基于远、近期合建的折多山公路隧道总体设计方案研究

为解决特长公路隧道升级改造困难问题,以折多山公路隧道项目为依托,创新性地提出远、近期合建的总体设计方案。通过交通量预测、工程造价、运营通风及逃生救援等方面综合比较,得出可实施的合建方案： 先期建设二级公路隧道主洞,设2段非贯通平导,后期直接将二级公路隧道作为高速公路隧道右洞,并贯通二级公路隧道平导作为高速公路隧道左洞。合建方案能有效节约工程造价,降低社会耗能。     

西津水利枢纽二线船闸下引航道布置方案对比

西津水利枢纽二线船闸工程对发展西江航运和流域经济具有重要作用。为研究二线船闸布置方案与原一线船闸布置的相互影响,采用水工模型试验研究二线船闸下引航道两类不同布置方案下的水流条件,通过分别测定一、二线船闸下引航道口门区纵、横向及回流流速三项指标,并进行对比分析得知:一、二线船闸下引航道口门区采用共用布置方案时,在中洪水流量情况下,口门区内横向及回流流速难以满足规范要求;当采用下引航道口门区分开布置形式时,二线船闸下引航道口门区多项流速在各级通航流量下基本满足规范要求。     

葛洲坝1号船闸增设防撞安全设施的探讨

葛洲坝1号船闸由于与三峡船闸匹配运行,船舶实行导航墙待闸,下行船舶在导航墙停靠时距离人字门较近,而且下行船舶首船进闸后停靠位置与下闸首人字门距离较近,都具有碰撞人字门的风险。针对葛洲坝1号船闸人字门存在被碰撞的风险,结合上、下闸首的现场情况分别就上、下闸首人字门增设防撞设施方案的可能性进行分析,提出提升式、侧开式和下沉式等方案,并讨论各方案实现的可能性、优势及不足,为船闸人字门防撞安全设施的方案设计及应用提供参考。     

特大型耙吸挖泥船研制及工程应用

针对特大型耙吸挖泥船多工况、大舱容、大挖深、精确与高效控制及良好的航行性能等问题,进行船型、系列化耙头、高效泥泵、耙臂泵和控制系统的研究。采用理论研究、大比例尺模型试验、实船验证等多种研究方法,解决了限制特大型耙吸挖泥船国产化的技术瓶颈。在上述研究成果的基础上,设计建造了2艘特大型耙吸挖泥船,两船服务于我国多个重大港口航道工程,经济和社会效益显著。     

水力式升船机的特点及关键技术

介绍水力式升船机的特点,对水力式升船机的关键设计技术进行论述。水力式升船机具有安全可靠、适应下游水位变幅大的特点。重点对水力式升船机的输水系统、机械系统、船厢出入水等关键技术进行探讨。认为输水系统重点要解决竖井水位同步和水流控制的问题,机械系统重点要解决无间隙传动和适应基础变形的问题,船厢出入水重点要解决出入过程中不平衡荷载的影响。     

大型升船机卷筒与主轴连接技术

大型升船机承载能力大,若卷筒与主轴仍采用常规连接形式很难满足要求。分析了卷筒与主轴的各种连接结构,针对景洪升船机开发一种新的连接技术,解决了加工和装配的工艺难题。通过理论计算确定结构尺寸,成功完成了16件大型卷筒装置的设计生产加工。     

涪江过军渡电航枢纽工程总体布置研究

根据过军渡电航枢纽工程水工模型试验,论述了上下游引航道口门区泥沙淤积与通航水流条件的变化,研究了船闸引航道的平面布置及不同通航流量情况下设计船队在船闸上下游引航道口门区及连接段的航行情况和航行要素,优化进出闸航线,并配合通航水流条件的观测对船闸引航道平面布置提出修改意见,从而选出通航条件好、工程量小、河道演变较稳定的推荐方案。     

半潜起重铺管船关键连接节点设计对比分析

针对半潜式起重铺管船的设计关键节点——立柱与上平台转角处,采用直接计算方法,对两种不同的设计连接形式进行分析研究。分别对两种不同连接形式在屈服强度、疲劳寿命和施工建造三个方面进行对比,得到较优的结构设计,可供相关设计者参考。     

Dynamics of inorganic nutrient species in the Bohai seawaters

Within the frame of a Sino-German Joint Research Program, two cruises of “R/V Dong Fang Hong 2” were carried out in September–October 1998 and April–May 1999, respectively, to understand the dynamics of nutrients in the Bohai. Nutrient species (NO₃⁻, NO₂⁻, NH₄⁺, PO₄³⁻ and SiO₃²⁻) are determined colorimetrically on board for five anchor and 30 grid stations. In situ incubation experiments are performed to determine planktonic nutrient uptake and benthic exchange flux. Nutrient concentrations display short-term variability and seasonal change in the Bohai, with higher levels in shallow coastal waters than in the Central Bohai. The influence of riverine discharge on nutrient levels can be seen from salinity isopleths, nutrient distribution and species ratios. Near-bottom (nb) waters have similar nutrient concentrations as to the surface waters in the Central Bohai, whereas stratification takes place in the Bohai Strait and North Yellow Sea. In situ incubation experiments provide evidence that the uptake ratio (i.e. N, P) by phytoplankton is proportional to the ratios among nutrient species in ambient waters. Based on the data of this study and previously publications, a preliminary estimate of nutrient budgets via riverine input and atmospheric deposition is established. The results indicate that atmospheric deposition gains importance over rivers in delivering nutrients into the Bohai and sustain the new production, following recent decrease in riverine inflow caused by drought periods in North China and damming practices. A historical review of nutrient data indicates that concentrations of nitrogen increase and phosphorus and silica decrease in the Central Bohai over last 40 years. This potentially has an important influence on the health of ecosystem in Bohai (e.g. food web and community structure), though further study is needed to examine the scenario in more detail.     

Application of new parameterizations of gas transfer velocity and their impact on regional and global marine CO2 budgets

One of the dominant sources of uncertainty in the calculation of air–sea flux of carbon dioxide on a global scale originates from the various parameterizations of the gas transfer velocity, k, that are in use. Whilst it is undisputed that most of these parameterizations have shortcomings and neglect processes which influence air–sea gas exchange and do not scale with wind speed alone, there is no general agreement about their relative accuracy.The most widely used parameterizations are based on non-linear functions of wind speed and, to a lesser extent, on sea surface temperature and salinity. Processes such as surface film damping and whitecapping are known to have an effect on air–sea exchange. More recently published parameterizations use friction velocity, sea surface roughness, and significant wave height. These new parameters can account to some extent for processes such as film damping and whitecapping and could potentially explain the spread of wind-speed based transfer velocities published in the literature.We combine some of the principles of two recently published k parameterizations [Glover, D.M., Frew, N.M., McCue, S.J. and Bock, E.J., 2002. A multiyear time series of global gas transfer velocity from the TOPEX dual frequency, normalized radar backscatter algorithm. In: Donelan, M.A., Drennan, W.M., Saltzman, E.S., and Wanninkhof, R. (Eds.), Gas Transfer at Water Surfaces, Geophys. Monograph 127. AGU,Washington, DC, 325–331; Woolf, D.K., 2005. Parameterization of gas transfer velocities and sea-state dependent wave breaking. Tellus, 57B: 87–94] to calculate k as the sum of a linear function of total mean square slope of the sea surface and a wave breaking parameter. This separates contributions from direct and bubble-mediated gas transfer as suggested by Woolf [Woolf, D.K., 2005. Parameterization of gas transfer velocities and sea-state dependent wave breaking. Tellus, 57B: 87–94] and allows us to quantify contributions from these two processes independently.We then apply our parameterization to a monthly TOPEX altimeter gridded 1.5° × 1.5° data set and compare our results to transfer velocities calculated using the popular wind-based k parameterizations by Wanninkhof [Wanninkhof, R., 1992. Relationship between wind speed and gas exchange over the ocean. J. Geophys. Res., 97: 7373–7382.] and Wanninkhof and McGillis [Wanninkhof, R. and McGillis, W., 1999. A cubic relationship between air−sea CO2 exchange and wind speed. Geophys. Res. Lett., 26(13): 1889–1892]. We show that despite good agreement of the globally averaged transfer velocities, global and regional fluxes differ by up to 100%. These discrepancies are a result of different spatio-temporal distributions of the processes involved in the parameterizations of k, indicating the importance of wave field parameters and a need for further validation.