Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Since the images selected for the comparison were taken in August of both 1989 and 1999, it <br />was possible to make a distinction between center pivot sprinklers that were actively irrigating <br />and those that were not active by the color of the image within the parcel. For comparison <br />purposes, it was assumed the circular parcels that were less red or even gray color in the <br />August images had been used to irrigate wheat that had previously been harvested. The <br />circular parcels that were brighter red color were assumed to be actively irrigating spring crops <br />such as corn. <br /> <br />Ideally, interpretation of satellite imagery should also be done in conjunction with site-specific <br />field inspection to verify the satellite imagery. This field inspection could not be done since the <br />Landsat photos were obtained prior to the actual study. However, for general comparison <br />purposes, the satellite imagery and the Baca County Assessor's office both show an increase in <br />the number of acres being irrigated and the crop selections that are being irrigated in the <br />District. The Baca County assessor's office shows 52,900 acres irrigated in 1989 and 106,300 <br />acres in 1999. Data also indicates more water was being used in the District in 1999 than was <br />being used in 1989. <br /> <br />5.2 ESTIMATED WATER USE <br />The ability to determine the amount of water actually being withdrawn from the aquifers <br />depends upon either direct measurement or approximation. Examples of direct measurement <br />include flow data obtained directly from wells that are either equipped with totalzing flow meters <br />or hour meters if the rate of discharge of the well is already known. The approximation method <br />utilizes equations and climatological data to estimate the volume of water required. These two <br />methods can be used together to provide accurate estimates of the overall pumpage for an <br />area. One method of estimating water demand is based upon the Blaney-Criddle method with <br />climatological input data from local sites. <br /> <br />The source of the crop coefficients used in the Blaney-Criddle formula are from the "Irrigation <br />Water Requirement Technical Release No. 21 If developed by the USDA's Soil Conservation <br />Service. Two sites within the District, Springfield and Walsh, which have climatological data, <br />were selected for this analysis. Springfield was selected because it has a longer period of data <br />and associated climatological averages than Walsh. Walsh was selected because it is <br />approximately twenty miles east of Springfield making it more centrally located and more nearly <br />the same elevation within the irrigated area of the District. In addition, Springfield is <br />approximately 600 feet higher in elevation than Walsh. <br /> <br />The estimated monthly and seasonal irrigation requirements per acre using the Blaney-Criddle <br />method were multiplied by the number of acres of the four major crops being irrigated to <br />estimate the peak monthly demand and seasonal demand to fully supply the respective <br /> <br />V-2 <br />