“…Finally, using a geometric mean of the two previously introduced flow rate scales ðF μ F e Þ 1=2 as a characteristic scale, we recover the scaling laws r* ∝ β Although the sizes of droplets immediately after they are created and their size distribution anywhere in an aerosol produced in electrospraying can be measured readily, experimentally determining the charge of such droplets at the instance of their formation is a formidable challenge. Indeed, the droplets may (i) deform, oscillate, and break as a result of aerodynamic and other forces (2, 13, 32); (ii) interact, collide, and possibly coalesce (33) with one another and with solid surfaces; and (iii) evaporate and shrink before their charge can be measured (24). Thus, there has been considerable variation in the experimentally reported values of droplet charge.…”