Lability

From Wikipedia, the free encyclopedia
  (Redirected from Labile)
Jump to: navigation, search
For the psychological term, see Labile affect.

Lability refers to something that is constantly undergoing change or something that is likely to undergo change.

Chemistry[edit]

The term is used to describe a transient chemical species. As a general example, if a molecule exists in a particular conformation for a short life-time, before adopting a lower energy conformation, the former molecular structure is said to have 'high lability' (such as C25, a 25-carbon fullerene spheroid). The term is sometimes also used in reference to reactivity - for example, a complex that quickly reaches equilibrium in solution is said to be labile (with respect to that solution). Another common example is the cis effect in organometallic chemistry, which is the labilization of CO ligands in the cis position of octahedral transition metal complexes.

Biochemistry[edit]

In reference to biochemistry, this is an important concept as far as kinetics is concerned in metalloproteins. This can allow for the rapid synthesis and degradation of substrates in biological systems.

Biology[edit]

Cells[edit]

Labile cells refer to cells that constantly divide by entering and remaining in the cell cycle.[1] These are contrasted with "stable cells" and "permanent cells".

An important example of this is in the epithelium of the cornea, where cells divide at the basal level and move upwards, and the top-most cells die and fall off.

Proteins[edit]

In medicine, the term "labile" means susceptible to alteration or destruction. For example, a heat-labile protein is one that can be changed or destroyed at high temperatures.

The opposite of labile in this context is "stable."[2]

Soils[edit]

Compounds or materials that are easily transformed (often by biological activity) are termed labile. For example, labile phosphate is that fraction of soil phosphate that is readily transformed into soluble or plant-available phosphate.[3] Labile organic matter is the soil organic matter that is easily decomposed by microorganisms.[4]

References[edit]

  1. ^ "Regeneration and Repair". 
  2. ^ Jackson CJ, Fox AJ, Jones DM, Wareing DR, Hutchinson DN (August 1998). "Associations between heat-stable (O) and heat-labile (HL) serogroup antigens of Campylobacter jejuni: evidence for interstrain relationships within three O/HL serovars". Journal of clinical microbiology 36 (8): 2223–8. PMC 105019. PMID 9665996. 
  3. ^ Mattingly, G. E. G. (1975). "Labile phosphate in soils". Soil Science 119: 369. Retrieved 29 August 2014. 
  4. ^ "Can simple measures of labile soil organic matter predict corn performance?". www.sciencedaily.com. Retrieved 29 August 2014.