In chemistry, an alkali (English pronunciation: /ˈælkəlaɪ/; from Arabic: Al-Qaly القلي, القالي ) is a basic, ionic salt of an alkali metal or alkaline earth metal element. Some authors also define an alkali as a base that dissolves in water. A solution of a soluble base has a pH greater than 7. The adjective alkaline is commonly used in English as a synonym for base, especially for soluble bases. This broad use of the term is likely to have come about because alkalis were the first bases known to obey the Arrhenius definition of a base and are still among the more common bases.
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Etymology
The word "alkali" is derived from Arabic al qalīy = the calcined ashes, referring to the original source of alkaline substance. Ashes were used in conjunction with animal fat to produce soap, a process known as saponification.
Common properties
Alkalis are all Arrhenius bases, which form hydroxide ions (OH-) when dissolved in water. Common properties of alkaline aqueous solutions include:
- Moderately concentrated solutions (over 10−3 M) have a pH of 7.1 or greater. This means that they will turn phenolphthalein from colorless to pink.
- Concentrated solutions are caustic (causing chemical burns).
- Alkaline solutions are slippery or soapy to the touch, due to the saponification of the fatty acids on the surface of the skin.
- Alkalis are normally water soluble, although some like barium carbonate are only soluble when reacting with an acidic aqueous solution.
- Acids and alkalis are measured on a pH scale
- Turns Universal Indicator Blue-Dark Purple.
Difference between alkali and base
The terms "base" and "alkali" are often used interchangeably, particularly outside of a scientific context.
There are various definitions for alkali. Alkali is often defined as a subset of base. However, two subsets are commonly chosen.
- A basic salt of an alkali metal or alkaline earth metal [1][2] (This includes Mg(OH)2 but excludes NH3.)
- Any base that is water-soluble and forms hydroxide ions [3][4][5] or the solution of a base in water [6]. (This excludes Mg(OH)2 but includes NH3.)
The second subset of base is also called an Arrhenius base.
Salts
Most basic salts are alkali salts, of which common examples are:
- sodium hydroxide (often called "caustic soda")
- potassium hydroxide (commonly called "caustic potash")
- lye (generic term, for either of the previous two, or even for a mixture)
- calcium carbonate (sometimes called "free lime" or "limewater")
- magnesium hydroxide is an example of an atypical alkali since it has low solubility in water (although the dissolved portion is considered a strong base due to complete dissociation of its ions).
Alkaline soil
Soil with a pH value higher than 7.3 is normally referred to as alkaline. This soil property can occur naturally, due to the presence of alkali salts. Although some plants do prefer slightly basic soil (including vegetables like cabbage and fodder like buffalograss), most plants prefer a mildly acidic soil (pH between 6.0 and 6.8), and alkaline soils can cause problems. In chemistry, an Alkali is a basic ionic salt of an alkali metal or alkaline earth metal element.
Alkali lakes
In alkali lakes (a type of salt lake), evaporation concentrates the naturally occurring alkali salts, often forming a crust of mildly basic salt across a large area.
Examples of alkali lakes:
- Alkali Lake (Oregon), Oregon, United States
- Baldwin Lake (San Bernardino County, California)
- Mono lake, California, United States
- Redberry Lake, Saskatchewan, Canada
- Spotted Lake, British Columbia, Canada
- Summer Lake, Oregon, United States
- Tramping Lake, Saskatchewan, Canada
- Lake Magadi, Kenya
- Lake Turkana, Kenya (the largest alkali lake in the world)