Effect of the pressurized duration on improving dredged slurry with air booster vacuum preloading     

Shanwei Ke  Peng Wang  Xueyue Geng  Jun Hai  Jinqiang Jin 《Marine Georesources & Geotechnology》2020,38(8):970-979

Abstract

Compared with traditional vacuum preloading, air booster vacuum preloading is more effective at strengthening dredged slurry and improving the consolidation process. Although many engineering practices have shown that the pressurized duration has a significant effect on the reinforcement effect, there is no standard available for determining the pressurized duration. In this study, five dredged slurry samples were tested to examine the effect of different pressurized durations on the consolidation. An extensive monitoring system was used to measure the vacuum pressure, pore water pressure, settlement, and water discharge during the test, while the water content and shear strength were measured after the test. The collected monitoring data were comprehensively analyzed to evaluate the reinforcement effect. The results revealed that the pressurization system can be used to reinforce deep dredged slurry and make the whole soil layer more homogeneous. If the pressurized duration is too short, the dissipation of pore water pressure is too little to achieve the pressurization effect. If the pressurized duration is too long, too much gas will be in the soil and enter the vacuum system, which will significantly reduce the vacuum pressure and thus the reinforcement effect. Based on these findings, the optimal pressurized duration was obtained.  相似文献   

Delimitation of Urban Growth Boundary Based on the Coordination of Ecology and Residential Activity Spaces: A Case Study of Jinan,China     

JIA Kun  ZHANG Chao  YANG Yanzhao  YOU Zhen 《资源与生态学报(英文版)》2019,10(5):518-524

Delimitation of an urban growth boundary (UGB) can effectively curb disorderly urban expansion, optimize urban development space and protect the ecological environment. Eco-environmental sensitivity was evaluated and areas prohibiting construction expansion were extracted by establishing an index system. Point of interest (POI) and microblog data were utilized to analyze the expansion of residential activity space. Urban space expansion potential was calculated using a comprehensive evaluation model, and an urban growth boundary for Jinan in 2020 was delimited combining the predicted urban expansion scale. The results showed that: (1) An evaluation of eco-environmental sensitivity can effectively protect ecological land and provide an ecological basis for urban expansion. Regions with high eco-environmental sensitivities in Jinan are located along the banks of the Yellow River and Xiaoqing River and in southeast mountainous areas, but eco-environmental sensitivities in the central, north and southeast areas are relatively low; (2) The model to evaluate urban residential activity expansion can quantify the spatial distribution of urban residents' activities. Regions with high potential for residential activity space expansion in Jinan are mainly concentrated in the middle of Jinan and most are part of existing built-up areas and surrounding areas; (3) The method that delimits urban growth boundaries based on the coordination of ecology and residential activity space is reasonable. Spatial expansion in Jinan mainly extends towards the east and west wings, and the boundary conforms to the spatial strategy guiding Jinan’s development and is consistent with the overall layout in related plans. Considering both ecological protection and the internal forces driving urban expansion, the method of urban growth boundary delimitation used in this study can provide a reference and practical help for studies and management of urban development in the new era.  相似文献   

火成岩体在现今陆坡形态调整中的作用：来自南海东沙群岛近海陆坡的启示     

梁超  解习农  王华  钟广见  刘恩涛  孙鸣  易海  秦春雨  曹海洋  何杰  赵彦璞 《海洋学报(英文版)》2019,38(5):109-117

对从南海东沙群岛近海陆坡（水深约500-3100m）采集到的二维地震剖面提取地形数据后进行统计学分析,结合地震相研究,发现研究区陆坡形态的变化与火成岩体,以及与火成岩体相关联的沉积过程存在着紧密地联系。共识别出了3种陆坡类型：（a）发育多个火成岩体的粗糙、陡的陆坡（类型1）;（b）发育单个火成岩体的较为光滑、平缓的陆坡（类型2）;（c）无火成岩体发育的光滑并且平缓的陆坡（类型3）。这些火成岩体形成于南海海底扩张之后,具有较为复杂的形态,在地震剖面上多表现为强振幅的杂乱反射。在类型1中,多个火成岩体将陆坡分为上部的两个或者多个次凹和下部的一个主凹,这些凹陷可以同时被沿坡流带来的沉积物充填。然而在类型2中,单个火成岩体将陆坡为一个上部的次凹和一个下部的主凹,只有当上部的次凹被沉积物填满后,沉积物才可以开始充填主凹。类型3为发育斜坡沉积的正常陆坡。研究区现今的陆坡形态是由于火成岩体的侵入和与火成岩体相关的沉积过程所共同导致的陆坡形态调整的结果。三种陆坡类型现今陆坡形态间的差异指示不同的沉积条件和陆坡形态调整。  相似文献   

盐度对变化2014年东北太平洋“暖泡”的作用   总被引：1，自引：0，他引：1  

智海  林鹏飞  张荣华  柴菲  刘海龙 《海洋学报(英文版)》2019,38(9):24-34

A significant strong, warm "Blob"(a large circular water body with a positive ocean temperature anomaly)appeared in the Northeast Pacific(NEP) in the boreal winter of 2013–2014, which induced many extreme climate events in the US and Canada. In this study, analyses of the temperature and salinity anomaly variations from the Array for Real-time Geostrophic Oceanography(Argo) data provided insights into the formation of the warm"Blob" over the NEP. The early negative salinity anomaly dominantly contributed to the shallower mixed layer depth(MLD) in the NEP during the period of 2012–2013. Then, the shallower mixed layer trapped more heat in the upper water column and resulted in a warmer sea surface temperature(SST), which enhanced the warm"Blob". The salinity variability contributed to approximately 60% of the shallowing MLD related to the warm"Blob". The salinity anomaly in the warm "Blob" region resulted from a combination of both local and nonlocal effects. The freshened water at the surface played a local role in the MLD anomaly. Interestingly, the MLD anomaly was more dependent on the local subsurface salinity anomaly in the 100–150 m depth range in the NEP.The salinity anomaly in the 50–100 m depth range may be linked to the anomaly in the 100–150 m depth range by vertical advection or mixing. The salinity anomaly in the 100–150 m depth range resulted from the eastward transportation of a subducted water mass that was freshened west of the dateline, which played a nonlocal role.The results suggest that the early salinity anomaly in the NEP related to the warm "Blob" may be a precursor signal of interannual and interdecadal variabilities.  相似文献   

急性低盐度胁迫对可口革囊星虫存活、Na+/K+-ATP酶及磷酸酶活力的影响     

游出超  董兰芳  曾梦清  蒋艳  许明珠  张琴 《海洋科学》2019,43(3):82-89

为探讨低盐度急性胁迫对可口革囊星虫(Phascolosoma esculenta)的影响规律,研究可口革囊星虫对急性低盐度胁迫的响应机制,本试验先通过急性毒性试验确定可口革囊星虫96 h内对低盐度的耐受范围,再选取96 h最小死亡率盐度,研究该盐度急性胁迫下可口革囊星虫(平均体质量0.85±0.07 g)体质量、体壁含水量、Na~+/K~+-ATP酶活力以及酸碱磷酸酶活力在96 h内的动态变化。结果表明:在本试验盐度3.0～7.0范围内,可口革囊星虫24 h的最大死亡率盐度是3.0,可口革囊星虫96 h的最小死亡率盐度为7.0;可口革囊星虫死亡率随盐度降低逐渐升高,但相同盐度下随着时间延长,可口革囊星虫死亡率基本不变,可口革囊星虫96h内能耐受的最低盐度是7.0;在低盐度7.0胁迫下,可口革囊星虫体质量和体壁含水量在12 h内显著增大(P0.05),12 h后趋于平稳(P0.05);Na~+/K~+-ATP酶活力也在6 h内显著升高至最大值(P0.05),6 h至12h又显著降低(P0.05),此后稳定在高于对照组水平;酸性磷酸酶和碱性磷酸酶活力变化趋势与Na~+/K~+-ATP酶活力类似,均是先显著升高(P0.05)后显著降低(P0.05),最后稳定在高于对照组水平。以上研究表明,可口革囊星虫能够通过Na~+/K~+-ATP酶、酸碱磷酸酶等渗透和免疫相关的生理调节机制,迅速响应低盐度环境,其对低盐度有很强的适应力和耐受力。  相似文献   

长江河口河槽近期沉积特征及影响因子分析     

李一鸣  张国安  游博文  李占海 《地理学报》2019,74(1):178-190

随着流域和河口水利工程建设,长江河槽沉积环境发生了巨大改变,对河势演变和河槽冲淤均产生重要影响。依据长江河口河槽大面积表层沉积物采样和各河槽定点水文观测资料,分析各河槽沉积特征,探讨其影响因子及作用机制。结果表明:河槽沉积物类型以砂质粉砂和粉砂质砂分布最广,粒径分布纵向上呈自西向东减小、横向上自北向南减小趋势,河槽总体主槽粗、边滩细。涨落潮泥沙输运和沉降过程影响河槽纵向沉积分布特征,风浪作用强化了口门段河槽南北沉积环境的差异,北支、北港口门段河槽受到偏北方向风浪作用强烈,沉积物粗化明显。不同泥沙来源是造成河槽整体沉积环境差异的主导因素,南支、南港上段表现为流域来沙的沉积特征,北港、南槽、北槽则表现为流域与海域来沙的混合沉积特征,口外沉积物对口内河槽的影响主要是为口内河槽提供细颗粒物质来源。  相似文献   

舟山海洋微塑料污染源头治理机制建设初探          下载免费PDF全文

季扬沁  尤仲杰  何力 《海洋开发与管理》2019,36(11):75-81

海洋微塑料污染2004年才被英国科学家发现并提出,至今已经成为世界最受关注的生态环境问题之一。课题组认为公众是海洋微塑料污染的最主要源头。因此课题组立足舟山海域微塑料污染情况,包括塑料垃圾(资源)处理等情况,基于对公众认知的调查问卷,尝试描述以公众为核心、联合各行为主体的海洋微塑料污染源头治理机制,同时提出机制建立条件、困境与未来。此外,课题组关注社区、公益组织和市场的相应行为,力求在未来更为关注政府行为。  相似文献   

精密单点定位在建立海岛礁大地基准中的应用研究     

陈娜  尤宝平  邓孟真  崔杨 《海洋测绘》2019,39(2):26-29

为探究精密单点定位(PPP)技术用于海岛礁大地基准建立的可行性,将PPP解算的坐标结果及其经过历元和框架转换后的坐标结果,分别与其2000国家大地坐标系(CGCS 2000)的已知坐标进行比对分析。结果表明,经过历元和框架转换后的PPP坐标结果与CGCS 2000坐标仅存在厘米级的差异,能够满足布设海控一级点的精度要求,可为PPP技术用于我国海岛礁大地基准的建立提供参考依据。  相似文献   

Bacterial communities fluctuate in abundance and diversity under simulated oil-contaminated seawater conditions     

LI Xiaohong  YOU Cai  QU Liang  ZHOU Bin  TANG Xuexi  XIAO Hui 《海洋湖沼学报（英文）》2019,(2):615-627

Marine bacteria have recently been identified as a potent solution for petroleum hydrocarbon degradation in response to hazardous oceanic oil spills. In this study, a mesocosm experiment simulating a petroleum spill event was performed to investigate changes in the abundance, structure, and productivity of bacterial communities in response to oil pollution. Cultured heterotrophic bacteria and total bacteria showed a consistent trend involving an immediate decrease in abundance, followed by a slight increase, and a steady low-level thereafter. However, the changing trend of bacterial productivity based on bacterial biomass and bacterial volume showed the opposite trend. In addition, the density of oil-degrading bacteria increased initially, then subsequently declined. The change in the bacterial community structure at day 0 and day 28 were also analyzed by amplified ribosomal DNA restriction analysis (ARDRA), which indicated that the species diversity of the bacterial community changed greatly after oil pollution. Alphaproteobacteria (40.98%) replaced Epsilonproteobacteria (51.10%) as the most abundant class, and Gammaproteobacteria (38.80%) became the second most dominant class in the whole bacterial community. The bacterial communities in oil-contaminated seawater (32 genera) became much more complex than those found in the natural seawater sample (16 genera). The proportion of petroleum-degrading bacteria in the oil-contaminated seawater also increased. In this study, culture-dependent and culture-independent approaches were combined to elucidate changes in both bacterial productivity and community structure. These findings will contribute to a better understanding of the role that bacteria play in material cycling and degradation in response to oil pollution.  相似文献   

琼东南盆地深水区钻井岩屑稀土元素地球化学特征及其对沉积物源和环境的指示     

姜龙杰  孙志鹏  翟世奎  刘新宇  尤丽  曹佳琪  张爱滨  毕东杰  张婉 《海洋科学》2018,42(4):89-100

对琼东南盆地深水区YL19A钻井岩屑样品进行了稀土元素(REE)地球化学特征分析,旨在研究琼东南盆地深水区的沉积物源及古环境变化。钻井岩屑样品的球粒陨石标准化REE配分模式总体呈轻稀土(LREE)富集、重稀土(HREE)亏损的右倾式,但在各时代地层之间表现出一定的差异。崖城组和陵水组岩屑呈明显的Eu正异常,而梅山组、三亚组和黄流组岩屑呈Eu的弱负异常,指示了沉积环境和沉积物源上的变化。在早渐新世时期,研究区物源以来自周边凸起的火山碎屑和陆源碎屑为主,沉积环境为海陆过渡相;自渐新世晚期开始,随着琼东南盆地全区发生海侵,研究区水深逐渐加大,沉积环境由海陆过渡相变为浅海相,物源变为远源陆源物质,并具有红河与海南岛多物源混合的特征,红河沉积物对物源的贡献相对较大,基性火山物质对物源的贡献减弱。YL19A钻井岩屑的REE地球化学特征在距今30、28.5、25.5和23.8Ma等地层界面处均发生明显的突变,对区域性构造运动事件有明显的响应。  相似文献