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Compliance & Closure, Inc <br /> Groundwater Sampling Protocol <br /> Latest Revision October 1999 <br /> used as indicators for assessing sufficient purging The purging parameters are measured to observe <br /> stabilization to a range of values typical for that aquifer and well Stable field parameters are recognized as <br /> indicative of groundwater aquifer chemistry entering the well Specific conductance (conductivity) meters are <br /> read to the nearest +10 umbos/cm and are calibrated daily, if possible Temperature is read to the nearest 0 I F <br /> Calibration of physical parameter meters will follow manufacturer's specifications Collected field data during <br /> purging activities will be entered on the Well Sampling Field Data Sheet <br /> In low yield formations, the well is purged such that the "standing" water is removed and the well is allowed to <br /> recharge (Normal field measurements will be periodically recorded during the purging process) In situations <br /> where recovery to 80% of static water level is estimated, or observed to exceed a two hour duration, a sample <br /> will be collected when sufficient volume is available for a sample for each parameter Attempts will be made so <br /> the well is not purged dry such that the recharge rate causes the formation water to cascade into the well <br /> In wells where free-phase hydrocarbons are detected, the free-phase portion will be bailed from the well and the <br /> estimated volume removed and recorded A groundwater sample will be collected if bailing reduces the amount <br />. of free-phase hydrocarbons to the point where they are not present in the well Well sampling will be conducted <br /> using one of the aforementioned methods depending on the formation yield However, if free-phase <br /> hydrocarbons persis throughout bailing, then a groundwater sample will not be collected <br /> Volatile organic groundwater samples are collected so that air passage through the sample does not occur or is <br /> minimal (to prevent volatiles from being stripped from the samples) sample bottles are filled by slowly running <br /> the sample down the side of the bottle until there is a positive convex meniscus over the neck of the bottle, the <br /> Teflon side of the septum (in cap) is positioned against the meniscus, and the cap screwed on tightly, the sample <br /> is inverted and the bottle lightly tapped The absence of an air bubble indicates a successful seal, if a bubble is <br /> evident, the cap is removed, more sample is added, and the bottle is resealed <br /> Chain-of-Custody <br /> Groundwater sample containers are labeled with a unique sample number, location, and date of collection All <br /> samples are logged into a chain-of custody form and placed in a chilled ice chest for shipment to a laboratory <br /> certified by the State of California Department of Health Services <br /> Sample Storage <br /> Groundwater samples coIIected in the field are stored in an ice chest cooled to 4 C while in transit to the office <br /> or analytical laboratory Samples are stored in a refrigerator overnight and during weekends and holidays The <br />