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Bone Composition and Structure

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Bone Composition and Structure

Comprehensive guide to bone composition, hierarchical organization, mineral and organic matrix components for basic science viva preparation

complete
Updated: 2024-12-24
High Yield Overview

BONE COMPOSITION AND STRUCTURE

Hierarchical Organization | 65% Inorganic | Type I Collagen | Lamellar Architecture

65%Inorganic (hydroxyapatite)
25%Organic (collagen, proteins)
10%Water
90%Type I collagen of organic matrix

BONE TYPES

Cortical (Compact)
Pattern80% mass, dense lamellar bone
TreatmentAppendicular skeleton, diaphyses
Cancellous (Trabecular)
Pattern20% mass, 80% surface area
TreatmentAxial skeleton, metaphyses

Critical Must-Knows

  • Bone is composite material - mineral provides stiffness, collagen provides toughness
  • Hydroxyapatite Ca10(PO4)6(OH)2 is the inorganic mineral phase
  • Type I collagen (90% of organic matrix) provides tensile strength
  • Lamellar bone is organized mature bone, woven bone is immature
  • Hierarchical structure: mineral crystals to lamellae to osteons to whole bone

Examiner's Pearls

  • "
    Bone mineral density increases with hydroxyapatite deposition
  • "
    Collagen fibril orientation determines mechanical anisotropy
  • "
    Osteoid is unmineralized organic matrix (14-day lag before mineralization)
  • "
    Cortical bone has lower remodeling rate than cancellous (3-5% vs 20-25% per year)

Clinical Imaging

Imaging Gallery

Bone microstructure of (a–c) Kansas Hesperornis tibiotarsus YPM 1491 and (d–f) Kansas Hesperornis femur YPM 1201. (a) Composite transverse section of tibiotarsus showing shape and general histology pa
Click to expand
Bone microstructure of (a–c) Kansas Hesperornis tibiotarsus YPM 1491 and (d–f) Kansas Hesperornis femur YPM 1201. (a) Composite transverse section of Credit: Wilson LE et al. via R Soc Open Sci via Open-i (NIH) (Open Access (CC BY))
Bone microstructure of Devon Island cf. Hesperornis femur (NUVF 286). (a) Composite transverse section of femur showing shape and general histology patterns. Scale bar, 5 mm. (b) Close-up of cortical
Click to expand
Bone microstructure of Devon Island cf. Hesperornis femur (NUVF 286). (a) Composite transverse section of femur showing shape and general histology paCredit: Wilson LE et al. via R Soc Open Sci via Open-i (NIH) (Open Access (CC BY))
Bone histology of the sacral supraspinous rod of Lithostrotia indet. MDT-Pv 4. (a) Complete cross section of the element. The areas occupied by bone tissue (white) and sediment (dashed lines) are show
Click to expand
Bone histology of the sacral supraspinous rod of Lithostrotia indet. MDT-Pv 4. (a) Complete cross section of the element. The areas occupied by bone tCredit: Cerda IA et al. via R Soc Open Sci via Open-i (NIH) (Open Access (CC BY))

Critical Bone Structure Exam Points

Composite Nature

Bone is a composite material combining mineral (stiffness) and organic matrix (toughness). Remove mineral and bone bends like rubber. Remove collagen and bone shatters like chalk. Both are essential.

Hydroxyapatite

Ca10(PO4)6(OH)2 is the key mineral. Calcium and phosphate ions substitute (carbonate for PO4, fluoride for OH) affecting bone quality. Fluoride increases density but brittleness.

Type I Collagen

90% of organic matrix is Type I collagen. Triple helix structure with crosslinks provides tensile strength. Collagen diseases (osteogenesis imperfecta) cause bone fragility.

Hierarchical Organization

Seven levels: mineral nanocrystals to collagen fibrils to lamellae to osteons to cortical/trabecular bone to whole bone. Defects at any level compromise strength.

At a Glance

Bone is a composite material comprising 65% inorganic mineral (hydroxyapatite Ca₁₀(PO₄)₆(OH)₂), 25% organic matrix, and 10% water. The mineral phase provides stiffness while Type I collagen (90% of organic matrix) provides tensile strength and toughness—remove mineral and bone bends like rubber; remove collagen and it shatters like chalk. The hierarchical organization spans seven levels from mineral nanocrystals to collagen fibrils to lamellae to osteons to whole bone. Cortical (compact) bone constitutes 80% of skeletal mass with slower remodeling (3-5% per year), while cancellous (trabecular) bone accounts for 80% of bone surface area with faster turnover (20-25% per year). Osteoid is unmineralized matrix with a 14-day lag before mineralization occurs.

Mnemonic

BONEBONE - Key Components

B
Both mineral and organic
Composite material - 65% mineral, 25% organic
O
Osteoid precedes mineralization
14-day lag from osteoid deposition to mineralization
N
Nanocrystals of hydroxyapatite
50nm × 25nm × 3nm crystals in collagen
E
Each lamella organized
Lamellar bone is organized mature bone

Memory Hook:BONE is both mineral and organic working together in organized layers

Mnemonic

COLLAGENCOLLAGEN - Organic Matrix

C
Crosslinks for strength
Pyridinoline and deoxypyridinoline crosslinks
O
One (Type I) is dominant
Type I collagen is 90% of organic matrix
L
Lamellae organization
Parallel collagen fibers in each lamella
L
Long triple helix
300nm tropocollagen triple helix
A
Aligned with stress
Collagen orientation follows mechanical loading
G
Glycine every third residue
Gly-X-Y repeat in collagen
E
Enzymatic crosslinking
Lysyl oxidase creates crosslinks
N
Non-collagenous proteins present
Osteocalcin, osteopontin, osteonectin

Memory Hook:COLLAGEN provides the organic scaffold with crosslinks for tensile strength

Overview

Bone is a specialized connective tissue that serves multiple functions: structural support, protection of vital organs, mineral homeostasis (calcium and phosphate reservoir), and hematopoiesis (bone marrow).

Why bone structure matters clinically:

Fracture Biomechanics

Understanding bone composition explains fracture patterns. High-energy trauma overcomes both mineral (compression) and collagen (tension) components. Osteoporotic bone has adequate mineral but poor microarchitecture.

Disease States

Osteogenesis imperfecta (collagen defect), osteomalacia (mineralization defect), and Paget disease (abnormal remodeling) all affect bone composition differently.

Composite Material Concept

Bone is nature's composite material combining the stiffness of mineral with the toughness of collagen. Remove the mineral (acid demineralization) and bone becomes flexible like rubber. Remove the collagen (heating) and bone becomes brittle like chalk. Both components are essential for normal mechanical properties.

Principles of Bone Composition

Hydroxyapatite: Ca10(PO4)6(OH)2

The mineral phase comprises 65% of bone weight and provides compressive strength and stiffness.

Crystal Structure

Chemical formula: Ca10(PO4)6(OH)2

Crystal dimensions:

  • Length: 50 nm
  • Width: 25 nm
  • Thickness: 2-3 nm
  • Hexagonal crystal structure

Location: Crystals deposit within and between collagen fibrils, aligned with fibril long axis.

Understanding crystal size and orientation is important for bone biomechanics.

Ion Substitutions in Hydroxyapatite

Common substitutions:

IonSubstitutes ForEffectClinical Example
Carbonate (CO3)Phosphate (PO4)Decreases crystallinity, increases solubilityNormal bone has 4-8% carbonate
Fluoride (F)Hydroxyl (OH)Increases crystallinity, decreases solubilityFluoride treatment for osteoporosis
Strontium (Sr)Calcium (Ca)May increase bone formationStrontium ranelate (historical osteoporosis drug)
Magnesium (Mg)Calcium (Ca)Affects crystal sizePresent in normal bone

Fluoride Effects

Fluoride substitutes for hydroxyl groups, creating fluorapatite which is more resistant to acid dissolution but also more brittle. High-dose fluoride treatment increases bone density but paradoxically increases fracture risk due to abnormal crystal structure.

Ion substitutions affect bone mineral quality and remodeling dynamics.

Mineralization Process

Osteoid mineralization lag time: 10-14 days

Mineralization Timeline

Osteoid DepositionDay 0

Osteoblasts secrete unmineralized organic matrix (osteoid). This layer is 10-15 micrometers thick at the mineralization front.

MaturationDays 1-10

Osteoid matures, collagen crosslinks form. Matrix vesicles (containing alkaline phosphatase) bud from osteoblasts.

Primary MineralizationDays 10-14

Rapid mineral deposition (70% of final mineral content). Matrix vesicles provide nucleation sites for hydroxyapatite crystals.

Secondary MineralizationMonths

Slow increase to 95% of final mineral content. Crystals grow and mature. Bone density increases.

Osteomalacia

Vitamin D deficiency impairs mineralization, leading to excess unmineralized osteoid. Bone is formed but not properly mineralized, resulting in soft, deformable bones (rickets in children, osteomalacia in adults).

The mineralization process is tightly regulated by osteoblasts and requires adequate calcium, phosphate, and vitamin D.

Organic Component - Matrix Proteins

The organic matrix comprises 25% of bone weight and provides tensile strength and toughness.

Type I Collagen - 90% of Organic Matrix

Structure:

  • Triple helix: two alpha-1(I) chains + one alpha-2(I) chain
  • Length: 300 nm (tropocollagen molecule)
  • Diameter: 1.5 nm
  • Gly-X-Y amino acid repeat (glycine every 3rd residue)

Assembly:

  1. Intracellular: Procollagen synthesis, hydroxylation (requires Vitamin C)
  2. Extracellular: Procollagen to tropocollagen (cleavage of N- and C-propeptides)
  3. Fibril formation: Tropocollagen self-assembles into fibrils (67 nm periodicity)
  4. Crosslinking: Lysyl oxidase creates covalent crosslinks (pyridinoline, deoxypyridinoline)

Osteogenesis Imperfecta

Osteogenesis imperfecta is caused by mutations in COL1A1 or COL1A2 genes, producing abnormal Type I collagen. This results in brittle bones with multiple fractures, blue sclerae, and hearing loss. The organic scaffold is defective despite normal mineralization.

Collagen provides the organic scaffold upon which mineral deposits.

Non-Collagenous Proteins - 10% of Organic Matrix

ProteinFunctionClinical Significance
OsteocalcinBinds calcium, regulates mineralizationSerum marker of bone formation
OsteopontinCell adhesion, inhibits mineralizationRegulates crystal size and growth
Osteonectin (SPARC)Binds collagen and mineralLinks organic and inorganic phases
Bone sialoprotein (BSP)Nucleation of hydroxyapatiteInitiates mineralization
Matrix Gla proteinInhibits mineralizationPrevents ectopic calcification

Osteocalcin is particularly important as a clinical marker. It is vitamin K-dependent (gamma-carboxylation of glutamate residues) and secreted by osteoblasts during bone formation.

Vitamin K and Bone

Vitamin K is required for gamma-carboxylation of osteocalcin. Vitamin K deficiency impairs osteocalcin function and may affect bone quality. Warfarin (vitamin K antagonist) may increase fracture risk with long-term use.

Non-collagenous proteins regulate mineralization and cell-matrix interactions.

Collagen Crosslinking

Enzymatic crosslinks (normal bone):

  • Lysyl oxidase converts lysine to allysine
  • Forms pyridinoline (PYD) and deoxypyridinoline (DPD) crosslinks
  • Mature, stable crosslinks increase tensile strength

Non-enzymatic crosslinks (advanced glycation end-products, AGEs):

  • Accumulate with aging and diabetes
  • Brittle, do not contribute to normal strength
  • Associated with reduced bone toughness

Diabetes and Bone Quality

Diabetes mellitus increases AGEs in bone collagen, reducing bone toughness despite normal or high bone mineral density. Diabetic patients have increased fracture risk independent of BMD.

Crosslink quality affects bone mechanical properties and fracture resistance.

Hierarchical Structure of Bone

Seven levels of organization: from nanoscale to whole bone level.

Hierarchical Levels of Bone Structure

LevelStructureSize ScaleKey Feature
1. MolecularTropocollagen + hydroxyapatite crystals1-100 nmMineral in collagen gap zones
2. NanoscaleMineralized collagen fibrils100-1000 nm67 nm periodicity (D-band)
3. SubmicronFibril arrays (lamellae)1-10 micrometersParallel fibers in each lamella
4. MicrostructureOsteons (Haversian systems)100-300 micrometersConcentric lamellae around central canal
5. MesostructureCortical vs trabecular bone0.1-1 mmDense vs porous architecture
6. MacrostructureWhole bone regions1-10 mmDiaphysis, metaphysis, epiphysis
7. OrganWhole bone10-100 mmIntegrated mechanical structure

Hierarchical Failure

Bone strength depends on integrity at all hierarchical levels. Osteoporosis (trabecular thinning at mesostructure level), osteogenesis imperfecta (collagen defect at molecular level), and osteomalacia (mineralization defect at nanoscale) all compromise bone strength through different mechanisms.

Understanding hierarchical structure explains how different diseases affect bone strength.

Cortical and Trabecular Bone

Longitudinal section of a long bone showing anatomical regions
Click to expand
Longitudinal section of a long bone (femur) demonstrating the key anatomical regions and structures. The proximal and distal epiphyses contain spongy (trabecular) bone with red bone marrow, capped by articular cartilage at the joint surfaces. The metaphyses contain the epiphyseal line (remnant of the growth plate) and trabecular bone. The diaphysis (shaft) consists of thick cortical (compact) bone surrounding the medullary cavity, which contains yellow bone marrow in adults. The periosteum covers the outer surface while the endosteum lines the medullary cavity. The nutrient artery penetrates the cortex to supply the bone marrow and inner cortex.Credit: OpenStax College via Wikimedia - CC BY 3.0

Cortical (Compact) Bone

Key characteristics:

  • 80% of skeletal mass
  • 20% of bone surface area
  • Porosity: 5-10%
  • Remodeling rate: 3-5% per year
  • Location: diaphyses of long bones, outer shell of all bones

Structure - Osteons (Haversian systems):

  • Central Haversian canal (blood vessels, nerves)
  • Concentric lamellae (4-20 layers)
  • Osteocyte lacunae and canaliculi
  • Cement line boundary
  • Diameter: 200-300 micrometers

Secondary osteons result from remodeling, surrounded by cement lines (reversal lines).

Cement Lines

Cement lines mark the boundary of remodeling cycles. They are hypermineralized and weaker than surrounding bone, serving as sites for crack initiation but also deflection (toughening mechanism).

Cortical bone provides mechanical strength and protection.

Trabecular (Cancellous, Spongy) Bone

Key characteristics:

  • 20% of skeletal mass
  • 80% of bone surface area
  • Porosity: 50-90%
  • Remodeling rate: 20-25% per year
  • Location: vertebrae, pelvis, metaphyses of long bones

Structure:

  • Network of interconnected struts (trabeculae)
  • Thickness: 50-300 micrometers
  • Oriented along stress lines (Wolff law)
  • Marrow spaces between trabeculae

Mechanical properties:

  • Lower modulus than cortical bone
  • Higher surface-to-volume ratio (more metabolically active)
  • Anisotropic (direction-dependent) strength

Osteoporosis

Osteoporosis affects trabecular bone earlier and more severely than cortical bone due to higher surface area and remodeling rate. Vertebral and hip fractures reflect trabecular bone loss.

Trabecular bone provides metabolic reserve and distributes loads.

Cortical vs Trabecular Comparison

FeatureCortical BoneTrabecular Bone
Mass proportion80%20%
Surface area proportion20%80%
Porosity5-10%50-90%
Remodeling rate per year3-5%20-25%
Primary locationDiaphyses, outer shellMetaphyses, vertebrae
Primary functionMechanical strengthMetabolic reserve

The higher remodeling rate of trabecular bone makes it more responsive to metabolic changes but also more vulnerable to resorptive diseases.

Lamellar versus Woven Bone

Lamellar vs Woven Bone

FeatureLamellar Bone (Mature)Woven Bone (Immature)
Collagen organizationHighly organized, parallel fibersRandom, disorganized fibers
Formation rateSlow (1-2 micrometers/day)Rapid (4-6 micrometers/day)
Mechanical strengthHighLow
Osteocyte densityLowHigh
When presentNormal adult bone, remodelingFracture callus, fetal bone, Paget disease

Lamellar bone:

  • Organized structure with collagen fibers parallel within each lamella
  • Alternating fiber orientation between lamellae (plywood-like)
  • Slow deposition allows optimal organization

Woven bone:

  • Rapidly formed during fracture healing
  • Disorganized collagen orientation
  • Weaker and more flexible than lamellar bone
  • Remodeled to lamellar bone over months

Paget Disease

Paget disease produces abnormal bone with both woven and lamellar patterns (mosaic pattern). The rapid, disorganized remodeling produces weak bone despite increased density. Jigsaw puzzle appearance on histology.

Understanding lamellar versus woven bone helps interpret fracture healing and bone pathology.

Clinical Relevance and Applications

Understanding bone composition and structure directly informs clinical decision-making in orthopaedic practice.

Clinical Correlations of Bone Structure

Structural LevelDisease/ConditionClinical Implication
Mineral phaseOsteomalacia/RicketsVitamin D supplementation, correct underlying cause
Collagen (organic)Osteogenesis imperfectaBisphosphonates, fracture prevention, genetic counseling
Trabecular microarchitectureOsteoporosisAntiresorptive therapy, fracture risk assessment
Cortical porosityAge-related bone lossMonitoring with DXA, fall prevention
Remodeling cyclePaget diseaseBisphosphonates to normalize remodeling

Implant Considerations

Bone quality affects implant fixation. Osteoporotic bone has reduced holding power for screws (trabecular loss reduces surface area for fixation). Cortical bone provides better screw purchase than cancellous bone. Consider cement augmentation or alternative fixation strategies in poor quality bone.

Fracture Healing Implications

  • Woven bone forms first in fracture callus
  • Remodeling to lamellar bone takes 12-18 months
  • Smoking impairs collagen synthesis
  • Vitamin D deficiency delays mineralization
  • NSAIDs may inhibit bone healing

Surgical Planning Applications

  • Assess bone quality on preoperative imaging
  • Cortical thickness guides plate selection
  • Trabecular patterns influence screw trajectory
  • Bone density affects implant choice
  • Consider bone grafting for defects

Evidence Base

Bone as Composite Material

5
Currey JD • J Bone Miner Res (2003)
Key Findings:
  • Bone mineral provides stiffness and compressive strength
  • Collagen provides tensile strength and toughness
  • Removing mineral makes bone flexible (elastic modulus drops 95%)
  • Removing collagen makes bone brittle (fracture toughness drops 60%)
Clinical Implication: Both mineral and organic components are essential for normal bone mechanical properties. Diseases affecting either component compromise bone strength.

Hierarchical Structure of Bone

5
Rho JY, Kuhn-Spearing L, Zioupos P • Med Eng Phys (1998)
Key Findings:
  • Seven hierarchical levels from nanoscale to whole bone
  • Mechanical properties emerge from organization at each level
  • Failure can initiate at any level depending on loading mode
  • Toughness mechanisms operate at multiple scales
Clinical Implication: Understanding hierarchical structure explains how different diseases affect bone strength through mechanisms at different scales.

Hydroxyapatite Crystal Structure in Bone

5
Weiner S, Wagner HD • Annu Rev Mater Sci (1998)
Key Findings:
  • Hydroxyapatite crystals are nanoscale (50×25×2-3 nm)
  • Crystals deposit in gap zones of collagen fibrils (67 nm periodicity)
  • Crystal orientation follows collagen fibril direction
  • Mineral-collagen interface is critical for mechanical properties
Clinical Implication: The nanoscale organization of mineral within collagen determines bone mechanical properties and explains mineralization disorders.

Basic Science Viva Scenarios

Practice these scenarios to excel in your viva examination

VIVA SCENARIOStandard

Scenario 1: Bone Composition (~3 min)

EXAMINER

"Describe the composition of bone and explain how each component contributes to its mechanical properties."

EXCEPTIONAL ANSWER
Bone is a composite material with three main components by weight: 65% inorganic mineral, 25% organic matrix, and 10% water. The inorganic phase is primarily hydroxyapatite, Ca10(PO4)6(OH)2, which provides compressive strength and stiffness. Hydroxyapatite crystals are nanoscale (50×25×2-3 nm) and deposit within collagen fibrils. The organic matrix is 90% Type I collagen, which provides tensile strength and toughness. Collagen molecules assemble into fibrils with 67 nm periodicity, and enzymatic crosslinks (pyridinoline, deoxypyridinoline) stabilize the structure. The remaining 10% of organic matrix consists of non-collagenous proteins like osteocalcin, osteopontin, and osteonectin, which regulate mineralization and cell-matrix interactions. The composite nature is critical: removing mineral makes bone flexible like rubber, while removing collagen makes it brittle like chalk. Both components working together provide bone's unique combination of stiffness and toughness.
KEY POINTS TO SCORE
Bone is 65% mineral, 25% organic, 10% water by weight
Hydroxyapatite Ca10(PO4)6(OH)2 provides stiffness and compressive strength
Type I collagen (90% of organic) provides tensile strength and toughness
Non-collagenous proteins (10% of organic) regulate mineralization
Composite nature essential - mineral alone is brittle, collagen alone is weak
Nanoscale mineral crystals deposit in collagen gap zones (67 nm periodicity)
COMMON TRAPS
✗Forgetting water as third component
✗Not explaining mechanical role of each component
✗Missing non-collagenous proteins
✗Not mentioning composite material concept
LIKELY FOLLOW-UPS
"What is the structure of hydroxyapatite?"
"What are the non-collagenous proteins and their functions?"
"How do collagen crosslinks form?"
VIVA SCENARIOChallenging

Scenario 2: Hierarchical Structure (~4 min)

EXAMINER

"Explain the hierarchical organization of bone from the molecular level to whole bone. How does this relate to fracture risk in osteoporosis?"

EXCEPTIONAL ANSWER
Bone has seven hierarchical levels of organization. At Level 1 (molecular), tropocollagen molecules (300 nm triple helices) combine with hydroxyapatite nanocrystals (50×25×2-3 nm). At Level 2 (nanoscale), mineralized collagen fibrils form with 67 nm periodicity. At Level 3 (submicron), fibrils organize into parallel arrays called lamellae (1-10 micrometers thick). At Level 4 (microstructure), lamellae arrange concentrically around central canals to form osteons (Haversian systems, 200-300 micrometers diameter). At Level 5 (mesostructure), we see cortical bone (dense, 5-10% porosity) versus trabecular bone (porous, 50-90% porosity). At Level 6 (macrostructure), different bone regions form (diaphysis, metaphysis, epiphysis). Finally, at Level 7 (organ), the whole bone integrates these structures. In osteoporosis, bone fails at multiple levels: trabecular thinning and loss of connectivity (Level 5), increased cortical porosity (Level 4), and altered collagen crosslinking (Level 2). This multi-level deterioration explains why osteoporotic bone fractures at lower loads than predicted by bone mineral density alone.
KEY POINTS TO SCORE
Seven levels: molecular to organ level
Level 1: Tropocollagen (300 nm) + hydroxyapatite crystals (50 nm)
Level 2: Mineralized fibrils with 67 nm periodicity
Level 3: Lamellae (parallel collagen arrays)
Level 4: Osteons (concentric lamellae, 200-300 micrometers)
Level 5: Cortical vs trabecular architecture
Level 6-7: Whole bone regions and organ
Osteoporosis affects multiple levels simultaneously
Trabecular thinning, cortical porosity, collagen changes all contribute
COMMON TRAPS
✗Not describing all levels systematically
✗Missing dimensions and size scales
✗Not linking to osteoporosis pathophysiology
✗Forgetting that osteoporosis is multi-level disease
LIKELY FOLLOW-UPS
"What is the diameter of an osteon?"
"Why does trabecular bone fail earlier in osteoporosis than cortical bone?"
"What are cement lines and why are they important?"

MCQ Practice Points

Bone Composition

Q: What is the approximate composition of bone by weight?

A: 65% inorganic mineral (hydroxyapatite), 25% organic matrix (90% Type I collagen), and 10% water. The inorganic phase provides stiffness and compressive strength, while the organic matrix provides toughness and tensile strength.

Hydroxyapatite Formula

Q: What is the chemical formula for hydroxyapatite, the primary mineral in bone?

A: Ca₁₀(PO₄)₆(OH)₂ - calcium phosphate hydroxide. Calcium and phosphate ions can be substituted (e.g., carbonate for phosphate, fluoride for hydroxyl) which affects bone quality. Fluoride increases density but also increases brittleness.

Cortical vs Cancellous Bone

Q: What is the key difference between cortical and cancellous bone in terms of remodeling rate?

A: Cortical bone: 3-5% annual turnover rate, comprises 80% of skeletal mass Cancellous bone: 20-25% annual turnover rate, comprises only 20% of mass but 80% of surface area

The higher surface area of cancellous bone explains its faster turnover and greater susceptibility to metabolic bone diseases.

Osteoid Mineralization

Q: What is the typical lag time between osteoid deposition and mineralization?

A: 10-14 days. Osteoid is unmineralized organic matrix secreted by osteoblasts. The mineralization lag time is clinically relevant - increased lag indicates osteomalacia, while decreased lag may indicate impaired matrix maturation.

Australian Context

FRACS Examination Relevance

Basic Science Viva:

  • Bone composition is a core basic science topic
  • Expect questions on hydroxyapatite formula (Ca₁₀(PO₄)₆(OH)₂)
  • Know Type I collagen structure and crosslinks
  • Understand composite material concept (mineral vs collagen)
  • Hierarchical structure from nanoscale to whole bone

Key Examination Points:

  • 65:25:10 ratio (mineral:organic:water)
  • Collagen provides toughness, mineral provides stiffness
  • Cortical vs trabecular remodeling rates (3-5% vs 20-25%)
  • Osteoid mineralization lag time (10-14 days)
  • Woven vs lamellar bone characteristics

Common Questions:

  • Describe bone composition and mechanical implications
  • Explain hierarchical organization of bone
  • Compare cortical and cancellous bone properties
  • Discuss clinical correlations (OI, osteomalacia, osteoporosis)

Training Resources

RACS/AOA Resources:

  • Basic Science Module - Bone Biology
  • FRACS Part I study guides
  • AOA SET Curriculum - Musculoskeletal Science

Australian Textbooks:

  • Miller Review of Orthopaedics (Basic Science chapters)
  • FRACS Orthopaedic Basic Science Revision Guide

Key Learning Objectives:

  • Describe bone composition at molecular level
  • Explain hierarchical organization
  • Correlate structure with mechanical properties
  • Relate to clinical bone diseases
  • Apply principles to implant fixation

Clinical Applications in Australia

Bone Density Assessment:

  • DXA (Dual-energy X-ray Absorptiometry) widely used
  • Medicare rebates available for at-risk populations
  • Trabecular bone score emerging as adjunct measure

Osteoporosis Guidelines:

  • Osteoporosis Australia clinical guidelines
  • PBS subsidized bisphosphonates, denosumab, teriparatide
  • Falls prevention programs

Metabolic Bone Disease:

  • Vitamin D deficiency common in Australian population
  • Screening recommendations for at-risk groups
  • PBS subsidized vitamin D supplementation criteria

Management Algorithm

📊 Management Algorithm
Management algorithm for Bone Composition Structure
Click to expand
Management algorithm for Bone Composition StructureCredit: OrthoVellum

BONE COMPOSITION AND STRUCTURE

High-Yield Exam Summary

Composition by Weight

  • •65% inorganic (hydroxyapatite mineral)
  • •25% organic (90% Type I collagen + 10% non-collagenous proteins)
  • •10% water
  • •Composite material: mineral = stiffness, collagen = toughness

Hydroxyapatite Mineral

  • •Ca10(PO4)6(OH)2 chemical formula
  • •Crystal size: 50nm × 25nm × 2-3nm (nanoscale)
  • •Deposits in collagen gap zones (67 nm periodicity)
  • •Ion substitutions: carbonate, fluoride, strontium affect properties

Collagen and Organic Matrix

  • •Type I collagen = 90% of organic matrix
  • •Triple helix (two alpha-1, one alpha-2 chain), 300 nm length
  • •Crosslinks: pyridinoline and deoxypyridinoline (enzymatic)
  • •Non-collagenous: osteocalcin, osteopontin, osteonectin, BSP

Hierarchical Levels

  • •Level 1-2: Tropocollagen + crystals → mineralized fibrils (67 nm)
  • •Level 3-4: Lamellae → osteons (200-300 micrometers)
  • •Level 5: Cortical (dense, 80% mass) vs trabecular (porous, 80% surface)
  • •Levels 6-7: Whole bone regions and organ

Cortical vs Trabecular

  • •Cortical: 80% mass, 5-10% porosity, 3-5% remodeling/year
  • •Trabecular: 20% mass, 80% surface, 50-90% porosity, 20-25% remodeling/year
  • •Trabecular affected first in osteoporosis (higher surface area)
  • •Cortical provides strength, trabecular provides metabolic reserve

Key Clinical Correlations

  • •Osteogenesis imperfecta: Type I collagen defect (brittle bones)
  • •Osteomalacia: Mineralization defect (soft bones, excess osteoid)
  • •Osteoporosis: Multi-level failure (trabecular loss, cortical porosity)
  • •Paget disease: Woven bone mosaic pattern (weak despite high density)
Quick Stats
Reading Time78 min
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