Residuum (geology)

Residuum is often used to refer to the soil and subsoil that forms as the result of long weathering over carbonate rocks (limestone and dolomite) bedrock.[1] It is defined primarily as “the unconsolidated weathered at least partly, mineral material that has accumulated as consolidated rocks disintegrated in place.[2] It is a type of soil parent material which has formed in place of origin. This distinguishes residuum from most other types of parent material. Parent material is classified by mode of transport.

Characteristics

Parent material is one of the soil forming factors defined as “unconsolidated organic and mineral materials in which soils form”. Making Parent material an important part of the soil forming process. The other soil forming factors are climate, organisms, relief and time. Parent materials are classified by their mode of transport into a system.[3] These modes of transport are by wind (aeloian), water, gravity (colluvial), ice (glacial till), lakes (lacustrine), oceans (marine) or in place (non transported).[4]

Soils derived from residuum are called residual soils. These soils are expected to be mineralogically similar to their underlying bedrock.[5] While residuum is similar to the term regolith, it is more specific. While regolith refers to all unconsolidated earth materials above the solid bed rock, including transported sediments such as sand or alluvium, residuum is strictly a non transported parent material. However, parent materials formed in place or "in-situ" can further be classified as saprolite or residuum. Residuum differs from saprolite through its structure and degree of weathering. Saprolite is commonly referring to weathered material retaining details or structural features of the bedrock. The distinguishing feature between these is that residuum no longer retains the structural features or details of its bed rock. It has undergone greater transformation and experienced a decrease in volume from its origins as saprolite and bedrock. This is what is known as consolidation.

Production

Residuum and their associated residual soils are a produced through chemical weathering of their bedrock. These soils and subsoils typically have their origins in hot humid tropical locations. Their thickness varies with climates. In temperate climate its presence is in relatively lower amounts occurring as a “thin blanket of loose material above the bedrock. In tropical climates it can be much thicker”.[6] A certain degree of landscape stability is inferred for residual soils.[7] Identification and survey of these soils are most conclusive "where fresh outcrops are rare and all surface materials look alike".[6] In contrast, "a decrease in the amount of rock fragments as depth increases, especially over saprolite, indicates that the soil materials probably has been transported down slope".[8] Identification of residuum is relevant in soil science and geology because accurate identification conveys direct and implicit info about soil itself, the environment in which it formed, and its current environment. Soils provide a records of prevailing and past environments climates and human activities and much more.[7]

In limestone terrains the boundary between bedrock and residuum is commonly very sharp, but may be highly irregular, defining pinnacles and even isolated blocks of fresh bedrock surrounded by reddish residual silts and clays derived from its decomposition. Resistant materials such as chert, silicified fossils, or beds of sandstone remain and may concentrate on the surface as float.

gollark: Or...<list><symbol>+</symbol><integer>1</integer><integer>1</integer></list>
gollark: Or HTML, if you want to just make the syntax weird and inconsistent.
gollark: * XML
gollark: Idea: systemd esolang.
gollark: ESOLANG

References
  1. Larry E. Kichler; Richard L. Henderson; United States. Natural Resources Conservation Service; Missouri. Dept. of Natural Resources; University of Missouri—Columbia. Agricultural Experiment Station; Polk County Soil and Water Conservation District (Mo.) (2000). Soil survey of Polk County, Missouri. The Service. p. 115.
  2. "Glossary of Soil Science Terms". nesoil.com. Retrieved 2018-05-09.
  3. "Plant and Soil Sciences eLibrary". passel.unl.edu. Retrieved 2018-05-09.
  4. "Plant and Soil Sciences eLibrary". passel.unl.edu. Retrieved 2018-05-09.
  5. PLASTER, R. W.; SHERWOOD, W. C. (1971). "Bedrock Weathering and Residual Soil Formation in Central Virginia". Geological Society of America Bulletin. 82 (10): 2813. Bibcode:1971GSAB...82.2813P. doi:10.1130/0016-7606(1971)82[2813:bwarsf]2.0.co;2. ISSN 0016-7606.
  6. Gandhi, S.M.; Sarkar, B.C. (2016). Essentials of Mineral Exploration and Evaluation. Elsevier. pp. 125–158. doi:10.1016/b978-0-12-805329-4.00013-2. ISBN 9780128053294.
  7. "SSM-Ch. 2. Landscapes, Geomorphology, and Site Description".
  8. Shamlin, Carolyn (April 1982). Soil Survey Manual: Agriculture Handbook. Government Printing Office. p. 54.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.