ライフサイエンスコーパス: remineralization

1 s to compare the dentifrices for root caries remineralization.

2 lization and protective factors that lead to remineralization.

3 hly concentrated fluoride solution increases remineralization.

4 osition within caries lesions during de- and remineralization.

5 with Ca and P ion releases are promising for remineralization.

6 des derived from DMP1 can be used for dentin remineralization.

7 g tissue homeostasis during regeneration and remineralization.

8 cements containing calcium phosphate promote remineralization.

9 vidence of intrafibrillar and interfibrillar remineralization.

10 leased high levels of Ca-PO(4) requisite for remineralization.

11 matter, and not the larger signal of organic remineralization advected from the Chukchi Sea in the ha

12 ive in the presence or absence of biomimetic remineralization after in vitro aging.

13 r diamine fluoride (SDF) is found to promote remineralization and harden the carious lesion.

14 l gain by the lesions, due to both increased remineralization and inhibition of demineralization over

15 d that previous estimates for sulphur-driven remineralization and loss of fixed nitrogen from the oce

16 dered, including potential control of carbon remineralization and metal bioavailability.

17 a show that early x-rays may actually detect remineralization and not new bone formation.

18 , mechanical, fluorescence, antitumoral, and remineralization and regeneration potential) of polymeri

19 hesis, particle settling, and organic matter remineralization, and are collectively termed the "biolo

20 e deep ocean, where decadal peaks in supply, remineralization, and sequestration of organic carbon ha

21 , contributing to elemental cycling, benthic remineralization, and ultimately sequestration of carbon

22 oint for assessing the success or failure of remineralization approaches in restorative dentistry.

23 with phosphohydrolase enzymes involved in P remineralization are quite large and could potentially l

24 ical changes in artificial caries undergoing remineralization as a function of depth, using Polarizat

25 LVM) may facilitate monthly pulses of carbon remineralization, as they occur continuously in illumina

26 was demonstrated between the in vivo calcium remineralization assay and the in vitro ALP assay of ost

27 The organic matter undergoes anoxic remineralization at depth via either sulfate- or iron-re

28 to pB was determined to be ideal for dentin remineralization, based on hydroxyapatite (HA) morpholog

29 ient cycle processes at the seafloor through remineralization, bioturbation, and burial of the sunken

30 rovide theoretical models enabling design of remineralization by calcite slurry dissolution with carb

31 h respect to fluorapatite can enhance enamel remineralization by reducing preferential remineralizati

32 However, the extent of subsurface lesion remineralization by the acidic solution was significantl

33 Mineral volume changes arising from remineralization can be measured on the basis of the opt

34 This study evaluated the in vivo remineralization capacity of resin-based calcium-phospha

35 This study evaluated the in vivo remineralization capacity of resin-based calcium-phospha

36 mescales, and highlight potential impacts on remineralization depth as phytoplankton communities resp

37 little about geographical variability in the remineralization depth of this sinking material and less

38 dynamic balance between demineralization and remineralization determines the end result.

39 fficient carbon sequestration because of low remineralization during downward transit that leads to e

40 zed; dramatic escalation of demineralization-remineralization dynamics is the likely biologic mechani

41 ant DFe sources are linked to organic matter remineralization, either in the water column or at conti

42 tions could exceed the release from particle remineralization, enhancing in situ anammox rates.

43 Both treatments resulted in similar remineralization for root caries lesions at study comple

44 siological state to enable spontaneous tooth remineralization from exogenous sources.

45 tite crystallization is a crucial process in remineralization; however, the role of SDF in crystal fo

46 pies directed at correcting demineralization-remineralization imbalance should, in principle, protect

47 /remineralization treatment, and significant remineralization in enamel under the NACP nanocomposite

48 Little is known about fluoride retention and remineralization in incipient caries lesions following a

49 librium below the thermocline suggest that P remineralization in the deep ocean is a byproduct of mic

50 Subsequent remineralization in the lower limb of the AMOC, between

51 sible for 70 to 92 per cent of the estimated remineralization in the twilight zone (depths of 50 to 1

52 . antarctica in the Southern Ocean, although remineralization in the upper water column has been prop

53 ted to FTIR and SEM analysis to evaluate the remineralization induced by such ion-releasing resins be

54 roscopy (SEM) were also used to evaluate the remineralization induced by the experimental ion-releasi

55 astern Tropical North Pacific OMZ 70% of POC remineralization is due to microbial respiration, indica

56 mineral loss remains, and a true subsurface remineralization is rarely achievable, because the surfa

57 inorganic P from organic matter degradation (remineralization) is the predominant, if not sole, pathw

58 We investigated fluoride and the remineralization kinetics of a single application of elm

59 The remineralization length scale (RLS, the vertical distanc

60 North Atlantic, from which we calculate the remineralization length scale for each site.

61 he NACP nanocomposite had the highest enamel remineralization (mean +/- SD; n = 6) of 21.8 +/- 3.7%,

62 The remineralization medium consists of a Portland cement/si

63 and 1000 ppm were evaluated in an intra-oral remineralization model.

64 d root lesions in an in vitro cyclic de- and remineralization model.

65 be explained by temperature, with shallower remineralization occurring in warmer waters.

66 id mixing or sedimentation and in many cases remineralization of a heavy nitrogen source consistent w

67 reconciled by considering relatively intense remineralization of a labile fraction of material in war

68 f global importance in carbon cycling is the remineralization of algae biomass by heterotrophic bacte

69 dynamics associated with the utilization and remineralization of alginate microhabitats promote the u

70 ralization concepts into regimes for in-situ remineralization of bone and teeth.

71 Rapid biological consumption and remineralization of carbon in the "twilight zone" (depth

72 Thus, in contrast to models that link remineralization of carbon to temperature, in the Northe

73 oxides influences the cycling of metals and remineralization of carbon.

74 potentially promising treatment regimen for remineralization of caries lesions in vivo.

75 vealing the capacity of Ca-P base to promote remineralization of caries-affected dentin.

76 m is the microbial-driven solubilization and remineralization of complex forms of phosphorus (P).

77 reducing the enzyme-mediated degradation and remineralization of demineralized dentin.

78 jective of this study was to investigate the remineralization of demineralized human enamel in vitro

79 the new NACP nanocomposite is promising for remineralization of demineralized tooth structures.

80 Remineralization of dentin during dental caries is of co

81 A widely used process for remineralization of desalinated water consists of dissol

82 reflecting a donor age-dependent decrease in remineralization of DFDBA.

83 The remineralization of enamel caries can lead to distinct o

84 is a restriction for in-situ solution-based remineralization of hypomineralized body tissues.

85 marine carbon burial occurs today, rates of remineralization of isotopically light carbon must have

86 ard explanations of these excursions involve remineralization of isotopically light organic matter an

87 Beaufort Sea reflects the local, short-term remineralization of labile organic matter, and not the l

88 Methanogenesis is the terminal step in the remineralization of organic matter and is carried out by

89 For the anaerobic remineralization of organic matter in marine sediments,

90 inst the common but oversimplified view that remineralization of organic matter is the major pathway

91 and sulfate ions derived from heterotrophic remineralization of organic matter.

92 sediment P dynamics, particularly the rapid remineralization of organic P and the stability of Fe mi

93 the surface production, sinking and interior remineralization of organic particles, keep atmospheric

94 suggests PUAs produced in situ stimulate the remineralization of phytoplankton-derived sinking organi

95 an temperature will likely lead to shallower remineralization of POC and hence reduced storage of CO2

96 illing of S. mutans by ME promotes effective remineralization of S. mutans-demineralized enamel compa

97 ation ratio, indicating it did not stimulate remineralization of sediment carbon stores.

98 Mineral-releasing cements may promote remineralization of soft residual dentin.

99 el remineralization by reducing preferential remineralization of the outer lesion and promoting miner

100 For subsurface lesions, preferential remineralization of the outer lesion was not observed wi

101 ar for both solutions, although preferential remineralization of the outer lesion was observed with t

102 -isotopic excursions resulted from increased remineralization of this reservoir.

103 s formation and intrusion, biological carbon remineralization, or both.

104 mposition, rank-abundance distributions, and remineralization over seasonal and interannual scales.

105 research that identifies the predominance of remineralization pathway and recycling of P within the C

106 er the two-solution rinse indicate a greater remineralization potential, while the enhanced fluoride

107 The remineralization produced by the two-solution rinse was

108 ermining the timing of these processes as OM remineralization progresses.

109 All samples were next subjected to a remineralization protocol consisting of two 45-min expos

110 The effect of the remineralization protocol on the demineralized slabs was

111 study tested the hypothesis that biomimetic remineralization provides a means for remineralizing inc

112 We also find that organic carbon remineralization rates in the deep Atlantic remained bro

113 then treated with a cyclic demineralization/remineralization regimen for 30 days.

114 destructively before and after exposure to a remineralization regimen.

115 al analysis, we demonstrated that biomimetic remineralization restored the nano-dynamic mechanical be

116 The biomimetic remineralization scheme provides a proof-of-concept for

117 A biomimetic remineralization scheme that incorporates non-classic cr

118 tes that the excess inorganic P generated by remineralization should have overwhelmed any pore water

119 r, increase in organic matter production and remineralization stimulates microbial Hg methylation res

120 olution rinses produced a greater (p < 0.05) remineralization than did the 250-ppm-F NaF rinse.

121 s, a larger labile fraction undergoes slower remineralization that continues over a longer length sca

122 ut of fixed nitrogen, through N-fixation and remineralization, to its loss by denitrification and ana

123 ineralization before cyclic demineralization/remineralization treatment, and significant remineraliza

124 ACP nanocomposite after the demineralization/remineralization treatment.

125 Its enamel remineralization was 4-fold that of a fluoride-releasing

126 n the lesions after imbibition in quinoline, remineralization was also apparent from the significant

127 For surface-softened lesions, the extent of remineralization was similar for both solutions, althoug

128 epellent, and calcium phosphate nanoparticle remineralization was suggested to provide maximal antica

129 level, bleeding on probing, and root caries remineralization were performed at baseline and 1 and 2

130 on (-6.1%), and driven by changes in pelagic remineralization with depth, results show that while ben

131 egions degraded in the absence of biomimetic remineralization, with significant decline [p < 0.05] in