In this paper, the phenomenon
Ess appearing in the daytime ionograms at Wuchang station (114°21.5'E,30°32.7'N) during the period 1964-1973 is analysed. It is discovered that the characteristics of this daytime phenomenon
Ess are very similar to those of the nighttime phenomenon
Em called '"nighttime thick-layer of motion". It is found that: (1) the heights of both
Ess-layer and
Em-layer descend gradually and their thickness become rather thinner during the processes of their formation and development; (2) their appearance rates are independent upon the geomagnetic actively
Kp or the sunspot number R; (3) both of them mainly appear in winter and spring. Of course, their diurnal behaviour are difference the
Ess mainly appear in the afternoon while the
Em mainly appear after midnight. Therefore, It is concluded that both
Ess and
Em are conneced with the convergent null in the vertical drift velocity of ionization, i.e., these phenomena are caused by the same dynamic process in the vally region of the ionosphere.