Analysis and Comparison of the Wells in the Pleasant Valley Area of Ventura County   -   2

2.1.3   Grimes Canyon Aquifer

Underlying the Fox Canyon aquifer is the Santa Barbara formation of Lower Pleistocene age. In places, the upper part of this formation contains a zone of highly permeable sand and gravel known as the Grimes Canyon Aquifer. In the Pleasant Valley ground-water Basin, the Grimes Canyon Aquifer occurs at depths below 1000 feet and is penetrated by only the deepest wells.


2.2   Wells Used in the Study

2.2.1   Pleasant Valley Water District Wells

Eleven wells were drilled in 1980 by the Pleasant Valley Water District. The wells were drilled using the hydraulic rotary method and were gravel packed. The wells ranged in depth from 943 to 1453 feet and were completed using wire wrap type of screen. The total length of well screen installed in these wells varied from 360 to 1060 feet.

The wells were developed using a jetting and air lift pumping technique with average times of development ranging from 40 to 60 hours per well.


2.2.2   Other Wells Used for Comparison

To compare the effect of different well screen types and lengths on the producing capabilities in the Pleasant Valley Basin, 23 other wells were chosen for analysis. These "Comparison" wells, also drilled by the hydraulic rotary method, were selected at random and represent a variety of screen types ranging from milled and punched slotted casing to shutter screen. Total depth of these wells vary from 268 feet to 1338 feet with lengths of screens from 120 to 1076 feet.

These wells were primarily developed by bailing, with development times averaging only four hours per well. The production results from these wells in general exceeded results from the Water District wells completed using wire wrap screens and developed using jetting and air lift pumping.

Figure 1 shows the location of the wells used in the study and Figure 6 (Appendix) summarizes the production properties. The Pleasant Valley Water District wells are numbered P-1 through P-11 and the comparison wells are numbered C-1 through C-24.


Back   |   R & D Home   |   Next