垂直水幕作用下扩建地下水封油库布局方式研究

为研究垂直水幕对扩建地下水封油库布局方式的影响,以某大型地下水封洞库分期建设工程为依托,采用有限元数值模拟方法,对有、无垂直水幕条件下扩建洞库的布局方式进行研究。研究结果表明： 1）当两期洞库间距较小时,在两期洞库之间设置垂直水幕可有效削弱拟建洞库对已建洞库水封可靠性的影响,随两期洞库间距的增加,垂直水幕的影响性逐渐减弱; 2）拟建洞库轴线方向对水封可靠性的影响受地形等条件的影响较大,在两期洞库之间设置垂直水幕对水封可靠性的影响较小; 3）随拟建洞库埋深的增加,拟建洞库的水封可靠性逐渐增强,已建洞库的水封可靠性却呈逐步减小趋势,在两期洞库之间设置垂直水幕可有效减小埋深对两期洞库水封可靠性的影响。     

Mechanism of Tunnel Water Inflow Caused by Bending Failure of a Waterproof Dike Based on a Circular Thin Plate Mechanical Model北大核心CSCD

Water bursts during tunnel construction endanger construction, and it is therefore necessary to reserve a waterproof dike with the required thickness to avoid water bursts and to take reinforcement of the dike and treatment of the structure liable to trigger a water burst. Using the water burst at K5+398 of the Mingyueshan tunnel of the Shanghai-Chengdu expressway as an example, and considering the type of tunnel section and the upright mudstone of the dike, the waterproof dike at the work face is simplified as a round thin plate. A formula for the calculation of a minimum safety thickness for the critical waterproof dike is deduced by analyzing the force applied on the water-proof dike, and the minimum safety thickness for the water burst section at K5+398 of the Mingyueshan tunnel is cal-culated. The numerical simulation analysis demonstrates the critical thickness of waterproof dike at K5+398 of the Mingyueshan tunnel is 1.4-1.55 m, and the calculated water inflow and water burst basically agree with the actual condition. © 2018, Editorial Office of "Modern Tunnelling Technology". All right reserved.     

西津水利枢纽二线船闸下游引航道右岸支流汇入口消能设施设计

西津水利枢纽二线船闸工程是建设"西江亿吨级黄金水道"的重要举措之一。为研究二线船闸下引航道停泊段右岸西竹坑支流的汇入对二线船闸下引航道内通航水流条件的影响,通过水工模型试验研究在支流沟内布置消能设施对支流入汇口处流速、流态的影响,提出斜向导流坝、消力墩和消力池的工程措施,为类似工程提供借鉴。     

基于植被生态需水的隧道排水量确定方法研究

隧道地下水大量渗漏易造成洞顶影响范围内生态环境破坏,针对如何确定合适涌渗水量以确保生态平衡问题,引入生态学、农学中有关植被生态需水概念,通过调研分析确定隧址区植被所允许的最大地下水位降深,结合地下水动力学方法以及经验公式,确定隧道涌渗水后地下水达到最大降深时疏干漏斗范围及体积;并通过疏干漏斗体积、涌渗水量以及储水系数关系确定隧道所允许排放的最大水量.结合算例并与实际工程中设计排水量进行对比,在考虑隧址区实际工程地质、水文地质条件情况下,所提出方法计算得出的排水标准与实际工程接近.该方法能够达到隧道工程与地下水环境生态平衡,可为隧道建设提供参考.     

Sidescan sonar survey of a dumping site in the Mecklenburg Bight (south-western Baltic Sea)

Two dumping test sites of dredged sediment (glacial till, mixed sediment with sand) in the south-western Baltic Sea were repeatedly investigated with sidescan sonar. The first survey was conducted before dumping, the second survey 1 week after dumping, and eight more surveys were run during the following three and a half years. Sidescan mosaics were calculated from raw data. Comparing the mosaics, it becomes obvious that the initial strong microrelief of the dumping sites vanishes with time. The heaps of dumped material were eroded. Coarse material remains at the surface, fine material fills in the gaps between the heaps. Fine sediment structures (filaments and aureoles) created by the dumping process, and elongated traces of dumped material outside the dumping places disappeared with time.     

一类动态交通分配中的输出流模型及其数值解法

已知路段输入流,基于Greenshields提出的速度-密度关系模型以及Jayakrishnan et.al提出的改进的Greenshields 速度-密度关系模型所描述的路段交通流特征,分别给出了关于路段输出流的常微分方程模型.针对无法得到该模型的解析解,利用龙格-库塔-芬尔格算法给出初始条件下的数值解.在已知输出流的条件下,每个时刻的路段交通流的行程时间也相应给出.仿真结果表明,针对两类不同速度-密度关系所建立的输出流模型,所得到每个时刻的输出流基本相似,但路段行程时间存在明显差异.与交通流调查数据比较,基于改进的Greenshields速度-密度关系的输出流模型的行程时间更接近真实情况.     

Silicon dynamics in the Oder estuary, Baltic Sea

Studies on dissolved silicate (DSi) and biogenic silica (BSi) dynamics were carried out in the Oder estuary, Baltic Sea in 2000–2005. The Oder estuary proved to be an important component of the Oder River–Baltic Sea continuum where very intensive seasonal DSi uptake during spring and autumn, but also BSi regeneration during summer take place. Owing to the regeneration process annual DSi patterns in the river and the estuary distinctly differed; the annual patterns of DSi in the estuary showed two maxima and two minima in contrast to one maximum- and one minimum-pattern in the Oder River. DSi concentrations in the river and in the estuary were highest in winter (200–250 μmol dm^− 3) and lowest (often less than 1 μmol dm^− 3) in spring, concomitant with diatom growth; such low values are known to be limiting for new diatom growth. Secondary DSi summer peaks at the estuary exit exceeded 100 μmol dm^− 3, and these maxima were followed by autumn minima coinciding with the autumn diatom bloom. Seasonal peaks in BSi concentrations (ca. 100 μmol dm^− 3) occurred during the spring diatom bloom in the Oder River. Mass balance calculations of DSi and BSi showed that DSi + BSi import to the estuary over a two year period was 103.2 kt and that can be compared with the DSi export of 98.5 kt. The difference between these numbers gives room for ca. 2.5 kt BSi to be annually exported to the Baltic Sea. Sediment cores studies point to BSi annual accumulation on the level of 2.5 kt BSi. BSi import to the estuary is on the level of ca. 10.5 kt, thus ca. 5 kt of BSi is annually converted into the DSi, increasing the pool of DSi that leaves the system. BSi concentrations being ca. 2 times higher at the estuary entrance than at its exit remain in a good agreement with the DSi and BSi budgeting presented in the paper.     

On the application of hydraulic theory to the deep-water flow through the Irbe Strait

A flow-dependent critical-point method for investigating topographically controlled flow in natural channels is applied to the bottom current through the Irbe Strait connecting the Baltic proper and the Gulf of Riga. This approach is based on the functional formalism due to Gill [Gill, A.E., 1977. The hydraulics of rotating-channel flow. J. Fluid Mech., 80, 641–671.], and here is used for the stratified flow structure observed during the IRBEX-95 field campaign. A critical section of the realizable flow regime was found to be located slightly downstream of the most pronounced horizontal constriction of the channel. The predicted baroclinic volume flux 7200 m³ s⁻¹ overestimates the observed mean bottom-water transport by around 30%, a discrepancy which most likely can be explained by the lack of sea level conditions and friction in the model.     

反坡斜井突涌水施工技术

通过对锦屏山隧道辅引3#施工支洞反坡施工,介绍反坡斜井突涌水条件下施工技术,根据实例论述了以防为主、防排结合的反坡斜井突涌水隧道施工方法.     

Ecophysiological growth characteristics and modeling of the onset of the spring bloom in the Baltic Sea

The onset of spring bloom in temperate areas is a transition period where the low productive, winter phytoplankton community is transformed into a high productive spring community. Downwelling irradiance, mixing depth and the ability of the phytoplankton community to utilize the light, are key parameters determining the timing of the onset of the spring bloom. Knowing these parameters would thus provide tools for modeling the spring bloom and enhance our knowledge of ecophysiological processes during this period.Our main objective with this study was to provide data for the growth characteristics of some key species forming the spring bloom in the Gulf of Finland, and to apply those results in a simple dynamic model for the onset of the spring bloom, in order to test if the timing of the spring bloom predicted by the models corresponds to field observations. We investigated the photosynthetic characteristics of three diatoms and two dinoflagellates (Chaetoceros wighamii, Melosira arctica, Thalassiosira baltica, Scrippsiella hangoei and Woloszynskia halophila), at low temperatures (4–5 °C). All of these species are common during spring bloom in the Baltic Sea.Cultures of these species were acclimated to different irradiance regimes prior to measurements of photosynthesis, respiration, pigment concentration and light absorption. We did not find a positive relationship between respiration and growth rate, and we hypothesize that this relationship, which is well established at higher temperatures, is negligible or absent at low temperatures (< 10 °C). Photosynthetic maximum (P_m), and maximum light utilization coefficient (α) was lowest and respiration (R) highest in the dinoflagellates.We made a model of the onset of the spring bloom in the western part of Gulf of Finland, using the obtained data together with monitoring data of mixing depth and water transparency from this area. Model results were compared to field observations of chlorophyll-a (Chl-a) concentration. There was a good agreement between the model predictions and the observed onset of the spring bloom for the diatoms. S. hangoei, however, was not able to reach positive production in the model, and W. halophila had the similar growth characteristics as S. hangoei. Consequently, these species must have other competition strategies enabling them to exist and grow during spring bloom.