Laserfiche WebLink
<br /> <br /> <br /> <br />16 <br />soils that are expected to develop excess pore water <br />pressures due to an increased load induced by <br />construction. This case is also only applicable when <br />undrained shear strengths are estimated to be less <br />than drained shear strengths. Both upstream and <br />downstream embankment slopes are evaluated under <br />the end-of-construction loading condition. The most <br />critical construction loading condition is typically at the <br />end of construction; however, staged construction may <br />require intermediate analyses. <br />For this loading condition, embankment and <br />foundation soils are analyzed using either drained or <br />undrained shear strengths depending on the <br />permeability and saturation of the soil. Fine-grained <br />soils generally have low permeability such that little <br />drainage occurs during construction. Therefore, when <br />saturated, these soils are assigned undrained (total <br />stress) shear strengths. Laboratory tests used to <br />measure undrained shear strengths of fine-grained <br />soils include the unconfined compression (UC) test, <br />unconsolidated-undrained (UU) triaxial test, <br />consolidated-undrained (CU’ or CU) triaxial test with or <br />without pore pressure measurements, and direct <br />simple shear (DSS) test. The shear strength envelope <br />used should be consistent with the analysis method <br />employed such that strengths are calculated based on <br />confining pressure prior to construction. <br />Soils that are free-draining have relatively high <br />permeability and are assigned drained (effective <br />stress) shear strengths with the phreatic surface <br />defined by groundwater conditions. Laboratory tests <br />used to measure drained shear strengths of free- <br />draining soils include the consolidated-drained (CD) <br />triaxial test, CU’ triaxial test, and direct shear (DS) test. <br />Steady-State Drained Loading Condition <br />The steady-state drained loading condition represents <br />the long-term stability of the embankment dam under <br />normal reservoir pool steady-state seepage conditions. <br />Pore water pressures are assumed to have reached <br />their steady-state condition with no excess pore water <br />pressures remaining from construction or elevated <br />reservoir pool levels. The phreatic surface and internal <br />piezometric conditions correspond to long-term, <br />normal operating conditions with the reservoir pool <br />conservatively modeled at the maximum normal <br />reservoir level, or service/principal spillway crest <br />elevation. Typically, only the downstream <br />embankment slope is evaluated under the steady-state <br />drained loading condition. The upstream embankment <br />slope is generally not analyzed because of stabilizing <br />water pressure on the upstream face, providing a <br />buttressing effect on the embankment. However, the <br />factor of safety can be low if the upstream slope is very <br />steep. In this case, analysis of the upstream <br />embankment slope may be warranted. <br />For this analysis, all embankment and foundation soils <br />are assigned drained (effective stress) shear strengths. <br />Laboratory tests used to measure drained shear <br />strengths include the CD triaxial test, CU’ triaxial test, <br />and DS test. <br />Rapid Drawdown Loading Condition <br />This condition represents a rapid lowering of the <br />reservoir from the steady-state, normal pool to a <br />significantly lower elevation, removing the buttressing <br />effect of the reservoir. During rapid drawdown of a <br />reservoir, the rate of unloading on the upstream slope <br />is typically assumed to occur instantaneously, such <br />that pore water pressures within the embankment do <br />not have time to dissipate in fine-grained (cohesive) <br />soils. This analysis assumes the embankment soils <br />below the normal pool phreatic surface are saturated <br />to steady-state conditions prior to drawdown and will <br />remain saturated after drawdown. Given adequate <br />drainage and time, pore water pressures will <br />eventually dissipate in the fine-grained embankment <br />soils. <br />The rapid drawdown loading condition should be <br />evaluated using a three-stage slope stability analysis as <br />described by Duncan, Wright, and Brandon [2] for <br />developing appropriate phreatic and shear strength <br />parameters. The first stage of the analysis calculates <br />the stress condition based on the existing steady-state <br />seepage conditions of the embankment dam before <br />drawdown. In the first stage, the phreatic surface and <br />internal piezometric conditions correspond to long- <br />term, normal operating conditions with the reservoir <br />pool conservatively modeled at the maximum normal <br />reservoir level, and all embankment and foundation <br />soils are assigned drained (effective stress) shear <br />strengths. <br />The second stage of the analysis calculates the stress <br />condition immediately after drawdown. In this stage,