ライフサイエンスコーパス: remineralization

1 vidence of intrafibrillar and interfibrillar remineralization.

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

3 s to compare the dentifrices for root caries remineralization.

4 lization and protective factors that lead to remineralization.

5 hly concentrated fluoride solution increases remineralization.

6 osition within caries lesions during de- and remineralization.

7 omise to enhance the effectiveness of dentin remineralization.

8 h structure against acid attacks and promote remineralization.

9 t with increased responsiveness to bacterial remineralization.

10 for the majority of dissolved organic matter remineralization.

11 ediments are crucial sites of organic matter remineralization.

12 eplenishes dissolved Zn in the ocean through remineralization.

13 , and promoting biomimetic dentinal collagen remineralization.

14 to reduced productivity, carbon export, and remineralization.

15 ous complex organic nitrogen utilization and remineralization.

16 owed potential in enamel regrowth and dentin remineralization.

17 acts on temperature-dependent organic matter remineralization.

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

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

20 g tissue homeostasis during regeneration and remineralization.

21 cements containing calcium phosphate promote remineralization.

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

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

24 ation provides the necessary ions for enamel remineralization and a guide for crystal growth due to t

25 ould respond to the critical pH value of de-/remineralization and acquire reversible antibiofilm effe

26 or achieve multiple functionalities, such as remineralization and antimicrobial activity antidegradat

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

28 nity indicates a size-dependent role for DOM remineralization and humification of DOM observed throug

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

30 the biosphere, but a small fraction escapes remineralization and is preserved over geological timesc

31 f a mechanistic understanding of mesopelagic remineralization and its sensitivity to ocean warming fo

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

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

34 values, supporting the view that changes in remineralization and not erosional P fluxes were the pri

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

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

37 trients promote an increase in productivity, remineralization and respiration offshore, with recurren

38 intrinsically linked through organic carbon remineralization and storage as dissolved inorganic carb

39 ansport pathways of organic carbon (OC), yet remineralization and transformation of OC in these syste

40 ules, leading to both surface and subsurface remineralization and tubule occlusion.

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

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

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

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

45 We consider various functional forms of remineralization appropriate for solid/compact particles

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

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

48 fter they have developed beyond the point of remineralization as cavities.

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

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

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

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

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

54 les raining out from the upper ocean undergo remineralization by bacteria colonized on their surface

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

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

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

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

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

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

61 mperature-dependent reduction in the rate of remineralization (degradation) of sinking organic matter

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

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

64 carbon (1.0 vs. 0.8 Pg C) because of deeper remineralization depths.

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

66 We found that enhanced organic matter remineralization, driven by increased microbial respirat

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

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

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

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

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

72 (SO(2)) emissions, export productivity, and remineralization from 67 to 65 million years ago using t

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

74 the flux vs. depth profile to the choice of remineralization function, relative particle density, pa

75 interactive effects, on DOM composition and remineralization have been documented in Arctic soils an

76 The limitations to assess dental enamel remineralization have been overcome by a methodology res

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

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

79 vironments, where it mediates organic carbon remineralization, impacting both local and global redox

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

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

82 ) shows that GAG removal reduced the rate of remineralization in mineralized tissues compared to the

83 ir interactions on Arctic DOM alteration and remineralization in the coastal ocean has not been consi

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

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

86 osynthetic fixation in the euphotic zone and remineralization in the mesopelagic zone.

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

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

89 of key bacterial players involved in carbon remineralization in the Weddell Sea, including its coast

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

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

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

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

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

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

96 The remineralization length scale (RLS, the vertical distanc

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

98 iruses in altering microbial utilization and remineralization length scales of organic matter in the

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

100 The remineralization medium consists of a Portland cement/si

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

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

103 Microbial remineralization, normalized to POC flux, ranged by 20-f

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

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

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

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

108 Bacterial remineralization of algal organic matter fuels algal gro

109 ng the phycosphere, are major players in the remineralization of algal-derived carbon.

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

111 g nutrients to primary producers through the remineralization of benthic-derived organic matter.

112 dation-dispersal cycles, which influence the remineralization of biomass in marine environments.

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

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

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

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

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

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

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

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

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

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

123 Fluoride facilitates the remineralization of dental hard tissues and affects bact

124 Remineralization of dentin during dental caries is of co

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

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

127 The remineralization of enamel caries can lead to distinct o

128 ng phototrophy via proteorhodopsins with the remineralization of high molecular weight organic matter

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

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

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

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

133 Here we used an in vitro model based on remineralization of mouse dental tissues to determine th

134 rm essential ecosystem functions such as the remineralization of organic carbon that exists as biopol

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

136 Methanogens are essential for the complete remineralization of organic matter in anoxic environment

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

138 o-thirds reaching 100 m depth owing to rapid remineralization of organic matter in the upper water co

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

140 ocesses, including marine oxygen production, remineralization of organic matter, and biofilm formatio

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

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

143 rising sulfate concentrations and increased remineralization of organic P by sulfate-reducing bacter

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

145 dence of prokaryoplankton on respiration and remineralization of phytoplankton-derived organic carbon

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

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

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

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

150 Below the surface ocean, remineralization of sinking organic matter rapidly regen

151 leted over a period of up to 12,000 y due to remineralization of sinking organic matter, culminating

152 ons by this mesoscale eddy transport and the remineralization of sinking particles.

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

154 ng-distance lateral transport with efficient remineralization of terrOC.

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

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

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

158 Biomarker ratios further indicate greater remineralization of this OC in the open ocean.

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

160 per layers yet promotes intensive aerobic OC remineralization of up to 0.7 gC m(-2) d(-1).

161 all marine organic matter is either complete remineralization or transformation to more stable produc

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

163 into lower MW compounds without significant remineralization, or that HMW HS was remineralized but r

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

165 accumulate in mesopelagic waters, where slow remineralization over the year reduces deep particle flu

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

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

168 The remineralization produced by the two-solution rinse was

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

170 odels that account for temperature-dependent remineralization promoted enhanced LL mesopelagic nutrie

171 e dual functions of MDP monomer with de- and remineralization properties might create a new epoch in

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

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

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

175 Sinking speed and remineralization rate determine flux attenuation in the

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

177 The temperature effect on remineralization rates of marine organic matter also pla

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

179 destructively before and after exposure to a remineralization regimen.

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

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

182 A biomimetic remineralization scheme that incorporates non-classic cr

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

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

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

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

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

188 ue opens opportunities in caries prevention, remineralization, tooth whitening, and nanomedicine deli

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

190 ACP nanocomposite after the demineralization/remineralization treatment.

191 cts of P26-CS and P32-CS hydrogels on dentin remineralization using 2 in situ experimental models tha

192 burial of organic carbon, which prevents its remineralization via oxygen-consuming processes, is cons

193 t sea surface processes, including bacterial remineralization (via the coupling of photooxidation of

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

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

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

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

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

199 ts could experience the greatest increase in remineralization with a 9% to 42% reduced potential for

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

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