宋晶, 王清, 张鹏, 江小亮. 2012: 高黏性吹填土固结过程中细颗粒迁移规律研究. 工程地质学报, 20(6): 1042-1049.
    引用本文: 宋晶, 王清, 张鹏, 江小亮. 2012: 高黏性吹填土固结过程中细颗粒迁移规律研究. 工程地质学报, 20(6): 1042-1049.
    SONG Jing, WANG Qing, ZHANG Peng, JIANG Xiaoliang. 2012: LABORATARY RESEARCH ON FINE PARTICLES MIGRATION OF HIGH CLAY DREDGER FILL IN CONSOLIDATION PROCESS. JOURNAL OF ENGINEERING GEOLOGY, 20(6): 1042-1049.
    Citation: SONG Jing, WANG Qing, ZHANG Peng, JIANG Xiaoliang. 2012: LABORATARY RESEARCH ON FINE PARTICLES MIGRATION OF HIGH CLAY DREDGER FILL IN CONSOLIDATION PROCESS. JOURNAL OF ENGINEERING GEOLOGY, 20(6): 1042-1049.

    高黏性吹填土固结过程中细颗粒迁移规律研究

    LABORATARY RESEARCH ON FINE PARTICLES MIGRATION OF HIGH CLAY DREDGER FILL IN CONSOLIDATION PROCESS

    • 摘要: 软土地基在真空预压过程中,受强大的真空吸力作用,产生固结压密。其中一类软土黏粒含量较大,排水固结过程中产生细颗粒迁移现象,令土体固结的同时细颗粒也积聚在排水板四周,形成泥膜,造成后期排水通道堵塞,降低了固结效率。本研究采用室内试验模拟吹填土排水固结过程,监测颗粒分布情况,探讨细颗粒迁移规律,从颗粒空间分布特征解释高黏性吹填土固结机理。研究证实,固结条件影响细颗粒迁移现象:自重沉淤固结期间,细颗粒迁移受边界条件及渗流路径影响; 加压固结期间,细颗粒迁移受附加荷载产生的垂直压力影响,随着土体含水量的减少,黏粒迁移趋势逐渐减弱,黏粒不再表现出明显的迁移趋势,土体中细颗粒分布从竖向条带状逐步转变为水平向条带状。同时,高黏性吹填土固结过程中,将土样未加分散剂测试得到的粉粒含量称为似粉粒,随着吹填土排水固结过程的持续,吹填土似粉黏比不断地增加。固结时间越长,似粉黏比随深度增加而减小的特征越明显; 与排水管水平距离较远的土体似粉黏比有所增大。似粉黏比作为吹填土固结过程的指标,与土体强度大小成正比,可间接反应强度变化规律,为确定流塑状态及软塑状态的高黏性吹填土固结程度提供了定性指标,直观地反映出土体固结程度。研究表明,随着固结排水过程的持续,排水速度减慢,吹填土粉黏比不断增加,固结程度迅速增加。

       

      Abstract: In the process of vacuum preloading consolidation, soft foundation is consolidated by powerful vacuum suction. A kind of soft clay has many fine particles that would be flowed to drain pipes with vacuum. The plastic pipes would be surrounded with clay. Then they would be formed with mud membrane. Through laboratory test, the course of drainage consolidation is simulated. It is aimed that the laws of particle migration can be resolved with the proposed approach. Test results confirm that the consolidation conditions affect the fine particle migration phenomenon. At the gravitational compaction consolidation stage, the fine particles are influenced by boundary conditions and seepage paths. However, at the pressure consolidation stage, the fine particles are influenced by the additional loading generated vertical pressure. Therefore, the tendency of particle migration is no more than weak. And The distribution of fine particles is changed from vertical gershgorim band to horizontal gershgorim band. Furthermore, the mass ratio of silt and clay is primary defined as aggregate clay ratio. It reflects the status of migration process. The aggregate clay ratio is considered as the indicator of migration. Data analysis results show that the indicator can effectively reflect the degree of consolidation. With the continuing process of consolidation drainage, the aggregate clay ratio is increasing gradually. It reflects indirectly the strength of high clay dredger fill. In the consolidation process, aggregate clay ratio is increased as the drainage velocity is changed lower.

       

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