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Titlebook: CENAS; Coastline Evolution Giuseppe Gambolati Book 1998 Springer Science+Business Media Dordrecht 1998 Deltas.Erosion.Groundwater.environm

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發(fā)表于 2025-3-21 16:09:47 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱CENAS
副標題Coastline Evolution
編輯Giuseppe Gambolati
視頻videohttp://file.papertrans.cn/221/220245/220245.mp4
叢書名稱Water Science and Technology Library
圖書封面Titlebook: CENAS; Coastline Evolution  Giuseppe Gambolati Book 1998 Springer Science+Business Media Dordrecht 1998 Deltas.Erosion.Groundwater.environm
描述The Upper Adriatic Sea basin comprises a very precarious coastal environment subject to continuous changes which prove appreciable not only over the geological scale but also in historical and modern times. According to some Authors the Venice Lagoon was formed 2000-3000 years ago, and other lagoons (e. g. the Grado Lagoon in the northernmost part of the Adriatic) are even more recent. In addition to lagoons, the Upper Adriatic coastal area includes salt and fresh-water marshes and reclaimed land separated by several watercourses originating from the Alpine and Apennine ranges with a ground elevation not exceeding in many places 2 m above the mean sea l. evel (msl). A significant fraction of this lowland is already now below msl because of natural and anthropogenic land subsidence, land reclamation and sea level rise occurred over the last century. Natural land subsidence is still under way as a result of deep downward tec- tonic movement and consolidation of soils deposited in the most recent time. An- thropogenic subsidence is primarily due to groundwater pumping for agricultural, industrial, civil, and tourist use, and to gas withdrawal from a large number of gas fields scattere
出版日期Book 1998
關(guān)鍵詞Deltas; Erosion; Groundwater; environment; sedimentary basin; hydrogeology; ecotoxicology
版次1
doihttps://doi.org/10.1007/978-94-011-5147-4
isbn_softcover978-94-010-6163-6
isbn_ebook978-94-011-5147-4Series ISSN 0921-092X Series E-ISSN 1872-4663
issn_series 0921-092X
copyrightSpringer Science+Business Media Dordrecht 1998
The information of publication is updating

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https://doi.org/10.1007/978-3-642-99715-0 and the related input parameters. The area investigated by the project is 350 km long and comprises three local sites south of the Po river delta (Ravenna, Cesenatico and Rimini) where a detailed coastal study has been performed. The results indicate that a general regression of the beach is to be
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Nahrungsversorgungssysteme heute und morgenstate of the beaches. The subjects are divided into two main themes (sea works and beach structure) rather than treat each site individually. The final scope of the work is to demonstrate how structural interventions along the coasts at the selected sites and the evolution of their sandy shores have
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Evaluation: Theoretische Betrachtung,reproduce the present day sediment thickness with a small excess hydrostatic pressure since the Adriatic Sea basin in known to be normally pressured. It is assumed that sedimentation in the last 0.5 My was substantially in equilibrium with subsidence so that the deposition surface remained at a cons
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Daten- und Programmschnittstellen, effective intergranular stress, is derived from a number of oedometric tests carried out on samples cored from deep boreholes scattered throughout the Upper Adriatic Sea basin. The results predict a final maximum land subsidence due to reservoir depletion equal to 20 cm over the gas field central a
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Kapitaldienst und Selbstkosten,0 and 100 year storms are estimated. Each of these storms is simulated for the bathymetry at present and in the year 2050 and 2100. The bathymetry changes due to subsidence and sea level rise. The extreme water level at the local site of Ravenna is used to determine the return period of the storm.
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