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Results for “Calcification, Physiologic”

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At least 181 records · Page 10Linked to original sources
PubMed2000

The growing years and prevention of osteoporosis in later life.

Ca is the major mineral in bone, and 99% of the Ca in the body resides in the skeleton. Skeletal mass is a determinant of risk of fracture in childhood as well as adulthood. Over 40% of adult peak bone mass is acquired during adolescence. This period is when lifestyle choices, including ensuring adequate dietary Ca, regular weight-bearing exercise and avoiding hormonal insufficiency, are especially important. Current Ca intakes for adolescent females are woefully inadequate.

Adolescent↗
PubMed1994

Calcium needs of adolescents.

Adolescents grow at the greatest rate of any age group after infancy and accumulate 37% of their total bone mass during this growth spurt. Because maximum bone mass is acquired during adolescence, the calcium deposited during adolescence determines the risk of osteoporosis and fracture in adulthood. Bone mass is dependent on calcium intake, growth and pubertal development, exercise, and genetic and racial factors. Unfortunately, during this time of tremendous calcium need, most adolescents eat a diet that is very deficient in calcium. Girls are twice as likely to be deficient as boys (85% vs 43%). Other factors contributing to poor bone mineralization include adolescent pregnancy, anorexia nervosa, excessive exercise, and various chronic medical conditions. To avoid osteoporosis in later life, adequate dietary calcium intake should be recommended and calcium supplementation considered in all adolescent patients.

Adolescent↗
PubMed1986

Heat resistance of bacterial spores correlated with protoplast dehydration, mineralization, and thermal adaptation.

Twenty-eight types of lysozyme-sensitive spores among seven Bacillus species representative of thermophiles, mesophiles, and psychrophiles were obtained spanning a 3,000-fold range in moist-heat resistance. The resistance within species was altered by demineralization of the native spores to protonated spores and remineralization of the protonated spores to calcified spores and by thermal adaptation at maximum, optimum, and minimum sporulation temperatures. Protoplast wet densities, and thereby protoplast water contents, were obtained by buoyant density sedimentation in Nycodenz gradients (Nyegaard and Co., Oslo, Norway). Increases in mineralization and thermal adaptation caused reductions in protoplast water content between limits of ca. 57 and 28% (wet weight basis), and thereby correlated with increases in sporal heat resistance. Above and below these limits, however, increases in mineralization and thermal adaptation correlated with increases in sporal resistance independently of unchanged protoplast water contents. All three factors evidently contributed to and were necessary for heat resistance of the spores, but dehydration predominated.

Adaptation, Physiological↗
PubMed2005

Changes in mineralization and biomechanics of tibial metaphyses in splinted rats.

The effect of 3 wk of splintage of a single hindlimb on the midarea and mineral content of both tibial metaphyses was assessed immediately after splint removal and after 1 mo of mobilization in 12-wk-old Sprague-Dawley rats. Immobilization reduced tibial metaphyseal bone mineral density (BMD) in immobilized limbs compared with "free" limbs of splinted animals and with controls. These changes persisted and were accentuated by relatively greater increases in tibial metaphyseal BMDs of unsplinted (control) animals after 7 wk. Immediately after splintage, tibial metaphyseal areas and total mineral contents of both hindlimbs of splinted animals were reduced compared with those of unsplinted animals. However, the relationship between mineralization and area differed between the free and immobilized limbs of splinted animals. The breaking strain and the breaking energy of immobilized and free femurs of splinted animals were impaired 4 wk after the removal of the splint. This impairment was correlated with an effect of splintage on femoral size with some additional local effect from immobilization. Thus osteoporotic changes consequent on immobilization include both local effects on mineralization and general effects on growth, which may separately influence the elastic properties of bone.

Adaptation, Physiological↗