Problem 112
Question
In the ore of what metal would you look for thorium? Explain.In the ore of what metal would you look for thorium? Explain.
Step-by-Step Solution
Verified Answer
Thorium is commonly found in the ore of the mineral monazite, a phosphate mineral containing rare earth elements and thorium. Monazite forms in granitic and other igneous rocks, as well as in metamorphic rocks, due to the similar physical and chemical properties of thorium and the rare earth elements it coexists with.
1Step 1: Understanding ore
An ore is a naturally occurring material that contains a metal or mineral in a high enough concentration to be economically mined. Ores can be formed in a variety of geological processes, and can be found distributed throughout the Earth's crust.
2Step 2: Understanding thorium
Thorium is a radioactive chemical element with symbol Th and atomic number 90. It is a metal in the actinide series of periodic table, and occurs naturally as a mineral, primarily as thorium-232. Thorium is used as a nuclear fuel, and also has potential applications in various other technologies.
3Step 3: Identifying the ore in which thorium appears
Thorium is commonly found in the ore of the mineral monazite. Monazite is a highly radioactive, reddish-brown phosphate mineral, primarily composed of the rare earth elements cerium, lanthanum, praseodymium, and neodymium, along with thorium and sometimes uranium.
4Step 4: Explaining why thorium is found in monazite ore
Monazite forms as an accessory mineral in granitic and other igneous rocks, as well as in metamorphic rocks. Over geological time, these rocks can be weathered and eroded, leading to the concentration of monazite in sedimentary deposits such as placer deposits, commonly found in river systems or along beach shores. The reason thorium is found in monazite is because of its similar physical and chemical properties to the rare earth elements it coexists with. This makes them more likely to form a solid solution with each other, leading to monazite hosting small amounts of thorium-232.
In conclusion, to look for thorium, you would principally search in the ore of the mineral monazite, which is a phosphate mineral containing rare earth elements and thorium.
Key Concepts
MonaziteRadioactive ElementsActinide Series
Monazite
Monazite is a noteworthy phosphate mineral rich in rare earth elements, serving as a significant source of thorium. It usually appears as a reddish-brown mineral and is known to be highly radioactive. The composition of monazite often includes elements like cerium, lanthanum, praseodymium, and neodymium.
These elements, known as rare earth elements, are essential in producing various modern technologies.
Monazite typically forms in specific geological settings:
These elements, known as rare earth elements, are essential in producing various modern technologies.
Monazite typically forms in specific geological settings:
- It is an accessory mineral in granitic and igneous rocks.
- Also found in metamorphic rocks.
- Concentrated in sedimentary deposits such as river placer deposits or along beach sands.
Radioactive Elements
Radioactive elements are characterized by their unstable nuclei and the emission of radiation as they decay to attain stability. Thorium, with its atomic number 90, fits this criterion as it naturally undergoes radioactive decay.
Here's what makes radioactive elements distinct:
Here's what makes radioactive elements distinct:
- They release energy in the form of particles or electromagnetic waves.
- The decay process transforms them from one element into another.
- This transformation is termed a 'decay chain'.
Actinide Series
The actinide series occupies a unique position on the periodic table, stretching from actinium to lawrencium, with thorium fitting right in. These elements, often radioactive, share characteristic properties and are primarily located in the f-block.
A few insights on actinide metals:
- They possess high atomic and ionic sizes.
- Display a distinct metallic radiance.
- Show complexity in their electronic structures due to f-orbital occupancy.
Other exercises in this chapter
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