模拟强震后高压输电接续管漏磁的检测方法研究          下载免费PDF全文

孙炎  侯立群  路晓明  杨东升  陈曦  崔贤成 《地震工程学报》2020,42(1):276-282

为维持强震影响下电力系统安全运行,改善高压输电效率及输电质量,提出强震影响下高压输电接续管漏磁检测方法。采用磁敏传感器获取漏磁通内的漏磁信号,通过计算提取接续管内漏磁信号特征量,依据这些特征实现高压输电接续管漏磁检测。构建高压输电接续管三维有限元几何模型,通过对模型的单元类型确定、材料选择、边界条件与荷载设置、传感器部署位置等,完成高压输电接续管仿真分析。实验结果表明：在Ⅸ度罕遇北京波影响下,接续管内漏磁信号特征量可评判缺陷深度,实现接线管漏磁检测。通过对DL/T1192-2012标准输电线接续管上表面和下表面两端的漏磁信号峰值检测等,证明了本文方法对强震影响下高压输电接续管漏磁进行检测的有效性。  相似文献   

Estimation of Oceanic Heat Flux Under Sea Ice in the Arctic Ocean     

LIN Long  ZHAO Jinping 《中国海洋大学学报(英文版)》2019,(3):605-614

Oceanic heat flux(Fw) is the vertical heat flux that is transmitted to the base of sea ice. It is the main source of sea ice bottom melting. The residual method was adopted to study oceanic heat flux under sea ice. The data acquired by 28 ice mass balance buoys(IMBs) deployed over the period of 2004 to 2013 in the Arctic Ocean were used. Fw values presented striking seasonal and spatial variations. The average summer Fw values for the Canada Basin, Transpolar Drift, and Multiyear Ice area were 16.8, 7.7, and 5.9 W m^-2, respectively. The mean summer F-w for the whole Arctic was 10.1 W m^-2, which was equivalent to a bottom melt of 0.4 m. Fw showed an autumn peak in November in the presence of the near-surface temperature maximum(NSTM). The average Fw for October to December was 3.7 W m^-2. And the average Fw for January to March was 1.0 W m^-2, which was approximately one third of the average Fw in the presence of NSTM. The summer Fw was almost wholly attributed to the incident solar radiation that enters the upper ocean through leads and the open water. Fw calculated through the residual method using IMB data was compared with that calculated through the parameterization method using Autonomous Ocean Flux Buoy data. The results revealed that the Fw provided by the two methods were consistent when the sea ice concentration exceeded 70% and mixing layer temperature departure from freezing point was less than 0.15℃. Otherwise, the Fw yielded by the residual method was approximately one third smaller than that provided by the parameterization method.  相似文献   

南方红壤侵蚀区长汀县不同生态恢复年限下芒萁叶绿素含量的高光谱估算模型     

邓超  陈志彪  陈海滨  陈志强 《地球信息科学学报》2019,21(6):948-957

芒萁是南方红壤侵蚀区生态恢复重要的地带性草本植物,对生态系统修复具有重要作用,监测其叶绿素含量能有效诊断生长健康状况。本文以福建省长汀县朱溪流域6个不同生态恢复年限下的芒萁叶片高光谱反射数据以及实测叶绿素含量为数据源,借助高光谱遥感技术分析不同恢复年限芒萁叶片原始光谱特征,筛选出光谱敏感波段并构建光谱指数,基于相关性分析,建立芒萁叶绿素单变量以及多元逐步回归模型,并确定最佳估算模型。结果表明：高光谱指数建立的单变量估算模型中,改进红边归一化植被指数（mNDVI₇₀₅）、叶面叶绿素指数（LCI）、红边指数（Vog）、比值光谱指数（RVI_603/407）、NDVI[603,407]高光谱指数建立的二次模型精度高,建模决定系数R²均超过了0.8,其中以高光谱指数为自变量建立的多元回归模型拟合R²值（0.886）最高。综合建模精度和模型验证精度,LCI指数构建的单变量模型以及基于高光谱指数的多元回归模型是估算芒萁叶片叶绿素含量最佳模型。本研究建立的叶绿素高光谱估算模型对快速、无损地监测水保植物芒萁生长具有重要意义。  相似文献   

南海风生近惯性能通量的敏感性分析     

孙宝楠  连展  袁业立  徐海洋 《海洋学报(英文版)》2019,38(4):136-145

After validated by the in-situ observation, the slab model is used to study the wind-generated near-inertial energy flux(NIEF) in the South China Sea(SCS) based on satellite-observed wind data, and its dependence on calculation methods and threshold criteria of the mixed layer depth(MLD) is investigated. Results illustrate that the total amount of NIEF in the SCS could be doubled if different threshold criteria of MLD are adopted. The NIEF calculated by the iteration and spectral solutions can lead to a discrepancy of 2.5 GW(1 GW=1×109 W). Results also indicate that the NIEF exhibits spatial and temporal variations, which are significant in the boreal autumn,and in the southern part of the SCS. Typhoons are an important generator of NIEF in the SCS, which could account for approximately 30% of the annual mean NIEF. In addition, deepening of the MLD due to strong winds could lead to a decrease of NIEF by approximately by 10%. We re-estimate the annual mean NIEF in the SCS,which is(10±4) GW and much larger than those reported in previous studies.  相似文献   

东南极中山站陆缘固定冰2011/2012年度的时空变化     

赵杰臣  杨清华  程斌  LEPP&#;RANTA Matti  谢苏锐  陈猛  于亦宁  田忠翔  李明  张林  惠凤鸣 《海洋学报(英文版)》2019,38(5):51-61

Annual observations of first-year ice(FYI) and second-year ice(SYI) near Zhongshan Station, East Antarctica,were conducted for the first time from December 2011 to December 2012. Melt ponds appeared from early December 2011. Landfast ice partly broke in late January, 2012 after a strong cyclone. Open water was refrozen to form new ice cover in mid-February, and then FYI and SYI co-existed in March with a growth rate of 0.8 cm/d for FYI and a melting rate of 2.7 cm/d for SYI. This difference was due to the oceanic heat flux and the thickness of ice,with weaker heat flux through thicker ice. From May onward, FYI and SYI showed a similar growth by 0.5 cm/d.Their maximum thickness reached 160.5 cm and 167.0 cm, respectively, in late October. Drillings showed variations of FYI thickness to be generally less than 1.0 cm, but variations were up to 33.0 cm for SYI in March,suggesting that the SYI bottom was particularly uneven. Snow distribution was strongly affected by wind and surface roughness, leading to large thickness differences in the different sites. Snow and ice thickness in Nella Fjord had a similar "east thicker, west thinner" spatial distribution. Easterly prevailing wind and local topography led to this snow pattern. Superimposed ice induced by snow cover melting in summer thickened multi-year ice,causing it to be thicker than the snow-free SYI. The estimated monthly oceanic heat flux was ～30.0 W/m2 in March–May, reducing to ～10.0 W/m2 during July–October, and increasing to ～15.0 W/m2 in November. The seasonal change and mean value of 15.6 W/m2 was similar to the findings of previous research. The results can be used to further our understanding of landfast ice for climate change study and Chinese Antarctic Expedition services.  相似文献   

Physical processes causing the formation of hypoxia off the Changjiang estuary after Typhoon Chan-hom, 2015     

GUO Yaru  RONG Zengrui  LI Bo  XU Zhao  LI Pixue  LI Xiaodan 《海洋湖沼学报（英文）》2019,(1):1-17

Severe hypoxia was observed in the submarine canyon to the east of the Changjiang estuary in July 14, 2015, two days after typhoon Chan-hom. The oxygen concentration reached as low as 2.0 mg/L and occupied a water column of about 25 m. A ROMS model was con?gured to explore the underlying physical processes causing the formation of hypoxia. Chan-hom passed through the Changjiang estuary during the neap tide. The strati?cation was completely destroyed in the shallow nearshore region when typhoon passing. However, it was maintained in the deep canyon, though the surface mixed layer was largely deepened. The residual water in the deep canyon is considered to be the possible source of the later hypoxia. After Chan-hom departure, not only the low salinity plume water spread further of fshore, but also the sea surface temperature(SST) rewarmed quickly. Both changes helped strengthen the strati?cation and facilitate the formation of hypoxia. It was found that the surface heat ?ux, especially the solar short wave radiation dominated the surface re-warming, the of fshore advection of the warmer Changjiang Diluted Water(CDW) also played a role. In addition to the residual water in the deep canyon, the Taiwan Warm Current(TWC) was found to ?ow into the deep canyon pre-and soon post-Chan-hom, which was considered to be the original source of the hypoxia water.  相似文献   

Recent satellite-derived sea ice volume flux through the Fram Strait: 2011–2015   总被引：1，自引：0，他引：1  

毕海波  王云鹤  张文峰  ZHANG Zehu  LIANG Yu  ZHANG Yi  胡文敏  付敏  黄海军 《海洋学报(英文版)》2018,37(9):107-115

The Fram Strait(FS) is the primary region of sea ice export from the Arctic Ocean and thus plays an important role in regulating the amount of sea ice and fresh water entering the North Atlantic seas. A 5 a(2011–2015) sea ice thickness record retrieved from Cryo Sat-2 observations is used to derive a sea ice volume flux via the FS. Over this period, a mean winter accumulative volume flux(WAVF) based on sea ice drift data derived from passivemicrowave measurements, which are provided by the National Snow and Ice Data Center(NSIDC) and the Institut Francais de Recherche pour d'Exploitation de la Mer(IFREMER), amounts to 1 029 km~3(NSIDC) and1 463 km~3(IFREMER), respectively. For this period, a mean monthly volume flux(area flux) difference between the estimates derived from the NSIDC and IFREMER drift data is –62 km~3 per month(–18×10~6 km~2 per month).Analysis reveals that this negative bias is mainly attributable to faster IFREMER drift speeds in comparison with slower NSIDC drift data. NSIDC-based sea ice volume flux estimates are compared with the results from the University of Bremen(UB), and the two products agree relatively well with a mean monthly bias of(5.7±45.9) km~3 per month for the period from January 2011 to August 2013. IFREMER-based volume flux is also in good agreement with previous results of the 1990 s. Compared with P1(1990/1991–1993/1994) and P2(2003/2004–2007/2008), the WAVF estimates indicate a decline of more than 600 km~3 in P3(2011/2012–2014/2015). Over the three periods, the variability and the decline in the sea ice volume flux are mainly attributable to sea ice motion changes, and second to sea ice thickness changes, and the least to sea ice concentration variations.  相似文献   

流域系统综合模拟与情景分析——自然地理综合研究的新范式?     

朱阿兴  朱良君  史亚星  秦承志  刘军志 《地理科学进展》2019,38(8):1111-1122

在全球环境变化和经济快速发展的背景下,经济发展与资源环境保护之间的矛盾日益激化,为解决或减弱这一矛盾,管理者需要新的知识体系和科学的决策工具。自然地理综合研究以自然地理要素空间变化及交互过程为主要研究内容,肩负着提供管理者所需新知识体系和科学决策工具的责任。流域作为空间上相对封闭的自然地理单元,其相对独立性为管理者的决策提供了天然的空间单元。流域内各地理要素的空间分布及其过程的交互机理自然成为管理者解决日益激化的矛盾所需的新知识体系,而流域系统综合模拟恰恰为建立这样的知识体系提供了极为有效的研究方式;在管理者评价各种决策的成效时,必须知道各种决策所产生的经济和环境效益,基于流域系统综合模拟的情景分析为管理者提供了所需要的科学决策工具。因此,从解决经济发展与资源环境保护之间矛盾的角度出发,流域系统综合模拟与情景分析应该成为新时代背景下自然地理学综合研究的新范式。文章结合2个小流域情景分析的研究案例,探讨了以流域系统综合模拟与情景分析为核心的现代自然地理综合研究需要解决的科学挑战,即流域系统综合模拟的系统化、空间化、定量化、易用化和决策化。  相似文献   

流域交通运输地理研究进展与展望     

吴威  梁双波  曹有挥 《地理科学进展》2019,38(8):1136-1149

流域交通运输地理在区域交通运输地理的理论框架下,以流域或流域的部分区域为研究区开展交通运输组织及其发展规律研究。论文从交通网络、运输联系及区域效应3个方面梳理了流域交通运输地理的研究进展。 ① 交通网络相关研究围绕综合交通发展水平与格局、网络连接特征与可达性、港口体系的空间结构与供应链等展开,多式联运正成为流域交通运输地理研究的新热点;② 运输联系主要研究客货运输联系规律和交通流,流域物流地理的研究重点正从物流产业布局与企业选址向物流网络与空间组织、物流供应链转移;③ 区域效应偏重于经济增长效应,资源环境生态效应研究较为薄弱。基于流域交通运输地理研究的侧重点,结合当前研究进展与流域发展需求,流域交通运输地理学未来应重视流域港口体系与水运发展,关注综合交通网络构建与运输组织以及多式联运,探究不同层级流域交通运输间的关联性,同时应加强流域交通运输的资源环境与生态效应研究。  相似文献   

Threshold sediment flux for the formation of river deltas in Hainan Island,southern China     

Li  Gaocong  Zhou  Liang  Qi  Yali  Gao  Shu 《地理学报(英文版)》2019,29(1):146-160

Journal of Geographical Sciences - The knowledge of geomorphological evolution from an estuary to a river delta is necessary to form the formulation of comprehensive land-ocean interaction...  相似文献