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| 1 | Environmental taxation and regional inequality in China显示文摘In order to combat environmental pollution, China enacted the Environmental Protection Tax Law in early 2018. Yet the impacts of the environmental tax on individual regions with different socioeconomic statuses, which are crucial for social justice and public acceptance, remain unclear. Based on a MultiRegional Input-Output(MRIO) table and a nationally regulated tax payment calculation method, this study analyzes the distributional impacts of an environmental tax based upon province’s consumption from both inter-provincial and rural-urban aspects. The national tax revenue based on the current levy mechanism is estimated to be only one seventh of the economic loss from premature mortality caused by ambient particulate matter(PM2.5). The taxation may slightly alleviate urban-rural inequality but may not be helpful with reducing inter-provincial inequality. We further analyze two alternative levy mechanisms. If each province imposes taxes to products it consumes(rather than produces, as in the current mechanism), with the tax rate linearly dependent on its per capita consumption expenditure, this would moderately increase the national tax revenue and significantly reduce inter-provincial inequality.To better compensate for the economic costs of air pollution and reduce regional inequality, it would be beneficial to increase the tax rate nationwide and implement a levy mechanism based on provincially differentiated levels of consumption and economic status. | Jingxu Wang Jintai Lin Kuishuang Feng Peng Liu Mingxi Du Ruijing Ni Lulu Chen Hao Kong Hongjian Weng Mengyao Liu Giovanni Baiocchi Yu Zhao Zhifu Mi Jing Cao Klaus Hubacek | 2019 | Science Bulletin2019，64，22： | 3 |
| 2 | Site-specific determination of TTR-related functional peptides by using scanning tunneling microscopy显示文摘为功能的肽的设计和优化, unravelling 单个积木的结构以及整体的性质是首要的。TTR1,源于人的 transthyretin,形成纤丝的肽在象家庭淀粉的 polyneuropathy 和老年的全身的淀粉样变性病那样的疾病被含有。基于 TTR1 脚手架,功能的肽 TTR1-RGD 被设计明确地与房间交往。这里,我们过去常扫描通道显微镜学(STM ) 与反向的顺序和修改前面的顺序分析 TTR1 相关的肽的集会结构。sitespecific 分析显示出下列:我) TTR1 肽涉及汇编,将近在订的表以内盖住全部长度组织。ii ) 为 TTR1-RGD 肽集会,当 RGDS 主题采用允许它支持房间粘附的灵活符合构造时, TTR1 主题形成订的表。关键地点清楚地作为连接器残余 Gly13 被识别。iii ) 尽管有在化学的差别,他们显示类似的集合的前面、反向的肽集会表演的仔细的检查特征,说明这些肽的柔韧的性质。iv ) Glycine 连接器残余在强烈建议顺序能被增加更多的连接器残余优化的 -strands, 被包括。进这些肽的装配结构的这些积累的卓见帮助解开驾驶肽集会的机制并且在新窗户中指示 sequenceprogrammed 肽 architectures.Open | Lanlan Yu Yongfang Zheng JingXu Fuyang Qu Yuchen Lin Yimin Zou Yanlian Yang Sally L. Gras Chen Wang | 2018 | Nano Research2018，11，1： | 1 |
| 3 | Rapid Screening of chloramphenicol in Turbot with photobacterium phosphoreum DB显示文摘A new,simple,rapid microbial assay was put forward for the detection of chloramphenicol(CAP)residues in Turbot muscles using luminescent bacteria DB(Photobacterium phosphoreum)as test organ-ism.By the luminescence inhibition of DB,the concentrations of CAP were determined.CAP spiked inTurbot muscle tissues ranging from 0.5 to 100μg/kg was extracted using ethyl acetate and hexane.Themethod had a good recovery of 93.69% with a minimum detection limit of 0.65μg/kg.It can be per-formed within 30min following simple extraction.The method therefore proved to be advantageous overchromatographic procedures as it was inexpensive,quite sensitive and can be adopted for rapid screeningof CAP in Turbot tissues. | 朱兰兰 Wang Jingxue Lin Hong Wang Yaqun Wang Jing Mei Cexia | 2009 | High Technology Letters2009，15，2： | 1 |
| 4 | Large Active Faults and the Wharton Basin Intraplate Earthquakes in the Eastern Indian Ocean显示文摘In recent years,great earthquakes occurred within the Wharton Basin in the eastern Indian Ocean,and they have been associa-ted with active faulting on the ancient oceanic crust.Large seismogenic faults were thought to be the fault reactivation on the ancient oceanic crust,but these phenomena are still unclear and require examination.This study used high-quality multibeam bathymetry and multichannel seismic data collected over the northern Ninetyeast Ridge to investigate detailed fault geometry,structure,and activity.We recognized 12 large linear active faults by integrating bathymetry maps and multichannel seismic reflection profiles.Our results showed that these faults have high angles,and they all displaced the basement and propagated to the seafloor with distinct fault scarps.They trended NWW-SEE with a spacing of 10–40km and were parallel to each other and the nearby subfault of the 2012 great intraplate earthquake,suggesting similar stress fields.These faults are also in agreement with the orientations of magnetic isochrons,implying their formation by seafloor spreading.Furthermore,regarding the strike-slip focal mechanism of 2012 earthquakes,we proposed that these faults were created early by a normal spreading process and then evolved into a strike-slip pattern since the ancient oceanic crust ap-proached the subduction zones. | CHEN Jie GUO Laiyin YANG Xiaodong ZHANG Jinchang ZHANG Zhiwen SUN Mengyu LIN Jingxue | 2023 | Journal of Ocean University of China2023，22，6： | 0 |
| 5 | A Vigor Role in Chinese Economy | Lin Jingxue | 2002 | 中国周刊2002，34，7： | 0 |
| 6 | Crustal Structure of the Jurassic Quiet Zone in the West Pacific Ocean:Insights from 2D Multichannel Seismic Reflection Profiles显示文摘The Jurassic oceanic crust is the oldest existing oceanic crust on earth,and although distributed sparsely,carries essential information about the earth's evolution.The area around the Pigafetta Basin in the west Pacific Ocean(also known as the Jurassic Quiet Zone,JQZ)is one of a few areas where the Jurassic oceanic crust is present.This study takes full advantage of high-resolution multichannel seismic reflection profiles in combination with bathymetry,magnetic,and gravity data from the JQZ to examine the structure,deformation,and morphology of the Jurassic oceanic crust.Our results show the following insights:1)The Moho lies at 2–3 s in two-way travel time beneath the seafloor with the segmented feature.The gaps between the Moho segments well correspond to the seamounts on the seafloor,suggesting the upward migration of magma from the mantle has interrupted the pre-existing Moho.2)The oceanic crust is predominantly deformed by crustal-scale thrust faults,normal faults cutting through the top of basement,and vertical seismic disturbance zones in association with migration of thermal fluids.The thrust faults are locally found and interpreted as the results of tectonic inversion.3)Seafloor morphology in the JQZ is characterized by fault scarps,fold scarps,seamounts,and small hills,indicating the occurrence of active faults.4)The oceanic crust in the JQZ and East Pacific Rise has many structural and geometrical variations,such as the thickness of sediments,seafloor topography,basement morphology,fault size and type. | YANG Xiaodong LIN Jingxue ZHANG Jinchang LUO Yiming ZHANG Xubo QIN Zhen HUANG Yanming | 2023 | Journal of Ocean University of China2023，22，5： | 0 |
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