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Advances in Water Treatment and Enviromental Management

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238 WATER TREATMENTA knowledge of the recession characteristics of Lough Muckno has permitted apo<strong>in</strong>t to be identified on the recession curve which will trigger the fill<strong>in</strong>g of storageto any selected target level while guarantee<strong>in</strong>g releases throughout the fill<strong>in</strong>gsequence. It rema<strong>in</strong>s to check that the recession factor has not been significantlyaltered by the outlet works which have been constructed over the past two years,s<strong>in</strong>ce other sources (3) have found this to be the case elsewhere.The presence of substantial natural storage <strong>in</strong> Lough Muckno greatly <strong>in</strong>fluencesthe recession rates on the hydrograph at gaug<strong>in</strong>g stations downstream. From theStorage/Elevation curve on Lough Muckno, <strong>and</strong> the rat<strong>in</strong>g curve for outflow fromthe lake <strong>in</strong>to the Clarebane River, it is possible to calculate an approximate decaycurve for the lake alone assum<strong>in</strong>g no <strong>in</strong>flow from the m<strong>in</strong>or lakes <strong>and</strong> catchmentupstream, <strong>and</strong> this has also been plotted on Fig 3. In future it is the behaviour ofLough Ross at low flow that will dom<strong>in</strong>ate the response of the lower catchmentdur<strong>in</strong>g regulation periods s<strong>in</strong>ce all <strong>in</strong>flows to Lough Muckno will be completelyabsorbed <strong>in</strong> replenish<strong>in</strong>g storage depletion. While an accurate Storage/Elevationcurve for Lough Ross has not been produced, there are <strong>in</strong>dications that its “no<strong>in</strong>flow”recession factor is of the order of 0.66 for flows <strong>in</strong> the region of 20 Mli/d, <strong>and</strong> thatit is somewhat larger (0.74) for flows <strong>in</strong> the region of 7.5 Ml/d.Recession Analysis of the hydrograph at Moyles Mill, <strong>in</strong> the Lower Fane Catchment,suggests that the recession at this po<strong>in</strong>t is still dom<strong>in</strong>ated by Lough Mucknoparticularly at medium <strong>and</strong> high flows. We are now research<strong>in</strong>g the extent to whichthe recession factor of 0.88 to 0.92 recorded at Moyles Mill changes as LoughMuckno becomes a more regulated reservoir. We have prudently assumed that itwill approach the “no-<strong>in</strong>flow” calculated recession for Lough Ross but this can notbe practically tested until the system is aga<strong>in</strong> exposed to a drought which requirespump<strong>in</strong>g on Lough Muckno.We attach importance to the Recession Analysis at Lough Muckno, Moyles Mill <strong>and</strong>Stephenstown <strong>in</strong> order(a)(b)(c)to m<strong>in</strong>imise the extent of pump<strong>in</strong>g from Lough Muckno <strong>and</strong>to ensure that pump<strong>in</strong>g is commenced <strong>in</strong> good time <strong>and</strong> then discont<strong>in</strong>uedwhen refill<strong>in</strong>g has taken place to an extent that resumed pump<strong>in</strong>g shortlyafterwards is not required.to determ<strong>in</strong>e the consequences of power failure on the Clarebane River dur<strong>in</strong>gpump<strong>in</strong>g periods.The Station at Lough Muckno will be unmanned <strong>and</strong> the <strong>in</strong>tention is to carry out amajor ma<strong>in</strong>tenance clean<strong>in</strong>g of screens, pumps etc. at the end of the pump<strong>in</strong>gseason. The sequence of operation required to set the pump<strong>in</strong>g regimen <strong>in</strong> tra<strong>in</strong>,while not particularly complex, would be such that a well def<strong>in</strong>ed, reliable endpo<strong>in</strong>t to the pump<strong>in</strong>g season should be established.5. MIGRATORY FISH MOVEMENTThe Control Structure <strong>in</strong>cludes two Fish Pass Gates which will <strong>in</strong> the <strong>in</strong>itial stagesof a drought simply act to divide the level difference between lake <strong>and</strong> river <strong>in</strong>to twosteps whilst flow to the Clarebane River spills over the gates. The PLC will controlgate lip level so that a m<strong>in</strong>imum depth of flow of 200mm over the Fish Pass Gatesalways exists, irrespective of m<strong>in</strong>imum Regulation Flow.Once pump<strong>in</strong>g commences, a fraction of the pumped flow will be delivered to a FishChamber which discharges over the downstream Fish Pass Gate (Fig 5). Fish

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