Jag antog alltid att det var en liknande effekt som den som ses i sandstormar i den verkliga världen, där saltning av sandpartiklarna (i detta fall framställda av sandmaskens rörelse som bryter mot ytan istället för genom vind) producerar statisk elektricitet.
As the force of wind passing over loosely held particles increases, particles of sand first start to vibrate, then to saltate ("leaps"). As they repeatedly strike the ground, they loosen and break off smaller particles of dust which then begin to travel in suspension. At wind speeds above that which causes the smallest to suspend, there will be a population of dust grains moving by a range of mechanisms: suspension, saltation and creep.
A recent study finds that the initial saltation of sand particles induces a static electric field by friction. Saltating sand acquires a negative charge relative to the ground which in turn loosens more sand particles which then begin saltating. This process has been found to double the number of particles predicted by previous theories.
(src: dammstorm )