Table 2 Conventional and traditional soil features.

From: FDRL: a data-driven algorithm for forecasting subsidence velocities in Himalayas using conventional and traditional soil features

Conventional soil features

Specific gravity

The ratio of the density of the soil particles to the density of water, used to make conclusions regarding mineral content and type of soil.

Optimum moisture content

Percentage moisture at which the soil compacts most, needed for determining slope stability under load.

Sand (%)

Indicates the percentage of coarse-grained fragments; higher sand content improves drainage and reduces cohesion.

Plasticity index (PI) (%)

Range of moisture within which soil acts plastically; higher values reflect greater capacity for deformation under stress.

Plastic limit (PL) (%)

Critical moisture percentage at which soil begins to act plastically, crucial to workability and slope performance.

Fines content (%)

Silt and clay particle percentage; affects permeability and cohesion, influencing slope strength.

Liquid limit (LL) (%)

Percentage at which moisture content transforms soil into liquid state from plastic; useful for classifying soil behavior under conditions of saturation.

Saturated water content (%)

Moisture content at the condition when pores in soil are saturated with water, influencing drainage capacity as well as saturated weight.

Porosity

Porosity measures the volume of voids in the soil; higher porosity provides greater retention of water and affects the rate of infiltration.

Gravel (%)

Percentage of coarse particles, which tend to improve drainage and reduce compaction of the soil.

Particle size

Particle Size Range of particle sizes in the sample; determines texture, permeability, and cohesion.

Saturated unit weight

Saturated Unit Weight Weight of the saturated soil per unit volume; critical to determine stability for full saturation.

Traditional soil features

Color of the soil

1. Red

2. Brown

3. Black

4. White

5. Green

6. yellow

Applied to predict fertility and drainage: red/brown = good drainage; black = high in organic matter; yellow = poor drainage; white or green soils indicate mineral or salt.

Content

1. Sand

2. Slit

3. Gravel

4. Clay

5. Rocks and Debris

6. Coarseness

Utilized to sort soil textures and types by appearance and texture, affecting drainage, cohesion, and root penetration.

Related to water

1. Retention

2. Drainage

3. Moisture

4. Dryness

5. Hardness

6. Smoothness

7. Density

Symbolizes soil-water relations impacting saturation potential and mechanical response to rainfall.

Smell

1. Earthy

2. Musty

3. Faul

Smell points to aeration and biological activity: earthy connotes healthy conditions, musty or stinking can suggest poor drainage or anaerobic areas.

Taste

1. Sweetness

2. Saltness

Historically associated with pH and mineral status, which may be related to vegetation cover and soil chemistry.

Fertility

1. Fertile

2. Plant health

3. Deforestation

4. Vegetation cover

Refers to the biological productivity and ecological stability of the soil, both being associated with erosion and slope stability.

Field test

1. Stickness

2. Crumbling

3. Clump

Textural features like stickiness (clay content), crumbling (structure), and clumping (root permeability) provide quick information regarding soil stability.