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Session K.pdf - Clarkson University

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17th International Symposium on IceSaint Petersburg, Russia, 21-25 June 2004International Association of Hydraulic Engineering and ResearchENSURING OF OPERATION OF WITHDRAWALSIN FRAZIL-ICE CONDITIONSI.N.Shatalina, 1 G.A.Tregub 1 , N.S.Bakanovichus 1ABSTRACTOn the rivers with a long period of ice flow, difficulties in water collecting can occur.The purpose of this paper is working out hydraulic ways of withdrawal strainer protectionagainst frazil and avoiding supercooling effect inside the system. This paper concernsdifficulties arising in the operation of river withdrawals situated in the frazil producingriver stretches. Methods of calculations of frazil flow parameters are given. Theconstruction of water strainers of umbrella-like type and system of collector well heatingon the basis of compositional resistive materials (CRM) ensuring safe operation ofwithdrawals in frazil-ice conditions are proposed. The results of experimental analysisof the new strainer construction and the parameters of the new heating system of thewater collector well are represented.METHOD OF ESTIMATION OF WATER SUPERCOOLING AND FRAZILDISCHARGE COMING INTO WITHDRAWALSOn the large rivers like the Neva and the Amur the period of autumn frazil flow cancontinue rather long, sometimes up to more than a month. In the period of frazil flowand the beginning of freezing-up there are plenty of polynyas – ‘factories of frazil’. Atthis time withdrawals can have ice difficulties connected with blocking of the strainerwindows with passing frazil and their freezing in supercooled water. The method of estimationof water supercooling and frazil discharge coming into water collectors isbased on the Pekhovich model (Pekhovich, 1983). According to this model a fewstretches along the river can be described, every of which has a definite number of icethermal parameters: 1) the stretch of water supercooling to the section of inside waterice formation; 2) the stretch going from this section to the section of frazil flowing up;3) the stretch of growing supercooling to the section of maximum supercooling ; 4) thestretch of supercooling decrease to the section of maximum intensification of inside waterice formation; 5) the stretch to the ice edge. The mentioned stretches are separatedfrom each other with distinct sections and have the definite water temperature t , its gra-1The B.E. Vedeneev All-Russian Institute of Hydraulic Engineering (VNIIG), Gzhatskaya str., 21,St.Petersburg, Russia.335

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