The solubility of a gas in a liquid increases with increasing pressure. to understand the above statement, consider a familiar example: cola. in cola and other soft drinks, carbon dioxide gas remains dissolved in solution as long as the can or bottle remains pressurized. as soon as the lid is opened and pressure is released, the co2 gas is much less soluble and escapes into the air. the relationship between pressure and the solubility of a gas is expressed by henry's law: s=kp, where s is concentration in m, k is the henry's law constant in units of mol/(l⋅atm), and p is the pressure in atm. note: since temperature also affects the solubility of a gas in an liquid, the henry's law constant is specific to a particular gas at a particular temperature. the following table provides some information on carbon dioxide solubility in water. s (mol/l) p (atm) k (mol⋅l−1⋅atm−1) t (∘c) 3.80×10−2 1.00 20.0 6.60×10−2 20.0 1.00 3.50×10−2 25.0 part a what is the henry's law constant for co2 at 20∘c?

What royal scientist used the 29th day of frozen vapor to encounter elements for mastering new culinary creations?

What is the empirical formula of c6h18o3? ch3o c2h5o c2h6o c2h5o5

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.