細粒料含量為影響顆粒性土壤之臨界狀態參數之重要因子,但其相關研究仍無一致之理論,本研究利用反覆單剪試驗系統,將渥太華砂與麥寮砂之細粒料混合配比,並以濕搗法製作試驗試體,進行K0狀態下不等向壓密不排水之單向剪動試驗,並根據試驗結果,探討與分析土壤之臨界狀態行為。研究結果顯示,在p'-τ平面上之臨界有效應力比與狀態轉換線之臨界有效應力比在細粒料含量0%至10%其斜率會隨著細粒料含量的增加而減少,而細粒料含量10%至100%範圍其臨界有效應力比隨著細粒料含量的增加僅些微增加;不排水剪力強度在細粒料含量20%至35%間有最低點存在,當細粒料含量小於該範圍時,不排水剪力強度隨著細粒料含量的增加而降低,而細粒料含量大於該範圍時,則有相反的趨勢;臨界狀態線會隨著細粒料含量的增加而降低,且傾斜趨勢漸緩,而類穩定狀態線亦有相同的趨勢,且在不同的細粒料含量下類穩定狀態線皆會比臨界狀態線低,且與臨界狀態線平行。
Fines content has been recognized as an important factor that affects the critical state soil parameters of granular soils, but no consistent correlation has been established. Undrained simple shear tests were performed on sand-fine mixtures prepared by moisture tamping method to study the critical state behavior under k0 conditions. The results show that the effective stress ratios on p'-τ plane at critical state and quasi-steady state decrease as fines content increases from 0 to 10% but only slightly increases from 10 to 100%. Undrained shear strength decreases as fines content increases from 0 to 20% and the minimum undrained shear strength observes around 20 to 35% fines content, which is in the proximity of transitional fines content. The trend reverses as fines content exceeds 35%. Additionally, fines content will lower the position of critical state line on p’-e plane and reduce the slope. Quasi-steady lines are parallel to the corresponding critical steady lines with smaller void ratios.