88 Ra

Radium (Ra) - Everyday Uses

Alkaline Earth Metals

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Understanding Radium: A Radioactive Element

Radium (Ra), with atomic number 88, is a radioactive alkaline earth metal. It is intensely radioactive, approximately a million times more radioactive than an equal mass of uranium. Its most stable isotope, Radium-226, has a half-life of 1600 years. This high radioactivity, while historically leading to various applications, also presents significant health hazards.

Historical and Niche Applications of Radium

While once thought to be beneficial, the widespread “everyday” uses of Radium have largely been discontinued due to its extreme radioactivity and associated health risks. The following represent either historical applications or highly specialized, niche uses:

  1. Luminous Paints: Historically, radium compounds were mixed with zinc sulfide to create phosphorescent paints. These paints were applied to watch dials, clock faces, and aircraft instrument panels to make them glow in the dark. This practice was widespread in the early to mid-20th century but was phased out due to the severe health consequences for workers exposed to radium.
  2. Medical Brachytherapy: Early forms of cancer treatment utilized radium for brachytherapy. Small sealed sources containing radium were implanted directly into or near tumors to deliver localized radiation doses. This method was effective but presented significant radiation protection challenges for medical staff and has largely been replaced by safer radioisotopes like iridium-192 or cobalt-60.
  3. Radium-Beryllium Neutron Sources: Radium-226 can be mixed with beryllium to create a neutron source. Alpha particles emitted by radium bombard the beryllium, causing it to emit neutrons. These sources were historically used in industrial applications such as well logging in the petroleum industry, moisture content measurements, and for initiating nuclear chain reactions in early atomic research.
  4. Calibration Standards: Due to its predictable decay and characteristic gamma emissions, radium sources have been used as calibration standards for radiation detection instruments, particularly in historical contexts. While still used in some specialized settings, other isotopes are now preferred for this purpose.
  5. Historical Quack Cures: In the early 20th century, before its dangers were fully understood, radium was incorporated into various purported health tonics, cosmetics, and medical devices, such as “radium water.” These products were marketed as cures for a wide range of ailments but were highly dangerous and often led to severe radiation poisoning. This practice is now universally condemned.

Natural Occurrence of Radium

Radium is not found free in nature. It is a radioactive decay product of uranium and is therefore found in all uranium-bearing ores. The primary source of radium is the uranium ore known as uraninite (pitchblende). Radium-226 is formed from the decay of uranium-238 through a series of intermediate radionuclides.

In India, significant deposits of uranium ores are found in areas such as Jaduguda in Jharkhand, Tummalapalle in Andhra Pradesh, Domiasiat in Meghalaya, and Rohil in Rajasthan. Since radium is a decay product of uranium, it is naturally present in minute quantities within the uranium ore extracted from these mining sites. However, its concentration is extremely low, making its extraction a complex process.

Extraction and Industrial Use

The extraction of radium is a challenging process due to its extremely low concentration in uranium ores and its intense radioactivity. Historically, radium was extracted as a byproduct during the processing of uranium ore. The classical method, pioneered by Marie Curie, involved a painstaking series of chemical separation steps:

  1. Crushing and Grinding: Uranium ore is crushed and ground into a fine powder.
  2. Acid Leaching: The powdered ore is treated with acids (e.g., sulfuric acid) to dissolve soluble components, including uranium and radium.
  3. Precipitation: Radium is chemically similar to barium. Therefore, barium salts (typically barium chloride) are added to the solution. Radium co-precipitates with barium sulfate or barium bromide due to their similar chemical properties, forming a mixed precipitate.
  4. Fractional Crystallization: The mixture of radium and barium salts is then subjected to repeated fractional crystallization. Radium salts are slightly less soluble than barium salts, allowing for their gradual separation and enrichment over many cycles. This step is labor-intensive and time-consuming.
  5. Purification: Further purification steps are employed to obtain radium in a relatively pure form.

Given the inherent dangers of handling highly radioactive materials and the extremely small quantities present, large-scale industrial extraction of pure radium is no longer common. Modern industrial “use” of radium is typically limited to its contained presence within nuclear waste from historical processing or for specific niche applications where its radioisotopic properties are indispensable and stringent safety protocols can be maintained. Its primary significance today lies more in historical context and as a natural component of the uranium decay chain.

Related Comparisons


Element Directory

1

H

Hydrogen

nonmetal

2

He

Helium

noble gas

3

Li

Lithium

alkali

4

Be

Beryllium

alkaline

5

B

Boron

metalloid

6

C

Carbon

nonmetal

7

N

Nitrogen

nonmetal

8

O

Oxygen

nonmetal

9

F

Fluorine

halogen

10

Ne

Neon

noble gas

11

Na

Sodium

alkali

12

Mg

Magnesium

alkaline

13

Al

Aluminum

post transition

14

Si

Silicon

metalloid

15

P

Phosphorus

nonmetal

16

S

Sulfur

nonmetal

17

Cl

Chlorine

halogen

18

Ar

Argon

noble gas

19

K

Potassium

alkali

20

Ca

Calcium

alkaline

21

Sc

Scandium

transition

22

Ti

Titanium

transition

23

V

Vanadium

transition

24

Cr

Chromium

transition

25

Mn

Manganese

transition

26

Fe

Iron

transition

27

Co

Cobalt

transition

28

Ni

Nickel

transition

29

Cu

Copper

transition

30

Zn

Zinc

transition

31

Ga

Gallium

post transition

32

Ge

Germanium

metalloid

33

As

Arsenic

metalloid

34

Se

Selenium

nonmetal

35

Br

Bromine

halogen

36

Kr

Krypton

noble gas

37

Rb

Rubidium

alkali

38

Sr

Strontium

alkaline

39

Y

Yttrium

transition

40

Zr

Zirconium

transition

41

Nb

Niobium

transition

42

Mo

Molybdenum

transition

43

Tc

Technetium

transition

44

Ru

Ruthenium

transition

45

Rh

Rhodium

transition

46

Pd

Palladium

transition

47

Ag

Silver

transition

48

Cd

Cadmium

transition

49

In

Indium

post transition

50

Sn

Tin

post transition

51

Sb

Antimony

metalloid

52

Te

Tellurium

metalloid

53

I

Iodine

halogen

54

Xe

Xenon

noble gas

55

Cs

Caesium

alkali

56

Ba

Barium

alkaline

57

La

Lanthanum

lanthanoid

58

Ce

Cerium

lanthanoid

59

Pr

Praseodymium

lanthanoid

60

Nd

Neodymium

lanthanoid

61

Pm

Promethium

lanthanoid

62

Sm

Samarium

lanthanoid

63

Eu

Europium

lanthanoid

64

Gd

Gadolinium

lanthanoid

65

Tb

Terbium

lanthanoid

66

Dy

Dysprosium

lanthanoid

67

Ho

Holmium

lanthanoid

68

Er

Erbium

lanthanoid

69

Tm

Thulium

lanthanoid

70

Yb

Ytterbium

lanthanoid

71

Lu

Lutetium

lanthanoid

72

Hf

Hafnium

transition

73

Ta

Tantalum

transition

74

W

Tungsten

transition

75

Re

Rhenium

transition

76

Os

Osmium

transition

77

Ir

Iridium

transition

78

Pt

Platinum

transition

79

Au

Gold

transition

80

Hg

Mercury

transition

81

Tl

Thallium

post transition

82

Pb

Lead

post transition

83

Bi

Bismuth

post transition

84

Po

Polonium

metalloid

85

At

Astatine

halogen

86

Rn

Radon

noble gas

87

Fr

Francium

alkali

88

Ra

Radium

alkaline

89

Ac

Actinium

actinoid

90

Th

Thorium

actinoid

91

Pa

Protactinium

actinoid

92

U

Uranium

actinoid

93

Np

Neptunium

actinoid

94

Pu

Plutonium

actinoid

95

Am

Americium

actinoid

96

Cm

Curium

actinoid

97

Bk

Berkelium

actinoid

98

Cf

Californium

actinoid

99

Es

Einsteinium

actinoid

100

Fm

Fermium

actinoid

101

Md

Mendelevium

actinoid

102

No

Nobelium

actinoid

103

Lr

Lawrencium

actinoid

104

Rf

Rutherfordium

transition

105

Db

Dubnium

transition

106

Sg

Seaborgium

transition

107

Bh

Bohrium

transition

108

Hs

Hassium

transition

109

Mt

Meitnerium

transition

110

Ds

Darmstadtium

transition

111

Rg

Roentgenium

transition

112

Cn

Copernicium

transition

113

Nh

Nihonium

post transition

114

Fl

Flerovium

post transition

115

Mc

Moscovium

post transition

116

Lv

Livermorium

post transition

117

Ts

Tennessine

halogen

118

Og

Oganesson

noble gas