91Ó°ÊÓ

To find the moles of a substance, you multiply its volume by its molarity. This is especially useful in reactions involving a solution, like with \(\mathrm{AgNO_3}\)in this case. When a problem provides molarity and a specific volume of a solution, you start by converting the volume from milliliters to liters. This step is crucial since molarity is defined in terms of liters:

• Conversion: \(37.20 \, \mathrm{mL} = 0.03720 \, \mathrm{L}\)

Next, use the formula\[ Moles\, of\, \mathrm{AgNO_3} = \mathrm{Volume\, (L) } \times \mathrm{Molarity\, (M)} \ = 0.03720\, \mathrm{L} \times 0.1000\, \mathrm{M} = 3.72 \times 10^{-3} \mathrm{moles}\]You've now got the moles of \(\mathrm{AgNO_3}\). Understanding this means having insight into the amount of substance present, which is vital for further calculations.

When \(\mathrm{AgNO_3}\) is mixed with chloride ions in a solution, a chemical reaction occurs, forming insoluble silver chloride (AgCl) as a precipitate. This means that all available chloride ions will react with \(\mathrm{AgNO_3}\) until one of the reactants is used up. The stoichiometry of the reaction follows a 1:1 ratio:

• Each mole of \(\mathrm{Cl^-}\) requires one mole of \(\mathrm{AgNO_3}\) to completely precipitate as \(\mathrm{AgCl}\).

Thus, the number of moles of chloride ions will be equal to the moles of \(\mathrm{AgNO_3}\) used, which we've already calculated to be\[3.72 \times 10^{-3} \mathrm{\, moles}\]This allows us to conclude the presence of \(\mathrm{Cl^-}\) ions in the original sample. This step is critical because it links the silver solution used to the chloride ions in the sample.

To proceed with the mass calculations, the molar mass of the compound, such as douglasite, becomes essential. Douglasite has the formula \(2\ \mathrm{KCl} \cdot \mathrm{FeCl}_2 \cdot 2\ H_2O\). Summing up the atomic masses gives the molar mass. Let's break it down:

• For \(\mathrm{KCl}:\)
  • Potassium (K): \(39.10 \, \mathrm{g/mol}\)
  • Chlorine (Cl): \(35.45 \, \mathrm{g/mol}\)
  \(2 \times (39.10 + 35.45)\)
• For \(\mathrm{FeCl}_2:\)
  • Iron (Fe): \(55.85 \, \mathrm{g/mol}\)
  • Chlorine: \(2 \times 35.45 \, \mathrm{g/mol}\)
• Water, \(\mathrm{H_2O}:\) \(2 \times (2 \times 1.01 + 16.00)\)

When added together, the molar mass of douglasite approximates to \[\mathrm{413.7 \, g/mol}\]This large number signifies the weight of one mole of douglasite, which is vital when calculating the mass of douglasite from its molar quantity.

Chloride ions are an essential component in many mineral forms. In this problem, douglasite is our source of \(\mathrm{Cl^-}\) ions. When you analyze a sample for its chloride content, underlying reactions involve its conversion into something measurable, such as \(\mathrm{AgCl}\) precipitate.In minerals like douglasite, the formula indicates the chloride content. Two moles of \(\mathrm{KCl}\) and one of \(\mathrm{FeCl_2}\) suggest three chloride ions per douglasite molecule. This formula tells us there is a fixed proportion of chloride within every mole of the mineral.This knowledge allows chemists to compute the potential release of chloride ions when the mineral is dissolved or altered chemically. Comprehending the amount of chloride ions helps in determining the mineral's composition and its potential usage in various chemical reactions.