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Numerical Simulation for Dehydration of Natural Gas using Joule Thompson Cooling Effect

机译：焦耳汤姆逊冷却效应对天然气脱水的数值模拟

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Tay Wee Horng; Lau Kok Keong; Shariff Azmi Mohd;
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1. Numerical simulation of the influence of flue gas discharge patterns on a natural draft wet cooling tower with flue gas injection [J] . Li Hong-Wei, Wu Kui-Bo, Wang Suo-Bin Applied thermal engineering: Design, processes, equipment, economics . 2019,第期

机译：烟道气注射烟道湿冷冷却塔对天然湿冷塔影响的数值模拟
2. Numerical simulation of nanodroplet generation of water vapour in high-pressure supersonic flows for the potential of clean natural gas dehydration [J] . Wen Chuang, Ding Hongbing, Yang Yan Energy Conversion & Management . 2021,第Mara期

机译：清洁天然气脱水潜力的高压超声波流量中纳米蒸汽的数值模拟
3. Numerical Simulation of an Industrial Absorber for Dehydration of Natural Gas Using Triethylene Glycol [J] . Dagde Kenneth Kekpugile, Akpa Jackson Gunorubon Journal of Engineering . 2014,第1期

机译：三乙二醇对天然气脱水工业吸收塔的数值模拟
4. Numerical Simulation for Dehydration of Natural Gas using Joule Thompson Cooling Effect [C] . Wee Horng Tay, Kok Keong Lau, Azmi Mohd Shariff International Conference on Process Engineering and Advanced Materials . 2016

机译：焦耳汤普森冷却效应的天然气脱水数值模拟
5. Dynamic Simulation and Control of a Natural Gas Dehydration Plant Under Upset Conditions [D] . ?Haque, Md Emdadul 2020

机译：镦锻条件下天然气脱水厂的动态仿真与控制
6. Numerical Simulations of Solidification Characteristicsof Molten Slag Droplets in Radiant Syngas Coolers for Entrained-FlowCoal Gasification [O] . Bo Wang, Jianyong Qiu, Qinghua Guo, 2021

机译：凝固特性的数值模拟辐射合成气冷却器中的熔渣液滴夹带流动煤气化
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。
8. Joule-Thomson Cooling Due to CO2 Injection into Natural Gas Reservoirs [R] . Oldenburg, C. M. 2006

机译：Joule-Thomson因二氧化碳注入天然气储层而降温

Numerical Simulation for Dehydration of Natural Gas using Joule Thompson Cooling Effect

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