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您的检索式：作者名="Zhao Daxian"
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| 1 | Versatile zero- to three-dimensional carbon for electrochemical energy storage显示文摘Secondary batteries have been widely developed and used in various fields,such as large-scale energy storage,portable electronics,and electric vehicles.Carbon-based materials have attracted considerable attention due to their abundance,environmental friendliness,tunable structure,and excellent chemical stability.Beyond the commercial carbon for batteries and supercapacitors,many studies focused on advanced and multifunctional carbon with various structures for electrochemical energy storage.This review summarizes the zero-to three-dimensional carbon-based materials and reviews their various electrochemical applications based on their structural characteristics.The importance of carbon structures and the relationship between materials'structures and electrochemical performance are discussed.Then,the prospects and potential challenges of using advanced carbon to formulate designs and develop novel carbonaceous materials with high electrochemical performance are further discussed. | Yuyue Zhao Yunlu Zhang Ying Wang Daxian Cao Xiao Sun Hongli Zhu | 2021 | Carbon Energy2021，3，6： | 3 |
| 2 | A delta-class glutathione transferase from the Chinese mitten crab Eriocheir sinensis : cDNA cloning, characterization and mRNA expression显示文摘 | Daxian Zhao Liqiao Chen Chuanjie Qin Hao Zhang Ping Wu Fengying Zhang | 2010 | Fish and Shellfish Immunology2010，，4： | 1 |
| 3 | The Geochemical Characteristics and Minerogenic Model for the Amo Hypothermal Tin Deposit in Ximeng County, Yunnan Province显示文摘Through studies on the element geochemistry, alteration of country rocks, ore-forming fluids and isotopegeochemistry of the Arno tin deposit in the metamorphic rocks of the Upper Proterozoic Ximeng Group, theauthors consider that the concentration of the B-F-Li-Rb-Cs-Sn association is related to acidic magmatism inthe study area. The Fe-Mg-Li tourmaline in the ore is the replaced product of the country rocks byhypothermal fluid. The δ18O values of mineral separates are +2.01- +13.16‰ and their δ34S values, +2.6-+7.2‰. The ore-forming materials were derived from hydrothermal fluid of granitic magma. For themineralization, the temperature is 450°-350℃, the pressure, 450-1000×105 Pa, and the age, Himalayan(21.5 Ma). According to the geochemical characteristics, a minerogenic model is established: the deposit is ahypothermal cassiterite-quartz vein type tin deposit controlled by the hidden Himalayan granites. | Zhao Daxian Tang Guangting The Fifth Geological Party, Yunnan Bureau of Geology and Mineral Resources, Simao,Yunnan Liu Linqun | 1991 | Acta Geologica Sinica(English Edition)1991，65，3： | 0 |
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