dual response
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2022 ◽  
Vol 276 ◽  
pp. 115556
Author(s):  
Denghui Li ◽  
Lian Liu ◽  
Honggao Yang ◽  
Jie Ma ◽  
Huiling Wang ◽  
...  

Molecules ◽  
2022 ◽  
Vol 27 (2) ◽  
pp. 489
Author(s):  
Xin Guo ◽  
Chang-Xiang Liu ◽  
Yuan Lu ◽  
Ya-Wen Wang ◽  
Yu Peng

A novel two-site chemodosimeter (SWJT-4) based on fluorescein skeleton to detect diethyl chlorophosphate (DCP) was designed and synthesized. It is a turn-on fluorescent probe for DCP with good selectivity and obvious color change in aqueous solution. Interestingly, the two oxime groups of SWJT-4 as dual response sites initiated different reactions with DCP to form a cyano group and an isoxazole ring, respectively. The corresponding mechanism was confirmed by 1H NMR, MS and DFT calculation. Moreover, SWJT-4 could be used as a fluorescent test paper to detect DCP vapor.


Author(s):  
Zhiming Gou ◽  
Aijing Wang ◽  
Minggang Tian ◽  
Yujing Zuo

The formation or destruction of pyrene excimer with strong emission change make it a versatile fluorophore to construct excimer emission-based fluorescence probes for various analytes detection. The distinct difference between...


2021 ◽  
Author(s):  
Niccolò Ragno ◽  
Nicoletta Tambroni ◽  
Michele Bolla Pittaluga

The morphodynamic evolution of river deltas is intimately tied to flow and sediment partitioning at bifurcations. In this work, we investigate the long-term equilibrium configuration of a simple delta network using an analytical model, which accounts for the effect of small tidal oscillations.Differently from individual bifurcations, where tidal action is always a stabilizing factor, in the case of a tree-like delta with multiple bifurcations a dual response emerges.Specifically, depending on the values of four reference parameters function of tidal amplitude, upstream flow conditions, and on the geometry of the channels, tides can either promote or discourage an unbalanced discharge distribution. This behavior primarily concerns the apex bifurcation, which is affected by the variations of the relative tidal amplitude at the internal nodes. In turn these variations depend on how flow and sediment are diverted upstream. Finally, we discuss the outcomes of the model performing a qualitative comparison with field and experimental tide-influenced deltas. Results highlight the need of including in a unified scheme river-influenced (i.e. depositional) and tide-influenced (i.e. erosional) effects.


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