The phrase "aggregate breakdown" is correct and usable in written English.
It can be used in contexts where you are discussing a summary or analysis of data that has been compiled or grouped together.
Example: "The report provided an aggregate breakdown of the sales figures for each quarter, allowing us to identify trends over the year."
Alternatives: "total analysis" or "combined summary".
This phenomenon led to soil aggregate breakdown and release of fine soil particles.
A new instability index, Ka, which considers aggregate breakdown mechanisms in interrill erosion processes, was proposed based on the disturbed sample results.
In contrast, structured soils can also release physically entrapped CO2 or give access to protected carbon sources inside aggregates due to aggregate breakdown by disruptive forces.
Soil aggregate breakdown is the first key step of splash erosion and is strongly influenced by soil internal forces, including electrostatic, hydration, and van der Waals forces.
To describe the effects of the drying wetting cycles on aggregate breakdown and water stability of aggregates, the yellow brown earth samples were subjected to several drying wetting cycles.
As is an aggregate stability index, which reflected the main mechanisms of aggregate breakdown in interrill erosion process, θ is the slope angle, I is the rainfall intensity, and q is the runoff rate.
During raindrop impact soil, aggregates breakdown and produce finer, more transportable particles and micro-aggregates.
The size distribution of water stable aggregates after breakdown in procedure (a) can be symbolized as follow: fleft({d}_iright)in left{{P}_{d_i}left|{d}_iin left{7.5,kern0.5em 3.5,kern0.5em 1.5,kern0.125right}right.right.375,kern0.5em 0.125right}right.right} (7 where, ( {P}_{d_i} ) is the mass percent content of the water stable aggregates with the diameter of d i.
By wet sieving method, the particle size distribution of water-stable aggregates after the breakdown of initial aggregates with different initial water content is listed in Table 4.
However, these figures are aggregates, neglecting the breakdown between public and private for profit (PFP) staff.
After the drying and rewetting by the runoffs, the original aggregates undergo the following breakdown and movement: (a) the original aggregates crack into smaller ones or reunite to larger ones; (b) water unstable aggregates are dissolved and washed away by runoffs; (c) the water stable aggregates have the possible to leak through the karst channels by the hydraulic forces (Fig. 9).
