3. Who is Chris Brown? – A bit of Academic History Graduated HS in 1987 and earned full-tuition academic scholarship to Temple U; Graduated Temple in 1991 and won senior civil engineering student & senior project awards; Went to Villanova for Masters Degree at night and graduated in 1997; Worked full-time and carried full academic load at UF to earn Ph.D.
4. Who is Chris Brown? – A bit of Work History Worked for U.S. Army Corps of Eng in Philadelphia from 1991 to 1999; Worked for Corps in Jacksonville from 1999 to 2006; Worked for Golder from 2006 to present; ??
6. Technical Expertise Communication Skills Leadership Skills MY PROFESSIONAL DEVELOPMENT MODEL Led me to go back to Villanova and then UF; This in turn pointed me to my Research interests….
7. ASR and CCS My interest in ASR and CCS was Prompted by my love of Groundwater hydrology….. ASR CCS
8. What is ASR ? Source: Groundwater or Surface Water Recovered Water to Users Or Environment Surficial Aquifer
9.
10.
11.
12. ASR Project Data Seattle, WA Portland, OR Salem, OR Beaverton, OR Calleguas, CA Alamogordo Highlands Ranch, CO Denver South, CO Myrtle Beach, SC Charleston, SC Hilton Head, SC Tampa Palm Bay Peace River Hialeah Boynton Beach International Sites Lytchett Minster, England Windhoek, Namibia Andrews Farm, Australia Clayton, Australia Washoe County, NV Salt Lake City, UT Lancaster, CA Las Vegas, NV Norfolk, VA Chesapeake, VA Wildwood Willunga, Australia Bolivar, Australia ## Northern India Florida Sites Broward County Lee County Olga Springtree Delray Beach Eastern Hillsboro Fiveash Manatee Rd Huron, SD Ankeny, IA Green Bay, WI Oak Creek, WI Lee County Cocoa Beach Ft. Myers St. Lucie Shell Creek Wichita San Antonio
4 4 About 60% of the ASR sites store surface water following treatment, and the remainder store groundwater from other aquifers, or the same aquifer at a different location. Storage zones are usually confined aquifers, but a few are unconfined shallow aquifers. Storage zone depths range from 200 ft to 2600 ft. Storage zone lithologies include sand, sandstone, clayey sand, limestone, dolomite, glacial drift, alluvial, basalt, … Bubbles of stored water usually don’t extend more than a few hundred feet around each ASR well, and they tend to stay close to the well during storage and recovery. Natural groundwater movement is usually just a few feet per year.
Possible reactions that may occur near and away from the borehole
ASR is by no means a trivial component of the Restudy The Restudy team correctly made some conservative assumptions regarding the level of pretreatment prior to ASR storage. Lessons learned from operational testing of the pilot ASR systems will allow refinement of these treatment assumptions. Aeration will increase dissolved oxygen
ASR is by no means a trivial component of the Restudy The Restudy team correctly made some conservative assumptions regarding the level of pretreatment prior to ASR storage. Lessons learned from operational testing of the pilot ASR systems will allow refinement of these treatment assumptions. Aeration will increase dissolved oxygen
ASR is by no means a trivial component of the Restudy The Restudy team correctly made some conservative assumptions regarding the level of pretreatment prior to ASR storage. Lessons learned from operational testing of the pilot ASR systems will allow refinement of these treatment assumptions. Aeration will increase dissolved oxygen
Sources & Notes: All data is for 2000. All calculations are based on CO2 equivalents, using 100-year global warming potentials from the IPCC (1996), based on a total global estimate of 41,755 MtCO2 equivalent. Land use change includes both emissions and absorptions; see Chapter 16. See Appendix 2 for detailed description of sector and end use/activity definitions, as well as data sources. Dotted lines represent flows of less than 0.1% percent of total GHG emissions.
Sources & Notes: WRI based on IEA, 2004b. Shares are based on gigawatt hours of generation.
Carbon capture and storage is the process of collecting CO2 and potentially other greenhouse gases at source, transporting it via a variety of modes, but primarily by pipeline, and injecting the CO2 into geologic strata or deep saline aquifers.
![“ Solving our Water and Global Warming Emergencies Using Subsurface Storage” ,[object Object],[object Object],[object Object],Presentation by Chris J. Brown, Ph.D., P.E., May 2009 Dis](https://image.slidesharecdn.com/unfresearchpresentation-1285778671626-phpapp01/85/Unf-Research-Presentation-1-320.jpg)
![Who is Chris Brown? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](data:image/gif;base64,R0lGODlhAQABAIAAAAAAAP///yH5BAEAAAAALAAAAAABAAEAAAIBRAA7)