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| 1 | Progress in the biological function of alpha-enolase显示文摘Alpha-enolase(ENO1), also known as 2-phospho-D-glycerate hydrolase, is a metalloenzyme that catalyzes the conversion of 2-phosphoglyceric acid to phosphoenolpyruvic acid in the glycolytic pathway. It is a multifunctional glycolytic enzyme involved in cellular stress, bacterial and fungal infections, autoantigen activities, the occurrence and metastasis of cancer, parasitic infections, and the growth, development and reproduction of organisms. This article mainly reviews the basic characteristics and biological functions of ENO1. | Hong Ji Jianfa Wang Jingru Guo Yue Li Shuai Lian Wenjin Guo Huanmin Yang Fanzhi Kong Li Zhen Li Guo Yanzhi Liu | 2016 | Animal Nutrition2016，，1： | 9 |
| 2 | Early warning for geo-hazards based on the weather condition in China显示文摘According to national early warning practice for geo-hazards from 2003 to 2005,it is systematically concluded that the basic characteristics of geo-hazards,early warning method and forecast result based on the geological maps of China in a scale 1∶6 000 000.With the contrast of different characters between sustained rainfall and typhoon rainfall inducing geo-hazards,the disaster reduction result and some problems are preliminarily analyzed.Some basic recognition is that early warning to geo-hazards is feasible,national scale forecast is only to call attention,but can't immediately be used to disaster reduction decision-making.And,the future direction is to build a united disaster reduction framework of early warning system including national,provincial and county levels based on weather factors in different scale of area. | Chuanzheng LIU Yanhui LIU Mingsheng WEN Can TANG Tiefeng LI Jianfa LIAN | 2006 | Global Geology2006，9，2： | 9 |
| 3 | Depositional architecture of the late Ordovician drowned carbonate platform margin and its responses to sea-level fluctuation in the northern slope of the Tazhong region, Tarim Basin显示文摘The Tazhong Uplift of the late Ordovician is a drowned rimmed carbonate platform. The carbonate rock of the late Ordovician Lianglitage Formation in the northern slope of the Tazhong region is one of the significant petroliferous intervals. Based on petrofacies, depositional cycles, natural gammaray spectrometry and carbon/oxygen isotope data from the Lianglitage Formation, one 2nd-order, three 3rd-order and several 4th-order sequences have been recognized, and the late Ordovician relative sealevel fluctuation curve has been established. The sequences O 3 l-1 and O 3 l-2 on the platform are composed of highstand and transgressive systems tracts, but lack the lowstand systems tract. The sequence O 3 l-3 is a drowning sequence. The sequence O 3 l-1 overlapped the eroded slope and pinched out to the northwest and landward. The highstand systems tract in the sequence O 3 l-2 consists of low-angle sigmoid and high-angle shingled progradation configuration. Major sedimentary facies of the Lianglitage Formation include reef and shoal in the platform margin and lagoon, which can be subdivided into coral-sponge-stromatoporoid reef complex, sand shoal, lime mud mound, and intershoal sea. Reefs, sand shoals and their complex are potential reservoir facies. The reefs and sand shoals in the sequence O 3 l-1 developed in the upper of its highstand systems tract. In the sequence O 3 l-2, the highstand systems tract with an internal prograding configuration is a response to the lateral shifting of the complex of reef and sand shoal. The transgressive systems tract, in particular the sand shoals, developed widely on the slope of the platform margin and interior. The reefs in the sequence O 3 l-3 migrated towards high positions and formed retrograding reefs in the western platform and low relief in the platform interior. Basinward lateral migration of the reefs and pure carbonate rock both characterize highstand systems tract and show that the rise of the relative sea-level was very slow. Shingled prograding stacking pattern of the 4th-order sequences and reefs grow horizontally, which represents the late stage of highstand systems tract and implies relative sealevel stillstand. Reefs migrating towards high land and impure carbonate rock both indicate transgressive systems tract and suggest that the relative sea-level rose fast. Erosional truncation and epidiagenetic karstification represent a falling relative sea-level. The relative sea-level fluctuation and antecedent palaeotopography control the development and distribution of reef complexes and unconformity karst zones. Currently, the composite zone of epidiagenetic karstic intervals and high-energy complexes of reefs and sand shoals with prograding configuration is an important oil and gas reservoir in the northern slope of the Tazhong carbonate platform. | Yang Xiaofa Lin Changsong Yang Haijun Han Jianfa Liu Jingyan Zhang Yanmei Peng Li Jing Bing Tong Jianyu Wang Haiping Li Huanpu | 2010 | Petroleum Science2010，7，3： | 8 |
| 4 | Differences of Hydrocarbon Enrichment between the Upper and the Lower Structural Layers in the Tazhong Paleouplift显示文摘Tazhong paleouplift 被划分成上面并且更低的结构的层,在奥陶纪碳酸盐岩石的顶由不顺从表面跳了。在从不同部分的二层的水库在数字变化,类型和储备,而是机制以前很少被研究。因此,机制的解释将在 Tazhong paleouplift 支持石油探索。在学习进化和 Tazhong paleouplift 的水库分发以后,在晚古苏格兰的、迟了的 Hercynian 和喜玛拉雅的时期的进化导致了,这被结束上面并且更低的结构的层。这也被定义在上面的结构的层,结构并且, stratigraphic 重叠水库为更低的结构的层在顶和 paleouplift 的上面的部分被开发,它被油水库统治, lithological 水库在 paleouplift 的更低的部分被开发,它被煤气的水库,和更多统治储备在更低的结构的层被发现比上面。通过累积条件的比较分析上面并且更低的结构的层,丰富差别的机制清楚地被解释。更低的结构的层的水库和封口条件比上面的层的那些好,它是更多的水库在前者被发现了的原因。在搬运人系统类型,陷井类型和收费时期在之间的差别上面并且更低的结构的层在水库类型和分布导致差别。一个累积模型为 Tazhong paleouplift 被建立。为上面的结构的层,,结构的水库和 stratigraphic 重叠水库为更低的结构的层在 paleouplift 的上面的部分被形成,捱过的外壳水库在顶被形成,礁石公寓水库在侧面的边缘上被形成,石灰岩地区常见的地形和里面水库在 paleouplift 的更低的部分被形成。 | JIANG Zhenxue YANG Haijun LI Zhuo PANG Xiongqi HAN Jianfa LI Dongxu HUANG Yuyan | 2010 | Acta Geologica Sinica(English Edition)2010，84，5： | 7 |
| 5 | Relationship between the parent charge transfer gap and maximum transition temperature in cuprates显示文摘One of the biggest puzzles concerning the cuprate high temperature superconductors is what determines the maximum transition temperature(Tc,max), which varies from less than 30 to above 130 K in different compounds.Despite this dramatic variation, a robust trend is that within each family, the double-layer compound always has higher Tc,maxthan the single-layer counterpart. Here we use scanning tunneling microscopy to investigate the electronic structure of four cuprate parent compounds belonging to two different families. We find that within each family, the double layer compound has a much smaller charge transfer gap size(DCT), indicating a clear anticorrelation between DCTand Tc,max. These results suggest that the charge transfer gap plays a key role in the superconducting physics of cuprates, which shed important new light on the high Tc mechanism from doped Mott insulator perspective. | Wei Ruan Cheng Hu Jianfa Zhao Peng Cai Yingying Peng Cun Ye Runze Yu Xintong Li Zhenqi Hao Changqing Jin Xingjiang Zhou Zheng-Yu Weng Yayu Wang | 2016 | Science Bulletin2016，61，23： | 3 |
| 6 | Application of butane geochemistry of natural gas in hydrocarbon exploration显示文摘In order to distinguish the source and migration direction of natural gas by geochemical characteristics of butane,the components and carbon isotopes of natural gas from major hydrocarbonbearing basins in China were analyzed.The results showed that:(1) Oil-type gas has i-C 4 /n-C 4 <0.8,δ 13 C butane <-28‰,δ 13 C i-butane <-27‰,δ 13 C n-butane <-28.5‰,whereas coal-type gas has i-C 4 /n-C 4 >0.8,δ 13 C butane >-25.5‰,δ 13 C i-butane >-24‰,δ 13 C n-butane >-26‰.(2) When δ 13 C i-butane-δ 13 C n-butane is greater than 0,the maturity of oil-type gas is generally more than 2.4% and that of coal-type gas is greater than 1.4%,whereas when the difference is less than 0,the maturity of oil-type gas is generally less than 1.1% and that of coal-type gas is less than 0.8%.(3) When natural gas migrates through dense cap rocks,the value of i-C 4 /n-C 4 increases,whereas when it migrates laterally along a reservoir,the value of i-C 4 /n-C 4 decreases.(4) Sapropelic transition zone gas with composition and carbon isotopic signatures similar to those of oil-type gas in the low thermal evolution stage is found to have a relatively high butane content.(5) The values of i-C 4 /n-C 4 and δ 13 C n-butane δ 13 C i-butane of gas which has suffered biological degradation are significantly higher than those obtained from thermogenic and bio-thermocatalytic transition zone gas.Thus,natural gas of different genetic types can be recognized through component analysis and carbon isotopic signatures of butane,the natural gas maturity can be estimated from the difference in carbon isotopic content between isobutane and n-butane,and the migration direction of natural gas can be determined from i-C 4 /n-C 4 ratios and transport conditions,which can also be used to thermogenic and bio-thermocatalytic transition zone gas. | Miao Zhongying Chen Jianfa Wang Jing Wang Guannan ZhangChen Li Wei | 2012 | Petroleum Science2012，9，4： | 3 |
| 7 | Identification and functional annotation of lncRNA genes with hypermethylation in colorectal cancer显示文摘 | Qi Liao Weiling He Jianfa Liu Yi Cen Liang Luo Chengliang Yu Yang Li Sitong Chen Shiwei Duan | 2015 | Gene2015，，： | 1 |
| 8 | Enhanced removal of nitrate by a novel composite; NanoscaIe zero valent iron supported on pillared clay显示文摘 | Yun Zhang Yimin Li Jianfa Li | 2011 | Chemical Engineering Journal2011，171，2： | 1 |
| 9 | 显示文摘 | LI Jianfa SONG Zhanqian GAO Hong | 2006 | Chem Ind Forest Prod2006，26，2： | 1 |
| 10 | Enhanced reduction of chloro- phenols by nauoscale zerovalent ironsupported on organobentonite 显示文摘 | Li Yimin Zhang Yun Li Jianfa | 2013 | Chemosphere2013，92，4： | 1 |
| 11 | Enhanced Cr(Ⅵ)removal by using the mixture of pillared bentonite and zero-valent iron显示文摘 | Zhang Yuling Li Yimin Li Jianfa | | 0，，： | 1 |
| 12 | Biodegradation of 2,4,6-trinitrophenol (picric acid) in a biological aerated filter (BAF)显示文摘 | Shen Jinyou He Rui Yu Hongxia Wang Lianjun Zhang Jianfa Sun Xiuyun Li Jiansheng Han Weiqing Xu Lu | 2009 | Bioresource Technology2009，，100： | 1 |
| 13 | New equation to decipher the relationship between carbon isotopic composition of methane and maturity of gas source rocks显示文摘The identification of the origin and source of natural gas is always a difficult and hot issue.Hereinto,the maturity identification is one of the most important scientific problems.Many empirical equations have been established to decipher the relationship between the maturity of gas source rocks and the carbon isotopic composition of natural gas.However,these equations proposed often fail to identify the maturity of the source rocks correctly,which in turn prevents the identification of genetic types and source rocks of the natural gas because the petroliferous sedimentary basins in China are complex and diverse,with multiple sets of source rocks and different thermal history.In this paper,the oil-associated gas from the Permian lacustrine source rocks and the coal-derived gas from the Jurassic source rocks in Junggar and Turpan-Hami basins have been investigated to decipher the relationship between the maturity(vitrinite reflectance)of gas source rocks and the carbon isotopic composition of methane.The equations established areδ^(13)C_(1)=25lgR_(o)-42.5 for oil-associated gas,andδ^(13)C_(1)=25lgR_(o)-37.5 for coal-derived gas.These new equations are suitable for the maturity identification of source rocks in most petroliferous basins,and favorable for the identification of the genetic type and source of natural gas,which is very important to improve the geological theory of natural gas. | Jianping CHEN Xulong WANG Jianfa CHEN Yunyan NI Baoli XIANG Fengrong LIAO Wenjun HE Limiao YAO Erting LI | 2021 | Science China Earth Sciences2021，64，3： | 1 |
| 14 | Controlled Release of Herbicide Acetochlor from Clay/Carboxylmethylcellulose Gel Formulations 显示文摘 | Li Jianfa Li Yimin Dong Huaping | 2008 | J Agr Food Chem2008，56，： | 1 |
| 15 | Leakage of mantle helium from the Liaodong Peninsula, China显示文摘The isotopic compositions of helium have been investigated in hot spring gases sampled from the Liaodong Peninsula, China. The 3He/ 4He ratios range from 0.14 Ra (0.14 times the atmospheric 3He/ 4He ratio of 1.40×10 -6) to 0.72 Ra. 3He/ 4He versus 4He/ 20Ne ratios and He contents suggest that a small amount of mantle-derived helium reaches the earth’s surface. Helium isotope ratios of the hot spring gases show a distribution pattern similar to the regional heat flow values, indicating that the positive thermal anomaly occurring in the area is closely associated with the presence of mantle-derived helium. The observations described above provide some significant evidence that the molten magma originating from partial melting of the upper mantle may have intruded into the continental crust along the activity fault. The coupling of the presence of mantle He and heat flow anomalies to seismic activity in studied region seem to imply that there is an internal relationship between mantle degassing and seismic | Jianguo Ren Xianbin Wang Jianfa Chen Chunyuan Li Hui Yang Ziyuan Ouyang | 1998 | Chinese Science Bulletin1998，43，9： | 1 |
| 16 | A Real-Time IterativeModel to Predict Urban Air Quality显示文摘 | Li Chaoyi Yang Weimin Shen Jianfa | 1991 | Meteorology andAtmospheric Physics1991，，47： | 1 |
| 17 | P2 asymmetry of Au's M-band flux and its smoothing effect due to high-Z ablator dopants显示文摘X-ray drive asymmetry is one of the main seeds of low-mode implosion asymmetry that blocks further improvement of the nuclear per-formance of“high-foot”experiments on the National Ignition Facility[Miller et al.,Nucl.Fusion 44,S228(2004)].More particularly,the P2 asymmetry of Au's M-band flux can also severely influence the implosion performance of ignition capsules[Li et al.,Phys.Plasmas 23,072705(2016)].Here we study the smoothing effect of mid-and/or high-Z dopants in ablator on Au's M-band flux asymmetries,by modeling and comparing the implosion processes of a Ge-doped ignition capsule and a Si-doped one driven by X-ray sources with P2 M-band flux asymmetry.As the results,(1)mid-or high-Z dopants absorb hard X-rays(M-band flux)and re-emit isotropically,which helps to smooth the asymmetric M-band flux arriving at the ablation front,therefore reducing the P2 asymmetries of the imploding shell and hot spot;(2)the smoothing effect of Ge-dopant is more remarkable than Si-dopant because its opacity in Au's M-band is higher than the latter's;and(3)placing the doped layer at a larger radius in ablator is more efficient.Applying this effect may not be a main measure to reduce the low-mode implosion asymmetry,but might be of significance in some critical situations such as inertial confinement fusion(ICF)experiments very near the performance cliffs of asymmetric X-ray drives. | Yongsheng Li Chuanlei Zhai Guoli Ren Jianfa Gu Wenyi Huo Xujun Meng Wenhua Ye Ke Lan Weiyan Zhang | 2017 | Matter and Radiation at Extremes2017，2，2： | 1 |
| 18 | Enhanced Removal of Nitrate by a Novel Composite:Nanoscale Zero Valent Iron Supported on Pillared Clay显示文摘 | Zhang Yun Li Yimin Li Jianfa | 2011 | Chem Eng J2011，171，2： | 1 |
| 19 | Adsorption of herbicides 2,4-D and acetochlor on inorganic-organic bentonites 显示文摘 | Jianfa Li Yimin Li Jinhong Lu | 2009 | Applied Clay Science2009，46，3： | 1 |
| 20 | Enhanced Cr(Ⅵ) removal by using the mixture of pillared bentonite and zero-valent iron显示文摘 | Zhang Yuling Li Yimin Li Jianfa | 2012 | Chemical Engineering Journal2012，，： | 1 |
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