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By Victoria M. Petrova

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1988. An introduction to boundary layer meteorology. Kluwer Academic Publishers: Norwell, MA, 666 p. , Mahrt, L. A simple model of the atmospheric boundary layer: sensitivity to surface evaporation. -Lay. Meteorol. 1986, 37, 129–148. United States Environmental Protection Agency (EPA). 0-A Relief Value Discharge Screening Model, EPA-450/4-88-024, 1989, 62 pp. Van Ulden, A. P. 1986. The spreading and mixing of a dense cloud in still air. A. Conference on Stably Stratified Flow and Dense Gas Dispersion, Oxford University Press: Chester, UK.

The main physical adsorbent classes are mesoporous silicates, zeolites, metalaluminophosphates, porous carbons and metal organic frameworks (Aristov Y. , 2011). Macroporous Pores Diameter>50 nm Microporous Pores Diameter<2 nm Porous materials Super-Misoporous 2nm>Pores Diameter>1nm Misoporous 50nm>Pores Diameter>2nm Figure 11. Porous materials classification. 1. Porous Carbons Activated carbon (AC) is another name of porous carbons with high degree of porosity (500-1500 m2/g). It is obtained by gasifying the char using an oxidizing agent and the raw material of wood, peat, coal, fossil oil, chark, bone, coconut shell or nut stone.

This cycle consists of three adsorbent-bed reactors in addition to two evaporator heat exchangers as shown in Figure 8. One of the evaporators is working at low evaporative temperature, while the other one is working at higher evaporative temperature. There are five operating modes controlled by five steps and these operating modes namely; low pressure adsorption, high pressure adsorption, desorption, preheating and precooling as 29 Adsorption Refrigeration shown in Table 4. During low pressure adsorption, the adsorbent-bed reactors are connected to the low pressure evaporator via the interconnecting valves.

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