Step 1: Understanding the Concept:
Imogolite is a unique aluminosilicate clay mineral with a distinct hollow, tube-like, thread-like molecular structure, commonly grouped under non-crystalline or poorly crystalline soil minerals.
Step 3: Detailed Explanation:
Let us analyze each statement regarding the mineralogical properties of imogolite:
- Statement (A) is correct: Imogolite, along with allophane, is a classic diagnostic mineral formed from the weathering of volcanic ash.
It is highly abundant in volcanic ash soils, which belong to the soil order Andisols.
- Statement (B) is incorrect: While Andisols containing imogolite do have very low bulk density, imogolite itself is non-plastic or has low plasticity and low cohesion when wet compared to crystalline silicate clays (like montmorillonite).
- Statement (C) is incorrect: High potassium ($K$) fixation capacity is a characteristic of crystalline 2:1 expanding and semi-expanding clay minerals (especially vermiculite and illite) due to their interlayer spaces.
Imogolite has a hollow tube structure and does not fix potassium in its interlayer spaces.
- Statement (D) is correct: Imogolite is classified as paracrystalline (poorly crystalline or short-range ordered) because it has structured molecular tubes but lacks the long-range three-dimensional crystalline order of minerals like kaolinite or montmorillonite.
Therefore, only statements (A) and (D) are correct, matching Option (D).
Step 4: Final Answer:
The correct characteristics of Imogolite are (A) and (D) only.