Loam

For other uses, see Loam (disambiguation).

Loam (in geology and soil science) is soil composed mostly of sand (particle size > 63 micrometres (0.0025 in)), silt (particle size > 2 micrometres (7.9×10⁻⁵ in)), and a smaller amount of clay (particle size < 2 micrometres (7.9×10⁻⁵ in)).^{[citation needed]} By weight, its mineral composition is about 40–40–20% concentration of sand–silt–clay, respectively.^[1] These proportions can vary to a degree, however, and result in different types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam.^[1]

Soil types by clay, silt and sand composition as used by the United States Department of Agriculture

In the United States Department of Agriculture, textural classification triangle, the only soil that is not predominantly sand, silt, or clay is called "loam". Loam soils generally contain more nutrients, moisture, and humus than sandy soils, have better drainage and infiltration of water and air than silt- and clay-rich soils, and are easier to till than clay soils. In fact, the primary definition of loam in most dictionaries is soils containing humus (organic content) with no mention of particle size or texture, and this definition is used by many gardeners. The different types of loam soils each have slightly different characteristics, with some draining liquids more efficiently than others. The soil's texture, especially its ability to retain nutrients and water, are crucial.^[2] Loam soil is suitable for growing most plant varieties.

Bricks made of loam, mud, sand, and water, with an added binding material such as rice husks or straw, have been used in construction since ancient times.

Classifications

Loam soils can be classified into more specific subtypes. Some examples are sandy loam, silt loam, clay loam, and silty clay loam. Different soil phases have some variation in characteristics like stoniness and erosion that are too minor to affect native vegetative growth but can be significant for crop cultivation.^[3]

Use in farming

 

Fine, loam-rich field ideal for farming vegetables in the UK

Loam is considered ideal for gardening and agricultural uses because it retains nutrients well and retains water while still allowing excess water to drain away.^[4] A soil dominated by one or two of the three particle size groups can behave like loam if it has a strong granular structure, promoted by a high content of organic matter. However, a soil that meets the textural (geological) definition of loam can lose its characteristic desirable qualities when it is compacted, depleted of organic matter, or has clay dispersed throughout its fine-earth fraction.^{[clarification needed]}

For example, pea can be cultivated in sandy loam and clay loam soils, but not more compacted sandy soils.^[5]

Use in house construction

Main article: Earth structure

Loam (the high-humus definition, not the soil texture definition) may be used for the construction of houses, for example in loam post and beam construction.^[6] Building crews can build a layer of loam on the inside of walls, which can help to control air humidity. Loam, combined with straw, can be used as rough construction material to build walls. This is one of the oldest technologies for house construction in the world. Within this there are two broad methods: the use of rammed earth, or unfired bricks (adobe).^[7]

Over the years, many different words for the same material and techniques were created, such as mudbricks, adobe or cob. This is often confusing, can extend the misunderstandings and problems in construction with loam. It was one of the reasons, why Switzerland started 1991 to create a Norm, followed by Germany who further created clear definitions and norms.^[8]

•  
  Loam with timber framing (Michelau in Oberfranken, Germany, 2007)
•  
  House with loam ground floor (Baligród, Poland, 2012)
•  
  Loam-timber-framed 1707 house, under restoration (Biesenthal, Germany, 2006)
•  
  Great Mosque of Djenné (Mali, 2004)

See also

• Loess – Sediment of accumulated wind-blown dust
• Grain size – Diameter of individual grains of sediment, or of lithified particles in clastic rocks
• Soil texture – Property of a soil

References

1. Kaufmann, Robert K.; Cutler J. Cleveland (2008). Environmental Science. McGraw-Hill. pp. 318–319. ISBN 978-0-07-298429-3.
2. R. B. Brown (September 2007). "Soil Texture" (PDF). Agronomy Fact Sheet Series: Fact Sheet SL-29. Cornell University, Department of Crop and Soil Sciences. Retrieved June 16, 2021.
3. United States Department of Agriculture Soil Survey, 1943
4. B. Rosie Lerner, "What is Loam?", Purdue University Consumer Horticulture, 6 January 2000. Retrieved 5 March 2017.
5. "Field Pea: Agronomy".
6. Schittich (Ed), Christian Schittich (2001). Building Simply. Birkhäuser Architecture. pp. 38–42. ISBN 3764372710.
7. Gerhard Koch, "Loam Construction – from a niche product to an industrial building system". Tokyo: Action for Sustainability – The 2005 World Sustainable Building Conference in Tokyo, Japan, September 2005. Retrieved 17 December 2012.
8. "Fachberichte :: IG Lehm Schweiz". www.iglehm.ch. Retrieved 2023-11-05.

External links

 

Wikimedia Commons has media related to Loam.