Jie Wang

Lanzhou University

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Bo Cao

Qufu Normal University

Hang Cui

Qinghai Normal University

Liubing Xu

South China Normal University

Jon Harbor

Purdue University West Lafayette

Baotian Pan

Lanzhou University

Pan Yao

Jiaying University

Yong Xiao

Beijing University of Chemical Technology

Hongjie Yang

Southwest Jiaotong University

Wenxu Hu

Southwest Jiaotong University

Baisheng Ye

Chinese Academy of Sciences

Cooperative Institutions

Chinese Academy of Sciences

201

University of Chinese Academy of Sciences

Lanzhou University

Tsinghua University

Northwest Institute of Eco-Environment and Resources

Sun Yat-sen University

Peking University

Ministry of Natural Resources

Institute of Tibetan Plateau Research

Beijing Normal University

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

FLUVIAL-LACUSTRINE SEDIMENTS AND HOLOCENE CLIMATIC AND HYDROLOGIC EVENTS IN THE RENQIU SECTION,CHINA

Marine Geology & Quaternary Geology (2005)

Cui Jian-xin Zhou Shang-zhe Han Haitao Jie Wang Liubing Xu

The histories of hydrologic and climatic events in central Hebei Plain,for the past 11 640 cal.aBP are reflected by the fluvial-lacustrine sediments using proxy records of grain size and magnetic susceptibility.We propose a model that explains variations in grain size and magnetic susceptibility of fluvial-lacustrine sediments as a record of Holocene climatic and hydrologic changes.The model is based on the site around Lake Baiyangdian and incorporates the processes of erosion and deposit that are correlative with regional climatic events.For the open lakes in the humid climatic regions of eastern China,the grain size is still reliable for the reconstruction of environmental changes.But as for the fluvial-lacustrine sediments in this region,the magnetic susceptibility has two kinds of mechanisms.Namely,in the fluvial sediments the magnetic mineral was much richer in coarse materials especially in the matter bigger than 125 μm.But to the lakes with great productivity,it positively correlates with the content of fine materials less than 10 μm in grain size. In the Holocene,this area has experienced three lake-spread episodes.The ages are 9 500~9 050,(8 110)~7 240 and 5 670~3 300 cal.aBP respectively.Once more,there were two major fluvial aggradation events at 9 050~8 110 and 6 700~6 240 cal.aBP when the lake contracted and the river course occupied the location of the lake basin.Both the lake extent and the river progradation were driven by climate changes.When the climate was warm and humid,the lake spread.In reverse,the river proceeded.

Aggradation

Progradation

Environmental Magnetism

Source

Cite

Citations (1)

Insight into the relationships between total suspended particles and mercury in meltwater in a typical glacierized basin in the inland Tibetan Plateau

Journal of Hazardous Materials (2023)

Xuejun Sun Qianggong Zhang Mingyue Li Jie Wang Zijian Lu

Meltwater

Accumulation zone

Mercury

10.1016/j.jhazmat.2023.131250

Cite

Citations (8)

Quaternary Glaciations

Developments in quaternary science (2011)

Shangzhe Zhou Jijun Li Jingdong Zhao Jie Wang Jingxiong Zheng

10.1016/b978-0-444-53447-7.00070-2

Cite

Citations (32)

Glacial advances and ESR chronology of the Pochengzi Glaciation, Tianshan Mountains, China

Science China Earth Sciences (2009)

Jingdong Zhao Shiyin Liu Jie Wang Yougui Song Jiankuo Du

Glacial landform

Terminal moraine

Landform

Deglaciation

10.1007/s11430-009-0109-9

Cite

Citations (10)

Experimental study on weathering mechanism of ancient bricks in Jiayuguan Wei-Jin tombs, Gansu, China

Heritage Science (2024)

Lihong An Zhen Qiao Jie Wang Fengrui Wang

Abstract This study focuses on the ancient bricks of Wei-Jin tombs in Jiayuguan, Gansu, China, analyzing the deterioration of the bricks under the long-term influence of natural environments and human activities. Currently, the ancient bricks exhibit various degradation diseases such as cracks, exfoliation, fracture, weathering, and microbial erosion, severely affecting the integrity of the cultural relics. Through on-site investigation and characterization testing, the physical and mechanical properties, compositional elements, pore size distribution, and thermal characteristics of the ancient bricks were analyzed. Indoor simulation experiments were conducted to study the impact of different types of environmental erosion cycles (such as H 2 O, HCl, NaOH, Na 2 SO 4 ) on the performance and structure of the ancient bricks, the patterns and causes of deterioration were also studied. The results indicate that the cyclic effects gradually transform the porosity of the ancient bricks into lateral microcracks, which continue to expand, leading to varying degrees of degradation of performance. The extent of the impact of these cycles on the properties of ancient bricks is in descending order: Na 2 SO 4 , HCl, NaOH, H 2 O. H 2 O, NaOH, HCl, Na 2 SO 4 .

10.1186/s40494-024-01229-x

Cite

Citations (1)

Cosmogenic 10Be dating of Guxiang and Baiyu Glaciations

Chinese Science Bulletin (2007)

Shangzhe Zhou Liubing Xu Patrick M. Colgan David M. Mickelson Xiaoli Wang

Surface exposure dating

Cosmogenic nuclide

10.1007/s11434-007-0208-y

Cite

Citations (61)

Dating of the Pleistocene Glaciations around the Daocheng Ice Cap

Journal of Glaciology and Geocryology (2004)

Liubing Xu Zhou Shang-zhe Cui Jian-xin Jie Wang

Plenty of glacial sediments since the earliest glaciation during the mid-Pleistocene are well preserved in the Daocheng Ice Cap area, southeastern Tibetan Plateau, where South Asian monsoon is active. Based on dating results of glacial deposits in this area using Electron Spin Resonance (ESR) and (()~(14)C) techniques, combined with glacial landforms and weathering differences of tills, it is believed that there were six major glaciations in the Daocheng Ice Cap area, corresponding to MIS-16, MIS-6, mid-MIS-3, early MIS-2, global LGM and postglacial period, respectively, with gradually decreasing glaciated extents. The earliest glaciation in this area occurred at about 571.2 ka BP, which means that the southeastern part of the Tibetan Plateau was uplifted above the snow line and began to develop glaciers at least 571.2 ka BP ago, and since then this region has been significantly uplifted. Before the Holocene, the glaciers in this region had ablated away completely and they did retreat gradually with several fluctuations.A noticeable result in this study is that during the last glacial cycle, the glaciers around the Daocheng Ice Cap advanced during the mid-Megainterstadial (MIS-3b), with a considerable extent, larger than that during the global LGM. Other researchers also have drawn similar conclusions about the Quaternary glaciers in the Himalayas. From these results, it is concluded that the glacial maximum during the last glacial period may not have occurred at the same time worldwide, contrary to what has usually been assumed. During the middle MIS-3, summer insolation was lower than that in the early and the late MIS-3, but the difference in insolation between land and sea could still induce a stronger summer monsoon. It brought heavy precipitation to the glaciers in the monsoon regions. Combined with the lower temperature, the heavier precipitation was favorable for most glaciers advancing in MIS-3b. During the Last Glacial Maximum, temperature was extremely low, but the summer monsoon was considerably weaker with little precipitation, which resulted in a depression of ELA less than that during MIS-3. The result further demonstrates that no unified ice sheet occurred in the Tibetan Plateau during the Quaternary.

Glacial landform

Last Glacial Maximum

Source

Cite

Citations (10)

Cosmogenic nuclide constraints on late Quaternary glacial chronology on the Dalijia Shan, northeastern Tibetan Plateau

Quaternary Research (2013)

Jie Wang Christine Kassab Jon Harbor Marc W. Caffee Hang Cui

Abstract Cosmogenic nuclide (CN) apparent exposure dating has become a widely used method for determining the age of glacial landforms on the Tibetan Plateau with > 1200 published ages. We present the first 10 Be exposure ages from the Dalijia Shan, the most northeastern formerly glaciated mountain range on the Tibetan Plateau. The moraine groups identified from field and remote sensing imagery mapping record four glacial events at 37.07 ± 3.70 to 52.96 ± 4.70 ka (MIS 3), 20.17 ± 1.79 to 26.99 ± 2.47 ka (MIS 2), 16.92 ± 1.49 to 18.76 ± 1.88 ka (MIS 2), and 11.56 ± 1.03 to 11.89 ± 1.06 ka (Younger Dryas). These ages indicate that glaciation in the northeastern Tibetan Plateau is much younger than previously thought. In addition, this record is consistent with many other regions on the Tibetan Plateau, with a local last glacial maximum during MIS 3 asynchronous with Northern Hemisphere last glacial maximum during MIS 2. The Dalijia Shan might also include an event of Younger Dryas age, but this needs to be tested in future studies.

Cosmogenic nuclide

Surface exposure dating

Chronology

Glacial landform

10.1016/j.yqres.2013.01.004

Cite

Citations (49)

Research on High Resolution Deformation Monitoring System Based on Computer Time Series

Yi Ling Jie Wang

This paper presents an automatic deformation monitoring system for time sequence monitoring of the rail transit engineering construction process. The double difference is obtained by combining the exact prior bit relative to the reference point. The displacement vector can be obtained by using the variation of the double difference between the reference point and the observed data. This project intends to obtain the ground object information with high consistency and accuracy through the combined detection method of multi-feature information and realize the inversion of elevation changes through the DInSAR time-series DInSAR data during the collection period of DINSAR images. Through the analysis of the measured data, the correctness of the algorithm's theoretical basis and mathematical model is verified.

Deformation monitoring

Basis (linear algebra)

10.1109/icdsca59871.2023.10393324

Cite

Citations (0)

A Study of the Regularity of Quaternary Geological History Evolution in Songliao Plain Based on Geological Remote Sensing Survey

Guotu ziyuan yaogan (2010)

Yunhao Chen Jie Wang Xiaobing Li

Coastal plain

Geological survey

10.6046/gtzyyg.2010.s1.32

Cite

Citations (2)