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| 1 | The ion chemistry of surface and ground waters in the Taklimakan Desert of Tarim Basin,western China显示文摘The physio-chemical and chemical features of water in natural conditions are controlled by the weath-ering of bedrocks,local climate,landforms and other geo-environmental parameters. In order to un-derstand the characteristics of water and the origins of the dissolved loads in the rivers and in the ground waters of the Taklimakan Desert,western China,we studied the ions in the water samples col-lected from rivers and wells. We collected water samples from four rivers (Keriya River,Cele River,Tumiya River and Yulongkashi River) in the southern desert and ground water samples from many parts of the desert. Major cations and anions were measured using ion-chromatograph and titration with HCl. The total dissolved solids (TDS),pH and conductivity were examined on site by a portable multi-parameter analyzer. The data show that the water in the rivers of southern Taklimakan is still of fresh water quality and slight alkalinity,although the TDS is comparatively higher than that of many other rivers of the world. The ground water is fresh to slightly saline,with TDS a little higher than that of river water in the study area. The concentration of ions is slightly different between the four rivers in the southern Taklimakan. However,the chemistries of ground water in all samples are to a large degree controlled by sodium and chloride. The ions in the ground water are concluded to be mainly from dissolving of evaporites,consistent with the dry climate in the region,whereas the ions in the rivers are mainly from rock weathering. Low-level human imprints are recognized in the ground water samples also. | ZHU BingQi YANG XiaoPing | 2007 | Chinese Science Bulletin2007，52，15： | 15 |
| 2 | Image detection and verification of visual navigation route during cotton field management period显示文摘In order to meet the actual operation demand of visual navigation during cotton field management period,image detection algorithm of visual navigation route during this period was investigated in this research.Firstly,for the operation images under natural environment,the approach of color component difference,which is applicable for cotton field management,was adopted to extract the target characteristics of different regions inside and outside cotton field.Secondly,the median filtering method was employed to eliminate noise in the images and realize smoothing process of the images.Then,according to the regional vertical cumulative distribution graph of the images,the boundary characteristic of the cotton seedling region was obtained and the central position of the cotton seedling row was determined.Finally,the detection of the candidate points cluster was realized,and the navigation route was extracted by Hough transformation passing the known point.The testing results showed that the algorithms could rapidly and accurately detect the navigation route during cotton field management period.And the average processing time periods for each frame image at the emergence,strong seedling,budding and blooming stages were 41.43 ms,67.83 ms,68.80 ms and 74.05 ms,respectively.The detection has the advantage of high accuracy,strong robustness and fast speed,and is simultaneously less vulnerable to interference from external environment,which satisfies the practical operation requirements of cotton field management machinery. | Jingbin Li Rongguang Zhu Bingqi Chen | 2018 | International Journal of Agricultural and Biological Engineering2018，11，6： | 4 |
| 3 | Formation of the highest sand dunes on Earth显示文摘 | Xiaoping Yang Louis Scuderi Tao Liu Philippe Paillou Hongwei Li Jufeng Dong Bingqi Zhu Weiwei Jiang Andrew Jochems Gary Weissmann | 2011 | Geomorphology2011，，1： | 2 |
| 4 | Formation and evolution of sand deserts in Xinjiang, Northwest China: I. Provenances of desert sands显示文摘沙的荒芜的风景处于自然条件是干旱气候和丰富的沙材料供应的一个地质的产品,因此沙的沙漠的形成是为理解在地球系统的各种各样的 stratigraphic/epigenetic 范围之间的相互作用的一个理想的学习目标。直到现在,然而,这些的起源和形成的知识在 Xinjiang 抛弃,中亚多样、不一致,系统的评论是必要的。在在包围 Xinjiang 沙漠的新生代阶层的这些沙漠和他们的成双的灰尘存款的内部区域的古老的风神的沙沉积是反映沙漠的沙材料和形成和进化的起源的直接、间接的线索。在外部区域基于 geochemical,荒芜的沙的矿物学、同位素的证据和相关存款,这篇论文在 Xinjiang 在沙的沙漠的发展考察研究进步,西北中国。许多证明建议在 Xinjiang 的荒芜的沙主要从古老的雨、冲积、河的沉积被采购并且因为本地沙供应,最后被完成。它指出在 Xinjiang 的构造结构的设置在 Tarim 盆和被地区性的水文学系统极大地影响的 Junggar 盆使沉积成为了两个,风神的进程从行星的风系统发源西,东方亚洲冬季季风和地形学的山脉山谷弯屈。然而,交通路径的方向在水文学动力学和风神的动力学之间是不同的,分别地,它被盆 tectonics 和地区性的大气的发行量线路的倾斜的结构决定并且决定了不同代理人交付的这些沉积的运输小径的 anisotropies。这在二大盆导致由岩屑形成的沉积交通的一个地质的周期并且大部分因此增加沉积混合的度,引申并且在沙起源的更年轻、更旧的沉积来源,以及复杂性和差异之间再循环。 | ZHU Bingqi YU Jingjie QIN Xiaoguang Patrick RIOUAL LIU Ziting XIONG Heigang | 2014 | Journal of Geographical Sciences2014，24，1： | 2 |
| 5 | Formation and evolution of sand deserts in Xinjiang, Northwest China:II. The palaeo-environmental reconstruction显示文摘基于 palaeoclimatic 和地质的历史和人的历史时期的 palaeoenvironmental 证据,这篇论文在 Xinjiang 在沙的沙漠的发展考察研究和进步。它指出在 Xinjiang 的构造结构的特征使 Tarim 盆和被焚风效果极大地影响的 Junggar 盆从行星的风系统发源西,东方亚洲海洋大陆人季风和地形学的山脉山谷弯屈。气候和环境的地区性的模式自从第四级被变化在第二等的规模伴随的全面坚持的干旱描绘。在盆并且在边缘的风神的沉积的形成是对全球气候变化的潜在的回答,特别地,亚洲内地的 aridification 由西藏的高原和它的包围高地升起推出了。为关于 Taklamakan 沙漠的形成时间的问题,因为在以前的研究使用的研究方法,目标和信息搬运人是不同的,目前在学术圆有许多争论。从在边并且在这些沙的沙漠和他们的按年代先后的数据的内地的风神的扔 / 摇的证据显示干旱气候和土地出现自从第三级的时期,风神的进程发生在 Tarim 盆和它的内地区域的边。然而,在集体规模的这些过程的持续时间时间应该在中间的更新世以后开始了并且持续到 Holocene。沙丘领域在的出现最近在绿洲区域的 2000 年应该被人的因素极大地影响。 | ZHU Bingqi YU Jingjie QIN Xiaoguang Patrick RIOUAL ZHANG Yichi XIONG Heigang | 2014 | Journal of Geographical Sciences2014，24，3： | 1 |
| 6 | Provenance of aeolian sediment in the Taklamakan Desert of western China,inferred from REE and major-elemental data显示文摘 | Yang Xiaoping Zhu Bingqi White P D | 2007 | Quaternary International2007，175，： | 1 |
| 7 | Recharge to the inter-dune lakes and Holocene climatic changes in the Badain Jaran Desert, western China显示文摘 | Xiaoping Yang Nina Ma Jufeng Dong Bingqi Zhu Bing Xu Zhibang Ma Jiaqi Liu | 2009 | Quaternary Research2009，，1： | 1 |
| 8 | Climatic and geological factors contributing to the natural water chemistry in an arid environment from watersheds in northern Xinjiang,China显示文摘 | ZHU Bingqi YU Jingjie QIN Xiaoguang | 2012 | Geomorphology2012，，： | 1 |
| 9 | Hydrogeochemistry of three watersheds (the Erlqis, Zhungarer and Yili) in northern Xinjiang, NW China显示文摘 | Bingqi Zhu Xiaoping Yang | 2011 | Applied Geochemistry2011，26，： | 1 |
| 10 | Climate change and water security in the northern slope of the Tianshan Mountains显示文摘Water security is under threat worldwide from climate change. A warming climate would accelerate evaporationand cryosphere melting, leading to reduced water availability and unpredictable water supply. However, thewater crisis in the Northern Slope of Tianshan Mountains(NSTM) faces dual challenges because water demandsforfast-growing urban areas have put heavy pressure on water resources. The mountain-oasis-desert system featuresglacier-fed rivers that sustain intensive water use in the oasis and end in the desert as fragile terminal lakes.The complex balance between water conservation and economic development is subtle. This paper investigateschanges in hydroclimatic variables and water security-related issues on the NSTM. The spatiotemporal variationsin glaciers, climatic variables, rivers, lakes and reservoirs, groundwater, surface water, human water use, andstreamflow were analyzed for the past four decades. The results show that temperature in the NSTM exhibitedan apparent upward trend with a more significant warming rate in the higher altitude regions. Glacier massloss and shrinkage was strong. The average annual streamflow increased from 1980-1989 to 2006–2011 at mosthydrological stations. The monthly dynamics of surface water area showed notable variability at both inter-annual and seasonal scales, revealing the impacts of both natural and anthropogenic drivers on surface wateravailability in the region. The terrestrial water storage anomaly showed a decreasing trend, which might berelated to groundwater pumping for irrigation. Human water use for agriculture and industry grew with theincrease in cultivated land area and gross domestic product (GDP). The increased agricultural water use wasstrongly associated with the expansion of oases. It is unclear whether water availability would remain high underfuture climatic and hydrological uncertainties, posing challenges to water management. In the context of rapidurban growth and climate change, balancing water for humans and nature is vital in achieving the SustainableDevelopment Goals (SDGs) in NSTM. This study provides a baseline understanding of the interplay among water,climate change, and socio-economic development in NSTM. It would also shed light on wise water managementunder environmental changes for other rapidly developing mountain-oasis-desert systems worldwide. | Qiuhong Tang Xingcai Liu Yuanyuan Zhou Puyu Wang Zhongqin Li Zhixin Hao Suxia Liu Gang Zhao Bingqi Zhu Xinlin He Fadong Li Guang Yang Li He Haoxin Deng Zongxia Wang Xiang Ao Zhi Wang Paul P.J.Gaffney Lifeng Luo | 2022 | Geography and Sustainability2022，3，3： | 1 |
| 11 | IMPA2 blocks cervical cancer cell apoptosis and induces paclitaxel resistance through p53-mediated AIFM2 regulation显示文摘Cervical cancer continues to be a concern,and the prognosis of locally advanced cervical cancer remains poor.IMPA2 was previously identified as a potential oncogene and regulator of tumor apoptosis.In this study,we aim to further elucidate the underlying mechanisms of IMPA2 gene in the regulation of cervical cancer apoptosis.First,we identify AIFM2 as an upregulated gene in IMPA2-silenced cervical cancer cells,and inhibition of AIFM2 reverses IMPA2 knockdown-induced apoptosis.Further study reveals that AIFM2 regulates cell apoptosis in a mitochondrial-dependent manner with a redistribution of mitochondrial membrane potential and intracellular Ca^(2+) levels.However,the analysis of the STRING database and our experimental results show that AIFM2 has little effect on cervical cancer progression and survival.Further mechanistic study demonstrates that IMPA2 and AIFM2 silencing inhibits apoptosis by activating p53.Meanwhile,the knockdown of IMPA2 enhances the chemosensitivity of cervical cancer cells by strengthening paclitaxel-induced apoptosis.Based on the above results,the IMPA2/AIFM2/p53 pathway may be a new molecular mechanism for paclitaxel treatment of cervical cancer and an effective strategy to enhance the sensitivity of cervical cancer cells to paclitaxel.Our findings display a novel function of IMPA2 in regulating cell apoptosis and paclitaxel resistance mediated by a disturbance of AIFM2 and p53 expression,potentially making it a novel therapeutic target for cervical cancer treatment. | Kexin Xie Lei Liu Min Wang Xianping Li Bingqi Wang Sheng Yin Wanxin Chen Yingrui Lin Xiaolin Zhu | 2023 | Acta Biochimica et Biophysica Sinica2023，55，4： | 0 |
| 12 | Geomorphological Evolution and Palaeoenvironmental Change in the Western Alashan Plateau, China显示文摘Although neotectonic activity is considered to be the main factor of the terrain evolution of the Qinghai Tibet Plateau and its surrounding high-altitude areas,further geomorphological analysis and literature analysis are needed for the understanding of the geomorphic evolution and the Quaternary environment change of the western area of the Alxa Plateau near the northern Tibet Plateau.The purpose of this study is to investigate the distribution of site-specific geomorphic units of the landforms developed in the vast topography of Ejina Basin(Western Alxa),in order to identify the geostructural and climatic causes of the geomorphic landscape and its impact on the change of paleoenvironment.At present,the climate and hydrological conditions in Ejina are relatively monotonous and stable.In addition to tectonic dynamic factors,the most widely distributed landform in the basin is climate landform.There are both geomorphological and sedimentological anomalies of Aeolian landforms occurred in the whole basin,indicating that the underlying surface effect(retention effect)of river(Ejina River)and its related uneven ground and weak wind erosion(deflation)process in the nearby area may be the important factors controlling the formation of Ejina dunes,rather than the arid climate.It is believed that the extensive interaction between the aeolian and fluvial processes is the main mechanism of the regional geomorphic difference in Ejina Basin.According to the comparability of regional geomorphology and sedimentology,the period of the formation of relic geomorphology in the edge of Ejina Basin can be reasonably attributed to the local glacial maximum of the last glacial.The geomorphic transformation from quasi plain and desert valley to desert plain,the appearance of widely moving sand dunes and the presence of large ancient lake geomorphology all indicate that the drought index of Ejina Basin is increasing on the scale of geomorphic formation.Paleogeomorphological and chronological evidences show that the climatic and hydrological conditions of the basin in the last glacial period and the early Holocene are much better than those at present.For example,the average annual precipitation in the area before 39-23ka BP is between 60-350 mm(about 36 mm today),but there are large waves in the Holocene.The coexistence of various climates and landforms in Ejina Basin and the resulting geomorphic diversity should be the composite result of various geomorphic processes and surface processes besides glaciation.The low aridity(relative humidity)in the Ejina Region in the late Pleistocene may be the result of the enhancement of the westerly rain belt and the weakening of the Asian Winter Monsoon in the arid region of Central Asia. | Bingqi Zhu | 2020 | Journal of Geological Research2020，2，1： | 0 |
| 13 | The recent evolution of dune landforms and its environmental indications in the mid-latitude desert area(Hexi Corridor)显示文摘The history of dune landform changes and dust activity at mid-latitudes is a good archive for exploring environmental changes and related landscape response.In this study,the dynamic changes,material sources,dust activity history and the influencing factors of typical sand dunes in the Hexi Corridor were comprehensively analyzed from the aspects of aeolian geomorphology,grain-size sedimentology,geochemistry and climatology.The results show that in the past half century,the typical crescent-shaped dunes and chains of crescent-shaped dunes in the study area have moved or swayed greatly,with an average speed ranging from 0.8 m/a(Dunhuang)to 6.2 m/a(Minqin).The dynamic changes of sand dunes are mainly affected by annual precipitation,annual average wind speed and annual gale days,which indicates that climate is the primary influencing factor of dune landform changes.The three-stage grain-size curve model of dune sands is obviously different from that of gobi sediments(two-stage),revealing the“immaturity”of the latter in sedimentology,while the former has experienced efficiently aeolian differentiation and non-local origin.The comprehensive evidences of paleogeography,sedimentology and geochemistry reveal that the source materials of sand dunes are mainly alluvial/proluvial and palaeo-fluvial sediments,including clastic sediments in the denudation/erosion zones of the north and south piedmonts.Indicators such as the proportion of surface fine particles,the coverage of surface salt crusts,and the content of erodible sandy materials indicate that the western gobi areas are not the main source areas of wind-blown dust in the central and eastern parts of the Hexi Corridor.The spatial distribution of the movement direction of sand dunes is similar to that of the regional dominant wind direction,which indicates that the difference in the dynamic evolution of dune landforms between the east and west of the Hexi Corridor should be controlled by the regional-scale wind system,that is,controlled by the dynamic mechanism rather than the difference in material sources.The warming and humidification of the Hexi climate is a synchronous response to the global warming and the strengthening of the Asian Summer Monsoon.It is also the main reason for the reduction of dust storms in the study area,which means that a potential inverse desertification process exists in the Hexi Corridor during the same period and it is also controlled by climate change.However,the process of desertification in the oasis areas during the period is caused by groundwater fluctuation affected by human activities. | ZHU Bingqi | 2022 | Journal of Geographical Sciences2022，32，4： | 0 |
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