For the multi‑step reaction A + B ⟶ C + D A+B⟶C+D the rate‑limiting step is unimolecular, with A A as the sole reactant. If [ A ] [A] and [ B ] [B] are both 0.125 M, 0.125 M, then the rate of reaction is 0.0070 M / s. 0.0070 M/s. What is the rate of the reaction if [ A ] [A] is doubled? rate: M / s M/s Starting with the original concentrations, what is the rate of the reaction if [ B ] [B] is halved? rate: M / s M/s Starting with the original concentrations, what is the rate of the reaction if [ A ] [A] and [ B ] [B] are both increased by a factor of 6 ? 6? rate:

How have the greenhouse gasses increased from the year 2000 to 2018

Which statements are true concerning mineral formation? check all that apply. the slower the cooling, the larger the crystals. the faster the cooling, the smaller the crystals. crystals formed from magma are smaller than crystals formed from lava. minerals can only form in solutions when the solution is heated deep underground. when a solution cools, elements and compounds leave the solution and crystallize as minerals. minerals formed from hot water solutions can form narrow channels in the surrounding rock.

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.