- Texture: Sandy soil is composed primarily of sand particles, which are larger in size compared to other soil types. It has a gritty texture and does not hold water well due to its large pores.

2. Clay Soil:

- Texture: Clay soil is characterized by a high concentration of tiny clay particles. It has a smooth, sticky texture when wet and becomes hard and cracked when dry. Clay soil holds water tightly due to its small pores.

3. Silty Soil:

- Texture: Silty soil consists mainly of silt particles, which are smaller than sand but larger than clay particles. It has a smooth and flour-like texture. Silty soil holds water relatively well but not as much as clay soil.

4. Loam Soil:

- Texture: Loam soil is a well-balanced mixture of sand, silt, and clay particles. It has a crumbly and fertile texture, allowing for good water drainage and nutrient retention.

5. Peat Soil:

- Texture: Peat soil is formed from the accumulation of partially decayed plant matter in waterlogged areas. It has a spongy and fibrous texture and is acidic in nature. Peat soil has a high water-holding capacity.

6. Chalky Soil:

- Texture: Chalky soil contains a significant amount of calcium carbonate (chalk) and has a high pH. It has a fine and powdery texture and tends to be alkaline in nature.

7. Gravelly Soil:

- Texture: Gravelly soil consists of a mixture of soil and small stones or gravel. It has a coarse texture and allows for good drainage.

8. Loess Soil:

- Texture: Loess soil is a fine-grained soil transported and deposited by wind. It has a uniform and homogeneous texture, making it suitable for agriculture.