The main difference is in their chemical composition, their temperature of formation, density, colour, cleavage and mineral habit.
Calcium and Sodium Rich Feldspars:
There can be a mix of calcium and sodium (more correctly termed solid solutions) in Feldspars between Albite and Anorthite which are known generally as Plagioclase feldspars.
Depending on the relative sodium and calcium contents they are given differing names:
Albite = 100 - 90 % Na, 0 - 10 % Ca
Oligoclase = 90 - 70 % Na, 10 - 30 % Ca
Andesine = 70 - 50 % Na, 30 - 50 % Ca
Labradorite = 50 - 30 % Na, 50 - 70 % Ca
Bytownite = 30 - 10 % Ns, 70 - 90 % Ca
Anorthite = 10 - 0 % Na, 90 - 100% Ca
Alkali Feldspars (containing Potassium and Sodium)
There is also a limited solid solution series between Albite and K-Feldspars which takes the following form which is further complicated by the temperature dependent stability of some of the mineral forms:
Albite = 100 - 90 % Na, 0 - 10 % K
Anorthoclase = 90 - 64 % Na, 10 - 36 % K
Sanadine: Contains varying amounts of Na. Stable at high temperature. Occurs in rapidly cooled rocks.
Orthoclase: Predominately K, minor amounts of Na. Stable at moderate temperatures.
Microcline: Predominately K, minor amounts of Na. Stable at lowest temperatures. Common in the most slowly cooled rock types such as granites and pegmatites.
The chemical formulas of the Plagioclase Feldspars are as follows:
Albite = NaAlSi3O8
Oligoclase = (Na,Ca)(Al,Si)AlSi2O8
Andesine = NaAlSi3O8 - CaAl2Si2O8
Labradorite = (Ca,Na)Al(Al,Si)Si2O8
Bytownite = (NaSi,CaAl)AlSi2O8
Anorthite = CaAl2Si2O8
The chemical formulas of the Alkali Feldspars are as follows:
Albite = NaAlSi3O8
Anorthoclase = ((Na,K)AlSi3O8)
Sanadine = (K,Na)(Si,Al)4O8
Orthoclase and Microcline = KAlSi3O8
Colour:
Albite - White
Oligoclase - Off-white or grey or pale shades of green, yellow or brown
Andesine - White or grey
Labradorite - Grey to smoky black
Bytownite - White, grey or colourless but can be pale shades of other colours
Anorthite - White, grey or colourless
Anorthoclase - Colourless, green, grey, grey pink, yellow
Sanadine - Off-white, yellow or pale shades of other colours
Microcline - Off-white,yellowish, flesh pink, brown or green
Orthoclase - Off-white, yellow, or shades of red, orange to brown
Density (g/cm3) :
Albite - 2.61
Oligoclase - 2.64 - 2.68
Andesine - 2.68 - 2.71
Labradorite - 2.70 - 2.74
Bytownite - 2.74 - 2.76
Anorthite - 2.76
Anorthoclase - 2.57 - 2.6
Sanadine - 2.56 - 2.53
Microcline - 2.5
Orthoclase - 2.53 - 2.56
Crystal Habit:
Albite - triclinic
Oligoclase - triclinic
Andesine - triclinic
Labradorite - triclinic
Bytownite - triclinic
Anorthite - triclinic
Anorthoclase - triclinic
Sanadine - monoclinic
Microcline - triclinic
Orthoclase - monoclinic
Cleavage:
Albite - Perfect in one direction, good in second.
Oligoclase - Perfect in one direction, good in second.
Andesine - Perfect in one direction, good in second.
Labradorite - Perfect in one direction, good in second.
Bytownite - Perfect in one direction, good in second.
Anorthite - Perfect in one direction, good in second.
Anorthoclase - Perfect in one direction, good in second.
Sanadine - Good in 2 directions.
Microcline - Perfect in one direction, good in second.
Orthoclase - Good in 2 directions.
Feldspar is not a specific substance, but a class of aluminosilicates of potassium, sodium and calcium.
It depends on the type of feldspar. Potassium Feldspar (also called K-Spar), contains potassium, aluminum, silicate: KAlSi3O8. Plagioclase Feldspar, on the other hand, contains calcium or sodium, aluminum, and silicate: NaAlSi3O8 or CaAl2Si2O8.
There are broadly three main types of feldspars: calcium, sodium and potassium. They have the following general chemical formulas:KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8The endmember mineral states are known as K-Feldspar, Albite and Anorthite which are the potassium, sodium and calcium feldspars respectively.There can be a mix of calcium and sodium (more correctly termed solid solutions) in Feldspars between Albite and Anorthite which are known generally as Plagioclase feldspars.For more information please see the related question
It varies from 2.52 - 2.74 grams/cc (Orthoclas=2.52 Anorthite=2.74) The density varies to heavier with greater amounts of Sodium or Calcium and lighter for Potassium Feldspar (Orthoclase)
Feldspars are a common non-metallic alumino-silicate mineral that have a hardness of 6 on Mohs scale and produce white streaks.There are broadly three main types: potassium, sodium and calcium rich feldspars. They have the following general chemical formulas:KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8The endmember mineral states are known as K-Feldspar, Albite and Anorthite which are the potassium, sodium and calcium feldspars respectively.Perhaps you mean feldspar?Feldspar is the most common rock mineral in the Earth's crust (about 60%).
Feldspar is not a specific substance, but a class of aluminosilicates of potassium, sodium and calcium.
It depends on the type of feldspar. Potassium Feldspar (also called K-Spar), contains potassium, aluminum, silicate: KAlSi3O8. Plagioclase Feldspar, on the other hand, contains calcium or sodium, aluminum, and silicate: NaAlSi3O8 or CaAl2Si2O8.
Feldspar, a major constituent of most igneous rocks, reacts with carbonic acid to produce residual clay minerals plus dissolved ions of metals (potassium, sodium or calcium, depending on the type of feldspar). Here, for example, is the reaction by which potassium feldspar is converted to kaolinite, a clay mineral: 4KAlSi3O8 + 4H2CO3 + 2H2O → Al4Si4O10(OH)8 + 4K+ + 4HCO3- + 8SiO2 feldspar + carbonic acid + water → kaolinite + dissolved potassium and bicarbonate ions + dissolved silica Similar reactions affect sodium feldspar and calcium feldspar.
There are broadly three main types of feldspars: calcium, sodium and potassium. They have the following general chemical formulas:KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8The endmember mineral states are known as K-Feldspar, Albite and Anorthite which are the potassium, sodium and calcium feldspars respectively.There can be a mix of calcium and sodium (more correctly termed solid solutions) in Feldspars between Albite and Anorthite which are known generally as Plagioclase feldspars.For more information please see the related question
It varies from 2.52 - 2.74 grams/cc (Orthoclas=2.52 Anorthite=2.74) The density varies to heavier with greater amounts of Sodium or Calcium and lighter for Potassium Feldspar (Orthoclase)
x Al(Al,Si)3O8, where x can be sodium (Na) and/or calcium (Ca) and/or potassium (K).
The Hartmannn solution contain sodium lactate and sodium, potassium, calcium chlorides.
Potassium has the larger radius (not raduis!).
Food is something you eat, and nutrients are the good things that your body gets out of food like calcium or potassium
The precipitate would be calcium carbonate, CaCO3.
Calcium or Potassium are not halogens but metals.
Feldspars are a common non-metallic alumino-silicate mineral that have a hardness of 6 on Mohs scale and produce white streaks.There are broadly three main types: potassium, sodium and calcium rich feldspars. They have the following general chemical formulas:KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8The endmember mineral states are known as K-Feldspar, Albite and Anorthite which are the potassium, sodium and calcium feldspars respectively.Perhaps you mean feldspar?Feldspar is the most common rock mineral in the Earth's crust (about 60%).