CONTENTS
Introduction
Definition
Analysis of calculus
- classification
- composition
Prevalence
Theories of formation
Development & mineralization
Intra oral distribution
3.
Localization &attachment of calculus
Detection of calculus
Assessment of calculus
Inhibition of formation of calculus
Clinical efficacy of anticalculus agents
Etiological significance
Conclusion
References
4.
INTRODUCTION
Dental calculus,or tartar as it is
sometimes called, is a deposit which
forms on the surfaces of the teeth.
Calculus consists of mineralized
bacterial plaque that forms on the
surfaces of natural teeth & dental
prostheses.
5.
This calculusplays an important role in
maintaining and accentuating
periodontal disease by keeping plaque
in close contact with the gingival tissue
& creating areas where plaque
removal is impossible. Therefore the
clinician must not only possess the
clinical skill to remove the calculus ,but
also must be conscientious about
performing this task
6.
Definition
Calculus isdental plaque that has
undergone mineralization.(Carranza)
When dental plaque calcifies , the
resultant deposit is called dental
calculus (Grant)
Mineralized dental plaque that is
permeated with crystals of various
calcium phosphates(Schroeder,1969)
7.
The calcifieddeposits
consists of mineralized
bacterial plaque that forms
on the surfaces of natural
teeth and dental
prostheses.
In 1683 Van Leeuwenhoek
described microorganisms
in tartar. He called them
‘animalcules’
8.
Origin ofthe word “Calculus”
According to Encyclopedia Britannia, "About 15 BC,
the Roman architect and engineer Vitruvius
mounted a large wheel of known circumference in a
small frame, in much the same fashion as the wheel
is mounted on a wheelbarrow; when it was pushed
along the ground by hand it automatically dropped a
pebble into a container at each revolution, giving a
measure of the distance traveled. It was, in effect,
the first odometer."
These odometers were used in taxi carriages. Each
time the wheel of the carriage turned, a pebble, a
calculus, dropped from a container into another. In
the end of the ride, the driver counted how many
pebbles had dropped, and that determined the price
of the transportation. This kind of usages of
pebbles gave the word Calculus its present
meaning.
9.
Any solidconcretion, formed in any
part of the body, but most frequent in
the organs that act as reservoirs, and
in the passages connected with them;
as, biliary calculi; urinary calculi, etc.
Urinary calculus
10.
Dental calculuscan be considered as
an ectopic mineralized structure.
(Math.) A method of computation; any
process of reasoning by the use of
symbols; any branch of mathematics
that may involve calculation
11.
ANALYSIS OFCALCULUS
Classification
According To Relation to the gingival
margin
for clinical convenience
Supragingival calculus (salivary)
Subgingival calculus (serumal)
12.
COMPOSITION
Varying amountsof inorg salts
deposited in an organic matrix.
Organic content (mature calculus)
- CHO & protiens in
complexes of glycoproteins,
mucoproteins
acid mucopolysaccharides
- desquamated epithelial cells,
bacteria ,WBCs
13.
Between 1.9%and 9.1% of the organic
component is carbohydrate, which consists of
galactose, glucose, rhamnose, mannose,
glucuronic acid, galactosamine, and
sometimes arabinose, galacturonic acid, and
glucosamine.
Proteins from saliva contain most of amino
acids
Lipids as cholesterolesters,
phospholipids,free fatty acids &neutral fats
Little et al 1964,66; CHO-1-9%
PROTIENS-30-40%
LIPIDS-0.2-0.5%
Electron microscopy& x-ray diffraction
studies,4 distinct phosphate crystals
In descending order of % composition
HA- Ca10(PO4)6 (OH )2 58%
Whitlockite Ca21(PO4)14 21%
Octacalcium phosphate 12%
Ca8H2(PO4)6 6 H2O
Brushite CaHPO4 2 H2O 9%
Trace amounts of Monetite & calcite
16.
composition
Different layersof same calculus has
different compositions
Supragingival calculus – clearly built
up in layers & yields a great
heterogeneity from one layer to
another with regard to mineral content.
On average, mineral content-37%
ranges from – 16-51%
some layers max density – 80%
17.
Exterior layers– OCP
Inner layers – HA
Proportion of crystal present in a
deposit influenced by many factors
(Schroeder &Bambauer ’66,
Schroeder ’69,Schwartz & Masler’71)
18.
Dynamic translationof mineral deposits in
calculus
Early calculus & brushite &
supra gingival deposits OCP
Posterior & whitlockite
Sublingually
Early –brushite,
Later- OCP,
final –HA &W
19.
Sub gingivalcalculus , some what
more homogenous with equally high
density of minerals.
On ave, density -58%
Ranges from – 32-78%,
max value-60-80%
Predominant mineral –HA, W
Ca:P, Na increases
20.
PREVALENCE
2 nationalsurveys –prevalence of calculus
in children.
O’Brien 1993
Bhat 1991
The third National Health and Nutrition
Examination Survey (NHANES) evaluated
9689 adults in the United States between
1988 and 1994.This survey revealed that
91.8% of the subjects had detectable
calculus and 55.1% had subgingival
calculus.
21.
Anerud ,Löe& Boysen 1991-
longitudinal study observed the
periodontal status of a group of Sri
Lankan tea laborers and a group of
Norwegian academicians for a 15-year
period.
22.
THEORIES OF CALCULUS
FORMATION
Salivary pH theory
Burchard 1895
Rapp 1946
Hodge & Leung 1950
Bacteriologic theory
Goodrich & Moseley 1916
Bulleid 1925,’54,
Naeslund 1925,’26- most comprehensive study
Bibby ’35
Yardeni ’48,Zander ‘60
23.
Physicochemical thoery
Prinz ’21
Enzymatic theory
Phosphatse
Adamson 1929 – gingival tissue
Smith 1930 – epithelium of gingiva
Zander 1941 – endothelial cells of
capillaries & in few CT fibres
Esterase
24.
Epitactic theory
Mandel1957 –inter cellular matrix of
plaque
Active concept
Best supported
INHIBITION THEORY(Russel &
Fleisch,1970)
25.
DEVELOPMENT &MINERALIZATION
Plaqueacts as a scaffold for
calcification when Ca binds to the
organic matrix & ppt calcium
phosphate salts.
Inter cellular zones & bacterial
surfaces are the first sites of
crystallization. Later crystals form
within bacteria.
REVERSAL PHENOMENON
26.
The averagedaily increment in
calculus formers is from 0.10% to
0.15% of dry weight.
MINERALIZATION
27.
The followingfactors increase the rate of
calculus formation:
Elevated salivary pH
Elevated salivary calcium concentration.
Elevated concentration of protein and urea in
submandibular salivary gland secretions
Higher total salivary lipid levels
Elevated bacterial protein and lipid
concentration.
Low individual inhibitory factors.
28.
CALCIFICATION PROMOTERS
Urea-Urea is a product from the
metabolism of nitrogen-containing
substances. Urea can be secreted in
normal saliva at concentrations of
between 5 and 10 mmol/L but can be
as high as 30 mmol/L in patients with
renal disease
Gingival crevicular fluid contains up to
60mmol/L urea (Golub et al., 1971).
29.
urease isresponsible for bacterial urea
hydrolysis. At a neutral pH, urea is
hydrolyzed by urease to NH4
+
and
bicarbonate
30.
The effectof urea metabolism on
plaque pH
Ammonia produced from ureolysis of
urea contributes to an increased
plaque pH that is an essential factor in
natural calculus formation.
31.
Bacteria responsible forthe
ureolysis in dental plaque
Bacteria suspected of having a role in
ureolysis include S. salivarius,
coagulase-negative staphylococci,
Actinomyces viscosus/naeslundii
32.
Among theseureolytic bacteria,
S. salivarius has attracted the most
attention.
major contributor to ureolysis in natural
saliva .
33.
MODES OF ATTACHMENT&
LOCALIZATION
Zander ’54 described four methods of
attachment,Moskow ’69 suggested the
5th
method.
1.attachment of organic matrix of
calculus into minute irregularities that
were previously insertion locations of
sharpey’s fibres.
2. attachment into cemental defects
3. penetration of MO
34.
4. attachmentmediated by organic
pellicle
5.attachment to cemental tears and
separations.
35.
Localization
Localization :several theories –
localization of supra gingival calculus
in areas of buccal surfaces of upper
molars & lingual surfaces of lower
anteriors
Burchard 1895,
Everett ’56
Leung ’51
King ’54
36.
Low sucroseconc
High saliva film velocity
Higher resting plaque pH
Detection of subgingival calculus
Rationale
Clerehugh ’96 WHO # 621probe
Endoscopy
Electronic calculus detection
Magnification with eye loupes
Radiograph
piezoelectric ultrasonic handpiece with a
conventional scaler insert. The impulse response of
the mechanical oscillation system is analysed by a
fuzzy logic-based computerized algorithm, which
classifies various surfaces. Meissner G et al 2006
41.
Assessment Of Calcified
Deposits
Simplified calculus index (Green &
Vermillion ’64 )
Calculus component of periodontal
disease index (Ramfjord ’59)
Calculus surface index (Ennever J,,
Sturzenberger & Radike ’61)
Calculus surface severity index
(Ennever J et al ’61)
42.
Marginal linecalculus index
(Muhleman & Villa ’67)
Volpe- Manhold index (Volpe A R &
Manhold J H ’62)
43.
Inhibition Of FormationOf
Calculus
Anti calculus efficacy
Grossman ’54 & Gunson ’55
Harrison ’63 enzymatic preparations
Stallard et al ’69 & Volpe et al ’69
antimicrobials & antibiotics
Stookey et al ’89 cetyl pyridinium
chloride ,chlorhexidine & mixtures of
Cu salts
44.
Formation ofsupragingival calculus
may be prevented or controlled by
1.Anti microbial agents & enzymes
2. Anti adhesive agents
3. Crystal growth inhibitors (currently
dominating)
CALCULUS SOFTENING GEL
A calculus softening gel is currently
available that may enhance
periodontal instrumentation
effectiveness.
The active ingredient is disodium
ethylene diamine tetra acetic
acid(EDTA), which is a calcium-
chelating agent.
Mechanisms of Action
White ’92
Aspects Of Calculus Inhibition
1.Retention of calculus inhibitor
2.Prevention of deposit adhesion
3.Reducing localized increase in
supersaturation
52.
4. Impacton phase transformation
5.Activity against crystallite overgrowth
CLINICAL IMPLICATIONS
Wearhaug1956 surface roughness
alone does not initiate gingivitis
Calculus always covered by an
unmineralized layer of viable bacterial
plaque
57.
Listgarten &Ellegard 1973
Allen & Kerr 1965
Friskopp &Hammerström 1980
Nyman et al 1986,’88,
Mombelli ‘95
58.
CONCLUSION
While thebacterial 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.
59.
Calculus playsan 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.
60.
REFERENCES
Clinical Periodontology– Carranza 7th &
10th
edition
Clinical Periodontology and implant
dentistry– Lindhe 4th
edition
Contemporary Periodontics- Genco,
Goldman and Cohen 6th
edn
Periodontal therapy – Henry M Goldman
& Walter Cohen 6th
ed
61.
Periodontics Grant, Stern & Everett 5th
edn
Proceedings of the 2nd
european workshop
on periodontology – chemicals in
periodontics, 1996
Supra gingival dental calculus
Periodontology 2000; 8:125
Supra gingival calculus & periodontal
diseases Periodontology 2000;15:74