Coupled transport-reaction pathways and distribution patterns between siliciclastic-carbonate sediments at the Ria de Vigo

This paper examines the linkages between the space-distribution of grain sizes and the relative percentage of the amount of mineral species that result from the mixing process of siliciclastic and carbonate sediments at the Ria de Vigo (NW of Spain).The space-distribution of minerals was initially determined, starting from a detailed mineralogical study based on XRD-Rietveld analysis of the superficial sediments. Correlations between the maps obtained for grain sizes, average fractions of either siliciclastic or carbonates, as well as for individual-minerals, were further stabilised. From this analysis, spatially organized patterns were found between carbonates and several minerals involved in the siliciclastic fraction. In particular, a coupled behaviour is observed between plagioclases and carbonates, in terms of their relative percentage amounts and the grain size distribution.In order to explain these results a conceptual model is proposed, based on the interplay between chemical processes at the seawater–sediment interface and hydrodynamical factors. This model suggests the existence of chemical control mechanisms that, by selective processes of dissolution-crystallization, constrain the mixed environment's long-term evolution, inducing the formation of self-organized sedimentary patterns.     

Species of Thaumatomastix (Thaumatomastigidae, Protista incertae sedis) from the Arctic sea ice biota (North-East Water Polynya, NE Greenland)

The sea ice biota of polar regions contains numerous heterotrophic flagellates very few of which have been properly identified. The whole mount technique for transmission electron microscopy enables the identification of loricate and scaly forms. A survey of Arctic ice samples (North-East Water Polynya, NE Greenland) revealed the presence of ca. 12 taxa belonging to the phagotrophic genus Thaumatomastix (Protista incertae sedis). Species of Thaumatomastix possess siliceous body scales and one naked and one scale-covered flagellum. The presence in both Arctic samples and sea ice material previously examined from the Antarctic indicates that this genus is most likely ubiquitous in polar sea ice and may be an important component in sea ice biota microbial activities.     

Pb and Pu in the Northeast Water Polynya, Greenland: particle dynamics and sediment mixing rates

Distributions of the radionuclides ²¹⁰Pb and ^239,240Pu in sediment cores from the Northeast Water Polynya, Greenland, showed that these nuclides reached depths of 5–15 cm by particle mixing and sediment accumulation. End-member average values of the particle mixing coefficient and sediment accumulation rate were 0.13 cm² y⁻¹ and 0.06 cm y⁻¹, obtained from the ²¹⁰Pb profiles by assuming that each process is dominant relative to the other. Both ²¹⁰Pb and ^239,240Pu were measured on four cores; using the Pu data to constrain mixing rates produced corrected sediment accumulation rates that were 20–80% of the values calculated by neglecting mixing. Organic carbon burial in the polynya sediments was ≤0.4 mmol m⁻² d⁻¹, based on measured POC values at depth in the sediments and sediment accumulation rates corrected for mixing. This value is about 1% of the independently measured POC flux leaving the euphotic zone and compares with benthic carbon remineralization rates of 7% calculated by others from O₂ uptake in the sediments.The inventories of excess ²¹⁰Pb in the sediments ranged from 6 to 28 dpm cm⁻². Relative to the atmospheric input of ²¹⁰Pb and in situ production from decay of ²²⁶Ra, approximately 5 dpm cm⁻² of ²¹⁰Pb was being removed from the water column. The difference between the removal from the water column and sediment inventories suggests a net import of ²¹⁰Pb to the polynya. This may occur by input of dissolved ²¹⁰Pb from offshore waters or by input of ²¹⁰Pb carried by sea ice. Particulate matter in land-derived fast ice adjacent to the polynya contained 330 ± 14 dpm of excess ²¹⁰Pb g⁻¹. If particles transported in sea ice are comparable to those extracted from fast ice, then sea ice transport into the polynya followed by melting may be an important source of excess ²¹⁰Pb to the area. Fast ice also may contribute ²¹⁰Pb if portions break off and melt within the polynya, as occurred in 1993.     

中国新型极地考察船冰载荷预估研究

本文针对中国新型极地考察船所受冰载荷进行了研究,其中包含了平整冰阻力和浮冰碰撞力.对于船舶设计者和建造者来说,船舶冰载荷的预估非常重要.本文采用经验公式方法计算了该船在平整冰中航行的冰阻力,并且与模型试验结果进行了对比.结果显示,计算和试验结果中的冰阻力都随船舶航行速度的增大而增大,经验公式方法可以预测出合理的平整冰阻力.通过计算得到了该船的性能曲线,即该船在不同厚度平整冰中航行所能达到的速度.此外,本文还考虑了该船与圆形浮冰之间的三维斜向碰撞问题,采用解析方法评估了浮冰对船舶的撞击力,研究了撞击位置、法向框架角度以及浮冰尺寸对碰撞力的影响.基于计算结果,本文就冰载荷的预测进行了讨论并提出了一些建议.     

车辆转向架前端加装弧形导流槽对转向架积雪结冰情况的影响

通过空气动力学仿真分析和风洞试验,研究车辆转向架前端加装弧形防风雪导流槽对车辆转向架积雪区域空气动力学性能的影响,以及对转向架区域积雪结冰情况的影响。研究发现:在车辆转向架前端安装弧形防风雪导流槽,可以减少气流对转向架区域的直接冲击;可增加底部气体流速,使夹带雪花颗粒的气流快速通过转向架区域;空气流经导流槽发生明显下扬,使原空气流线在进入转向架区域时发生的上扬现象消失;安装弧形导流槽对整个转向架区域的积雪情况有明显改善作用。     

接地面部分溶化条件下冰面轮胎摩擦力的研究

综合运用流体动力润滑理论的能量守恒定律，提出了接地面部分溶化条件下冰面上汽车轮胎的摩擦力或牵引力的理论计算模型。证明了正常工作条件下，接地面上冰产生溶化的可能。对不同制动和驱动条件下轮胎摩擦力进行了计算，取得了同试验数据吻合很好的预测结果。并同已有预测模型进行了比较，比较结果表明：本文依据严格的润滑理论所推导出的冰面轮胎牵引力模型比其它已有理论模型更接近试验结果。     

Life cycle assessment of heated apron pavement system operations

Heated pavement systems (HPS) offer an attractive alternative to the cumbersome process of removing ice and snow from airport pavements using traditional snow removal systems. Although snow and ice removing efficiency and economic benefits of HPS have been assessed by previous studies, their environmental impact is not well known. Airport facilities offering public or private services need to evaluate the energy consumption and global warming potential of different types of snow and ice removal systems. Energy usage and emissions from the operations of hydronic heated pavement system using geothermal energy (HHPS-G), hydronic HPS using natural gas furnace (HHPS-NG), electrically heated pavement system (EHPS), and traditional snow and ice removal system (TSRS) are estimated and compared in this study using a hybrid life cycle assessment (LCA). Based on the system models assessed in this study, HPS application in the apron area seems to be a viable option from an energy or environmental perspective to achieve ice/snow free pavement surfaces without using mechanical or chemical methods. TSRS methods typically require more energy and they produce more greenhouse gas (GHG) emissions compared to HPS during the operation phase, under the conditions and assumptions considered in this study. Also, HPS operations require less energy and have less GHG emissions during a snow event with a smaller snowfall rate and a larger snow duration.     

冰区航行船舶电力推进轴系机电耦合的扭振分析

通过螺旋桨桨叶与冰块的相互作用过程,建立单冰块对螺旋桨扭转振动的激励函数;同时建立机电耦合振动数学模型,推导得到机电耦联动力学方程,研究电机电磁激励力对扭转振动的影响。以3500吨科考船电力推进轴系为研究对象,基于冰载荷激励力和电磁激励力对轴系扭转振动进行分析,为复杂的船舶电力推进轴系在冰区航行时的振动研究奠定了基础。     

冰载荷冲击下的船舶推进轴系瞬态扭转振动响应分析

传统的推进轴系扭转振动响应计算聚焦于稳态响应,而传递矩阵法、系统矩阵法,可以取得满意的稳态计算结果,但无法处理冰区船舶、海洋工程船舶所遇到的变载荷、变惯量等瞬态工况。为了克服频域扭振计算方法在处理瞬态条件扭振问题的局限性,使用 Newmark 法从时域求解轴系扭转振动微分方程组,基于该算法对某船推进轴系在冰载荷作用下的瞬态响应做了数值计算。其结果表明,在冰载荷冲击下,轴系瞬态扭矩比稳态扭矩大;通过时频分析,在冰载荷作用期间,出现了明显的螺旋桨叶频激励,因此须避免冰载荷激励产生轴系扭转振动的叶次共振。 Newmark 法扭振计算结果与实船测试结果对比表明,该方法在稳态响应计算和时域曲线上都与实际测量结果基本一致,具有工程实用性。