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Both barium (Ba) and radium (Ra) are members of Group \(2 \mathrm{~A}\) and are expected to exhibit similar chemical properties. However, Ra is not found in barium ores. Instead, it is found in uranium ores. Explain.

Short Answer

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Radium's radioactivity links it to uranium decay series, explaining its presence in uranium ores, unlike stable barium.

Step by step solution

01

Introduction to Group 2A

Barium (Ba) and radium (Ra) are members of Group 2A of the periodic table, also known as the alkaline earth metals. Members of this group typically exhibit similar chemical properties due to having two valence electrons. However, their physical properties and occurrence in nature can vary due to differences in size, reactivity, and radioactivity.
02

Radioactivity of Radium

Radium is a radioactive element, while barium is not. The intense radioactivity of radium affects its occurrence in nature. Radium is often associated with the decay series of uranium and thorium because it is a byproduct of these radioactive decay processes. As uranium decays, radium is one of the intermediate products, which is why radium is often found in uranium ores.
03

The Formation of Ores

Ores form based on the chemical and physical properties of elements, including their stability and ability to form compounds. Radium's radioactive nature, coupled with its presence in the decay chain of uranium, results in its accumulation in uranium ores. Barium, on the other hand, is a stable element that often forms compounds with sulfate or carbonate, leading to its occurrence in different types of rocks and ores.
04

Conclusion on Ore Association

Due to the difference in radioactive properties and natural formation processes, radium is primarily found in uranium ores as a decay product, while barium is found in its typical mineral forms, such as barite (barium sulfate), which usually doesn't contain radium. This separation in their occurrences highlights the significant impact of radioactivity and decay series on the distribution of radium in nature.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Radioactivity
Radioactivity is a fascinating phenomenon where certain elements emit energy in the form of particles or electromagnetic waves. It occurs because the nuclei of radioactive atoms are unstable, and they release energy to reach a more stable configuration. This process is significant in understanding why certain elements, like radium, are found in specific locations, such as uranium ores. Due to radium's radioactivity, it is a part of decay chains, where materials emit radiation until they transform into stable elements. This radioactive nature of radium separates it from barium, which is not radioactive and therefore found in different types of ores.
Barium Ores
Barium ores are an important source of the element barium. Barium is commonly found in mineral forms like barite, which is barium sulfate (\( ext{BaSO}_4 \)). These ores are non-radioactive and widely found in various geological formations. Barium tends to form stable compounds with sulfates or carbonates, which leads to its natural occurrence in these ores. Understanding the chemical behavior of barium helps in identifying its presence in nature, and it explains why barium is not found alongside radioactive elements like radium.
Uranium Ores
Uranium ores are crucial for extracting uranium, a radioactive element used as a fuel in nuclear reactors. These ores, such as uraninite, contain uranium in multiple oxidation states, allowing it to exist in various chemical forms. Uranium goes through radioactive decay, producing daughter elements, including radium. This series of decay stages explains why radium is commonly found within uranium ores. The presence of radium in uranium ores is a direct result of the decay series that uranium undergoes, illustrating the natural relationship between radioactive elements.
Chemical Properties
Chemical properties refer to the behavior of elements and compounds during chemical transformations. For alkaline earth metals like barium and radium, these properties often include reactivity with water and acids, forming hydroxides and salts. Their similar chemical properties arise because they both possess two electrons in their outermost electron shell, leading to comparable reactivity. However, despite these similarities, their different physical properties, such as radioactivity in radium, impact their presence in nature and distinguish their formation of ores.
Periodic Table
The periodic table is a fundamental tool in chemistry, organizing elements in a manner that highlights their properties and relationships. Barium and radium, both in Group 2A, are classified as alkaline earth metals. This group shares chemical similarities due to having two valence electrons. These similarities are why barium and radium are expected to exhibit alike chemical behaviors. However, the periodic table also marks differences, such as radium's radioactivity, showing how the periodic table not only classifies elements but also hints at their unique characteristics.
Decay Series
The decay series is a sequence of radioactive decay processes where unstable isotopes gradually transform into more stable forms. In a decay series, starting from an original radioactive isotope, various intermediate products, such as radium, are formed until a stable element, often lead, is reached. This series explains radium's association with uranium ores, as uranium decays to form radium among other elements. Each step in a decay series involves the release of particles and energy, contributing to the changing stability and properties of the elements involved.

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Most popular questions from this chapter

List the factors that affect the intensity of radiation from a radioactive element.

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Strontium-90 is one of the products of the fission of uranium-235. This strontium isotope is radioactive, with a half-life of 28.1 years. Calculate how long (in years) it will take for \(1.00 \mathrm{~g}\) of the isotope to be reduced to \(0.200 \mathrm{~g}\) by decay.

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Nuclear waste disposal is one of the major concerns of the nuclear industry. In choosing a safe and stable environment to store nuclear wastes, consideration must be given to the heat released during nuclear decay. As an example, consider the \(\beta\) decay of \({ }^{90} \mathrm{Sr}(89.907738 \mathrm{amu})\) : $$ { }_{38}^{90} \mathrm{Sr} \longrightarrow{ }_{39}^{90} \mathrm{Y}+{ }_{-1}^{0} \beta \quad t_{1 / 2}=28.1 \mathrm{yr} $$ The \({ }^{90} \mathrm{Y}(89.907152 \mathrm{amu})\) further decays as follows: \({ }_{39}^{90} \mathrm{Y} \longrightarrow{ }_{40}^{90} \mathrm{Zr}+{ }_{-1}^{0} \beta \quad t_{1 / 2}=64 \mathrm{~h}\) Zirconium- \(90(89.904703 \mathrm{amu})\) is a stable isotope. (a) Use the mass defect to calculate the energy released (in joules) in each of the preceding two decays. (The mass of the electron is \(5.4857 \times 10^{-4}\) amu.) (b) Starting with 1 mole of \({ }^{90} \mathrm{Sr}\), calculate the number of moles of \({ }^{90} \mathrm{Sr}\) that will decay in a year. (c) Calculate the amount of heat released (in kJ) corresponding to the number of moles of \({ }^{90} \mathrm{Sr}\) decayed to \({ }^{90} \mathrm{Zr}\) in part \((\mathrm{b}).\)

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