Step 1: Understanding the Concept:
Soil structure refers to the spatial arrangement and organization of primary soil particles (sand, silt, and clay) and organic matter into secondary units called aggregates or peds.
Unlike soil texture, which is a permanent physical property representing the relative proportion of particle sizes, soil structure is a dynamic property that can be influenced by biological activity, climate, and management practices.
It defines the nature and volume of pore spaces, which in turn governs the movement of air, water, and heat through the soil profile.
Step 2: Detailed Explanation:
Soil structure is a comprehensive term that encompasses several architectural aspects of the soil matrix.
The very fragments or clods into which the soil breaks up (Statement A) are a manifestation of the structural strength and bonding within the soil.
These units are often characterized by their shape (granular, platy, blocky, prismatic) and size.
Furthermore, the three-dimensional arrangement of individual mineral grains and organic constituents (Statement B) represents the fundamental microscopic level of structure.
This arrangement is mediated by cementing agents such as clay, organic matter, and iron/aluminum oxides.
Crucially, soil structure includes the assemblage of aggregates (peds) and voids (Statement C).
These voids exist both within the aggregates (micropores) and between the aggregates (macropores).
The macropores are vital for drainage and aeration, while micropores are essential for moisture retention.
Statement D is more descriptive of soil fabric or micro-organization in a general sense, but the standard definitions of structure in pedology specifically emphasize statements A, B, and C as they relate to the grouping of particles into peds.
Step 3: Final Answer:
Soil structure is defined by the fragments/clods, the 3D arrangement of mineral/organic components, and the assemblage of peds and voids. Therefore, A, B, and C are the correct defining attributes.