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A bistable [2]pseudorotaxane 1⊂CBPQT·4PF 6 and a bistable [2]rotaxane 2·4PF 6 have been synthesised to measure the height of an electrostatic barrier produced by double molecular oxidation (0 to +2). Both systems have monopyrrolotetrathiafulvalene (MPTTF) and oxyphenylene (OP) as stations for cyclobis(paraquat- p -phenylene) (CBPQT 4+ ). They have a large stopper at one end while the second stopper in 2 4+ is composed of a thioethyl (SEt) group and a thiodiethyleneglycol (TDEG) substituent, whereas in 1⊂CBPQT 4+ , the SEt group has been replaced with a less bulky thiomethyl (SMe) group. This seemingly small difference in the substituents on the MPTTF unit leads to profound changes when comparing the physical properties of the two systems allowing for the first measurement of the deslipping of the CBPQT 4+ ring over an MPTTF 2+ unit in the [2]pseudorotaxane. Cyclic voltammetry and 1 H NMR spectroscopy were used to investigate the switching mechanism for 1⊂CBPQT·MPTTF 4+ and 2·MPTTF 4+ , and it was found that CBPQT 4+ moves first to the OP station producing 1⊂CBPQT·OP 6+ and 2·OP 6+ , respectively, upon oxidation of the MPTTF unit. The kinetics of the complexation/decomplexation process occurring in 1⊂CBPQT·MPTTF 4+ and in 1⊂CBPQT·OP 6+ were studied, allowing the free energy of the transition state when CBPQT 4+ moves across a neutral MPTTF unit (17.0 kcal mol −1 ) or a di-oxidised MPTTF 2+ unit (24.0 kcal mol −1 ) to be determined. These results demonstrate that oxidation of the MPTTF unit to MPTTF 2+ increases the energy barrier that the CBPQT 4+ ring must overcome for decomplexation to occur by 7.0 kcal mol −1 . 

Abstract Reduced stomatal conductance is a common plant response to rising atmospheric CO₂and increases water use efficiency (W). At the leaf-scale,Wdepends on water and nitrogen availability in addition to atmospheric CO₂. In hydroclimate modelsWis a key driver of rainfall, droughts, and streamflow extremes. We used global climate data to derive Aridity Indices (AI) for forests over the period 1965–2015 and synthesised those with data for nitrogen deposition andWderived from stable isotopes in tree rings. AI and atmospheric CO₂account for most of the variance inWof trees across the globe, while cumulative nitrogen deposition has a significant effect only in regions without strong legacies of atmospheric pollution. The relation of aridity andWdisplays a clear discontinuity.Wand AI are strongly related below a threshold value of AI ≈ 1 but are not related where AI > 1. Tree ring data emphasise that effective demarcation of water-limited from non-water-limited behaviour of stomata is critical to improving hydrological models that operate at regional to global scales.