Static batch settling behaviors of dredged and filled sediment and its steady-state macroscopic evaluation criteria
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摘要: 关于疏浚吹填泥沙的静态间歇沉降行为与机理及其稳态宏观评价标准,目前暂未深入研究。这是当今疏浚吹填泥沙地基采用真空过滤排水固结技术进行处理时无法科学判断最佳启动时间的主要原因之一。鉴于此,先对疏浚吹填泥沙的静态间歇沉降行为进行理论研究,建立了颗粒悬浮液的沉降速度与平均孔隙比的理论关系式。然后,获取典型工程现场的疏浚吹填泥沙,配制典型浓度试样,开展静态间歇沉降模型试验研究。研究结果表明:①黏粒(d<0.005 mm)含量是影响疏浚吹填泥沙静态间歇沉降行为与机理的关键因素之一;②颗粒通量最大值Gmax往往出现在试验难以测出的非常低的浓度条件下,且黏粒含量越高,越难通过试验方式测得;③对于黏粒含量为40%~60%的疏浚吹填泥沙,建议将“平均孔隙比累计变化率为60%~75%”作为静态间歇沉降稳定状态的宏观评价标准。Abstract: The static batch settling behaviors and mechanism of dredged and filled sediment and its steady-state macroscopic evaluation criteria have not been studied in depth yet. This is one of the main reasons why the optimal start-up time cannot be scientifically judged when the dredged and filled sediment foundations are treated by the vacuum filtration drainage consolidation technology today. In view of this, a theoretical study on the static batch settling behaviors of the dredged and filled sediment is conducted, and the theoretical relationship between the settling velocity of particle suspension and the average pore ratio is established. Based on the dredged and filled sediment from typical engineering sites and the configured typical concentration specimens, the experimental researches on the static batch settling model are carried out. The results indicate that: (1) The content of clay particles (d < 0.005 mm) is one of key factors affecting the static batch settling behaviors and mechanism of the dredged and filled sediment. (2) The maximum particle flux Gmax often occurs at very low concentrations that are difficult to measure experimentally. The higher the viscous content, the more difficult it is to measure experimentally the maximum particle flux during static batch settlement. (3) For the dredged sediment whose clay content is within 40% to 60%, the cumulative change rate of the average porosity ratio of 60% to 75% can be taken as the criterion for evaluating the steady state of its batch settling process.
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表 1 配制试样的基本物理指标
Table 1 Basic physical indices for preparation of specimens
试样 物理性质 界限含水率 颗粒组成/% 颗粒比重Gs 含水率/% 液限wL/% 塑限
wP/%塑性指数IP 砾粒
(角砾)
>2.00 mm粗砂
2.00~0.50 mm中砂
0.50~0.25 mm细砂
0.25~0.075 mm粉粒
0.075~
0.005 mm黏粒
<
0.005 mmⅠ组-南沙 2.712 380 50.8 24.4 26.4 0.00 0.00 1.45 20.75 37.10 40.70 Ⅱ组-惠州 2.703 548 56.9 40.6 30.3 0.00 0.00 1.25 0.90 36.95 60.90 表 2 不同条件下平均孔隙比累计变化率统计值
Table 2 Statistical values of cumulative change rate of average void ratio under different conditions
试样名称 黏粒含量/%
d<0.005 mm沉积环境 沉积筒直径 初始含水率/% 初始密度
/(g·cm-3)沉积时间
/d初始孔隙比 沉积稳定时孔隙比 平均孔隙比累计变化率/% 南水北调东线—淮安四站 53.4 淡水+海水 3.1 cm 424.0 1.140 30 11.53 3.51 69.6 53.4 淡水+海水 3.1 cm 530.0 1.110 30 14.42 3.53 75.5 南水北调东线—白马湖 47.0 海水 3.2 cm 380.0 1.149 80 10.07 5.992 40.5 47.0 淡水+海水 3.2 cm 570.0 1.102 80 15.105 6.548 56.7 47.0 淡水+海水 3.2 cm 760.0 1.078 80 20.14 6.599 67.2 47.0 淡水+海水 3.2 cm 950.0 1.063 80 25.175 6.678 73.5 47.0 海水 4.3 cm 369.5 1.150 21 10.1 6.1 39.6 47.0 海水 5.3 cm 369.5 1.150 21 10.1 5.7 43.6 47.0 海水 6.0 cm 369.5 1.150 21 10.1 5.7 43.6 天津滨海新区 47.0 海水 高2 m
直径80 cm400.0 1.120 366 11.6 3.2 72.4 I组南沙试样 40.7 海水 高1.3 m
直径33.4 cm380.0 1.150 240 10.311 2.714 73.7 II组惠州试样 60.9 海水 高1.3 m
直径33.4 cm547.0 1.115 240 14.667 5.331 63.7 -
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