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2012-10-24 KCDP Minutes Final
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2012-10-24 KCDP Minutes Final
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<br />that the monitoring of the Park be integrated with the other existing monitoring efforts <br />40 <br />being done by surrounding developments to provide more comprehensive results. <br />41 <br /> <br /> <br />A way must be found to incorporate the development wants/needs of the surrounding <br />42 <br />communities as stated in the KCDP with the protection efforts/requirements that the Park <br />43 <br />works to ensure. <br />44 <br /> <br /> <br />There is a very important aspect that to be understood, the water recharge rate and how <br />45 <br />that affects the aquifer. <br />46 <br />The meeting took a recess at 2:50 and resumed at 2:56 <br />47 <br />Department of Water Supply/Waimea Water Service <br />48 <br />Steve Bowles and David Barnes provided the Action Committee with an update of the Kona <br />49 <br />districts unique water resources and services. <br />50 <br /> <br /> <br />Knowledge is collected over time and constantly– we can plan two ways – operate in fear <br />51 <br />and regulate or we can plan in knowledge <br />52 <br /> <br /> <br />Keauhou Hydralogic refers to a calculation area and includes multiple aquifers and utilizes <br />53 <br />several factors to provide information for the sustainable yield/water resources in a certain <br />54 <br />area and are modified as new information is discovered. <br />55 <br /> <br /> <br />An important resource plan that is still relevant today is the Keauhou to Kailua Plan done <br />56 <br />in the 1991. The plan notes that potable water is being brought in from Keauhou into <br />57 <br />North Kona. There is a zone indicating the limits of a basal lens however this has now <br />58 <br />become a area for high level water drill sites. <br />59 <br /> <br /> <br />Because of lava flows from Hualalai there have been indications that there seems to be a <br />60 <br />hybrid water system in the North Kona district – where there is artisian water under <br />61 <br />pressure at a depth under tracite flows, high level water, and lower slope waters/ground <br />62 <br />basal level water. These indication leads to a tentative determination that there are <br />63 <br />multiple aquifer conditions within the Keauhou Hydralogic forming a very complex system <br />64 <br />that are still being investigated. <br />65 <br /> <br /> <br />Important information source for the sharing of current knowledge is the Kona Water <br />66 <br />Roundtable. <br />67 <br /> <br /> <br />State Water Commission has a state-wide policy of decision making based on sustainable <br />68 <br />yield (which is still being investigated/questioned) and will take over management of the <br />69 <br />aquifer unit when the pumpage reaches 90% of the sustainable yield. <br />70 <br /> <br /> <br />The development (e.g. housing) that has been established in the area re-charges the aquifer <br />71 <br />systems. The data has not been analyzed on the full impact of the re-charge to the aquifer. <br />72 <br />Questions and Comments include: <br />73 <br /> <br /> <br />Clarification of what the differences of water quality of the water from the high level water <br />74 <br />and the basal lens. <br />75 <br /> <br /> <br />Water demand needs to be determined based on two factors – meter track of existing <br />76 <br />water usage and future population growth and not based on zoning based. <br />77 <br />Page 2 of 5 <br /> <br />
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