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4篇 您的检索式:作者名="Xinlu Sun"
    题名 作者 年代 出处 被引量
1Automatic Navigation for Rat-Robots with Modeling of the Human Guidance显示文摘Chao Sun Nenggan Zheng Xinlu Zhang Weidong Chen Xiaoxiang Zheng 2013Journal of Bionic Engineering2013,10,1:5
2Identification of Styryl Sulfonyl Fluoride as a Near-Perfect Michael Acceptor for Diversified Protein Bioconjugations显示文摘Cysteine(Cys)-specific bioconjugation has widespread applications in the synthesis of protein conjugates,particularly for the functionalization of antibodies.Here,we report the discovery of transstyryl sulfonyl fluoride(SSF)as a near-perfect Michael acceptor for Cys-specific protein bioconjugation.Compared to maleimides,which are predominantly used,SSF exhibited better chemoselectivity,selfstability,and conjugate stability while maintaining comparable reactivity.Using SSF-derived probes,proteins can be readily modified on the Cys residue(s)to install functionalities,for example,fluorescent dyes,toxins,and oligonucleotides,without influencing the activity.Further applications of SSF-derived serum-stable antibody-drug conjugates and PD-L1 nanobody-oligo conjugates demonstrate the great translational value of SSF-based bioconjugation in drug development and single-cell sequencing.Qingsong Wu Qi Xue Ji Li Qinheng Zheng Xinlu Zhao Wannan Li Shiming Sun Wanxing Sha Yang Yang Yi Yang Jie P.Li 2023CCS Chemistry2023,5,10:0
3The global mismatch between equitable carbon dioxide removal liability and capacity显示文摘Limiting climate change to 1.5℃and achieving net-zero emissions would entail substantial carbon dioxide removal(CDR)from the atmosphere by the mid-century,but how much CDR is needed at country level over time is unclear.The purpose of this paper is to provide a detailed description of when and how much CDR is required at country level in order to achieve 1.5℃and how much CDR countries can carry out domestically.We allocate global CDR pathways among 170 countries according to 6 equity principles and assess these allocations with respect to countries'biophysical and geophysical capacity to deploy CDR.Allocating global CDR to countries based on these principles suggests that CDR will,on average,represent~4%of nations'total emissions in 2030,rising to~17%in 2040.Moreover,equitable allocations of CDR,in many cases,exceed implied land and carbon storage capacities.We estimate~15%of countries(25)would have insufficient land to contribute an equitable share of global CDR,and~40%of countries(71)would have insufficient geological storage capacity.Unless more diverse CDR technologies are developed,the mismatch between CDR liabilities and land-based CDR capacities will lead to global demand for six GtCO_(2)carbon credits from 2020 to 2050.This demonstrates an imperative demand for international carbon trading of CDR.Pu Yang Zhifu Mi Yi-Ming Wei Steef V.Hanssen Lan-Cui Liu D’Maris Coffman Xinlu Sun Hua Liao Yun-Fei Yao Jia-Ning Kang Peng-Tao Wang Steven J.Davis 2023National Science Review2023,10,12:0
4Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge,Bohai Bay Basin,East China显示文摘The structural style, fault activity, strike-slip displacement, and the formation mechanism and hydrocarbon migration and accumulation in the center tectonic zone in the northeast Shaleitian Bulge of Zhangjiakou-Penglai Fault Zone were studied by seismic attribute analysis, structural geometric analysis, fault activity analysis, structure evolution history and simulation of hydrocarbon migration, based on 3-D seismic and drilling data. The main results are as follows:(1) The study area is a superimposed tectonic zone, which experienced early(Paleocene and Eocene) extension and late(Oligocene and Pliocene-Quaternary) strike-slip and pull-apart.(2) The sinistral strike slip of the northeast Shaleitian Bulge of Zhangjiakou-Penglai Fault Zone went through two periods, Oligocene and Pliocene-Quaternary, and the Bohai section was active earlier than the inland section.(3) The sinistral strike slip displacement of Zhangjiakou-Penglai Fault is 4 km since Cenozoic, including 1 km in the Oligocene, and 3 km in the Pliocene-Quaternary.(4) The strike-slip movements have resulted in the increase of fault activity and basin-mountain restructure in the fault zone, also contributed to the formation of the central tectonic belt and the conjugate evolution in north-east structural belt.(5) The conjugate strike slip of the Zhangjiakou-Penglai Fault Zone dominated the migration and accumulation of hydrocarbon in shallow formations by controlling the injection points and segments of hydrocarbon from the deep layers to shallow layers.PENG Jingsong WEI Ajuan SUN Zhe CHEN Xinlu ZHAO Dijiang 2018Petroleum Exploration and Development2018,45,2:0
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