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双语推荐:天津滨海地区

建立可靠的地层年代标尺对于研究滨海地区晚新生代沉积物记录的沉积环境变化、新构造运动及古气候演化具有重要意义。对位于天津滨海地区迄今所获得的最长的全取心钻孔G2(深1226m)进行了详细的磁性地层学研究,在此基础上探讨了该孔年代地层划分及其区域构造意义。结果表明,G2孔的底界年龄约为8.5Ma。其中,1226~658m为晚中新世,属馆陶组上部,658~303m属上新世明化镇组,303m以上属第四纪马棚口组、佟楼组、塘沽组和天津组,全新统天津组底界深度为19.4m。G2孔包含2个沉积速率较高(大于200m/Ma)的时期,分别为8.5~6.43Ma和3.58~3.03Ma。这2个时期与晚中新世以来青藏高原的扩展隆升在时间上有很好的可比性,指示高原隆升可能对华北地区的沉积和构造演化有重要影响。
It is of great importance to establish reliable chronologic framework in Binhai area for understanding the late Cenozoic depositional environment change, neotectonic movement and evolution history of paleoenvironment. In this paper, the authors pres-ent the magneto-stratigraphic investigation result in drill hole G2 (1226m), which is the longest drill hole in the Tianjin coastal area. On such a basis, the chronostratigraphic subdivision and its tectonic significance were also discussed. The results show that the core of this drill hole began deposition at about 8.5Ma BP. The strata of 1226~658m may be correlated to late Miocene and assigned to upper member of Guantao Formation, the strata of 658~303m belong to Pliocene Minghuazhen Formation, and the upper strata of more than 300m belong to Quaternary, including Mapengkou, Tonglou, Tanggu and Tianjin formations. The basal lower boundary of Ho-locene is identified at about 19.4m by 14C dating. Given the chronostratigraphic scal

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天津港园林绿化建设为主要研究对象,探讨在滨海重盐碱地区绿化建设过程中存在的问题及制约绿化建设可持续性的主要因素,提出依托技术创新、理念创新,“开源节流”建设节约型园林,推动生态文明建设的建议。
In this study, taking Tianjin Port landscape construction as the main research object, we discussed the main restriction factors existing in construction process of greening in the heavy saline area, searched the factors which restricting green building sustainability. Through technical innovation, more and more new technologies were used in the green construction. From the consideration of long-term development, we want to explore one way of sustainable development in the Binhai New Area landscape construction process.

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鉴于天津滨海地区地铁工程环境的复杂性和特殊性,对影响耐久性的氯离子侵蚀、硫酸盐侵蚀、杂散电流、碳化破坏和冻融破坏等主要外部工程环境因素进行了分析和阐述,主要分析了其成因、机理及现行规范中的相关规定等,为工程的耐久性设计、施工及运营提供参考借鉴。最后建议天津滨海地区地铁工程建设引入针对性的耐久性专题研究,以保证百年设计目标的顺利实现。
In view of the complexity and particularity of the subway engineering environment in Tianjin coastal area,the main external engineering environmental factors of durability are analyzed and expounded,such as chloride ion corrosion, sulfate attack,carbonation,stray current and freeze-thaw damage and so on,the causes of formation,the failure mechanism and the relevant regulations of current codes are analyzed to provide reference for the durability design,the construction and operation.Finally,it is suggested that durability study should be introduced in the engineering construction,in order to en-sure the design goal.

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旅游城市化已成为多元城市化过程中的一种重要模式,而气候条件又是旅游城市化道路的重要限制条件。基于环渤海主要滨海城市10个站点1951-2011年气温、风速、降水、相对湿度等气象数据,利用人体气候舒适度(BCMI)的计算方法,设计人体旅游气候舒适度等级标准,评价环渤海主要滨海城市不同时期气候舒适性及其差异与成因。结果表明:①环渤海滨海旅游地在一年中的6-9月处于人体气候舒适性的5级,即最为舒适;4月、5月和10月感觉凉爽,大部分人感觉舒适;②大连、锦州、丹东、营口、威海等城市夏季气候湿润、气温适中,是我国避暑疗养的旅游胜地;③潍坊(7月)、天津(7、8月)、沧州(7、8月)、滨州(7、8月)等地气温较高,舒适性较差,然而这些地区以及威海在4月、10月的人体气候舒适度要高于大连、锦州、丹东、营口、唐山,更适于旅游;④气温低、风大、干旱是环渤海滨海旅游地在非舒适期内(11月-3月)的普遍特征。
Tourism urbanization has become a kind of important mode in the process of multivariate urbanization, and the climatic condition is an important constraint. The study selects meteorological data from 10 sites in link Bohai sea coastal cities, and uses the human body climate comfort (BCMI) and human body tourism climate comfort level standards to evaluate the climate comfort in different periods and its difference and cause of link Bohai sea coastal cities. The results show that: (1) the human body comfort level of Bobai tourist destination is 5 from June to September which means the most comfort-able; April, May and October feels cool, most people feel comfortable; (2)Dalian, Jinzhou, Dandong, Yingkou, Weihai have moderate temperatures in summer, they are the summer vacation convalesce tourist resorts in our country; (3) during the July and Au-gust, the temperature is high in Weifang, Tianjin, Cangzhou and Binzhou, but in April and October the BCMI in these areas and Weihai is high tha

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通过时间基准和空间基准的连接,对PSInSAR方法进行了扩展,对覆盖华北平原约20万km2的500余景Envisat ASAR数据进行了处理,获取了该地区2006~2010年的地表沉降速率。分析表明,华北平原多个沉降中心沉降速率处于较高发展态势,从北京-廊坊-天津到任丘、沧州、泊头、衡水、德州、南宫,再到邯郸,地面沉降已连成一片;天津市的静海-滨海地面沉降最为突出,两地沉降中心区的平均沉降速率分别达到62mm/a和67 mm/a,北京东部、沧州、泊头-衡水-德州、邯郸等老沉降区的沉降速率分别达到36 mm/a、34mm/a、37mm/a、29mm/a。利用天津地区同期水准测量结果检验了本文的研究结果,差值均小于10mm,表明PSInSAR方法反演结果与水准测量获得的结果是一致的。
Estimation of processes for slow change in small scale surfaces is one of the main advantages of PSInSAR technology.We present a mathematical framework for the datum connection for time-space referencing,applying it to 500 scenes composed of Envisat ASAR images covering about 200 000 km2 of the North China Plain,obtained the rate of ground subsidence in the study area during the pe-riod of 2006-2010.The experimental results show that:(1)the multiple subsidence centers in North China Plain were still in an evolving state,connecting Beijing,Langfang,Tianjin,Renqiu,Cang-zhou,Botou,Hengshui,Dezhou,Nangong and Handan into a continuous area.(2)The most promi-nent ground subsidence was in Tianjin’s Jinghai and Binhai areas having average subsidence rates of 62mm/a and 67mm/a along the line of sight,respectively.The subsidence of the old centers,to the east of Beijing,Cangzhou,Botou- Hengshui- Dezhou,Handan,had rates of 36mm/a,34mm/a, 37mm/a,29mm/a,respectively.(3 )The experimental
区域一体化进程中政府协调机制的构建是区域合作发展中重要的问题之一,欧盟、日本、美国以及我国的长三角地区、广佛同城、天津滨海新区为我们提供了不同路径、不同模式的行政协调机制。我们应对这些模式进行比较总结,取长补短,立足现实,构建适合本地区域发展的政府协调机制。
The construction of government coordination mechanism is one of important problems in regional cooperation and development in the process of regional integration. The European Union, Japan and the United States as well as China''s Yangtze River Delta region, with the city of Guangzhou-Foshan, Tianjin Binhai New area provide different modes and pathes about administrative coordination mechanism for us. Basing on reality, we should construct local government coordination mechanisms for regional development after summarizing these models and learning from each other.

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在室内三轴蠕变试验的基础上,分析了天津滨海地区重塑饱和软黏土的非线性蠕变特性。蠕变试验采用分级加载的方式进行,利用"陈氏法"对实测数据进行处理,得到饱和软黏土在不同应力状态下的蠕变试验曲线。在此基础上,依据黏土的应力-应变、应变-时间关系,分别用Singh-Mitchell和Mesri经验模型拟合试验数据。总结拟合结果,结合滨海软黏土的蠕变特性,提出一种分段拟合的Mesri模型,在蠕变前期,模型的应力-应变关系采用双曲线函数,应变-时间关系采用幂函数;在蠕变后期,模型的应力-应变关系采用双曲线函数,应变-时间关系采用双曲线函数,以两条拟合曲线的交点作为分段拟合的分界点。对比分析表明,该方法能更好地描述具有衰减稳定特性的蠕变曲线。选取天津滨海地区原状土蠕变试验数据对该模型进行验证,拟合结果较好,由此建立了适用于具有衰减稳定蠕变特性的滨海软黏土非线性蠕变模型。
Based on the indoor triaxial creep tests, the nonlinear creep properties of the remoulded saturated soft clay in coastal area of Tianjin were analyzed. The creep tests were carried out by the step loading method, and the creep curves of the soft clay under different stress states were got by processing the measured data by Mr. Chen′s method. In addition, Singh-Mitchell model and Mesri model were respectively used to fit the test curves which are the stress-strain isochronal curves and strain-time curves. Combining with the fitting results and the creep proper-ties of the coastal clay, a piecewise fitting Mesri model was put forward. In the early stage of the creep, the hyperbol-ic function was taken to describe the stress-strain relationship, and the power function was used to describe the strain-time relationship. In the late stage of the creep, two different kinds of hyperbolic functions were respectively used to matching the stress-strain relationship and the strain-time

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气候变化引起的海平面上升将给沿海地区社会经济发展和生态环境带来严重的影响。津冀沿海地区地势低平极易受到海平面上升的直接影响,该文以津冀沿海地区为例,对海平面上升风险评估方法进行示范应用,评估该地区海平面上升的风险,区划海平面上升风险,并提出风险管理的建议。结果表明,天津滨海新区、河北黄骅市等地面临的海平面上升风险较高,在沿海发展规划和重大工程建设中应充分考虑海平面上升因素。
Sea level rise which caused by climate change will bring serious affect to the socio-economic devel-opment and ecological environment of coastal areas.The low-lying coastal areas of Tianjin and Hebei province are vulnerable to the direct impact of the sea level rise.The coastal areas of Tianjin and Hebei are taken as an example to demonstrate the application of the risk assessment methods of the sea level rise,zoning the risk of the sea level rise ,and to give the recommendations of the risk management.The results show that,Tianjin Binhai New Area and Huang Hua have high risk of sea level rise,the factor of sea level rise should be fully considered in the coastal de-velopment planning and major construction projects.

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天津滨海地区地处渤海湾西岸,晚新生代沉积了巨厚的松散沉积物。地下水位下降、地层自然固结、地表载荷的加速增长等复合因素造成了严重的地面沉降。利用在天津滨海新区塘沽地区施工的一眼1 226 m全取芯钻孔,通过原状样品测试分析,系统研究了晚新生代土层的物理力学性质、黏性土固结特征,并结合欠固结黏性土层沉降量计算等方法阐述了土层固结状态空间特征,探讨了土层固结特征与地面沉降的相关关系。结果表明:该地区0~100 m深度土层具有低天然密度、高孔隙比、高含水率、高压缩性等特点,表现出软土的性质,在地表荷载增大的情况下,易发生地面沉降;100~550 m的黏性土大都处于超固结和微超固结状态,主要是由于过去地下水的大量开采造成的;550 m以下的黏性土多为正常固结,局部存在欠固结黏性土夹层。钻孔中存在合计约218 m的欠固结黏性土夹层,这些欠固结黏性土夹层在自重应力下的最终沉降量为1 985 mm,沉降量最大的土层对应于第1、6含水组,分别达614 mm和665 mm,这一沉降过程完成所需时间为数十年甚至上百年。
Tianjin coastal area (TCA), located at the coastal region on the west of the Bohai Gulf, has suffered severe land subsidence due to compaction of the huge thick unconsolidated sediments deposited since Late Cenozoic era. Several factors, including groundwater level decline, clayey soils natural consolidation and surface loading rapid increase are the primary causes of land subsidence in this region. A borehole with depth of 1 226 m is drilled at Tanggu in the TCA;and core samples are extracted at various depths. Through laboratory test of these undisturbed soil samples, the physical and mechanicanl properties and the engineering geological properties of all kinds of clayey soils are analyzed. Integrating estimation of total compaction of the under-consolidated clayey soils, the spatial characteristics of natural consolidation of the unconsolidated sediment layers are delineated;and the relation between consolidation characteristics and land subsidence is discussed. The results indicate

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天津滨海地区的海堤多采用大型充砂袋作为堤心,一般的地基处理方式为铺设水平砂垫层和打入竖向塑料排水板,堤心充砂袋临海侧设有块石垫层和栅拦板护面,在海堤施工过程中要求监测堤身沉降量。根据某海堤工程沉降监测实例,分析沉降量设计值与监测值存在差异的原因,就沉降监测点的布置和埋设方法等提出若干参考建议。
Large-scale sand bags are used to be core of dikes in Tianjin Binhai Area. In general,the subgrade soil is consolidated by laying horizontal sand bedding and inserting vertical plastic drains. The sand-bag dike core on the exposed side is protected by rubble bedding and armor gratings. The settlement of dike will be observed during the construction. One dike settlement observation example is adopted to analyze the cause for the difference between the design settlement value and the observed data. Meanwhile,suggestions are brought forward for laying and embedding the settlement measuring points.

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