This document provides an overview of calculus (dental tartar). It defines calculus, discusses its history, classification, prevalence, formation, composition, and theories of mineralization. Calculus is a hard deposit formed from mineralization of dental plaque. It consists mainly of calcium phosphate crystals like hydroxyapatite and whitlockite. Calculus forms more readily in some individuals and locations in the mouth. Various local factors in plaque are thought to increase calcium and phosphate levels and pH, leading to precipitation of crystals and calculus formation.
3. CONTENTS
Definitions
History
Classification
Supragingival calculus
Subgingival calculus
Prevalance
Rate of formation
Attachment of calculus
Diagnosis
Formation of calculus
Theories of mineralization
Clinical significance
Anticalculus agents
Indices
Future research
CONCLUSION
REFERENCES
4. Calculus is derived from Greek words Calcis-lime stone,
Tartar- white encrustation inside casks.
DEFINITION:
Calculus is a hard deposit that is formed by mineralization of
dental plaque on the surfaces of natural teeth and dental
prosthesis, generally covered by a layer of unmineralized
plaque.
Carranza's clinical periodontology(11th ed)
Calculus is a hard concretion that forms on teeth or dental
prosthesis through calcification of bacterial plaque
Glossary of periodontal terms(2001),4th edition
5. Calculus consists of mineralized bacterial plaque that forms on the surface of
natural teeth and dental prosthesis, covered on its external surface by vital,
tightly adherent, non mineralized plaque
Genco
When dental plaque calcifies ,the resulting deposit is called calculus
Grant
9. This shift in perception, which became most apparent in the 196O's, was largely a
response to two lines of investigation
1.Experimental and electron microscopic studies of developing plaque and
calculus demonstrated that supra and subgingival calculus was mineralized plaque
covered by an unmineralized bacterial layer
(Mandei, et al. 1957, Mandei 1960, Muhleman & Schroeder 1964, Oshrain et
al, 1968);
2.The experimental demonstration in humans that plaque, allowed to develop in
the absence of oral hygiene, results in a gingivitis which is reversible on the
resumption of tooth cleaning
(Loeet al,1965)
10. It was not until 1969 that Schroder provided a more appropriate
definition of calculus other than a calcified deposit adhering to the
teeth.
He Defined Dental Calculus As,
MINERALIZEDDENTALPLAQUETHAT IS PERMEATEDWITH
CRYSTALS OF VARIOUS CALCIUMPHOSPHATES.
(Perio 2000 vol.8 1995)
11. Classification
According to location
Supragingival calculus
Subgingival calculus
According to source of mineralization
Salivary calculus
Serumal calculus (Jenkins, Stewart 1966)
According to surface
Exogenous
Endogenous (Melz 1950)
12. According to initiation and rate of accumulation, calculus
formers are classified as:
-non calculus formers
- Slight calculus formers
-moderate calculus formers
-heavy calculus formers
(Muhler and Ennever 1962)
13. Subgingival calculus can be further classified according to the
morphology:
Crusty,spiny nodular
Ring like or ledge like
Veneer type
Fingerlike or fern like extension
Individual island or spots
Combination of all
16. INORGANIC MATRIX
70-80%
Calcium and phosphorous constitute the major
element and Ca/P ratio ranges from 1.6 to more
than 2
(Little et al,1963;Lundberg ,1966;
Shroeder,1969)INORGANIC
CALCIUM PHOSPHATE
75.9%
CALCIUM CARBONATE
3.1%
MAGNESIUM
PHOSPHATE
TRACES
COMPOSITION
17. The principle inorganic components are:
(Muhler and Enever,1962)
20. Hydroxyapatite and Octacalcium phosphate are detected most
frequently in supragingival calculus. (97-100%)
Brushite - mandibular anterior region; present only in the early-stage
supragingival calculus
(Rowles, 1964).
When supragingival calculus ages- Brushite
HAP,OCP&WHT
(Shroeder,1967)
Magnesium whitlockite - in the posterior areas
21. The composition of calculus varies and depends upon:
1. Concentration of Ca & P
2. Relative amount of ions present locally
3. pH of saliva
4. Presence of other minerals which are calcification promoters like
urea,fluoride,silicon,etc.
22. SUPRAGINGIVALCALCULUS
at low ph &high Ca:P at high ph
SUBGINGIVALCALCULUS
OCP HAP
BRUSHITE HAP & WHT
WHT
Anaerobic
condition
Mg Zn
carbon
ates
At pH of saliva
23. LIGHT MICROSCOPY
Calculus tooth interface is smooth
External mineralized surface is irregular
Covered by non mineralized plaque
Contain many non mineralized lacunae
STRUCTURE
24. TRANSMISSIONELECTRONMICROSCOPY
The mineralized intermicrobial areas of the body of the calculus
contained predominantly small, randomly orientated needle-
shaped/platelet-shaped crystals (a).
Areas containing crystals of larger columnar and roof-tile shapes were
also observed (b)
25. SCANNING ELECTRON MICROSCOPY
Appeared in one piece with a relatively smooth surface.
Under low magnification - thin at the incisal/occlusal part and
thickened apically.
Under high magnification - covered with dense layer of filament
(1micron thick with an estimated length of 25 to 100 microns.)
Fracture surface of Supragingival calculus generally had a smooth,
crystalline appearance.
26. X-ray BeamDiffraction Analysis
DISTRIBUTIONOFCALCIUMPHOSPHATECOMPOUNDS
OCP - detected near the superficial layer always in contact with
saliva
HA was the main component - Middle layer of the calculus .
WL - adjacent to the gingival and subgingival calculus.
Brushite - very rare ; adjacent to the gingiva.
28. COMPOSITION
Similar to supragingival calculus except that it has higher
concentration of-Ca,Mg,Fl.
Ca:P ratio is higher
Na content increases with depth of periodontal pocket
Salivary proteins are absent.
Supragingival & subgingival calculus contains 37% & 58% mineral
content by volume respectively
29. CRYSTALS
Whitlockite – mainly found
Same HAP, more WL, less Brushite and OCP as compared to
supragingival calculus
WL to HAP ratio is higher
30. LIGHT MICROSCOPY
Unlike supragingival calculus, lacunae of stained organic material
were not seen within the body of subgingival calculus.
The calculus surface previously in contact with the tooth was usually
flat and mineralized
The external/oral surface was fairly regular and covered by a non-
mineralized plaque layer of variable thickness
31. TRANSMISSIONELECTRONMICROSCOPY
The calcification - more homogeneous and
consisted of small randomly orientated needle- and
platelet-shaped crystals (a).
Areas with flat "bulk-shaped" crystals seen [as
described by Sundberg & Friskopp (1985),] within
which were fewer bacterial cell structures (b).
32. SCANNING ELECTRONMICROSCOPY
Under low magnification - clusters of small
deposits in the incisal/ occlusal part and larger
deposits that tend to fuse in apical part.
High magnification - subgingival fracture
surface were rougher than supra gingival,
grooves and holes that gave sub gingival
fracture a ‘worm eaten’ look. Filaments did not
dominate the surface of subgingival calculus
and no pattern of orientations were seen
33. X-RAY BEAMDIFFRACTIONANALYSIS
In subgingival calculus - OCP is scarcely found.
The main constituent is WL and HAP.
Brushite is totally absent
34. PREVALENCE
Subgingival calculus - interproximal surface ; least- buccal
surfaces.
Maxillary incisors and bicuspids - least involved.
Supragingival calculus starts forming with 6 years of eruption age
while Subgingival at 8 yrs of age ; Subgingival calculus is least
before 20 yrs of age.
Deposition of supragingival calculus - maximal scores around 25
to 30 yrs. of age; By age 45 only a few teeth ,typically the
premolars were without calculus
By age 30 - all surfaces of all teeth had subgingival calculus
without any pattern of predilection.
35. RATE OF FORMATION
Plaque mineralization begins within 24-72 hrs and takes an average of
12 days to mature.
Soft plaque is hardened by mineralization between 1st and 14th days
of plaque formation.
Calcification is reported to occur in as little as 4-8 hrs. (Tibetts 1970)
Calcifying plaque may become 50% mineralized in 2 days and 60%
to 90%mineralization in 12 days
36. All plaque does not necessarily undergo calcification.
Calculus is formed in layers which are often separated by a thin
cuticle that becomes embedded in calculus as calcification
progresses.
Plaque has the ability to concentrate calcium at 2 to 20 times its
level in saliva.
37. The initiation of calcification and the rate of calculus accumulation
vary from person to person for different teeth and at different times
of same person
According to this they are classified as heavy, moderate or slight
calculus former
(Muhler and Ennever 1962)
slight moderate heavy
38. Early plaque of heavy calculus former - more calcium, three
times more phosphorous and less potassium than that of non-
calculus former
Total protein and total lipid levels - elevated in Heavy calculus
formers.
Light calculus formers - higher levels of parotid
pyrophosphate.
The average daily increment in calculus former- 0.10% to
0.15% of dry weight
The time required by calculus to reach the maximal level has
been reported as 10 weeks(Conroy 1968) and 6 months.(Volpe
1969)
39. MICROBIOLOGY OF DENTAL CALCULUS
Lustman et al, (1976) In SEM, noted the presence of calcified masses
having a spongy appearance and containing empty spaces representing the
former sites of degenerated organisms.
Friskopp & Hammarstrom (1980) With TEM & SEM found differences in
the nature of the microbial coverings.
* On supragingival calculus filamentous organisms, oriented at right
angles to the surface dominated,
* Subgingival calculus was covered by cocci, rods and filaments with no
distinct pattern of orientation.
40. CALCULUS ATTACHMENT
Attachment by
means of organic
pellicle on enamel
Mechanical
interlocking in
cemental resorption
lacunae
Close adaptation of
calculus
undersurface
depressions to
gently sloping
mounds on the
unaltered
cementum surface.
Penetration of
calculus bacteria in
cementum. But this
mode of attachment
was not
acknowledged
THEFOLLOWING4 MODESOF ATTACHMENTHASBEENDESCRIBED:-
41. ATTACHMENT OF CALCULUS ON IMPLANT
Attachment to pure titanium is less intimate than to root surfaces structure.
Smooth machined implants have less micro porosities for retention.
(This would mean that calculus may be chipped off from implants without affecting it)
Matarraso etal 1996
42. ROLE OF MICRO-ORGANISMS IN MINERALIZATION
Mineralization of plaque starts both extracellulary & intracellulary by gram +ve
and –ve microorganisms.
Filamentous organisms,diptheroids,bacterionema and vellionella species.
Bacterial plaque may actively participate in the mineralization of calculus by
forming phosphates, which changes the Ph of plaque and induces mineralization.
43. Theories of mineralization
TWOPRINCIPALCATEGORIES
a) Mineral precipitation results from local rise in the degree of saturation
of Ca and P ions and may be due to rise in ph.
b) Seeding agents induces small foci of calcification that enlarge and
coalesce to form a calcified mass.
44. FEW PROPOSED THEORIES ARE:
1. Booster mechanism
2. Epitactic concept
3. Inhibition theory
4. Transformation theory
5. Bacterial theory
6. Enzymatic theory
45. BOOSTER MECHANISM
Calcification will occur in a particular locus when local pH +
calcium and phosphorous concentrations precipitation of a
calcium phosphate salt.
Factors such as
1. loss of CO2 & production of ammonia could account for an
elevation in pH;
2. Acid or alkaline phosphatase activity could result in a higher
phosphate concentration;
3. Liberation of bound or complexed calcium from the salivary
proteins would produce higher calcium levels.
46. Saliva –
CO2 tension= 54- 65 mmHg
Atmosphere CO2 tension= 0.3
mmHg
CO2
CO2
CO2
Increase in salivary pH
Dissociation of phosphoric
acid
Phosphate ions
Calcium phosphate crystal
formation
BOOSTER THEORY
48. EPITATIC THEORY
Seeding agents induce small foci of calcification enlarge and coalesce to form the
calcified mass.
Intercellular matrix or plaque plays an important role. Carbohydrate protein
complexes initiates the calcification by removing calcium from saliva by
chelation and binds with the nuclei that induce subsequent deposition of minerals.
Epitactic refers to crystal formation through seeding by another compound which
is similar to hydroxyapatite crystals leading to precipitation of calcium salts from
the metastable solution of saliva.
49. NUCLEATING MOLECULES
Some types of collagen and proteoglycans (Boskey 1981).
Calcium –phospholipid-phosphate complexes are
important nucleators in numerous calcifications including
calculus.(Bosky et al in 1981)
Bacteria are thought to be important nucleators( Ennever et
al in 1976)
50. INHIBITION THEORY
Calcification at specific sites - because of inhibiting mechanism at
non-calcifying sites.
The sites where calcification occurs , the inhibitor is apparently
altered or removed.
Possible inhibiting substance- pyrophosphate & other
polyphosphates.
Among controlling mechanisms is the enzyme alkaline
pyrophosphatase - hydrolyze the pyrophosphate phosphate
(Russell and Fleisch 1970).
Pyrophosphate inhibits calcification - prevents the initial nucleus from
growing, possibly by poisoning the growth centers of the crystals
51. TRANSFORMATION THEORY
Hypothesis - hydroxyapatite need not arise exclusively via
epitaxis or nucleation.
Amorphous non-crystalline deposits and brushite can be
transformed into octacalcium phosphate and then to
hydroxyapatite (Eanes et al 1970).
It has been suggested that controlling mechanism in
transformation mechanism can be pyrophosphate (Fleisch et al
1968).
52. BACTERIOLOGICAL THEORY
Oral microorganisms are the primary cause of calculus, and that
they are invovled in its attachment to the tooth surface.
Leptotrichia and Actinomyces have been considered most often
as the causative microorganism.
53. ENZYMATICTHEORY
Calculus formation is the resultant of the action of
phosphatases derived from either oral tissues or oral
microorganism on some salivary phosphate containing
complex,most probably phospheric esters of the
hexophosphoric group.(Adamson.KT 1929)
54. DIAGNOSTIC AIDS
Visual examination
Gentle air blast
Transillumination
Gingival tissue color change
Tactile examination
Probe
Explorer
Radiographs
56. Highly calcified interproximal calculus deposits - detectable as
radioopaque projections
However, the sensitivity level of calculus detection by radiographs
is low.
The location of calculus does not indicate the bottom of the
periodontal pocket because the most apical plaque is not sufficiently
calcified to be visible on radiographs.
Radiograph
58. Concept of nanobacteria
Cifecioglu et al 2003 &Demir T 2008
stated that nanobacteria may be present in dental calculus and may play
a role in calcification of dental calculus.
Nanobacteria may be considered as a risk factor for the periodontal
disease.
Zang et al found nanobacteria from the crevicular fluid of patients
with chronic periodontitis and stated that it can be cultured and
identified from dental calculus too.
59. Role of calculus in periodontal disease summarized as:
• Brings plaque bacteria close to supporting tissues.
• Provides fixed nidus for plaque accumulation.
• Interferes with local self cleansing mechanisms.
• Reservoir for substances like endotoxins, antigenic materials and
bone resorbing factors because of its permeability and porous
nature.
60. ORAL HYGIENE AND THE CONTROL OF
CALCULUS
TOOTHBRUSHING
Toothpaste abrasives may interfere with supragingival calculus
formation, either by removal of the matrix for the deposition of
salts or removal of the calculus in the early stages of calcification.
Using a quantitative scoring procedure, Villa in 1968 was able to
demonstrate that thorough brushing alone could reduce calculus
formation by as much as 50 percent on the lingual surfaces of the
lower anterior teeth.
61. SCALING AND ROOT PLANING
It is the most commonly practiced therapeutic intervention for
calculus formation.
Scaling and root planing is done to remove plaque and
calculus from crowns and root surface of teeth.
Sickles, curettes and ultrasonic and sonic instruments are most
commonly used for the removal of calculus.
62. Laser
Laser most commonly used in periodontal therapy include
1. Semiconductor diode laser(gallium,arsenide,alluminium)
2. Solid state laser such as Nd:YAG(neodenium doped-yttrium
aluminium garnet),Er:YAG &
Er,Cr:YSGG(yttrium,scandilium,garnet,galium)
3. Carbon dioxide laser
Among all lasers - Er:YAG laser is most suitable for the non
surgical periodontal debridement.
67. Earliest techniques - wooden stick + aromatic sulphuric acid &
introduced into a periodontal pocket to dissolve calculus(Barker
1872).
Niles (1881) - the nitro muriatic acid.
Other acids included - 20% trichloroacetic acid, bifluoride of
mercury and 10% sulphuric acid.
Disadvantages:
i. Caustic to soft tissues
ii. Decalcify tooth structure. (Stones (1939) and grossman (1954)
so their use was discontinued
ACIDS
68. ALKALIS
Badanes (1929) argued that it was the action of the mild alkalis
contained in the waters that dissolved the principal organic
constituents of salivary calculus.
These findings agreed with those of Prinz (1921), but the idea failed
to find support.
69. CHELATING AGENTS
These chemicals remove calcium from solution.
• Sodium hexametaphosphate was found to remove
supragingival calculus from extracted teeth in 10 to 15 days
(Kerr & Field 1944).
• Warren et al. (1964) exposed extracted teeth to a saturated
solution of sodium hexametaphosphate for 24 h and found a
large reduction in the hardness of the cementum and the
decalcification of the calculus was less than that of cementum.
Because of this nonspecific demineralization effect, the use of
chelating agents in anticalculus dentifrices ceased.
70. EDTA
Jabro et al. (1992) found that application of EDTA gel
(SofscaleTM) resulted in ease of calculus removal.
However, subsequent studies by Maynar et al. (1994), Smith et al.
(1994), Harding et al.(1996) and Nagy et al. (1998) have failed to
confirm this effect.
Smith et al. (1994) noted that sufficient time has to be allowed for
the gel to penetrate the bulk of the calculus deposit and this may
negate the reason for using it.
71. ENZYMES
Mode of action – 1.To break down plaque matrix OR
2. To affect the binding of the calculus to the tooth.
The first enzyme to be tested- mucinase (Stewart 1952)Calculus
formation reduced & calculus formed was softer and more easily
removed (Stewart 1952).
Aleece & Forscher (1954) - introduced mylase.
Enzyme with high proteolytic and low amylase activity- most
effective inhibitor of calculus formation. Draus et al. (1963)
Dehydrated pancreas (Viokase) - tested on the basis of a high
proteolytic enzyme activity - reduce calculus formation by 60%
(Jensen 1959).
Enzymes of fungal origin have also been tested.
72. Urea
The anticalculus effect - ability to dissolve the
mucoproteinaceous material within which the calcium salts are
deposited and/or by increasing the solubility of calcium salts in
saliva.
It was found that increasing the concentration of urea resulted in
progressive inhibition of calcium deposition.
A maximum inhibition of 70% was reached at a concentration of
30% urea.
Urea concentrations greater than 30% led to a progressive
decrease in inhibition.
73. But the addition of urea to the oral cavity result in ammonia
production via urease activity increases the pH of saliva and
plaque increase in calculus deposition.
Then came into research, the concept of inhibiting urease
activity.
Ethanehydroxydiphosphonate (EHDP) or acetohydroxamic acid
(AHA) were tested for their anti calculus potential
74. Results demonstrated a significant reduction in calculus
formation in both the EHDP and AHA groups.
But such changes were not significant in humans. ( Son
&Muhlemann 1971)
This finding together with the observation that AHA had been
shown to increase caries (Regolati & Muhlemann 1971) led to a
decline in interest in AHA as an anticalculus agent.
75. MISCELLANEOUS CHEMICALAGENTS
Attempts have been made to prevent calculus deposition by
coating the teeth with adhesive to alter the binding of the calculus
to the tooth.
Dimethylpolysiloxane and cyanoacrylate monomer adhesive,- no
effect
Silicones- no effect
Lactone- effective but caused de-mineralisation of teeth.
Sulphonated polystyrene membrane – effective but temporary
76. Sodium ricinoleate - interferes with the attachment of
microorganisms to teeth. (Dossenbach & Muhlemann (1961)
The results showed almost total absence of microorganisms, and
calculus formation was almost totally inhibited.
Unfortunately, sodium ricinoleate had a particularly unacceptable
taste and needed to be applied at high concentrations.
77. Watt et al. (1993) postulated - changing the electrostatic nature of
the tooth surface in calculus prevention
The magnetic water was thought to bring Ca2 and PO4 ions closer
together, consequently reducing attachment.
The group using a magnetic water irrigator had 44% greater
reduction in calculus volume and a 42% greater reduction in
calculus area when compared with the group using an irrigator
with no magnetic water.
78. CALCIUM LACTATE
Schaeken et al. (1990) investigated a 5% calcium lactate solution on
calcium and phosphate levels in saliva.
The group using the dentifrices with calcium lactate had a 44%
reduction in calculus and those using the calcium lactate with sodium
lauryl sulphate had a 47% reduction in calculus with respect to the
control group.
The authors concluded that calcium lactate probably did not act as an
inhibitor of crystal growth but may offset secretion and activity of
salivary phosphoproteins.
79. ANTIMICROBIALS
Penicillin- no effect
Cetylpyridinium chloride- no effect
Chlorhexidine
Chlorhexidine is a cationic bis-biguanide which acts by being adsorbed
onto the bacterial cell wall, leading to damage of the permeability
barriers. At higher concentrations, precipitation and coagulation of the
cytoplasmic contents occurs (Hennessey 1977).
Many studies have confirmed that chlorhexidine is an excellent
antiplaque agent (Lo¨ e & Schiott 1970, Hamp et al. 1973, Tepe et
al.1983)
80. NIDDAMYCIN
Strong activity toward a variety of gram positive organisms;
streptococci, enterococci, corynebacteria, bacilli and certain
protozoas.
No known medical uses; not significantly absorbed orally or
systemically, and no in vivo bacterial resistance had been reported
(Stallard et al.1969).
Research into the use of Niddamycin as an anticalculus agent was
discontinued - concern over the development of bacterial cross
resistance to other antimicrobials.
81. TRICLOSAN
Triclosan ( trivial name of 2,4,4-trichloro-2-hydroxydiphenyl ether) a
non-ionic antibacterial agent with a wide spectrum of activity against
bacteria, fungi and yeasts.
When delivered from a dentifrice- seems to bind to oral mucous
membranes and tooth surfaces, and is particularly well retained in
plaque.
Triclosan is predominantly used in combination with other anti-
calculus
82. PVM/ MA copolymer
PVM/MA Copolymer is a copolymer of methyl vinyl ether and
maleic anhydride and is used as a binder.
Promotes uptake of triclosan by enamel and buccal epithelial
cells (Nabi et al., 1989).
Composed of two groups: an attachment group and a
solubilizing group.
The solubilizing group retains triclosan in surfactant micelles so
that the attachment group can have enough time to react with
tooth surfaces via calcium in the liquid adherent layer.
83. INHIBITORSOF MINERALISATION
Metals
Use of heavy metals - suggested by Hanke (1940) - in solution,
these metals suffered from having a disagreeable metallic taste, or
caused an unsightly discoloration of the teeth.
Mechanisms by which they can affect calculus formation:
i. Firstly, they inhibit plaque growth.
ii. Secondly, metal salts are potent inhibitors of mineralization
(Bachra & van Harskamp 1970, Thomas 1982).
Metal ions can bind to hydroxyapatite although this binding is
reversible.
84. ZINC IONS
ZINC ions
1. Reduce plaque acidogenicity (Opperman 1980)
2. Plaque growth (Saxton 1986)
It inhibits crystal growth by binding to the surface of solid Ca P
(Gilbert 1988)
Zn at a conc of 0.1mmol/L inhibits the formation of
DCPD,OCP and amorphous Ca P but at a higher conc of 0.5-2
mmol/L promotes the formation of amorphous CaP.
85. BISPHOSPHONATES
Bisphosphonates are a group of synthetic pyrophosphate analogues
thought to prevent calculus deposition by inhibiting crystal growth.
86. VITAMINC
Vitamin C is a surface active organophosphorus compound that
has been shown to be effective in inhibiting the in vitro
crystallization of calcium phosphate on to smears of
supragingival calculus (Turesky et al. 1965).
Vitamin C inhibits crystal growth by a crystal poisoning
mechanism.
87. Turesky et al.(1967) tested the efficacy of a chloromethyl analogue
of victamine C - victamine C solution reduced calculus deposition
by 46.8% compared to water controls.
Mechanism:
Vitamin C has a characteristic taste which might have
promoted saliva flow, thus reducing calculus levels.
(but Gilmore compared effect of quinine sulphate and vitamin C
and found quinine sulphate having similar taste did not inhibit
calculus formation)
88. Pyrophosphates
Pyrophosphate could prevent calcification by
1. Interrupting the conversion of amorphous calcium phosphate to
hydroxyapatite (Fleisch & Bisaz 1962
2. Inhibiting crystal growth
3. Reduce acquired pellicle formation.
Lower concentrations of pyrophosphate were noted in the parotid
saliva of calculus formers than in saliva of non-formers (Vogel &
Amdur 1967).
The concentration of pyrophosphate in the plaque of low calculus
formers was also significantly greater than that in heavy calculus
formers (Edgar & Jenkins 1972).
89. Pyrophosphate - binds to two sites on the HAP surface, and one
of the two sites needs to be bound by phosphate ion to permit
crystal growth to occur. If this site is bound by pyrophosphate,
phosphate ion cannot adsorb onto crystal, and thus crystal
growth is inhibited.
Pyrophosphate undergo rapid hydrolysis in the oral cavity by
bacterial and host phosphatases (Gaffar et al 1986)
The addition of co polymer PVM/MA is believed to prevent
this hydrolysis
91. CLINICAL MEASUREMENT
Two indices – quantitating calculus deposits
calculus component of OHI
calculus component of PI
Calculus surface index (Ennever 1961)
Marginal line calculus index (Muhlem 1967)
Volpe – manhold index (1965)
Calculus surface severity index
92. EFFECT OF MEDICATION
A quantitative recording of supragingival deposits among
systemically medicated and non-medicated patients presenting for
a routine dental examination and prophylaxis indicated the
following:
1) a tendency for more plaque and less calculus to form among the
older individuals (65 years and older) regardless of the use or non-
use of medication;
2) a statistically significant reduction of calculus among individuals
medicated with ß-blockers, diuretics, vitamin C, anticholinergics,
synthroid, or allopurinol despite the high quantity of plaque present.
3) neither the patient's sex nor the time interval between prophylaxis
are important factors in the quantity of calculus or plaque formed in
either medicated or non-medicated individuals
(Turesky etal1992)
93. CONCLUSION
While the bacterial plaque that coats the teeth is the
main etiologic factor in the development of
periodontal disease, the removal of subgingival
plaque and calculus constitute the cornerstone of
periodontal therapy.
Calculus plays an important role in maintaining and
accentuating periodontal disease by keeping plaque in
close contact with the gingival tissue and creating
areas where plaque removal is impossible. Therefore
the clinician must possess the clinical skill to remove
the calculus and other irritants as a basis for adequate
periodontal and prophylactic therapy.
94. REFERENCES:
CARRANZA –CLINICAL PERIODONTOLOGY 10TH ED
JAN LINDHE – CLINICAL PERIODONTOLOGY AND IMPLANTOLOGY 4TH ED
SUPRAGINGIVALCALCULUS: FORMATIONANDCONTROL(YE JIN)
SUPRAGINGIVAL CALCULUS AND PERIODONTAL DISEASE, PERIO2000
(ROBINM . DAVIESR, OGERP . ELLWOODA, NTHONYR . VOLPE&MARGAREET. P
ETRONE)
CALCULUS REVISITED:A review
,Mandei ID and Gaffar 249-257Periodontol J9S6;
ANTICALCULUS AGENTS
(Fairbrother KJ, Heasman PA: Anticalculus agents. J Clin Periodontol 2000; 27:285–
301. C Munksgaard, 2000.)
First person association between dental deposits and oral diseases can be found in the writings of Hippocrates (460-377 BC).They noted the deleterious effect of calculus (pituita) on gums and teeth.
It was Albucasis (936-1013), who clearly described the relation between calculus and disease and advocated thorough removal of deposits.
Paracelsus a swiss- german physician and alchemist introduced the term tartar as a designation for a variety of stony concretions that form in humans.
For nearly 5,000 years, calculus was considered to be the prime etioiogic agent in periodontal disease. In the past 25 years, however, calculus has been deposed by plaque, and the hardened criminal has come to be viewed as a fossilized remnant of minor significance.
Levels of calculus and location of formation are population specific and are affected by :
oral hygiene habits,
access to professional care,
diet,
age,
ethnic origin,
time since last dental cleaning,
systemic disease
the use of prescription medications.
Once highly mineralized, calculus can become cement-like in terms of both physical hardness (Vickers Hardness averaging 30-40 units, maximum observed =190) and adhesive strength.
Forces up to 2.0 kg are required for calculus removal during scaling.
(Dental calculus: recent insights into occurrence, formation, prevention, removal and oral health effects of supragingival and subgingival deposits. Eur J Oral Set 1997: 105: 508-522)
Supramarginal calculus/Coronal calculus/Salivary /Extragingival calculus
Location -The tightly adherent calcified deposits that form on the clinical crowns of the teeth above the free gingival margin.(visible in oral cavity)
Color -usually white-yellow in colour but can darken with age and exposure to tobacco
Texture and consistency –hard clay like consistency.
Easily detachable from tooth surface
Salivary secretions are the main source of mineral salts.
Lingual surface of mandibular anteriors and facial surfaces of maxillary 1st and 2nd molars.
Surfaces of dentures and dental appliances.
Crowns of teeth out of occlusion.
The concentration of phospholipids in heavy calculus formers is significantly higher than that of slight calculus former (Slomiany et al,1981)
Thus phospholipid plays an important role in calculus formation.
To END dis slide with- Generally two or more crystal forms are found in calculus.
When supragingival calculus ages, the amount of brushite declines as the amount of HAP,OCP&WHT increases..
At normal ph..ocp converts to hap
At low ph n high ca:p..brushite is formed
Which converts to hao n wl at high ph
n anaerobic condition n other element essential for wl formation
The ultrastructure of young and mature supragingival calculus was similar.
Channels of organic matrix containing non- mineralized areas were often observed extending into the calculus from the calculus/plaque interface (Fig. 3a).
Individual mineralized bacteria could also be observed within these generally non-mineralised areas (Fig. 3b and d).
Supragingival calculus always appeared in one piece with a relatively smooth surface.
Under low magnification the Supragingival calculus was thin at the incisal/occlusal part and thickened apically.
Under high magnification the Supragingival calculus is covered with dense layer of filament .These filaments were 1micron thick with an estimated length of 25 to 100 microns.
Fracture surface of Supragingival calculus generally had a smooth, crystalline appearance.
OCP was detected in the areas of supragingival calculus near the superficial layer always in contact with saliva
In the middle layer of the calculus HA was the main component .
Supragingival calculus adjacent to the gingival and subgingival calculus contain WL.
Bru in calculus is very rare and is found only in the supragingival calculus adjacent to the gingiva.
Submarginal calculus/Serumal calculus
Location-below the crest of marginal gingiva (not visible on routine examination)
Color-dark brown or greenish black
Texture and consistency-hard and dense crusty, spiny or nodular deposits
Firmly attached to tooth surface.
Crevicular fluid and inflammatory exudates are the main source of mineral salts.
Found on any root surfaces with a periodontal pocket.
Whitolockite is found mainly in subgingival calculus
Subgingival calculus has same HAP more WL, less BRU and OCP as compared to supragingival calculus
WL to HAP ratio is higher in subgingival calculus
The calcification within the body of subgingival calculus was more homogeneous than supragingival calculus and consisted of small randomly orientated needle- and platelet-shaped crystals (a).
Subgingival calculus usually appeared in band like clusters of deposits with varying sizes and rough surfaces.
Under low magnification it has complex appearance. There are clusters of small deposits in the incisal/ occlusal part and larger deposits that tend to fuse in apical part.
High magnification revealed that subgingival fracture surface were rougher than supra gingival grooves and holes that gave sub gingival fracture a ‘worm eaten’ look. Filaments did not dominate the surface of subgingival calculus and no pattern of orientations were seen
The supragingival calculus is more common in children compared to subgingival calculus
The subgingival calculus is generally slightly prevalant than supragingival calculus and it appears after the age of 40 years in 47-100% and increases with age.
The prevalance of both type of calculus is approx 3% higher in males than in females
All plaque does not necessarily undergo calcification.
Plaque that does not develop into calculus reaches a plateau of maximal mineral content within 2 days.
Calculus is formed in layers which are often separated by a thin cuticle that becomes embedded in calculus as calcification progresses.
Plaque has the ability to concentrate calcium at 2 to 20 times its level in saliva.
Calcification of plaque is delayed in children.(Turesky 1961)
In children, asthmatic form calculus as twice as other children.
Cigarette smokers accumulate more calculus than nonsmokers.
People who are fed with tube for long time develop heavy calculus in 30 days.
In B & C, less plaque tend to accumulate.
In the 10-15 age group, 43% of normal children and 90-100% of children with cyctic fibrosis and asthma have calculus.This clinical observation may reflect elevation in salivary calcium and phosphorus in children with these disease .(Wotman et al 1973)
Intro- Two modes of mineralization, type A and type B centers, have been distinguished ultra structurally.
In electron microscope - individual crystal appears as needlelike structures from 5-10 m long; plate-like and ribbon-like crystals also may be seen.
According to this theory, calcification will occur in a particular locus when the local pH and calcium and phosphorous concentrations are high enough to allow for precipitation of a calcium phosphate salt. Factors such as
loss of CO2
production of ammonia could account for an elevation in pH;
acid or alkaline phosphatase activity could result in a higher phosphate concentration;
liberation of bound or complexed calcium from the salivary proteins would produce higher calcium levels
Saliva in the major salivary ducts is secreted at a high CO2 tension, about 54 to 65 mm Hg, where as CO2 pressure in atmospheric air is only about 0.3 mm Hg.
Saliva emerging from the salivary ducts loses CO2 to the atmosphere as result of this large difference in CO2 tension.
Since pH in saliva depends largely on the ratio between bicarbonates and free carbonic acid, the pH in saliva will increase when CO2 escapes.
With rise in the alkalinity the dissociation of phosphoric acid increases thus increasing the concentration of less soluble secondary and tertiary phosphate ions.
This increase in phosphate ions leads to a situation where solubility product of calcium phosphate is exceeded and crystals form.
Carbonic anhydrase an enzyme present in the saliva may be involved in this reaction.
Ammonia formation from urea raises pH in vitro during periods of reduced salivary flow such as sleep .
This favors the precipitation of calcium phosphate.
Mandel and thompson 1967 found that rapid calculus producers have a higher than average urea concentrations in saliva which increases ammonia levels in plaque
The concentration of calcium and phosphate in saliva is not high enough to precipitate but is sufficient to support the growth of hydroxyapatite once an initial seed or nucleus is formed.
Inro - A number of nucleating molecules have been suggested including some types of collagen and proteoglycans (Boskey 1981).
Current evidences suggest that calcium –phospholipid-phosphate complexes are important nucleators in numerous calcifications including calculus.(Bosky et al in 1981)
Also bacteria are thought to be important nucleators( Ennever et al in 1976)
Another approach considers calcification as occurring only at specific sites because of existence of an inhibiting mechanism at non-calcifying sites.
The sites where calcification occurs , the inhibitor is apparently altered or removed.
One possible inhibiting substance is thought to be pyrophosphate and possible other polyphosphates.
Among the controlling mechanisms is the enzyme alkaline pyrophosphatase which hydrolyze the pyrophosphate to phosphate (Russell and Fleisch 1970)
The pyrophosphate inhibits calcification by preventing the initial nucleus from growing, possibly by poisoning the growth centers of the crystals
Visual examination:
Supragingival calculus and subgingival calculus just below the gingival margin can be easily visualized with good lighting.
Light deposits of supragingival calculus are often difficult to see when they are wet with saliva.
Compressed air may be used to dry supragingival calculus until it is chalky white and readily visible
Air may also be directed into the pocket in steady stream to deflect the marginal gingiva away from the tooth so that subgingival deposits near the surface can be seen.
Tactile exploration
Requires the skilled use of fine pointed explorer or probe.
The explorer is held with light but stable modified pen grasp.
The pads of the thumb and the middle finger should perceive the slight vibration conducted through the shank.
Method:
After the stable finger rest.
Tip of the instrument is inserted to the base of the pocket and light exploratory strokes are activated in vertical direction.
When calculus is encountered the tip is advanced apically until the termination of the calculus if felt on the root surface.
The distance between apical edge of the calculus and the bottom of the pocket ranges from 0.2 to 1.0 mm.
When proximal surfaces are explored the instrument tip should be extended at least halfway across the surface past the contact area.
Both supragingival calculus and subgingival calculus may be seen on radiographs
Highly calcified interproximal calculus deposits are readily detectable as radioopaue projections that protrude into the interdental space.
However, the sensitivity level of calculus detection by radiographs is low.
The location of calculus does not indicate the bottom of the periodontal pocket because the most apical plaque is not sufficiently calcified to be visible on radiographs.
Under the best of the circumstances, conventional oral radiography was a poor diagnostic method for the detection of calculus (Buchanan etal1987)
Significance of calclulus..acts as secondary etiologic factor
Supragingival calculus is less tenacious and less calcified than subgingival so easy to scale.
Adverse effect of scaling and root planing
Root surface loss
Patient discomfort
Solubilizing calculus and organic matrix
Inhibit plaque adhesion, formation and mineralization
Inhibition of crystal growth and nucleation inhibitors.
Earliest techniques utilized a wooden stick which was moistened with aromatic sulphuric acid and introduced into a periodontal pocket to dissolve calculus(Barker 1872).
Niles (1881) suggested the nitro muriatic acid.
advocated mild alkali for calculus removal but this idea was not supported.
An enzyme with high proteolytic and low amylase activity was the most effective inhibitor of calculus formation. Draus et al. (1963)
Then EHDP inhibits calculus formation in rats by working as a crystal growth inhibitor (Regolati et al. 1970, Briner et al. 1971).
came into research, the concept of inhibiting uAHA-7(CH3 CO-NHOH) is a potent, non-competitive, and almost irreversible, inhibitor of urease (Kobashi et al.1962).
rease activity, therefore reducing the amount of ammonia produced from urea.
The different responses between humans and the rats could be due to
(i) differences in the oral clearance of AHA, (ii) concentrations of the AHA used in the human experiment being 50% to 75% lower than in the rat experiment, (iii) differences in the inorganic phosphorous or urea content of saliva.
Niddamycin is a macrolide antibiotic.
It shows a strong activity toward a variety of gram positive organisms; streptococci, enterococci, corynebacteria, bacilli and certain protozoas.
No known medical uses; not significantly absorbed orally or systemically, and no in vivo bacterial resistance had been reported (Stallard et al.1969).
Significant reduction in calculus was found by numerous authors. Stallard et al. (1969) Volpe et al. (1970) Rokita et al. (1975)
Research into the use of Niddamycin as an anticalculus agent was discontinued - concern over the development of bacterial cross resistance to other antimicrobials.
Micelles-An electrically charged particle built up from polymeric molecules or ions and occurring in certain colloidal electrolytic solutions like soaps and detergents
The use of heavy metals to inhibit plaque formation was initially suggested by Hanke (1940) who also recognized that, in solution, these metals suffered from having a disagreeable metallic taste, or caused an unsightly discoloration of the teeth.
Mechanisms by which they can affect calculus formation. Firstly, they inhibit plaque growth.
Secondly, metal salts are potent inhibitors of mineralization (Bachra & van Harskamp 1970, Thomas 1982). The metal ion adsorbs to the surface of the growing crystal, and prevents the attachment of lattice ions. Consequently, crystal growth is slowed or inhibited. Metal ions can also bind to hydroxyapatite although this binding is reversible.
DCPD- dicalcium phosphate dehy
Kohut & Grossman (1986) tested a zinc chloride and sodium fluoride dentifrice for calculus inhibitory activity-41.1% reduction.
drate
Bisphosphonates are a group of synthetic pyrophosphate analogues which interact strongly with minerals (Fleish & Russell 1972), and are thought to prevent calculus deposition by inhibiting crystal growth.
Muhlemann et al. (1970) found that ethanehydroxy-diphosphonate ( EHDP) solution reduced calculus formation by 49% and by 16% in rapid and slow calculus formers respectively.
Pyrophosphate is a small molecule and has been reported to inhibit crystal growth by binding to the surface of crystal. Pyrophosphate binds to two sites on the HAP surface, and one of the two sites needs to be bound by phosphate ion to permit crystal growth to occur. If this site is bound by pyrophosphate, phosphate ion cannot absorb onto crystal, and thus crystal growth is inhibited.
Pyrophosphate undergo rapid hydrolysis in the oral cavity by bacterial and host phosphatases (Gaffar et al 1986)
The addition of co polymer PVM/MA is believed to prevent this hydrolysis
Dentrifice containing 3.3% pyrophosphate and PVM/MA significantly reduced calculus formation than pyrophosphate alone (Schiff 1992)
Theoretically, various anti-calculus agents, which were discussed above, can also be active against calculus formation on implant surfaces in addition to tooth surfaces