A motion planning algorithm for the feed support system of FAST     

姚蕊  姜鹏  孙京海  于东俊  孙纯 《天文和天体物理学研究(英文版)》2020,(5):117-126

The paper relates to a motion planning algorithm for the feed support system of the Five-hundred-meter Aperture Spherical radio Telescope(FAST).To enhance the stability of the feed support system,the start/termination planning segments are adopted with an acceleration and deceleration section.The source switching planning adopts a combination of a line segment and focal segment to realize stable control of the feed support system.Besides,during the observation trajectory,a transition segment which is not used for observation data is planned with a required time.Through an example simulation,a smooth change is realized via the motion planning algorithm and presented in this paper.  相似文献   

湖南仁里超大型钽铌矿床工作进展及找矿思路     

杨世珍  周芳春  李建斌  刘翔  李建康  黄志飚  苏俊男  李鹏 《中国地质调查》2020,7(4):28-36

湖南仁里超大型钽铌矿床钽铌铍矿资源丰富,Ta₂O₅资源量达到了超大型规模,BeO资源量达到了大型规模。为进一步研究湖南仁里超大型钽铌矿床稀有金属的赋存特征、成矿规律及矿产资源综合利用前景,开展了地球化学分析、电子探针、包裹体、同位素测年及可选性试验等研究工作,通过系统梳理仁里超大型钽铌矿床的工作进展,进一步探讨了该矿床的下一步找矿思路。仁里钽铌矿床共(伴)生矿种多,稀有金属综合回收率及矿产资源采选综合利用率高,具有极大的开发利用价值,可作为绿色、环保、无尾矿范例进行高效勘查与开发。仁里矿区钽铌铍矿资源丰富,具有较好的找矿潜力,加大地质勘查资金投入有望取得钽铌铍锂等稀有金属找矿新进展。下一步应对矿区2、3、5、6号主矿脉深部矿体进行控制,力争取得钽铌铍矿找矿突破,同时加强对矿区西部或西南部隐伏锂辉石白云母钠长石伟晶岩的研究工作,力争取得锂辉石白云母钠长石伟晶岩型锂矿找矿突破。  相似文献   

RESEARCH ON THE CHARACTERISTICS OF QUATERNARY ACTIVITIES OF SU-XI-CHANG FAULT          下载免费PDF全文

ZHANG Peng  ZHANG Yuan-yuan  XU Han-gang  LIU Jian-da  CHEN Jian-qiang  LI Li-mei  LI Jin-liang  GU Qin-ping  JIANG Xin 《地震地质》2019,41(5):1172-1184

Running across the urban areas of Changzhou, Wuxi and Suzhou, the NW-trending Su-Xi-Chang Fault is an important buried fault in Yangtze River Delta. In the respect of structural geomorphology, hilly landform is developed along the southwest side of the Su-Xi-Chang Fault, and a series of lakes and relatively low-lying depressions are developed on its northeast side, which is an important landform and neotectonic boundary line. The fault controlled the Jurassic and Cretaceous stratigraphic sedimentary and Cenozoic volcanic activities, and also has obvious control effects on the modern geomorphology and Quaternary stratigraphic distribution. Su-Xi-Chang Fault is one of the target faults of the project "Urban active fault exploration and seismic risk assessment in Changzhou City" and "Urban active fault exploration and seismic risk assessment in Suzhou City". Hidden in the ground with thick cover layer, few researches have been done on this fault in the past. The study on the activity characteristics and the latest activity era of the Su-Xi-Chang Fault is of great significance for the prevention and reduction of earthquake disaster losses caused by the destructive earthquakes to the cities of Changzhou, Wuxi and Suzhou. Based on shallow seismic exploration and drilling joint profiling method, Quaternary activities and distribution characteristics of the Su-Xi-Chang Fault are analyzed systematically. Shallow seismic exploration results show that the south branch of the Su-Xi-Chang Fault in Suzhou area is dominated by normal faulting, dipping to the north-east, with a dip angle of about 60° and a displacement of 3~5m on the bedrock surface. The north branch of the Su-Xi-Chang Fault in Changzhou area is dominated by normal faulting, dipping to the south, with a dip angle of about 55°~70° and a displacement of 4~12m on the bedrock surface. All breakpoints of Su-Xi-Chang Fault on the seismic exploration profiles show that only the bedrock surface was dislocated, not the interior strata of the Quaternary. On the drilling joint profile in the Dongqiao site of Suzhou, the latest activity of the south branch of Su-Xi-Chang Fault is manifested as reverse faulting, with maximum displacement of 2.9m in the upper part of Lower Pleistocene, and the Middle Pleistocene has not been dislocated by the fault. The fault acts as normal fault in the Pre-Quaternary strata, with a displacement of 3.7m in the Neogene stratum. On the drilling joint profile in the Chaoyang Road site of Changzhou, the latest activity of the north branch of Su-Xi-Chang Fault is manifested as reverse faulting too, with maximum displacement of 2.8m in the bottom layer of the Middle Pleistocene. The fault acts as normal fault in the Pre-Quaternary strata, with a displacement of 10.2m in the bedrock surface. Combining the above results, we conclude that the latest activity era of Su-Xi-Chang Fault is early Middle Pleistocene. The Su-Xi-Chang Fault was dominated by the sinistral normal faulting in the pre-Quaternary period, and turned into sinistral reverse faulting after the early Pleistocene, with displacement of about 3m in the Quaternary strata. The maximum magnitude of potential earthquake on the Su-Xi-Chang Fault is estimated to be 6.0.  相似文献   

Changes in run‐off and sediment load in the three parts of the Yellow River basin,in response to climate change and human activities     

Chaojun Gu  Xingmin Mu  Peng Gao  Guangju Zhao  Wenyi Sun 《水文研究》2019,33(4):585-601

Hydrological regimes in the Yellow River have changed significantly because of climate change and intensive human interventions. These changes present severe challenges to water resource utilization and ecological development. Variation of run‐off, suspended sediment load (SSL), and eight precipitation indices (P1: 0–12 mm·day^?1, P12: 12–25 mm·day^?1, P25: 25–50 mm·day^?1, P50: P ≥ 50 mm·day^?1 and corresponding rainfall day: Pd1, Pd12, Pd25, Pd50 day year^?1) in three critical parts of the Yellow River basin (source region: SRYRB, upper reaches: URYRB, middle reaches: MRYRB) were investigated for the period from 1960 to 2015. The results show that run‐off and SSL significantly decreased (P < 0.01) in the URYRB and the MRYRB, whereas their decline in the SRYRB was insignificant (P > 0.05). Moreover, run‐off in the URYRB had one change point in 1987, and SSL in the URYRB as well as run‐off and SSL in the MRYRB had two change points (in the 1970s and the 1990s). Over the same period, only Pd1 and Pd12 in the SRYRB showed significant increasing trends, and an abrupt change appeared in 1981. The optimal precipitation indices for assessing the effects of precipitation on run‐off and SSL in the URYRB and MRYRB were Pd50 and P12, respectively. A double‐mass curve analysis showed that precipitation and human activities contributed to approximately 20% and 80% of the reduction in run‐off, respectively, for both the SRYRB and the MRYRB. However, the contribution rate of precipitation and human activities on SSL reduction was approximately 40% and 60% in the URYRB and 5% and 95% in the MRYRB, respectively. Human activities, primarily soil and water conservation measures and water extraction (diversion), were the main factors (>50%) that reduced the run‐off. However, the dominant driving factors for SSL reduction were soil and water conservation measures and reservoir interception, for which the contribution rate was higher than 70% in the MRYRB. This work strengthens the understanding of hydrological responses to precipitation change and provides a useful reference for regional water resource utilization.  相似文献   

2008年汶川MS8.0地震电离层图像信息长时程演化初探     

宋程  张永仙  夏彩韵  张小涛 《地震》2019,39(2):135-146

应用改进的图像信息方法, 结合DEMETER电磁卫星的电子温度数据, 对2008年汶川M_S8.0地震进行了长时程的回溯性预测研究。 与以往的地震电离层演化图像提取异常的研究相比, 将其回溯的时程延长至震前近11个月, 并向震后延长48 d。 在长期连续的异常扰动演化图中, 出现了两个明显的异常时段, 且在震前2个月短期内异常扰动明显减弱并趋于背景值。 两个时段出现的异常扰动分布位置及其形态以及持续时间皆不重复, 这体现了前兆异常的不易确定, 难以定性及定量识别的特点。 电离层异常扰动特征的长时程研究, 有评估其预测参数和模型可靠性的实际作用, 也为应用中国卫星观测数据服务于地震预报等研究积累经验, 具有借鉴意义。  相似文献   

秦岭—大别东段应力状态研究     

倪红玉  刘泽民  洪德全  赵朋  汪小厉 《地震》2019,39(3):138-148

本文首先通过Snoke发展的利用P波、 SV波和SH波的初动和振幅比方法计算秦岭—大别东段2008年以来83次M_L≥2.5地震的震源机制解, 然后通过FMSI方法反演得到平均应力场的方向特征: 近东西向的水平挤压和近南北向的水平拉张作用, 与参数统计结果一致; 进而通过震源机制的一致性参数分析应力场方向的变化信息。 分析表明震源机制解呈现了由变化紊乱、 偏离平均应力场到变化一致、 趋于平均应力场再到变化紊乱、 偏离平均应力场的变化过程, 在显著地震前, 研究区整体的震源机制一致性参数处于持续低值状态; 计算了2008年以来93次M_L≥2.5地震的视应力, 拟合视应力与震级的关系, 分析扣除震级影响的差视应力随时间变化特征, 近似反映研究区应力大小的变化。 分析表明显著地震前研究区的差视应力值呈现出明显的先上升后下降的变化过程, 在下降过程中发生地震; 最后利用震源机制一致性参数和差视应力综合分析研究区的应力状态, 均表明显著地震前震源区的构造应力场增强。 目前研究区的震源机制一致性参数较高、 差视应力较低, 研究区的应力水平较低。  相似文献   

汤东活动断裂带土壤H2、Rn地球化学特征     

胡宁  马志敏  王明亮  王宇  娄露玲  夏修军  张宝山  王文净  郭德科 《地震》2019,39(2):174-182

为研究汤东断裂带土壤气体地球化学特征及其所反映的构造地球化学背景, 采用野外监测的方法分析了张河村与邢李庄村两条测线的土壤H₂、 Rn分布特征。 结果表明, 张河村H₂浓度、 Rn活度浓度的分布范围分别为0.24×10^-6～174.7×10^-6、 13.3～69.8 kBq·m^-3, 背景值分别为14.26×10^-6, 24.8 kBq·m^-3。 邢李庄测线H₂浓度、 Rn活度浓度的分布范围11.8×10^-6～67.06×10^-6、 43.6～72.6 kBq·m^-3, 背景值分别为37.13×10^-6、 72.6 kBq·m^-3。 张河村测线在90～105 m处, H₂、 Rn出现强烈高值异常, 而120～150 m处出现高值异常。 异常值位于断裂带附近, H₂、 Rn气体测值对断裂位置具有良好的指示作用。 气体异常主要受汤东活动断裂构造控制, 汤东断裂下方的深大断裂和汤阴地堑中下地壳的低速体对深部气体释放有重要作用。  相似文献   

鲫鱼(Carassius auratus)半胱亚磺酸脱酸酶CSAD基因克隆及其表达研究     

李晓洁  唐建洲  宋鹏  伍琴  瞿符发  刘臻  鲁双庆 《海洋与湖沼》2018,49(1):134-141

本研究以鲫鱼(Carassius auratus)为研究对象,采用巢式PCR和RACE技术克隆鲫鱼半胱亚磺酸脱酸酶CSAD基因c DNA序列,并且利用实时荧光定量PCR检测了CSAD m RNA在鲫鱼不同组织和昼夜节律中的相对表达水平,同时还研究了牛磺酸对鲫鱼肠道CSAD m RNA表达的影响。结果表明:(1)鲫鱼CSAD基因c DNA序列包含186bp的5?UTR序列,675bp的3?UTR序列,1503bp开放阅读框,编码500个氨基酸。同源性分析表明,鲫鱼和鲤鱼的同源性为97.2%。系统发育分析表明,鲫鱼与鲤鱼之间的亲缘关系最接近,置信度为100。经预测,其编码的蛋白质的分子量和等电点分别为56.82k Da和5.77;(2)Ca CSAD m RNA在肌肉、心脏、肠道及肝脏中的表达水平较高,在脑和鳃组织中的相对表达量较低;(3)鲫鱼肠道CSAD m RNA的相对表达量在6:00am点时最高,9:00pm点时相对表达量最低;(4)鲫鱼CSAD的相对表达丰度随着牛磺酸添加量的增加而逐渐下降。本研究结果不仅有助于理解鲫鱼CSAD基因的分子特征,同时将为进一步研究鱼类CSAD营养调控功能提供理论依据。  相似文献   

Modelling the time‐dependent behaviour of granular material with hypoplasticity          下载免费PDF全文

Shun Wang  Wei Wu  Zhen‐Yu Yin  Chong Peng  Xuzhen He 《国际地质力学数值与分析法杂志》2018,42(12):1331-1345

This paper presents a constitutive model for time‐dependent behaviour of granular material. The model consists of 2 parts representing the inviscid and viscous behaviour of granular materials. The inviscid part is a rate‐independent hypoplastic constitutive model. The viscous part is represented by a rheological model, which contains a high‐order term denoting the strain acceleration. The proposed model is validated by simulating some element tests on granular soils. Our model is able to model not only the non‐isotach behaviour but also the 3 creep stages, namely, primary, secondary, and tertiary creep, in a unified way.  相似文献   

TECTONIC INDICATIONS OF OCCURRENCE OF MODERATE-TO-STRONG EARTHQUAKES IN CHAOHU-TONGLING AREA,ANHUI PROVINCE     

GUO Peng  HAN Zhu-jun  ZHOU Ben-gang  ZHOU Qing  MAO Ze-bin 《地震地质》2018,40(4):832-849

The Chaohu-Tongling area in Anhui Province is a typical moderate-to-strong earthquake active area in the mainland of China. Four earthquakes occurred in this area, displayed as a NNE-trending zonal distribution, including the 1585 M5(3/4) Chaoxian earthquake and the 1654 M5(1/4) Lujiang earthquake, which formed a striking moderate-to-strong seismic activity zone. Field survey, shallow geophysical prospecting, drilling data, collection and dating of chronology samples and comprehensive analysis of fault activity indicate that the Fanshan, Xiajialing and Langcun faults are not active since Quaternary. The NNE-trending Tongling Fault is a buried middle-Pleistocene fault, but it can produce moderate-to-strong earthquakes and control the evolution and development of three en echelon geologic structures. The intensity of the four earthquakes is characterized by southward progressive decrease, which is in accordance with the characteristics that the subsidence range of Wuwei Basin is obviously larger than that of Guichi Basin to its south since late Cenozoic. In terms of deep structure, the characteristics of spatial distribution of Tongling Fault indicate that it corresponds to a NNE-striking Bouguer gravity anomaly gradient belt. So there is a spatial correspondence between the middle-Pleistocene Tongling Fault, the en echelon structures, the differential movement of the neotectonics, the Bouguer gravity anomaly gradient belt and the moderate-to-strong seismic activity belt in the Chaohu-Tongling area, indicating that they should be the tectonic indications of occurrence for moderate-to-strong earthquakes.  相似文献