Page 178 - Defrosting for Air Source Heat Pump
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172                                         Defrosting for Air Source Heat Pump

         FEC for an ASHP unit with a vertically installed multicircuit outdoor coil was first
         demonstrated.
            The same as the tube surface temperature shown, it could be seen from
         Figs. 6.18–6.20, that the orders of the fin surface temperature curves were different
         from that shown in Fig. 3.16 in Chapter 3. In Case 1, the order was observed at
         T 3 > T 1 > T 2 from 202 s to 220 s into defrosting. With respect to the order in Case 2,
         it was at T 3 > T 2 > T 1 from 125 s to 150 s, and at T 1 > T 2 > T 3 from 185 s to 240 s.
         When it came to Case 3, the order was at T 1 > T 2 > T 3 from 80 s to 185 s, and at
         T 1 > T 3 > T 2 from 185 s to 220 s. However, in Chapter 3, the fin temperature curves
         were always shown at T 1 > T 2 > T 3 because of the negative effects of downward-
         flowing melted frost. The same as the previous reason that tube surface temperature
         curves show, this contradictory phenomenon should be resulted from a lower FEC and
         uneven distribution of refrigerant.
            In addition, as shown in Figs. 6.18–6.20, the durations of fin surface temperature
         that reached 24°C were 235 s in Case 1, 218 s in Case 2, and 196 s in Case 3, respec-
         tively. The durations decreased with their FECs increasing. This further demonstrates
         the negative effects of a lower FEC on the RCD performance of an ASHP unit with a
         multicircuit outdoor coil.
            Fig. 6.21 presents the measured refrigerant volumetric flow rate during defrosting
         in the three cases. It was observed that the measured refrigerant volumetric flow rate
         kept fluctuating severely from 0 s to 80 s, especially during the first 40 s into
         defrosting. This was because that compressor discharge pressure increased suddenly
         at the start of an RCD operation, and the internal diameter of the EEV was very small.
         In addition, a lot of energy was consumed during defrosting at the frost-melting stage
         described in Chapter 4, with a lot of refrigerant changing phases from the gas state to
         the two-phase state. Therefore, the measured refrigerant volumetric flow rate fluctu-
         ated with severe pressure changes. When the defrosting process came into the water
         layer vaporizing stage described in Chapter 4, the pressures of compressor suction and
         discharge both increased, leading to the refrigerant volumetric flow rate change from
         increasing to decreasing. As shown in Fig. 6.21, from Case 1 to Case 3, their peak
         values came out at 180 s, 180 s, and 174 s, respectively. Here, it is further confirmed
         that the defrosting performance would be improved with a higher FEC as a defrosting
         start for an ASHP unit with a vertically installed multicircuit outdoor coil.
            Fig. 6.22 shows the variation of the measured temperature of the surrounding air
         and the measured melted frost collected in Cylinder C during defrosting in the three
         cases. Before the water was collected, the temperature of the surrounding air was
         measured. When the frost melted and flowed into the water-collecting cylinder, the
         temperature of the melted frost collected was measured. As shown in Fig. 6.22, the
         temperatures of the melted frost collected reached their lowest value at 150 s in Case
         1, 145 s in Case 2, and 135 s in Case 3, respectively. This phenomenon could also
         directly demonstrate the negative effects of a lower FEC on the RCD performance
         of an ASHP unit with a multicircuit outdoor coil. It was obvious that the temperature
         of the melted frost collected was very low, at about 0.2–0.4°C at the beginning of the
         melted frost collection. The temperatures of the melted frost collected would increase
         sharply with the heat from the surrounding air and the later high temperature melted
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