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Shuifan Zhou,Zhenqing Hou,Yang Li,Fei Cui,Mengmeng Jia,Xiangrui Yang,Yange Wang,Liya Xie,Qiqing Zhang 한국고분자학회 2014 Macromolecular Research Vol.22 No.1
The efficacy of magnetic nanoparticles (MNPs) for biomedical applications depends on the specic targetingcapacity, blood circulation time and magnetic susceptibility. Functionalized chitosan-coated Fe3O4 nanoparticles(CS-coated Fe3O4 NPs) were synthesized by a non-solvent-aided coacervation procedure followed by a chemicalcrosslinking procedure. The surfaces of CS-coated Fe3O4 NPs were successfully functionalized with folate-poly(ethyleneglycol)-COOH (FA-PEG) to obtain novel FA-PEG-CS-coated Fe3O4 NPs endowed with long blood circulationand specic targeting capacity. The as-synthesized NPs were characterized by dynamic light scattering, transmissionelectron microscope, X-ray diffraction, thermal gravimetric analysis, vibration sample magnetometer, Fourier transforminfrared spectroscopy, and confocal laser scanning microscopy. As a result, the novel FA-PEG-CS-coated Fe3O4 NPsshowed excellent biocompatibility, magnetic properties, good dispersibility, and proper hydrodynamic sizes in an aqueousmedium. The specific targeting capacity of the as-synthesized NPs to cancer cells was also investigated. It wasobserved that the uptake of the FA-PEG-CS-coated Fe3O4 NPs by HeLa cells was significantly enhanced comparedto the CS-coated Fe3O4 NPs and mPEG-CS-coated Fe3O4 NPs. These results clearly indicate that our novel FA-PEGCS-coated Fe3O4 NPs with remarkable specific targeting capacity, long blood circulation, and superparamagnetismhold great promise for biomedical applications, including targeted drug delivery and hyperthermia therapy.
magnetostratigraphy, 26Al-10Be, Yx02 borehole, tectonic evolution, Daxing Uplift, Beijing Sub-plain
Fubing He,Xiwei Xu,Fang Tian,Zhenhua Liu,Yueze Zhang,Lingyan Bai,Yubin Cui,Kai Wang,Wenzhi Niu,Jingbo Ni,Xiaoyong Liu,Mengmeng Cao 한국지질과학협의회 2024 Geosciences Journal Vol.28 No.2
The buried Daxing Uplift connects the Beijing Sag and Dachang Sag, which is the critical tectonic unit for understanding the structural evolution of the Beijing Sub-plain and its linkages to regional tectonics. This study combines paleomagnetic, 26Al-10Be isochron dates and sedimentary analyses from a new borehole (Yx02) in the northeastern Beijing Sub-plain to shed fresh light on regional tectonic processes and the sedimentary history since the Pliocene. The main findings are as follows: (1) the Daxing Uplift had formed three depositional episodes: alluvial-fan, lacustrine-delta, and alluvial-fan sedimentation since the Cenozoic; (2) The borehole records the Brunhes, Gauss normal chron, and the Matuyama, Gilbert reversed chron in the Daxing Uplift, the corresponding depths are 0–148.9 m, 148.9–315.0 m, 315.0–520.5 m and 520.5–650 m; (3) An important tectonic event started in ~4.3 Ma, disintegrated NE-trending basin and range terrain, reactivated the NW-trending Nankou-Sunhe fault, and formed Shunyi fault in Beijing Sub-plain. Sedimentation occurs exclusively in the Beijing Sag and the northeastern Daxing Uplift during ~4.3–1.77 Ma; (4) During ~1.77–1.07 Ma, a transition from an extension to a strike-slip occurred, and is described not only in a progressively higher increase of the overall deposition rate, but also in a decrease of the relative deposition disparity between sags and uplifts. Since then, the Beijing Sub-plain has been shaped, associated with an overall subsidence depression in the Bohai Bay Basin. This work enhances our understanding of the formation and evolution of the Beijing Sub-plain, the division of tectonic episodes, and the initiation time of the latest tectonic movement in the break-up region, North China Craton, since the Neogene.