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Provenance of colorless and brown volcanic glass in late Pleistocene tephra layers in the Western Philippine Sea

Journal of Oceanology and Limnology 2024年第05期 1438-1449页

作者： fuqing jiang Zhishun ZHANG Zhaohui ZHANG Guoliang ZHANG Peng HUANG Xiaojing ZHOU Zhifang XIONG Congying LI Tiegang LI Key Laboratory of Ocean Observation and Forecasting and Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences Laboratory for Marine Geology Qingdao Marine Science and Technology Center University of Chinese Academy of Sciences Institute of Marine Chemistry and Environment Ocean College Zhejiang University College of Marine Technology and Environment Dalian Ocean University Key Laboratory of Marine Sedimentology and Environmental Geology First Institute of Oceanography Ministry of Natural Resources

Tephra layers in the western Philippine Sea,characterized by abundant volcanic glass shards,may provide crucial evidence on the eruption history of volcanoes and tectonic evolution of the western Pacific.A 220-ka sediment core from the Benham Rise in the western Philippine Sea offers new insights into the provenance of four intercalated tephra layers （T1–T4,in chronological order） containing either colorless or brown glass *** to primitive mantle,all glass shards are enriched in large-ion lithophile elements,such as Rb,Cs,and Pb,and depleted in high field-strength elements,such as Th,Nb,and Ta,indicating a subduction-related *** colorless glass shards are characterized by high SiO2（>78%） and light rare earth element （LREE） contents as well as high La/Sm ratios （>9）,low FeO and MgO contents （100）,pointing to a rhyolitic composition and a medium-K calc-alkaline serial *** contrast,the brown glass shards are characterized by lower SiO2（<63%） and LREE contents,higher FeO,MgO,and CaO contents,lower La/Sm （<6） and Ba/Th （<75）,and similar Sr/Y ratios （<15）,indicating derivation from medium to high-K calc-alkaline andesite *** glass shards from layers T3 （152 ka） and T4 （172 ka） were correlated with volcanic deposits from the Taal and Laguna Caldera in the Maccolod Corridor,respectively,while the colorless glass shards from layers T1 （36.5 ka） and T2 （61.2 ka） were likely sourced from the Irosin Caldera in the Bicol *** the provenance of late Pleistocene tephra layers in the western Philippine Sea is helpful to complement a Philippine volcanic history and establish a regional tephrochronostratigraphy.

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集群化发展模式下风电场预测、规划及控制关键技术综述

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电力工程技术 2024年第1期43卷 86-99页

作者：陶思钰江福庆南京航空航天大学自动化学院江苏南京211106

随着我国风电行业的快速发展,规模化发展风电对能源转型的推进至关重要。然而,由于风电场所处的复杂环境和高昂的建设运营成本等因素,集群化发展模式下的风电场面临着一系列技术难点和挑战。因此,文中针对集群化发展模式下风电场的建设... 详细信息

随着我国风电行业的快速发展,规模化发展风电对能源转型的推进至关重要。然而,由于风电场所处的复杂环境和高昂的建设运营成本等因素,集群化发展模式下的风电场面临着一系列技术难点和挑战。因此,文中针对集群化发展模式下风电场的建设和运营,重点总结了相关的预测、规划及控制关键技术。文中围绕风电场集群的关键技术与研究思路进行了归纳总结;针对风电场集群的特点,包括风资源量化表征与预测技术、多风电场协同优化规划技术以及多风电场控制与运行技术进行了详细探讨,对于每个技术领域,分析了当前的研究现状和取得的成果;最后,阐明了风电场集群建设和运营关键技术领域的发展趋势,并指出了待解决的技术难点,通过总结这些技术的研究成果为我国风电的规模化、集群化开发提供参考。

关键词：风电场集群风电机组组合预测协同规划协调控制人工智能(AI)

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Quantitatively distinguishing sediments from the Yangtze River and the Yellow River using δEu_N-ΣREEs plot

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Science China Earth Sciences 2009年第2期52卷 232-241页

作者： jiang fuqing ZHOU XiaoJing LI AnChun LI TieGang Key laboratory of Marine Geology and Environment Institute of OceanologyChinese Academy of SciencesQingdao 266071China Graduate University Chinese Academy of SciencesBeijing 100049China

Sediment samples were collected from the lower channel of the Yangtze River and the Yellow River and the contents of rare earth elements (REEs) were measured. In addition, some historical REEs data were collected from published literatures. Based on the δEuN-ΣREEs plot, a clear boundary was found be-tween the sediments from the two rivers. The boundary can be described as an orthogonal polynomial equation by ordinary linear regression with sediments from the Yangtze River located above the curve and sediments from the Yellow River located below the curve. To validate this method, the REEs con-tents of sediments collected from the estuaries of the Yangtze River and the Yellow River were meas-ured. In addition, the REEs data of sediment Core 255 from the Yangtze River and Core YA01 from the Yellow River were collected. Results show that the samples from the Yangtze River estuary and Core 255 almost are above the curve and most samples from the Yellow River estuary and Core YA01 are below the curve in the δEuN-ΣREEs plot. The plot and the regression equation can be used to distin-guish sediments from the Yangtze River and the Yellow River intuitively and quantitatively, and to trace the sediment provenance of the eastern seas of China. The difference between the sediments from two rivers in the δEuN-ΣREEs plot is caused by different mineral compositions and regional climate patterns of the source areas. The relationship between δEuN and ΣREEs is changed little during the transport from the source area to the river, and from river to the sea. Thus the original information on mineral compositions and climate of the source area was preserved.

关键词： sediment provenance Yangtze River Yellow River δEuN-ΣREEs plot

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Relative paleointensity of the geomagnetic field during the past 200 ka from the West Philippine Sea and its chronological significance

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Science China Earth Sciences 2009年第8期52卷 1115-1126页

作者： QingYong Meng AnChun Li TieGang Li fuqing jiang XiaoJing Zhou Key Lab of Marine Geology & Environment Institute of Oceanology Chinese Academy of Sciences Qingdao 266071 China Graduate University of the Chinese Academy of Sciences Beijing 100049 China

Our rock magnetic analysis of core Ph05 from the West Philippine Sea demonstrates that the core preserves a strong, stable remanent magnetization and meets the magnetic mineral criteria for relative paleointensity (RP... 详细信息

关键词： West Philippine Sea relative paleointensity geomagnetic field

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Sedimentation rates and provenance analysis in the Southwestern Okinawa Trough since the mid-Holocene

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Chinese Science Bulletin 2009年第7期54卷 1234-1242页

作者： LI ChuanShun jiang Bo LI AnChun LI TieGang jiang fuqing Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences Qingdao 266071 China Graduate University Chinese Academy of Sciences Beijing 100049 China China Ocean Press Beijing 100081 China

As a high-sedimentation rate depocenter along the path of the Kuroshio Current, the southwesternmost part of the Okinawa Trough is a key area to understand the Kuroshio history and sediments transpor-tation. A 34.17-m-long sediment core was obtained by the advanced piston corer of Marco Polo/IMAGES XII MARION DUFRESNE during the May 2005 from the Southern Okinawa Trough at site MD05-2908. The recovered sediments were analyzed by AMS 14C dating, coarse size fraction (>63 μm) extraction and moisture content determination in order to study its sedimentation flux and provenance. The depth-age relationship of core MD05-2908 was well constrained by 17 14C dating points. The sediments span across the mid-Holocene (6.8 ka B.P.) and have remarkablely high sedimentation rates between 1.8 and 21.2 m ka?1, which is well consistent with the modern observations from sediment traps. We identified five 70―200 a periods of abnormally rapid sedimentation events at 6790―6600 a B.P., 5690―5600 a B.P., 4820―4720 a B.P., 1090―880 a B.P., and 260―190 a B.P., during which the highest sedimentation rate is up to 21.2 m/ka. In general, the lithology of the sediments were dominated by silt and clay, associated with less than 5% coarse size fraction (>63 μm). As the most significant sediment source, the Lanyang River in northeastern Taiwan annually deliver about 10Mt materials to the coastal and offshore region of northeast Taiwan, a portion of which could be carried northward by currents toward the study area. Therefore, we concluded that the 5 abnormally rapid sedimentation events may be related to intensified rainfall in Taiwan and thus increased materials to our study area at that time. However, a few extreme-rapid sedimentation events cannot be explained by normal river runoff alone. The large earth-quakes or typhoons induced hyperpycnal discharge of fluvial sediment to the ocean may also act as a potential source supply to the Okinawa Trough.

关键词：南冲绳海槽沉积速率河流沉积物异常事件中期西南泥沙来源马可波罗

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Paleoenvironment evolution of the East Philippine Sea recorded in the new-type ferromanganese crust since the terminal Late Miocene

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Science China Earth Sciences 2007年第8期50卷 1179-1188页

作者： XU ZhaoKai LI AnChun jiang fuqing LI TieGang MENG QingYong JIN Ning Key Laboratory of Marine Geology and Environment Institute of OceanologyChinese Academy of SciencesQingdao 266071China Graduate University of Chinese Academy of Sciences Beijing 100039China

From systemic research of microstructure, geochemistry, uranium-series and 10Be isotope dating on a new-type deepwater ferromanganese crust from the East Philippine Sea, the paleoenvironment evolu-tion of the target area since the terminal Late Miocene was recovered. The vertical section changes of microstructure and chemical composition are consistent in the studied crust, which indicate three major accretion periods and corresponding paleoenvironment evolution of the crust. The bottom crust zone was formed in the terminal Late Miocene (5.6 Ma) with loose microstructure, high detritus content and high growth rate. Reductions of mineral element content, accretion rate and positive Ce-anomaly degree at 4.6 Ma indicate temporal warming, which went against the crust accretion and finally formed an accretion gap in the terminal Middle Pliocene (2.8―2.7 Ma). The more active Antarctic bottom sea-waters in the Late Pliocene (2.7 Ma) facilitated the fast transfer to the top pure crust zone. Hereafter, with the further apart of volcanic source and the keeping increase of eolian material (1.0 Ma), although surrounding conditions were still favorable, mineral element content still shows an obvious reducing trend. It thereby offers new carrier and data for the unclear paleoceanographic research of the target area since the terminal Late Miocene.

关键词： new-type ferromanganese crust record paleoenvironment evolution uranium-series dating 10Be isotope dating East Philippine Sea

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Superior low cycle fatigue property from cell structures in additively manufactured 316L stainless steel

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Journal of Materials Science & Technology 2022年第16期111卷 268-278页

作者： Luqing Cui Dunyong Deng fuqing jiang Ru Lin Peng Tongzheng Xin Reza Taherzadeh Mousavian Zhiqing Yang Johan Moverare Department of Management and Engineering Division of Engineering MaterialsLinköping UniversityLinköping SE-58183Sweden Shenyang National Laboratory for Materials Science Institute of Metal ResearchChinese Academy of SciencesShenyang 110016China School of Materials Science and Engineering The University of New South WalesSydneyNSW 2052Australia I-Form Advanced Manufacturing Research CentreDublin City UniversityDublin 9Ireland Ji Hua Laboratory Foshan 528200China

We have investigated the low cycle fatigue(LCF)properties and the extent of strengthening in a dense additively manufactured stainless steel containing different volume fractions of cell structures but having all other microstructure characteristics the *** samples were produced by laser powder bed fusion(L-PBF),and the concentration of cell structures was varied systematically by varying the annealing ***-controlled fatigue experiments performed on samples with a high fraction of cell structures reveal an up to 23 times increase in fatigue life compared to an essentially cell-free sample of the same grain *** electron microscopy characterizations reveal that the cell structures serve as the soft barriers to the dislocation propagation and the partials are the main carrier for cyclic *** cell structures,stabilized by the segregated atoms and misorientation between the adjacent cells,are retained during the entire plastic deformation,hence,can continuously interact with dislocations,promote the formation of nanotwins,and provide massive 3D network obstacles to the dislocation *** compositional micro-segregation caused by the cellular solidification features serves as another nonnegligible strengthening mechanism to dislocation ***,the cell structures with a high density of dislocation debris also appear to act as dislocation nucleation sites,very much like coherent twin *** work indicates the potential of additive manufacturing to design energy absorbent alloys with high performance by tailoring the microstructure through the printing process.

关键词： Additive manufacturing 316L stainless steel Fatigue behavior Cellular structure Nanotwins

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Geochemistry of rare earth elements in the mid-late Quaternary sediments of the western Philippine Sea and their paleoenvironmental significance

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Science China Earth Sciences 2014年第4期57卷 802-812页

作者： XU ZhaoKai LI TieGang WAN ShiMing YIN XueBo jiang fuqing SUN HanJie JinYong CHOI DhongIl LIM Key Laboratory of Marine Geology and Environment Institute of OceanologyChinese Academy of Sciences Department of Oceanography Kunsan National University South Sea Institute Korea Institute of Ocean Science and Technology

Based on a δ180 chronology, rare earth elements （REE） and other typical elements in sediments from core MD06-3047 in the western Philippine Sea were analyzed to constrain the provenances of the sediments and investigate quantitative changes in the Asian eolian input to the study area over the last 700 ka. Among the competing processes that might affect REE compositions, sediment provenance is the most important one. Provenance analysis suggests that the study sediments have two provenance end-members; local volcanic sources are dominant, and eolian dust from the Asian continent has a smaller contribution. During glacial periods, eolian input to the western Philippine Sea was enhanced. In contrast, material supply from local volcanics in- creased during interglacial periods. Changes in eolian input to the study area were probably related to the strength of the East Asian winter monsoon （EAWM） as well as aridity in the Asian continent on an orbital time scale, and were partly influenced by local control factors on shorter time scales. Therefore, we propose that the present study expands the application of the REE-based method for quantitatively estimating the eolian component from the mid-latitude northern Pacific to the low-latitude western Pacific. Additionally, the study preliminarily confirms the influence of EAWM-transported eolian materi- al on sedimentation in the western Philippine Sea since 700 ka.

关键词： eolian dust sediment provenance rare earth elements East Asian winter monsoon glacial/interglacial cycle western Philippine Sea

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A preliminary study on fingerprinting approach in marine sediment dynamics with the rare earth elements

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Acta Oceanologica Sinica 2010年第4期29卷 62-77页

作者： ZHOU Xiaojing LI Anchun jiang fuqing MENG Qingyong Key Laboratory of Marine Geology ＆ Environment Institute of Oceanology Chinese Academy of Sciences Qingdao 266071 China Graduate School of the Chinese Academy of Sciences Beijing 100039 China

Locating the quantitized natural sediment fingerprints is an important work for marine sediment dynamics *** total of 146 sediment samples were collected from the Shelf of the East China Sea and five rivers,including Huanghe （Yellow）,Changjiang （Yangtze）,Qiantang,Ou and Min *** sediment grain size and the contents of rare earth elements （REEs） were measured with laser particle size analyzer and ICP-MS *** results show that absolute REE content （ΣREE） and the concentration ratio of light REEs to heavy REEs （L/HREE） are different in the sediments among those *** are higher REE contents in being less than 2 m and 2–31 μm fractions in the Changjiang Estuary surface *** REE contents of bulk sediment are dominated by the corresponding values of those leading *** of sediment is higher close to the estuaries and declines seaward on the inner shelf of the East China Sea （ECS）.The L/HREE ratio has a tendency of increase southward from 28 ？ *** conditions plays a predominate role on spacial distributions of the surficial sediment’s REE *** some situations,the currents tend to remove the coarser light grains from initial populations,as well as the deposit of the finer heavy mineral *** other situations,the currents will change the ratio of sediment constituents,such as ratio between silts and clays in the *** a result,the various values of REE or L/HREE ratio in different bulk sediments are more affected by the change of size-fractions than source *** the long-term stable hydrodynamic environment,i.e.,the East China Sea Shelf,new sediment transport model based on the size and density gradation concept may help to understand the spatial distribution patterns of REE parameters.

关键词： rare earth elements fingerprints East China Sea Shelf sediment transport

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Sea-level changes controlled detrital sediment inputs to the Bicol Shelf in the western Philippine Sea since 150 ka

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Journal of Oceanology and Limnology 2020年第4期38卷 1153-1168页

作者： ZHANG Zhishun jiang fuqing LI Tiegang YANG Dezhou ZHOU Xiaojing XIONG Zhifang QIU Xiaohua JIA Qi YAN Yu FENG Xuguang Key Laboratory of Marine Geology and Environment Institute of OceanologyChinese Academy of SciencesQingdao 266071China Center for Ocean Mega-Science Chinese Academy of SciencesQingdao 266071China University of Chinese Academy of Sciences Beijing 100049China Laboratory for Marine Geology Qingdao National Laboratory for Marine Science and TechnologyQingdao 266237China Key Laboratory of Marine Sedimentology and Environmental Geology First Institute of OceanographyMinistry of Natural ResourcesQingdao 266061China Key Laboratory of Ocean Circulation and Waves Institute of OceanologyChinese Academy of ScienceQingdao 266071China School of Marine Science and Environment Dalian Ocean UniversityDalian 116023China No.1 Institute of Geology and Mineral Resources of Shandong Province Jinan 250014China School of Geography and Ocean Science Nanjing UniversityNanjing 210023China

Detrital sediments derived from the Philippine Islands are one of the main sources of deep-sea sediments in the western Philippine ***,systematic research on their characteristics and transport mechanisms are *** used parametric end-member analysis to quantitatively partition the grain size of detrital sediments in core MD06-3052 from the Bicol Shelf in the western Philippine Sea;three endmembers EMI,EM2,and EM3,whose respective modes were at 2,10,and 45 μm,were *** also measured the Sr and Nd isotopic compositions of different size fractions(20 μm) of the detrital sediments and the results showed that the detrital sediments mainly originate from the Philippine *** EMI and EM2 are transported to the Bicol Shelf mainly by surface and bottom currents from the islands,and component EM3 is delivered by gravity flow from the exposed shelf during low sea-level *** content of the total detrital fraction and the three end-members,as well as the mass accumulation rates(MARs) of the coarse detritus(EM2 and EM3),were considerably higher during glacial periods(40-14 ka and 150-130 ka) than during other intervals;the glacials corresponded to a low sea level,while the MAR of the fine detritus(EMI) did not increase remarkably during 40-14 *** therefore concluded that the input of coarse detritus to the Bicol Shelf from the islands was mainly controlled by sea-level *** of the input of fine-grained detritus(EM1) was influenced not only by sea level but also by ocean currents and regional ***,our results help understand "source-to-sink" processes in the western Pacific marginal seas and their response to global change.

关键词： Bicol Shelf late Pleistocene grain size sea level change

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