Most sedimentation compression lines are located above the intrinsic compression lines ; their locations depend on the sedimentation condition and the action after sedimentation 大多數(shù)天然粘土的沉積壓縮曲線位于重塑土固有壓縮曲線的上方,其位置取決于沉積條件和沉積后的作用。
The sedimentation compression lines , intrinsic compression lines can be normalized by a void index , then the difference of the structural clays and reconstituted clays are showed 天然粘土的沉積壓縮曲線、重塑土的壓縮曲線可以用孔隙指數(shù)來歸一化,它清晰地顯示出結(jié)構(gòu)性土和重塑土的內(nèi)在差別。
Most sedimentation compression lines of natural clays are located above the intrinsic compression lines of reconstituted clays ; theirs locations are dependent on the sedimentation condition and the action after sedimentation 大多數(shù)天然粘土的沉積壓縮曲線位于重塑土固有壓縮曲線的上方,其位置取決于沉積條件和沉積后的作用。
The sedimentation compression lines of natural clays , intrinsic compression lines of reconstituted clays and oedometer compression curves can be normalized by a void index , then the difference of the structural clays and reconstituted clays as well as the gradual damage course of soil structure are showed apparently 用孔隙指數(shù)來歸一化天然粘土的沉積壓縮曲線、重塑土的壓縮曲線和固結(jié)儀壓縮曲線,可以很清晰地揭示出結(jié)構(gòu)性土與重塑土的內(nèi)在差別、固結(jié)儀試驗中土體結(jié)構(gòu)性的漸進破壞過程。