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provide water to the test basin. The low‐pressure alarm was never triggered during the field
                       investigation.

                        2.4. MONITORING ACTIVITIES


                       The telemetry built in to the engineered water conveyance and flow control system
                       minimized the need for onsite monitoring. Nevertheless, documentation of water meter
                       readings for each test basin and maintenance of the systems was needed, especially at three
                       sites where flows into the test basin fell below the minimum threshold of the digital paddle
                       meter (approximately 25 gpm). For these three tests, routine twice‐weekly site visits by DRE
                       staff were supplemented by additional site visits by Valley District staff to document water
                       meter readings and calculate average vertical infiltration rates for time periods between
                       meter readings.

                       It is likely that recharged water reached the water table at some investigation sites during or
                       following infiltration testing. Groundwater level monitoring was conducted during testing at
                       one site (Wildwood Creek Basins), where an existing piezometer (YRP‐PZ3; constructed in
                       EX‐4) is located relatively close to the test basin, and the depth to water (104 feet‐bgs in
                       2014) is shallow enough that a measurable groundwater level response was expected.
                       Confirmation of such a water level response is useful for validating the vertical migration of
                       recharge water and inferring the degree of horizontal spreading of recharged water below
                       the test basin. Water level monitoring in existing piezometers at the Wilson Creek Basins
                       and Oak Glen Creek Basins was not performed, due to the significant horizontal distance
                       between the piezometer and test basin and relatively deep water table at both sites (272
                       and 302 feet‐bgs in 2014, respectively).

                        2.5. BEST MANAGEMENT PRACTICES

                       All field activities were conducted to ensure minimal disturbance to native vegetation and
                       minimize soil erosion along channel banks. The following site management practices were
                       implemented to satisfy requirements specified by the SBCFCD:

                            No sediments were discharged to the storm drain system or receiving waters.
                            Sediments generated on the construction site were retained.
                            No construction‐related materials, waste, spills, or residue were discharged to
                              streets, drainage facilities, receiving waters, or adjacent property by wind or runoff.
                            Non‐stormwater runoff from equipment, vehicle washing, or any other activity were
                              contained within the project site.
                            Erosion from slopes and channels were prevented.
                            Grading was not conducted during the wet season (October 1st through May 31st).
                              All erosion‐susceptible slopes were protected to prevent sediment discharge from
                              the project site. Straw wattles were used to contain temporary stockpiled soils.







                        Infiltration Testing at Eleven
                        Investigation Sites in the Yucaipa
                        Basin, Yucaipa Valley, CA                   8                   TODD GROUNDWATER

                             Yucaipa Sustainable Groundwater Management Agency - January 23, 2019 - Page 27 of 137
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