Boundary Modification Determination and Approach Sample Clauses

Boundary Modification Determination and Approach. Based on the work and review of the basin characterizations, CHG and GSI will determine, along with District staff, whether there is merit for requesting boundary modifications from DWR for the two fringe areas under consideration. If we conclude that it is appropriate to pursue a BBMR, CHG will provide a scope of work in consultation with District staff detailing the approach (e.g., scientific vs jurisdictional, external vs internal), strategies, and analysis for a boundary modification request to include, but not limited to, the tasks outlined below. However, once the basin boundary modification requests announcement is posted, additional data and analysis may be required to be included in the application submittal(s). CHG will assist and support the District in preparing all the technical analysis of the basin boundary modification application(s) to DWR. We will need approval from the District to proceed with the scope of work that is specific to boundary modification.
Sample 1
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Boundary Modification Determination and Approach. To support a boundary modification for the Nipomo Valley and Southern Bluffs fringe areas, GSI’s approach will focus on the following lines of evidence that may be identified in the basin characterization effort: • Effects of Faults – Where upthrown fault blocks of crystalline bedrock on the northeastern side of the Wilmar Avenue fault are adjacent to aquifer strata on the southwestern side of the fault, the hydrogeologic setting may support a boundary modification effort. Where there are water-bearing strata on both sides of the fault, there may be opportunities for future aquifer testing to assess the fault’s impediment to groundwater flow. • Topographic Displacement – Uplifted terraces such as the Southern Bluffs and Nipomo Valley may have xxxxx tapping Franciscan bedrock, or may have xxxxx tapping terrace deposits that are adequate for local uses, but may be physically disconnected from the larger basin. • Synoptic Water Levels – A round of water levels collected at the same time can be used to develop a groundwater elevation topographic map. The groundwater flow direction and gradient obtained from these data can be key information in determining the quantity of underflow from an alluvial valley to the larger basin. • Synoptic Water Quality Data – Water quality sampling in both the Santa Xxxxx Valley Basin and the smaller areas considered for boundary modification may indicate distinct water chemistry, which could support a boundary modification effort. • Hydrographs – Distinct historical patterns of water levels between the Santa Xxxxx Valley Basin and smaller fringe areas could support a boundary modification effort. For example, water levels that are declining in the larger basin but are in equilibrium in the fringe areas could support the modification effort.
Sample 1

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