电网换相换流器型高压直流输电(line commutated converter based high voltage direct current,LCC-HVDC)是新能源大规模并网、远距离外送的关键。而直流闭锁、换相失败等故障可能导致送端短时无功过剩并引发暂态过电压,危及运行安全...电网换相换流器型高压直流输电(line commutated converter based high voltage direct current,LCC-HVDC)是新能源大规模并网、远距离外送的关键。而直流闭锁、换相失败等故障可能导致送端短时无功过剩并引发暂态过电压,危及运行安全。文中突破传统基于电压-电流级联控制的电流源外特性快速无功补偿装置的技术原理,提出一种应用构网型无功补偿装置(grid-forming based reactive power compensation device,GFM-RPC)抑制新能源送端暂态过电压的方法,构建基于微分-代数关系的电压动态分析模型,阐明GFM-RPC抑制暂态过电压机理,并分析GFM-RPC相比现有基于静止同步补偿器(static synchronous compensator,STATCOM)抑制暂态过电压方法的优势。利用仿真验证GFM-RPC抑制新能源送端暂态过电压的效果,并分析主要参数对过电压抑制效果的影响。研究表明,STATCOM这类电流源外特性的无功补偿装置在直流输电系统故障瞬间呈现出恶化电压动态的“反调”特性,而GFM-RPC能够克服这种“反调”特性,并且通过合理的参数配置可以进一步抑制电压幅值的超调量。展开更多
Jiama is a giant,high-grade porphyry copper system in the Gangdese metallogenic belt,Tibet.Multistage intermediate-felsic porphyries intruded in this deposit,some of which are strongly associated with copper-polymetal...Jiama is a giant,high-grade porphyry copper system in the Gangdese metallogenic belt,Tibet.Multistage intermediate-felsic porphyries intruded in this deposit,some of which are strongly associated with copper-polymetallic mineralization.These ore-bearing porphyries include monzogranite,granodiorite,and quartz diorite porphyries.A new granite aplite dyke was found in the south of Jiama.Its age,genesis,and relationship with ore-related magmatism are obscure.Here,its emplacement age and petrogenesis were determined using mineralogy,zircon U-Pb dating,geochemistry,and Sr-Nd-Pb isotope studies.The zircon LA-ICP-MS U-Pb age of the aplite dyke is 16.66±0.21 Ma(n=14,MSWD=0.66),earlier than that of the ore-bearing porphyries(~15 Ma)in Jiama.Furthermore,the aplite exhibits high amounts of silicon(SiO_(2)=73.39%-74.74%),potassium(K_(2)O=5.12%-6.61%),aluminum(Al_(2)O_(3)=14.25%-14.69%),and light/heavy rare earth elements(LREE/HREE=12.12-16.19)as well as negative europium(δEu=0.47-0.72)and weak negative cerium anomalies(δCe=0.84-0.93).The aplite dyke is characteristic of metaluminous-peraluminous I-type granite,which is rich in large-ion lithophile elements(Rb,Ba,Th and U)and depleted in high-field-strength elements(Nb,P and Ti).The aplite dyke and ore-bearing porphyries in the Jiama deposit are the results of a partial melting of the juvenile lower crust,according to whole-rock geochemistry and Sr-Nd-Pb isotope data,but the dyke and ore-bearing porphyries were emplaced from the same magma chamber at different times.Thus,the aplite dyke shows the composition of the early evolution stage of shallow magma in the Jiama deposit and is the product of rapid condensation and crystallization.展开更多
文摘电网换相换流器型高压直流输电(line commutated converter based high voltage direct current,LCC-HVDC)是新能源大规模并网、远距离外送的关键。而直流闭锁、换相失败等故障可能导致送端短时无功过剩并引发暂态过电压,危及运行安全。文中突破传统基于电压-电流级联控制的电流源外特性快速无功补偿装置的技术原理,提出一种应用构网型无功补偿装置(grid-forming based reactive power compensation device,GFM-RPC)抑制新能源送端暂态过电压的方法,构建基于微分-代数关系的电压动态分析模型,阐明GFM-RPC抑制暂态过电压机理,并分析GFM-RPC相比现有基于静止同步补偿器(static synchronous compensator,STATCOM)抑制暂态过电压方法的优势。利用仿真验证GFM-RPC抑制新能源送端暂态过电压的效果,并分析主要参数对过电压抑制效果的影响。研究表明,STATCOM这类电流源外特性的无功补偿装置在直流输电系统故障瞬间呈现出恶化电压动态的“反调”特性,而GFM-RPC能够克服这种“反调”特性,并且通过合理的参数配置可以进一步抑制电压幅值的超调量。
基金supported by the National Key Research and Development Program of China(Grant No.2022YFC2905001)National Natural Science Foundation of China(Grant Nos.42272093 and 42230813)+2 种基金Basic Research Fund of Chinese Academy of Geological Sciences(Grant Nos.JKYZD202316,KJ2102,KK2116,and JKY202208)Geological Survey Project(Grant No.DD20221684)China Scholarship Council(Grant No.CSC202206400059)。
文摘Jiama is a giant,high-grade porphyry copper system in the Gangdese metallogenic belt,Tibet.Multistage intermediate-felsic porphyries intruded in this deposit,some of which are strongly associated with copper-polymetallic mineralization.These ore-bearing porphyries include monzogranite,granodiorite,and quartz diorite porphyries.A new granite aplite dyke was found in the south of Jiama.Its age,genesis,and relationship with ore-related magmatism are obscure.Here,its emplacement age and petrogenesis were determined using mineralogy,zircon U-Pb dating,geochemistry,and Sr-Nd-Pb isotope studies.The zircon LA-ICP-MS U-Pb age of the aplite dyke is 16.66±0.21 Ma(n=14,MSWD=0.66),earlier than that of the ore-bearing porphyries(~15 Ma)in Jiama.Furthermore,the aplite exhibits high amounts of silicon(SiO_(2)=73.39%-74.74%),potassium(K_(2)O=5.12%-6.61%),aluminum(Al_(2)O_(3)=14.25%-14.69%),and light/heavy rare earth elements(LREE/HREE=12.12-16.19)as well as negative europium(δEu=0.47-0.72)and weak negative cerium anomalies(δCe=0.84-0.93).The aplite dyke is characteristic of metaluminous-peraluminous I-type granite,which is rich in large-ion lithophile elements(Rb,Ba,Th and U)and depleted in high-field-strength elements(Nb,P and Ti).The aplite dyke and ore-bearing porphyries in the Jiama deposit are the results of a partial melting of the juvenile lower crust,according to whole-rock geochemistry and Sr-Nd-Pb isotope data,but the dyke and ore-bearing porphyries were emplaced from the same magma chamber at different times.Thus,the aplite dyke shows the composition of the early evolution stage of shallow magma in the Jiama deposit and is the product of rapid condensation and crystallization.
