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| 1 | Variations of temperature and precipitation of snowmelt period and its effect on runoff in the mountainous areas of Northwest China显示文摘在西北中国的干旱陆地的水资源主要源于雪和冰河在多山的区域融化水。snowmelt 时期的发作,停止,长度,温度和降水上的学习因此具有为相当分配有限的水资源并且采取科学的水资源管理措施的大意义。用从在时期上的 8 个多山的气象站的每日的吝啬的温度和降水 19602010 在西北中国的干旱陆地,这份报纸分析 snowmelt 时期和它的空间变化的气候变化并且探索流量的敏感到 snowmelt 的长度,温度和降水时期。结果证明当吝啬的结束日期 9.19 天以后移动了时, snowmelt 时期的那吝啬的发作 15.33 天早变了。当那仅仅 10.16 天早在北 Qilian 山移动了时,在南部的 Tianshan 山的 snowmelt 时期的发作 20.01 天早移动了。吝啬的降水和空气温度由 47.3 公里增加了并且 0. | LI Baofu CHEN Yaning CHEN Zhongsheng LI Weihong ZHANG Baohuan | 2013 | Journal of Geographical Sciences2013，23，1： | 14 |
| 2 | Preparation and anisotropic properties of textured structural ceramics: A review显示文摘Ceramics are usually composed of randomly oriented grains and intergranular phases, so their properties are the statistical average along each direction and show isotropy corresponding to the uniform microstructures. Some methods have been developed to achieve directional grain arrangement and preferred orientation growth during ceramic preparation, and then textured ceramics with anisotropic properties are obtained. Texture microstructures give particular properties to ceramics along specific directions, which can effectively expand their application fields. In this review, typical texturing techniques suitable for ceramic materials, such as hot working, magnetic alignment, and templated grain growth(TGG), are discussed. Several typical textured structural ceramics including α-Al2O3 and related nacre bioinspired ceramics, Si3N4 and SiAlON, h-BN, MB2 matrix ultra-high temperature ceramics, MAX phases and their anisotropic properties are presented. | Zhuo ZHANG Xiaoming DUAN Baofu QIU Zhihua YANG Delong CAI Peigang HE Dechang JIA Yu ZHOU | 2019 | Journal of Advanced Ceramics2019，8，3： | 14 |
| 3 | Hydrological and water cycle processes of inland river basins in the arid region of Northwest China显示文摘The increasing shortage in water resources is a key factor affecting sustainable socio-economic development in the arid region of Northwest China(ARNC). Water shortages also affect the stability of the region's oasis ecosystem. This paper summarizes the hydrological processes and water cycle of inland river basins in the ARNC, focusing on the following aspects: the spatial-temporal features of water resources(including air water vapor resources, runoff, and glacial meltwater) and their driving forces; the characteristics of streamflow composition in the inland river basins; the characteristics and main controlling factors of baseflow in the inland rivers; and anticipated future changes in hydrological processes and water resources. The results indicate that:(1) although the runoff in most inland rivers in the ARNC showed a significant increasing trend, both the glaciated area and glacial ice reserves have been reduced in the mountains;(2) snow melt and glacier melt are extremely important hydrological processes in the ARNC, especially in the Kunlun and Tianshan mountains;(3) baseflow in the inland rivers of the ARNC is the result of climate change and human activities, with the main driving factors being the reduction in forest area and the over-exploitation and utilization of groundwater in the river basins; and(4) the contradictions among water resources, ecology and economy will further increase in the future. The findings of this study might also help strengthen the ecological, economic and social sustainable development in the study region. | CHEN Yaning LI Baofu FAN Yuting SUN Congjian FANG Gonghuan | 2019 | Journal of Arid Land2019，11，2： | 12 |
| 4 | Discovery of mantle and lower crust xenoliths from early Cretaceous volcanic rocks of southwestern Tianshan,Xinjiang显示文摘In Tuoyun area of southwestern Tianshan, mantle and lower crust xenoliths are present In the volcanic rocks with ages of 101-123 Ma. Mantle xenoliths include mineral megacrysts such as kaersutite and pargasite, feldspar, biotite, and rare pyroxene and rock fragments such as perodotite, pyroxenite, amphibolite, and rare glimmerite. Lower crust xenoliths are mainly banded and massive granulite. The volcanic rocks were produced by within-plate magmatism. Occurrence of hydrous and volatile mineral megacrysts, amphibolite, and some pyroxenite containing hydrous and volatile minerals indicates that mantle metasomatism was intense. Undoubtedly, this discovery is very important to understanding of the crust-mantle structure and geodynamic background in depth in southwestern Tianshan and geological correlation with adjacent regions. | Baofu Han Xuechao Wang Guoqi He Tairan Wu Maosong Li Yulin Liu Shiguang Wang | 1999 | Chinese Science Bulletin1999，44，12： | 11 |
| 5 | 华北克拉通西部陆块北缘新生代岩石圈地幔特征的初步研究显示文摘凉城、四子王旗、三义堂和大同的地幔包体的岩石学和矿物的主、微量元素成分显示华北克拉通中、西部北缘总体为过渡型岩石圈地幔,为原始地幔经过不同程度的熔体抽取和后期交代富集作用的残留。凉城岩石圈地幔经历的熔体抽取程度最低,后期交代富集作用比较强烈,这与其橄榄岩中尖晶石的Cr#较低,并且共存的单斜辉石的Mg#较低一致。三义堂岩石圈地幔经历的熔体抽取程度最高,后期交代富集作用最强烈,不同样品甚至同一样品中不同单斜辉石颗粒的La/Yb和LREE配分模式变化范围非常大,且矿物边部比核部更富集微量元素。大同、四子王旗岩石圈地幔经历的熔体抽取程度介于凉城和三义堂之间,但后期的交代富集作用明显不如凉城和三义堂强烈。研究区的岩石圈地幔主要受硅酸盐熔体交代作用的影响,只有三义堂岩石圈地幔还可能也受到了碳酸盐交代作用的影响。 | 王亚妹 William L GRIFFIN 韩宝福 WANG YaMei HAN BaoFu | 2011 | 岩石学报2011，27，10： | 9 |
| 6 | Reconstruction of sea surface temperature series in the last 220 years by use of reef corals in Xisha waters, South China Sea显示文摘On the basis of construction of the growth rate thermometers by use of Ponies lutea from the northern part of the South China Sea and the hindcast sea surface temperature (SST) in the last 100 years, we reconstructed the SST series in the past 220 years in the Xisha waters and analyzed the characteristics of the climatic change of that period. The results show that | Baofu Nie Tegu Chen Zicheng Peng | 1999 | Chinese Science Bulletin1999，44，22： | 6 |
| 7 | Geochemical characteristics of the metapelites from the Xingxingxia group in the Eastern Segment of the Central Tianshan:Implications for the provenance and paleoweathering显示文摘Metapelites from the Mesoproterozoic Xingxingxia group in the Eastern Segment of the Central Tianshan, Northwestern China, were analyzed for major and trace elements, includ-ing rare earth elements. Compared with post-Archean shales, the metapelites are enriched in Sr, Hf and Zr. The other elements are similar to the compositions of the Phanerozoic North American Shale Composite and the Post-Archean Australian average Shale (PAAS). The characteristics of Al2O3/TiO2, Cr/Zr, Cr/Th, Th/Sc and high Zr concentration suggest that these pelites could be derived from a significant proportion of felsic and a few proportion of participation of mafic mate-rials in nature. These rocks display highly fractionated REE patterns, and average (La/Yb)n = 18.6. Several samples have slightly negative Eu anomalies (Eu/Eu* = 0.7―0.84) in comparison with PAAS (Eu/Eu* = 0.65), indicating contribution from young immature materials. The low K2O/Al2O3 values of these metapelites suggest that their source materials could contain minimal alkali feldspar. In the A-CN-K triangular diagram, the sample data array intersects the feldspar join, indicating that the source had a plagioclase: K-feldspar ratio of approximately 5:1, repre-senting weathered products from components that could approximately correspond to granodio-rites and tonalites. The low Chemical Index of Alteration (CIA) and high Index of Compositional Variability (ICV) values suggest low degrees of weathering of the source and low compositional maturity of the sediments, respectively. The geochemical characteristics of the metapelites from the Xingxingxia group also demonstrate that these sediments were deposited in a back-arc background within a continental-arc system. | LI Qiugen LIU Shuwen HAN Baofu WANG Yueran DANG Qingning | 2005 | Science China Earth Sciences2005，48，10： | 4 |
| 8 | Platinum-group element geochemistry of Cenozoic basalts from the North China Craton: Implications for mantle heterogeneity显示文摘42 新生代(主要中新世) 从北方中国 Craton 的 Jining, Chifeng, Fansi, Xiyang,和 Zuoquan 区域的暗岩样品(NCC 暗岩此后) 为铂组元素(PGE,包括的 O,红外, Ru, Rh,磅,和 Pd ) 被分析。他们中的大多数是碱的暗岩和 tholeiites,所有几乎不他们显示很少外壳的污染。NCC 暗岩的全部的 PGE 内容从 0.1 ~ 0.9 ppb 变化,原始披风的比那些低的大部分 23.5 珍视 ppb。这些暗岩的原始使披风正常化的 PGE 模式定义积极斜坡和 Pd/Ir 比率从 1.2 ~ 25 变化。以 PGE 内容和 Pd/Ir 比率,他们相当类似于海中央山脉暗岩。在 PGE 之间没有明显的否定关联,显示在 magmatic 期间的橄榄石,辉石,或硫化物的部分结晶化处理对在 NCC 暗岩的 MgO, Ni,和 Cu 不能是为观察 PGE 变化的控制因素。NCC 暗岩的观察 Pd/Ir 变化要求异构的披风采购的 non-chondritic 的参与。基于 Sr-Nd-Pb-Hf 同位素的 systematics 和不兼容元素的签名,一混合部分在岩流圈的顶从 asthenospheric 橄榄岩和围住的披风 eclogites 融化为这些 NCC 暗岩的起源被建议。eclogites 的透镜从再循环的大陆人外壳的 upwelling 被导出在期间向西从 600 km 断绝地区的和平的板的 subduction。这些暗岩的 PGE 地球化学提供独立证据支持这个结论和观察 Pd/Ir 变化可以在拍的 peridotitic 的比例反映变化, eclogitic 融化。 | ZHANG WenHui ZHANG HongFu SUN YaLi FAN WeiMing HAN BaoFu TANG YanJie | 2015 | Science China Earth Sciences2015，58，6： | 4 |
| 9 | H_2S Gas Sensitivity of Nanocrystalline Tin Dioxide Doped with Ytterbium (Yb) and Praseodymium (Pr)显示文摘<正>The influence of Yb_2O_3 and Pr_2O_3 doping on electrical and gas sensing properties of tin dioxide was studied.A doping content of 0.5wt%~5wt% was investigated by mechanical mixing.The significant improvement on sensitivity and selectivity to 200μg/g hydrogen sulphide gas has been achieved by 3wt% Pr_2O_3 and 5wt% Yb_2O_3 adding.The better response and revovery properties of Pr or Yb doped tin dioxide sensor for 200μg/g hydrogen sulphide gas were found.The maximum sensitivity to H_2S gas is observed at about 120℃.Pr has stronger catalysis than Yb for H_2S reaction on SnO_2 surface.S~ 2-) was oxidized to S~ 6+) on the SnO_2 surface according to XPS. | Fengmin Liu Xishuang Liang Yuehua He Biao Wang Baofu Quan | 2006 | 稀有金属材料与工程2006，35，A03： | 2 |
| 10 | A Hierarchical Approach Based on Fast Marching Method in Multi Player Pursuit-Evasion Game显示文摘 | FANG Baofu PAN Qishu HONG Bingrong PIAO Songhao CAI Zesu DING Lei | 2012 | Chinese Journal of Electronics2012，21，1： | 2 |
| 11 | Microstructural evolution of h-BN matrix composite ceramics with La-Al-Si-O glass phase during hot-pressed sintering显示文摘BN/La-Al-Si-O composite ceramics were fabricated by hot-pressed sintering using hexagonal boron nitride(h-BN),lanthanum oxide(La_(2)O_(3)),aluminia(Al_(2)O_(3)),and amorphous silica(SiO_(2))as the raw materials.The effects of sintering temperature on microstructural evolution,bulk density,apparent porosity,and mechanical properties of the h-BN composite ceramics were investigated.The results indicated that La-Al-Si-O liquid phase was formed during sintering process,which provided an environment for the growth of h-BN grains.With increasing sintering temperature,the cristobalite phase precipitation and h-BN grain growth occurred at the same time,which had a significant influence on the densification and mechanical properties of h-BN composite ceramics.The best mechanical properties of BN/La-Al-Si-O composite ceramics were obtained under the sintering temperature of 1700℃.The elastic modulus,flexural strength,and fracture toughness were 80.5 GPa,266.4 MPa,and 3.25 MPa·m^(1/2),respectively. | Baofu QIU Xiaoming DUAN Zhuo ZHANG Chen ZHAO Bo NIU Peigang HE Delong CAI Lei CHEN Zhihua YANG Yujin WANG Dechang JIA Yu ZHOU | 2021 | Journal of Advanced Ceramics2021，10，3： | 2 |
| 12 | High resolution Porites Mg/Ca thermometer for the north of the South China Sea显示文摘High resolution Mg/Ca ratios in the skeleton of a Porites lutea from the coastal area in the North of the South China Sea were precisely analyzed by ICP-MS. Compared with the instrument measured SST records, the Mg/Ca ratios strongly correlate with the SSTs, even in time of 1982/83 EI N(?)io. Therefore, a coral Mg/Ca thermometer for the North of the South China Sea was established.Based on ICP-MS technique it can report sea surface temperatures to an accuracy of±0.5℃. | Gangjian Wei Xianhua Li Baofu Nie Min Sun Haichen Liu | 1999 | Chinese Science Bulletin1999，44，3： | 2 |
| 13 | Depletedmantle source for the Ulungur River A-type granites from North Xinjiang, China: Geochemistry and Nd-Sr isotopic evidence, and implication for Phanerozoie crustal growth显示文摘 | Han baofu Wang shiguang Jahn borming | 1997 | Chemical Geology1997，138，： | 1 |
| 14 | Structure of1-butylpyridinium tetrafluoroborate ionic liquid:quantum chemistry and molecular dynamic simulationstudies显示文摘 | Sun Hui Qiao Baofu Zhang Dongju | 2010 | J Phys Chem A2010，114，11： | 1 |
| 15 | Age, geochemistry, and tectonic implications of a late Paleozoic stitching pluton in the North Tian Shan suture zone, western China显示文摘 | Han Baofu Guo Zhaojie Zhang Zhieheng | 2010 | Geological Society of America Bulletin2010，122，： | 1 |
| 16 | Structural integrity monitoring of steam generator tubing using transient acoustic signal analysis显示文摘 | LU Baofu UPADHYAYA B R PEREZ R B | 2005 | IEEE Transactions on Nuclear Science2005，52，： | 1 |
| 17 | Investigation of a new catalytic combustion-type CH4 gas sensor with low power consumption显示文摘 | Sun LiangYan Quan Baofu Qiu Fabin | 2000 | Sensors and Actuators B2000，，： | 1 |
| 18 | Osteopontin protects against cardiac ischemia-reperfusion injury through late preconditioning显示文摘 | Yongyi Wang Baofu Chen Dafu Shen Song Xue | 2009 | Heart and Vessels2009，，2： | 1 |
| 19 | Detail feature recognition and decomposition in solid model显示文摘 | Baofu Li Jin Liu | 2002 | Computer-Aided Design2002，，5： | 1 |
| 20 | Structural,Kinematic and Geochronological Study of the Main Tianshan Shear Zone in the Borohoro Ranges,NW China显示文摘The western segment of the Main Tianshan shear zone(MTSZ)branches into three major dextral strike-slip shear zones in the Borohoro Ranges,northwestern China.Mylonitic rocks within these zones exhibit vertical foliations,subhorizontal lineations,and dextral kinematics.The microstructures and CPO patterns of calcite and quartz in the tectonites suggest shearing at temperatures of 200℃ to 500℃ or above.The amount of dextral displacement along the zones is less than 100 km.LA-ICP-MS U-Pb dating of zircons from some pre-kinematic granites gave ages of 364-325 Ma and 316 Ma,and zircons from a syn-kinematic leucogranite gave an age of 291 Ma.We propose that dextral shearing along the MTSZ started in the earliest Permian.Our data indicate that collision between the Yili and Junggar plates might have finished before 325 Ma or 316 Ma,with a tectonic transformation from 325 Ma to 300 Ma,resulting in intracontinental transpression from 300 Ma or 291 Ma.We suggest that the formation of the Kazakhstan orocline(KO)took place in two stages,with the early stage of bending driven by convergence related to oblique subduction,and the late stage possibly associated with lateral disarticulation as a result of the dextral strike-slip shear zones. | LIU Tianlun CHEN Siyu ZHANG Bo CAI Keda HAN Baofu QU Junfeng GUO Lei WANG Meng | 2021 | Acta Geologica Sinica(English Edition)2021，95，5： | 1 |
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