Biomedical subjects

P Roschger

Publications and source records attributed to P Roschger.

At least 19 recordsLinked to original sources

PubMed2006

Bone osteonal tissues by Raman spectral mapping: orientation-composition.

Bone is a composite material with a hierarchical structure. Its strength depends on its structural and material properties. In the present study, Raman microspectroscopic and Imaging analyses were employed to study 12 osteons in tissue sections from the femoral midshaft of a healthy human female, with a spatial resolution of approximately 1mum. Spatial changes in amount of mineral and organic matrix, as well as the variation in the mineral content were determined, imaged, and plotted as a function of the polarization of incident light. The results showed that the prominent bands, such as nu(1) PO(4) and amide I, commonly used for the determination of mineral and organic compositions, are quite sensitive to the orientation and the polarization direction of the incident light. On the other hand, bands such as amide III, nu(2) PO(4) and nu(4) PO(4) are less susceptible to the orientational effects. As a result, exclusive consideration of the nu(1) PO(4) and amide I bands for the calculation of material properties might lead to erroneous conclusions. Amide III, nu(2) PO(4) and nu(4) PO(4) Raman bands should also be taken into consideration for compositional analysis of bone structures, especially ones with unknown orientational features. Moreover, the results of the present study demonstrate the versatility of the analytical technique, and provide insights into the organization of bone tissue at the ultrastructural level.

Bone Density↗

PubMed2006

Lead accumulation in tidemark of articular cartilage.

OBJECTIVE: Determination of the spatial distribution of the toxic element lead (Pb) and other trace elements in normal articular cartilage and subchondral bone from adult humans with no history of work-related exposure to Pb. METHODS: Four macroscopically normal femoral heads and three patellas were harvested from randomly selected forensic autopsies. All subjects died of acute illnesses, had no history of work-related exposure to Pb and had no metabolic bone disease. The elemental distribution of lead (Pb) together with zinc (Zn), strontium (Sr) and calcium (Ca) in the chondral and subchondral region was detected using high resolution synchrotron radiation induced micro X-ray fluorescence (SR mu-XRF) analysis. SR mu-XRF line scans in conventional and SR mu-XRF area scans in confocal geometry were correlated to backscattered electron (BE) images visualizing the mineralized tissue. RESULTS: In all samples, we found a highly specific accumulation of Pb in the tidemark, the transition zone between calcified and non-calcified articular cartilage. Pb fluorescence intensities in the tidemark, which is thought to be a metabolically active mineralization front, were 13-fold higher when compared to subchondral bone. Pb intensities in the subchondral region were strongly correlated with Zn, but were distinctly different from Ca and Sr. CONCLUSIONS: The finding of the highly specific accumulation of lead in the tidemark of human articular cartilage is novel. However at this point, the exact mechanisms of the local Pb accumulation as well as its clinical implications are unknown.

Calcium↗

PubMed2005

Association of COLIA1 Sp1 alleles with defective bone nodule formation in vitro and abnormal bone mineralization in vivo.

Previous work identified a G/T polymorphism affecting a Sp1 binding site in a regulatory region of the COLIA1 gene that predisposes to osteoporotic fractures by affecting bone strength through mechanisms that are partly independent of differences in bone mineral density (BMD). To clarify the mechanisms by which COLIA1 Sp1 alleles influence bone strength we used quantitative backscattered electron imaging (qBEI) to characterize bone mineralization in biopsy samples from subjects of different COLIA1 genotype and studied the ability of osteoblast-like cells cultured from subjects of different genotypes to form mineralized bone nodules. The qBEI analysis showed a significant (P = 0.014) reduction in mineralization in bone biopsies from G/T heterozygotes (n = 6) compared with G/G homozygotes (n = 7) and a significant increase in heterogeneity of mineralization (P = 0.017). The in vitro studies showed that osteoblasts derived from G/T heterozygotes (n = 5) were significantly less able to produce mineralized bone nodules than G/G homozygotes (n = 10) at all time-points examined (P < 0.0001). We conclude that carriage of the COLIA1 Sp1 "T" allele is associated with an impaired ability of osteoblast-like cells to form mineralized bone nodules in vitro and with abnormalities of bone mineralization in vivo. This suggests that the increased bone fragility in carriers of the COLIA1 Sp1 allele may result in part from defects in bone mineralization.

Aged↗

PubMed2005

Combined treatment with PTH (1-34) and OPG increases bone volume and uniformity of mineralization in aged ovariectomized rats.

The combination of PTH with OPG has been proposed as a potential therapy in patients with severe osteoporosis. In the present study, we examined the bone material of aged ovariectomized (OVX) rats treated either with PTH (1-34) or OPG alone or in combination of both. The micro- and nanostructural characteristics of the mineralized bone were evaluated using quantitative backscattered electron imaging (qBEI) and small-angle X-ray scattering (SAXS). Rats (n=68) were either sham-operated or ovariectomized (OVX) at the age of 3 months, and 15 months later, OVX animals were treated either with vehicle, OPG (10 mg/kg), PTH (80 microg/kg) or a combination of both during 5.5 months. All treatments were by subcutaneous injection, 3 days per week. Secondary metaphyseal spongiosa from distal femora was assessed for mineralized bone volume (BV/TV), for the mean Ca-concentration (Camean), the width of the bone mineralization density distribution (Cawidth), as well as the average mineral particle thickness parameter (T) and the degree of alignment of the mineral particles (rho). A remarkable increase of BV/TV up to 139% (P<0.001) was observed in the PTH-treated groups independently of OPG. Camean was slightly increased (+1.7%, P<0.05) in the OPG-treated group. Cawidth was reduced (-6.4%, P<0.01, and -8.9%, P<0.001) in animals treated with OPG and PTH+OPG, respectively. In contrast, Cawidth in sham-operated rats was 16.0% (P<0.001) higher than in OVX. The T parameter was not altered in the trabecular bone within the group of treated and untreated OVX rats. However, the non-ovariectomized animals exhibited a significantly lower T value (-7.1%, P<0.01) with respect to OVX. In conclusion, qBEI and SAXS data of OVX rats suggest that PTH alone was responsible for increase of bone volume, whereas OPG positively influenced the homogeneity and density of mineralization without affecting the nanostructure of the bone material.

Animals↗

PubMed2005

Two different correlations between nanoindentation modulus and mineral content in the bone-cartilage interface.

The biomechanical properties of the zone of calcified cartilage (ZCC) in articulating joints are of clinical relevance due to the role ZCC plays in load transfer from cartilage to bone. To determine the micron-level mechanical properties and their correlation to mineral concentration in the ZCC, we combined nanoindentation (for micrometer level stiffness E(r) and hardness H) and quantitative back-scattered electron imaging or qBEI (for micrometer level mean calcium concentration Ca(Mean)) to study the ZCC-subchondral bone junction in 3 embedded human patellae. Nanoindentation line scans were correlated to qBEI analysis in the ZCC. The correlation between local stiffness and local mineral content was different in calcified cartilage compared to bone. The stiffness and hardness of calcified cartilage was typically lower than subchondral bone for the same mineral content. ZCC showed a wider range of variation in calcium content (1-28 wt %) compared to subchondral bone (16-26 wt %). 2D material property maps of the ZCC were generated from the mechanical-mineral correlation, showing that bands of high and low stiffness were found between the bone and tidemark, and between the ZCC and the unmineralized cartilage.

Adult↗

PubMed2004

Synchrotron diffraction study of deformation mechanisms in mineralized tendon.

The high stiffness and toughness of biomineralized tissues are related to the material deformation mechanisms at different levels of organization, from trabeculae and osteons at the micrometer level to the mineralized collagen fibrils at the nanometer length scale. Quantitatively little is known about the sub-micrometer deformation mechanisms under applied load. Using a parallel-fibred mineralized tissue from the turkey leg tendon as a model for the mineralized collagen fibrils, we used in situ tensile testing with synchrotron x-ray diffraction to measure the average fibril deformation with applied external strain. Diffraction peak splitting occurred at large strains, implying an inhomogeneous elongation of collagen fibrils. Scanning electron microscopy measurements lead us to conclude that the inhomogeneous mineralization in mineralized tendon is at the origin of the high fracture strain.

Animals↗

PubMed2004

Normal mineralization and nanostructure of sclerotic bone in mice overexpressing Fra-1.

Increased bone mass due to elevated number of active osteoblasts has been reported for transgenic mice overexpressing the transcription factor Fra-1. To explore the potential of the anabolic action of Fra-1 in treatment of osteoporosis, we examined the integrity of bone matrix generated in Fra-1 transgenic mice. Femora from Fra-1 transgenic (Fra-1 tg) and wild-type littermates were analyzed for bone mineralization density distribution (BMDD) and nanostructure using quantitative backscattered electron imaging (qBEI) and scanning small angle X-ray scattering (scanning-SAXS), respectively. For comparison, we studied mice lacking c-Fos (Fos-/-), which develop osteopetrosis because of the absence of osteoclasts. Morphometrical analysis of metaphyseal spongiosa revealed an up to 5-fold increase in bone volume for Fra-1 transgenic compared to wild type. BMDD indicated a transient lower mineralization of bone for Fra-1 transgenic at 5 and 8 weeks, which became comparable to that of wild-type mice by 8 months. The homogeneity of mineralization was not altered in the Fra-1 transgenic mice at any ages examined. However, it was strikingly reduced in Fos-/- due to an abundance of hypermineralized cartilage. The bone nanostructure did not show abnormalities in Fra-1 transgenic or Fos-/-. These results provide a rationale for the development of therapeutic applications involving Fra-1-induced bone formation.

Animals↗

PubMed2003

Mineralized microstructure of calcified avian tendons: a scanning small angle X-ray scattering study.

The micrometer level spatial distribution of the size, shape, and orientation of mineral crystallites in the calcifying matrix of tendons near the edge of the mineralizing front was investigated by scanning small angle X-ray scattering using synchrotron X-ray radiation. Using a special microbeam arrangement enabling 20 microm beam resolution and short measurement times, linear diffraction scans were made on sections from the normally calcifying tendons (tibialis cranialis) from the domestic turkey, which calcify in the distal to proximal direction. A change in shape and arrangement of mineral crystals was observed within the first 200 microm of the mineralization front, and the mineral crystal distribution was highly anisotropic with crystals aligned parallel to the fiber axis. In a cross-section of the tendon cut at right angles to the fiber axis, the orientation distribution of crystals was not azimuthally symmetric, and showed a small but nonzero anisotropy and a continuous change in mean orientation angle across the width of the tendon cross-section.

Animals↗

PubMed2003

Targeted overexpression of vitamin D receptor in osteoblasts increases calcium concentration without affecting structural properties of bone mineral crystals.

Increased cross-sectional area and strength of long bones has been observed in transgenic mice with 2-fold (OSV9) and 3-fold (OSV3) elevation of osteoblast vitamin D receptor (VDR) levels. In the present study, mineralization density distributions, including typical calcium content (Ca(Peak)) and homogeneity of mineralization (Ca(Width)) of femoral bone and growth plate cartilage, were determined by quantitative backscattered electron imaging (qBEI). Fourier-transform infrared (FTIR) microspectroscopy was used to examine mineral content, collagen and crystal maturation, and scanning small angle X-ray scattering (scanning-SAXS) for studying mineral particle thickness and alignment. In addition, X-ray diffraction (XRD) of distal tibiae revealed mineral particle c-axis size. In trabecular bone, the increase in Ca(Peak) was significant for both OSV9 (+ 3.14%, P = 0.03) and OSV3 (+ 3.43%, P = 0.02) versus controls with 23.61 +/- 0.45 S.D. wt% Ca baseline values. In cortical bone, Ca(Peak) was enhanced for the OSV3 mice (+ 1.84%, P = 0.02) versus controls with 26.61 +/- 0.28 S.D. wt% Ca, and OSV9 having intermediate values. Additionally, there was significantly increased homogeneity of mineralization as denoted by a reduction of Ca(Width) (-8.4%, P = 0.01) in primary spongiosa. FTIR microspectroscopy, with the exception of an increased collagen maturity in OSV3 trabecular bone (+ 9.9%, P = 0.02), XRD, and scanning-SAXS indicated no alterations in the nanostructure of transgenic bone. These findings indicate that elevation of osteoblastic vitamin D response led to formation of normal bone with higher calcium content. These material properties, together with indications of decreased bone resorption in secondary spongiosa and increased cortical periosteal bone formation, appear to contribute to the improved mechanical properties of their long bones and suggest an important physiological role of the vitamin D-endocrine system in normal bone mineralization.

Animals↗

PubMed2003

Characteristics of mineral particles in the human bone/cartilage interface.

Bone and cartilage consist of different organic matrices, which can both be mineralized by the deposition of nano-sized calcium phosphate particles. We have studied these mineral particles in the mineralized cartilage layer between bone and different types of cartilage (bone/articular cartilage, bone/intervertebral disk, and bone/growth cartilage) of individuals aged 54 years, 12 years, and 6 months. Quantitative backscattered electron imaging and scanning small-angle X-ray scattering at a synchrotron radiation source were combined with light microscopy to determine calcium content, mineral particle size and alignment, and collagen orientation, respectively. Mineralized cartilage revealed a higher calcium content than the adjacent bone (p<0.05 for all samples), whereas the highest values were found in growth cartilage. Surprisingly, we found the mineral platelet width similar for bone and mineralized cartilage, with the exception of the growth cartilage sample. The most striking result, however, was the abrupt change of mineral particle orientation at the interface between the two tissues. While the particles were aligned perpendicular to the interface in cartilage, they were oriented parallel to it in bone, reflecting the morphology of the underlying organic matrices. The tight bonding of mineralized cartilage to bone suggests a mechanical role for the interface of the two elastically different tissues, bone and cartilage.

Bone and Bones↗

PubMed2003

Constant mineralization density distribution in cancellous human bone.

The degree of mineralization of bone matrix is an important factor in determining the mechanical competence of bone. The remodeling and modeling activities of bone cells together with the time course of mineralization of newly formed bone matrix generate a characteristic bone mineralization density distribution (BMDD). In this study we investigated the biological variance of the BMDD at the micrometer level, applying a quantitative backscattered electron imaging (qBEI) method. We used the mean calcium concentration (Ca(Mean)), the most frequent calcium concentration (Ca(Peak)), and full width at half maximum (Ca(Width)) to characterize the BMDD. In none of the BMDD parameters were statistically significant differences found due to ethnicity (15 African-American vs. 27 Caucasian premenopausal women), skeletal site variance (20 ilium, 24 vertebral body, 13 patella, 13 femoral neck, and 13 femoral head), age (25 to 95 years), or gender. Additionally, the interindividual variance of Ca(Mean) and Ca(Peak), irrespective of biological factors, was found to be remarkably small (SD < 2.1% of means). However, there are significant changes in the BMDD in the case of bone diseases (e.g., osteomalacia) or following clinical treatment (e.g., alendronate). From the lack of intraindividual changes among different skeletal sites we conclude that diagnostic transiliac biopsies can be used to determine the BMDD variables of cancellous bone for the entire skeleton of the patient. In order to quantify deviations from normal mineralization, a reference BMDD for adult humans was calculated using bone samples from 52 individuals. Because we find the BMDD to be essentially constant in healthy adult humans, qBEI provides a sensitive means to detect even small changes in mineralization due to bone disease or therapeutic intervention.

Adult↗

PubMed2001

Structural development of the mineralized tissue in the human L4 vertebral body.

Knowledge of the structural development of the human vertebrae from non-weight-bearing before birth to weight-bearing after birth is still poor. We studied the mineralized tissue of the developing lumbar L4 vertebral body at ages 15 weeks postconception to 97 years from the tissue level (trabecular architecture) to the material level (micro- and nanostructure). Trabecular architecture was investigated by 2D histomorphometry and the material level was examined by quantitative backscattered electron imaging (for typical calcium content, CaMaxFreq) and scanning small-angle X-ray scattering (for mean mineral particle thickness). During early development, the trabecular orientation changed from a radial to a vertical/horizontal pattern. For bone area per tissue area and trabecular width in postnatal cancellous bone, the maximum was reached at adolescence (20 years), while for trabecular number the maximum was reached at childhood (approximately 1 year). CaMaxFreq was lower in early bone (approximately 21 wt%) than in mineralized cartilage (approximately 29 wt%) and adolescent bone (approximately 23 wt%). In conclusion, the changes at the tissue level were observed to continue throughout life while the development of bone at the material level (CaMaxFreq, mineral particle thickness and orientation) is essentially complete after the first years of life. CaMaxFreq and mean particle thickness increase rapidly during the first years and reach saturation. Remarkably, when these parameters are plotted versus logarithm of age, they appear linear.

Adolescent↗

PubMed2001

Graded microstructure and mechanical properties of human crown dentin.

The mineralized tissue of intertubular dentin is a collagen-mineral composite with considerable local variations of mechanical properties. Area scans of human coronal dentin were made by complementary methods to investigate correlations between local mechanical properties and the density, size, and crystallinity of the mineral particles. Scanning images from the same specimen were collected with Fourier-transform infrared microspectroscopy in reflectance mode (FTIR-RM), small angle X-ray scattering (SAXS), quantitative backscattered electron imaging (qBEI), and Nanoindentation in an atomic force microscope. The mineral content of dentin was found to decrease and the thickness of mineral crystals to increase towards the dentin-enamel junction (DEJ). Hardness and elastic modulus both decreased towards the DEJ. In a correlation analysis, the mineral content and, even more, the thickness of mineral crystals were found as the best predictors of hardness. The dentin layer close to the DEJ corresponds to a local minimum in hardness and elastic modulus, a configuration known to be an effective obstacle for crack propagation. Hence, the observed variations of mechanical and structural properties in an area between 0 and 1.5 mm below the DEJ define crown dentin as a gradient material optimized for its mechanical function.

Crystallization↗

PubMed2001

Alendronate increases degree and uniformity of mineralization in cancellous bone and decreases the porosity in cortical bone of osteoporotic women.

The strength of bone is correlated with bone mass but is also influenced significantly by other factors such as structural properties of the matrix (e.g., collagen mutations) and the mineral. Changes at all levels of this organization could contribute to fracture risk. We investigated the effects of alendronate (Aln) treatment on the density of mineralization and the ultrastructure of the mineral/collagen composite, size and habitus of mineral particles in iliac cancellous bone, as well as on the porosity of iliac cortical bone from postmenopausal osteoporotic women. Twenty-four transiliac bone biopsies from Phase III Aln (10 mg/day) trials (placebo and Aln after 2 and 3 years of treatment, n = 6 per group) were studied. The mineral structure was investigated by quantitative backscattered electron imaging (qBEI) and by scanning small-angle X-ray scattering (scanning-SAXS). qBEI histograms reflect the bone mineralization density distribution (BMDD), whereas SAXS patterns characterize the size and arrangement of the mineral particles in bone. We found that: (i) the relative calcium content of osteoporotic bone was significantly lower than that of data-base controls; (ii) mineralization was significantly higher and more uniform after Aln treatment; (iii) size and habitus of the mineral particles was not different between placebo and Aln-treated groups; and (iv) the porosity of cortical bone was reduced significantly by Aln treatment. We conclude that Aln treatment increases the degree and uniformity of bone matrix mineralization without affecting the size and habitus of the mineral crystals. It also decreases the porosity of the corticalis. Together these effects may contribute to the observed reduction in fractures.

Alendronate↗

PubMed2001

Age- and genotype-dependence of bone material properties in the osteogenesis imperfecta murine model (oim).

Cortical mineralization of long bones was studied in collagen alpha2(I)-deficient mice (oim) used as a model for human osteogenesis imperfecta. Aspects of the age development of the mice were characterized by combining nanometer- to micrometer-scale structural analysis with microhardness measurements. Bone structure was determined from homozygous (oim/oim) and heterozygous (oim/+) mice and their normal (+/+) littermates as a function of animal age by small-angle X-ray scattering (SAXS) and quantitative backscattered electron imaging (qBEI) measurements. SAXS studies found anomalies in the size and arrangement of bone mineral crystals in both homozygous and heterozygous mice aged 1-14 months. Generally, the crystals were smaller in thickness and less well aligned in these mice compared with control animals. An increase in the mean crystal thickness of the bone was found within all three genotypes up to an age of 3 months. Vicker's hardness measurements were significantly enhanced for oim bone (homozygotes and heterozygotes) compared with controls. The microhardness values were correlated directly with increased mineral content of homozygous and heterozygous compared with control bone, as determined by qBEI analysis. There was also a significant increase of mineral content with age. Two possibilities for collagen-mineral association are discussed for explaining the increased hardness and mineral content of oim/oim bone, together with its decreased toughness and thinner mineral crystals. As a consequence of the present measurements, one model for oim bone could incorporate small and densely packed mineral crystals. A second model for possible collagen-mineral association in oim material would consist of two families of mineral crystals, one being smaller and the other being much larger than the crystals found in normal mouse long bones.

Age Factors↗

PubMed2000

Analysis of the hierarchical structure of biological tissues by scanning X-ray scattering using a micro-beam.

The outstanding mechanical properties of biological tissues such as wood or bone are mainly due to their hierarchical structure and to their optimization at all levels of hierarchy. It is therefore essential to characterize the structure at all levels to understand the complex behavior of such tissues. Structures down to the micrometer level are accessible to light or scanning electron microscopic observation. In the case of bone this includes, for example, morphometry of the trabecular architecture or the bone mineral density distribution in cortical and trabecular bone. To characterize the sub-micrometer structure of, e.g., the collagen-mineral composite in the case of bone or the cellulose microfibrils in the case of wood, other methods, such as transmission electron microscopy or X-ray scattering are necessary. The recent availability of extremely brilliant synchrotron X-ray sources has led to the development of the new techniques of scanning small-angle X-ray scattering and scanning X-ray microdiffraction, which are capable of providing structural information on the micrometer and the nanometer level, simultaneously. As a basic principle of the method the specimen is scanned across an X-ray beam which has a diameter of few micrometers. Measuring the X-ray absorption at each position provides an image of the specimen (microradiography) with resolution similar to light microscopy, in the micrometer range. Moreover, the X-ray scattering pattern is analyzed at each specimen position to provide parameters characterizing the structure in the nanometer range. The present paper reviews the principles of the techniques and demonstrates their application to biological materials, such as wood or bone.

Biomechanical Phenomena↗

PubMed1999

Scanning small angle X-ray scattering analysis of human bone sections.

Scanning small-angle X-ray scattering (scanning SAXS) was applied for the first time on bone to compare results from SAXS directly with those from other position-sensitive methods, such as light and polarized light microscopy, back-scattered electron imaging, and radiographic imaging. Since scanning SAXS is a nondestructive method of investigation, images from all these techniques could be obtained from the same bone sections. Thus, it could be shown that both the collagen and the mineral crystals were predominantly aligned parallel to the trabeculae and, therefore, to principle stress directions. Moreover, the mean crystal thickness as determined by scanning SAXS was found to be different at various positions inside the trabecular and cortical structure. Finally, it could be shown that scanning SAXS is suitable for detecting local changes in bone material, e.g., due to fluoride treatment.

Adolescent↗

PubMed1999

[Osteoporosis and metabolic bone diseases; clinical relationship].

Metabolic bone diseases with disturbed bone remodeling lead to loss of biomechanical quality and atraumatic fractures. Differential diagnosis, prevention and adequate treatment should already start early in the course of these disorders to prevent fractures. Thus, clinical osteology is more than the simplified connection "low bone mineral density--fractures--osteoporosis". This review summarizes physiological relations between bone tissue and calcium homoeostasis as well as the relation between structure and function. In addition, the main metabolic osteopathies "osteoporosis, primary hyperparathyroidism and osteomalacia" are presented from a clinical point of view. The importance and the diagnostic values of biochemical parameters and of the transiliacal biopsy are discussed. In this respect the quantitative measurement of the mineralization density (bone mineral density distribution = BMDD) seems to be of high value and extends the well established bone histomorphometry. This recently introduced method has the power to distinguish between small differences in the degree of mineralization of the matrix with high precision and reproducibility. The results of quantitative backscattered electron imaging in the scanning electron microscope improve the differential diagnosis of bone diseases with alterations in mineralization density, helps to detect mixed etiology (e.g. osteoporosis plus osteomalacia) and facilitate decision making for treatments. The value of biochemical, radiological, osteodensitometric and histopathological tests for diagnosis and treatment depends on the knowledge of the clinical relations and the complex interactions between calcium-, phosphate- and bone metabolism.

Age Factors↗