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Formation, growth and variability of sand spit at Rushikulya River mouth, South Odisha coast, India

机译:Rushikulya河口,印度南奥迪沙河口的沙子吐制,增长和变异

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Sand spits are depositional landform and most active features near the coastal bays and inlets. The combine interactions between the wind, wave transformation, tidal variation, availability of sediment and river discharge decide the spit morphology, growth and orientation. The beaches around Rushikula river inlet is known as one of the largest rookeries of the olive ridley turtle. The spatial and temporal evolution of the sand spit, geomorphology changes and sediment distribution based on the data collected during 2005-2011 at different time intervals on the both sides of the inlet are assessed. Shoreline oscillation and geomorphology are monitored using real time global positioning system (RTK-GPS). The shoreline undergoes natural phases of erosion and deposition process, however, the entrapment of huge longshore sediment during southwest monsoon months near the river inlet triggers northerly progression of the sand spit and small temporary islands that are highly conducive for formation of nesting habitat. Sediment samples (n=210) collected at different transects representing fore, mid and backshore are analyzed to understand the role of grain size in erosion/ accretion process.
机译:沙唾液是靠近沿海湾和入口附近的沉积地貌和最活跃的功能。沉积物和潮汐变化,沉积物和河流排放的可用性之间的相互作用决定了吐痰形态,生长和方向。 Rushikula River Inlet附近的海滩被称为橄榄渣龟的最大新手之一。基于在入口两侧的不同时间间隔的基于2005 - 2011年期间收集的数据的砂吐,地貌变化和沉积物分布的空间和时间演变。使用实时全球定位系统(RTK-GPS)监测海岸线振荡和地貌。海岸线经历了侵蚀和沉积过程的自然阶段,然而,在河口入口附近的西南季风月内捕获巨大的龙岸沉积物触发了对灌木吐痰和小临时岛屿的北进展,这是对形成筑巢栖息地的形成。分析了在不同横断的不同横断波上收集的沉积物样品(n = 210),以了解晶粒尺寸在侵蚀/增齿过程中的作用。

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