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The inertia terms of the track elastic displacements are derived using the TCS arc length to couple the system dynamics.
The MS has been designed with an atmospheric interface in order to couple the system to a commercially available differential mobility spectrometer.
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In order to couple the systems, we soon realized that the key variable to track is surface soil moisture.
By feeding this into the reference of the INA121, the unwanted DC offsets in the measured electrode signals were essentially zeroed out AC coupling the system.
As with the temperature coupling, the system can also be coupled to a pressure bath.
By coupling the system to bosonic thermal baths, we studied the interplay between disorder and thermalization.
All simulations were run for 15 ns at room temperature (300 K) coupling the system to an external bath.
The temperature of the system was maintained by coupling the system to a heat bath at 300 K using the Berendsen method [54].
The simulations were performed at neutral pH with runs of 10 ns at room temperature (300 K) coupling the system to an external bath.
At 500.5 ns the simulations continued at 1 bar pressure by coupling the system to external heat and pressure bath.
Due to the global coupling of the system, the invariant subspaces are all nontrivial cluster states.
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