Chapter 7: Problem 3
In the uranium-238 decay series, radium-226 is an immediate radioactive parent of radon-222. Consider its position in the periodic table and indicate its usual oxidation state, its probable mobility in water, and factors affecting its solubility in soil/water systems.
Short Answer
Expert verified
Radium has an oxidation state of +2, limited water mobility, and its solubility in soil is influenced by pH and other ions.
Step by step solution
01
Identify Radium's Position and Oxidation State
Radium (Ra) is located in Group 2 of the periodic table known as the alkaline earth metals. The alkaline earth metals typically have an oxidation state of +2. Therefore, radium often forms ionic compounds where it is in the +2 oxidation state.
02
Discuss Radium's Mobility in Water
Radium ions, due to their +2 charge, can dissolve in water as cations. However, their actual mobility is influenced by factors such as the presence of other ions and compounds in water, which could lead to the formation of insoluble salts that decrease its mobility.
03
Examine Factors Affecting Radium's Solubility in Soil/Water
Radium's solubility in soil and water systems is affected by the pH, the presence of other anions like carbonate or sulfate that can form insoluble compounds with radium, and organic matter that may complex with radium. In alkaline conditions, radium is less soluble due to the formation of insoluble radium carbonate.
Unlock Step-by-Step Solutions & Ace Your Exams!
-
Full Textbook Solutions
Get detailed explanations and key concepts
-
Unlimited Al creation
Al flashcards, explanations, exams and more...
-
Ads-free access
To over 500 millions flashcards
-
Money-back guarantee
We refund you if you fail your exam.
Over 30 million students worldwide already upgrade their learning with Vaia!
Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Uranium-238 decay series
The uranium-238 decay series is a fascinating sequence of transformations where uranium-238 undergoes radioactive decay. This series consists of a series of decay steps, ultimately resulting in the creation of a stable isotope, lead-206.
Uranium-238 begins its decay by undergoing alpha decay to form thorium-234, which itself is radioactive and continues the decay process. Along this decay pathway, radium-226 becomes an important intermediate. Radium-226 further decays into radon-222, another radioactive atom, contributing to the sequence of decays.
Understanding this series helps explain how uranium transforms through a series of radioactive isotopes, impacting concepts like nuclear stability and energy release. Each decay step releases radiation, typically in the form of alpha or beta particles and sometimes gamma rays. These processes are critical for scientists to understand radioactive materials and their behaviors over time.
Radioactive decay
Radioactive decay is a process by which unstable atomic nuclei lose energy by emitting radiation. This phenomenon can take various forms, such as alpha decay, beta decay, and gamma decay.
- **Alpha Decay** involves the release of alpha particles, which consist of two protons and two neutrons. This process decreases the atomic number by 2 and the mass number by 4.
- **Beta Decay** can either involve the transformation of a neutron into a proton with the release of an electron (beta-minus decay) or the conversion of a proton into a neutron with the release of a positron (beta-plus decay).
- **Gamma Decay** involves the release of gamma rays, a form of electromagnetic radiation, often following alpha or beta decay when the nucleus rearranges itself into a more stable state.
Radioactive decay is integral to understanding not only the behavior of nuclear materials but also applications like carbon dating and medical imaging.
Alkaline earth metals
Alkaline earth metals belong to Group 2 of the periodic table and include elements like beryllium, magnesium, calcium, strontium, barium, and radium. These metals commonly exhibit a +2 oxidation state due to the loss of two outermost electrons, forming stable ionic compounds.
Some hallmark properties of these metals include:
- They are shiny, silvery-white, and somewhat reactive at standard temperature and pressure.
- They react readily with water, albeit not as vigorously as their Group 1 counterparts, the alkali metals.
- They form oxides and hydroxides that are basic in nature.
Radium, being an alkaline earth metal, shares these properties. However, it is unique due to its heavier atomic mass and radioactivity. Understanding these properties helps in predicting the chemical behavior and reactions of radium, especially in its interaction with other substances.
Oxidation state
The oxidation state is a concept used to describe the degree of oxidation of an atom in a chemical compound. This refers to the number of electrons lost, gained, or shared by an atom.
In the case of radium, as part of the alkaline earth metals, the most common oxidation state is +2. This results from the atom losing its two outermost electrons to achieve a stable electron configuration.
The oxidation state is essential in predicting how an element will react chemically. For radium, achieving a +2 oxidation state means it readily forms compounds like radium chloride (RaCl₂) by bonding with other atoms to create stable ionic networks.
Radium mobility in water
Radium's mobility in water is primarily influenced by its chemical nature as well as environmental factors. In water, radium can exist as a soluble ion due to its +2 charge, but many factors can alter its mobility.
These factors include:
- The presence of anions such as sulfate and carbonate, which can react with radium to form insoluble salts, effectively reducing its mobility.
- The pH level of the water, where alkaline conditions may decrease radium’s solubility.
- The concentration of other ions, which might compete with radium or facilitate its precipitation.
Understanding how radium interacts in aqueous environments is crucial, especially in assessing its impacts on water safety and environmental health.
Soil/water solubility factors
The solubility of substances like radium in soil and water can vary due to numerous factors. These include chemical reactions that occur based on environmental conditions.
Factors that impact solubility include:
- **pH Levels:** Acidic environments may enhance solubility, while alkaline conditions tend to reduce it, promoting the formation of insoluble compounds.
- **Presence of Complexing Agents:** Organic matter and other complexing agents can bind with radium, affecting its solubility and mobility.
- **Temperature:** Generally, higher temperatures can increase solubility, though this effect varies with different compounds.
- **Other Anions Present:** Anions such as carbonates, phosphates, and sulfates may lead to the formation of low-solubility salts with radium.
Understanding these factors is important for predicting the mobility and bioavailability of radium in natural settings, essential for environmental monitoring and remediation efforts.