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| 1 | The oasis expansion and eco-environment change over the last 50 years in Manas River Valley, Xinjiang显示文摘The oasis expansion and economic development of the Manas River Valley is one of the most successful examples in Xinjiang. In this paper, the oasis spatial distribution pattern and dynamic change were examined using imageries of Landsat MSS, TM and ETM, land use and topographic maps in six different periods (such as 1949, 1962, 1976, 1989, 1999 and 2001) over the last 50 years in the valley. The oasis expansion process could be divided into two stages according to the annual rate of oasis area increase, the fast oasization stage (from 1949 to 1976) when the oasis area ex-panded from 156.385 km2 in 1949 to 3,639.491 km2 in 1976 because of rapidly increased population and quickly enlarged farmland area; and the urbanization stage (from 1976 to 2001) when the ex-pansion ratio of farmland slowed down, and the urbanization process quickened, the total oasis area reached 5042.440 km2 in 2001. With the continuous expansion of oasis and farmland, a large quantity of river water was drawn into irrigation ditch and plain lakes, so only a small quantity of river water could flow into lakes, as a result, the Manas Lake dried up, salization and basification problems happened in the low-lying oasis region. The natural swamp around the lake was shrunk greatly and biodiversity decreased significantly. The driving force analysis reveals that human activities, such as reclamation and population growth, played a major role in the oasis expansion and ecological dete-rioration in the Manas River Valley. So further efforts should be made to improve the efficiency of water resource utility and adjust layout of the regional agricultural and animal husbandry to keep the sustainable development of oasis economic belt of the northern slope of Tianshan Mts. | CHENG Weiming ZHOU Chenghu LIU Haijiang ZHANG Yang JIANG Yan ZHANG Yichi YAO Yonghui | 2006 | Science China Earth Sciences2006，49，2： | 24 |
| 2 | Mass elevation effect and its forcing on timberline altitude显示文摘集体举起效果的概念(massenerhebungseffect, MEE ) 被 A 介绍。de Quervain 大约 100 年以前排队为象树那样的温度相关的参数说明观察趋势并且比在他们的外部边缘上在中央阿尔卑斯山脉发生在更高的举起的 snowline。它广泛地也在世界的另外的区域被观察了,但是没有重要,更不用说量,关于这现象的研究。特别,它完全通常在开发树带界线举起的恰当的模型被忽视了,与仅仅看作影响因素的经度或纬度。这篇论文试着确定到树带界线的 MEE 的贡献举起。认为更多广泛陆地团并且特别越高在陆地质量的内部的山底,越 greater 集体举起效果,这篇论文作为 MEE 的大小拿山底举起(MBE ) 。我们收集树带界线举起的 157 个数据点,并且把他们的纬度,经度和 MBE 用作独立变量在东南的欧亚的大陆为树带界线举起造一个多重线性回归方程。结果生产到树带界线高度活动范围 25.11% , 29.43% ,和 45.46% 的纬度,经度和 MBE 的贡献分别地。北纬度的诺思 | HAN Fang YAO Yonghui DAI Shibao WANG Chun SUN Ranhao XU Juan ZHANG Baiping | 2012 | Journal of Geographical Sciences2012，22，4： | 12 |
| 3 | Diversity and Geographical Pattern of Altitudinal Belts in the Hengduan Mountains in China显示文摘This paper analyses the diversity and spatial pattern of the altitudinal belts in the Hengduan Mountains in China.A total of 7 types of base belts and 26 types of altitudinal belts are identified in the study region.The main altitudinal belt lines,such as forest line,the upper limit of dark coniferous forest and snow line,have similar latitudinal and longitudinal spatial patterns,namely,arched quadratic curve model with latitudes and concave quadratic curve model along longitudinal direction.These patterns can be together called as 'Hyperbolic-paraboloid model',revealing the complexity and speciality of the environment and ecology in the study region.This result further validates the hypnosis of a common quadratic model for spatial pattern of mountain altitudinal belts proposed by the authors.The spatial pattern of altitudinal belts is closely related with moisture-related exposure effect in the Hengduan Mountains.Different combinations (spectra) of altitudinal belts and different base belt types appear in windward and leeward flanks and even in the same flanks of different ranges.This is closely related with the parallel mountain ranges of the Hengduan Mountains,which,at nearly right angle with the moving direction of prevailing moisture-laden air masses from west and east,hold up the warm and humid monsoon wind from moving into the core region and result in different moisture conditions in windward and leeward flanks.However,how to quantitatively describe the moisture-related exposure effect needs further study.In addition,the data quality and data accuracy at present also affect to some extent the result of quantitative modeling and should be improved with RS/GIS in the future. | YAO Yonghui ZHANG Baiping HAN Fang, PANG Yu | 2010 | Journal of Mountain Science2010，7，2： | 11 |
| 4 | A study of the contribution of mass elevation effect to the altitudinal distribution of timberline in the Northern Hemisphere显示文摘作为生态的转变地区,高山的树带界线长在许多地里吸引了科学家的注意,特别在最近的年里。许多单一、二盐基的恰当的模型被开发了探索在树带界线举起和纬度或温度之间的关系。然而,这些模型通常在地区性的规模上并且不能被用于另外的区域;在另一方面,半球规模并且大陆人规模模型通常基于大约 100 树带界线数据并且在精确是必然低的。现在的文章收集树带界线的 516 个数据地点,并且作为依赖变量作为独立变量和树带界线举起拿纬度,陆性率和集体举起效果(MEE ) 开发一个第三的线性回归模型。陆性率用 WorldClim 和山库举起释放的气象学的数据被计算(作为集体举起效果的一个代理) 根据 SRTM 90 米的分辨率举起数据被提取。结果证明线性模型的决心(R2 ) 的系数象 0.904 一样高,并且到树带界线举起的纬度,陆性率和 MEE 的贡献率是 45.02%(p=0.000 ) , 6.04%(p=0.000 ) 并且 48.94%(p=0.000 ) 分别地。这意味着 MEE 简单地是在大陆人和半球的规模上贡献树带界线的举起分发的主要因素。到树带界线高度的 MEE 的贡献率在不同区域不同,例如, 50.49%(p=0.000 ) 在北美洲, 48.73%(p=0.000 ) 在东方欧亚大陆,并且 43.6%(p=0.000 ) 在里面西方的欧亚大陆,而是它通常很高。 | ZHAO Fang ZHANG Baiping PANG Yu YAO Yonghui | 2014 | Journal of Geographical Sciences2014，24，2： | 10 |
| 5 | Folate receptor-mediated boron-10 containing carbon nanoparticles as potential delivery vehicles for boron neutron capture therapy of nonfunctional pituitary adenomas显示文摘Invasive nonfunctional pituitary adenomas(NFPAs) are difficult to completely resect and often develop tumor recurrence after initial surgery.Currently,no medications are clinically effective in the control of NFPA.Although radiation therapy and radiosurgery are useful to prevent tumor regrowth,they are frequently withheld because of severe complications.Boron neutron capture therapy(BNCT) is a binary radiotherapy that selectively and maximally damages tumor cells without harming the surrounding normal tissue.Folate receptor(FR)-targeted boron-10 containing carbon nanoparticles is a novel boron delivery agent that can be selectively taken up by FR-expressing cells via FR-mediated endocytosis.In this study,FR-targeted boron-10 containing carbon nanoparticles were selectively taken up by NFPAs cells expressing FR but not other types of non-FR expressing pituitary adenomas.After incubation with boron-10 containing carbon nanoparticles and following irradiation with thermal neutrons,the cell viability of NFPAs was significantly decreased,while apoptotic cells were simultaneously increased.However,cells administered the same dose of FR-targeted boron-10 containing carbon nanoparticles without neutron irradiation or received the same neutron irradiation alone did not show significant decrease in cell viability or increase in apoptotic cells.The expression of Bcl-2 was down-regulated and the expression of Bax was up-regulated in NFPAs after treatment with FR-mediated BNCT.In conclusion,FR-targeted boron-10 containing carbon nanoparticles may be an ideal delivery system of boron to NFPAs cells for BNCT.Furthermore,our study also provides a novel insight into therapeutic strategies for invasive NFPA refractory to conventional therapy,while exploring these new applications of BNCT for tumors,especially benign tumors. | DAI CongXin CAI Feng HWANG Kuo Chu ZHOU YongMao ZHANG ZiZhu LIU XiaoHai MA SiHai YANG YaKun YAO Yong FENG Ming BAO XinJie LI GuiLin WEI JunJi JIAO YongHui WEI ZhenQing MA WenBin WANG RenZhi | 2013 | Science China(Life Sciences)2013，56，2： | 8 |
| 6 | V4C3Tx MXene:A promising active substrate for reactive surface modification and the enhanced electrocatalytic oxygen evolution activity显示文摘Presented are the synthesis,characterizations,and reactive surface modification(RSM)of a novel nine atomic layered V4C3Tx MXene.With the advantages of the multilayered V4C3Tx MXene that can simultaneously support the RSM reaction and keep the inner skeleton stable,a series of amorphous Ni/Fe/Vternary oxide hydroxides thin layer can be successfully modified on the surface of the V4C3Tx MXene(denoted as MOOH@V4C3Tx,M=Ni,Fe,and V)without disrupting its original structure.Attributed to the in situ reconstruction of highly active oxide hydroxide layer,the nanohybrids exhibited an enhanced oxygen evolution reaction(OER)activity and excellent long-time stability over 70 hours.In particular,a current density of 10 mA cm−2 can be reached by the nanohybrid with the optimized Ni/Fe ratio at an overpotential(η)as low as 275.2 mV,which is comparable to most of the state-of-the-art OER catalysts and better than other MXene-based derivatives.Demonstrated by the tunable physicochemical properties and excellent structural stability of these nanohybrids,we may envision the promising role of the M4X3-based MXenes as substrates for a wide range of energy conversion and storage materials. | Cheng-Feng Du Xiaoli Sun Hong Yu Wei Fang Yao Jing Yonghui Wang Shuiqing Li Xianhu Liu Qingyu Yan | 2020 | InfoMat2020，2，5： | 8 |
| 7 | Seasonal variation of snow microbial community structure in the East Rongbuk glacier, Mt. Everest显示文摘The bacterial diversity and abundance in the snow of East Rongbuk glacier, Mt. Everest were examined through 16S rRNA gene clone library and flow cytometry approaches. In total, 35 16S rRNA gene sequences were obtained, which belong to α, β, γ-Proteobacteria, Actinobacteria, Firmicutes, CFB, Cyanobacteria, Eukaryotic chloroplast, and TM7 candidate phylum respectively. γ-Proteobacteria was the dominant bacterial group in this region, while the genera Acinetobacter and Leclercia were domi- nant on the genus level. The community structure varied seasonally. The bacterial abundance in sum- mer snow was higher than that in winter. Moreover, the snow bacterial community structures in both seasons were diverse, with not only common species but season-specific species. The common species most likely originated from the Tibet Plateau. Bacteria in summer snow are affiliated with marine environ- ment, whereas bacteria in winter snow are closely related to more diverse environments and show the feature of resistance to cold. Seasonal variations of abundance and bacterial diversity were most proba- bly due to the seasonal characteristics of climate and atmospheric circulation in Mt. Everest. | LIU Yongqin YAO Tandong KANG Shichang JIAO Nianzhi ZENG Yonghui SHI Yang LUO Tingwei JING Zhefang HUANG Shijun | 2006 | Chinese Science Bulletin2006，51，12： | 7 |
| 8 | Allergic diseases, immunoglobulin E, and autoimmune pancreatitis: a retrospective study of 22 patients显示文摘 | Guo Limei Huang Yonghui Wang Tianli Shi Xueying Chang Hong Yao Wei Huang Xuebiao | 2014 | Chinese Medical Journal2014，，23： | 5 |
| 9 | Research on cohesive sediment erosion by flow: An overview显示文摘Erosion of cohesive sediment by flow is a very complicated phenomenon occurring worldwide. Understanding and modeling of the erosion process are important for many issues such as the breaching of embankments, riverbank stability, siltation of harbors and navigation channels, service life of reservoirs, distribution of (heavy metal) pollutants and water quality problems. In the last few decades, numerous studies have been done on the erosion of cohesive sediment by flow. Nevertheless, the factors affecting the erosion resistance of cohesive sediment are still not fully understood and the knowledge of the physics of cohesive sediment erosion is in- adequate, as a result the mathematical modeling of this erosion is far from satis- factory. In this paper an overview of the studies on the erosion resistance, erosion threshold and the erosion rate of cohesive sediment by flow is presented. The outcomes achieved so far from the studies and the existing problems have been analyzed and summarized, based on which recommendations are proposed for future research. | YongHui Zhu JinYou Lu HongZhi Liao JiaSheng Wang BeiLin Fan ShiMing Yao | 2008 | Science China(Technological Sciences)2008，51，11： | 5 |
| 10 | Microbial community structure in major habitats above 6000 m on Mount Everest显示文摘Bacterial abundance in surface snow between 6600 and 8000 m a.s.l. on the northern slope of Mt. Ev- erest was investigated by flow cytometry. Bacterial diversity in serac ice at 6000 m a.s.l., glacier melt- water at 6350 m, and surface snow at 6600 m a.s.l. was examined by constructing a 16S rRNA gene clone library. Bacterial abundance in snow was higher than that in the Antarctic but similar to other mountain regions in the world. Bacterial abundance in surface snow increased with altitude but showed no correlation with chemical parameters. Bacteria in the cryosphere on Mt. Everest were closely related to those isolated from soil, aquatic environments, plants, animals, humans and other frozen environ- ments. Bacterial community structures in major habitats above 6000 m were variable. The Cyto- phaga-Flavobacterium-Bacteroides (CFB) group absolutely dominated in glacial meltwater, while β-Proteobacteria and the CFB group dominated in serac ice, and β-Proteobacteria and Actinobacteria dominated in surface snow. The remarkable differences among the habitats were most likely due to the bacterial post-deposition changes during acclimation processes. | LIU YongQin YAO TanDong KANG ShiChang JIAO NianZhi ZENG YongHui HUANG SiJun LUO TingWei | 2007 | Chinese Science Bulletin2007，52，17： | 5 |
| 11 | Progress on Integrated Control of Tobacco Black Shank显示文摘Tobacco black shank is one of the devastating diseases of tobacco. In recent years,this disease widely occurred in most tobacco-growing areas,which caused disastrous losses and has severely threatened the sustainable development of flue-cured tobacco. In order to lay a theoretical foundation for the better control of tobacco black shank,the occurrence characteristics and integrated control strategis of this disease were systematically discussed according to the aspects of agricultural control,chemical control,biological control,etc. | Yonghui XIE Yonggui ZHANG Liquan ZHU Daogui YOU Yao LU | 2015 | Agricultural Biotechnology2015，4，4： | 3 |
| 12 | The implication of mass elevation effect of the Tibetan Plateau for altitudinal belts显示文摘加热效果(或集体举起效果, MEE ) 由于它的巨大的身体西藏的高原(TP ) 是强烈的。一些研究为亚洲气候在夏天和它的含意作为热来源在它的角色上被承担了,但是很少被了解了它为山的分发的 MEE 的含意高度的带(MAB ) 。用遵守并且遥远地察觉到数据的空气温度数据, MAB/treeline 数据,和翠菊 GDEM 数据,这份报纸总体上比较 MAB 和高山的 treelines 的高度 TP 和包围山脉 / 低地并且从 MEE 的观点解释差别。结果示威:1 ) 在一样,举起,空气温度和逐渐地种季节的长度从东方边增加到内部 TP,例如,在 4500 m (相应于 TP 的吝啬的高度) ,每月吝啬的温度是 3.58 敨映敬? | YAO Yonghui XU Mei ZHANG Baiping | 2015 | Journal of Geographical Sciences2015，25，12： | 3 |
| 13 | Adsorption equilibrium for Z-ligustilide on C18-bonded silica from supercritical carbon dioxide显示文摘Adsorption equilibrium is of great importance for the preparative supercritical fluid chromatography(pre-SFC) in defining supercritical adsorption behavior and the industrial amplification.This paper presents adsorption isotherms of Z-ligustilide from supercritical carbon dioxide(SC-CO_2) on C18-bonded silica.Adsorption behavior was studied at 305.15 K,313.15 K and 323.15 K with SC-CO_2 density varying from 0.687 g·cm^(-3) to0.863 g·cm^(-3) with the elution by characteristic points(ECP) method.The adsorption amount of Z-ligustilide from SC-CO_2 on C18-bonded silica decreased with the increasing density of the mobile phase as well as the increasing temperature.Adsorption equilibrium data were fitted by Langmuir and Freundlich isotherm models,and the Langmuir isotherm model performed better for describing the whole adsorption process on the column.The monolayer saturation adsorption capacity of Z-ligustilide is in the range of 3.0 × 10^(-4) mg·cm^(-3) to5.5 × 10^(-4) mg·cm^(-3) with an average value of 4.0 × 10^(-4) mg·cm^(-3). | Huisheng Lü Shuangyan Liu Yonghui Li Fanmei Meng Dawei Yao Xufei Mo | 2016 | Chinese Journal of Chemical Engineering2016，24，12： | 1 |
| 14 | Mass elevation effect and its contribution to the altitude of snowline in the Tibetan Plateau and surrounding areas显示文摘 | Han Fang Zhang Baiping Yao Yonghui | 2011 | Arctic Antarctic and Alpine Research2011，43，2： | 1 |
| 15 | Ecological anomalies inthe East China Sea:Impacts of the Three Gorges Dam?显示文摘 | NIanzhi Jiao Yao Zhang Yonghui Zeng | 2007 | Water Re-search2007，41，6： | 1 |
| 16 | Ecological anomalies in the East China sea: impacts of the Three Gorges Dam显示文摘 | Jiao Nianzhi Zhang Yao Zeng Yonghui | 2007 | Water Research2007，41，6： | 1 |
| 17 | Magnitude and Forming Factors of Mass Elevation Effect on Qinghai-Tibet Plateau显示文摘Mass elevation effect(MEE) refers to the thermal effect of huge mountains or plateaus, which causes the tendency for temperature-related montane landscape limits to occur at higher elevations in the inner massifs than on their outer margins. MEE has been widely identified in all large mountains, but how it could be measured and what its main forming-factors are still remain open. This paper, supposing that the local mountain base elevation(MBE) is the main factor of MEE, takes the Qinghai-Tibet Plateau(QTP) as the study area, defines MEE as the temperature difference(ΔT) between the inner and outer parts of mountain massifs, identifies the main forming factors, and analyzes their contributions to MEE. A total of 73 mountain bases were identified, ranging from 708 m to 5081 m and increasing from the edges to the central parts of the plateau. Climate data(1981–2010) from 134 meteorological stations were used to acquire ΔT by comparing near-surface air temperature on the main plateau with the free-air temperature at the same altitude and similar latitude outside of the plateau. The ΔT for the warmest month is averagely 6.15℃, over 12℃ at Lhatse and Baxoi. A multivariate linear regression model was developed to simulate MEE based on three variables(latitude, annual mean precipitation and MBE), which are all significantly correlated to ΔT. The model could explain 67.3% of MEE variation, and the contribution rates of three independent variables to MEE are 35.29%, 22.69% and 42.02%, respectively. This confirms that MBE is the main factor of MEE. The intensive MEE of the QTP pushes the 10℃ isotherm of the warmest month mean temperature 1300–2000 m higher in the main plateau than in the outer regions, leading the occurrence of the highest timberline(4900 m) and the highest snowline(6200 m) of the Northern Hemisphere in the southeast and southwest of the plateau, respectively. | ZHANG Shuo ZHANG Baiping YAO Yonghui ZHAO Fang QI Wenwen HE Wenhui WANG Jing | 2016 | Chinese Geographical Science2016，26，6： | 1 |
| 18 | Spatial patterns of Pinus tabulaeformis and Pinus massoniana forests in Qinling-Daba Mountains and the boundary of subtropical and warm temperate zones显示文摘The Qinling Mountains is not only the geographical boundary between North and South China,but also the boundary between subtropical and warm temperate zones.It plays an important role in the geo-ecological pattern of China.However,there is controversy about the specific location of this geographical boundary in academic community due to the complexity,transition and heterogeneity of the transitional zone,as well as the differences in the delimitation indicators and research purposes.To further reveal the characteristics of the North-South transitional zone and clarify the specific location of the geo-ecological boundary between North and South China,combined with SRTM topographic data,temperature and precipitation data,Pinus massoniana forest and Pinus tabulaeformis forest,which represent subtropical coniferous forest in South China and temperate coniferous forest in North China respectively,were chosen to analyze their spatial distributions in the Qinling-Daba Mountains and the climatic conditions at their boundary with the climatic indexes of annual precipitation,the coldest month(January) average temperature,the warmest month(July) average temperature and the annual average temperature.The results show that:(1) Pinus massoniana and Pinus tabulaeformis forests and the climate indicators of their boundary can be used as one of the vegetation-climate indexes for the delimitation of subtropical and warm temperate zones.The boundary between the subtropical coniferous forest(Pinus massoniana forest) and temperate coniferous forest(Pinus tabulaeformis forest) is located along the south slope of Funiu Mountain to the north edge of Hanzhong Basin(the south slope of Qinling Mountains) at an altitude of 1000–1200 m,where the climatic indictors are stable:the annual precipitation is about 750–1000 mm,the annual average temperature is about 12–14℃,the coldest monthly average temperature is 0–4℃,and the warmest monthly average temperature is about 22–26℃.(2) It can be more scientifically to delimitate the boundary of subtropical and warm temperate zones in China by comprehensively considering the vegetation-climate indicators.Additionally,the boundary between subtropical and warm temperate zones in Qinling-Daba Mountains should be a transitional zone consisting of the boundaries of coniferous forests,broad-leaved forests and shrubs between subtropical and warm temperate zones.The results provide a scientific basis for the selection of delimitation index of subtropical and warm temperate zones. | YAO Yonghui HU Yufan KOU Zhixiang ZHANG Baiping | 2020 | Journal of Geographical Sciences2020，30，9： | 1 |
| 19 | Tectonic geomorphological characteristics for evolution of the Manas Lake显示文摘Owing to global climatic changes and human activities,the lakes have changed dramatically in the Junggar Basin of Xinjiang in recent 50 years. Based on the remote sensing images from Beijing Satellite No.1 in 2006 together with the measured topographical data in 1999 and other data since the 1950s,this paper analyzes mainly the features of landforms around the Manas Lake and the changes of feeding sources of the lake. The results are as follows:(1) Tectonic movement brought about the fundamental geomorphological basis for lacustrine evolution,and the Manas Lake is one of small lakes broken up from the Old Manas Lake due to tectonic movement and drought climate; the Manas Lake had existed before the Manas River flowed into it in 1915. The geomorphologic evidences for evolution of the Manas Lake include:(a) Diluvial fans and old channels at the north of the lake indicate that the rivers originating from the north mountains of the Junggar Basin had fed the Old Manas Lake and now still feed the lake as seasonal rivers; (b) The Old Manas Lake was fed by many rivers originating from the mountains,except for the Manas River,from the evidence of small lakes around the Manas Lake,old channels,alluvial fans,etc.; (c) The elevations of the alluvial and diluvial fans are near to the 280 m a.s.l. and all of the small lakes and lacustrine plains are within the range of the 280 m a.s.l.,which may prove that the elevation of the Old Manas Lake was about 280 m a.s.l.; (d) Core analysis of the Manas Lake area also indicates that the Manas Lake has existed since Late Pleistocene epoch. (2) Analysis on the feeding relations between the lakes and the lacustrine evolution shows that human activities are one of main driving forces of the lacustrine evolution in recent 50 years,and it is the precondition of restoring and maintaining the lacutrine wetlands in the study area to satisfy the feeding of the Baiyang and Manas rivers to the Manas Lake. | Yao, YongHui Li, HuiGuo | 2010 | Journal of Arid Land2010，2，3： | 1 |
| 20 | Hybeanones A and B,Two Highly Modified Polycyclic Polyprenylated Acylphloroglucinols from Hypericum beanii显示文摘Hybeanones A and B(1 and 2),two highly oxygenated and rearranged polycyclic polyprenylated acylphloroglucinols(PPAPs),were isolated from the aerial parts of Hypericum beanii.Their structures comprising absolute configurations were elucidated by spectroscopic analysis,single-crystal X-ray diffraction,and quantum chemical calculations.Compounds 1 and 2 are defined by a newly assembled cyclopentanone unit fused to a tricyclic γ-lactone unit via a ketone carbonyl.The breakage of C-1/C-2 linkage via retro-Claisen reaction,attack from C-1 to C-19,and Baeyer-Villiger oxidation at C-1/C-23 bond were presumed to be the key steps in the assembly of 1 and 2.The isolates 1 and 2 showed potential acetylcholinesterase(AchE)inhibitory activities,with IC50 values of 21.34±1.48 and 18.79±2.36μmol/L,respectively. | Beiye Yang Changxing Qi Zeyu Yao Shuang Lin Fengli Li Weiguang Sun Zhengxi Hu Yonghui Zhang | 2022 | Chinese Journal of Chemistry2022，40，1： | 0 |
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