Step 1: Understanding the Question:
The question tests the fundamental understanding of how electrical charges are generated on the surfaces of soil clay minerals.
Detailed Explanation:
• Permanent Charge (Statement I):
Permanent negative charge is "fixed" in the mineral structure during its formation.
It occurs due to isomorphous substitution, where a central cation of higher valence is replaced by one of lower valence without changing the physical structure of the crystal.
For example: $Al^{3+}$ replacing $Si^{4+}$ in the tetrahedral sheet, or $Mg^{2+}$ replacing $Al^{3+}$ in the octahedral sheet. This leaves a net negative charge that is independent of soil pH. Statement I is True.
• pH-Dependent Charge (Statement II):
Charges that result from exposed crystal edges or broken bonds are variable or pH-dependent.
On the edges, hydroxyl groups ($OH$) can either lose a proton (becoming negative at high pH) or gain a proton (becoming positive at low pH).
These are not "permanent" because they change with the acidity of the surrounding solution. Statement II is False.
• Significance:
$2:1$ clays like montmorillonite have mostly permanent charge. $1:1$ clays like kaolinite and humus have mostly pH-dependent charge.
Step 2: Final Answer:
Statement I correctly identifies isomorphous substitution as the source of permanent charge, whereas Statement II incorrectly attributes it to crystal edges.