Atomic and physical Chalcogens show similar patterns in
electron configuration, especially in the outermost
shells, where they all have the same number of
valence electrons, resulting in similar trends in chemical behavior: All chalcogens have six
valence electrons. All of the solid, stable chalcogens are soft and do not
conduct heat well. tend to increase towards the chalcogens with higher atomic numbers.
Isotopes Out of the six known chalcogens, one (oxygen) has an atomic number equal to a nuclear
magic number, which means that their
atomic nuclei tend to have increased stability against radioactive decay. It has an additional 28 isomers. With the exception of livermorium, all chalcogens have at least one naturally occurring
radioisotope: oxygen has trace 15O, sulfur has trace 35S, selenium has 82Se, tellurium has 128Te and 130Te, and polonium has 210Po. Among the lighter chalcogens (oxygen and sulfur), the most neutron-poor isotopes undergo
proton emission, the moderately neutron-poor isotopes undergo
electron capture or
β+ decay, the moderately neutron-rich isotopes undergo
β− decay, and the most neutron rich isotopes undergo
neutron emission. The middle chalcogens (selenium and tellurium) have similar decay tendencies as the lighter chalcogens, but no proton-emitting isotopes have been observed, and some of the most neutron-deficient isotopes of tellurium undergo
alpha decay. Polonium isotopes tend to decay via alpha or beta decay. Isotopes with nonzero
nuclear spins are more abundant in nature among the chalcogens selenium and tellurium than they are with sulfur. for
solid oxygen Oxygen's most common
allotrope is diatomic oxygen, or O2, a reactive paramagnetic molecule that is ubiquitous to
aerobic organisms and has a blue color in its
liquid state. Another allotrope is O3, or
ozone, which is three oxygen atoms bonded together in a bent formation. There is also an allotrope called
tetraoxygen, or O4, and six allotropes of
solid oxygen including "red oxygen", which has the formula O8. Sulfur has over 20 known allotropes, which is more than any other element except
carbon. The most common allotropes are in the form of eight-atom rings, but other molecular allotropes that contain as few as two atoms or as many as 20 are known. Other notable sulfur allotropes include
rhombic sulfur and
monoclinic sulfur. Rhombic sulfur is the more stable of the two allotropes. Monoclinic sulfur takes the form of long needles and is formed when liquid sulfur is cooled to slightly below its melting point. The atoms in liquid sulfur are generally in the form of long chains, but above 190 °C, the chains begin to break down. If liquid sulfur above 190 °C is
frozen very rapidly, the resulting sulfur is amorphous or "plastic" sulfur. Gaseous sulfur is a mixture of diatomic sulfur (S2) and 8-atom rings. Selenium has at least eight distinct allotropes. The gray allotrope, commonly referred to as the "metallic" allotrope, despite not being a metal, is stable and has a hexagonal
crystal structure. The gray allotrope of selenium is soft, with a
Mohs hardness of 2, and brittle. Four other allotropes of selenium are
metastable. These include two
monoclinic red allotropes and two
amorphous allotropes, one of which is red and one of which is black. The red allotrope converts to the black allotrope in the presence of heat. The gray allotrope of selenium is made from
spirals on selenium atoms, while one of the red allotropes is made of stacks of selenium rings (Se8). although its typical form is hexagonal. Polonium has two allotropes, which are known as α-polonium and β-polonium. α-polonium has a cubic crystal structure and converts to the rhombohedral β-polonium at 36 °C.
Chemical Oxygen, sulfur, and selenium are
nonmetals, and tellurium is a
metalloid, meaning that its chemical properties are between those of a
metal and those of a nonmetal. although it has some metallic properties. Also, some allotropes of selenium display characteristics of a metalloid, even though selenium is usually considered a nonmetal. Even though oxygen is a chalcogen, its chemical properties are different from those of other chalcogens. One reason for this is that the heavier chalcogens have vacant
d-orbitals. Oxygen's electronegativity is also much higher than those of the other chalcogens. This makes oxygen's
electric polarizability several times lower than those of the other chalcogens. For
covalent bonding a chalcogen may accept two electrons according to the
octet rule, leaving two
lone pairs. When an atom forms two
single bonds, they
form an angle between 90° and 120°. In 1+
cations, such as hydroxonium|, a chalcogen forms three
molecular orbitals arranged in a
trigonal pyramidal fashion and one lone pair. Double bonds are also common in chalcogen compounds, for example in chalcogenates (see below). The
oxidation number of the most common chalcogen compounds with positive metals is −2. However the tendency for chalcogens to form compounds in the −2 state decreases towards the heavier chalcogens. Organic sulfur compounds such as
thiols have a strong specific smell, and a few are utilized by some organisms. Oxygen ions often come in the forms of
oxide ions (),
peroxide ions (), and
hydroxide ions (). Sulfur ions generally come in the form of
sulfides (),
bisulfides (),
sulfites (),
sulfates (), and
thiosulfates (). Selenium ions usually come in the form of
selenides (),
selenites () and
selenates (). Tellurium ions often come in the form of
tellurates (). Except for polonium, the chalcogens are all fairly similar to each other chemically. They all form X2− ions when reacting with
electropositive metals.
Sulfide minerals and analogous compounds produce gases upon reaction with oxygen. ==Compounds==