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Agenda - 10-21-1986
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Agenda - 10-21-1986
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Last modified
10/17/2016 12:14:57 PM
Creation date
9/26/2016 3:32:56 PM
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BOCC
Date
10/21/1986
Meeting Type
Regular Meeting
Document Type
Agenda
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-t -2- <br /> • <br /> Piedmont. Minerals withdraws 0.25 mgd, 3 or 4 days a week with none <br /> drawn the rest. Most of this is lost in process or from evaporation ,from <br /> their sediment ponds. - : <br /> . The 3.2 miles of river between Lake Ben Johnson and the wastewater outfall <br /> is the section of river most impacted by abnormal low stream flows. The <br /> Eno River. State. Park begins several miles below the outfall and has. - <br /> the river flow augmented by this approximately 0.8 mgd of effluent. Over <br /> twenty miles downstream, ' Durham, who operates a wastewater treatment plant "_ . <br /> discharging to the Eno has found its 7Q10 dropping from 2.6 cfs in the <br /> _ • <br /> early 1970's to 0.6 cfs in recent years, due totally to the out-of-basin <br /> • transfers. in the upper Eno. . <br /> From 1977 through 1985 there have been increasing times of NO flow in the <br /> Hillsborough section of the Eno, reaching over 12 weeks in 1985. This year, <br /> in recognition of the increasing impacts of these low to no--flows, a strong <br /> effort was made to assure a high flow condition, as it turned out, in the <br /> face of a potentially very serious drought condition. Reservoir management <br /> strategies were developed by Orange County with assistance from the Division - <br /> of Water REsources and ways were found to release water through the dams to <br /> maintain some stream flow. <br /> These efforts were marginally effective, in part because of opposition ._ <br /> from several sources to the maintenance of ANY stream flow, and in part because <br /> of the learning process of managing, for the first time, a reasonably complex . <br /> system of dams and water withdrawls. Water conservation regulations were <br /> proposed, established, and then modified to reduce stream flows below the <br /> 7Q10 at various stages keyed to the level of water in the Lake Orange <br /> impoundment. By early June flow had reached 7Q10. From mid June to present <br /> the daily levels have been below 7Q10, as low as 0 to 20% for many days (except <br /> for 1-2 days several times from rainfall in August). <br />
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