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| 1 | Composition, origin and weathering process of surface sediment in Kumtagh Desert, Northwest China显示文摘Kumtagh 沙漠是在中国的八最大的沙漠之一,但是因为存取的困难,以前糟糕调查我们的学科交差的学习。在这份报纸, 33 件代表性的表面沉积样品从在实验室荒芜、分析的 Kumtagh 被收集获得重矿物质部件和 geochemical 元素内容。结果证明重矿物质的各种各样的类型在这些样品是在场的,与绿帘石和角闪石的高水平。Si 和艾尔收起化学作文的大部分。与上面的大陆人外壳(UCC ) 的 geochemical 元素的平均作文相比,除了 Si 和 Ca,所有元素被弄空到某个度;Fe, Mg, Ca, P, Ti 和 Mn 在他们的内容有高关联系数。矿物质和 Kumtagh 荒芜的沉积的 geochemical 作文在 Altyn Tagh 山脉和 Taklamakan 沙漠的附近与 Altyn Tagh 山脉,和冲积/洪水的扇子的表面沉积的岩石的有类似,显示 Kumtagh 荒芜的沉积的一主要来源位于 Altyn Tagh 山脉。在 Aqik 山谷和 Shule 河的更低的活动范围的冲积沉积物和湖沉积是容易的被侵蚀并且搬运由强壮在东北弯屈进 Kumtagh 沙漠,形成沙漠的另一来源扔。一张 A-CN-K 第三的图证明由 Na 和 K 的损失捱过的弱度化学药品发生在这些沉积,而 A-CNK-FM 第三的图建议 Fe 和 Mg 经历了重要化学区别。物理捱过过程为 mafic 矿物质在好粒子引起容易的侵蚀和丰富,这样粗糙的荒芜的沙粒子能相对在 Fe 和 Mg 被弄空。在经历不太化学的捱过的干旱区域的沉积的矿物质和 geochemical 作文被物理捱过主要影响。 | XU Zhiwei LU Huayu ZHAO Cunfa WANG Xianyan SU Zhizhu WANG Zhenting LIU Hongyi WANG Lixin LU Qi | 2011 | Journal of Geographical Sciences2011，21，6： | 13 |
| 2 | Earth surface processes and their effects on human behavior in monsoonal China during the Pleistocene-Holocene epochs显示文摘There is a wide diversity of landforms in China.The topography of three major terraces,decreasing in height stepwise from west to east,was formed by the early Miocene.With the commencement of the Great Northern Hemisphere Glaciations(GHGs)and the glacial-interglacial cycles in the Pleistocene,thick loess deposits accumulated in north China,and fluvial terraces were formed and lakes expanded and contracted in eastern and central China.The earliest evidence of hominins in China is dated to ~1.7 Ma;they occupied the monsoon-dominated region for a long interval,until the late Pleistocene,~50 ka.In this study,we investigated a large area rich in the relics and artifacts of early man.The results indicate that the early humans occupied riverine areas,especially medium-sized fluvial basins,and lake shores.Even in the relatively recent geological past,the occupation and abandonment of settlements were directly forced by the shifting of sand dune fields in the desert-loess transitional zone,which in turn was closely associated with variations in the monsoon climate and vegetation patterns.Our observations indicate that landforms were one of the main determinants of early human behavior,in that loess tableland,large alluvial plains,desert-Gobi areas,and the Tibetan Plateau,were not suitable environments for early human settlement.We infer that the early humans in China adapted their behavior to specific landforms and landform processes.The monsoon climate,which shapes the large-scale step-like pattern of fluvial landforms,promotes vegetation coverage and dominates soil formation,provides a crucial context for early human adaptation.The adaptation of early humans to earth surface processes in East Asia is investigated for the first time in this study.Future investigations will provide further information that will increase our understanding of the linkage between early human behavior and landform processes in East Asia. | LU Huayu ZHUO Haixin ZHANG Wenchao WANG Shejiang ZHANG Hongyan SUN Xuefeng JIA Xin XU Zhiwei WANG Xianyan | 2017 | Journal of Geographical Sciences2017，27，11： | 12 |
| 3 | Climatic and tectonic controls on the fluvial morphology of the Northeastern Tibetan Plateau (China)显示文摘The geomorphological evolution of the Northeastern Tibetan Plateau(NETP)could provide valuable information for reconstructing the tectonic movements of the region.And the considerable uplift and climatic changes at here,provide an opportunity for studying the impact of tectonic and monsoon climate on fluvial morphological development and sedimentary architecture of fluvial deposits.The development of peneplain-like surface and related landscape transition from basin filling to incision indicate an intense uplift event with morphological significance at around 10–17 Ma in the NETP.After that,incision into the peneplain was not continuous but a staircase of terraces,developed as a result of climatic influences.In spite of the generally persisting uplift of the whole region,the neighbouring tectonic blocks had different uplift rates,leading to a complicated fluvial response with accumulation terraces alternating with erosion terraces at a small spatial and temporal scale.The change in fluvial activity as a response to climatic impact is reflected in the general sedimentary sequence on the terraces from high-energy(braided)channel deposits(at full glacial)to lower-energy deposits of small channels(towards the end of the glacial),mostly separated by a rather sharp boundary from overlying flood-loams(at the glacial-interglacial transition)and overall soil formation(interglacial).Pronounced incision took place at the subsequent warm-cold transitions.In addition,it is hypothesized that in some strongly uplifted blocks energy thresholds could be crossed to allow terrace formation as a response to small climatic fluctuations(10~3–10~4 year timescale).Although studies of morpho-tectonic and geomorphological evolution of the NETP,improve understanding on the impacts of tectonic motions and monsoonal climate on fluvial processes,a number of aspects,such as the distribution and correlation of peneplain and the related morphological features,the extent and intensity of tectonic movements influencing the crossing of climatic thresholds,leading to terrace development,need to be studied further. | WANG Xianyan Jef VANDENBERGHE LU Huayu Ronald VAN BALEN | 2017 | Journal of Geographical Sciences2017，27，11： | 6 |
| 4 | Distribution and Forming Model of Fluvial Terrace in the Huangshui Catchment and its Tectonic Indication显示文摘黄水河,黄河的一条主要支流,穿过显示出梯田的不同模式的一系列构造地减退并且高举的区域形成。黄水河的河的梯田的分发被学习通过地志并且印射的 sedimentologic 梯田。在 Haiyan 盆的三个平台,在 Huangyuan 盆的四个平台,在 Xi'ning 盆的 19 个平台(四个高平台可以属于另一条河) ,在 Ping'an 盆,在 Ledu 盆的五个平台和在 Minhe 盆的 12 个平台的九个平台被认出。Sedimentology 研究证明黄水河的 geomorphologic 和 sedimentological 模式,在西藏的边缘被定位,与在另外的区域的河的不同。平台的形成过程在黄水集水是更复杂的:累积平台和侵蚀梯田在每盆被形成,当侵蚀平台在另外的盆被形成时,累积平台在一些盆被开发,显示河的沉积可以与在另外的盆的河切口同时发生在一些盆。在黄水集水的这些二种河的平台的形成过程的一个概念的模型在这篇论文向前被带。首先,因为气候的变化或构造运动,河的平衡状态被打破,并且河在整个集水在所有盆切入直到到达一个新平衡状态。然后,下游的盆快速减退并且平衡状态再被打破,并且当河快速在沉淀盆积累时,河在在上游的盆切入直到再走近一个新平衡州。最后,因为气候的变化或构造运动和累积平台,河在整个集水切入当侵蚀平台在另外的盆被形成时,在沉淀盆被形成。累积平台的存在在黄水集水在亚盆暗示了构造沉淀。这些构造沉淀运动逐渐地从下游的 Minhe 盆发展了到在上游的 Huangyuan 盆。标明日期平台顺序有潜力揭开在在集水的沉淀之间的关系并且地区性在东北西藏的高原构造。 | WANG Xianyan LU Huayu Jef VANDENBERGHE CHEN Zhongyan LI Langpin | 2010 | Acta Geologica Sinica(English Edition)2010，84，2： | 3 |
| 5 | Tectonically-controlled infilling of the eastern Nihewan Basin,North China,since the middle Pleistocene显示文摘关于 Nihewan 盆的更新世进化的性质和原因有重要争论,诺思中国。我们在二个主要地点, Hutouliang 和 Donggou 学习了东方 Nihewan 盆沉积外形。领域观察的联合和沉积谷物尺寸分发的大小被用来重建自从中间的更新世,和光学地刺激的光大小,沉积环境的顺序被用来标明日期沉积。我们的结果显示一个浅湖沿着 Sanggan 河占据了盆中心,以前可能在完全消失前持续 440 kyr 直到 ~~ 340 kyr 以前。它被结束了 ~ 的河统治沉积累积的一个阶段接替 30 kyr 以前。我们建议峡的形成源于亲戚沿着 Liulengshan 差错 ~ Niuxin 山高举 140 kyr 以前。不管多么 ~ 30 kyr 以前,差错可能变得不活跃, Shixia 附近的河 downcutting 不再是由亲戚的偏移量高举,它从那时起在 Nihewan 盆从免职引起了移动到剥光。paleolake ~ 的消失 340 kyr 以前可以是盆 infilling 的进行中的过程的顶点。 | HAN ZhiYong LI XuSheng WANG Yong WANG XianYan YI ShuangWen LU HuaYu | 2016 | Science China Earth Sciences2016，59，7： | 2 |
| 6 | Placenta-derived IL-32β activates neutrophils to promote preeclampsia development显示文摘Immune activation at the maternal-fetal interface is a main pathogenic factor of preeclampsia(PE).Neutrophils(PMNs)are activated in PE patients,but the mechanism and consequences of PMN activation need to be further explored.Here,we demonstrated that interleukin-32(IL-32)expression was significantly upregulated in syncytiotrophoblasts(STBs)and that IL-32β was the major isoform with increased expression in the placenta of severe PE(sPE)patients.Furthermore,the level of IL-32 expression in the placenta was correlated with its level in the serum of sPE patients,indicating that IL-32 in the serum is derived mainly from the placenta.Then,in vitro experiments showed that IL-32β could highly activate PMNs and that these IL-32β-activated PMNs were better able to adhere to endothelial cells(HUVECs)and enhance the expression of vascular cell adhesion molecule-1(VCAM-1)and intercellular cell adhesion molecule-1(ICAM-1)in HUVECs,which could be reversed by preincubation with the NADPH oxidase inhibitor VAS 2870.In addition,we showed that IL-32β mainly activated PMNs by binding to proteinase 3.Finally,IL-32β administration induced a PE-like phenotype in a pregnant mouse model.This study provides evidence of the involvement of IL-32β in the pathogenesis of PE. | Dan Liu Qiang Li Hailin Ding Guangfeng Zhao Zhiyin Wang Chenrui Cao Yimin Dai Mingming Zheng Xiangyu Zhu Qianwen Wu Ya Wang Honglei Duan Huirong Tang Xianyan Lu Yayi Hou Yali Hu | 2021 | Cellular & Molecular Immunology2021，18，4： | 2 |
| 7 | Drainage evolution in intermontane basins at the Qinling-Daba Mountains显示文摘River capture is of great significance to landform evolution and hominine migration.In the Qinling-Daba Mountains,there is a viewpoint that Jialing River captured Hanjiang River,but this is still controversial.In this paper,we discuss the drainage evolution processes in intermountain basins at the Qinling-Daba Mountains based on a combination of detrital zircon UPb geochronology and geomorphic indexes.We suggest that the Hanjiang River gradually captured the Jialing River from east to west,accompanied by the evolution of the ancient Yangtze River.In terms of geomorphic evidences,wide valleys did not match with discharge,and a series of wind gaps developed in the Shiquan-Ankang basin.In addition,the valley shapes and width-toheight ratios(Vf)indicate two possible rapid incisions.The hypsometric integrals(HI)reflect that the landform gradually changes from the old stage to the youth stage from west to east.Theχvalues show that the drainage divide is moving to the side of the Yuehe River,and the Yuehe River is gradually shrinking.According to the sedimentary records,the zircon U-Pb age distributions indicate the provenance change.The high-altitude terraces show three age peaks(200–250,400–505,and 700–900 Ma),with the dominant Indosinian age peak(200–250 Ma),while the modern fluvial sediments only show a single peak of Jinning(700–900 Ma).These data show that there are two major river captures:(1)The ancient Hanjiang River cut through the regional compression ridge,and then captured the Hanzhong Basin river system(a part of the ancient Jialing river system)from east to west,and(2)The southern tributary captured the trunk with the uplift of the divide in the Shiquan-Ankang Basin,forming the modern drainage pattern in the upper Hanjiang River.The activities of the regional strike-slip fault,and the associated compression uplift played a key role in the river captures,the drainage evolution,and related landforms in the Shiquan-Ankang basin.In addition,it is shown that the evolution of the upper tributary basins lagged behind the response of the trunk channel to the tectonic activities and river captures.The interconnected wide valleys caused by river capture may have provided convenient geomorphological conditions for human migration into the Qinling-Daba Mountains along those river valleys. | Wanting XIE Xianyan WANG Hanzhi ZHANG Quanyu LIU Shejiang WANG Huayu LU | 2021 | Science China Earth Sciences2021，64，11： | 1 |
| 8 | Bioceramic scaffolds with triply periodic minimal surface architectures guide early-stage bone regeneration显示文摘The pore architecture of porous scaffolds is a critical factor in osteogenesis,but it is a challenge to precisely configure strut-based scaffolds because of the inevitable filament corner and pore geometry deformation.This study provides a pore architecture tailoring strategy in which a series of Mg-doped wollastonite scaffolds with fully interconnected pore networks and curved pore architectures called triply periodic minimal surfaces(TPMS),which are similar to cancellous bone,are fabricated by a digital light processing technique.The sheet-TPMS pore geometries(s-Diamond,s-Gyroid)contribute to a 3‒4-fold higher initial compressive strength and 20%-40%faster Mg-ion-release rate compared to the other-TPMS scaffolds,including Diamond,Gyroid,and the Schoen’s I-graph-Wrapped Package(IWP)in vitro.However,we found that Gyroid and Diamond pore scaffolds can significantly induce osteogenic differentiation of bone marrow mesenchymal stem cells(BMSCs).Analyses of rabbit experiments in vivo show that the regeneration of bone tissue in the sheet-TPMS pore geometry is delayed;on the other hand,Diamond and Gyroid pore scaffolds show notable neo-bone tissue in the center pore regions during the early stages(3-5 weeks)and the bone tissue uniformly fills the whole porous network after 7 weeks.Collectively,the design methods in this study provide an important perspective for optimizing the pore architecture design of bioceramic scaffolds to accelerate the rate of osteogenesis and promote the clinical translation of bioceramic scaffolds in the repair of bone defects. | Miaoda Shen Yifan Li Fengling Lu Yahui Gou Cheng Zhong Shukun He Chenchen Zhao Guojing Yang Lei Zhang Xianyan Yang Zhongru Gou Sanzhong Xu | 2023 | Bioactive Materials2023，，7： | 1 |
| 9 | Synergetic pretreatment of waste activated sludge by Fe(II)–activated persulfate oxidation under mild temperature for enhanced dewaterability显示文摘 | Guangyin Zhen Xueqin Lu Baoying Wang Youcai Zhao Xiaoli Chai Dongjie Niu Aihua Zhao Yuyou Li Yu Song Xianyan Cao | 2012 | Bioresource Technology2012，，： | 1 |
| 10 | The impacts of base level and lithology on fluvial geomorphic evolution at the tectonically active Laohu and Hasi Mountains,northeastern Tibetan Plateau显示文摘Previous researches had emphasized tectonic impacts on the fluvial system at the tectonically active areas,while the effects of lithology and local base level change have received relatively rare attention.Here we investigated fluvial landforms at different spatial scales,focusing on knickpoints and channel network reorganization from an area affected by the Haiyuan Fault in the northeastern Tibetan Plateau.The geomorphic indices,i.e.,drainage pattern andχanomalies,were calculated and investigated.The results show that two regional radial drainages formed around the Laohu and Hasi Mountains.Within the interior of the radial drainage,tributaries from the southeast side of the Laohu Mountain experienced near 180°direction change.We interpret this as the gradual drainage capture originating from the height difference(~190 m)of the local base level between the two catchments.Some tributaries from the Hasi Mountain show alternating gorges and broad valleys controlled by lithology.Besides,tectonic uplift and the lowering of base level(from the incision of the Yellow River)triggered an autogenic positivefeedback transition from parallel to dendritic drainage patterns.These observations suggest that base level change and lithology play a crucial role in landscape evolution,even in a tectonically active region. | Zhengchen LI Xianyan WANG Yang YU Huiping ZHANG Qi SU Xiaodong MIAO Huayu LU | 2021 | Science China Earth Sciences2021，64，6： | 0 |
| 11 | Diverse Climatic and Anthropogenic Impacts on Desertification in the Middle Reaches of Yarlung Zangbo River Catchment on the Tibetan Plateau显示文摘The unique desertification processes occurring under the Alpine climate and ecosystem on the Tibetan Plateau could provide critical clues to the natural and anthropogenic impacts on desertification.This study used the Landsat data to investigate the spatial and temporal distribution of desertification from 1990 to 2020 in two areas(Shannan and Mainling),within the Yarlung Zangbo River Basin.The results show not only distinct spatial patterns but also various temporal changes of desertification.In Shannan,aeolian sand was distributed over wide areas from valley floor to mountain slope,while in Mainling,it is distributed sporadically at the footslope.The aeolian sandy land initially expanded before undergoing long-term shrinkage in Shannan.While in Mainling,it steadily expanded followed by a rapid decrease.These changes are attributed to both climate change and human activites.The increase in temperature causes desertification expansion in Shannan,while favorable climate conditions coupled with decreasing human activity promoted desertification reversal.However,both the expansion and shrinkage of desertification were sensitive to human activity in Mainling.This highlights the diverse responses of desertification to natural and anthropogenic impacts on different backgrounds of climatic and vegetation coverage.A threshold of climatic conditions may control the dominance factors in desertification,shifting from natural to anthropogenic elements. | Qi Yu Xianyan Wang Zhiyong Han Xiaodong Miao Huayu Lu | 2023 | Journal of Earth Science2023，34，6： | 0 |
| 12 | Application of River Longitudinal Profile Morphometrics to Reveal the Uplift of Lushan Mountain显示文摘The stream power model was applied to Lushan Mt. in South China in order to verify its capability of interpreting the uplift of a small block mountain. On a log-log plot, the longitudinal profiles of 9 rivers derived from a 30 m DEM exhibit primary characteristics similar to those derived from a 5 m DEM; however, the 5 m DEM clearly reveals more minor knickpoints, and the positions of knickpoints are pinpointed more accurately. All of the studied rivers on the block mountain are in a transient state due to geological perturbations. Some of them exhibit two segments in steady state separated by a slopebreak knickpoint. Such rivers generally develop in a longitudinal valley, which are less perturbed by substrate inhomogeneities. The similar heights of the slope-break knickpoints and the similar uplift rate indicated by the k_(sn) values demonstrate an almost simultaneous headward erosion induced by the fall in base level. This modelling result is consistent with the mode of formation of this particular block mountain. Our study demonstrates that the stream power model is applicable to a small tectonicallyactive massif only if the channel segments are in a steady state. | HAN Zhiyong LI Xusheng WANG Nairui CHEN Gang WANG Xianyan LU Huayu | 2017 | Acta Geologica Sinica(English Edition)2017，91，5： | 0 |
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