DEFORMATION OF SOILS AND DISPLACEMENTS OF STRUCTURES Х ECSMFE



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PROCEEDINGS OF ТНЕ TENTH EUROPEAN CONFERENCE ON SOIL MECHANICS AND FOUNDATION ENGINEERING / FLORENCE / 26-30 МАУ 1991 DEFORMATION OF SOILS AND DISPLACEMENTS OF STRUCTURES Х ECSMFE Editor ASSOCIAZIONE GEOTECNICA ITALIANA OFFPRINT А.А. BALKEMA / АОТТЕАОАМ / BROOKFIELD /1991

Time-settlement of а water supplying channel Tassement dependant du temps du canal adducteur T.S.GERMANOV, University of Architecture and Civil Engineering, Sofia, Bulgaria N.DIMITROV & BR.STANTCHEV, Eneгgopгoject, Sofia, Bulgaria ABSTRACT: А geotechnica1 design of а water supplying channe1 for the "Кoz1oduy" Nuc1ear Power Station has been given. The channe1 region is characterized with complicated ground conditions. Stratifications are characterized with: high ground water 1eve1; sci1s are presented by: 1ayers of organic с1ау and various consistency с1ау (at soft to stiff); fine 1оеss silty sands and 1оеss s sands (tending to 1iqиefaction under dynamic 1oads); loess - col1ausib1e and compacted by its natura1 weight; graver1y sands, grave1s etc. А detailed investigation of the soil properties has been implemented in 1aboratory conditions and in situ. Standard and non-standard soil characteristics and properties have been determined. Va1ues of sett1errent at the end of the construction and during exr1oitation have been ca1cu1ated. А geotechnica1 structure: improving the ground base and acce1erating the consolidation process has been suggested. RESUМE: Il est donne un project geotechnique du саnа1 adducteur de lа centra1e atomiqиe de "Кoz1odoui". La region du саnа1 est avec dfs conditions terrestres соmрliques. Les stratifications se characterisent par: un haut niveau de 1'еаu scuteraine; les soils sont presantes par:des couches d'argi1e organiqиe et d'argi1e de differentes consistances; des sables, fins silteux (d'une tendance de liquefaction sons des charges dinamiques) 1оеss - donnant lieu а des effondrerrent et соmрасtе par sons propre poid; des sable de grains moyens, graviers et d'outres. Il est effectur une investigation detai11e des proprietes des sols au 1aboratoire et in-situ. Sont determinesdes characteristiqиes et proprietes du sol standarts at non-standart. Sont саlсu1еs les valeurs du tassement en fin de construction et pendant 1 'exp1oitation. Une structure geotechnique de reinforcerrent de la base terrestre et d'acce1eration de lа consolidation est proposee. 1 INTRODUCTION А basic problem for the accelerated putting into operation of reactor б in the "Kozloduy" Nuclear Power Station is to insure its safety. This is of significant importance for the energy crisis in Bulgaria to be overcome. Apart from the technical problems concerning the reactor's safe work it is necessary that additional technical water supply be constructed for а short period of time (Fiq.1) The existing problems made it necessary for this project to be taken into consideration first: The existing problems made it necessary for this project to be taken into consideration first: 413 Figure 1. Situation of new water supplying for the Nuclear Power Station "Kozloduy" NR6 - nuclear reactor 6 HC - hot channel CH - cold channel 1.The existing channels, connecting the other reactors to the Danube river, constructed by retaining earth dam walls were damaged in 1988 and this necessitated urgent repair works. 2. Soil conditions are extremely complicated. The new hydrotechnical channels permanent way is

directed South-North and passes through the Danube floodplain. The soil and hydraulic conditions are characterized with а number of phenomena and processes as: -high groundwater level, partly confined groundwater: -collapse due to wetting with or without additional load of loesses layers which causes short time differential settlements; -thixotropy of some silty and fine-grand ey sands which under dynamic loads and great hydraulic gradients turn into liquefaction conditions; -swampy regions under long-term and high groundwater head. 3. Earthquake intensity, according to the macro land register in Bulgaria is VII (Richter scale). The variety in soil stratification can be seen on Fiq.2. improved soil base. 2 SOIL PROPERTIES 2.1 Standard tests Using а number of boreholes, soil samples and standard penetration tests the soil properties of 37 cross sections to а depth of 18 m have been investigated. The total new channels longitude is 2.75krn. Laboratory and in situ investigations have been done in order to determine the physical and mechanical properties of soils. Design soil characteristics are seen in table 1. Table 1. Soil characteristics stra type ρ Е tum of 0 g/cm No. soil MPa ϕ'. 0 о Soft 1 silty Soft 2 organic 3 Fine sand 1.60 15. 26 с' MPa k m/d 1.76 6.0 13 0.013 0.0104 1.89 5.2 18 0.03-0.0014 2 х10 3 4 Gravel 1.70 23. 30-50х10 3 5 Stiff silty 2.0 24. 20-0.0001 Modulus of linear deformations (Е 0 ) is determined by trial loading in situ and shear strength parameters (ϕ and с') by unconsolidated undrained test. The other physical parameters density of soil (ρ), permeability coefficient (k) and consistency-using standard tests. Figure 2. Typical soil sections The energy crisis in Bulgaria supposes that the hydrotechnical channels be constructed for а very short period. А reinforced concrete structure has been taken permitting prefabricated units to be used. The main problem in these complicated soil conditions is to minimize the deformations along and across the channel. This necessitated the working out of geotechnical design considering the effect of time as well as geotechnical structure design over an 413 2.2 Non-standard tests The solving of the mixed problem of the consolidation theory considering creeping of the soil skeleton has been used for the best time settlement forecast (Germanov 1988). This necessitated longterm tests for the determination of settlement parameters according to the theory of the linear creep of layers. The methodology given in Germanov (1988) has been used. Results are shown in table 2, where m 0 and m l are coefficients of instantaneous consolidation and of creep (secondary) volume deformation; η - the parameter of creeping

speed. ТаЫе 2. stratum No. type of soil m 0 1 Soft silty 2 Soft organic МPа -1 m l МPа -1 η d 1 0.000209 0.0032 0.0603 0.000334 0.0024 0.0792 In order to evaluate the possibilities for liquefaction of saturated sands some dynamic triaxial tests at various relative densities have been implemented (Kostov 1989). In accordance with the macro seismic land register in Bulgaria channels come into an area of VII intensity of earthquake (Richter-scale) equal to coefficient of seismicity К с =0.11. Laboratory tests have been implemented based on the Seed and Idriss (1971) method where pore pressure increase is registered in the process of cyclic triaxial load. The forecast of the liquefaction phenomena of saturated sands is implemented by determination of the liquefaction factor FLs as а ratio of the cyclic load coefficient (conforming to а certain number of cycles of given seismic intensity) to the cyclic load coefficient depending on the reaction specter. The results of the laboratory investigation are given in table 3 where FLs (0.11) and FLs (0.29) are respectively liquefaction factors at coefficient of seismicity К с =0.11 and К с = 0.29 - Id - density index. Table 3. Type of sand Id (%) FLs(0.11) FLs(0.29) Loess sand 50 1.51 0.571 77 1.95 0.740 Alluvial sand 36 2.08 0.790 72 2.62 0.990 The investigation proves that at earthquake intensity of VII (Richter-scale) liquefaction of saturated sand is hardly probable. 3 TIME-SETTLEMENT OF ТНЕ BASE There are two layers of s in the base which are of low-permeability, saturated and strongly deformable. During construction and exploitation great settlement is probable which necessitates an investigation of the base consolidation. For the settlement at the end of construction and during exploitation to be determined Germanov's variants (1977 & 1979) have been used for which professional computer programs have been worked out. Clays are examined as multy-phase soil medium consisting of soil skeleton with the creeping property filled with deformable fluid due to incomplete saturation. The construction works time-table is taken according to the scheme in Fig.4 at final term of construction load 24 months. Service load is taken according to Fig.4. It is accepted in the algorithm that the full consolidation settlement of the layers of gravel and sands will come at the end of construction and timedepending will come into the stratum. Cross deformations of the base for some specific profiles where layers are of greater thickness are shown on Fig.5 The calculation results showed: Maximum general settlements of the channel base are 4-8ст which is acceptable for this kind of Structure. Relative deformations are up to the acceptable limits as well. More than 50% (for some regions to 80%) settlement will come out during construction. Fig.3. Chart of construction period 414

Due to the small thickness of the layers and the presence of bidirectional filtration values of pore pressure are low (2.3-2.5 KPa) which shows that the influence on the bearing capacity of the base could be neglected. In this way an uniform load and decreasing of deformations is guaranteed, which is а precondition for faultless exploitation of the hydrotechnical equipment in the Nuclear Power Station. Fig.4 Service load: a. Structure of channel 1 b. Load (MPa) Figure 6. Geotechnical structure for improvement of the base. 1. Lateral wall 2. Bottom of channel 3. Counter-fill 4. Groove 5. Sand-gravel mixture base 6. Sand-gravel mixture piles 0.80cm REFERENCES Figure 5. Settlement curves: 1. At the end of construction period 2. 5 years after construction 4 GEOTECHNICAL STRUCTURE FOR IMPROVEMENT ОР ТНЕ BASE Germanov, Т. 1988. Creep and ageing effects on stresses and deformations of saturated ed soils. Proc. Int. Conf. on Rheology and soil mechanics, Coventry, pp 194-203. Germanov, Т. 1977. Deformation of the soil base during construction. Stroitelstvo 12, рр 11-13, Sofia (in Bulgarian). Germanov, Т. 1979. Deformation of the soil base under high embankments. Patishta 2, рр 4-6, Sofia (in Bulgarian). Seed, Н.В. & I.M.ldriss 1971. Simplified procedure for evaluating soil liquefaction potential. Proc., ASCE. Kostov, V. 1989. Evaluating the possibility of saturated sand liquefaction. Annuare de inst. d'areh. genie eiv., Sofia, vol.xxxiv. рр 65-74 In Bulgarian). In order to accelerate consolidation during construction period and to improve the base а gravel base of 1.75т thickness and gravel piles Б of 0.80т diameter situated in chess order at а distance of 4.0m and depth of up to 5.0m have been designed (Fig.6). 415