目的:压缩性和渗透性是垃圾填埋场竖向隔离墙材料的2个重要指标。本文旨在探讨不同凹凸棒土添加量对砂-凹凸棒土隔离墙材料压缩性和渗透性的影响,并在Kozeny-Carman方程的框架下建立经验公式来预测砂-凹凸棒土隔离墙材料的渗透系数。创新点:1.系统全面地研究了不同凹凸棒土添加量对砂-凹凸棒土隔离墙材料压缩性和渗透性的影响;2.建立经验公式,预测砂-凹凸棒土隔离墙材料的渗透系数。方法:1.通过固结试验和刚性壁渗透试验,得出不同凹凸棒土添加量对砂-凹凸棒土隔离墙材料压缩性和渗透性的影响(图3和4,表1);2.通过公式推导,建立经验公式来预测砂-凹凸棒土隔离墙材料的渗透系数(公式(3)和(4))。结论:1.压缩指数(Cc)和回弹指数(Cs)均随回填料中凹凸棒土含量(Ap)的增加而增大,且Cc和Cs与Ap均有很好的线性关系:Cc=0.0062Ap+0.0161(r2=0.9914),Cs=0.0009Ap-0.0058(r2=0.9888)。2.用Casagrande和Taylor方法计算的固结系数(Cv)值均随回填料中凹凸棒土含量的增加而降低。3.利用太沙基固结理论计算的回填料渗透系数(ktheory)随回填料中凹凸棒土含量的增加而降低;在有效固结压力σ′<100 k Pa的情况下,只有凹凸棒土含量Ap≥30%,ktheory才会低于10-9 m/s;用刚性壁渗透试验测得的渗透系数kf与ktheory有相同的变化特征。4.基于试验数据提出了2种预测砂-凹凸棒土回填料渗透系数的方法,其中方法 2更好;由于这些方法都是经验公式,所以它们能否应用于原位场地或其它类型回填料仍需进一步的研究。
The radial sand ridge system （RSRS） located at Jiangsu coast of China attracts much attention on its origin and mechanic of formation for its special structure and potential land resource. Due to complicated hydrodynamic condition, the Jiangsu RSRS is a hot debated on its potential sources, Yangtze River or Yellow River？ We collected ten sand samples from surface sediments along the west coast of Bohai Sea and Yellow Sea from the modern Yellow River estuary to Yangtze River estuary in summer, 2013. The samples are analyzed by method of detrital zircon age for source identification of the RSRS sediments. The U-Pb age spectra of detrital zircon grains of the samples show a wide range from Cenozoic to Late Archean with several age peaks. Comparing the age spectra between the Yangtze River and the Yellow River, the detrital zircons have younger age （〈100 Ma） group in the Yangtze River. These age distribution of the Jiangsu coastal RSRS sediments are similar to that of the Yangtze River, but different from the Yellow River. The samples located adjacent to the old Yellow River Delta show more wide-range age distribution, implying a compounded origination from the both rivers. Based on these findings it is proposed that, contrary to common opinion, the main sediment source of the Jiangsu RSRS is the Yangtze River, rather than the Yellow River. By implication, there should be evidence of hydrodynamic mechanics of oceanic currents and tidal motion. This aspect awaits confirmation in future research.
The Jianggang Harbour-centered radial sand ridge(RSR) is the largest sand body in the Yellow Sea. Its formation and evolution are of interest for scientists of various fields; however, the sediment provenance is uncertain. In this study, rare earth element(REE) geochemical compositions of the RSR sediments together with their potential sources are investigated to identify the provenance of the RSR sediments. The typical parameters((La/Yb)_N,(La/Sm)_N and(Gd/Yb)_N) as well as the upper continental crust-normalized patterns of REEs can only be associated with source rocks, and thus can be used as effective tracers for the origin and sources of sediments. However, the REE contents of sediments are affected by many factors, such as particle sorting and chemical weathering. Onshore RSR sediments are different in REE geochemical composition from offshore RSR sediments to some extent, suggesting that not all of the offshore RSR sediments have the same sources as the onshore RSR sediments. Meanwhile, the sediments adjacent to the northeast of Cheju Island and at Lian Island near the Lianyun Harbour were not the source of the RSR sediments due to their distinctive REE patterns, dEu,(La/Yb)_N,(Gd/Yb)_N and(La/Sm)_N. The Korean river sediments could be dispersed to the Jiangsu Coast slightly impacting the fine fractions of the RSR sediments, particularly the offshore RSR sediments. Additionally, geochemical comparisons show that the modern Yellow River was responsible for the onshore RSR sediments, whereas the sediment loads from the Yangtze River could serve as a major contributor to the RSR, particularly the offshore RSR. In addition, the offshore RSR could also be partly fed by an unknown source due to some high values of(La/Yb)_N,(La/Sm)_N and La contents differing from those of the Chinese and Korean river sediments.
