Sort the following into the classification for a reaction that is NOT at equilibrium versus a reaction system that has reached equilibrium. Drag the appropriate items to their respective bins.
The rate at which products form from reactants is equal to the rate at which reactants form from products.
The concentrations of reactants and products are stable and cease to change.
The concentration of products is increasing, and the concentration of reactants is decreasing.
The ratio of products to reactants is not stable.
The ratio of products to reactants does not change.
Chemical equilibrium is a dynamic state.
The rate of the forward reaction is greater than the rate of the reverse reaction.
The state of chemical equilibrium will remain the same unless reactants or products escape or are introduced into the system. This will disturb the equilibrium.
The forward and reverse reactions proceed at the same rate.
The products are gaseous and escape the vessel into the atmosphere.
The reaction has reached equilibrium.
The reaction has not reached equilibrium.

What is the relationship between wind and ocean waves? question 17 options: wind moving at higher speeds will transfer more energy to the water, resulting in stronger waves. wind moving at higher speeds will transfer energy over a larger part of the ocean water, resulting in waves with a shorter wavelength. winds moving at higher speeds with cause water to move forward at faster rates, causing larger ocean waves. winds moving at higher speeds will affect deeper water, resulting in waves that move at a faster rate. how do temperature and salinity affect deepwater currents? question 15 options: as temperatures and salinity levels of water increase, the water rises to the surface where it creates currents as it moves to colder regions. they create changes in wind direction, moving denser water in the same direction as the wind and causing the deepwater circulation patterns found in the ocean. they equalize the forces on undersea currents caused by the coriolis effect as they replace more dense water with less dense water. they create density differences that cause dense deepwater currents to flow toward the equator where they displace less dense, warmer water above them.