Field Trip - Northern Guam Lens Aquifer Jun 2014 | Página 4

Abstract This field trip takes you to four sites, each of which is a premier example of the four basic components of the Northern Guam Lens Aquifer: the tight, nonproductive volcanic basement rock that constitutes the floor of the aquifer; the porous and soluble water-bearing limestone bedrock that is the source of our drinking water; the surface catchment that captures the recharging rainwaters; and the features of the surface that control and distribute the entry of water into the aquifer. At each site, we observe and discuss the geological and hydrological properties that control the capture, storage, and production of potable water, and the opportunities and challenges faced by geologists and engineers in exploring, developing, and managing groundwater production. While traveling between sites we observe features of regional importance to groundwater development and aquifer protection. We also discuss basic facts and statistics related to drinking water production, consumption, and conservation on Guam and nationwide. Table of Contents The Northern Guam Lens Aquifer (NGLA) 6 Basic Facts 6 Water Processes 7 Surface of the Aquifer 8 Groundwater Basins and Zones of the Aquifer 9 Production and Observation Wells 10 Idealized profile of a Carbonate Island Karst Aquifer 12 Cross-section of the NGLA along the Yigo Trough 14 16 Stop 1 The Floor of the Aquifer – the Volcanic Basement Rock 18 Stop 2 The Core of the Aquifer – the Limestone Bedrock 20 Stop 3 Plumbing of the Aquifer – Surface and Internal Drainage 22 Stop 4 The Roof of the Aquifer – the Water Catchment System 4 Field Trip Map and Schedule of Stops 24 From Sustainable Yield to Sustainable Management 26 Managing Supply and Demand 28 Further Reading 30 Authors 32 Acknowledgments 33 5