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35篇 您的检索式:作者名="LI Yinhui"
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1Progresses on microwave remote sensing of land surface parameters显示文摘Highly accurate observations at various scales on the land surface are urgently needed for the studies of many areas,such as hydrology,meteorology,and agriculture.With the rapid development of remote sensing techniques,remote sensing has had the capacity of monitoring many factors of the Earth's land surface.Especially,the space-borne microwave remote sensing systems have been widely used in the quantitative monitoring of global snow,soil moisture,and vegetation parameters with their all-weather,all-time observation capabilities and their sensitivities to the characteristics of land surface factors.Based on the electromagnetic theories and microwave radiative transfer equations,researchers have achieved great successes in the microwave remote sensing studies for different sensors in recent years.This article has systematically reviewed the progresses on five research areas including microwave theoretical modeling,microwave inversion on soil moisture,snow,vegetation and land surface temperatures.Through the further enrichment of remote sensing datasets and the development of remote sensing theories and inversion techniques,remote sensing including microwave remote sensing will play a more important role in the studies and applications of the Earth systems.SHI JianCheng DU Yang DU JinYang JIANG LingMei CHAI LinNa MAO KeBiao XU Peng NI WenJian XIONG Chuan LIU Qiang LIU ChenZhou GUO Peng CUI Qian LI YunQing CHEN Jing WANG AnQi LUO HeJia WANG YinHui 2012Science China Earth Sciences2012,55,7:24
2Present Geothermal Fields of the Dongpu Sag in the Bohai Bay Basin显示文摘The Dongpu sag is located in the south of the Bohai Bay basin, China, and has abundant oil and gas reserves. To date, there has been no systematic documentation of its geothermal fields. This study measured the rock thermal conductivity of 324 cores from 47 wells, and calculated rock thermal conductivity for different formations. The geothermal gradient and terrestrial heat flow were calculated for 192 wells on basis of 892 formation-testing data from 523 wells. The results show that the Dongpu sag is characterized by a medium-temperature geothermal field between stable and active tectonic areas, with an average geothermal gradient of 32.0°C/km and terrestrial heat flow of 65.6 mW/m2. The geothermal fields in the Dongpu sag is significantly controlled by the Changyuan, Yellow River, and Lanliao basement faults. They developed in the Paleogene and the Dongying movement occurred at the Dongying Formation depositional period. The geothermal fields distribution has a similar characteristic to the tectonic framework of the Dongpu sag, namely two subsags, one uplift, one steep slope and one gentle slope. The oil and gas distribution is closely associated with the present geothermal fields. The work may provide constraints for reconstructing the thermal history and modeling source rock maturation evolution in the Dongpu sag.ZUO Yinhui QIU Nansheng HAO Qingqing ZHANG Yunxian PANG Xiongqi LI Zhongchao GAO Xia 2014Acta Geologica Sinica(English Edition)2014,88,3:9
3Meso–Cenozoic Tectono-Thermal Evolution History in Bohai Bay Basin, North China显示文摘The thermal history of sedimentary basins is a key factor for hydrocarbon accumulation and resource assessment, and is critical in the exploration of lithospheric tectono-thermal evolution. In this paper, the Cenozoic thermal histories of nearly 200 wells and the Mesozoic thermal histories of 15 wells are modeled based on the vitrinite reflectance and apatite fission track data in Bohai Bay Basin, North China. The results show that the basin experienced Early Cretaceous and Paleogene heat flow peaks, which reveals two strong rift tectonic movements that occurred in the Cretaceous and the Paleogene in the basin, respectively. The thermal evolution history in Bohai Bay Basin can be divided into five stages including(1) the low and stable heat flow stage from the Triassic to the Jurassic, with the heat flow of 53 to 58 m W/m2;(2) the first heat flow peak from the Early Cretaceous to the middle of the Late Cretaceous, with a maximum heat flow of 81 to 87 m W/m2;(3) the first post-rift thermal subsidence stage from the middle of the Late Cretaceous to the Paleocene, with the heat flow of 65 to 74 m W/m2 at the end of the Cretaceous;(4) the second heat flow peak from the Eocene to the Oligocene, with a maximum heat flow of 81 to 88 m W/m2; and(5) the second thermal subsidence stage from the Neogene to present, with an average heat flow of 64 m W/m2.Yinhui Zuo Nansheng Qiu Jiawei Li Qingqing Hao Xiongqi Pang Zhongying Zhao Qi Zhu 2015Journal of Earth Science2015,26,3:6
4Multiple Dolomitization and Fluid Flow Events in the Precambrian Dengying Formation of Sichuan Basin, Southwestern China显示文摘The Precambrian Dengying Formation is a set of large-scale, extensively dolomitized, carbonate reservoirs occurring within the Sichuan Basin. Petrographic and geochemical studies reveal dolomitization was a direct result of precipitation by chemically distinct fluids occurring at different times and at different intensities. Based on this evidence, dolomitization and multiple fluid flow events are analyzed, and three types of fluid evolution models are proposed. Results of analysis show that Precambrian Dengying Formation carbonates were deposited in a restricted peritidal environment(630–542 Ma). A high temperature and high Mg^(2+) concentration seawater was a direct result of dolomitization for the micrite matrix, and for fibrous aragonite in primary pores. Geochemical evidence shows low δ^(18)O values of micritic dolomite varying from-1.29‰ to-4.52‰ PDB, abundant light rare earth elements(REEs), and low dolomite order degrees. Microbes and meteoric water significantly altered dolomite original chemical signatures, resulting in algal micritic dolomite and the fine-grained, granular, dolosparite dolomite having very negative δ^(18)O values. Finely crystalline cement dolomite(536.3–280 Ma) and coarsely crystalline cement dolomite have a higher crystallization degree and higher order degree. The diagenetic sequence and fluid inclusion evidence imply a linear correlation between their burial depth and homogenization temperatures, which closely resemble the temperature of generated hydrocarbon. Compared with finely crystalline dolomite, precipitation of coarsely crystalline dolomite was more affected by restricted basinal fluids. In addition, there is a trend toward a more negative δ^(18)O value, higher salinity, higher Fe and Mn concentrations, REE-rich. Two periods of hydrothermal fluids are identified, as the exceptionally high temperatures as opposed to the temperatures of burial history, in addition to the presence of high salinity fluid inclusions. The early hydrothermal fluid flow event was characterized by hot magnesium-and silicon-rich fluids, as demonstrated by the recrystallized matrix dolomite that is intimately associated with flint, opal, and microcrystalline quartz in intergranular or intercrystalline pores. This event was likely the result of a seafloor hydrothermal chimney eruption during Episode I of the Tongwan Movement(536.3±5.5 Ma). In contrast, later hydrothermal fluids, which caused precipitation of saddle dolomite, were characterized by high salinity(15–16.05 wt% NaCl equivalent) and homogenization temperatures(250 to 265°C), δ^(18)O values that were more enriched, and REE signatures. Geochemical data and the paragenetic sequence indicate that this hydrothermal fluid was related to extensive Permian large igneous province activity(360–280 Ma). This study demonstrates the presence of complicated dolomitization processes occurring during various paleoclimates, tectonic cycles, and basinal fluids flow; results are a useful reference for these dolomitized Precambrian carbonates reservoirs.PENG Bo LI Zongxing LI Guorong LIU Chenglin ZHU Shifa ZHANG Wang ZUO Yinhui GUO Yingchun WEI Xiaojie 2018Acta Geologica Sinica(English Edition)2018,92,1:5
5Meso-Cenozoic lithospheric thermal structure in the Bohai Bay Basin,eastern North China Craton显示文摘The Bohai Bay Basin is a region where part of the North China Craton has been thinned and destroyed. It has experienced two periods of crustal thinning that occurred during the Cretaceous and Paleogene, but investigations of its Mesozoic and Cenozoic lithospheric thermal structure are limited. Therefore, in this study,the distributions of mantle heat flow, crustal heat flow, and Moho temperatures during the Meso-Cenozoic are calculated based on analyses of the thermal history of the Bohai Bay Basin. The results indicate that the ratio of mantle heat flow to surface heat flow peaked during the late stages of the early Cretaceous and during the middle to late Paleogene. The corresponding mantle heat flow was more than 65% of the surface heat flow. Moho temperatures reached three peaks: 900-1100℃ in the late stages of the early Cretaceous;820-900℃ in the middle to late Paleogene; and(in the Linqing Depression, Cangxian Uplift, and Jizhong Depression) 770-810℃ during the early Neogene. These results reveal that the Bohai Bay Basin experienced significant geological change during the Cretaceous, including the transformation of lithospheric thermal structure from 'cold mantle and hot crust' before the Cretaceous to 'hot mantle and cold crust' after the Cretaceous. The results also indicate that the basin experienced two large-scale rifting events.Therefore, this work may provide the thermal parameters for further investigations of the geodynamic evolution of eastern China.Zongxing Li Yinhui Zuo Nansheng Qiu Jun Gao 2017Geoscience Frontiers2017,8,5:4
6The Distribution of Petroleum Resources and Characteristics of Main Petroliferous Basins along the Silk Road Economic Belt and the 21st-Century Maritime Silk Road显示文摘The Silk Road Economic Belt and the 21st-century Maritime Silk Road Initiative,abbreviated as the Belt and Road Initiative,is a primary development strategy of China's future international cooperation.Especially,the energy resource cooperation,including oil and gas resources cooperation,is an important part of this initiative.The Belt and Road has undergone complicated geological evolution,and contains abundant mineral resources such as oil,gas,coal,uranium,iron,copper,gold and manganese ore resources.Among these,Africa holds 7.8% of the world's total proven oil reserves.The oil and gas resources in Africa are relatively concentrated,with an overall low exploration degree and small consumption demand.Nigeria and Libya contain the most abundant oil resources in Africa,accounting for 2.2%and 2.9%of the world's total reserves,respectively.Nigeria and Algeria hold the richest natural gas resources in Africa,occupying 2.8%and 2.4%of the world's total reserves,respectively.Africa's oil and gas resources are mainly concentrated in Egypt,Sultan and Western Sahara regions in the northern Africa,and the Gulf of Guinea,Niger River and Congo River area in the western Africa.The Russia-Central Asia area holds rich petroleum resources in Russia,Kazakhstan,Turkmenistan and Uzbekistan.The potential oil and gas areas include the West Siberia Basin,East Siberia Basin and sea continental shelf in Russia,the northern and central Caspian Basin in Kazakhstan,the right bank of the Amu-Darya Basin,the East Karakum uplift and the South Caspian Basin in Turkmenistan,and the Amu-Daria Basin,Fergana Basin,Afghan-Tajik Basin and North Ustyurt Basin in Uzbekistan.The Middle East oil and gas resources are mainly distributed in the Zagros foreland basin and Arabian continental margin basin,and the main oil-producing countries include Saudi Arabia,Iran and Iraq.The Asia Pacific region is a new oil and gas consumption center,with rapid growth of oil and gas demand.In 2012,this region consumed about 33.6%of the world's total oil consumption and 18.9%of the world's total natural gas consumption,which has been ranked the world's largest oil and gas consumption center.The oil and gas resources are concentrated in China,Indosinian,Malaysia,Australia and India.The abundant European proven crude oil reserves are in Norway,Britain and Denmark and also rich natural gas resources in Norway,Holland and Britain.Norway and Britain contain about 77.5%of European proven oil reserves,which accounts for only 0.9%of the world's proven reserves.The Europe includes main petroliferous basins of the Voring Basin,Anglo-Dutch Basin,Northwest German Basin,Northeast German-Polish Basin and Carpathian Basin.According to the analysis of source rocks,reservoir rocks,cap rocks and traps for the main petroliferous basins,the potential oil and gas prospecting targets in the Belt and Road are mainly the Zagros Basin and Arabic Platform in the Middle East,the East Barents Sea Basin and the East Siberia Basin in Russia-Central Asia,the Niger Delta Basin,East African rift system and the Australia Northwest Shelf.With the development of oil and gas theory and exploration technology,unconventional petroleum resources will play an increasingly important role in oil and gas industry.HAO Qingqing ZUO Yinhui LI Lintao CHEN Weijun YI Junjie WU Lei 2017Acta Geologica Sinica(English Edition)2017,91,4:3
7Functional defect-patching of a zeolite membrane for the dehydration of acetic acid by perva- poration 显示文摘Chen Zan Yin Dehong Li Yinhui 2011Journal of Membrane Science2011,369,12:1
8Functional defect-patching of a zeolite membrane for the dehydration of acetic acid by pervaporation显示文摘Zan Chen Dehong Yin Yinhui Li Jianhua Yang Jinming Lu Yan Zhang Jinqu Wang 2011Journal of Membrane Science2011,,1:1
9Amylose-directed synthesis of CuS composite nanowires and microspheres显示文摘Li Yinhui Hua Jiwen Liu Guojun 2013Carbohydrate Polymers2013,92,:1
10The effect of large heat input on the microstructure and corrosion behaviour of simulated heat affected zone in 2205 duplex stainless steel显示文摘Yinhui Yang Biao Yan Jie Li Jia Wang 2011Corrosion Science2011,,11:1
11The effect of keratinocyte growth factor-2(KGF-2) on the proliferation of human keratinocytes显示文摘Objective;In vitro studies have shown that KGF-2 has a proliferative effect on neonatal foreskin kerati-nocytes.Cells from adult donors have been shown to respond to KGF-1 to a lesser degree than neonatal keratino-cytes.The purpose of the study was to investigate the proliferative effect of KGF-2 on keratinocytes from an adultsubject.Methods;Standard medium was Keratinocyte Growth Medium without BPE,hydrocortisone and EGF.Ke-ratinocytes cultured from a 48-year-old subject were seeded at 2 10~4 in 32 mm ...Yang Yinhui Fu Xiaobing Li Junyou Research Department of Burn Institute,304th Hospital,Beijing 100037 2002感染.炎症.修复2002,3,2:1
12Petroleum Distribution Characteristics of the Americas and the Exploration Prospect Analysis显示文摘The world's present demand for oil and gas is still in a rapid growth period, and traditional oil and gas resources account for more than 60% of the global oil and gas supply. The Americas is the world's second largest production and consumption center of liquid fuel, and is also the world's largest natural gas producer. In 2016, the Americas had 85.3 billion tons of proven oil reserves and 18.7 trillion m^3 of proven natural gas reserves, which account for 35.4% and 10.0% of world's total reserves, respectively. It produced 1267.1 Mt of oil and 1125.4 billion m^3 of natural gas, which account for 28.9% and 31.7% of the world's total production, respectively. The crude oil and natural gas reserves are mainly distributed in the U.S., Canada and Venezuela. The U.S. is the earliest and most successful country in shale gas exploration and development, and its shale gas is concentrated in the southern, central and eastern U.S., including the Marcellcus shale, Barnett shale, Eagle Ford shale, Bakken shale, Fayettevis shale, Haynsvill shale, Woodford shale and Monterey/Santos shale. The potential oil and gas resources in the Americas are mainly concentrated in the anticline and stratigraphic traps in the MiddleUpper Jurassic slope deposition of the North Slope Basin, the Paleozoic Madsion group dolomite and limestone in the Williston Basin, dominant stratigraphic traps and few structural traps in the Western Canada Sedimentary Basin, the Eocene structural-stratigraphic hydrocarbon combination, structuralunconformity traps and structural hydrocarbon combination, and the Upper Miocene stratigraphicstructural hydrocarbon combination in the Maracaibo Basin of Venezuela, the stratigraphic-structural traps and fault horst, tilting faulted blocks and anticlines related to subsalt structure and basement activity in the Campos Basin, the subsalt central low-uplift belt and supra-salt central low-uplift belt in the Santos Basin of Brazil, and the structural-stratigraphic traps in the Neuquen Basin of Argentina. In addition, the breakthrough of seismic subsalt imaging technology makes the subsalt deepwater sea area of eastern Barzil an important oil and gas potential area.HAO Qingqing LI Lintao ZUO Yinhui CHEN Weijun WU Lei YI Junjie 2018Acta Geologica Sinica(English Edition)2018,92,1:1
13Fabrication of SiO2 hollow microsphere with urchin-like structure based on template from directed assembly of block copolymer显示文摘Li Yinhui Sun Jianping Zhang Ganwei 2010Colloid & Polymer Science2010,288,:1
14The effect of large heat input on the microstructure and corrosion behavior of simu- lated heat affected zone in 2205 duplex stainless steel显示文摘Yinhui Yang Biao Yan Jie Li et a/ 2011Corrosion Science2011,53,11:1
15Sol-gel synthesis of silica/ amylose composite particles with core-shell structure显示文摘Li Yinhui Hu Jiwen Liu Guojun 2012Polymer2012,53,15:1
16Parameter estima- tion of FH signals based on STFT and music algorithm 显示文摘Li Tong Tang Yinhui Lv Jun 2010International Conference on Computer Appli- cation and System Modeling2010,,5:1
17β-Cyclodextrin carbon-based nanoparticles with a core-shell-shell structure for efficient adsorption of crystal violet and bisphenol A显示文摘Textile wastewater contains highly toxic,nondegradable,carcinogenic organic pollutants,causing severe damage to the ecological environment.In this work,β-cyclodextrin carbon-sphere-based nanocomposite(CS/SiO_(2)@β-CD)with a core-shell-shell configuration was prepared by hydrothermal synthesis and subsequent sedimentation-azeotropic distillation with SiO_(2)as intermediate layer for the removal of crystal violet(CV)and bisphenol A(BPA).The chemical structure and morphology of the CS/SiO_(2)@β-CD were characterized by FT-IR,SEM and TEM.The effects of contact time,pH,temperature and initial concentration of the absorbates on the adsorption property were explored.The CS/SiO_(2)@β-CD showed excellent adsorption capacity on CV and BPA,and the maximum adsorption capacity was 87.873 mg g^(-1)and 165.095 mg g^(-1),respectively.Their adsorption process was in line with the pseudo-second-order and pseudo-first-order kinetic models,respectively.The adsorption thermodynamics could be better fitted by Langmuir model than by Freundlich model.The calculated thermodynamic parameters(-ΔG0,ΔS0 andΔH0)illustrated the adsorption of CV was endothermic,in contrast,the adsorption of BPA was exothermic process.Furthermore,the CS/SiO_(2)@β-CD showed excellent recovery performance,making it a potential adsorbent for the practical treatment of textile wastewater.Tian Tian Mengling Liu Yinhui Li Jian Han Liang Ren Heike Lorenz Qing Wu Jianxin Chen 2022Particuology2022,20,3:1
18Circulating Micro RNAs are promising novel biomarkers of acute myocardial infarction显示文摘Wang Rongrong Li Ning Zhang Yinhui 2011Intern Med2011,50,17:1
19Functional defect- patching of a zeolite membrane for the dehydration of acet- icacid by pervaporation显示文摘Chen Zan Yin Dehong Li Yinhui 2011J Membr Sci2011,369,12:1
20The effect of large heat input on the microstructure and corrosion behaviour of simulated heat affected zone in 2205 duplex stainless steel 显示文摘Yang Yinhui Yah Biao Li Jie 2011Corrosion Science2011,53,:1
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