上海外环线浦东段(二期)沥青面层技术要点

该文对上海城市外环线浦东段 (二期 )工程沥青面层技术做了简要的介绍 ,提出了施工过程中重点考虑的因素。     

高吸水性表面环境修复剂的制备条件研究

研究了以(NH4)2S2O8—NaHSO3为引发剂,环氧氯丙烷为交联剂,淀粉和部分中和的丙烯酸(钾)、丙烯酰胺为原料进行交联接枝.在有氧状态和无氧状态下采用水溶液聚合法合成了高吸水性表面修复剂.在这两种状态下,比较了温度、引发剂用量对表面修复剂吸水率的影响,同时对单体混合物的温度变化进行了研究.     

杭州城市交通拥挤现状及对策

在分析杭州市交通供需现状的基础上,提出了规划多中心结构和混合功能区,以减少不必要的出行以及合理配置交通源,并对改善中心区交通提出切实可行的对策。     

揭阳市东山区沟口村民房墙体开裂问题研究

相邻建筑物在地基中产生的沉降总是相互影响,需要从新旧建筑物的强度、刚度、结构类型、地质情况、荷载大小等方面进行分析,从而提出对不同类型结构的处理方法。     

论海运提单的运输合同属性

通过提单的历史演变及有关立法及业务实际程序考察,论述提单的运输合同属性,更正有关立法的误会。     

从京沪高速公路（临沂段）路面大修中谈交通管制

高速公路大、中修过程中大多采用边通车,边维修的方法,因此,大、中修过程中的交通管制就显得尤为重要。以京沪高速公路路面大修(临沂段)施工过程中的交通管制为例,通过对减速距离等参数的分析,得出了交通管制与减速距离的关系,并对京沪高速公路(临沂段)大修中利用中央分隔带紧急开口绕行时交通诱导设施布置方案的安全性进行了分析与探讨。     

旅客列车发车时间域优化研究

在大量问卷调查的基础上,根据旅客对不同到发时间域选择的偏好,确定了各发车时间域旅客出行的方便系数。利用目标规划原理,以旅客出行方便程度最大为目标,构造了三级控制策略。在考虑客运站到发线能力,以及旅客列车必须在合理的时间域发车等约束条件下,建立旅客列车发车时间域的目标规划模型。利用该目标规划模型,可根据旅客列车实际运行的需要,通过变化控制策略和赋予各目标的优先因子,实现对列车发车时间域的优化。根据模型约束目标正负偏差变量,计算了各级控制策略实现程度系数。最后,以太原站始发旅客列车为实例,利用变换方案对该目标规划模型的运用进行了分析,并将目标规划优化结果和传统确定发车时间域的结果以及指派模型优化结果进行比较分析。     

新型码头钢-混凝土组合面板

基于特殊需要,提出了带型钢加劲肋的钢板-混凝土组合板这一新型组合码头面板。以加劲肋形式、组合板厚度和栓钉布置为参数,进行了9块组合板的力学性能试验。试验结果表明,通过适当地选择型钢加劲肋形式、合理地布置栓钉和确定混凝土厚度,可以保证组合作用的发挥。组合板的正截面承载力可按基于修正平截面假定的极限状态计算;组合板的变形,可在按现行钢结构设计规范计算的基础上,加上考虑界面滑移影响的附加变形值予以修正。计算值与试验值吻合较好。     

因地制宜,综合施治,务实解决街坊小区积水顽症

上海市杨浦区某些街坊小区一遇暴雨即产生严重的积水问题。通过调查研究，找出病症，提出改造方案．有效地解决了小区的积水顽症。本文结合实际，总结了若干综合技术措施和行政管理、协调手段。     

Distribution of suspended sediment in the coastal sea off the Ganges–Brahmaputra River mouth: observation from TM data

Remote sensing technique was applied to estimate suspended sediment concentration (SSC) and to understand transportation, distribution and deposition of suspended sediment in the estuary and throughout the coastal sea, off the Ganges–Brahmaputra River mouth. During low river discharge period, zone of turbidity maximum is inferred in the estuary near the shore. SSC map shows that maximum SSC reaches 1050 mg/l in this period. Magnitude of SSC is mainly owing to resuspension of the bottom surface sediments induced by tidal currents flowing over shallow water depths. The influence of depth on resuspension is farther revealed from the distribution and magnitude of SSC along the head of Swatch of No Ground (SNG) submarine canyon. During high river discharge period, huge river outflow pushed the salt wedge and flashes away the suspended sediments in the coastal sea off the river mouth. Zone of turbidity maximum is inferred in the coastal water approximately within 5–10 m depth of water, where the maximum SSC reaches 1700 mg/l. In this period, huge fluvial input of the suspended sediments including the resuspended bottom sediments and the particles remaining in suspension for longer period of time since their initial entry control mainly the magnitude of SSC. In the estuary near the shore, seasonal variation in the magnitude of SSC is not evident. In the coastal sea (>5 m water depth), seasonal influence in the magnitude of SSC could be concluded from the discrepancy between SSC values of two different seasons. Transportation and deposition of suspended sediments also experiences seasonal variations. At present, suspended sediments are being accumulated on the shallow shelf (between 5 and 10 m water depth) in low discharge period and on the mid-shelf (between 10 and 75 m water depth) during high discharge period. An empirical (exponential) relationship was found between gradual settle down of suspended sediments in the coastal sea and its lateral distance from the turbidity maximum.