Understanding the soil texture is the first step in determining whether your soil is clay or sand. You don’t need sophisticated tools to know your soil type. You can touch and use your eyes.
A successful planting season depends on knowing your soil type and understanding how to provide the nutrients your soil is missing.
The blog post below will define soil texture and its importance in identifying your soil as clay or sand.
How Do You Determine Soil Texture?
Soil is made of solids, liquids, and gases. Solids consist of minerals ( sand, silt, and clay) and organic matter( living and non-living forms. Liquids( mostly water) and gases( more carbon dioxide and less oxygen) fill the pores found between the solid particles.
Soil texture refers to the size and distribution of sand, silt, and clay in a soil or mix. Soil texture is so important that it affects the function and behavior, including
Soil water: The soil texture affects the infiltration, percolation rates, and ability to hold water. The soil’s drainage characteristics impact the agricultural production of the plants grown. Well-drained soils are more productive compared to soils that have poor drainage. The well-drained soils have good root development compared to the roots that grow in waterlogged soils.
Infiltration and percolation are the rate water moves in and through the soil. Soils on level terrain have more infiltration and percolation than those on sloped terrain. Runoff occurs when water inputs exceed the inflation capacity of the soil.
Surface layers consisting of sandy textures or strongly developed aggregates have larger pores and, therefore, more inflation and percolation than clayey or no aggregates.
Soil Structure: The arrangement of soil particles( sand, silt, and clay) into peds and aggregates. Soil structure is created when microbial gums, iron oxides, organic matter, and clay bind soil particles. The shape, size, and strength of aggregates define soil structure.
The soil structure is dynamic as it can be altered through activities like plowing, rototilling, and adding organic matter. Well-developed structure enhances soil-plant relationships and affects the:
- Exchange of soil air with the atmosphere
- Rate of water movement through the soil
- Size and amount of pore space
- Amount of water a soil can hold
- The ease with which plants extend their roots
Crusting phenomenon occurs on bare soils. Crusts are created when raindrops’ impact destroys the surface layer’s structure. Under these circumstances, the clay particles and organic matter that bind aggregates are washed away. Soils low in organic matter are most subject to crusting.
Crusts may nearly stop air exchange between the soil and the atmosphere, impede water infiltration, and inhibit seedlings’ emergence.
Nutrient holding capacity: The soil’s ability to hold nutrients is measured in Cation exchange capacity or CEC. The nutrient-holding capacity determines how soils hold and release nutrients.
Clay minerals, organic matter, and plant nutrients in ionic form have electrical charges. In soil, clay minerals and organic matter have a negative charge. Cations nutrients such as potassium can be held near negatively charged clay and organic minerals.
The higher the clay and organic matter content, the higher the CEC will be. Plants mainly absorb nutrients from soil solutions Clay soil is sufficient to hold and release more than enough plant nutrients in cation form for vigorous plants.
Sandy soils with clay or organic matter need to hold sufficient cation nutrients.
Ease of cultivation: Soil texture affects the ease at which the soil can be tilled and worked on. Clay soil can be waterlogged and difficult to work with. Soils with large percentages of clay are a challenge compared to sandy soils soil particles can hold onto water when wet. When dry, the soil can easily break and be tilled easier.
Sandy soils are known for their poor drainage. When pressed together, sandy soil has a hard time holding its form. The soil is easy to manipulate in your hand
|2.0 – 0.05
|0.05 – 0.002
|10x – 100x magnification
|*25.4mm = 1-inch
Particles greater than 2.0mm are considered to as rock fragments and are not considered in the soil texture table above. The soil texture triangle can be used to identify if the soil is sand, clay, or silt using the fractions provided in the table.
How Can You Tell If Soil Is Clay? A simple way of identifying clay soil is by touch and sight. When dry, the soil feels hard. When squeezed, a moist mass will form a durable cast and forms a flexible ribbon when squeezed between the thumb and forefingers.
Typically, clay soils have poor drainages but have a high nutrient-holding capacity compared to sandy soils.
How Can You Tell If Soil Is Sand? Sandy soil is also referred to as Coarse texture soil. The soils have low water holding capacity, excessive drainage, and are low in nutrients, especially nitrogen and potassium.
A simple way to identify sand soil is by touch. These soils feel gritty. When squeezed, a moist mass will form a cast; however, the cast will crumble when touched.
These soils are dominated by individual particles that can be seen without magnification.
The low nitrogen content in sandy soils causes plants to have stunted growth. The Leaves turn pale green to yellow. Typically, the oldest leaves are affected first, but the whole plant may turn yellow in severe cases.
In potassium-deficient sandy soils, the plants exhibit signs of leaves becoming gray or tan at or near the edge of the margins. The older leaves are first affected with characteristic scorching symptoms around the leaf margins.
Do plants grow better in clay or sand?
Both clay and sandy soils are not considered the best option for planting your vegetables and flowers. Clay soils retain water longer than sandy soil. The water hold capacity of clay soil can negatively affect root development. Water-logged soils can lead to the leaching of nutrients in the soil. Prolonged exposure to water can lead to roots rooting and dying off.
On the other hand, sandy soil’s poor drainage can lead to excessive leaching of nutrients. Sandy soils have low nutrient quantities needed for plant development and growth. Loamy soils are the best option for growing your plants. The soil is characterized by medium texture and typically has good drainage and ideal water-holding capacity.