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| 1 | 喜马拉雅山佩枯岗日冰川地貌的年代学、平衡线高度和气候研究显示文摘喜马拉雅山珠穆朗玛峰-希夏邦马峰地区是青藏高原南部现代冰川集中发育区之一,古冰川遗迹亦十分丰富,是研究第四纪青藏高原冰川形成和演化的关键区,一直备受地貌和第四纪环境研究者的关注.应用原地宇宙核素10Be暴露年龄测试技术,对采自希夏邦马峰西北佩枯岗日拉曲谷地冰碛垄上的冰川漂砾进行年代学研究;结合冰川地貌分析方法,对古冰川平衡线高度(ELA)和气候特征进行探讨.结果表明:末次冰期时,拉曲谷地冰川扩张,发育了山麓冰川,拉曲Ⅰ冰川面积99.9 km2,平衡线海拔5 620 m;拉曲Ⅱ冰川面积97.6 km2,平衡线海拔5 600 m;与现代平衡线高度相比,拉曲Ⅰ和拉曲Ⅱ的平衡线分别下降380 m、400 m.拉曲在末次冰期存在多次冰进,拉曲Ⅰ的10Be暴露年龄在42.1~22.3 ka;拉曲Ⅱ的10Be暴露年龄在18.6~14.8 ka.根据地貌法恢复末次冰期拉曲Ⅰ平衡线高度的温度为-10.7℃,拉曲Ⅱ为-10.6℃,降水量分别为251~461 mm和261~480 mm,显示出当时雪线高度的温度状况和现代冰川雪线高度的温度状况接近,但是降水比现在少得多,冰川气候类型为亚大陆型,印度季风减弱带来的水气变少. | 刘耕年 Li Yingkui 陈艺鑫 张梅 李川川 孔屏 Harbor J. Caffee M.W. | 2011 | 冰川冻土2011，33，5： | 28 |
| 2 | Evaluating the Provenance of Metasedimentary Rocks of the Jiangxian Group from the Zhongtiao Mountain Using Whole-Rock Geochemistry and Detrital Zircon Hf Isotope显示文摘在这研究,整个岩石的 geochemical 和 Nd,同位素的数据,以及从 Jiangxian 的沉积岩石组织的 Palaeoproterozoic 元的由岩屑形成的锆石 Hf 同位素被介绍评估他们的起源和构造历史的特征。专业和踪迹元素作文比得上Archean以后上面的大陆人外壳( PA-UCC ),但是在 LILE 有细微丰富,与例外 C 和 Sr ,和在含铁和镁的元素的细微弄空, HFS 元素例如 Nb 和 Ta ,并且一些主要元素,例如 CaO 和 Na 2 O 。 geochemical 数据表明收集了沉积岩石经历了中间的来源与化学索引捱过的元从 72~78 的改变值,K交代作用的变化的度,和 post-depositional Na 的损失,以及可以忽略的排序,并且从捱过被导出主要, felsic 和 non-mafic 摇。到 Trans 北方中国 Orogen 和作为为元的最可能的来源, Jiangxian 的沉积岩石组织的北方中国 craton 的东方块的由岩屑形成的锆石点上的选择的陆 Hf 同位素的分析。然而,从北方中国 craton 的西方的块的岩屑的贡献能被排除。沉积可能在一个活跃大陆人边缘背景以内在背弧盆被扔。 | LI Qiugen CHEN Xu LIU Shuwen WANG Zongqi ZHOU Yingkui ZHANG Jian WANG Tao | 2009 | Acta Geologica Sinica(English Edition)2009，83，3： | 15 |
| 3 | Lake variations in response to climate change in the Tibetan Plateau in the past 40 years显示文摘The Qinghai-Tibetan Plateau plays an important role in global climate and environmental change and holds the largest lake area in China,with a total surface area of 36,900 km^(2).The expansion and shrinkage of these lakes are critical to the water cycle and ecological and environmental systems across the plateau.In this paper,surface areas of major lakes within the plateau were extracted based on a topographic map from 1970,and Landsat MSS,TM and ETM+satellite images from the 1970s to 2008.Then,a multivariate correlation analysis was conducted to examine the relationship between the changes in lake surface areas and the changes in climatic variables including temperature,precipitation,evaporation,and sunshine duration.Initial results suggest that the variations in lake surface areas within the plateau are closely related to the warming,humidified climate transition in recent years such as the rise of air temperature and the increase in precipitation.In particular,the rising temperature accelerates melting of glaciers and perennial snow cover and triggers permafrost degradation,and leads to the expansion of most lakes across the plateau.In addition,different distributions and types of permafrost may cause different lake variations in the southern Tibetan Plateau. | Jingjuan Liao Guozhuang Shen Yingkui Li | 2013 | International Journal of Digital Earth2013，6，6： | 7 |
| 4 | Much late onset of Quaternary glaciations on the Tibetan Plateau:determining the age of the Shishapangma Glaciation using cosmogenic 26Al and 10Be dating显示文摘The onset of Quaternary glaciations is a critical event in the climate and tectonic history of the Tibetan Plateau.The Shishapangma Glaciation,defined based on the till deposit from the northern slopes of Mt.Shishapangma,has been identified as the oldest glaciation on the Tibetan Plateau.However,the timing of this glaciation has not been constrained.We measured^(10)Be and^(26)Al concentrations of a set of boulders on top of this till and simulated their complex exposure-burial histories.The simulated results indicate that the formation age of this till is likely around 835.2±241.0 ka,representing the minimum timing of glacial onset on the Tibetan Plateau.The Shishapangma Glaciation is apparently much younger than the glacial onset in many other areas of the world,such as Europe and North America,and was likely driven by the coupled effect between tectonic uplift and climate cooling during the early–middle Pleistocene transition. | Yixin Chen Yingkui Li Mei Zhang Zhijiu Cui Gengnian Liu | 2018 | Science Bulletin2018，63，5： | 7 |
| 5 | Designing Advanced Aqueous Zinc-Ion Batteries:Principles,Strategies,and Perspectives显示文摘Aqueous zinc-ion batteries(AZIBs)are an appealing battery system due to their low cost,intrinsic safety,and environmental-friendliness,while their application is plagued by the obstacles from the cathode,electrolyte,and zinc anode.Summarizing the design principles and strategies toward the optimization of cathode,electrolyte,and zinc anode is crucial for the development of AZIBs.Herein,we present a comprehensive analysis of the design principles and promising strategies toward the improvement of AZIBs.Firstly,the various reaction mechanisms are summarized and the existing issues associated with the cathode,electrolyte,and zinc anode are discussed to guide the rational design of AZIBs.Subsequently,we provide an in-depth and comprehensive discussion on the design principles and strategies for the electrodes/electrolyte/separator optimization,and analyze the advantages and disadvantages of various strategies.Importantly,the design principles and strategies of the newly appeared conversion-type AZIBs,such as Zn-S battery and Zn-Se battery,are also discussed and analyzed.The effect of design strategies on the electrochemical performance and the relationship between the current issues and strategies are also unveiled in detail.Finally,some research trends and perspectives are provided for designing better AZIBs. | Yan Li Zhouhao Wang Yi Cai Mei Er Pam Yingkui Yang Daohong Zhang Ye Wang Shaozhuan Huang | 2022 | Energy & Environmental Materials2022，5，3： | 4 |
| 6 | Area,lake-level and volume variations of typical lakes on the Tibetan Plateau and their response to climate change,1972-2019显示文摘Most lakes have undergone significant changes on the Tibetan Plateau in recent decades,affecting water resources on the Tibetan Plateau and its surrounding areas.In this paper,we investigated the variations of 25 lakes in five sub-regions on the Tibetan Plateau from 1972 to 2019 based on SRTM DEM data and Landsat imagery.We used a method to derive lake-levels based on DEM and lake boundaries delineated from Landsat imagery,and then calculated the changes in lake area,level,and volume in 1972 to 2019.We also analyzed the potential impacts of temperature,precipitation,glacial and permafrost melting in lake changes during this period.The results show that the lakes tended to shrink until 2010 in southern and western plateau,after which they began to expand gradually but the overall trend is still shrinking.Limited meltwater from glaciers and permafrost and low precipitation are the main reasons for their shrinkage.The lakes in the central plateau,northwest plateau and northeast plateau tend to expand overall.The reason for the expansion of the lakes is not only precipitation but also the melting of glaciers and permafrost.Overall,the lake changes have gone through 3 phases,namely a slight decrease during 1972-2000,a rapid increase during 2000-2010,and a slowdown in the last decade(2010-2019).Multiple factors such as temperature,precipitation,the state of glaciers and permafrost have contributed to the changes in the lake. | Ju Zhang Qingwu Hu Yingkui Li Haidong Li Jiayuan Li | 2021 | Geo-Spatial Information Science2021，24，3： | 2 |
| 7 | Microstructure and Performance of 2Y-PSZ/TRIP Steel Composites显示文摘2Y-PSZ/TRIP steel composites have been sintered by hot-pressing method. Their microstructure and mechanical properties were investigated by means of SEM, TEM, XRD and static tension, split Hopkinson pressure bar method.The results showed that the strength and elastic modulus of 2Y-PSZ/TRIP steel composites at room temperature decreased with the increase of 2Y-PSZ content. The main reason was that the combining strength was quite weak between the grains of ZrO2. Distortion induced martensite transformation and plasticity during the dynamic loading increased the strength and distortion capability of the composites. The transformation was carried out mainly through twins formation. The shape of martensite induced by distortion was lamellate with substructures of twins. The habit plane was near {259}γ with no mid-ridge and no explosion phenomena. The interface was straight between the austenite and martensite induced by distortion. The increase of 2Y-PSZ content, on the one hand, made the composite dynamic flow stress improved. Thereby, the fracture strength was improved. On the other hand, it depressed both the distortion capability and the martensite transformation induced by distortion. This resulted in the decrease of dynamic fracture strength. | Yingkui GUO, Yu ZHOU, Dongbo LI, Xiaoming DUAN and Tingquan LEISchool of Materials Science and Engineering, Harbin Institute of Technology, Harbin 150001, China | 2003 | Journal of Materials Science & Technology2003，19，2： | 2 |
| 8 | Glacial valley cross-profile morphology, Tian Shan Mountains, China显示文摘 | Yingkui Li Gengnian Liu Zhijiu Cui | 2001 | Geomorphology2001，，1： | 1 |
| 9 | A facile method to prepare CdS/polystyrene composite particles显示文摘 | Xinjian Cheng Qiang Zhao Yingkui Yang Sie Chin Tjong Robert K.Y. Li | 2008 | Journal of Colloid And Interface Science2008，，1： | 1 |
| 10 | Approach to soil erosion assessment in terms of land-use structure changes显示文摘 | Jinren Ni Yingkui Li | 2000 | Journal of Soil and Water Conservation2000，58，3： | 1 |
| 11 | Effect of crustal porosity on lunar magma ocean solidification显示文摘The lunar ferroan anorthosites,formed by plagioclase flotation from the crystallization of the lunar magma ocean,have an age span of over~200 Ma.However,previous thermal models predicted a much shorter time range.We propose that a much smaller thermal conductivity of anorthositic crust due to its high porosity may have delayed the solidification of the lunar magma ocean.Our thermal simulation results,using the thermal conductivity of porous lunar crust,show that crystallization of a 1000 km deep magma ocean could be prolonged to tens of millions of years,and up to 180 Ma under some extreme conditions.The porous crust alone can’t explain the large crustal age span,however.Other circumstances must be taken into consideration,such as a thick lunar soil. | Mingming Zhang Yingkui Xu Xiongyao Li | 2021 | Acta Geochimica2021，40，2： | 0 |
| 12 | A helium stratified and ingassed lower mantle: resolving the helium paradoxes显示文摘It is generally believed a variation of 3He/4He isotopic ratios in the mantle is due to only the decay of U and Th,which produces4 He as well as heat.Here we show that not only3He/4He isotopic ratios but also helium contents can be fractionated by thermal diffusion in the lower mantle.The driving force for that fractionation is the adiabatic or convective temperature gradient,which always produces elemental and isotopic fractionation along temperature gradient by thermal diffusion with higher light/heavy isotopic ratio in the hot end.Our theoretical model and calculations indicate that the lower mantle is helium stratified,caused by thermal diffusion due to*400℃temperature contrast across the lower mantle.The highest3He/4He isotopic ratios and lowest He contents are in the lowermost mantle,which is a consequence of thermaldiffusion fractionation rather than the lower mantle is a primordial and undegassed reservoir.Therefore,oceanicisland basalts derived from the deepest lower mantle with high3He/4He isotopic ratios and less He contents—the long-standing helium paradox,is solved by our model.Because vigorous convection in the upper mantle had resulted in disordered or disorganized thermal-diffusion effects in He,Mid-ocean ridge basalts unaffected by mantle plume have a relatively homogenous and lower!3He/4He isotopic compositions.Our model also predicts that 3He/4He isotopic ratios in the deepest lower mantle of early Earth could be even higher than that of Jupiter,the initial He isotopic ratio in our solar system,because the temperature contrast across the lower mantle in the early Earth is the largest and less4 He had been produced by the decay of U and Th.Moreover,the early helium-stratified lower mantle owned the lowest He contents due to over-degassing caused by the largest temperature contrast.Consequently,succeeding evolution of the lower mantle is a He ingassed process due to secular cooling of the deepest mantle.This explains why significant amount of He produced by the decay of U and Th in the lower mantle were not released,another long-standing heat–helium paradox. | Honggang Zhu Xuefang Li Yingkui Xu | 2020 | Acta Geochimica2020，39，1： | 0 |
| 13 | The effect of grid size on the quantification of erosion,deposition,and rill network显示文摘Hillslope rill/interrill erosion has been investigated from the perspective of runoff transport of sediment.Recent advances in terrestrial laser scanning can provide high-resolution elevation data up to centimeter levels,and temporal digital elevation models(DEMs)enabled the detection and quantification of sediment redistribution.Erosion and deposition are spatially heterogeneous across hillslopes,and the choice of resolution is critical when using a DEM to study the spatial pattern of the processes.This study investigates the influence of grid size on the sediment change calculation and rill network delineation based on two surveys using a terrestrial laser scanner on a hillslope with well-developed rills in 2014 and 2015.Temporal DEMs were used to quantify elevation changes and used to delineate rill networks.We produced DEM pairs of incremental grid sizes(1-cm,2-cm,5-cm,8-cm,10-cm,15-cm,20-cm,and 30-cm)for DEM difference and rill network delineation.We used the 1-cm DEM as the reference to compare the results produced from other DEMs.Our results suggest that erosion mainly occurs on the rill sidewalls,and deposition on the rill floors,with patches of erosion/deposition within the interrill areas.Both the area and volume of detectable change decrease as the grid size increases,while the area and volume of erosion are less sensitive compared to those of deposition.The total length and number of rills decrease with the increased grid size,whereas the average length of rills increases.The mean offset between delineated rill network and the reference increases with larger grid sizes.In contrast to the erosion and deposition detected within rills,minor changes are detected on the interrill areas,indicating that either no topographic changes occurred or the changes were too small to be detected on the interill areas by our finest 1-cm DEMs.We recommend to use the finest possible grid size that can be achieved for future studies. | Xiaoyu Lu Yingkui Li Robert A.Washington-Allen Yanan Li Haidong Li Qingwu Hu | 2017 | International Soil and Water Conservation Research2017，5，3： | 0 |
| 14 | Long-term hydrological impacts of land use/land cover change from 1984 to 2010 in the Little River Watershed,Tennessee显示文摘Assessing long-term hydrological impacts of land use/land cover(LULC)change is of critical importance for land use planning and water resource management.The Little River Watershed,Tennessee,is an important watershed supporting drinking water and recreational activities within and around the Great Smoky Mountains National Park in the Unites States.However,the potential hydrological impacts of LULC change,especially urbanization in recent decades,are not quantified.This paper assessed the long-term impacts of LULC change on streamflow and non-point source pollution using the Soil and Water Assessment Tool(SWAT)and a detailed LULC record from 1984 to 2010.The SWAT was first calibrated and validated using observed streamflowin 2010 and then simulated using different LULC patterns in 1984-2010 to quantify the long-term hydrological impacts caused by the LULC change.Simulated results indicated a minor 3%increase in streamflow for the whole watershed from 1984 to 2010,but with a distinct spatial pattern.The increase in streamflow is closely related to urban development.Almost no streamflow increase occurred in the upper watershed within the national park,whereas>10%increase occurred in the lower watershed,especially in areas close to cities.Model simulation also suggested 34.6%reduction in sediment and about 10%reduction in nutrient loads from 1984 to 2010,closely related to the decrease in agricultural land.However,without calibration and validation,the simulated reduction in the sediment and nutrient loads may be problematic because SWAT mainly simulates the static LULC patterns,whereas LULC transitions,such as construction phases,may generate more sediment and nutrient loads.In addition,the simulation also did not account for the sediment and nutrients generated from stream bank erosion. | Chunhao Zhu Yingkui Li | 2014 | International Soil and Water Conservation Research2014，2，2： | 0 |
| 15 | RPA3 is transcriptionally activated by YY1 and its depletion enhances radiosensitivity of triple-negative and HER2-positive breast cancer显示文摘RPA3(Replication Protein A3)(14 kD)is a part of the canonical heterotrimeric replication protein A complex(RPA/RP-A).This study aimed to explore the functional role of RPA3 and the mechanisms of its dysregulation in breast cancer.Data from the Cancer Genome Atlas(TCGA)-breast cancer patients and GSE75688 were utilized for gene expression and survival analysis.Breast cancer cell lines MDA-MB-231 and SK-BR-3 were used for in-vitro cell studies.Clonogenic assay and immunofluorescent staining ofγ-H2AX were performed to examine radiation-induced cytotoxicity.Systemic correlation analysis was performed to identify potential transcription factors(TFs)regulating RPA3 expression.ChIP-qPCR and dual-luciferase assay were conducted to verify the transcriptional activating effect of YY1 on RPA3 expression.Bioinformatic analysis showed that RPA3 expression was upregulated in breast cancer.Its upregulation was associated with poor survival of basal-like and HER2+cases.RPA3 inhibition by siRNA reduced colony formation and increasedγ-H2AX foci formation after irradiation in MDA-MB-231 and SK-BR-3 cells.RPA3 expression was transcriptionally activated by YY1 via promoter binding in the two cell lines.Both RPA3 and YY1 expression were positively correlated with their gene-level copy numbers.RPA3 might serve as a potential target for radio-sensitization in basal-like and HER2+breast cancer. | YANFEI LI LULU DAI KE CAI YINGKUI SONG XIQING LIU | 2021 | BIOCELL2021，45，3： | 0 |
| 16 | Photothermal‐boosted polaron transport in Fe_(2)O_(3)photoanodes for efficient photoelectrochemical water splitting显示文摘Introduction of the photothermal effect into transition-metal oxide photoanodes has been proven to be an effective method to improve the photoelectrochemical(PEC)water-splitting performance.However,the precise role of the photothermal effect on the PEC performance of photoanodes is still not well understood.Herein,spinel-structured ZnFe_(2)O_(4)nanoparticles are deposited on the surface of hematite(Fe_(2)O_(3)),and the ZnFe_(2)O_(4)/Fe_(2)O_(3)photoanode achieves a high photocurrent density of 3.17 mA cm^(-2)at 1.23 V versus a reversible hydrogen electrode(VRHE)due to the photothermal effect of ZnFe_(2)O_(4).Considering that the hopping of electron small polarons induced by oxygen vacancies is thermally activated,we clarify that the main reason for the enhanced PEC performance via the photothermal effect is the promoted mobility of electron small polarons that are bound to positively charged oxygen vacancies.Under the synergistic effect of oxygen vacancies and the photothermal effect,the electron conductivity and PEC performance are significantly improved,which provide fundamental insights into the impact of the photothermal effect on the PEC performance of small polaron-type semiconductor photoanodes. | Xiaoqin Hu Jing Huang Yu Cao Bing He Xun Cui Yunhai Zhu Yang Wang Yihuang Chen Yingkui Yang Zhen Li Xueqin Liu | 2023 | Carbon Energy2023，5，9： | 0 |
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