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61.
海冰板的环形屈曲的压缩破坏   总被引:2,自引:0,他引:2  
在轴对称条件下,给出海冰板的环向屈曲面临载荷,从细观力学的观点分析了微裂纹开裂的条件,扩展方向并给出绕海洋平台柱腿冰的损伤区的尺度。所给出的临界半径是一个与冰材料力学特征,冰的微结构参数一海洋平台柱腿半径相关的特征参数。对现场所观察和测量的结构给出了解释和定量分析。  相似文献   
62.
本文用理想结构单元法对空间刚架结构进行了极限强度分析,理想结构单元法在于将结构分成最大可能的单元。以简单的形式归并几何非线性与材料非线性。按增量形式加载,直到达到极限强度。本文根据Rashed理论导出了对称的切向方程组,节省了存贮单元、改善了破坏准则的描述。算例结果与非线性有限单元法结果十分吻合。  相似文献   
63.
In this study, organic carbon (OC), total nitrogen (TN), stable carbon isotopic (δ13COC) and CuO reaction product compositions were used to identify the sources of organic matter (OM) and to quantify the relative importance of allochthonous and autochthonous contributions to the western Adriatic Sea, Italy. Suspended particulate material (195 samples) and surficial sediments (0–1 cm, 70 samples) from shallow cross-shelf transects were collected in February and May 2003, respectively. Vertical water column profiles were acquired along the same transects. Data include depth, potential temperature, salinity, density and chlorophyll fluorimetry.Along the western Adriatic shelf in the near-shore region, the phytoplankton growth was influenced by dynamics of the buoyant plumes from the Po and Appennine rivers. A small amount of very fine terrigenous material remained suspended within the coastal current and was exported southward along the shelf to the slope. High variability in the bulk composition was detected in the Po prodelta surficial sediments, whereas the western Adriatic shelf, although a larger area, exhibited a narrower range of values.A significant decoupling was observed between suspended particles in the water column and surficial deposits. The organic material collected in the water column was compositionally heterogeneous, with contributions from marine phytoplankton, riverine–estuarine phytoplankton and soil-derived OM. Frequent physical reworking of surficial sediments likely leads to the efficient oxidation of marine OC, resulting in the observed accumulation and preservation of refractory soil-derived OC delivered by the Po and Appennine rivers.  相似文献   
64.
中太平洋铁锰结壳铅同位素研究   总被引:5,自引:0,他引:5  
已有研究表明大洋中溶解的铅(Pb)来源于陆源物质,但是,对Pb进入大洋的途径争议很大。为此分析了取自中太平洋两块铁锰结壳样品的Pb同位素组成,获得了整个新生代的中太平洋Pb同位素演化历史。结果表明这两块结壳的Pb同位素随时间的演化曲线与中北太平洋沉积物岩心LL44-GPC3中风成碎屑的Pb同位素演化曲线相似。证实该区深水中的天然溶解铅主要来自风成粉尘,并且50Ma之前中太平洋中溶解Pb同位素组成主要取决于源自美洲的风成粉尘的输入,40Ma之后主要取决于源自亚洲的风成粉尘的输入。  相似文献   
65.
通过对长江三角洲及其邻近区域埋藏古土壤、潮坪、长江下游河道浸滩、舟山滨岸风成沙丘、南京黄土古土壤序列沉积体的磁组构测量统计分析,取得了各自的标志特征。该2特征揭示出,舟山滨岸风成沙丘与南京黄土吉土壤序列沉积的搬运介质能量位相基本一致,其物源来向却显示出巨大差异;上述两类沉积体与上述现今潮坪、河道漫滩沉积体地搬运介质能量位相及物源来向均显示出绝然不同的标志特征。然而浸滩物源来民南京黄土的物尖兵为向却  相似文献   
66.
本文介绍了海水中砷标准物质的研制过程,其中包括溶液的配制、均匀性和稳定性检验,标样的分析方法。并对标准物质的定值数据进行统计处理,两种浓度的定值结果分别为:1.00μg/cm3±0.04μg/cm3和51.0μg/dm3±2.6μg/dm3。两种浓度砷标准物质的稳定期均为一年  相似文献   
67.
南海现代沉积物中正构烷烃碳分子组合特征及其指示意义   总被引:5,自引:0,他引:5  
利用1998年6~9月南海海洋环境调查及1987年SO-50中德联合调查中所取得的资料,对南海沉积物中正构烷烃碳分子组合特征进行分析和研究,并将南海与渤海、黄海、东海现代沉积过程中的正构烷烃碳分子组合特征进行对比,结果表明:(1)南海北部沉积物中正构烷烃碳分子分布范围为nC15~nC33,双峰群,居前的低碳数主峰碳为nC19~nC22,居后的高碳数主峰碳为nC27,nC24以后奇碳的优势明显,OEP为2.13,nC23-/nC24 值平均为1.53,沉积物中陆源输入居多;南海南部沉积物中正构烷烃碳分子分布范围为nC15~nC33,呈双峰群,居前的低碳数峰群以nC19~nC23为主峰碳,居后的高碳数峰群以nC27或nC29为主峰碳,OEP为1.58,nC23-/nC24 值平均为2.15,沉积物中海洋生物来源居多。南海沉积物中正构烷烃碳分子为海洋和陆源两种有机质来源。(2)南海南部处于典型热带海洋环境,生物生产力较高,大量硅质、钙质生物在海域繁殖,生物效应降低了陆源物质的丰度。物源效应和生物效应的差异是南海南、北部现代沉积物的碳分子组合分布变化的主要原因。(3)南海现代沉积物各站位沉积物中正构烷烃的P r/Ph值基本小于1,说明沉积物沉积时为缺氧还原的沉积环境,但局部海域沉积环境具有较强的氧化性,沉积物在沉积过程中一定程度上受到涌升的南极底层水的影响。(4)南海与东海、黄海、渤海不同海域沉积物中正构烷烃碳分子组合特征对比可知,各海域沉积物均显示出物源效应。  相似文献   
68.
Surficial sediment (about 5 mm) was scraped off in 15 stations selected in the Vie Estuary, a small estuary on the French Atlantic coast. The samples, prepared using the suitable methods, were used for comparing the behaviour of periphytic algae, sporopollinic and other palynologic material, ostracoda and foraminifera for proposing a synthetic evaluation of the information provided by each of them. Dinoflagellate cysts, which are found in an almost monospecific assemblage in low-salinity water, are dispersed by tidal currents, but the location of tintinnids in only the lower reaches shows a limited inward transport. Sporopollinic material is clearly related to the adjacent vegetation, indicating a local origin, and then little influence of transport on the microbenthos, even if fragments of freshwater crustaceans and of Pediastrum alga are found down to the mouth in the sporopollinic deposits. This limited transport of microbenthos allows the use of periphytic algae, benthic ostracoda and benthic foraminifera as indicators of local environmental conditions. It was then possible to determine the extent of marine influence in the estuary, to discriminate between the main channel and adjacent basins, and between different stages of evolution of the basins, from a recently dug basin to a eutrophicated one.  相似文献   
69.
A new natural rutile reference material is presented, suitable for U‐Pb dating and Zr‐in‐rutile thermometry by microbeam methods. U‐Pb dating of rutile R632 using laser ablation ICP‐MS with both magnetic sector field and quadrupole instruments as well as isotope dilution‐thermal ionisation mass spectrometry yielded a concordia age of 496 ± 2 Ma. The high U content (> 300 μg g?1) enabled measurement of high‐precision U‐Pb ages despite its young age. The sample was found to have a Zr content of 4294 ± 196 μg g?1, which makes it an excellent complementary reference material for Zr‐in‐rutile thermometry. Individual rutile grains have homogeneous compositions of a number of other trace elements including V, Cr, Fe, Nb, Mo, Sn, Sb, Hf, Ta and W. This newly characterised material significantly expands the range of available rutile reference materials relevant for age and temperature determinations.  相似文献   
70.
Solid matrix 3H reference materials are challenging to prepare given the volatile nature of 3H and are often unrepresentative of the range of 3H forms that may be encountered during routine analysis. As a result, few 3H reference materials are currently available, undermining verification of analytical techniques for environmental 3H measurement. To address this, an International Working Group on Organically‐Bound Tritium Analysis determined to produce a tritium natural matrix reference material (NMRM). The reference material comprises marine sediment blended with sewage sludge contaminated with 3H‐organic species arising from authorised discharges from a radiopharmaceutical manufacturing site. Previous studies have demonstrated that the 3H species have persisted in the environment over three decades providing valuable supporting data to underpin the characterisation of the NMRM. The preparation and characterisation of the NMRM are described along with the subsequent application of the reference material in an international intercomparison exercise involving nineteen laboratories from nine countries. A reference value of 168 ± 22 Bq kg?1 was derived from the data arising from the proficiency test.  相似文献   
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