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| 1 | Altitude dependency of trends of daily climate extremes in southwestern China, 1961-2008显示文摘A total of 12 indices of temperature extremes and 11 indices of precipitation ex-tremes at 111 stations in southwestern China at altitudes of 285-4700 m were examined for the period 1961-2008. Significant correlations of temperature extremes and elevation in-cluded the trends of diurnal temperature range, frost days, ice days, cold night frequency and cold day frequency. Regional trends of growing season length, warm night frequency, coldest night and warmest night displayed a statistically significant positive correlation with altitude. These characteristics indicated the obvious warming with altitude. For precipitation extreme indices, only the trends of consecutive dry days, consecutive wet days, wet day precipitation and the number of heavy precipitation days had significant correlations with increasing alti-tude owing to the complex influence of atmospheric circulation. It also indicated the increased precipitation mainly at higher altitude areas, whereas the increase of extreme precipitation events mainly at lowers altitude. In addition, the clearly local influences are also crucial on climate extremes. The analysis revealed an enhanced sensitivity of climate extremes to ele-vation in southwestern China in the context of recent warming. | Li Zongxing He Yuanqing Theakstone, Wilfred H. Wang Xufeng Zhang Wei Cao Weihong Du Jiankuo Xin Huijuan Chang Li | 2012 | Journal of Geographical Sciences2012，22，3： | 36 |
| 2 | Spatial distribution and temporal trends in potential evapotranspiration over Hengduan Mountains region from 1960 to 2009显示文摘在 19612009 期间在 Hengduan 山区域基于 20 个车站的气象学的数据,潜在的土壤水分蒸发蒸腾损失总量的年度、季节的变化与 Penman-Monteith 模型一起在联合被分析。与在 ArcGIS 下面的花键插值的方法,潜在的土壤水分蒸发蒸腾损失总量的空间分发被介绍研究地区性的差别,并且关联分析被用来讨论影响潜在的土壤水分蒸发蒸腾损失总量的主导的因素。结果显示自从 1960 年代,年度潜在的土壤水分蒸发蒸腾损失总量显示出一个减少的趋势,特别从 1980 年代到 1990 年代,当自从 2000,它显示出一个增加的趋势时。地区性的潜在的土壤水分蒸发蒸腾损失总量显示出 0.17 公里 a1 的率。在 Hengduan 山的北方,中间和南方的潜在的土壤水分蒸发蒸腾损失总量在学习时期上展出了减少的趋势,并且它的地区性的趋势在从西南的衰落上到东北。 | ZHU Guofeng HE Yuanqing PU Tao WANG Xufeng JIA Wenxiong LI Zongxing XIN Huijuan | 2012 | Journal of Geographical Sciences2012，22，1： | 16 |
| 3 | Source of major anions and cations of snowpacks in Hailuogou No.1 glacier, Mt. Gongga and Baishui No.1 glacier, Mt. Yulong显示文摘积雪场样品是从二条冰河的 colleted:在 2006 年 6 月的 Baishui No.1 冰河和 Hailuogou No.1 冰河。海盐离子 tracer。 | LI Zongxing HE Yuanqing PANG Hongxi YANG Xiaomei JIA Wenxiong ZHANG Ningning WANG Xufeng NING Baoying YUAN Lingling SONG Bo | 2008 | Journal of Geographical Sciences2008，18，1： | 13 |
| 4 | Design of aircraft structures against threat of bird strikes显示文摘In this paper, a method to design bird-strike-resistant aircraft structures is presented and illustrated through examples. The focus is on bird strike experiments and simulations. The explicit finite element software PAM-CRASH is employed to conduct bird strike simulations, and a coupled Smooth Particles Hydrodynamic(SPH) and Finite Element(FE) method is used to simulate the interaction between a bird and a target structure. The SPH method is explained, and an SPH bird model is established. Constitutive models for various structural materials, such as aluminum alloys, composite materials, honeycomb, and foam materials that are used in aircraft structures,are presented, and model parameters are identified by conducting various material tests. Good agreements between simulation results and experimental data suggest that the numerical model is capable of predicting the dynamic responses of various aircraft structures under a bird strike,and numerical simulation can be used as a tool to design bird-strike-resistant aircraft structures. | Jun LIU Yulong LI Xiancheng YU Xiaosheng GAO Zongxing LIU | 2018 | Chinese Journal of Aeronautics2018，31，7： | 8 |
| 5 | Automatic Method for Synchronizing Workpiece Frames in Twin-robot Nondestructive Testing System显示文摘The workpiece frames relative to each robot base frame should be known in advance for the proper operation of twin-robot nondestructive testing system. However, when two robots are separated from the workpieces, the twin robots cannot reach the same point to complete the process of workpiece frame positioning. Thus, a new method is proposed to solve the problem of coincidence between workpiece frames. Transformation between two robot base frames is initiated by measuring the coordinate values of three non-collinear calibration points. The relationship between the workpiece frame and that of the slave robot base frame is then determined according to the known transformation of two robot base frames, as well as the relationship between the workpiece frame and that of the master robot base frame. Only one robot is required to actually measure the coordinate values of the calibration points on the workpiece. This requirement is beneficial when one of the robots cannot reach and measure the calibration points. The coordinate values of the calibration points are derived by driving the robot hand to the points and recording the values of top center point(TCP) coordinates. The translation and rotation matrices relate either the two robot base frames or the workpiece and master robot. The coordinated are solved using the measured values of the calibration points according to the Cartesian transformation principle. An optimal method is developed based on exponential mapping of Lie algebra to ensure that the rotation matrix is orthogonal. Experimental results show that this method involves fewer steps, offers significant advantages in terms of operation and time-saving. A method used to synchronize workpiece frames in twin-robot system automatically is presented. | LU Zongxing XU Chunguang PAN Qinxue MENG Fanwu LI Xinliang | 2015 | Chinese Journal of Mechanical Engineering2015，28，4： | 6 |
| 6 | Multiple Dolomitization and Fluid Flow Events in the Precambrian Dengying Formation of Sichuan Basin, Southwestern China显示文摘The Precambrian Dengying Formation is a set of large-scale, extensively dolomitized, carbonate reservoirs occurring within the Sichuan Basin. Petrographic and geochemical studies reveal dolomitization was a direct result of precipitation by chemically distinct fluids occurring at different times and at different intensities. Based on this evidence, dolomitization and multiple fluid flow events are analyzed, and three types of fluid evolution models are proposed. Results of analysis show that Precambrian Dengying Formation carbonates were deposited in a restricted peritidal environment(630–542 Ma). A high temperature and high Mg^(2+) concentration seawater was a direct result of dolomitization for the micrite matrix, and for fibrous aragonite in primary pores. Geochemical evidence shows low δ^(18)O values of micritic dolomite varying from-1.29‰ to-4.52‰ PDB, abundant light rare earth elements(REEs), and low dolomite order degrees. Microbes and meteoric water significantly altered dolomite original chemical signatures, resulting in algal micritic dolomite and the fine-grained, granular, dolosparite dolomite having very negative δ^(18)O values. Finely crystalline cement dolomite(536.3–280 Ma) and coarsely crystalline cement dolomite have a higher crystallization degree and higher order degree. The diagenetic sequence and fluid inclusion evidence imply a linear correlation between their burial depth and homogenization temperatures, which closely resemble the temperature of generated hydrocarbon. Compared with finely crystalline dolomite, precipitation of coarsely crystalline dolomite was more affected by restricted basinal fluids. In addition, there is a trend toward a more negative δ^(18)O value, higher salinity, higher Fe and Mn concentrations, REE-rich. Two periods of hydrothermal fluids are identified, as the exceptionally high temperatures as opposed to the temperatures of burial history, in addition to the presence of high salinity fluid inclusions. The early hydrothermal fluid flow event was characterized by hot magnesium-and silicon-rich fluids, as demonstrated by the recrystallized matrix dolomite that is intimately associated with flint, opal, and microcrystalline quartz in intergranular or intercrystalline pores. This event was likely the result of a seafloor hydrothermal chimney eruption during Episode I of the Tongwan Movement(536.3±5.5 Ma). In contrast, later hydrothermal fluids, which caused precipitation of saddle dolomite, were characterized by high salinity(15–16.05 wt% NaCl equivalent) and homogenization temperatures(250 to 265°C), δ^(18)O values that were more enriched, and REE signatures. Geochemical data and the paragenetic sequence indicate that this hydrothermal fluid was related to extensive Permian large igneous province activity(360–280 Ma). This study demonstrates the presence of complicated dolomitization processes occurring during various paleoclimates, tectonic cycles, and basinal fluids flow; results are a useful reference for these dolomitized Precambrian carbonates reservoirs. | PENG Bo LI Zongxing LI Guorong LIU Chenglin ZHU Shifa ZHANG Wang ZUO Yinhui GUO Yingchun WEI Xiaojie | 2018 | Acta Geologica Sinica(English Edition)2018，92，1： | 5 |
| 7 | Recent Changes in Precipitation Extremes in the Heihe River Basin,Northwest China显示文摘Changes in rainfall extremes pose a serious and additional threat to water resources planning and management,natural and artificial oasis stability,and sustainable development in the fragile ecosystems of arid inland river basins. In this study,the trend and temporal variation of extreme precipitation are analyzed using daily precipitation datasets at 11 stations over the arid inland Heihe River basin in Northwest China from 1960 to 2011. Eight indices of extreme precipitation are studied.The results show statistically significant and large-magnitude increasing and decreasing trends for most indices,primarily in the Qilian Mountains and eastern Hexi Corridor. More frequent and intense rainfall extremes have occurred in the southern part of the desert area than in the northern portion. In general,the temporal variation in precipitation extremes has changed throughout the basin. Wet day precipitation and heavy precipitation days show statistically significant linear increasing trends and step changes in the Qilian Mountains and Hexi Corridor. Consecutive dry days have decreased obviously in the region in most years after approximately the late 1980 s,but meanwhile very long dry spells have increased,especially in the Hexi Corridor. The probability density function indicates that very long wet spells have increased in the Qilian Mountains. The East Asian summer monsoon index and western Pacific subtropical high intensity index possess strong and significant negative and positive correlations with rainfall extremes,respectively. Changes in land surface characteristics and the increase in water vapor in the wet season have also contributed to the changes in precipitation extremes over the river basin. | CHENG Aifang FENG Qi Guobin FU ZHANG Jiankai LI Zongxing HU Meng WANG Gang | 2015 | Advances in Atmospheric Sciences2015，32，10： | 5 |
| 8 | Meso-Cenozoic lithospheric thermal structure in the Bohai Bay Basin,eastern North China Craton显示文摘The Bohai Bay Basin is a region where part of the North China Craton has been thinned and destroyed. It has experienced two periods of crustal thinning that occurred during the Cretaceous and Paleogene, but investigations of its Mesozoic and Cenozoic lithospheric thermal structure are limited. Therefore, in this study,the distributions of mantle heat flow, crustal heat flow, and Moho temperatures during the Meso-Cenozoic are calculated based on analyses of the thermal history of the Bohai Bay Basin. The results indicate that the ratio of mantle heat flow to surface heat flow peaked during the late stages of the early Cretaceous and during the middle to late Paleogene. The corresponding mantle heat flow was more than 65% of the surface heat flow. Moho temperatures reached three peaks: 900-1100℃ in the late stages of the early Cretaceous;820-900℃ in the middle to late Paleogene; and(in the Linqing Depression, Cangxian Uplift, and Jizhong Depression) 770-810℃ during the early Neogene. These results reveal that the Bohai Bay Basin experienced significant geological change during the Cretaceous, including the transformation of lithospheric thermal structure from 'cold mantle and hot crust' before the Cretaceous to 'hot mantle and cold crust' after the Cretaceous. The results also indicate that the basin experienced two large-scale rifting events.Therefore, this work may provide the thermal parameters for further investigations of the geodynamic evolution of eastern China. | Zongxing Li Yinhui Zuo Nansheng Qiu Jun Gao | 2017 | Geoscience Frontiers2017，8，5： | 4 |
| 9 | Effect of sub-cloud evaporation on the δ^18O of precipitation in Qilian Mountains and Hexi Corridor, China显示文摘sub-cloud evaporation;;precipitation;;stable isotope;;Qilian | ZongXing Li Qi Feng YaMin Wang JianGuo Li XiaoYan Guo YongGe Li | 2016 | Research in Cold and Arid Regions2016，8，5： | 4 |
| 10 | Geothermal regime and hydrocarbon kitchen evolution in the Jianghan Basin显示文摘The present geothermal gradient and terrestrial heat flow was calculated of 18 wells in the Jianghan Basin.Thermal gradient distribution of the Jianghan Basin was obtained based on data of systematical steady-state temperature and oil-test temperature.The basin-wide average thermal gradient in depth interval of 0-4000 m is 33.59℃/km.We report nine measured terrestrial heat flow values based on the data of detailed thermal conductivity and systematical steady-state temperature.These values vary from 41.9 to 60.9 mW/m 2 with a mean of 52.3±6.3 mW/m 2.However,thermal history analyses based on vitrinite reflectance(VR) and apatite fission track(AFT) data indicate that thermal gradient in the northern and southern Qianbei Fault reached its peak of ~36 and ~39℃/km respectively in the Middle Jurassic and the Oligocene,and it descended during the early Miocene to the present-time value.Furthermore,tectonic subsidence analysis reveals that the tectonic subsidence of the Jianghan Basin in the Cretaceous to early Miocene was characterized by synrift initial subsidence followed by the subsequent thermal subsidence.The thermal history and tectonic subsidence history of Jianghan Basin are of great significance to petroleum exploration and hydrocarbon source assessment,because they bear directly on issues of petroleum source rock maturation.Based on the thermal history and tectonic subsidence history,with the combination of geochemical and thermal parameters,the maturation and the hydrocarbon generation intensity evolution history of the P2d source rocks are modeled.The results show that the P2d source rocks are in a higher degree of maturation at present,and the Yuan'an and Herong sags are the two most important kitchens in the Late Jurassic,Xiaoban Sag is another most important kitchen during the Late Cretaceous to late Paleogene,and the Zhijiang and Mianyang sags are other two important hydrocarbon kitchens in the Late Cretaceous.The Mianyang Sag and Yichang Ramp are the favorable exploration targets in the future.This study may provide new insight for the understanding of the oil and gas exploration potential for the Jianghan Basin. | LI ZongXing XU Ming ZHAO Ping SUN ZhanXue ZHU ChuanQing | 2013 | Science China Earth Sciences2013，56，2： | 3 |
| 11 | Discovery of Palaeozoic Karsts in the Qaidam Basin and Their Oil and Gas Prospects显示文摘Objective Complex geological factors have been constraining the oil and gas exploration in the Paleozoic strata of the Qaidam Basin,although there are high-quality hydrocarbon source rocks.One of the most important reasons may be reservoir densification due to the multiple stages of destructive cementation,which has hindered our understanding of the Paleozoic petroleum enrichment rules in the Qaidam basin.In recent years,the | PENG Bo LIU Chenglin LI Zongxing MA Yinsheng CAO Jun WANG Bing ZHANG Xu | 2016 | Acta Geologica Sinica(English Edition)2016，90，5： | 2 |
| 12 | Geothermal Field and Tectono-Thermal Evolution since the Late Paleozoic of the Qaidam Basin,Western China显示文摘The Qaidam basin is the largest intermountain basin inside Tibet,and is one of the three major petroliferous basins in western China.This study discussed the geothermal field and tectono-thermal evolution of the basin,in an effort to provide evidence for intracontinental or intraplate continental dynamics and basin dynamics,petroleum resources assessment,and to serve petroleum production. | LI Zongxing LIU Chenglin MA Yinsheng | 2015 | Acta Geologica Sinica(English Edition)2015，89，2： | 2 |
| 13 | Changes of daily climate extremes in southwestern China during 1961–2008显示文摘 | Li Zongxing Yuanqing He Puyu Wang Wilfred H. Theakstone Wenling An Xufeng Wang Aigang Lu Wei Zhang Weihong Cao | 2011 | Global and Planetary Change2011，，： | 2 |
| 14 | Time-varying sliding mode control of missile based on suboptimal method显示文摘This paper proposes a time-varying sliding mode control method to address nonlinear missile body kinematics based on the suboptimal control theory.The analytical solution of suboptimal time-varying sliding surface and the corresponding suboptimal control law are obtained by solving the state-dependent Riccati equation analytically.Then,the Lyapunov method is used to analyze the motion trend in sliding surface and the asymptotic stability of the closed-loop system is validated.The suboptimal control law is transformed to the form of pseudo-angle-of-attack feedback.The simulation results indicate that the satisfactory performance can be obtained and the control law can overcome the influence of parameter errors. | LI Zongxing ZHANG Rui | 2021 | Journal of Systems Engineering and Electronics2021，32，3： | 2 |
| 15 | Changes of the hydrological cycle in two typical Chinese monsoonal temperate glacier basins,: A response to global warming?显示文摘学习反应到在瓷器适度的冰河区域水文学系统温暖是必要的以便提供为持续开发要求的信息。结果显示温暖的气候影响了水文学周期。当到融化的冰河区域题目增加了,脱离季节变得更长,到年度河分泌物的 meltwater 的贡献增加了。在更高的举起冰河的脱离的更早的发作导致了在一年更早发生的最小的分泌物的时期。季节的流量变化被雪和冰河统治融化,并且 meltwater 的增加在丽江盆和 Hailuogou 盆导致了年度水周期的变化。在冰川的区域的下游的区域的流量的增加振幅比降水的强壮得多,源于从在二盆的冰河区域的 meltwater 的突出的增加。在 glacierized 盆的继续的观察应该被承担以便监视变化,以揭示在气候,冰河,水文学和水供应之间的关系,并且在维持持续地区性的开发帮助。 | PANG Hongxi LI Zongxing Wilfred H. THEAKSTONE | 2012 | Journal of Geographical Sciences2012，22，5： | 1 |
| 16 | Thermal History since the Paleozoic in the Eastern Qaidam Basin,Northwest China显示文摘The Qaidam Basin is the one of the three major petroliferous basins in northeastern Tibetan Plateau, which has experienced multiphase superimposition and transformation. The study of thermal history not only plays an important role on revealing the tectonic origin of the Qaidam Basin and the forming mechanism and uplift history of the Tibetan Plateau,but also can provide scientific evidence for the assessment of oil and gas resources. This work used balanced cross-section technique and apatite fission track ages with modeling of fission track length distribution to infer that the eastern Qaidam Basin has experienced significant tectonic movement in the Early Jurassic movement(~200 Ma), which caused the carboniferous uplift and denudation, the geological movement in the Late Cretaceous, characterized by early stretching and late northeast-southwest extrusion; the Himalayan movement in multi-stage development in eastern Qaidam Basin, which can be divided into the early Himalayan movement(41.1–33.6 Ma) and the late Himalayan movement(9.6–7.1 Ma, 2.9–1.8 Ma), and large-scale orogeny caused pre-existing faults reactivated in late Himalayan movement. On the basis of burial history reconstruction, the thermal history of eastern Qaidam Basin was restored. The result shows that the thermal history in eastern Qaidam Basin shows slow cooling characteristics; the paleo-geothermal gradient of eastern Qaidam Basin was 38–41.5℃/km, with an average value of 39.0℃/km in the Late Paleozoic, 29–35.2℃/km, with an average value of 33.0℃/km in the Early Paleogene; the geothermal gradient of the Qaidam Basin increased in the Late Paleogene, which was similar to the present geothermal gradient in the Late Neogene. The characteristics of the tectono-thermal evolution since Paleozoic in the eastern Qaidam Basin are mainly controlled by magmatic thermal events in the study area. | WANG Li LI Zongxing LIU Chenglin PENG Bo FANGXinxin YUAN Guide | 2019 | Acta Geologica Sinica(English Edition)2019，93，2： | 1 |
| 17 | Physical growth of children and adolescents inChina over the past 35 years显示文摘 | ZongX N Li H | 2014 | Bull World Health Organ2014，92，8： | 1 |
| 18 | Hydraulic redistribution of soil water by roots of two desert riparian phreatophytes in northwest China’s extremely arid region显示文摘 | Tengfei Yu Qi Feng Jianhua Si Haiyang Xi Zongxing Li Aifang Chen | 2013 | Plant and Soil (-)2013，，1： | 1 |
| 19 | Altitude effects of climatic variation on Tibetan Plateau and its vicinities显示文摘 | Lu Aigang Kang Shichang Li Zongxing | 2010 | Journal of Earth Science2010，21，18： | 1 |
| 20 | Abscisic acid and hydrogen peroxide induce a novel maize group C MAP kinase gene, ZmMPKT, which is responsible for the removal of reactive oxygen species显示文摘 | ZongX J LiD P Gu L K Li D Q Liu L X Hu X L | 2009 | Planta2009，229，3： | 1 |
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