leirjord

Leirjord, also known as clay soil, is a type of soil characterized by its fine particles and dense structure. The particles in leirjord are smaller than those found in silt or sand, giving it a smooth, sticky feel when wet and a hard, cloddy texture when dry. This small particle size results in very low porosity, meaning there are few spaces between the particles.

The low porosity of leirjord significantly impacts its drainage and aeration. Water drains very slowly through clay soil, which can lead to waterlogging and a lack of oxygen for plant roots. Conversely, leirjord can retain a considerable amount of moisture, which can be beneficial in dry periods but can also make it difficult to work with when wet.

Leirjord is often rich in nutrients due to the ability of its fine particles to hold onto essential minerals. However, its poor structure can make these nutrients less accessible to plants. The plasticity of wet leirjord makes it easy to mold, a property that has been utilized for centuries in pottery and construction.

The composition of leirjord can vary, but it typically contains a high percentage of clay minerals. Depending on the specific mineralogy and the presence of other soil components, leirjord can range in color from gray to reddish-brown. Its dense nature can make it difficult for plant roots to penetrate, and it can compact easily under pressure.