We know that is aqueous solution the following equilibrium operates......
H_2O(l) rightleftharpoonsH^(+) + HO^-
H^+ and HO^- are the characteristic cation, and characteristic anion of the water solvent. Sometimes, we write H^+ as H_3O^+, i.e. the "hydronium ion". As far as anyone knows this is a cluster of 3-4 (or more) water molecules, with an extra PROTON, H^+ to give H_7O_3^+, or H_9O_4^+, we use H^+ and H_3O^+ as convenient shorthands.
As with any equilibrium we can quantify it......
K=([H^+][HO^-])/[[H_2O(l)]]
Because [H_2O] is so large, it can be removed from the equation, and we get
K_w=[H^+][HO^-]=[H_3O^+][HO^-]=10^(-14) at 298*K. Now back in the day before the advent of electronic calculators, scientists used log tables to the "base e" or "base 10" to simplify products and quotients of very large and very small numbers.
We DEFINE pH=-log_10[H_3O^+], and pOH=-log_10[HO^-], and thus if we take log_10 of
K_w=[H^+][HO^-]=[H_3O^+][HO^-]=10^(-14).....
..............we gets.................
log_10K_w=log_10[H_3O^+]+log_10[HO^-]=log_10(10^-14)
And on rearrangement,
-14=log_10[H_3O^+]+log_10[HO^-], and multiplying thru by -1..
14=underbrace(-log_10[H_3O^+])_(pH)underbrace(-log_10[HO^-])_(pOH)
And finally our defining relationship......pH+pOH=14. Wheww!
And so we can at last address your question. I will do the first row in the table. I suggest that you have a go at the rest yourself.
"Solution A", [H^+]=3.7xx10^-8*mol*L^-1; pH=-log_10(3.7xx10^-8)=7.43; pOH=14-7.43=6.57. And [HO^-]=10^(-6.57)=2.70xx10^-7*mol*L^-1.
Over to you for B and C and D hoss............
One final caveat: I stress that H^+ is equivalent to H_3O^+; which expression you use is a matter of personal preference, but be consistent.