Abstract:The possibility of exploiting low-temperature heat sources has been of great significance with ever increasing energy demand. Optimum and cost-effective design of the power cycles provide a means of utilization of low-temperature heat sources which might otherwise be discarded. In this analysis, the performance of the Kalina cycle system 11 (KCS11) is examined for low-temperature geothermal heat sources and is compared with an organic Rankine cycle. The effect of the ammonia fraction and turbine inlet pressure… Show more
“…Bombarda et al [14] conducted a comparison between the thermodynamic performances of Kalina cycle and an ORC cycle, for the case of heat recovery from two diesel engines, and the calculation results show that the quantities of net electric power produced by the Kalina cycle and the ORC are about the same. Hettiarachchi et al [16] investigated the performance of the Kalina cycle system with low temperature heat sources and found that the dual pressure KC has better overall performance at moderate pressures than that of the ORC.…”
“…Bombarda et al [14] conducted a comparison between the thermodynamic performances of Kalina cycle and an ORC cycle, for the case of heat recovery from two diesel engines, and the calculation results show that the quantities of net electric power produced by the Kalina cycle and the ORC are about the same. Hettiarachchi et al [16] investigated the performance of the Kalina cycle system with low temperature heat sources and found that the dual pressure KC has better overall performance at moderate pressures than that of the ORC.…”
“…(1) (gross power density) taken at standard conditions DT ¼ 20 C and T ¼ 300 K. The average seawater density q is taken as 1025 kg m À3 , the seawater specific enthalpy c p as 4000 J kg À1 K À1 , and the OTEC combined turbo-generator efficiency e tg as 0.75. Despite their simplicity, the proposed power formulas capture the basic behavior of OTEC systems based on pure-fluid, low temperature Rankine cycles, with thermodynamic efficiencies approximately half the Carnot limit of DT over T. If more complex cycles were considered, e.g., of the Kalina type [22], Eqs. (1) and (2) should be modified accordingly.…”
Global rates of ocean thermal energy conversion (OTEC) are assessed with a highresolution (1 deg  1 deg) ocean general circulation model (OGCM). In numerically intensive simulations, the OTEC process is represented by a pair of sinks and a source of specified strengths placed at selected water depths across the oceanic region favorable for OTEC. Results broadly confirm earlier estimates obtained with a coarse (4 deg  4 deg) OGCM, but with the greater resolution and more elaborate description of key physical oceanic mechanisms in the present case, the massive deployment of OTEC systems appears to affect the global environment to a relatively greater extent. The maximum global OTEC power production drops to 14 TW, or about half of previously estimated levels, but it would be achieved with only one-third as many OTEC systems. Environmental effects at maximum OTEC power production are generally similar in both sets of simulations. The oceanic surface layer would cool down in tropical OTEC regions with a compensating warming trend elsewhere. Some heat would penetrate the ocean interior until the environment reaches a new steady state. A significant boost of the oceanic thermohaline circulation (THC) would occur. Although all simulations with given OTEC flow singularities were run for 1000 years to ensure stabilization of the system, convergence to a new equilibrium was generally achieved much faster, i.e., roughly within a century. With more limited OTEC scenarios, a global OTEC power production of the order of 7 TW could still be achieved without much effect on ocean temperatures.
“…At present, the heat recovery from high temperature gases, as in the modern combined cycles, or in multi-megawatts coal thermoelectric plants, is monopolized by the steam Rankine cycles and the more believable application of the Kalina cycle is restricted to medium-low temperatures heat sources (typical maximum temperatures of 300-400 • C in the case of heat recovery, and 100-120 • C in the binary geothermal plants) and to small power conversion systems [8,9,10,11].…”
To cite this version:Paola Bombarda, Costante Invernizzi, Claudio Pietra. Heat recovery from Diesel engines: a thermodynamic comparison between Kalina and ORC cycles. Applied Thermal Engineering, Elsevier, 2009, 30 (2-3) This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Although the obtained useful powers are actually equal in value, the Kalina cycle requires a very high maximum pressure in order to obtain high thermodynamic performances (in our case, 100 bar against about 10 bar for the ORC cycle). So, the adoption of Kalina cycle, at least for low power level and medium-high temperature thermal 2 ACCEPTED MANUSCRIPT sources, seems not to be justified because the gain in performance with respect to a properly optimized ORC is very small and must be obtained with a complicated plant scheme, large surface heat exchangers and particular high pressure resistant and no-corrosion materials.
ACCEPTED MANUSCRIPT
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