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Architecture and management of a geological repository - Andra

Architecture and management of a geological repository - Andra

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When the packages are put in place this may reduce the cell monitoring capacity as the evolution <strong>of</strong>the condition <strong>of</strong> the thermal <strong>and</strong> radiological environment may gradually reduce the reliability <strong>of</strong> thesensors on the sleeve. These conditions are less restrictive outside the buffer, which attenuates thedose rate <strong>and</strong> imposes a radial thermal gradient. Thus, the lifetime <strong>of</strong> the monitoring equipment can beextended to several decades outside the buffer.Cell sealing leads to gradual resaturation <strong>of</strong> the swelling clay in the cell plug <strong>and</strong> imposes the sametransmission constraints as those set out above for B <strong>and</strong> C cells. In addition to the bore-holetransmission options or the use <strong>of</strong> a wireless system, the concept <strong>of</strong> a spent fuel cell <strong>of</strong>fers thepossibility <strong>of</strong> routing the cables through the metal lining.As the drifts are gradually closed, the evolution <strong>of</strong> the monitoring system, which relates essentially tothe measurement transmission equipment, is identical to that described for the C cells (§ 10.3.8.4).10.3.10 The monitoring system <strong>of</strong> st<strong>and</strong>ard cellsThe distribution <strong>of</strong> the monitoring equipment proposed in the above sections are appropriate for themonitoring <strong>of</strong> a selection <strong>of</strong> control cells. The monitoring <strong>of</strong> the st<strong>and</strong>ard cells relies upon a smalleramount <strong>of</strong> equipment. It is suggested that a st<strong>and</strong>ard B cell contains fiber optic cables <strong>and</strong> aninstrumented section in the useful part <strong>of</strong> the cell. A st<strong>and</strong>ard (C or CU) cell contain the fiber optic <strong>and</strong>an instrumented section at the metal plug.10.3.11 Observation <strong>of</strong> driftsThe monitoring <strong>of</strong> drifts focuses on the main phenomena which characterises these structures, inparticular the initial deconfinement <strong>of</strong> the host rock, the formation <strong>of</strong> a damaged zone, a gradualdesaturation <strong>of</strong> the near-field, the creep <strong>of</strong> the rock <strong>and</strong> the re-pressurising <strong>of</strong> the lining.10.3.11.1 Drift observation systemThe options for the use <strong>of</strong>monitoring equipment arecomparable to those describedfor the B cells (cf. section10.3.7.1). They are based oninstrumented drift sections. Onesuch section is illustrated inFigure 10.3.19. Only the depth <strong>of</strong>the bore-holes, which makes itpossible to install a greaternumber <strong>of</strong> extensometers,differentiates it from anequivalent section <strong>of</strong> a B cell(cf. Figure 10.3.1).The sensors distributed in eightmonitoring units make it possibleto monitor the mechanicalstrength <strong>and</strong> the dimensionalstability <strong>of</strong> the structure, thehygrometric conditions in theFigure 10.3.19 Illustration <strong>of</strong> the monitoring equipmentdistribution options in a drift sectiondrift, the mechanical <strong>and</strong> hydraulic evolutions in the near-field, the evolution in the thermal field, <strong>and</strong>possibly the chemical modification undergone during the operation period.DOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM414/495

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