There are few plants in the desert to provide the organic material.
Desert soils are low in organic matter because the arid conditions limit the decomposition of plant material that would contribute to organic content. The low moisture levels also hinder the growth of vegetation that could add to the organic matter in the soil.
Soils get their organic material from the plants that live, or have lived, in them. Deserts have few plants to provide this material.
Deserts typically have sandy soils with low organic matter content. These soils are often well-drained and have low fertility due to the arid conditions. Additionally, desert soils may be alkaline in nature.
Desert soils are typically sandy or sandy-loam soils with low organic matter content. They have low moisture retention capacity and are often nutrient-poor. These soils are formed through the weathering of rocks and minerals in arid environments.
Arctic soils and desert soils are similar because both are low in organic matter, nutrient-rich, and have minimal vegetation cover due to harsh environmental conditions such as extreme cold in the Arctic and low precipitation in deserts. These conditions limit the breakdown of organic matter and nutrient cycling in the soils, resulting in similar characteristics despite the different climates.
Aridisols are soils that develop in the driest climates, characterized by low precipitation and high evaporation rates. These soils are often found in desert regions and have limited organic matter and nutrient content.
The four regional categories of California's soils are coastal, foothill valley, desert, and mountain soils. Coastal soils are found near the ocean and are characterized by high organic content. Foothill valley soils are found in the inland valleys and support a variety of agricultural crops. Desert soils are found in the arid regions of the state and have low organic matter. Mountain soils are found in the higher elevations and are often rocky and less fertile.
Deserts typically have sandy soils with low organic matter, resulting in a light color like white or beige. The lack of moisture and vegetation in deserts limits the accumulation of organic matter that would give soil a darker, brown color commonly seen in more fertile regions. Additionally, desert soils are often rich in mineral salts, which can influence soil coloration.
Alfisols: These are moderately weathered soils with good fertility and a clay-rich subsoil. Mollisols: These are fertile, dark-colored soils known for their high organic matter content, originated from grassland areas. Aridisols: These are dry soils found in arid and semi-arid regions, characterized by low organic matter and distinct layers due to limited leaching. Spodosols: These are acidic soils commonly found in forested areas, characterized by distinct horizons with accumulation of organic matter and iron/aluminum oxides.
Topsoil in the desert tends to be thin, with low organic matter content and a high mineral composition due to arid conditions. In grasslands, topsoil is typically deeper, richer in organic matter, and supports a more diverse ecosystem due to higher precipitation levels that promote plant growth and decomposition.
There is very little topsoil in deserts; in fact, one millimeter of topsoil can take hundreds of years to form in a desert. The plant life in deserts evolved through selection to be less reliant on water and are therefore very slow to grow. Little plant life, little decay due to low moisture, and extremely slow growth rates could account for the low content of organic matter in desert soils.
The wettest climate would typically lead to the development of peat soil, characterized by high organic content due to waterlogged conditions. In the driest climate, arid soils such as desert soils or aridisols would develop, with low organic matter content and minimal water availability.