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Titlebook: Estuarine Morphodynamics of the Sunderbans; Gautam Kumar Das Book 2015 Springer International Publishing Switzerland 2015 Brackish Waters

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樓主: 冠軍
21#
發(fā)表于 2025-3-25 04:46:49 | 只看該作者
https://doi.org/10.1007/978-3-642-66740-4alance and depletion of mangrove vegetation with its diverse floral and faunal habitats. A comprehensive multidisciplinary approach for management of Sunderbans as well as awareness among the Sunderbans dwellers about importance of mangrove and its conservation is the need of the hour.
22#
發(fā)表于 2025-3-25 07:55:13 | 只看該作者
23#
發(fā)表于 2025-3-25 12:16:15 | 只看該作者
Mangrove Ecosystems,tem. Hydrological, biogeochemical and ecological functions of mangrove have direct bearing on socio-economic benefits of the region. The mangrove ecosystem of Sunderbans is highly disturbed due to over exploitation of mangrove forests and unplanned land use pattern.
24#
發(fā)表于 2025-3-25 18:44:55 | 只看該作者
25#
發(fā)表于 2025-3-25 23:52:04 | 只看該作者
The Slow Infection Caused by Visna Virus,d sizes. The intricate network of rivers, tidal creeks and inlets with dynamic flow pattern accelerates the process of erosion and accretion and make the geomorphic set-up of the area a complex one. The important morphotypes of Sunderbans are beaches and inlets, creeks and estuaries, mudflats, coastal dunes, sand flats and mangrove swamps.
26#
發(fā)表于 2025-3-26 01:09:02 | 只看該作者
H?kan Persson,Lennart Philipsonise the lower estuarine zone. The other conspicuous landforms are mudflats, back swamps, salt marshes, tidal creeks with mangrove, coastal dunes, beaches, tidal flats etc. Construction of embankment for protection of erosion in Sunderbans is found to have an adverse impact on the fragile ecology of the Sunderbans.
27#
發(fā)表于 2025-3-26 05:24:14 | 只看該作者
28#
發(fā)表于 2025-3-26 11:53:43 | 只看該作者
29#
發(fā)表于 2025-3-26 13:47:32 | 只看該作者
30#
發(fā)表于 2025-3-26 17:48:05 | 只看該作者
The Slow Infection Caused by Visna Virus,t block of halophytic mangrove forest. It has passed through a dynamic and complex physiographical and geomorphological history. Prograding in phases towards Bay of Bengal during Plio-Pleistocene inter-glacial period, it has left behind numerous distinctive landforms and islands of various shapes an
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