Main Title |
Study of reutilization of wastewater recycled through groundwater / |
Author |
Boen, Doyle F.,
|
Other Authors |
|
Publisher |
United States Environmental Protection Agency, Office of Research and Monitoring, |
Year Published |
1972 |
Report Number |
EPA16060-DDZ-07/71; EPA 600-R-71-007; W7208982 |
OCLC Number |
00447923 |
Subjects |
Water reuse--California--San Jacinto River Valley ;
Artificial groundwater recharge ;
San Jacinto River Valley (Calif)
|
Additional Subjects |
Water reuse--California--San Jacinto Valley ;
Water, underground--Artificial recharge
|
Internet Access |
|
Holdings |
Library |
Call Number |
Additional Info |
Location |
Last Modified |
Checkout Status |
EJBD |
EPA 600-R-71-007 |
v.1 |
Headquarters Library/Washington,DC |
08/07/2019 |
EJBD |
EPA 600-R-71-007 |
v.2 |
Headquarters Library/Washington,DC |
08/07/2019 |
EJBM |
TD429.B63 |
|
Headquarters Library/Washington,DC |
03/22/2010 |
EJDD |
EPA-600/R-71-007 |
v.1 |
Env Science Center Library/Ft Meade,MD |
03/14/1997 |
ELBD ARCHIVE |
EPA 600-R-71-007 |
Received from HQ |
AWBERC Library/Cincinnati,OH |
10/04/2023 |
EMBD |
WPCR 16060 DDZ 07/71 |
|
NRMRL/GWERD Library/Ada,OK |
06/10/1994 |
|
Collation |
2 volumes : illustrations, maps, charts, plans ; 28 cm |
Notes |
"July 1971." "Eastern Municipal Water District, Hement, California." Includes bibliographical references. |
Contents Notes |
Volume 1. Volume I -- Volume 2. Volume II. A project to demonstrate the feasibility and safety of recycling water under operating conditions was performed in the Hemet-San Jacinto Valley of the State of California. Since the Valley is a closed basin, and is dependent in part upon imported water, it was felt that recycling of the water would ultimately lead to a reduction in the salt input and resultant degradation of the existing underground reservoir. The project added considerable knowledge and experience to the technology of intermittent wastewater percolation and associated monitoring techniques. A novel feature of the project was the employment of highly sensitive temperature probes to trace the lateral migration of the recharged water, much of which appears to be escaping as shallow underflow to the San Jacinto River and hence not reaching the deep groundwater table. |