. http://dx.doi.org/10.24843/blje.2017.v17.i02.p02.
Texte intégralTorrecillas, Cristina, Carmen Zarzuelo, Jorge de la Fuente, Bismarck Jigena-Antelo et Gonçalo Prates. « Evaluation and Modelling of the Coastal Geomorphological Changes of Deception Island since the 1970 Eruption and Its Involvement in Research Activity ». Remote Sensing 16, no 3 (29 janvier 2024) : 512. http://dx.doi.org/10.3390/rs16030512.
Texte intégralFoerst, M., et N. Rüther. « Measuring bank retreat in fluvial environments with Terrestrial Laser Scanning (TLS) ». Earth Surface Dynamics Discussions 1, no 1 (19 novembre 2013) : 951–72. http://dx.doi.org/10.5194/esurfd-1-951-2013.
Texte intégralLi, Yongshan, Xiaopeng Jia, Haibing Wang, Jian Wang et Qimin Ma. « Shrinking Desert Channel Response to Increasing Human Interferences and Changing Natural Factors in the Upper Yellow River ». Water 15, no 24 (8 décembre 2023) : 4226. http://dx.doi.org/10.3390/w15244226.
Texte intégralOutridge, P. M., R. W. Macdonald, F. Wang, G. A. Stern et A. P. Dastoor. « A mass balance inventory of mercury in the Arctic Ocean ». Environmental Chemistry 5, no 2 (2008) : 89. http://dx.doi.org/10.1071/en08002.
Texte intégralEric, DIANGONE, AKOBE Apie Colette, Amani Etché Mireille, MONDE Sylvain et COULIBALY Aoua. « MORPHOLOGICAL EVOLUTION OF THE BOTTOM OF THE POTOU LAGOON OVER THE LAST TEN YEARS (COASTAL ZONE OF COTE D'IVOIRE) ». International Journal of Research -GRANTHAALAYAH 8, no 10 (23 octobre 2020) : 37–46. http://dx.doi.org/10.29121/granthaalayah.v8.i10.2020.1588.
Texte intégralPandey, Alok Kumar, Sharad Kumar Tripathi et Avijit Mahala. « An Appraisal of Soil Erosion in Dehradun Valley ». Journal of Scientific Research 66, no 05 (2022) : 09–11. http://dx.doi.org/10.37398/jsr.2022.660502.
Texte intégralThèses sur le sujet "Erosion-sedimentation Balance"
García, Marcelo. « Évolution oligo-néogène de l'Altiplano occidental (arc et avant-arc du Nord du Chili, Arica) : tectonique, volcanisme, sédimentation, géomorphologie et bilan érosion-sédimentation ». Grenoble 1, 2001. https://theses.hal.science/tel-00546057.
Texte intégralThe oligo-neogene geodynamic evolution of Altiplano, at the latitude od "Codo de Arica", is characterised by an important compressive defonnation and volcanism. In the eastern part of the chain (Bolivia), the shortening is weIl documented (190-280 km), and it explain a very thick crust (65 km). However, in the western part, the geological history is not weIl known and in part controversial. The study of the Arica region, on three regional transects (to scale 1:50. 000), permit to propose a representative model for the geodynamic evolution of the western Altiplano. The Oligocene (-35-26 Ma) is characterised by fluvial sedimentation, recorded in the deeper part of the Central Depression. The deposits, up to 500 m thickness, cover a topographically smooth regional unconformity. They are polymictic and provene from the East, from the erosion of a proto-Cordillera Occidental. They are cut by subvertical west-vergent faults. The Late Oligocene-Early Miocene (26-19 Ma) is a period of intense effusive and explosive volcanism. To the East (Cordillera Occidental), the volcanic arc is represented by a maximum of 2. 500 m of andesites, dacites and rhyolitic ignimbrites, with alluvial and Iacustrine intercalations. This arc, very actif, was asociated to formation of collapse calderas. To the West (Precordillera and Central Depression), the fore-arc deposits are represented by up to 1. 000m of rhyolitic ignimbrites (extra-caldera), with fluvial and lacustrine intercalations. In the Coastal Cordillera, oligo-miocene alluvial sedimentation is recorded in restricted bassins (<200 m thickness). Throughout this cycle, no evidence has been found for important tectonic compressive activity, except in a gentle folding in the Cordillera Occidental. The Neogene (--18-0Ma) is characterised by a andesite-dacitic volcanism, mainly effusif, developed in the Cordillera Occidental with a modest volume respect to the previous period. This volcanism was coeval of restricted fluvial syntectonic sedimentation. The deformation is represented by a west-vergent thrusts and folds system, involving the basement, and with a minimum shortening estimate to he 7 km. This deformation developed essentially in the west part of the Cordillera Occidental, between 18 and 5 Ma with Plio-Quaternary little reactivations. This implies a velocity of horizontal shortening, during Neogene, close to 0,54 km/Ma. In the Central Depression, during Miocene, fluvial and lacustrine sedimentation is represented by a maximum of 350 m of volcanoclastic deposits, which provene from the East. Close 12 Ma, the fluvial sedimentation ceased and a regional pedimentation surface developed. Afetr it, the fore-arc was afected by strong incision (down to 1. 000 m) concentrated in a few valleys. The event would he associated to a regional climatic change, which have induced the desiccation of Atacama, coeval with an eustatic descent (maximum of 200 m). During Late Miocene-Quaternary, however, the incision is not only explain by exogene phenoma. Therefore, un major uplift (--800 m) of the fore-arc is infered. The uplift and marine abrasion have generated an abrupt coastal cliff, and in the incised valleys produced important ground-mass collapses. The coeval deformation ofthe fore-arc is located at the fault and gentle tlexure-folds associated to the blind propagation of the subvertical faults, which induce important vertical displacement (up to 850 m) and negligeable shortening (up to 100 m). The uplift of the Precordillera produced between 12 and 10 Ma, and it has been followed by a giant gravitational collapse. The Oligo-Neogene volcanic rocks ofArica are high-potassium calc-alkaline, and its composition do not vary significantly with time. However, we note an increasing enrichment of lithophiles elements, a more important participation of gamet as residual phase in the lower crust, and a relative decreasing ofthe partial fusion rate in the mantle source. On the other hand, the structural evolution and the erosion-sedimentation balance show that the Cordillera Occidental of Arica region bas been uplif and exposed to erosion since Eocene. In the considered period (Oligo-Neogene), the crustal thickning of the western Altiplano was slow respect to the eastern Altiplano and not only associated to the tectonic processus
Chapitres de livres sur le sujet "Erosion-sedimentation Balance"
Ash, Moumita, et Plabani Roy. « RECENT ADVANCES IN RADIOTRACER TECHNIQUES FOR SOIL EROSION AND SEDIMENTATION STUDIES ». Dans Futuristic Trends in Agriculture Engineering & ; Food Sciences Volume 2 Book 9, 232–50. Iterative International Publishers, Selfypage Developers Pvt Ltd, 2023. http://dx.doi.org/10.58532/v2bs9ch17.
Texte intégralFuller, Michael S., et Peter D. Roffers. « Erosion due to a century of road construction and maintenance at Mount Diablo State Park, California ». Dans Regional Geology of Mount Diablo, California : Its Tectonic Evolution on the North America Plate Boundary. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.1217(07).
Texte intégralActes de conférences sur le sujet "Erosion-sedimentation Balance"
Chechko, Vladimir, Vladimir Chechko, Boris Chubarenko et Boris Chubarenko. « SEDIMENT BALANCE OF THE VISTULA LAGOON ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b94303c55f9.63278465.
Texte intégralChechko, Vladimir, Vladimir Chechko, Boris Chubarenko et Boris Chubarenko. « SEDIMENT BALANCE OF THE VISTULA LAGOON ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43153db8ae.
Texte intégralRapports d'organisations sur le sujet "Erosion-sedimentation Balance"
Bradford, Joe, Itzhak Shainberg et Lloyd Norton. Effect of Soil Properties and Water Quality on Concentrated Flow Erosion (Rills, Ephermal Gullies and Pipes). United States Department of Agriculture, novembre 1996. http://dx.doi.org/10.32747/1996.7613040.bard.
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