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A tectono-thermal perspective on the petroleum generation,accumulation and preservation in the southern Ordos Basin, North china

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Petroleum Science 2024年第3期21卷 1459-1473页

作者： Peng Yang zhan-Li Ren Jin-Hua Fu Hong-Ping Bao Hui xiao Zheng Shi Kun Wang Yuan-Yuan {2. Wen-Hui liu Wen-Hou Li State Key Laboratory of Continental Dynamics Department of GeologyNorthwest UniversityXi'an710069ShanxiChina National Engineering Laboratory for Exploration and Development of Low-Permeability Oil and Gas Fields Exploration and Development Research Institute of PetroChina Changqing Oilfield CompanyXi'an710018ShaanxiChina Shaanxi Key Lab of Petroleum Accumulation geology School of Earth Science and EngineeringXi'an Shiyou UniversityXian710065ShaanxiChina Wuxi Research institute of Petroleum geology Petroleum Exploration and Production Research InstituteSINOPECWuxi214126JiangsuChina

The southern Ordos Basin has excellent petroleum exploration ***,the tectono-thermal history and the controls on petroleum generation,accumulation and preservation conditions in southern basin are *** this study,we analyzed the present geothermal field,paleo-geothermal gradient,maturity of the hydrocarbon source rocks,uplift and cooling process and tectono-thermal evolution *** the study area,for the Ordovician,Permain and the Triassic strata,the present temperature is low(3070℃)in the southeastern area but high(80140℃)in the northwestern *** paleogeothermal gradient varied from 2.℃/km to 30℃/km with a heat flow of 58—69 m W/m^(2.(i.e.,a medium-temperature basin).The paleo-temperatures are higher than the present temperatures and the maximum paleo-temperatures controlled the thermal maturity of the source *** vitrinite reflectance(Ro)values of the Triassic strata are>0.7%and the thermal maturity reached the middlemature oil generation *** Rovalues of the Permian-Ordovician strata are>1.8%and the thermal maturity reached the over-mature gas generation *** southern Ordos Basin has experienced the multiple tectonic events at the Late Ordovician Caledonian(452.Ma),Late Triassic(2.5 Ma),Late Jurassic(165160 Ma),End-Early Cretaceous(110100 Ma)and Cenozoic(since 40 Ma).A large-scale tectonothermal event occurred at the End-Early Cretaceous(110100 Ma),which was controlled by lithospheric extension,destruction and *** event led to the highest paleo-temperatures and thermal maturities and coeval with the peak period of petroleum generation and *** southern Ordos Basin has undergone rapid and large-scale uplift since the Late Cretaceous due to expansion of the northeastern margin of the Tibetan Plateau,uplift of the Qinling orogenic belt and thrust faulting in the liupanshan tectonic *** southern Ordos Basin experienced tectonic overprinting that was strong in the south and weak in the *** str

关键词： Fission-track dating Vitrinitereflectance Geothermal field Tectono-thermal evolution Petroleum geology Ordos Basin

The issues on the commercialization of perovskite solar cells

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Materials Futures

Materials Futures 2024年第2期3卷 1-35页

作者： Lixiu zhang Yousheng Wang Xiangchuan Meng Jia zhang Pengfei Wu Min Wang Fengren Cao Chunhao Chen Zhaokui Wang Fu Yang {2.dong Li Yu Zou Xi Jin Yan Jiang Hengyue Li Yucheng liu Tongle Bu Buyi Yan Yaowen Li junfeng fang Lixin {2. Junliang Yang Fuzhi Huang Shengzhong liu Jizhong Yao Liangsheng Liao Liang Li Fei zhang Yiqiang zhan Yiwang Chen Yaohua Mai Liming Ding Center for Excellence in Nanoscience(CAS) Key Laboratory of Nanosystem and Hierarchical Fabrication(CAS)National Center for Nanoscience and TechnologyBeijing 100190People’s Republic of China institute of New Energy Technology College of Information Science and TechnologyJinan UniversityGuangzhou 510632People’s Republic of China institute of Polymers and Energy Chemistry(IPEC) Nanchang UniversityNanchang 330031People’s Republic of China School of Information Science and Technology Fudan UniversityShanghai 200433People’s Republic of China School of Chemical Engineering and Technology Tianjin UniversityTianjin 300072People’s Republic of China School of Physical Science and Technology Soochow UniversitySuzhou 215006People’s Republic of China institute of Functional Nano&Soft Materials(FUNSOM) Soochow UniversitySuzhou 215123People’s Republic of China institute of optoelectronics Fudan UniversityShanghai 200433People’s Republic of China College of Chemistry Chemical Engineering and Materials ScienceSoochow UniversitySuzhou 215123People’s Republic of China School of Physics and Electronic Science East China Normal UniversityShanghai 200241People’s Republic of China State Key Laboratory for Artificial Microstructure and Mesoscopic Physics Department of PhysicsPeking UniversityBeijing 100871People’s Republic of China College of Biophotonics South China Normal UniversityGuangzhou 510631People’s Republic of China School of Materials Science and Engineering Beijing Institute of TechnologyBeijing 100081People’s Republic of China School of Physics and Electronics Central South UniversityChangsha 410083People’s Republic of China School of Materials Science and Engineering Shaanxi Normal UniversityXi’an 710119People’s Republic of China State Key Laboratory of Advanced Technology for Materials Synthesis and Processing Wuhan University of TechnologyWuhan 430070People’s Republic of China Microquanta semiconductor Hangzhou 311121People’s Republic of China

Perovskite solar cells have aroused a worldwide research upsurge in recent years due to their soaring photovoltaic performance,ease of solution processing,and low *** power conversion efficiency record is constantly being broken and has recently reached 2..1%in the lab,which is comparable to the established photovoltaic technologies such as crystalline silicon,copper indium gallium selenide and cadmium telluride(CdTe)solar ***,perovskite solar cells are standing at the entrance of industrialization,where huge opportunities and risks ***,towards commercialization,challenges of up-scaling,stability and lead toxicity still remain,the proper handling of which could potentially lead to the widespread adoption of perovskite solar cells as a low-cost and efficient source of renewable *** review gives a holistic analysis of the path towards commercialization for perovskite solar cells.A comprehensive overview of the current state-of-the-art level for perovskite solar cells and modules will be introduced first,with respect to the module efficiency,stability and current status of *** will then discuss the challenges that get in the way of commercialization and the corresponding strategies to address them,involving the upscaling,the stability and the lead toxicity *** into the future direction of commercialization of perovskite photovoltaics was also provided,including the flexible perovskite cells and modules and perovskite indoor ***,the future perspectives towards commercialization are put forward.

关键词： commercializations perovskite solar cells state-of-the-art level challenges and perspectives indoor photovoltaics

Biostratigraphic and Chemostratigraphic Correlation for the Base of the Middle Ordovician between Yichang and Western Zhejiang Areas,South china

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Acta Geologica Sinica(English Edition) 2011年第2期85卷 320-329页

作者： zhang yuandong Axel MUNNECKE CHEN Xu cheng {2. liu xiao State Key Laboratory of Palaeobiology and Stratigraphy Nanjing Institute of Geology and Palaeontology Nanjing 210008 China GeoZentrum Nordbayern FG Palaoumwelt University Erlangen-Nuremberg D-91054 Erlangen Germany Research institute of Petroleum Exploration and Development East China Company SINOPEC Nanjing 210011 China

The base of the Middle Ordovician （i.e. Dapingian Stage） has been defined at the first appearance datum （FAD） of conodont Baltoniodus？ triangularis at Huanghuachang, Yichang, china,but the precise correlation of the boundary to regions of other facies remain to be resolved. Herein we review the biostratigraphy and chemostratigraphy of the Huanghuachang Global Standard Stratotype-Section and Point （GSSP） section, and present our latest stratigraphic work on the nearby Chenjiahe s ection in Yichang, and the Hengtang Quarry section, Jiangshan, Zhejiang, which is regarded as representative of slope facies. The conodont and graptolite biostratigraphy as well as chemostratigraphy of the Chenjiahe section indicate that the base of the Middle Ordovician also falls within the graptolite Azygograptus suecicus Zone, and coincides with a high or maximum δ13C value within a minor positive carbon isotope excursion, suggesting that the base boundary can be readily recognized across the entire Yangtze Gorges area. The integrated graptolite and conodont biostratigraphy and chemostratigraphy of the Hengtang section, Jiangshan, indicates that the basal boundary probably falls within the graptolite lsograptus caduceus imitatus Zone that overlies the Azygograptus suecicus Zone, and coincides with a remarkable drop of δ13C. This difference indicates that a multi-disciplinary approach is critical to identify the base boundary in those regions where the Baltoniodus ？ triangularis is absent.

关键词： Graptolite biostratigraphy chemostratigraphy Middle Ordovician slope facies South china

CEPC Technical Design Report

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Radiation Detection Technology and Methods 2024年第1期8卷 I0003-I0016,1-1091页

作者： Waleed Abdallah Tiago Carlos Adorno de Freitas Konstantin Afanaciev Shakeel Ahmad Ijaz Ahmed xiaocong Ai Abid Aleem Wolfgang Altmannshofer Fabio Alves Weiming An Rui An Daniele Paolo Anderle Stefan Antusch Yasuo Arai Andrej Arbuzov Abdesslam Arhrib Mustafa Ashry Sha Bai Yu Bai Yang Bai Vipul Bairathi Csaba Balazs Philip Bambade Yong Ban Tripamo Bandyopadhyay Shou-Shan Bao Desmond P.Barber Ayse Bat Varvara Batozskaya Subash Chandra Behera Alexander Belyaev Michele Bertucci xiao-Jun Bi Yuanjie Bi Tianjian Bian Fabrizio Bianchi Thomas Biekotter Michela Biglietti Shalva Bilanishvili Deng Binglin Denis Bodrov Anton Bogomyagkov Serge Bondarenko Stewart Boogert Maarten Boonekamp Marcello Borri Angelo Bosotti Vincent Boudry Mohammed Boukidi Igor Boyko Ivanka Bozovic Giuseppe Bozzi Jean-Claude Brient Anastasiia Budzinskaya Masroor Bukhari Vladimir Bytev Giacomo Cacciapaglia Hua Cai Wenyong Cai Wujun Cai Yijian Cai Yizhou Cai Yuchen Cai Haiying Cai Hua{2. Cai Lorenzo Calibbi Junsong Cang Guofu Cao Jianshe Cao Antoine Chance Xuejun Chang Yue Chang Zhe Chang Xinyuan Chang Wei Chao Auttakit Chatrabhuti Yimin Che Yuzhi Che Bin Chen Danping Chen Fuqing Chen Fusan Chen Gang Chen Guoming Chen Hua-Xing Chen Huirun Chen Jinhui Chen Ji-Yuan Chen Kai Chen Mali Chen Mingjun Chen Mingshui Chen Ning Chen Shanhong Chen Shanzhen Chen Shao-Long Chen Shaomin Chen Shiqiang Chen Tianlu Chen Wei Chen Xiang Chen xiaoyu Chen Xin Chen Xun Chen Xurong Chen Ye Chen Ying Chen Yukai Chen Zelin Chen Zilin Chen Gang Chen Boping Chen Chunhui Chen Hok Chuen {2. Huajie {2. Shan {2. Tongguang {2. Yunlong Chi Pietro Chimenti Wen Han Chiu Guk Cho Ming-Chung Chu xiaotong Chu Ziliang Chu Guglielmo Coloretti Andreas Crivellin Hanhua Cui xiaohao Cui Zhaoyuan Cui Brunella D'Anzi Ling-Yun Dai Xinchen Dai Xuwen Dai Antonio De Maria Nicola De Filippis Christophe De La Taille Francesca De Mori Chiara De Sio Elisa Del Core Shuangxue Deng Wei-Tian Deng Zhi Deng Ziyan Deng Bhupal Dev Tang Dewen Biagio Di Micco Ran Ding Siqin Dingl Yadong Ding Haiyi Dong Jianin AGH University of Science and Technology Faculty of Physics and Applied Computer ScienceKrakow Anhui University HefeiAnhui Applied Physics Department Federal Urdu University of ArtsScience and TechnologyIslamabad Banaras Hindu University Institute of ScienceVaranasi Bandirma Onyedi Eylul University Bandirma Beihang University Beijing Beijing Computational Science Research Center Beijing Beijing Conveyi LTD Beijing Beijing Glass Research institute Co. LtdBeijing Beijing institute of Technology Beijing Beijing Normal University Beijing Brown University ProvidenceRI Budker institute of Nuclear Physics Novosibirsk Cadi Ayyad University Laboratory of Fundamental and Applied PhysicsPolydisciplinary FacultyMarrakech Cairo University Giza Center for Theory and Computation National Tsing Hua UniversityHsinchu Central china Normal University WuhanHubei Central South University ChangshaHunan Centro de Fisica Teorica de Particulas Universidade Tecnica de LisboaLisboa chengdu KaitengSifang Digital Radio&TV Equipment Co. LtdChengduSichuan china academy of engineering physics MianyangSichuan china building materials academy Beijing china Center of Advanced Science and Technology Beijing china institute of Atomic Energy Beijing china Jiliang University HangzhouZhejiang china Nuclear Instrument CO. LTDBeijing china University of Geosciences Beijing china University of Geosciences WuhanHubei china University of Mining and Technology XuzhouJiangsu china West Normal University NanchongSichuan Chongqing University Department of PhysicsChongqing Chulalongkorn University Bangkok City University of Hong Kong Department of PhysicsHong Kong Cockcroft institute Daresbury Cornell University IthacaNY CPPM(AMU/IPhU&CNRS/INP) Marseille Dalian Minzu University DalianLiaoning Dalian University of Technology Department of PhysicsDalian Deutsches Elektronen-Synchrotron DESY Hamburg Dzhelepov Laboratory of Nuclear Problems of Joint institute for Nuclear Research(DLNP JINR) Dubna East china University Of Science And Technol

The Circular Electron Positron Collider(CEPC)is a large scientific project initiated and hosted by china,fostered through extensive collaboration with international *** complex comprises four accelerators:a 30 GeV Linac,a 1.1 GeV Damping Ring,a Booster capable of achieving energies up to 180 GeV,and a Collider operating at varying energy modes(Z,W,H,and tt).The Linac and Damping Ring are situated on the surface,while the subterranean Booster and Collider are housed in a 100 km circumference underground tunnel,strategically accommodating future expansion with provisions for a potential Super Proton Proton Collider(SPPC).The CEPC primarily serves as a Higgs *** its baseline design with synchrotron radiation(SR)power of 30 MW per beam,it can achieve a luminosity of 5×10^(34)cm^(-2.s^(-1)per interaction point(IP),resulting in an integrated luminosity of 13 ab^(-1)for two IPs over a decade,producing 2.6 million Higgs *** the SR power to 50 MW per beam expands the CEPC's capability to generate 4.3 million Higgs bosons,facilitating precise measurements of Higgs coupling at sub-percent levels,exceeding the precision expected from the HL-LHC by an order of *** Technical Design Report(TDR)follows the Preliminary Conceptual Design Report(Pre-CDR,2.15)and the Conceptual Design Report(CDR,2.18),comprehensively detailing the machine's layout,performance metrics,physical design and analysis,technical systems design,R&D and prototyping efforts,and associated civil engineering ***,it includes a cost estimate and a preliminary construction timeline,establishing a framework for forthcoming engineering design phase and site selection *** is anticipated to begin around 2.2.-2.2.,pending government approval,with an estimated duration of 8 *** commencement of experiments and data collection could potentially be initiated in the mid-2.30s.

关键词： initiated exceeding precise

Comment on"Mudflat/distal fan and shallow lake sedimentation (upper Vallesian-Turolian) in the Tianshui Basin,Central china:Evidence against the late Miocene eolian loess"by ***-Zarza,***,***,***,***,***-Perez,***-Garcia,X.X

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Recent progress in perovskite solar cells:from device to commercialization

中国科学院地质与地球物理研究所第十届(2.10年度)学术年会

作者： Z.T.Guo~(a,*),J.Y Ge~a,G.Q,xiao~(b,c),Q.Z.Hao~a,H.B.Wu~a,T.zhan~a,L {2.~a,L Qin~a,F.M.Zeng~a,B.Y.Yuan~a a {2. of geology and Geophysics,chinese academy of sciences,P.O.Box 982.,Beijing 10002.,china b {2. of Earth Environment,chinese academy of sciences,Xian 710075,china c Graduate School of the chinese academy of Science,Beijing 100039,china

Alonso-Zarza et al.(2.09)argued that the Miocene sedimentary sequence near Qinan(QA-I)(Guo et al., 2.02.,north to Tianshui in Central china,represents mudflat/distal fan and shallow lake *** we show that they(1)did not take into account extensive observational evidence supporting an eolian origin;(2.erroneously correlated deposits of different origins and small lateral extent occurring in different geomorphic units;(3)inferred a common origin for distal fans in the Tianshui and Qinan regions despite contrasting tectonic and geomorphic conditions;and(4)in some cases misinterpreted features typical of eolian ***,their study is not a sufficient basis for challenging earlier interpretations of Asian paleoclimates.

关键词： Miocene and Pliocene eolian deposits fan and distal fan sediments Asian drying

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Science china Chemistry 2022年第12期65卷 2369-2416页

作者： Xinhui Luo Xuesong Lin Feng Gao Yang Zhao xiaodong Li Liqing zhan Zexiong Qiu Jin Wang Cong Chen Lei Meng xiaofeng Gao Yu zhang Zijian Huang Rundong fan Huifen liu Yanrun Chen xiaoxue Ren Jiahong Tang Chun-Hao Chen Dong Yang Yongguang Tu xiao liu Dongxue liu Qing Zhao Jingbi You junfeng fang Yongzhen Wu Hongwei Han xiaodan zhang Dewei Zhao Fuzhi Huang Huanping Zhou Yongbo Yuan Qi Chen Zhaokui Wang Shengzhong(Frank)liu Rui Zhu Jotaro Nakazaki Yongfang Li Liyuan Han State Key Laboratory of Metal Matrix Composites School of Material Science and EngineeringShanghai Jiao Tong UniversityShanghai 200240China State Key Lab for Mesoscopic Physics and Frontiers Science Center for Nano-optoelectronics School of PhysicsPeking UniversityBeijing 100871China Key Laboratory of Semiconductor Materials Science Institute of SemiconductorsChinese Academy of SciencesBeijing 100083China School of Physics and Electronic Science Engineering Research Center of Nanophotonics&Advanced InstrumentMinistry of EducationEast China Normal UniversityShanghai 200241China Key Laboratory for Advanced Materials and institute of Fine Chemicals School of Chemistry and Molecular EngineeringEast China University of Science and TechnologyShanghai 200237China Wuhan National Laboratory for Optoelectronics Huazhong University of Science and TechnologyWuhan 430074China institute of Photoelectronic Thin Film Devices and Technology Renewable Energy Conversion and Storage CenterSolar Energy Research CenterNankai UniversityTianjin 300350China College of Materials Science and Engineering&Engineering Research Center of Alternative Energy Materials&Devices Ministry of EducationSichuan UniversityChengdu 610065China Beijing National Laboratory for Molecular sciences CAS Key Laboratory of Organic SolidsInstitute of ChemistryChinese Academy of SciencesBeijing 100190China State Key Laboratory of Advanced Technology for Materials Synthesis and Processing Wuhan University of TechnologyWuhan 430070China Beijing Key Laboratory for Theory and Technology of Advanced Battery Materials Key Laboratory of Polymer Chemistry and Physics of Ministry of EducationSchool of Materials Science and EngineeringPeking UniversityBeijing 100871China School of Physics and Electronics Hunan Key Laboratory of Nanophotonics and DevicesCentral South UniversityChangsha 410083China Experimental Center for Advanced Materials School of Materials Science and EngineeringBeijing Institute of TechnologyBeijing 100081China Jia

Perovskite solar cells(PSCs) are undergoing rapid development and the power conversion efficiency reaches 2..7% which attracts increasing attention on their commercialization *** this review,we summarized the recent progress of PSCs based on device structures,perovskite-based tandem cells,large-area modules,stability,applications and ***,the challenges and perspectives are discussed,aiming at providing a thrust for the commercialization of PSCs in the near future.

关键词： perovskite solar cells device engineering stability application

不同相态二氧化碳前置酸压碳酸盐岩裂缝形成规律

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石油勘探与开发 2021年第3期48卷 639-645页

作者：郭建春詹立苟波张然刘超李骁任冀川西南石油大学油气藏地质及开发工程国家重点实验室成都610500 西华大学机械工程学院成都610500 陕西延长石油(集团)有限责任公司研究院西安710065 陕西省陆相页岩气成藏与开发重点实验室(筹) 西安710065

选取延安气田下古生界马五1亚段碳酸盐岩露头,开展了清水、液态CO_(2.、超临界CO_(2.作用下的真三轴压裂实验,同时采用CT扫描技术,分析了碳酸盐岩中压裂裂缝的起裂和扩展规律。研究表明,超临界CO_(2.黏度低,扩散性强,压裂过程中滤失量大... 详细信息

选取延安气田下古生界马五1亚段碳酸盐岩露头,开展了清水、液态CO_(2.、超临界CO_(2.作用下的真三轴压裂实验,同时采用CT扫描技术,分析了碳酸盐岩中压裂裂缝的起裂和扩展规律。研究表明,超临界CO_(2.黏度低,扩散性强,压裂过程中滤失量大,有利于提高井筒周围岩石孔隙压力,明显降低碳酸盐岩的破裂压力,但压裂过程中井筒压力上升缓慢,致裂岩石所消耗的超临界CO_(2.体积远大于清水;天然裂缝不发育的碳酸盐岩,采用清水、液态CO_(2.压裂易发生张性破坏,压裂裂缝主要沿最大水平主应力方向扩展,采用超临界CO_(2.压裂易发生剪性破坏且水平应力差对压裂裂缝形态影响较小,近井筒处压裂裂缝扩展方向与最大水平主应力方向呈45°夹角,随扩展延伸距离的增加,在离井筒较远处逐渐转向最大水平主应力方向,裂缝迂曲度与前者相比有所增加;天然裂缝发育的碳酸盐岩,清水易沟通低逼近角天然裂缝,压裂后易形成“阶梯状”裂缝,裂缝形态相对简单,液态CO_(2.黏度低,易沟通高逼近角天然裂缝,压裂后易形成多方向缝,裂缝形态相对复杂,沟通高逼近角天然裂缝是碳酸盐岩压后形成复杂裂缝的关键。

关键词：碳酸盐岩前置酸压液态CO_(2. 超临界CO_(2. 裂缝起裂裂缝扩展

快速城镇化进程中珠江三角洲硝酸型地下水赋存特征及驱动因素

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环境科学 2021年第10期42卷 4761-4771页

作者：吕晓立刘景涛韩占涛朱亮张玉玺中国地质科学院水文地质环境地质研究所石家庄050061 河北省地下水污染机理与修复重点实验室石家庄050061 生态环境部土壤与农业农村生态环境监管技术中心北京100012

随着经济的发展,我国地下水硝酸盐污染日趋严重,城镇化和工业化是硝酸型地下水频繁显现的主要驱动力.本文以城镇化快速发展的珠江三角洲为研究区,运用数理统计、主成分分析及"双因子"等方法探讨了研究区浅层硝酸型地下水的赋存环境特征... 详细信息

随着经济的发展,我国地下水硝酸盐污染日趋严重,城镇化和工业化是硝酸型地下水频繁显现的主要驱动力.本文以城镇化快速发展的珠江三角洲为研究区,运用数理统计、主成分分析及"双因子"等方法探讨了研究区浅层硝酸型地下水的赋存环境特征和驱动因素.结果表明,珠江三角洲地区地下水硝酸盐含量总体较高,全区1538组地下水样品中,硝酸盐浓度大于地下水Ⅲ类水质标准(88.6 mg·L^(-1))87组,超标率为5.7%;硝酸型水2.4组,占样品总数的18.5%.研究区硝酸型水分布广泛,主要分布于丘陵区及其与平原区交界处.其中广州、东莞、佛山和珠海等地区受城镇化和工业化影响出现了条带状的高溶解性总固体(TDS)硝酸型水,而在周边丘陵河谷区分布低TDS硝酸型水.西江、东江平原区,受工业废水及海咸水入侵影响,地下水TDS明显升高,该区域地下水NO_(3)^(-)质量浓度超Ⅲ类水标准但未影响水化学类型,然而工业化导致该区域硫酸型水频繁显现.研究区硝酸型水赋存于酸性或弱酸性环境,通常具有TDS和总硬度含量较低,Cl^(-)、SO_(4)^(2.)和K^(+)浓度较高等特征.硝酸型水的形成主要受生活污水、工业废水、农业氮肥、化粪池和垃圾渗滤液泄漏等影响.通常,高TDS硝酸型水的污染负荷高于低TDS硝酸型水.硝酸型水尤其是低TDS硝酸型水的圈定有利于识别出人类活动影响更为强烈的地下水,能够尽早识别出硝酸盐含量低但已具有潜在污染风险的地下水,对地下水的污染防控具有重要意义.

关键词：硝酸型地下水赋存环境特征驱动因素珠江三角洲城镇化

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杧果细菌性干枯病病原菌的分离与鉴定

中国南方果树 2019年第3期48卷 1-5页

作者：何忠勤柳凤詹儒林何红杨倩肖俊峰张榕王彬广东海洋大学农学院广东湛江524088 中国热带农业科学院南亚热带作物研究所广东湛江524091

细菌性干枯病是发生在广东杧果产区杧果上的一种新病害,为明确该病的病原菌种类,通过稀释涂布法分离和纯化、致病性测定,并结合形态学、生理生化特性及16S rDNA序列分析,对病原菌的种类进行鉴定。结果表明,从杧果干枯病病样中分离获得... 详细信息

细菌性干枯病是发生在广东杧果产区杧果上的一种新病害,为明确该病的病原菌种类,通过稀释涂布法分离和纯化、致病性测定,并结合形态学、生理生化特性及16S rDNA序列分析,对病原菌的种类进行鉴定。结果表明,从杧果干枯病病样中分离获得的菌株NY01,革兰氏染色呈阴性,菌体杆状,最适培养温度2.℃,最适pH值7.0～7.2.刺伤接种到健康杧果叶片,4 d后叶片呈现典型病斑。以菌株NY01的DNA为模板,扩增获得的16S rDNA片段,经BLAST分析,菌株NY01 16SrDNA序列与Sphingomonas sanguinis(登录号KT766073)的亲缘关系最近,同源性达到99.63%。经形态学、生理生化及16S rDNA序列分析将菌株NY01鉴定为血红鞘氨醇单胞菌***。血红鞘氨醇单胞菌能够引起杧果细菌性干枯病在国内属首次报道。

关键词：杧果血红鞘氨醇单胞菌病原菌分离鉴定