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| 1 | Estimating Moho basement and faults using gravity inversion in Yushu-earthquake area,China显示文摘A gravity survey was conducted one month after the 2010 Yushu earthquake in the epicenter area.The cross-fault survey line was 500 km long,from Langqian county to Qingshuihe county,in a transition zone between Bayan Har block and Qiangtang block,in an area of high elevation,large undulating terrain,and complex geological features.An interpretation of the data was carried out together with other kinds of data,such as seismic exploration and magnetic exploration.The result shows that gravity is sensitive to fault boundary;the geologic structure of the region is complex at middle and upper depths,and the density profile reveals an eastward-pushing fault movement. | Yang Guangliang | 2012 | Geodesy and Geodynamics2012，3，2： | 4 |
| 2 | A Method for Crude Oil Selection and Blending Optimization Based on Improved Cuckoo Search Algorithm显示文摘Refineries often need to find similar crude oil to replace the scarce crude oil for stabilizing the feedstock property. We introduced the method for calculation of crude blended properties firstly, and then created a crude oil selection and blending optimization model based on the data of crude oil property. The model is a mixed-integer nonlinear programming(MINLP) with constraints, and the target is to maximize the similarity between the blended crude oil and the objective crude oil. Furthermore, the model takes into account the selection of crude oils and their blending ratios simultaneously, and transforms the problem of looking for similar crude oil into the crude oil selection and blending optimization problem. We applied the Improved Cuckoo Search(ICS) algorithm to solving the model. Through the simulations, ICS was compared with the genetic algorithm, the particle swarm optimization algorithm and the CPLEX solver. The results show that ICS has very good optimization efficiency. The blending solution can provide a reference for refineries to find the similar crude oil. And the method proposed can also give some references to selection and blending optimization of other materials. | Yang Huihua Ma Wei Zhang Xiaofeng Li Hu Tian Songbai | 2014 | China Petroleum Processing & Petrochemical Technology2014，16，4： | 4 |
| 3 | Weak Hardy-type spaces associated with ball quasi-Banach function spaces I:Decompositions with applications to boundedness of Calderón-Zygmund operators显示文摘Let X be a ball quasi-Banach function space on R^(n).In this article,we introduce the weak Hardytype space WH_(X)(R^(n)),associated with X,via the radial maximal function.Assuming that the powered HardyLittlewood maximal operator satisfies some Fefferman-Stein vector-valued maximal inequality on X as well as it is bounded on both the weak ball quasi-Banach function space WX and the associated space,we then establish several real-variable characterizations of WH_(X)(R^(n)),respectively,in terms of various maximal functions,atoms and molecules.As an application,we obtain the boundedness of Calderón-Zygmund operators from the Hardy space H_(X)(R^(n))to WH_(X)(Rn),which includes the critical case.All these results are of wide applications.Particularly,when X:=M^(q)_(p)(R^(n))(the Morrey space),X:=L^(p)(R^(n))(the mixed-norm Lebesgue space)and X:=(EΦq)t(Rn)(the Orlicz-slice space),which are all ball quasi-Banach function spaces rather than quasiBanach function spaces,all these results are even new.Due to the generality,more applications of these results are predictable. | Yangyang Zhang Dachun Yang Wen Yuan Songbai Wang | 2021 | Science China Mathematics2021，64，9： | 3 |
| 4 | Temporal gravity changes before the 2008 Yutian Ms7.3 earthquake显示文摘Based on the data of the repeated gravity observation network in Chinese mainland since 1998,we analyzed the temporal changes of regional gravity field before the 2008 Yutian Ms7.3 earthquake.The result shows some mid-to-long term(two to ten years)changes during the earthquake's preparation.Notable features are a gravity increase lasting several years and a relatively large-scaled gradient zone of gravity change,the former indicating a continuous energy accumulation and the latter a possible location of seismic rupture.These gravity changes showed a trend of increase-accelerated increase-decelerated increase,similar to that of the Tangshan Ms7.8 earthquake in 1976.The maximum accumulated gravity change related to the earthquake reached 200×10-8 ms-2. | Shen Chongyang Li Hui Sun Shaoan Yang Guangliang Xuan Songbai Tan Hongbo Liu Shaoming | 2012 | Geodesy and Geodynamics2012，3，1： | 3 |
| 5 | Poly (DL-lactic acid) surfaces modified by silk fibroin: ettects on the culture of osteoblast in vitro显示文摘 | Kaiyong Cai Kangde Yao Songbai Lin Zhiming Yang Xiuqiong Li Huiqi Xie Tingwu Qing and Laibao Gao | 2002 | Biomaterials2002，23，4： | 1 |
| 6 | Wenchuan Ms8.0 earthquake coseismic slip distribution inversion显示文摘By using GPS and gravity data before and after the Wenchuan Ms8.0 earthquake and combining data from geological surveys and geophysical inversion studies, an initial coseismic fault model is constructed. The dip angle changes of the fault slip distribution on the fault plane are inversed, and the inversion results show that the shape of the fault resembles a double-shovel. The Yingxiue Beichuan Fault is approximately 330 km long, the surface fault dip angle is 65.1, which gradually reduces with increasing depth to 0 at the detachment layer at a depth of 19.62 km. The Guanxiane Jiangyou Fault is approximately90 km long, and its dip angle at the surface is 55.3, which gradually reduces with increasing depth; the fault joins the Yingxiue Beichuan Fault at 13.75 km. Coseismic slip mainly occurs above a depth of 19 km. There are five concentrated rupture areas, Yingxiu,Wenchuan, Hanwang, Beichuan, and Pingwu, which are consistent with geological survey results and analyses of the aftershock distribution. The rupture mainly has a thrust component with a small dextral strikeeslip component. The maximum slip was more than10 m, which occurred near Beichuan and Hanwang. The seismic moment is 7.84 1020 Nm(Mw7.9), which is consistent with the seismological results. | Tan Hongbo Wu Guiju Xuan Songbai Yang Guangliang Fan Wenhua Shen Chongyang | 2015 | Geodesy and Geodynamics2015，6，3： | 1 |
| 7 | Fetal umbilical vein transplantation for the repair of middle cerebral artery injury显示文摘It is necessary to investigate the longitudinal tensile mechanical characteristics of the middle cerebral artery and the fetal umbilical vein prior to applying fetal umbilical vein transplantation fo repair of injured middle cerebral artery.Fifteen fresh fetal umbilical vein specimens and 15 norma human fresh cadaver middle cerebral artery specimens were collected for longitudinal tensile testing at the speed of 0.5 mm/min and at normal human temperature.The results showed that under 16.0 kPa physiological stress,the strain value of fetal umbilical vein specimens was larger while the maximal stress and elastic modulus values were less than those of middle cerebral artery specimens.Our findings indicate that fetal umbilical vein has good elastic properties and the stress-strain curve of the fetal umbilical vein is similar to that of the middle cerebral artery.Feta umbilical vein transplantation can,therefore,potentially repair the injured middle cerebral artery. | Xuhui Hou Yi Yuan Jian Yin Songbai Yang Lili Xie Shiji Wang | 2013 | Neural Regeneration Research2013，8，34： | 1 |
| 8 | Molecular characterization, induced expression, and transcriptional regulation of porcine S100A12 gene显示文摘 | Hongbo Chen Lei Cheng Songbai Yang Xiangdong Liu Ying Liu Juan Tang Xinyun Li Qigai He Shuhong Zhao | 2010 | Molecular Immunology2010，，7： | 1 |
| 9 | Effects of brachial plexus injury anastomosis simulation on biomechanical properties of adult brachial plexus显示文摘BACKGROUND:Previous studies of peripheral nerve mechanical properties in animals have utilized one-dimensional drawing methods. OBJECTIVE:To analyze the effects of brachial plexus injury anastomosis simulation on biomechanical properties of adult brachial plexus by observing tensile mechanical properties,stress relaxation,and creep deformation of the brachial plexus in normal human cadavers and brachial plexus from simulated brachial plexus injury anastomosis samples. DESIGN,TIME AND SETTING:The in vitro experiment was performed at the Mechanics Experimental Center,Jilin University,China from April to May 2007. MATERIALS:A total of six adult,male cadavers,who had died from acute trauma,and were aged 20-29 years,were supplied by the Research Room of Anatomy,Medical Department,Jilin University,China. AG-10TA Universal Material Testing Machine (Shimadzu,Japan) was used in this study. METHODS:A total of 36 samples of fresh brachial plexus were collected from the cadavers,comprising 12 C5 nerve roots,12 C6 nerve roots at the left and right sides of the superior truck,and 12 C7 nerve roots at the middle truck. The C5 and C6 nerve roots were processed into 50 samples and the C7 nerve roots into 24 samples. A total of 36 C5 and C6 nerve root samples were randomly assigned to a non-surgery control group (n = 18) and brachial plexus injury anastomosis simulation group (n = 18). Brachial plexus injury simulation anastomosis samples underwent an incision in the middle,and then received anastomosis. Samples in both groups underwent a tension test at 5 mm/min on the AG-10TA universal material testing machine. A total of 24 sam-ples from the C6 superior trunk and C7 middle trunk of the brachial plexus were subjected to stress relaxation and creep tests. Test duration was 7 200 seconds. A total of 100 data points were collected and analyzed using a normalization method. MAIN OUTCOME MEASURES:The following parameters were measured:tension maximum displacement,maximum load,maximum stress,maximum strain and stress-strain curve,stress relaxation at 7 200 seconds,creep deformation at 7 200 seconds,stress relaxation,and creep curve in the non-surgery control group and brachial plexus injury simulation anastomosis group. RESULTS:The tension maximum load of brachial plexus was (140.36 ± 30.50) N,maximum stress was (10.67 ± 2.52) MPa,maximum displacement was (7.78 ± 1.48) mm,and maximum strain was (31.64 ± 5.32)% in the non-surgery control group. The tension maximum load of brachial plexus was (93.23 ± 20.65) N,maximum stress was (7.09 ± 1.57) MPa,maximum displacement was (6.13 ± 0.86) mm,and maximum strain was (24.55 ± 3.45)% in the brachial plexus injury simulation anastomosis group. The above-mentioned indices were greater in the non-surgery control group than in the brachial plexus injury simulation anastomosis group (P < 0.01). Stress relaxation at 7 200 seconds was 2.07 MPa and 2.11 MPa,respectively,in the non-surgery control and brachial plexus injury simulation anastomosis groups. Creep deformation at 7 200 seconds was 4.68% and 3.52%,respectively,in the non-surgery control and brachial plexus injury simulation anastomosis groups. CONCLUSION:Decreased tension maximum load,maximum displacement,maximum stress,maximum strain,and creep deformation at 7 200 seconds affected the biomechanical properties of the brachial plexus following brachial plexus injury. | Xuhui Hou Xinying Li Songbai Yang Jian Yin Hongshun Ma | 2010 | Neural Regeneration Research2010，5，6： | 1 |
| 10 | Highly Effective Inactivation of Pseudomonas sp HB1 in Water By Atmospheric Pressure Microplasma Jet Array显示文摘 | Xianhui Zhang Dongping Liu Hongzhe Wang Linying Liu Songbai Wang Si-ze Yang | 2012 | Plasma Chemistry and Plasma Processing2012，，： | 1 |
| 11 | The Absence of LPA 2 Attenuates Tumor Formation in an Experimental Model of Colitis-Associated Cancer显示文摘 | Songbai Lin Dongsheng Wang Smita Iyer Amr M. Ghaleb Hyunsuk Shim Vincent W. Yang Jerold Chun C. Chris Yun | 2009 | Gastroenterology2009，，5： | 1 |
| 12 | Isostatic anomaly characteristics and tectonism of the New Britain Trench and neighboring Papua New Guinea显示文摘In this paper, we calculated Bouguer gravity anomalies and Airy-Heiskanen isostatic anomalies in the New Britain Trench and surrounding areas of Papua New Guinea. The calculations are based on a topographic model and a gravity anomaly model from the Scripps Institute of Oceanography. Characteristics of the isostatic anomaly and the earthquake dynamic environment of this region are analyzed,and the results show that there are obvious differences in the isostatic state between each block in the region. Tectonic movements are very intense in regions with high positive or negative isostatic gravity anomalies, and a number of sub-plates in this area are driven by external tectonic action, such as plate subduction and thrusting, of the Pacific, Indo-Australian and Eurasian plates. From the distribution of the isostatic gravity anomaly, the tectonic action of anti-isostatic movement obviously is the main source of power. Based on isostatic gravity and spatial distribution of earthquakes in the region, it is obvious that further contraction of the Indo-Australian Plate will result in the southwestern part of the Solomon Plate becoming part of the Owen Stanley thrust belt, and the northern part will enter the lower part of the Bismarck Plate. The eastern part of the Solomon Plate will enter the front of the Pacific Plate, resulting in northward and eastward migration of significant earthquakes along the Solomon Plate. | Guangliang Yang Chongyang Shen Jiapei Wang Songbai Xuan Guiju Wu Hongbo Tan | 2018 | Geodesy and Geodynamics2018，9，5： | 1 |
| 13 | Genetic diversity of RNA viruses infecting invertebrate pests of rice显示文摘Invertebrate species are a natural reservoir of viral genetic diversity,and invertebrate pests are widely distributed in crop fields.However,information on viruses infecting invertebrate pests of crops is limited.In this report,we describe the deep metatranscriptomic sequencing of 88 invertebrate samples covering all major invertebrate pests in rice fields.We identified 296 new RNA viruses and 13 known RNA viruses.These viruses clustered within 31 families,with many highly divergent viruses constituting potentially new families and genera.Of the identified viruses,13 RNA viruses clustered within the Fiersviridae family of bacteriophages,and 48 RNA viruses clustered within families and genera of mycoviruses.We detected known rice viruses in novel invertebrate hosts at high abundances.Furthermore,some novel RNA viruses have genome structures closely matching to known plant viruses and clustered within genera of several plant virus species.Fortyfive potential insect pathogenic RNA viruses were detected in invertebrate species.Our analysis revealed that host taxonomy plays a major role and geographical location plays an important role in structuring viral diversity.Cross-species transmission of RNA viruses was detected between invertebrate hosts.Newly identified viral genomes showed extensive variation for invertebrate viral families or genera.Together,the large-scale metatranscriptomic analysis greatly expands our understanding of RNA viruses in rice invertebrate species,the results provide valuable information for developing efficient strategies to manage insect pests and virus-mediated crop diseases. | Haoran Wang Shufen Chao Qing Yan Shu Zhang Guoqing Chen Chonghui Mao Yang Hu Fengquan Yu Shuo Wang Liang Lv Baojun Yang Jiachun He Songbai Zhang Liangsheng Zhang Peter Simmonds Guozhong Feng | 2024 | Science China(Life Sciences)2024，67，1： | 0 |
| 14 | Discovery and Tectonic Significance of Paleoproterozoic Ophiolite from North Huangling Dome, Yangtze Craton显示文摘 | HAN Qingsen PENG Songbai CEN Yang JIANG Xingfu | 2015 | Acta Geologica Sinica(English Edition)2015，89，A02： | 0 |
| 15 | Influence of crustal layering and thickness on co-seismic effects of Wenchuan earthquake显示文摘Using the PSGRN/PSCMP software and the fault model offered by USGS and on the basis of finite rectangular dislocation theory and the local layered wave velocity structures of the crust-upper-mantle, the influences of crustal layering and thickness on co-seismic gravity changes and deformation of Wenchuan earthquake have been simulated. The results indicate that: the influences have a relationship with the attitude of faults and the relative position between calculated points and fault. The difference distribution form of simulated results between the two models is similar to that of co-seismic effect. For the per centum distribution, it's restricted by the zero line of the co-seismic effects obviously. Its positive is far away from the zero line. For the crustal thickness, the effect is about 10%-20%. The negative and the effect over 30% focus around the zero line. The average influences of crustal layering and thickness for the E-W displacement, N-S displacement, vertical displacement and gravity changes are 18.4%,18.0%,15.8% and 16.2% respectively,When the crustal thickness is 40 km, they are 4.6%,5.3%,3.8% and 3.8%. Then the crustal thickness is 70 km, the average influences are 3.5%, 4.6%,3.0% and 2.5% respectively. | Tan Hongbo Shen Chongyang Xuan Songbai Yang Guangliang | 2011 | Geodesy and Geodynamics2011，2，1： | 0 |
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