groundwater 101 groundwater impacts during drought nidis – middle acf meeting – may 18,2010

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Groundwater 101 Groundwater Impacts During Drought NIDIS – Middle ACF Meeting – May 18,2010

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Groundwater 101Groundwater Impacts During DroughtNIDIS – Middle ACF Meeting – May 18,2010

Topics

Introduction – Questions about groundwater?

Recharge, Surface Water, Groundwater Interactions

Major Georgia Aquifers and Recharge Areas

Surface/groundwater interactions in varying geologic conditions

Groundwater level response to drought – recent examples

Conceptual Model of Groundwater Flow and Stream-Aquifer Interaction

Conceptual Model of Groundwater Flow and Stream-Aquifer Interaction

Source: USGS Circular 1139

Major Aquifers and Aquifer Systems

Piedmont Aquifer– Fracture Flow Dominated

Source: USGS OFR96-483

Middle ACF – Cretaceous Aquifer

Source: USGS OFR96-492

Lower ACF – Typical Floridan

Source: USGS OFR95-321

Georgia Groundwater Recharge Areas

Source: Georgia Geologic Survey

ACF Groundwater Recharge Areas

Source: Georgia Geologic Survey

Statewide Groundwater Monitoring Network, GA 2008

USGS Network About 180 continuously monitored wells (29 in real time) About 20 synoptic wells measured bimonthly

EPD is cooperator on 137 wells

Other cooperators include: City of Brunswick and Glynn County; Albany WG&L; City of

Lawrenceville; Lee County; Flint River Planning and Policy Center; and, McIntosh County

Groundwater Monitoring Network

Source: USGS Groundwater Watch

Online Data

Summary Statistics & Maps for Prior Yrs.

Source: USGS SIR 2009-5070

Surficial Aquifer

Source: USGS SIR 2009-5070

UFA: Southwestern Area

Source: USGS SIR 2009-5070

UFA: Southwestern Area (Albany)

Source: USGS SIR 2009-5070

Claiborne/Gordon Aquifer

Source: USGS SIR 2009-5070

Clayton Aquifer

Source: USGS SIR 2009-5070

Cretaceous Aquifer System

Source: USGS SIR 2009-5070

Crystalline-rock Aquifers

Source: USGS SIR 2009-5070

Conclusions

Almost all aquifers affected by drought during recent event Various factors contribute to drought response time in aquifer

Aquifer type Proximity to recharge areas Type of recharge and flowpath - “flashiness” of aquifer Compounding usage/issues (ag, municipal, over-usage, etc.) Water conservation/reuse

Recent drought showed rate of decline increased as drought progressed

Thank You - Questions?

For More Information Contact:

Joe Volpe

Golder Associates Inc.

Atlanta, GA

[email protected]

www.golder.com