The only motive force sufficient to move enough water through the rock, so that it may act as an efficient denitrating site, is the force generated by the animals, mostly the worms, living in their burrows. These worms move back and forth in their burrows and in doing so they move the water in the burrows in a pulsating fashion. Many of the burrows and pores are interconnected, either intentionally or by happenstance, and these interconnections result in water movement into and out of the rock. Additionally, many of the worms and other animals in the rock pump water over themselves in their burrows. They do this to facilitate gas exchange over their gills, but the net result is a significant, constant, and moderate current through the rock. Such a current, coupled with oxygen utilization of animals in the rock, could result in the interior of the rock becoming the efficient denitrification site that it has been thought to be.