Final answer:
The statement is false because groundwater in aquifers moves through porous spaces and is part of the hydrologic cycle, contributing to the recharge of surface water bodies.
Step-by-step explanation:
The statement 'Water stored in aquifers is stationary and does not take part in the hydrologic cycle.' is false. Groundwater, which includes water in aquifers, is an integral part of the hydrologic or water cycle. Water within aquifers moves through the porous spaces in sediments and rocks, and can eventually rejoin surface water bodies such as lakes, streams, and rivers. Furthermore, groundwater plays a crucial role in maintaining the flow of these surface water bodies, particularly during periods when there is little rainfall. This movement of groundwater helps to recharge water bodies from below. However, it is important to note that some very deep groundwater in bedrock can remain in place for a very long time, effectively making it a non-renewable resource in human time scales. Nonetheless, the majority of groundwater is indeed part of the continuous process of the water cycle.
Additionally, human activities such as the drawing up of water for drinking or irrigation can heavily influence groundwater levels. When groundwater is extracted faster than it is replenished, aquifers can become depleted, impacting the availability of fresh water for communities and ecosystems. Thus, the conservation and sustainable management of groundwater resources are crucial for long-term water security.