controlling mechanism

控制机制
  • 文章类型: Journal Article
    DNA纳米技术的兴起推动了DNA分子机器的发展,能够在纳米尺度上执行特定的操作和任务。得益于DNA分子的可编程性以及DNA杂交和链置换的可预测性,基于DNA的分子机器可以设计为具有各种结构和动态行为,并且由于其独特的优势而在生物传感领域得到了广泛的应用。这篇综述总结了已报道的基于DNA的分子机器的控制机制,并介绍了基于DNA的分子机器在扩增检测中的生物传感应用。多重检测,实时监控,空间识别检测,和生物标志物的单分子检测。还讨论了基于DNA的分子机器在生物传感中的挑战和未来方向。
    The rise of DNA nanotechnology has driven the development of DNA-based molecular machines, which are capable of performing specific operations and tasks at the nanoscale. Benefitting from the programmability of DNA molecules and the predictability of DNA hybridization and strand displacement, DNA-based molecular machines can be designed with various structures and dynamic behaviors and have been implemented for wide applications in the field of biosensing due to their unique advantages. This review summarizes the reported controlling mechanisms of DNA-based molecular machines and introduces biosensing applications of DNA-based molecular machines in amplified detection, multiplex detection, real-time monitoring, spatial recognition detection, and single-molecule detection of biomarkers. The challenges and future directions of DNA-based molecular machines in biosensing are also discussed.
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  • 文章类型: Journal Article
    大型河口连续体中重金属的复杂转化限制了我们对其污染历史的理解。这项研究调查了重金属的沉积组成,主要元素,总有机碳,晶粒尺寸,和放射性核素研究长江口(YRE)四个沉积物岩心(E1-E4)中重金属积累模式的时空变化及其控制机制。结果表明,由于在稳定的沉积环境中连续沉积,只有YRE远端前表面的E3很好地反映了重金属污染历史,E1和E2明显记录了河流和河口项目和过程的影响。YRE近端前缘的E1通过沉积物疏浚和倾倒活动记录了强烈的人为干扰,产生了一层异常低的210Pbex和少量重金属浓度的厚层。YRE中间前缘的E2显示,随着重金属浓度的降低,其上游粗化趋势对沉积物排放减少的影响最近增加。洪水和风暴事件在E2和E3的核心沉积物中留下了不同的印记,它们的粗地层单位具有较少的重金属浓度。来源分析表明,河口沉积物中的重金属主要来自自然过程,但受人类活动的影响很大。通过对潮汐河到河口的核心数据的比较研究,发现了近几十年来重金属积累历史与社会经济发展的直接联系,尽管有显著的时空差异,这是由晶粒尺寸共同决定的,离岸距离,水动力条件,沉积状态,除河口过程外,还有沉积速率。这警告我们要从大型河口系统中单个或稀疏的核心数据中仔细解释重金属历史,该系统具有类似于YRE的强烈自然力和人为干扰。
    Complex transformations of heavy metals in the mega-river-estuary continuum limit our understanding of their pollution history. This study investigated sedimentary compositions of heavy metals, major elements, total organic carbon, grain size, and radionuclides to study spatiotemporal variations in heavy metal accumulation patterns and their controlling mechanisms in four sediment cores (E1-E4) from the Yangtze River Estuary (YRE). Results show that only E3 in the distal YRE front mirrors well the heavy metal pollution history due to its continuous deposition in a stable sedimentary environment, while E1 and E2 record the influence of riverine and estuarine projects and processes apparently. E1 in the proximal YRE front registers intense human disturbance through sediment dredging and dumping activities to produce a thick layer of abnormal low 210Pbex and minor heavy metal concentrations. E2 in the intermediate YRE front demonstrates the recently increasing influence of reduced sediment discharge by its upcore coarsening trend with decreased heavy metal concentrations. Flood and storm events left different imprints in core sediments of E2 and E3 by their coarse stratal units with fewer heavy metal concentrations. The source analysis indicates that heavy metals in estuarine sediments mainly come from natural processes but are significantly affected by human activities. A direct linkage of the heavy metal accumulation history with the socioeconomic development in recent decades is found by a comparison study of core data from the tidal river to the estuary, albeit with a remarkable spatiotemporal difference, which is jointly determined by grain size, offshore distance, hydrodynamic condition, depositional status, and sedimentation rate besides estuarine processes. This warns us to carefully interpret the heavy metal history from single or sparse core data in a mega estuary system with intense natural forces and human disturbances analogous to the YRE.
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  • 文章类型: Journal Article
    The Gan River is a large tributary of the Yangtze River in Jiangxi Province, South-central China. Hydrochemical data for this river were analyzed for the period 1958-2016. Ca2+, Na+ + K+, HCO3-, and SO42- were dominant in river water, and pH and total dissolved solids (TDS) varied from 6.0 to 8.8 and 15.7 to 141 mg/L, respectively. The chemical composition of river water was different between the two periods 1958-1979 and 1980-2016. Monthly yields of all ions were positively correlated with river runoff. Monthly yields of SO42-, NO3-, and Cl- were more positively correlated with river runoff before 1980, indicating non-point sources, while multiple sources were indicated after 1980. Sea salt-sourced Cl- comprised less than 19% of the total Cl- in river water. Weathering of basin rocks with sulfuric acid reflected strengthening of anthropogenic activities after 1980. This was reflected by increases in Cl-/(Na+ + Cl-) and SO42-/(Na+ + Cl-) with gross domestic production, population, coal consumption, fertilizer use, and wastewater discharge. Although water quality in the Gan River makes the water acceptable for drinking according to the World Health Organization standards, increases in Cl- and NO3- concentrations after 1980 are of some concern.
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