潮汐资源建模:奥尔德尼竞赛

Rajput Krishna Pal, D. N. Srikanth, Kannappan Lakshmanan
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引用次数: 2

摘要

当我们将海洋视为能源来源时,潮汐能是从海洋中提取能源的最可靠和可行的选择之一。海岸水动力背后的推力主要来自潮汐及其与不同海岸边界的相互作用,也取决于海底剖面。海底剖面和成分产生了表面粗糙度剖面,这对流动产生了阻力并改变了速度场[1]。通过将潮汐效应分解为振幅和相位组合的谐波潮汐常数,将这些复杂的特性简化到一定程度。奥尔德尼竞赛(位于奥尔德尼岛和法国海牙角之间)是可以大规模提取潮汐能的重要地点之一。在我们的研究中,海洋边界主要受8个潮汐常数(Kl, K2, M2, N2, Ol, P1, Ql, S2)的强迫,这些潮汐常数为海水提供运动。这些潮汐常数是从LeProvost潮汐数据库中预测出来的,该数据库是一组合法文件,是为全球定义的。同时,采用二次变摩擦系数函数对海床表面粗糙度进行补偿。采用基于有限元的二维模型(Advance circulation-ADCIRC)对奥尔德尼赛区的潮汐能密度进行了估算。该模型与在新加坡某些地点收集的现场数据进行了验证,这为该模型的有效性奠定了基础。从速度场出发,推导出平均功率密度(APD)的估计,知道APD与速度值的立方成正比。模型计算的速度场和潮汐高程与实测数据比较,均在适宜的范围内。本文介绍了一种利用开源软件模型和具有最高分辨率的数据源进行潮汐能功率密度预测的独特方法。这些数据有助于在偏远的海洋位置定位较高的潮汐能站点,从而有助于将部署成本降至最低。
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Tidal Resource Modeling: Alderney Race
When we consider sea as a source of energy, tidal energy is one of the most assuring and doable options for extracting energy from the sea. The thrusting force behind the coastal hydrodynamics comes majorly from tides and their interaction with diverse coastal boundaries and it also depends on the seabed profile. The seabed profile and composition give rise to a surface roughness profile which creates a drag force on the flow and modifies the velocity field [1]. These complex characteristics are simplified to a certain level by dividing the tides effect into certain harmonic tidal constants which occurs as a combination of amplitude and phase. Alderney Race (between the islands of Alderney and the cape of La Hague, France) is one of such vital locations where tidal energy can be extracted at a large scale. In our study, the ocean boundaries are mainly forced by 8 tidal constants (Kl, K2, M2, N2, Ol, P1, Ql, S2) that provide motion to ocean water. These tidal constants are predicted from the LeProvost Tidal Database which is a set of legi files and was defined for the entire globe. Also, a quadratically varying friction coefficient function was employed to compensate for the seabed surface roughness. A finite element based 2-dimensional modeling (Advance circulation-ADCIRC) was conducted to estimate the tidal energy density in the region of Alderney Race. This model was validated with the field data collected at certain locations in Singapore and this formed a base for the validity of this model. The estimation of the average power density (APD) is derived from the velocity field, knowing APD to be proportional to the cube of the velocity value. The velocity field and tidal elevation calculated by the model are within the suitable limits as compared with the field data. This paper introduces a unique way of forecasting tidal energy power density using the open source software models and data sources with a maximum level of resolution. The data helps to site the higher tidal energy sites in a remote ocean location and thereby helps to minimize the deployment costs.
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