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Hair analysis as an indicator of mineral status of livestock.

Despite several inherent characteristics that would appear to make hair a useful biopsy tissue, many problems make interpretation of data derived from hair analysis difficult. Endogenous minerals are incorporated into hair by several routes. Most attention on hair mineral incorporation has focused on element uptake within the hair follicle. Minerals incorporated within the follicle are presumably chemically or physically associated with cortical cells of the hair shaft and reflect mineral status at the time that the hair filament was synthesized. Because hair follicles in most species regularly go through cycles of intense metabolic activity and quiescence, mineral incorporation through the follicle is not a continual process. Mineral deposition onto hair does not cease when the follicle is not producing a hair fiber. The hair shaft is continuously exposed to several elements through contact with secretions from sebaceous, apocrine and eccrine glands. Significant quantities of major and trace elements of endogenous origin are adsorbed onto the hair surface via these secretions, especially when hair growth is not occurring or is very slow. For several elements significant correlations exist between mineral concentrations in hair and mineral intake. These correlations, however, are usually quite low. Non-dietary factors such as sex, age, hair color, sire, body location and contamination affect mineral levels in hair. Dietary intake of calcium, phosphorus and iron are also known to affect uptake of other elements in hair. Because many factors cause variation in mineral content in hair, hair analyses are not precise indicators of mineral status. Hair mineral analyses may be useful, however, when combined with other indicators of mineral status to provide a more precise assessment of mineral status in livestock.

Animals↗

The locus of mineral crystallites in bone.

The organic content of mineralized tissues has been found to decrease with increasing tissue density, from about 60% of the mineral weight in light bone like deer antler to 1 to 2% in hyperdense bone like porpoise petrosal. The ratio of the weight of mineral that can fill the collagen hole zones to the total mineral content can be no greater than 20% for deer antler and decreases to less than 5% for hyperdense bone. Moreover, the dimensions of hydroxyapatite crystallites have been determined by various investigators to be larger than the intermolecular spacing of collagen molecules. Such crystallites can only be fitted within the collagen fibril if collagen molecules are packed differently from the accepted models. Electron micrographs of fish dentin, at a very early stage of mineralization, show the needle-like crystallites lying in dense strips between collagen fibrils and practically no crystallites within the fibrils. A similar pattern of dense strips of crystallites between fibrils can be identified in examples from more advanced stages of mineralization, taken from fish dentin, cat dentin and cow tibia, even though some of the needle-like crystallites are superimposed on the fibril banded pattern. In every instance there are regions of the fibrils where there are no visible needle-like crystallites. Examination of the work of others shows a similar distribution of the mineral component, except that none exactly resemble the micrograph of the earliest stage of fish dentin provided in this report. The collagen banding is observed to be in spatial phase over many fibrils. The needle-like crystallites may be observed to be bunched in phase with the collagen banding and with the same spatial periodicity. The bunching is most obvious in the least densely mineralized specimens. This observation can account for the x-ray and neutron diffraction patterns which shown the axial period of the mineral to be like that of the collagen axial macroperiod and to be in phase with the hole zones of collagen fibrils. These prior studies were interpreted to show that the crystallites must be within the hole zones. Our images are interpreted to show that most of the mineral is outside of the collagen fibrils in the extrafibrillar volume. The interpretation is in agreement with neutron diffraction studies of various mineralized tissues as well as with earlier diffraction studies of mineralized turkey leg tendon and with the calculations of the amount of mineral that can be contained within the collagen of mineralized tissue.

Animals↗

Nutritional implications of the interactions between minerals.

It is well recognized that the absorption, retention and metabolism of most essential minerals can be markedly influenced by the presence of antinutrient factors in the diet (i.e. fiber and phytate). However, in addition, interactions can also occur between essential minerals. Indeed, under some circumstances, these interactions can be profound and have significant implications for human health. Interactions between essential minerals can be broadly classified as direct or indirect. Direct interactions are generally competitive phenomena that occur during the intestinal absorption and/or during the tissue utilization of a mineral. Indirect interactions occur when one of the minerals is involved in the metabolism of the other mineral, or when a deficiency or toxicity of one of the minerals results in hormonal changes or tissue damage which affects the metabolism of the other mineral. In this review we have focused our comments on direct interactions between essential minerals, and we present suggested levels at which an excess of a mineral (coined "X") can significantly alter the metabolism of another mineral (coined "Y") for several of the known competitive interactions. This level is characterized as the lowest X/Y ratio of the dietary intakes which has been shown to produce negative consequences on the metabolism of the element Y (assuming the intake of Y is physiological). Moreover, the importance of the physiological status of the animal with regard to the determination of these ratios is discussed. The calculated X/Y ratio at which interactions may be predicted to occur is generally higher than the ratio calculated for most minerals using typical dietary intakes of X and Y in Western-type diets. However, ratios which might be predicted to result in negative interactions do occur in select food products, and can be reached as a consequence of supplementation (either through food enrichment or therapeutic use of supplements). In fact, considering the ready availability of dietary supplements, such interactions may become commonplace. Finally, the interactions between essential and non-essential minerals (heavy metals) are briefly discussed, as are indirect mineral interactions.

Animals↗

Mineralization of decalcified bone occurs under cell culture conditions and requires bovine serum but not cells.

The purpose of this study was to develop an in vitro model system for bone matrix mineralization in the absence of cells. For this model, we utilized EDTA-decalcified new-born rat tibias with the cartilaginous ends intact, allowing us to visually determine the specificity of mineralization within the bone. Our results show that supplementation of DMEM culture medium with 10mM beta-glycerophosphate and 15% fetal bovine serum (FBS) results in non-physiological mineral percipitation in the tibia because of the generation of supraphysiological (5mM) levels of inorganic phosphate in the medium. The same medium supplemented only with inorganic phosphate to a final concentration of 2mM failed to mineralize a decalcified tibia matrix. However, additional supplementation of this medium with as little as 5% FBS resulted in mineralization of those regions of the type I collagen where mineral was found prior to decalcification, with no evidence for mineralization in the cartilage at the bone ends or in the periosteum. Analysis of the mineral by Fourier-transform infrared spectroscopy and powder X-ray diffraction shows that tibias that have been decalcified and then remineralized contain an apatitic mineral that is strikingly similar to the mineral in normal bone. Tendon, a type I collagen matrix not normally mineralized in vivo, also mineralizes when incubated in DMEM containing 2mM Pi and as little as 1.5% FBS, but not when incubated in DMEM without serum. These data indicate that serum contains a nucleator of type I collagen matrix mineralization, and that mineralization of type I collagen under cell culture conditions requires serum but not living cells.

Animals↗

Effects of vertebral bone fragility and bone formation rate on the mineralization levels of cancellous bone from white females.

Back-scattered electron microscopy was used to study mineralization levels of human iliac cancellous bone of white females (N = 49). Mineralization levels were assessed by converting bone pixel grayscale levels to atomic number (Z) using known calibration standards. The data set consisted of bone biopsies from normal and vertebral fracture subjects that had either high or low values for bone formation rate (BFR(s)) within their respective groups (fracture/low BFR(s), N = 12; fracture/high BFR(s), N = 10; normal/low BFR(s), N = 12; normal/high BFR(s), N = 15). The following three measures of mineralization were quantitatively determined for each specimen: an overall mean mineralization (Z(mean)), the mineralization of trabecular packets deep within the interior of trabeculae (Z(deep)), and the mineralization of superficial exterior packets (Z(superficial)). Two-way analysis of variance revealed that the high BFR(s) group had a significantly lower Z(superficial) than the low BFR(s) group [mean (SD) 10.383 (0.270) vs. 10.563 (0.289)], and there was no significant interaction. BFR(s) had no effect on Z(mean) or Z(deep). For the pooled data, Z(deep) was significantly higher than Z(superficial) [10.866 (0.242) vs. 10.471 (0.291)]. There was no significant difference in Z(mean), Z(deep), or Z(superficial) between normals and those with vertebral fracture, but the standard deviations of the mineralization measures in the fracture group were at least double that of the normal group. Frequency histograms show that the two groups have fundamentally different mineralization distributions. The normal group demonstrates typical Gaussian distributions centered around the mean, and the distributions of the fracture group are bimodal, with peaks occurring at either the high or low tails of the distributions of the normal group. We hypothesize that both low and high patterns of mineralization might detrimentally affect bone material properties, with low mineralization levels causing reduced stiffness and strength and high mineralization resulting in reduced fracture toughness. The degree to which the mineralization differences may affect strength and stiffness of individual elements is estimated. The higher standard deviations of mineralization measures in the fracture group may reflect an inability to properly regulate trabecular level stress and strain. Forward stepwise regression analysis showed significant relationships between Ob.S/OS and both Z(superficial) and Z(mean), suggesting that the osteoblast may play an important role in regulating mineralization.

Aged↗

Radiographic features of aortic bulb/valve mineralization in 20 dogs.

The radiographic features of aortic bulb/valve mineralization in 20 dogs were reviewed. Extent, shape, number, and location of mineralization were recorded. Five of the dogs had additional alternate imaging examinations, including bone scintigraphy, echocardiography, and thoracic computed tomography. A necropsy was done on one dog, and the area of mineralization was evaluated using routine histology. The median age was 10 (mean 9.7; SD +/- 2.7) years. There were five males, seven neutered males, one female, and seven neutered females. The breeds were: Irish setter (6); rottweiler (7); chow-chow (1); miniature dachshund (1); borzoi (1); English setter (1); English springer spaniel (1); great Dane (1); and greyhound (1). Dogs with both right and left lateral radiographs (n = 17) had mineralization visible on both views, more conspicuously on the right lateral radiograph (n = 12). Aortic bulb mineralization was identified on the ventrodorsal radiograph of only one dog. On lateral radiographs, the aortic bulb mineralization was localized within the 4th intercostal space and in the craniodorsal quadrant of the cardiac silhouette. In nine of the dogs, there were complex or multiple mineralizations and in 11 dogs, there was a single curvilinear mineral opacity oriented in a caudoventral to craniodorsal direction. In all radiographs, the mineralization was in the expected position of the aortic bulb, and echocardiography (n = 4), spiral computed tomography (n = 2), and necropsy (n = 1) confirmed that the mineralization was within the aortic bulb. Clinical pathologic data of the dogs suggested no reason for metastatic mineralization. Exact etiopathogenesis of the lesions were not determined in this study. Based on the histologic findings in one dog, the mineralization seen in the aortic root is similar to a form of dystrophic mineralization called Monckeberg's calcific arteriosclerosis in humans. No clinical signs attributable to the mineralization were observed.

Animals↗

Mineralization of [14C]hexadecane and [14C]phenanthrene in crude oil: specificity among bacterial isolates.

Bacteria isolated from freshwater, marine, and estuarine samples were tested for the ability to produce 14CO2 from n-[1-14C]hexadecane or [9-14C]phenanthrene added to Prudhoe Bay crude oil. Of 138 isolates tested, 54 (39%) mineralized the model aliphatic compound hexadecane and 6 (4%) mineralized the model aromatic compound phenanthrene. None mineralized both compounds. There was no apparent correlation between degradative ability and genus or source. Additional hydrocarbon-degrading bacteria from diverse sources were tested and found to mineralize either hexadecane or phenanthrene. Of 61 hexadecane- and 21 phenanthrene-mineralizing bacteria tested, none mineralized both model compounds. Selected isolates and commercially available cultures were tested for mineralization of specific 14C-labelled mono-, di-, and tri-cyclic aromatics. An apparent hierarchy of degradation was observed: strains mineralizing the mono- and di-cyclic aromatics toluene and naphthalene did not mineralize biphenyl or the tricyclic aromatics anthracene and phenanthrene, whereas those strains that mineralized the tricyclic aromatics also mineralized the smaller substrates. Similarly, not all n-alkane-mineralizing isolates tested mineralized the isoprenoid pristane. A combined culture consisting of one aliphatic- and one aromatic-degrading isolate was tested for mineralization of the model compounds and for degradation of other crude oil components by gas chromatography. No synergism or antagonism was observed compared with degradation by the individual isolates.

Alkanes↗

Calcaneus as a site for assessment of bone mineral density: evaluation in cadavers and healthy volunteers.

OBJECTIVE: The value of calcaneal dual-energy X-ray absorptiometry for monitoring changes in bone mineral density has not yet been established. Accordingly, the focus of this study was to determine the usefulness of the calcaneus as the site for bone mineral density measurement with dual-energy X-ray absorptiometry. SUBJECTS AND METHODS: Dual-energy X-ray absorptiometry of the calcaneus was performed in 19 specimens derived from 11 cadavers and 337 healthy volunteers to assess accuracy, in vivo precision, and age-related changes in bone mineral density. We also compared calcaneal bone mineral density determined by dual-energy X-ray absorptiometry with lumbar spine bone mineral density determined by dual-energy X-ray absorptiometry (L1-L4) or quantitative CT (L3). RESULTS: Studies of specimens showed that dual-energy X-ray absorptiometry had an error rate of 6%. In addition, strong correlations were found between bone mineral content and ash weight (r = .97, p < .0001) and between bone mineral density and ash density (r = .87, p < .0001). In vivo studies showed moderate correlations between calcaneal bone mineral density determined by dual-energy X-ray absorptiometry and lumbar spine bone mineral density determined by dual-energy X-ray absorptiometry (men, r = .77, p < .0001; women, r = .76, p < .0001) and lumbar spine bone mineral density by quantitative CT (men, r = .68, p < .0001; women, r = .68, p < .0001). Calcaneal bone mineral density measured by dual-energy X-ray absorptiometry and lumbar spine bone mineral density measured by quantitative CT continued to decrease throughout the postmenopausal period. However, lumbar spine bone mineral density determined by dual-energy X-ray absorptiometry did not show further decreases in subjects more than 70 years old. CONCLUSION: Taken together, these results suggest that the calcaneus can be used as an additional site for determining bone mineral density to assess osteopenia in patients when deformities of the spine make quantitative CT or other methods of density measurement impossible.

Absorptiometry, Photon↗

Association of hypogonadism and estradiol levels with bone mineral density in elderly men from the Framingham study.

BACKGROUND: Both hypogonadism and low estrogen levels adversely affect bone health in young men. In elderly men, who are at greatest risk for osteoporotic fracture, the influence of hypogonadism on bone mineral density remains unclear, as does the relative effect of estrogen status compared to hypogonadism. OBJECTIVE: To examine the relation of hypogonadism and estrogen status to bone mineral density in elderly men. DESIGN: Community-based, prospective cohort study. SETTING: Framingham, Massachusetts. PATIENTS: Male participants of the Framingham Study. MEASUREMENTS: Total testosterone, total estradiol, and luteinizing hormone were measured in participants at all four biennial examinations from 1981 to 1989. Values from at least three of four examinations were averaged. Hypogonadism was defined as a mean testosterone level less than 10.4 nmol/L (<3.0 ng/mL) or a mean luteinizing hormone level of 20 IU/L or greater. An alternate definition of hypogonadism based only on a mean testosterone level less than 10.4 nmol/L (<3.0 ng/mL) was also used. In 1988-1989, bone mineral density was measured at the proximal femur (femoral neck, Ward triangle, and trochanter) and lumbar spine by using dual-photon absorptiometry and at the radial shaft by using single-photon absorptiometry. The association of hypogonadism with bone mineral density was examined with adjustment for confounders, including estradiol levels. A similar model that adjusted for hypogonadism was used to examine the association of estradiol level (ranked as quartiles) with bone mineral density. RESULTS: Of 448 men with bone mineral density measurements, 405 had evaluable hormone levels (mean age, 75.7 years [range, 68 to 96 years]); 71 (17.5%) of the 405 men were hypogonadal. Bone mineral density at any site did not significantly differ in hypogonadal men compared with eugonadal men (for example, bone mineral density at the femoral neck was 0.89 g/cm(2) vs. 0.87 g/cm(2), respectively; P > 0.2), even when alternate definitions of hypogonadism were used. In contrast, compared with the lowest estradiol quartile, men with higher estradiol levels had greater mean bone mineral density at all sites (for example, bone mineral density at the femoral neck was 0.84 g/cm(2), 0.88 g/cm(2), 0.86 g/cm(2), and 0.91 g/cm(2) from the lowest to the highest estradiol quartile; P for trend = 0.002). The difference in mean bone mineral density between men in the lowest and those in the highest estradiol quartile levels was similar to the effect of 10 years of aging on bone mineral density. CONCLUSIONS: In elderly men, hypogonadism related to aging has little influence on bone mineral density, but serum estradiol levels have a strong and positive association with bone mineral density.

Aged↗

Effects of bisphosphonates on matrix mineralization.

Bone strength is determined not only by the volume of bone tissue and the microarchitectural organization of this bone, but also by the degree of mineralization of bone matrix. The mineralization process consists of a primary deposition of mineral substance on the calcification front, followed by a slow and progressive increase of the mineral deposition named secondary mineralization. In osteoporosis, there is a negative imbalance between bone resorption and bone formation, resulting in bone loss, and microarchitectural deterioration of the trabecular network. Therapeutic agents for osteoporosis could increase bone strength by three separate, but interrelated effects on bone tissue: 1) the prevention of bone loss and thus the preservation of bone microarchitecture, 2) an increase in the volume of bone matrix, and 3) an increase in the degree of mineralization to a level similar to that seen in healthy premenopausal women, through a prolongation of the duration of secondary mineralization. Therefore the use of antiresorptive agents that reduce bone turnover, as bisphosphonates, provide a rational approach to treatment of osteoporosis. Extensive phase III clinical trials have shown that osteoporotic women treated orally with alendronate (ALN) for 3 years or more had substantial increases in bone mineral density (BMD) of approximately 10% at the spine together with reductions of about 50% in the incidence of vertebral fractures. Since a marked reduction in activation frequency was evidenced in the transiliac biopsies taken after treatment with ALN compared to placebo (PLA), without detectable increase in cancellous bone volume, it was hypothesized that the increase in BMD and the reduction in the incidence of fragility fractures were due, in a substantial part, to an increase in the degree of mineralization of bone (DMB). The mean DMB was measured by quantitative microradiography on transiliac bone biopsies taken from 53 postmenopausal osteoporotic women who had been treated with ALN (10 mg/day) during 2 (9 patients) or 3 years (16 patients) or with PLA (15 and 13 patients, respectively). In the same patients, BMD values were obtained by dual-energy X-ray absorptiometry on lumbar spine at the beginning and end of treatment. Histomorphometric parameters and activation frequency of new remodeling units were also measured on the biopsies. After 2 years of ALN, mean DMB in compact bone was 9.3% (p=0.0035) and in cancellous bone was 7.3% (p=0.0009) higher, respectively, versus PLA. After 3 years of ALN, mean DMB in compact bone was 11.6% (p=0.0002) and in cancellous bone was 11.4% (p=0.0001) higher, respectively, versus PLA. After 2 and 3 years of ALN and compared to the corresponding PLA, the distribution of the DMB clearly showed a shift towards the highest mineralization values and a decrease of the number of bone structure units having low values of mineralization. The between group differences in mean DMB were similar to those of BMD at the lumbar spine level (+8.7% after 2 years +9.6% after 3 years, respectively), suggesting that mean DMB augmentation probably accounts for the major part of the increase in BMD seen with ALN. These results support our model that the reduction in the activation frequency caused by the antiresorptive effect of ALN is followed by a prolonged secondary mineralization which increases the percentage of bone structure units having reached a maximum degree of secondary mineralization and, through this mechanism, mean DMB. That these effects contribute to improved bone strength is demonstrated by the reduction in fracture incidence previously demonstrated in these patients. In conclusion, quantitative microradiography gives access to the mineral dimension of bone tissue which has been insufficiently taken into account until now as an important determinant of bone strength and quality of bone.

Journal Article↗

[Early change of pulmonary ventilation in new coal miners].

OBJECTIVE: To study the early effects of coal dust on lung function in new underground coal miners. METHODS: Two hundred and eighty-seven male miners were selected from new employees at the Xuzhou Mining Group Company as study group, and 132 male students at a mining technical school were selected as control. Data collection included: individual demographic parameters, family medical history, occupational history, and smoking history, measurement of dust concentrations in work areas, and lung function tests. This prospective cohort study took place over 3 years during which time total dust and respirable dust concentrations in the new coal miners' work areas were measured twice each month. For both miner and student groups, FVC and FEV(1) were tested initially before dust exposure, and then 15 times over the 3 years. RESULTS: The average total dust and respirable dust concentrations in the miners' work areas were 23.8 mg/m(3) and 8.9 mg/m(3) respectively, which greatly exceeded national health criteria. During the first year of dust exposure, the miners's average FVC was higher than that of the controls (5.19 L vs 4.92 L, P < 0.01). During the 2nd and 3rd year the difference in average FVC between miners and control group was not significant (5.14 L vs 5.12 L, P > 0.05). Before dust exposure, the miners' FEV(1) was significantly higher than that of the control group (4.48 L vs 4.28 L). In the miners group, FEV(1) declined rapidly during the first year following dust exposure (from 4.48 L to 4.25 L), and in the 2nd and the 3rd year the average FEV(1) of the miners was significantly lower than that of controls (4.34 L vs 4.56 L, P < 0.01), although there were some fluctuations during the follow-up period. Overall, the average FEV(1) of miners group showed a significant decline during the study. There were significant correlations between FVC or FEV(1) and age, height, weight, and smoking. The three-year total loss of FVC and FEV(1) in smoking miners (154 ml, 184 ml) were greater than in non-smoking miners (83 ml, 91 ml). CONCLUSION: There are apparent effects of coal dust on lung function in new underground coal miners, with FEV(1) being more impacted than FVC. Smoking may aggravate the effect of dust exposure on reducing lung function.

Adolescent↗

[Research on mineralization process of organic phosphorus in black soil in Northeast China].

Buried bag and incubation experiments were conducted to study mineralization process of organic phosphorus in black soil in Northeast China under different time sequences. The results showed that both the content and mineralized velocity of organic P decreased gradually as time went on, the cumulative mineralized rate increased step by step, whether it was used by the method of incubation or buried bag. Under incubation, two treatments' mineralized velocity reached the maximum at first month (31.67, 38.75 mg x kg(-1) x month(-1), respectively), and their cumulative mineralized rate and mineralized velocity at six months were 7.94%, 13.26 mg x kg(-1) x month(-1) and 9.24%, 17.99 mg x kg(-1) x month(-1), respectively. Under buried bag, the mineralized velocity of five treatments all reached the maximum at first year (55.67, 55.65, 49.60, 19.71, 22.52 mg x kg(-1) month(-1), respectively), and the cumulative mineralized rate and mineralized velocity of maize root and wheat root treatments at three years both were approximately 50% and 35 mg x kg(-1) x month(-1), which were higher than those under soybean root andgrass root treatments. From two methods of studies on the mineralization process of organic P, it could be seen that the original content of organic P influenced its mineralized rate and mineralized velocity: the higher of the original content of organic P, the higher of its mineralized rate and mineralized velocity.

China↗

[Mineralization patterns in the dentine of the floor of the pulp chamber of porcine molars].

The relationship between the arrangement of the matrix fibre bundles and the shape of the mineralization front (mineralization pattern) were observed in the dentine of the subpulpal wall of porcine molars. The observations were made using mainly light microscopy and scanning electron microscopy on the primary dentine excluding the secondary dentine. The results obtained shows that the dentine of the subpulpal wall consists of two parts, a surface layer and the circumpulpal dentine. The surface layer can be divided into two sublayers according to the arrangement of it's matrix fibres. The mineralization pattern was also observed to have another two sublayers which did not correspond with the two fibrous subdivisions. Adjacent to the dentine-cement junction, there is a layer, measuring about 3 microns in thickness, in which the matrix fibres run parallel to the junction. The second layer is characterized by two types of fibre bundles which run perpendicularly to the dentine-cement junction. These outer radially oriented fibres are about 1-2 microns in diameter, and the inner radially oriented fibre bundles are coarse, 10 microns in diameter. In the outermost 10 microns, mineralization begins as an aggregation of mineral granules, and forms a hypermineralized layer which overlays the junctional region between the fibres which are oriented parallel and perpendicular to the dentine-cement junction. Except for the most-superficial layer, mineralizing cones surround the radial fibre bundles at the mineralizing front. The circumpulpal dentine, which forms the floor of the pulp chamber, can also be divided into two layers by the differences in their fibrous matrix. The fibres of both of these layers lay in the plane of the predentine surface. However, in the outer layer the fibres of the matrix are randomly arranged around and between the dentinal tubules, whereas in the inner layer the fibres have a preferred orientation extending radially from a central region between the roots. In the outer layer, calcospherites, which are the units of the mineral aggregation, appear at the mineralizing front. In the inner layer, at the mineralizing front, ridges, measuring approximately 10-15 microns in width, 10 microns in height and 100 microns in length, also have a preferred orientation, 90 degrees to the fibre direction. Microradiographs show that a higher mineralized "lamellae-like' region exists in the center of each ridge-crest. X-ray diffraction indicates two preferred crystallite orientation, one is parallel to the matrix fibres and the other perpendicular to the predentine surface. The latter seems to be situated in the highly mineralized lamellae. In the circumpulpal dentine, therefore the mineralizing units have a spheritic shape in the outer layer, and a columner shape in the inner layer. As far as the author is aware the columnar mineralization unit in mammalian dentine has not been described before.

Animals↗

Patterns of mineralization in vitro.

Various patterns of mineralization are found in the organism during fetal and postnatal development. Different findings and theories have been published in the literature with regard to the mechanisms of mineralization, many of which are controversely discussed. In the present study the different patterns of mineralization observed in the organoid culture system of fetal rat calvarial cells were investigated by electron microscopy. In organoid culture, calvarial cells grow and differentiate at high density, and deposition of osteoid and mineralization of the matrix occur to a very high extent. Different types of mineralization could be observed more or less simultaneously. It was found that hydroxyapatite crystals were formed at collagen fibrils as well as in the interfibrillar space. Mineralization was frequently seen in necrotic cells and cellular remnants as well as in extra- and intracellular vesicles. Addition of bone or dentin matrices or the artificial hydroxyapatite Interpore 200 to the cells caused an increased mineralization in the vicinity and on the surface of the matrices with and without participation of collagen. On previously formed mineralized nodules, an apposition of mineralizing material appeared due to matrix secretion by osteoblasts. It is concluded that initiation of mineralization occurs--at least in vitro--at every nucleation point under appropriate conditions. These mineralization foci enlarge by further apposition as well as by cellular secretion of a mineralizing matrix. Furthermore, cell necroses may liberate mineralizable vesicles. All these patterns of mineralization are the result of different activities of one cell type.

Animals↗

Mineralization during matrix-vesicle-mediated mantle dentine formation in molars of albino rats: a microanalytical and ultrastructural study.

The purpose of this study was to elucidate the mineralization process of mantle dentine by ultrastructural and element-analytical investigation of matrix vesicles and successive stages. Upper second molars of albino rats were cryofixed and embedded in resin after freeze drying. Semithin dry sections were prepared for analyzing the calcium and phosphorus concentrations in the mineralized matrix vesicles or noduli, larger mineralized islands, and the mantle dentine. For ultrastructural studies, it was necessary to reduce section contact with hydrous fluids to a minimum in order to avoid preparation artifacts. The first mineral deposits were recognized as dot-like formations both in the interior of matrix vesicles and in association with the inner vesicle membrane. This indicated the existence of mineral nucleating sites located both at the inner membrane and at calcium-phosphate-binding macromolecules in the interior of the matrix vesicles. A significantly higher mineral content was found in mineralized matrix vesicles than in the mineralized extravesicular regions of the mineralized islands, suggesting the existence of a rapidly and densely mineralized matrix in the matrix vesicles. A significant increase in mineral content per volume proceeding from the mineralized islands to mantle dentine suggested a further increase in the density of mineral.

Animals↗

Mineralization of CCl4 with copper oxide.

Experimentally, CCl4 was effectively mineralized by CuO to yield stable inorganic species of CO2 and CuCl2 (CCl4 + 2CuO --> 2CuCl2 + CO2). High CCl4 conversions (63-83%) were found in the mineralization process performed at 513-603 K for 10-30 min. Using X-ray-absorption near edge structure (XANES) and X-ray photoelectron spectroscopies, we found that most CuCl2 was encapsulated in the CCl4-mineralized product solid (mineralization at 513 K for 30 min). At higher mineralization temperatures (563-603 K), CuCl2 was found to be predominant on the surfaces of the mineralization product. Speciation of copper in the mineralization product solid was also studied by extended X-ray absorption fine structure (EXAFS) spectroscopy. Bond distances of Cu-O and Cu-Cl in the CCl4-mineralized product solid were 1.93-1.94 and 2.10-2.12 , respectively, which were greater than those of normal CuO and CuCl2 by 0.03-0.07 A. The increase of the bond distances for Cu-O and Cu-Cl might be due to Cl insertion and concomitant structural perturbation of unreacted CuO in the mineralization process. Forthe second shell around copper atom, bond distances of Cu-(O)-Cu also increased by 0.03-0.05 A, and the coordination numbers of Cu-O and Cu-(O)-Cu decreased, as expected, in the mineralization process. In addition, stoichiometrically excess oxygen atoms were found on the solid surfaces, and they might play an important role in the mineralization of CCl4, leading to the formation of CO2 and Cl. Chloride atoms might be further captured by CuO, yielding CuCl2 in the mineralization process. This work exemplifies the utilization of X-ray spectroscopies (XANES, EXAFS, and XPS) to reveal the speciation and possible reaction pathway in a very complex mineralization process in detail.

Carbon Tetrachloride↗

Infrared spectroscopic studies of galvanic effect influence on surface modification of sulfide minerals by surfactant adsorption.

The influence of interaction between mineral components in natural mixtures on the adsorption of organic and inorganic species on the mineral surfaces is recognized. However, the surface phenomena have been meagerly investigated. In this study the formation of different surface species of surfactant (amyl xanthate, C5H11OC(S)S-) adsorbed on FeS2, PbS, and CuFeS2 has been spectroscopically investigated in single-mineral and complex systems. The type and amount of adsorbed species were determined directly on each mineral surface by infrared external reflection spectroscopy. Galvanic interaction between grains of different minerals could have tremendous consequence on the adsorption of surfactants on each mineral component and their future reactivity. The detected changes are dramatic, from no adsorption to the formation of several layers of hydrophobic or hydrophilic surface products depending on which minerals are in contact. It has been documented that even very short contact time between different mineral grains by collision is sufficient to produce dramatic modification of the surface composition and structure. The results obtained indicate clearly that the observations and conclusions aboutthe surfactant adsorption made in a single mineral system cannot be simply extrapolated to describe the real situation in natural multicomponent mineral systems. The obtained information on sulfide mineral interaction in complex systems is indispensable to understand processes taking place in nature at mineral-water interfaces (dissolution of heavy metals). An additional benefit is the improved ability to design efficient separation processes of these minerals.

Adsorption↗

Aluminum inhibits both initiation and progression of mineralization of osteoid nodules formed in differentiating rat calvaria cell cultures.

Osteoid nodules form in cultures of fetal rat calvaria (RC) cells grown in medium containing 10% fetal bovine serum (FBS) and 50 microns/ml of ascorbic acid. When 10 mM beta-glycerophosphate (beta-GP) is added, the nodules mineralize in two phases: an initiation phase that is dependent upon alkaline phosphatase activity for cleavage of beta-GP to inorganic phosphate (P(i)) and a progression phase that proceeds independently of the activity of alkaline phosphatase and does not require exogenous phosphate. We have used this system to investigate the effects of aluminum (Al3+)on mineralization. When AlCl3 was added to culture medium at concentrations of 0, 3, 10, 30, 100, and 300 muM, the total concentrations of aluminum were 0.98, 6.07, 16.82, 40.19, 88.45, and 284.52 muM, respectively. The corresponding free Al3+ concentrations, assessed after ultrafiltration, were found to be 1.11, 1.75, 3.40, 6.22, 5.38, and 12.11 muM. In cultures in which osteoid was formed and mineralization initiated in the presence of added Al+ (3-300 muM), a dose-dependent inhibition of mineralization occurred. Osteoid formed in the presence of added Al3+ mineralized normally when Al3+ was removed from cultures at the time of initiation of mineralization with beta-GP. In osteoid nodules grown in the absence of Al3+, addition of Al3+ (3-300 muM) at the start of the initiation phase of mineralization resulted in a dose-dependent inhibition of mineralization. Addition of Al3+ to cultures after mineralization had been initiated in the absence of Al3+ inhibited progression of mineralization at added Al3+ concentrations of 10 muM and above. Al3+ did not decrease the conversion of beta-GP to P(i) and caused a small but significant increase in alkaline phosphatase activity at added concentrations of 100 muM or greater. The data show that Al3+ inhibits both the initiation and progression phases of mineralization starting at added concentrations of 3-10 muM (approximately 1.7-3.4 muM free Al3+) and that mineralization of osteoid formed in the presence of Al3+ is unaffected if Al3+ is removed prior to the initiation of mineralization.

Alkaline Phosphatase↗