Question

Chlorine- 36 is a convenient radiotracer. It is a weak beta emitter, with \(t_{1 / 2}=3 \times 10^{5}\) yr. Describe how you would use this radiotracer to carry out each of the following experiments. (a) Determine whether trichloroacetic acid, \(\mathrm{CCl}_{3} \mathrm{COOH}\), undergoes any ionization of its chlorines as chloride ion in aqueous solution. (b) Demonstrate that the equilibrium between dissolved \(\mathrm{BaCl}_{2}\) and solid \(\mathrm{BaCl}_{2}\) in a saturated solution is a dynamic process. (c) Determine the effects of soil \(\mathrm{pH}\) on the uptake of chloride ion from the soil by soybeans.

Short answer

(a) To determine whether trichloroacetic acid ionizes its chlorines, synthesize Chlorine-36 labeled trichloroacetic acid and dissolve it in water. Measure the initial radioactivity, separate the chloride ions, and measure their radioactivity. If there is significant radioactivity in the separated chloride ions, it indicates ionization. (b) To demonstrate that the equilibrium between dissolved BaCl2 and solid BaCl2 is dynamic, create a saturated solution with Chlorine-36 labeled BaCl2, measure the initial radioactivity, and re-establish equilibrium. Then, measure the radioactivity again. If it changes, the equilibrium is dynamic. (c) To determine the effects of soil pH on chloride ion uptake, treat soil samples with different pH levels using Chlorine-36 labeled chloride ions, plant soybeans, and grow them. Harvest the soybeans, separate chloride ions, and measure their radioactivity. Comparing radioactivity levels will indicate the effect of soil pH on chloride ion uptake.

Step-by-step solution

Prepare the radiotracer labeled trichloroacetic acid

To perform the experiment, synthesize trichloroacetic acid, CCl3COOH, with one of the chlorines labeled using the Chlorine-36 radiotracer. This can be done by reacting Chlorine-36 with acetic acid and other reagents required for the synthesis.

Dissolve the labeled trichloroacetic acid in water

Dissolve the synthesized radiotracer-labeled trichloroacetic acid in water to create an aqueous solution.

Measure the radioactivity of the solution

Measure the radioactivity of the initial chlorines-containing aqueous solution using a beta counter. Record the initial radioactivity.

Separate chloride ions

Separate the chloride ions from the solution using an appropriate technique, such as precipitation with a silver nitrate solution to form silver chloride (AgCl) or ion exchange chromatography.

Measure the radioactivity of separated chloride ions

Measure the radioactivity of the isolated chloride fraction using a beta counter.

Determine ionization

If the radioactivity of the separated chloride ions is significant compared to the initial radioactivity, it indicates that trichloroacetic acid undergoes ionization of its chlorines as chloride ions in the aqueous solution. #Experiment (b)#

Prepare a saturated solution

Dissolve solid barium chloride, BaCl2 in water until the solution becomes saturated. Add Chlorine-36 labeled barium chloride to the solution.

Remove the solid BaCl2 and measure radioactivity

Separate the solid BaCl2 from the solution using filtration and measure the radioactivity of the dissolved BaCl2 in the solution using a beta counter. Record the initial radioactivity.

Allow the system to reach equilibrium

Allow the solution to re-establish equilibrium with the solid BaCl2. Give sufficient time for the process to occur.

Measure the radioactivity again

Remove the solid BaCl2 from the solution again using filtration and measure the radioactivity of the dissolved BaCl2 in the solution using a beta counter.

Compare radioactivity

If the radioactivity has changed after the equilibrium has been re-established compared to the initial radioactivity, it demonstrates that the equilibrium between dissolved BaCl2 and solid BaCl2 in a saturated solution is a dynamic process. #Experiment (c)#

Prepare soil samples

Collect soil samples with different pH levels and treat them with a solution containing Chlorine-36 labeled chloride ions.

Plant soybeans

Plant soybean seeds in the treated soil samples, and grow them under controlled conditions.

Harvest soybean plants

Harvest the soybean plants after they have grown and developed.

Measure radioactivity in harvested soybeans

Separate the chloride ions from the harvested soybeans and measure their radioactivity using a beta counter.

Analyze the data

Compare the radioactivity levels in the harvested soybeans from different soil pH samples. The differences in radioactivity will indicate the effect of soil pH on the uptake of chloride ions from the soil by soybeans.

Key concepts

Chlorine-36 Usage

Chlorine-36 is a radioactive isotope of chlorine used extensively in environmental and geological studies due to its long half-life of approximately 300,000 years. As a radiotracer, it enables researchers to trace the presence and movement of chloride ions in various systems. For instance, scientists can assess the ionization behavior of organic molecules in water by introducing Chlorine-36 labeled compounds.

In the context of examining the ionization of trichloroacetic acid, Chlorine-36 provides a means to detect and measure the formation of chloride ions in an aqueous solution. By measuring the radioactivity before and after separation of chloride ions, researchers can infer the extent to which ionization has occurred. This methodology is invaluable in understanding the behavior of chemicals in environments ranging from laboratory solutions to natural water systems.

Ionization in Aqueous Solution

Ionization is the process by which a neutral molecule loses or gains an electron, forming charged particles known as ions. In aqueous solutions, the ability of a substance to ionize has significant implications for its reactivity, solubility, and biological activity.

For substances like trichloroacetic acid, assessing ionization can reveal how it dissociates to form chloride ions and hydrogen ions. By using a radiotracer such as Chlorine-36, scientists can directly measure the presence of ionized chlorine and quantitatively evaluate the extent of ionization. This information helps in understanding the chemical's behavior in solution, such as its interaction with other substances, its biological availability, and its environmental impact.

Dynamic Chemical Equilibrium

Chemical equilibrium represents a state in which the rate of the forward reaction equals the rate of the reverse reaction, causing the concentrations of reactants and products to remain constant over time. However, 'dynamic' indicates that reactions are still occurring.

By tagging barium chloride with Chlorine-36, we can observe changes in the system's radioactivity over time to confirm the dynamic nature of equilibrium. If the radioactivity of the dissolved barium chloride changes after some time, it is evidence that the system is indeed dynamic, as solid barium chloride continues to dissolve and precipitate maintaining the equilibrium state. Understanding the dynamic nature of chemical equilibria is crucial for applications ranging from industrial synthesis to environmental monitoring.

Soil pH Effect on Ion Uptake

Soil pH plays a critical role in the availability of nutrients to plants as it influences the solubility and ionization state of nutrients in the soil. Different pH levels can either enhance or inhibit the uptake of ions by plant roots.

Using Chlorine-36 labeled chloride ions allows for precise tracking of the ion movement into plants, enabling researchers to study how variations in soil pH affect the absorption of these ions by soybeans or other crops. Such experiments provide valuable information for agricultural practices, aiding in the optimization of soil conditions for better crop yield and health.