A method for frost jacking prediction of single pile in permafrost     

Liu  Jiankun  Wang  Tengfei  Tai  Bowen  Lv  Peng 《Acta Geotechnica》2020,15(2):455-470

In this paper, a model is proposed to simulate frost jacking performances of a pile foundation within an axisymmetric pile–soil system through a coupling strategy. We consider three diversified stages for frost heave of adjacent foundation soil below freezing point, where mathematical expressions for the volumetric strain are given in terms of volumetric ice content, negative temperature and porosity. A modified strain-softening model characterizing frozen soil–pile interactions is established based on experimental results, taking into account the effects of normal pressure, negative temperature and moisture content. The proposed computational approach is then illuminated and validated via the numerical example of a simplified bridge pile foundation under natural permafrost condition. Variation of temperature regime, volumetric ice content, displacement and stress over time is analyzed. This model can be further applied to evaluating effects of different countermeasures that mitigate frost jacking hazard of single pile subjected to cold climate.

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华东地区能见度时空变化特征及影响因子分析     

董芳淑  廉丽姝  孙博雯  程禛  朱艳冰 《气象科技》2023,51(4):510-519

为探究华东地区能见度变化情况,利用1973—2020年的能见度数据、2014—2019年的气象要素和污染物浓度数据,采用趋势分析、经验正交函数(Empirical Orthogonal Function, EOF)分解、相关分析的方法,分析了能见度时空变化特征及影响因子。结果表明：(1)1973—2020年能见度呈显著(p<0.01)下降趋势,变化倾向率为-1.315 km/10a,季节之间存在差异,夏、秋季能见度下降速率较大分别为1.681 km/10a、1.443 km/10a;冬、春季下降幅度相对较小分别为1.092 km/10a、1.091 km/10a。其中,1973—2012年能见度呈显著(p<0.01)下降趋势,变化倾向率为-1.204 km/10a, 2013—2020年能见度呈不显著(p>0.05)增加趋势,变化倾向率为2.229 km/10a,近8年(2013—2020年)来能见度存在明显改善。(2)华东地区南部、北部能见度较好,中部能见度较差。EOF分解第1模态表明华东地区能见度整体变化趋势一致,第2模态具有明显的区域差异。(3)能见度与相对湿度...  相似文献   

Editorial     

D.Q. Bowen 《Quaternary Science Reviews》1990,9(4)

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Pleistocene deposits at Stoke Goldington,in the valley of the Great Ouse,UK     

C. P. Green  G. R. Coope  R. L. Jones  D. H. Keen  D. Q. Bowen  A. P. Currant  D. T. Holyoak  M. Ivanovich  J. E. Robinson  R. J. Rogerson  R. C. Young 《第四纪科学杂志》1996,11(1):59-87

At Stoke Goldington in the valley of the Great Ouse in Buckinghamshire a river terrace at a height of about 7 m above the floodplain is underlain by fluvial sediments representing climatic fluctuations in the late Middle Pleistocene. Near the base of the succession, at a level only 1 m above the modern floodplain, a fossil assemblage, including pollen, plant macrofossils, molluscs, insects and ostracods, provides evidence for the local development of herb-rich grassland under temperate climatic conditions. The fossil record, amino-acid racemisation ratios and uranium disequilibrium dating all suggest deposition of this material during Oxygen Isotope Stage 7. The deposits containing the temperate assemblage are immediately overlain by typical cold-climate gravels of the Great Ouse. These have been subjected to a later cut-and-fill episode, with the fill accumulating in cool climatic conditions. The cut-and-fill episode was succeeded by aggradation, forming the overlying terrace surface. Amino-acid racemisation ratios indicate that the fill was emplaced, and the terrace surface created, during or after Oxygen Isotope Stage 5. © 1996 John Wiley & Sons, Ltd.  相似文献   

河北省小营盘金矿控矿因素与找矿方向     

王志民  张运强  李瑞红  李朋伟  郝森  乔衍溢  张鑫  岳喜能  郭利东  安博文  赵旭 《地质论评》2023,69(Z1):197-199

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Mineralogy,geochemistry, and sulfur isotope characteristics of sediment-hosted hydrothermal sulfide minerals from the southern Okinawa Trough     

Yamin Yang  Zhigang Zeng  Xuebo Yin  Xiaoyuan Wang  Shuai Chen  Haiyan Qi  Zuxing Chen  Bowen Zhu 《海洋学报(英文版)》2021,40(10):129-143

Studies of the mineralogy and sulfur isotope composition of sediment-hosted hydrothermal sulfide minerals in cores are important for understanding the seafloor mineralization environment and material source and reconstructing the hydrothermal history. However, the source of ore-forming materials and the history of hydrothermal activity in the southern Okinawa Trough (SOT) remain unclear. Here, the mineralogy and sulfur isotope characteristics of sulfides from gravity core HOBAB4-S2, collected between the Yonaguni Knoll IV hydrothermal field (HF) and the Tangyin HF, was investigated. Enrichments in Zn (up to 321×10?6), Cu (up to 73.7×10?6), and Pb (up to 160×10?6) and the presence of pyrite, galena, pyrrhotite and minor sphalerite and chalcopyrite provide evidence for the input of hydrothermal materials into the sediments. The pyrite morphologies include disseminated cubic, pentagonal dodecahedron, and framboidal forms. Except for minor framboidal pyrite, euhedral pyrite from core HOBAB4-S2 is mainly of hydrothermal origin with Co/Ni ratios >1 and S/Fe atomic ratios <2 in the Cu-Zn-Pb-rich layers. The occurrences of hexagonal pyrrhotite, high-Co (up to 0.17%) pyrite and high-Fe sphalerite indicate that the hydrothermal precipitates formed at medium-high temperatures and low-sulfur fugacity (fS₂) environments. The δ34S values of sulfides (0.21‰–3.45‰) with low- fS₂ mineral assemblages (e.g., pyrrhotite ± high-Fe sphalerite) in the core are significantly lower than those of magmatic rocks and seawater, indicating possible incorporation of previously formed biogenic sulfur in the sediment. Combined with the age model of the core, it is suggested that hydrothermal activity likely began in the Tangyin HF before AD 1445–1483 and that at least three active episodes may have occurred since then.  相似文献   

一种地电阻率场地干扰的快速检测方法     

侯博文  谢佳兴  刘庆华  宋建锁 《地震地磁观测与研究》2020,41(4):78-82

对2018年洛阳地震台地电阻率观测区域出现的1次典型漏电干扰进行分析。经初步分析、干扰源模拟定位、干扰源现场调查等,确定干扰源的位置。通过对此次干扰的分析与排查,归纳总结出一种便利、快速的干扰检测定位方法。  相似文献   

B, Sr, O and H Isotopic Compositions of Formation Waters from the Bachu Bulge in the Tarim Basin     

CAI Chunfang PENG Licai MEI Bowen XIAO Yingkai 《《地质学报》英文版》2006,80(4):550-556

In order to elucidate the origin and migration of basinal brines in the Bachu Bulge, Tarim Basin, we have carried out analyses on chemical composition, and boron, hydrogen and oxygen isotopes of formation waters together with the XRD of clay minerals from the Paleozoic strata. The waters show Ca, B, Li and Sr enrichment and SO4 depletion in the Carboniferous and Ordovician and K enrichment in part of the Ordovician relative to seawater. The relationship between δD and δ^18O shows that all the data of the waters decline towards the Global Meteoric Water Line with the intersection of them close to the present-day local meteoric water, suggesting that modern meteoric water has mixed with evaporated seawater. The ^87Sr/^86Sr ratios range from 0.7090 to 0.7011, significantly higher than those of the contemporary seawater. The δ^11B values range from ＋19.7 to ＋32.3‰, showing a decrease with the depth and B concentrations. The results suggest that isotopically distinct B and Sr were derived from external sources. However, since the percentages of illite are shown to increase with depth among clay minerals in the study area, i.e., illite is due to precipitation rather than leaching during deeper burial, it is unlikely for illite to have contributed a significant amount of B to the waters. Thus, B with low δ^11B values is interpreted to have been added mainly from thermal degradation of kerogen or the basalts in the Cambrian and Lower Ordovician.  相似文献   

袖珍水翼突防潜艇的设计构想及运用研究          下载免费PDF全文

张博文  王晟洵  杨理华  谢亚轩 《数字海洋与水下攻防》2020,3(5):425-430

针对潜艇机动性不高以及传统水面攻击快艇隐蔽性不强的弊端,为使二者优势互补、扬长避短,阐述了一种袖珍水翼突防潜艇的设计构想。从设计构想、结构布局、应用研究等方面对该构想进行了分析,研究了袖珍水翼突防潜艇的使用与发展价值及潜在的军事战术应用,并指出了当前设计中可完善的问题。  相似文献   

考虑东北航线的亚欧LNG运输发展潜力研究   总被引：1，自引：1，他引：0  

李振福  陈卓  韦博文 《世界地理研究》2020,29(4):686-696

北极海冰的加速消融为北极航线的开发利用带来了机遇,北极地区的经济价值凸显。北极东北航线为亚欧间的LNG运输提供了新的运输通道。为使亚欧间的LNG运输更为经济合理,基于海运里程和单船必要运费率两方面比较通过北极东北航线、苏伊士运河航线、好望角航线进行跨亚欧LNG运输的经济性。在此基础上,采用负指数网络配流方法计算不同路径的配流比例,研究东北航线的亚欧间LNG运输发展潜力。结果表明,整体而言,采用东北航线进行跨亚欧LNG运输的海运里程更短,单船必要运费率更低,配流比例更高,其中,日本袖浦使用东北航线的经济性最为显著。将跨亚欧LNG运输通道的经济性分析和交通分配相结合,为亚洲地区更为经济合理地进行LNG运输提供参考。  相似文献