Alfisols

Alfisols are latitudinally the most widespread of the twelve soil orders defined by the United States Department of Agriculture (USDA) [3]. These are mildly acidic soils with significant accumulation of clays, possessing a soil moisture regime that is moist for most of the year. Alfisols are typically well-drained and commonly used for agriculture.

Definition:

Alfisols are found in a variety of climates around the world. Some areas where they are prominent include West Africa immediately south of the Sahara Desert, eastern India, much of Europe and western Russia, the Midwest and Great Lakes regions of the United States, parts of the Australia coastline, and various other areas of the world [5].

The distribution of alfisols often forms a buffer between other soil orders with differing soil moisture regimes [5]. In warm climates they can occur adjacent to Aridisols (dry soils), separating them from various other soil orders associated with humid climates. An example where this occurs is in Texas, where alfisols in central and east Texas separate the dry West Texas soils from the humid southeastern United States. In mesic or cool climates Alfisols often occur adjacent to Mollisols (grassland soils).

Description:

Diagnostic features of alfisols include a thin ochric epipedon, which is a light-colored surface horizon, and a prominent argillic horizon [2]. The argillic horizon is a product of silicate clay accumulation in the B horizon via illuviation, and cation exchange capacity in this horizon is over 35% saturated with base-forming cations [2]. Soil water potential greater than 1500 kPa is considered a “moist” soil moisture regime, and alfisols typically exceed this for most of the year [5]. However, for at least 3 months during periods of plant growth, soil moisture in alfisols is below this threshold [5].

Temperate forests and cropland commonly occur on alfisols, and net primary productivity is usually high. In some areas, particularly eastern Europe/western Russia and the Midwestern United States, there is substantial occurrence of loess [3]. Loess refers to the depositional products of soil erosion by wind. These soils are generally very fertile, as evidenced by the loess deposits in the intensively cultivated Midwestern United States.

Soil Classification

Similar to lifeforms, soils are classified into their own "taxnomic" groups. Alfisols are one of twelve orders of classified soils, within alfisols there are five suborders.

Geographic Distribution of Suborders

Aqualfs- found south of the Mississippi and throughout Indiana and Ohio. They are often used as soils for our most produced crops such as corn, rice, and soybeans.

Ustalfs- The most prevalent suborder of the group, can be found across the eastern United States from Wisconsin to New Yrok, and down to Texas. Moisture levels are higher in this group when compared to others.

Cryalfs- higher elevations are home to this group specifically the Rocky Mountain states.

Xeralfs- can also be used as a cropland or grazing land for cattle. Found in the eastern half of United States from Texas to California, up to Washington.

Udalfs-

Ecology:

Around the world, alfisols are used intensively for agriculture. In the United States, particularly the Midwest and Great Lakes regions, major crops include grains, corn, and hay [3]. Dairy farming is also common in these areas. Alfisols in Mediterranean climates (i.e. Europe and California) are cultivated for fruits, nuts, and various specialty crops such as olives [3]. An important process that occurs in alfisol agroecosystems is crop straw decomposition, which increases soil organic matter and nutrient availability [6]. Alfisols that are low in organic matter are susceptible to soil erosion, particularly in agricultural areas [1]. A variety of best management practices for agriculture are utilized in these areas, such as crop rotations, cover cropping, and fallowing [1].

The geographic and climatic diversity of alfisols means that a greater variety of flora and fauna exists compared to other soil orders. Astigmatic mites are often found at their greatest densities in agroecosystems after events that increase soil organic matter, such as harvest, tillage, and the application of soil amendments [4]. Enchytraeids are often found at higher densities in alfisols compared to other soils – they are typically associated with high acidity and organic matter found in temperate forests, grasslands, and agricultural areas [4]. Other prominent soil fauna in agroecosystems include Carabidae (ground beetles) and various species of mound-building and humivorous termites [4].

References

[1]Adekiya, A.O., and others. Soil productivity improvement under different fallow types on Alfisol of a derived savanna ecology of Nigeria. 2021. Heliyon. 7:e06759.

[2]Brady, Nyle C., and Weil, Ray R. “Elements of the Nature and Properties of Soils.” 2000. Prentice Hall. Upper Saddle River, NJ.

[3]Christopherson, Robert W. “Geosystems: An Introduction to Physical Geography, Tenth Edition.” 2017. Pearson. Hoboken, NJ.

[4]Coleman, David C., Callaham Jr., Mac A., and Crossley Jr., D. A. “Fundamentals of Soil Ecology, Third Edition.” 2018. Academic Press. Cambridge, MA.

[5]Soil Taxonomy, Second Edition. 1999. United States Department of Agriculture Natural Resources Conservation Service. pg. 163.

[6]Li, Ji-Fu, and Zhong, Fang-Fang. Nitrogen release and re-adsorption dynamics on crop straw residue during straw decomposition in an Alfisol. 2021. Journal of Integrative Agriculture. 20(1):248–259.

[7] Distribution map from USDA, Natural Resource Conservation Service Soils