The electromagnetic and gravitational-wave radiations of X-ray transient CDF-S XT2     

Hou-Jun Lü  Yong Yuan  Lin Lan  Bin-Bin Zhang  Jin-Hang Zou  En-Wei Liang 《天文和天体物理学研究(英文版)》2021,(2)

Binary neutron star(NS)mergers may result in remnants of supra-massive or even stable NS,which have been supported indirectly by observed X-ray plateau of some gamma-ray burst(GRB)afterglows.Recently,Xue et al.(2019)discovered an X-ray transient CDF-S XT2 that is powered by a magnetar from merger of double NS via X-ray plateau and following stepper phase.However,the decay slope after the plateau emission is slightly larger than the theoretical value of spin-down in electromagnetic(EM)dominated by losing its rotation energy.In this paper,we assume that the feature of X-ray emission is caused by a supra-massive magnetar central engine for surviving thousands of seconds to collapse into a black hole.Within this scenario,we present the comparisons of the X-ray plateau luminosity,break time,and the parameters of magnetar between CDF-S XT2 and other short GRBs with internal plateau samples.By adopting the collapse time to constrain the equation of state(EOS),we find that three EOSs(GM1,DD2,and DDME2)are consistent with the observational data.On the other hand,if the most released rotation energy of magnetar is dominated by GW radiation,we also constrain the upper limit of ellipticity of NS for given EOS,and its range is[0.32-1.3]×10^-3.Its GW signal cannot be detected by Advanced LIGO or even for more sensitive Einstein Telescope in the future.  相似文献   

Current Vertical Motion Analysis of Northwestern Margin of Ordos Based on Precise Leveling     

Guo Baozhen  Ta L  Zhou Haitao  Su Guangli 《中国地震研究》2018,32(1):113-118

Ordos block was squeezed by the Qinghai-Tibetan block and North China block, and the tectonic activity was intense. In the periphery of Ordos block, there was a series of folds zones and compressed faults with complicate structures. This paper used three-phase data of 1980,1990 and 2014 to calculate vertical velocity of Northwestern margin of Ordos and the analytical results indicated that ① the Hetao basin between the rise of Yinshan fault block and Ordos fault block showed relatively subsidence, in which Linhe basin was the most evident and the subsidence rate was about 2-4mm/a. The subsidence rate of Jartai -Yinchuan rift zone on the western margin of Ordos block was about 2mm/a; ② the whole testing zone exhibited the evident inherited movement characterized by mountain rise and basin subsidence; ③the two leveling section through the northern margin fault and Dengkou-Benjing fault showed that the difference between vertical velocities on two sides of the fault was less than 0.5mm/a.  相似文献   

Terahertz band simulations using two different radiative transfer models     

Linjun PAN  Daren Lü 《中国科学:地球科学(英文版)》2018,61(10):1482-1490

A high-resolution dual-band terahertz (THz) radiometer was designed to measure vertical distributions of chemical elements in the middle atmosphere of the Tibetan Plateau. A forward simulation, which always should be conducted firstly for the development of a matching retrieval algorithm, has not been done before. We use two radiative transfer models, ARTS and AM, to simulate the water vapor, ozone and carbon monoxide spectra on the plateau based on the spectral design of the THz radiometer. The emission line characteristics of the three gases in this spectral band are identified. Reasons for the differences in the spectral simulations between the two models are analyzed for individual gases. The impact of several different spectral parameter settings on the simulations are evaluated through a series of sensitivity experiments. This study suggests that the ARTS is more suitable for the development of the THz radiometer retrieval algorithm. An optimal parameter setting of the ARTS for the three elements are given.  相似文献   

灌河口近岸海域春季海洋环境现状调查     

周超凡  矫新明  毛成责  张鹏  Lü Ying 《广东海洋大学学报》2018,(5)

【目的】调查灌河口邻近海域生态环境状况。【方法】2016年5月对该海域进行水质、沉积物和生物生态现状调查。【结果与结论】水质主要超标因子为无机氮、磷酸盐;沉积物质量监测项目全部符合一类沉积物质量标准。浮游植物生物多样性指数丰富(3.11),浮游动物、游泳动物的生物多样性指数较丰富(大于2),底栖生物较贫乏(0.97)。底栖生物密度与沉积物硫化物显著正相关。浮游植物密度与叶素绿a显著正相关。小型网浮游动物密度与水温、化学需氧量显著负相关,其种类与营养盐、化学需氧量显著负相关,二者均与盐度显著正相关。  相似文献   

Depth of closure: New calculation method based on sediment data     

Luis Aragonés  Jose Ignacio Pagán  Isabel López  José C.Serra 《国际泥沙研究》2018,33(2):198-207

Obtaining depth of closure (DoC) in an accurate manner is a fundamental issue for coastal engineering, since good results for coastal structures and beach nourishment depend mainly on DoC. Currently, there are two methods for obtaining the DoC, mathematical formulations and profile surveys. However, these methods can incur important errors if one does not take into account the characteristics and morphology of the area, or if one does not have a sufficiently long time series. In this work the DoC is obtained from the break in the trend of the sediment with the depth, that is, in general with the increase of the depth a decrease in the size of the sediment takes place. However, at one point this tendency changes and the size increases, and then decreases again. When comparing the point where the minimum sediment size occurs before the increase, it is observed that the error incurred is small compared to other methods. If the Standard Deviation of Depth Change (SDDC) method is considered as the most accurate method, the error incurred by the proposed method is less than 7%. In addition, it can be seen that the dispersion of the sediment method always occurs outside the zone of bar movement. Whereas in the methods of profiles survey (using 2 cm precision profiles), sometimes the DoC is obtained within the active zone of bar movement. In addition, where the relative minimum of the median sediment size is found, and the sizes of 0.063 and 0.125 mm predominate in the composition of the sample. Therefore, this new method allows the precise location of the DoC to be obtained in a fast and simple way. Furthermore, this method has the advantage that it is not affected by the modifications that may be experienced by both the study area and the cross-shore beach profile.  相似文献   

里奥格兰德裂谷南部地壳结构的地球物理约束     

L.E.Thompson  A.A.Velasco  A.Zamora  M.Hussein  张晓曼  余庆坤 《世界地震译丛》2018,(4)

里奥格兰德裂谷仍有地质活动发生的证据,主要有第四纪断层作用、地震活动和裂谷低速扩张。利用绘制的地壳厚度与地震波速比所生成的约束地壳模型横剖面,来突出里奥格兰德裂谷南部的区域扩张。计算了147个台站的接收函数和它们的叠加,使用的数据包括地球透镜计划美国台阵移动阵列、以前收集的美国西南部数据,并使用克里金插值方法对地壳和速度结果进行了插值。再将上述接收函数结果作为反演密度剖面的一个约束条件,得到了一个新的、优化的重力反演方法。最终,得到了约束地壳模型。该模型显示里奥格兰德裂谷南部地区存在浅层莫霍面(30km),此结果比前人得到的要厚。在盆岭区,里奥格兰德裂谷西部地壳分层,接近大平原的里奥格兰德裂谷东部存在较厚的地壳,且伴有密度大的低速层。我们也发现特拉华盆地表现出显著的地球物理异常,其原因可能是该盆地存在厚的饱和沉积物。考虑到其他研究中并没有发现该区域有深部地幔异常,本文提出裂谷可能是上地幔小尺度对流的结果,并得出里奥格兰德裂谷处于盆岭区和大平原的最小边界处,也可能是板块俯冲的终点。  相似文献   

Spatio-temporal variations of harmful algal blooms along the coast of Guangdong,Southern China during 1980–2016     

LI Li  Lü Songhui  CEN Jingyi 《中国海洋湖沼学报》2019,(2)

Harmful algal blooms(HABs) have become a recurring problem, posing severe impacts on marine ecosystems, fisheries, mariculture industry, and even public health. In this study, the geographic information system(GIS) was utilized to determine spatial and temporal characteristics of HAB events in the coastal waters of Guangdong from 1980–2016. We analyzed distribution patterns and characteristics of HABs by dividing the coast of Guangdong into well-known bays, estuary and coastal waters. Results showed that there were a total of 337 HABs recorded in Guangdong coastal waters. Spatial and temporal distributions varied among dif ferent regions. Most HABs occurred in the Mirs Bay, followed by the west coast of Daya Bay, while a few occurred in the west and east coasts of Guangdong but with an increasing trend in the past two decades. HABs occurred mostly in warmer months of March to May in the western coast of Guangdong, March and April in Mirs Bay, April in Zhujiang(Pearl) River estuary, November in eastern coast of Guangdong. For Daya Bay, most HABs were reported between March and September.The most frequently occurring HABs species were Noctiluca scintillans, P haeocystis globosa, Skeletonema costatum and Scrippsiella trochoidea, occurring mostly in Mirs Bay, western Guangdong coast area, eastern Guangdong coast area and Zhujiang River estuary and Daya Bay, respectively. Ichthyotoxic blooms were more common than toxic blooms, and Heterosigma akashiwo, Chattonella marina, Karenia mikimotoi and P haeocystis globosa were the most common ichthyotoxic species. Our results provide baseline information useful for policy making and management of HABs in the region.  相似文献   

Preface to Special Issue on the National Report to the IUGG Centennial by CNC-IAMAS(2011–2018)     

Daren Lü  Jianchun BIAN 《大气科学进展》2019,36(9):885-885

正The 27th General Assembly of the International Union of Geodesy and Geophysics(IUGG), which also marks the 100 th anniversary of IUGG, will be held during 8–18 July 2019 in Montréal, Canada. The Chinese National Committee(CNC)for the International Association of Meteorology and Atmospheric Sciences(IAMAS) has a more than 30-year tradition of  相似文献   

Description and Phylogenetic Position of Dinosaur Eggshells from the Luanchuan Area of Western Henan Province, China     

Kohei TANAKA  Lü Junchang  Yoshitsugu KOBAYASHI  Darla K. ZELENITSKY  XU Li  JIA Songhai  QIN Shuang  TANG Min’an 《《地质学报》英文版》2011,85(1):66-74

Here, we examine 145 dinosaur eggshells from a new fossil locality in the Qiupa Formation (Upper Cretaceous) of the Luanchuan area in western Henan Province, China. The eggshells display elongatoolithid macro- and microstructures, including ridges and nodes on the outer surface, two ultrastructural layers, and an undulatory boundary between the mammillary and continuous layers. A phylogenic analysis shows that the Luanchuan eggshells belong to the ooclade Elongatoolithidae. Within Elongatoolithidae, the thickness ratio of the mammillary layer to the entire eggshell, and the porosity of the Luanchuan eggshells are comparable to the oogenera Macroolithus and Elongatoolithus. There is no direct evidence for the taxonomic identity of the Luanchuan eggshells; however, they were likely laid by oviraptorids based on their phylogenetic position and their similarities with known oviraptorid eggs.  相似文献   

Geochemical Stratigraphy and Microvertebrate Assemblage Sequences across the Silurian/Devonian Transition in South China     

ZHAO Wenjin  WANG Nianzhong  ZHU Min  Ulrich MANN  Ulrich HERTEN  Andreas LüCKE 《《地质学报》英文版》2011,85(2):340-353

Carbon isotope (δ13Corg) analyses of non-marine clastic rocks and neritic carbonates and black shales spanning the Silurian/Devonian transition are compared from two richly fossiliferous sequences in Qujing of East Yunnan and Zoige of Sichuan, South China. The two sections, Xishancun and Putonggou sections in South China, reveal positive δ13Corg shifts happening in the Upper Pridoli and Lower Devonian and reaching peak values as heavy as ?25.2‰ (Xishancun) and ?19.9‰ (Putonggou) in the lowermost Lochkovian following the first occurrence of the thelodont Parathelodus and the conodont Icriodus woschmidti woschmidti (only in Putonggou Section and together with Protathyris-Lanceomyonia brachiopod fauna). These results replicate a globally known positive shift in δ13Corg from the uppermost Silurian to the lowermost Devonian. The δ13Corg variations across the Silurian/Devonian Boundary (SDB) at the two sections in South China exhibit a shift in carbon isotopic composition similar to the detailed SDB curves from the borehole Klonk-1 drilled at top of the Klonk Global Standard Stratotype-Section and Point (GSSP) in the Prague Basin, Czech Republic. In addition, four microvertebrate assemblages, including the Liaojiaoshan, Xishancun, Yanglugou and Xiaputonggou assemblages, are recognized from the Silurian/Devonian transition exposed in the Xishancun and Putonggou sections, respectively. The results from both carbon isotope stratigraphy and microvertebrate assemblage sequences suggest that the SDB in South China is located at the base of the Xishancun Formation (between sample QX-20 and sample QX-21) in the Xishancun Section and the lower part of the Xiaputonggou Formation (between sample ZP-09 and sample ZP-10) in the Putonggou Section. The isotopic trend for organic carbon together with the changes of microvertebrate remains across the SDB can offer an approach to a potential correlation of the SDB from different sedimentary facies, which help to correlate the marine with non-marine deposits.  相似文献