# Freezing trend of water

In this experiment, I used a digital temperature probe to measure the freezing point of water and some other salt solutions.

I was just wondering if there was any explanations for 1. The first plateau and 2. The dip in temperature right before the freezing point. (2.) can be observed for other salt solutions.

I think that the dip before the freezing point is caused by the formation of ice needing a 'nucleation point', which requires the temperature to be much lower such that a regular structure can be formed. I have no good explanation for 1. but it could be due to uneven cooling or some sort of issue with the probe.

Please give some suggestions that explains 1. and 2. if possible, even if you are unsure. Thank you for the help!

• What is your experimental set-up? You are freezing water and other salt solutions, please add some details. Are you stirring the system? Salt solutions should not freeze at zero degrees. I feel this is rather an uneven cooling issue. – M. Farooq Feb 12 at 4:01
• I agree with your nucleation explanation for the dip prior to freezing. – A.K. Feb 12 at 4:05
• What are the two differently colored lines? Agree with M. Farooq: are you stiring? What kind of probes are you using, what previous calibration did you do, how are you cooling the sample? etc – Buck Thorn Feb 12 at 8:55
• @M.Farooq@Try Hard, The coloured lines are just different trials; I am using a plastic container with 100ml of each solution (water, NaCl, FeCl3 etc.) and the temperature probe is here: pasco.com/prodCatalog/PS/PS-3201_wireless-temperature-sensor/…. I am not stirring the solution, but simply setting the container with no lid into the fridge until it freezes. The image is only for distilled water, other salt solutions produces a similar graph with a different freezing point. – Goldsphere Feb 12 at 10:02
• Is the water deionized? (as in, not the sample you added salt to - obviously) – Buck Thorn Feb 12 at 10:25

The plateau observed around $$\pu{2^\circ C}$$ may be due to density differentials across the sample. At about $$\pu{4^\circ C}$$ water reaches its maximum density. Above this temperature, the colder water at the surface sinks, creating convection currents and accelerating the cooling process. As you dip below about $$\pu{4^\circ C}$$ the convective currents cease (around 3000 s), since the density gradient is stable: colder, less dense water is at the top. The water at the top of the sample continues to cool and decrease in density without sinking. If the thermometer is placed away from the air interface, it should at this point measure a slowly changing temperature as the temperature gradient toward the interface builds up. The temperature behavior will be a response to heat diffusion instead of heat convection.