The coefficient of curvature for a well graded soil, must be from-
1.0 to 3.0
Soil grading refers to the distribution of particle sizes in a soil sample. It's a crucial characteristic that affects the soil's engineering properties like shear strength, permeability, and compressibility. Soils can be broadly classified as well-graded, poorly-graded, or gap-graded.
To quantify the particle size distribution obtained from a sieve analysis, two important coefficients are used: the Coefficient of Uniformity ($C_u$) and the Coefficient of Curvature ($C_c$).
These coefficients are calculated using specific particle sizes determined from the particle size distribution curve:
The formulas for the coefficients are:
\(C_u = \frac{D_{60}}{D_{10}}\)
\(C_c = \frac{D_{30}^2}{D_{10} \times D_{60}}\)
Well-graded soil contains a good distribution of particle sizes, from coarse to fine, resulting in a dense and stable structure. According to the Unified Soil Classification System (USCS), the criteria for well-graded gravel (GW) and well-graded sand (SW) are defined based on their $C_u$ and $C_c$ values.
| Soil Type | $C_u$ Criterion | $C_c$ Criterion |
|---|---|---|
| Well-Graded Gravel (GW) | $C_u > 4$ | $1 \le C_c \le 3$ |
| Well-Graded Sand (SW) | $C_u > 6$ | $1 \le C_c \le 3$ |
As seen from the table, for both well-graded gravel and well-graded sand, the Coefficient of Curvature ($C_c$) must fall within the range of 1.0 to 3.0. The question asks for the coefficient of curvature for a "well graded soil," which generally refers to gravel or sand in the context of these grading coefficients.
Therefore, for a soil to be classified as well graded (specifically gravel or sand), its coefficient of uniformity must meet a minimum value ($>4$ for gravel, $>6$ for sand), AND its coefficient of curvature must be between 1.0 and 3.0, inclusive.
Based on the standard soil classification criteria, the coefficient of curvature for a well-graded soil (gravel or sand) must be from 1.0 to 3.0.
| Term | Formula | Significance | Criteria for Well-Graded Soil (Sand/Gravel) |
|---|---|---|---|
| Coefficient of Uniformity ($C_u$) | \(C_u = \frac{D_{60}}{D_{10}}\) | Indicates uniformity of particle sizes. Higher $C_u$ means wider range of sizes. | $C_u > 4$ (Gravel), $C_u > 6$ (Sand) |
| Coefficient of Curvature ($C_c$) | \(C_c = \frac{D_{30}^2}{D_{10} \times D_{60}}\) | Indicates the shape of the particle size distribution curve between $D_{10}$ and $D_{60}$. | $1 \le C_c \le 3$ (Both Gravel and Sand) |
Besides well-graded soils, other types of grading exist:
Well-graded soils are generally preferred for engineering purposes like road bases, foundations, and embankments because they can be compacted to achieve high densities and strength due to the interlocking of different-sized particles and the filling of voids by finer particles.
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