The phrase "a molal" is correct and usable in written English.
It is typically used in chemistry to refer to a concentration unit that expresses the number of moles of solute per kilogram of solvent.
Example: "To prepare a 1 molal solution, dissolve one mole of the solute in one kilogram of the solvent."
Alternatives: "one molal" or "molality of one".
The hydration shells of ions at interfaces differ from those in the bulk solutions as demonstrated by a simulation of a 2.2 molal Lil solution between Lennard-Jones walls.
This work presents DES (dual end-member sets -code, a code that takesets -codetional molal scode descripthat of solutakescomposition and implements the DH-ASF model for that solution.
In the present study molecular dynamics simulations of the structure of a 2.2 molal aqueous NaCl solution in the vicinity of an idealized metal surface are reported.
This paper reports molecular dynamics simulations of the magnetite (001 -water interface, both in pure water and in the presence of a 2.3 molal solution of NaClO4.
A 10 molal sodium hydroxide solution was used to activate fly ash at solution: ash ratios of 2 1 and 4 1, and at a solution: (soil + ash) ratio of 0.40.
The solubility of O2 at 3000 m elevation, 40°C, in a 1 molal ionic strength solution is approximately 140 μM.[66] This means that over the course of fluid flow from recharge to discharge at the 5-way, every liter of water must be completely re-oxygenated about 7500 times.
The standard state convention adopted for aqueous species other than H2O corresponds to unit activity of a hypothetical one molal solution referenced to infinite dilution at any temperature and pressure [30, 47].
For aqueous species other than H2O, the standard state was unit activity of the species in a hypothetical 1 molal solution referenced to infinite dilution at any temperature and pressure.
The standard state for minerals and pure water is unit activity, and for all aqueous species other than dissolved CO2 is unit activity in a hypothetical 1 molal solution referenced to infinite dilution at any pressure and temperature.
Shown are calculated values of the net charge per residue (a) and standard molal Gibbs energy of formation from the elements (b) at 25°C and 1 bar for surface-layer proteins from archaeal species listed in Table 1.
