Thus, hydrologic variability (e.g., inputs, water levels, depths), sediment-water interchange, and wind have greater effects than they do in deep, permanent, freshwater lakes.
These results suggest that water molecules move in single file in the AqpM channel with occasional water-water interchange events.
Water-water interchanges do not affect p f because the latter is related to the displacement of individual water molecules inside the channel and is not influenced by the occurrence of water-water interchanges.
Values of indicates that the single-fileness of the water molecules inside the channel is interrupted by occasional water-water interchanges that increase p d, i.e., more water molecules traverse the channel per unit time [ 28, 37, 38].
The observation that the higher transport rate appears to be in an opposite trend with respect to experimental results can be explained by the wider pore of GlpF that could allow more water-water interchanges and thus more permeation events per unit time, increasing the value of p d (see below).
Our results shows that, in terms of the p f / p d ratio, AqpM presents a similar level of single-fileness with respect to strict aquaporins (see table 2) but with an average value of suggesting that AqpM allows more water-water interchanges than strict aquaporins.
Neighbouring waters with the interchange of warm and cold currents offer good fishing ground for cuttlefish, which is exported, and various other marine products.
and bus interchanges), water treatment (sewage, dams, pipelines, etc).
Civil engineers focus on structures and facilities such as transportation routes, features (tunnels, bridges, flyovers), and hubs (such as airports and bus interchanges), water treatment (sewage, dams, pipelines, etc).
This concept of a global ocean as a continuous body of water with relatively free interchange among its parts is of fundamental importance to oceanography.
