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The salt transport pattern is of great significance in the regional environmental management for salt intrusion prevention.
As the initial water contents increases, the bulb-type transport pattern is shifted to a trapezoidal shape.
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Along the main fluvial channel, the transport pattern was directed to the northeast (point 5) (Fig. 7) and the degree of concentration (MRL) was relatively high (Fig. 7).
Methanol and sodium chloride transport patterns are similar in neutral hydrogels, while substantial differences are observed in ion exchange polymers.
Water vapor transport patterns were also examined to determine the possible mechanisms causing the impacts of ENSO regimes on seasonal precipitation changes.
As discussed above, sediment-transport patterns were measured during a summer season (May to July 2011), via tracer experiments and geomorphological observation.
Therefore, the sediment-transport patterns were examined in both normal (calm) conditions and in an episodic depositional event.
Instead, sediment-transport patterns were estimated on the basis of the observation of the geomorphological development derived from a fluvial flooding event of 17 19 July (Fig. 3).
In contrast, sediment-transport patterns are better reconstructed via the P-GSTA method, especially around the river mouth and braided channels (Fig. 12).
The sediment-transport patterns were also estimated on the basis of the observation of geomorphological development (Figs. 4 and 5) during the period from 16 May to 31 July 2011.
In transport terminology, the cooperative pattern is also referred to as "SO: System Optimal (or System Equilibrium)" versus the non-cooperative, referred to as "UE," which are both the result of solving traffic assignment problems (TAP) [17, 18].
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