A study of the temperature distribution in the OTEC cold water pipe using a heat and mass transfer approach

A. I. Firmansyah, Mukthasor, D. Satrio, S. Rahmawati, H. Ikhwani, W. A. Pratikto
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Abstract

The difference between sea water temperature at a depth of around 1000 m and sea water temperature at sea level is generally used as a parameter in the design of Ocean Thermal Energy Conversion (OTEC). In practice, electricity generation is determined by the difference between the temperature of the cold seawater coming out of the Cold Water Pipe (CWP) and the temperature of the seawater at the surface. The temperature of cold sea water increases due to heat transfer experienced by cold sea water flowing through the CWP, which comes into contact with surrounding sea water which has a higher temperature. This in turn provides a lower actual temperature difference, and therefore reduces the design power capacity. However, many previous studies did not consider these lower temperature differences. This may be acceptable for cases with practically small heat transfer such as CWP with low thermal conductivity combined with good insulation used in 1000 m CWP vertical floating systems. Unfortunately, this may not be the case for many of OTEC’s proposed alternative sites, which are located on land systems that require CWP lengths of five km or more. This raises the need for careful investigation to determine the temperature of the sea water coming out of the CWP, where it is necessary to calculate the temperature distribution of the cold sea water flowing through the CWP. This paper aims to estimate the temperature distribution of cold sea water flowing through the CWP and the increase in temperature of cold sea water leaving the CWP. Analysis based on the principles of mass and heat transfer was carried out in this research, where modelling was carried out numerically using a finite volume approach. For the case considered, the change in sea water temperature at CWP from depth to the surface occurs 1-3°C, which is the accumulation of each change in sea water depth. The results of this research illustrate that designing an OTEC system with a long CWP must consider the temperature distribution of cold sea water flowing through the CWP to produce a more realistic design.
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利用传热和传质方法研究 OTEC 冷水管中的温度分布
在海洋热能转换(OTEC)的设计中,通常采用 1000 米左右深度的海水温度与海平面海水温度之差作为参数。实际上,发电量取决于从冷水管道(CWP)流出的冷海水温度与海面海水温度之差。流经冷水管道的冷海水与周围温度较高的海水接触后会发生热传递,从而导致冷海水温度升高。这反过来又降低了实际温差,从而降低了设计功率容量。然而,之前的许多研究并未考虑这些较低的温差。对于热传导实际上较小的情况,如 1000 米 CWP 垂直漂浮系统中使用的导热系数低且隔热性能良好的 CWP,这种情况可能是可以接受的。遗憾的是,对于 OTEC 提议的许多替代场址来说,情况可能并非如此,这些场址位于陆地系统上,需要 5 千米或更长的 CWP。这就需要进行仔细调查,以确定从 CWP 流出的海水温度,其中有必要计算流经 CWP 的冷海水的温度分布。本文旨在估算流经化武生产厂的冷海水的温度分布以及离开化武生产厂的冷海水的温度升高情况。本研究根据传质和传热原理进行分析,并采用有限体积法进行数值模拟。在所考虑的情况下,CWP 海水温度从深度到表面的变化为 1-3°C,即海水深度每次变化的累积值。研究结果表明,在设计具有较长 CWP 的 OTEC 系统时,必须考虑流经 CWP 的冷海水的温度分布,以便设计出更切合实际的系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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