路基在地下暗河作用下变形失稳相似模型试验

文章依托昌金高速公路B2-1标岩溶地下洞河路基塌陷展开研究,通过对塌陷段进行相似模型模拟试验,分析了地下暗河不同宽度对上部路堤沉陷与失稳的影响,提出了塌陷的处治建议,为类似工程提供参考。     

粉喷桩应用若干问题的探讨

结合广东地区粉喷桩的经验,探讨了粉喷桩处理软基的若干问题。     

大桥主墩沉井施工方案及监控

沉井下沉是沉井施工的一个关键工序,也是一项工程成败的关键,因此做好沉井下沉是一项工程的重中之重。本文结合印度泰米尔纳度邦凯瑞大桥的沉井施工,重点阐述了钢壳沉井在不同地质情况下下沉时出现的各种问题,及其解决方案。     

湿陷性黄土地区公路构造物地基处理

针对湿陷性黄土地区土质的勘探、试验、湿陷等级确定、构造物类别划分等几个方面提出了湿陷性黄土公路构造物地基处理时应注意的一些问题并提出改进措施。     

古代木质沉船整体打捞技术

首次提出了一种适用于古代木质沉船的整体打捞方案,并且通过"南海1号"古沉船整体打捞模型试验对此方案进行了验证。     

Wind-triggered events of phytoplankton downward flux in the Northeast Water Polynya

Phytoplankton carbon fluxes were studied in the Northeast Water (NEW) Polynya, off the eastern coast of Greenland (79° to 81°N, 6° to 17°W), during summer 1993. The downward flux of organic particles was determined during 54 days using a sediment trap moored at a fixed location, below the pycnocline (130 m). The hypothesis of the present study is that wind events were ultimately responsible for the events of diatoms downward flux recorded in the trap.Wind conditions can influence the vertical transport of phytoplankton by affecting (1) the environmental conditions (e.g. hydrostatic pressure, nutrient concentrations, and irradiance) encountered by phytoplankton during their vertical excursion, and (2) the aggregation and disaggregation of phytoplankton flocs. The first mechanism affects the physiological regulation of buoyancy, whereas the second one affects the size and shape of settling particles.Using field data (wind velocity, density profiles and phytoplankton abundance), we assessed the potential aggregation and the vertical excursion of phytoplankton in surface waters. The results show that, upstream from the trap, wind and hydrodynamic conditions were sometimes favourable to the downward export of phytoplankton. Lag-correlation between time series of wind and phytoplankton downward flux shows that flux events lagged wind events by ca. 16 days. Given that the average current velocity in the top 100 m was ca. 10 cm s⁻¹, a lag of 16 days corresponded to a lateral transport of ca. 130 km, upstream from the sediment trap, where phytoplankton production was lower than at the location of the trap. According to that scenario, 21% to 60% of primary production was exported to depth during wind events. If we had assumed instead a tight spatial coupling between the material collected in the trap and the relatively high phytoplankton production at the location of the trap, we would have concluded that <7% of primary production was exported to depth. The difference between the two scenarios has great implications for the fate of phytoplankton. Our results stress the importance of investigating the spatial coupling between surface and trap data before assessing the pathways of phytoplankton carbon cycling.