ライフサイエンスコーパス: mineral

1 re higher in wines from the right bank (less mineral).

2 adiogenic elements (e.g., He and Pb) in host mineral.

3 e the sorption processes at surfaces of clay minerals.

4 ein, dietary fiber, polyphenols, and certain minerals.

5 15 volatile compound data and 83.8% using 13 minerals.

6 water during this time to form hydrated clay minerals.

7 nteraction of secreted organics with Fe(III) minerals.

8 ace sulfide minerals in addition to silicate minerals.

9 ewater that forms upon oxidation of sulfidic minerals.

10 by weathering of trace sulfide and carbonate minerals.

11 dy directly due to dilution by detrital clay minerals.

12 of organic cation sorption to soils and soil minerals.

13 and the crystalline structure of U-V bearing minerals.

14 e permeability (integrity) was unaffected by minerals.

15 egradable organic carbon, and geogenic U(IV) minerals.

16 neral interactions depended on the nature of minerals.

17 eadily measurable concentrations of magnetic minerals.

18 rmation rates were faster in the presence of minerals.

19 , pancreas morphology, and micronutrient and mineral absorption.

20 is specifically activated by carboxylic and mineral acids but does not respond to sweet- and bitter-

21 stion methods (classical digestion utilizing mineral acids, microwave digestion, and lithium borates

22 fate of organic matter associated with soil mineral and aggregate fractions in some of the ecosystem

23 The management of chronic kidney disease-mineral and bone disorders has recently changed.

24 is site had a higher abundance of lignins in mineral and microaggregate fractions and suberin in the

25 orm due to self-organization of the manifold mineral and organic soil components to distinct mineral

26 ined by the spatial arrangement of the solid mineral and organic soil components, and the resulting p

27 mapping of the composition and structure of minerals and associated biological materials is critical

28 ous precursor particles as observed in other minerals and biominerals?

29 ly to be common in a wider family of complex minerals and could be exploited for a single-step synthe

30 on test, proximate composition, amino acids, minerals and electrophoresis] were determined.

31 reting the significance of shock features in minerals and for using them as diagnostic indicators of

32 on dioxide through the breakdown of silicate minerals and is thought to stabilize Earth's long-term c

33 in soils with a capability to reduce Fe(III) minerals and molecular oxygen, and thereby generating Fe

34 nsible for the decreased bioaccessibility of minerals and protein, mainly at higher temperatures.

35 c and inorganic bonds in metal complexes and minerals and therefore, has been employed to predict soi

36 ns of lipids, proteins, total dietary fiber, minerals and vitamin E.

37 radation of trichloroethene (TCE) by in situ minerals, and C2H2 is known to inhibit bacterial dechlor

38 face areas and equilibrium constants of clay minerals, and cation exchange capacity.

39 latively more Nb-bearing minerals, Y-bearing minerals, and zircons formed during Rodinian assembly, w

40 corresponding Nb-bearing minerals, Y-bearing minerals, and zircons result from significant non-arc ma

41 salinity in general hinders As release from minerals; and (4) the magnitude and quantitative uncerta

42 Fe minerals are absent in/on all organically preserved cell

43 ed Cr(VI) in the same horizons where Cr(III)-minerals are colocated with biogenic Mn(III/IV)-oxides,

44 ament-forming rods) and intra-microfossil Fe minerals are consistent with oxygenic photosynthesizers

45 nd pathways of Cr(VI) reduction by such clay minerals are poorly understood.

46 ption (e.g., marine polychaetes and squids), minerals are thought to be indispensable for tooth-harde

47 Iron(II/III)-bearing clay minerals are widespread potential reductants of Cr(VI),

48 een consistently observed to use ferric iron minerals as an electron sink for fermentation.

49 d cause substantial dissolution of carbonate minerals, as expected, increasing effective fracture vol

50 tritional components, including proteins and minerals, as well as bioactive compounds such as glucosi

51 The presence of these minerals, as well as other chemical features, suggests t

52 ent (nutritional value, sugars, fatty acids, minerals, ascorbic acid and tocopherols), whereas the co

53 The specific mineral assemblage provides evidence for a moderate Hade

54 te tubes and filaments with morphologies and mineral assemblages similar to those of filamentous micr

55 eral and organic soil components to distinct mineral assemblages, which are in turn stabilized by bio

56 Clay mineral-bearing locations have been targeted for martian

57 tes Geobacter sulfurreducens from the Mn(IV) mineral birnessite by a 1.4 mum thick wall containing <2

58 blood cell survival and iron deficiency; and mineral bone disease caused by disturbed vitamin D, calc

59 Findings from research into mineral bone disorder associated with CKD (CKD-MBD) coul

60 ed hyperphosphatemia in a mouse model of CKD-mineral bone disorder, and it reduced hyperphosphatemia

61 m land-carbon models that explicitly include mineral-bound C pools.Most molecular scale knowledge on

62 loading at the site, and the depletion of Al mineral buffering capacity after approximately 5 years.

63 ia plays an essential role in producing MnOx minerals by oxidizing Mn(2+)(aq) at rates that are 3 to

64 The levels of the minerals: Ca, K, Mg, Na, P, and the trace elements: Cd,

65 rse tricarboxylic acid (rTCA) cycle and clay mineral catalysts coevolved remains a mystery in the puz

66 The overall effect of mineral changes on the reservoir has yet to be quantifie

67 roach whereby application of a bioresorbable mineral coating improves microparticle-based transfectio

68 factor (bFGF) released from a nanostructured mineral coating maintains its biological activity for we

69 port a growing workforce, and development of mineral commodity supply chains.

70 hesized to mimic the presence of their major mineral components, including metal oxides, calcium, and

71 However, the mineral composition of Fe plaque and thus its potential

72 The production, mass, size, and mineral composition of passion fruit pulp were evaluated

73 In contrast, antioxidant activity and mineral composition were beneficially affected by mid-to

74 The aim of this study was to assess the mineral composition, antioxidant activity, total phenoli

75 The biochemical and mineral compositions of the curds and the cheese yields

76 Iron (Fe) oxide mineral concentrations were elevated in surface sediment

77 le-body (WB) and skeletal site-specific bone mineral content (BMC) relative to linear growth in a hea

78 antify the dialyzable fraction and the total mineral content after microwave-assisted digestion.

79 ssed every 6 mo included the total-body bone mineral content and density, cortical and trabecular bon

80 ed as a differentiated product with a higher mineral content and several nutritional properties.

81 al parameter values, volatile compounds, and mineral content ii) to investigate the potential of abov

82 All techniques showed that the mineral content of the raw and cooked samples in a water

83 on and malting on the proximate composition, mineral content, amino acids and total phenolic content

84 arly, changes in spine and femoral neck bone mineral contents (BMCs) were not significantly different

85 hermore, the vitamins (A, K and B group) and mineral contents (N, P, Na, K, Ca, Mg and Fe) were stimu

86 that crystallization of soil is enhanced and mineral contents of calcite and anorthite in soil are in

87 and nutritional properties, macro- and micro-mineral contents, and pollen counts.

88 hat chemistry of both the organic ligand and mineral contribute to values of binding free energy and

89 35%) and reactivity of the rapidly reacting mineral control the development and erodibility of the a

90 findings have implications for understanding mineral controls on As cycling in the soil-rice nexus, a

91 ction controlling its mobilization, and clay minerals could mitigate As mobilization with surface com

92 ound to posses' high protein, carbohydrates, minerals, crude fibers, polyphenols and antioxidants thu

93 ion studies (GWASs) identified multiple bone mineral density (BMD) and fracture-associated loci.We co

94 Little is known about bone mineral density (BMD) during pregnancy.

95 ss (ALM), quadriceps strength (QS), and bone mineral density (BMD) in 2986 men and women, aged 19-72

96 rol (CON)].RCE significantly attenuated bone mineral density (BMD) loss at the L2-L4 lumbar spine ver

97 Bone mineral density (BMD) measured by dual-energy x-ray abso

98 nt and density, cortical and trabecular bone mineral density (BMD), BMC, and bone area at the 4% tibi

99 aimed at preventing fracture, improving bone mineral density (BMD), or preventing or delaying osteopo

100 accompanied by diminishing weight loss, bone mineral density (BMD), trabecular thickness, trabecular

101 e diagnosed primarily by measurement of bone mineral density (BMD).

102 ally relevant, significant decreases in bone mineral density (BMD).

103 e association study summary datasets of bone mineral density (BMD).

104 Bone mineral density and abdominal fat and paraspinal muscle

105 m autism have been reported to have low bone mineral density and increased risk for fracture, yet the

106 tic factors with pleiotropic effects on bone mineral density and lean mass.Bone mineral density and l

107 s on bone mineral density and lean mass.Bone mineral density and lean skeletal mass are heritable tra

108 In this population-based cohort study, bone mineral density and risk factors were used to calculate

109 racture genetic risk score (Fx-GRS) and bone mineral density genetic risk score (BMD-GRS) modify the

110 ombined assessment of bone strength and bone mineral density is a cost-effective strategy for osteopo

111 ragility fractures in patients with low bone mineral density is beyond the scope of the guideline.

112 Bone mineral density is known to be a heritable, polygenic tr

113 ereas ST-SPI diet only reduced cortical bone mineral density loss 3 wk post-OVX.

114 ealed increased remodelling and reduced bone mineral density portrayed by increased carbonate to phos

115 Lumbar spine bone mineral density showed a mean increase by day 85 and at

116 or one severe vertebral fracture and a bone mineral density T score of less than or equal to -1.50.

117 and greater decreases from baseline in bone mineral density than did those who received placebo; the

118 y adoptive transfer, and bone turnover, bone mineral density, and indices of bone structure and turno

119 o their metabolic bone status including bone mineral density, calcium kinetics studies, and markers o

120 should not routinely screen or monitor bone mineral density, serum creatinine, magnesium, or vitamin

121 inhibition could be applied to enhance bone mineral density, stability, and regeneration in non-life

122 reases in bone formation biomarkers and bone mineral density, suggesting that sclerostin inhibition c

123 ne disease that is characterised by low bone mineral density, typically assessed using dual-energy X-

124 which tested the effect of denosumab on bone mineral density, we assessed the impact of this drug on

125 Texture parameters, but not bone mineral density, were associated with lowest lifetime we

126 loss of total, trabecular, and cortical bone mineral density, whereas ST-SPI diet only reduced cortic

127 dividuals with RTS have decreased areal bone mineral density.

128 rdinated metabolisms and activities of these mineral-depositing communities have had a profound impac

129 c resonance (NMR) spectroscopy, we show that mineral deposition is biologically driven.

130 indicated by alkaline phosphatase activity, mineral deposition, and transcriptional expression of os

131 Granitoid-hosted mineral deposits are major global sources of a number of

132 raphy images and what would be expected from mineral dissolution alone suggest that there is erosion

133 tations and mineral spatial distributions on mineral dissolution and carbonation reactions in fractur

134 The mineral dissolution from image analysis was comparable t

135 nd collect effluent to assess the individual mineral dissolution.

136 icus species is characterized by a unique 3D mineral distribution that is preserved in different envi

137 Mineral dust aerosols are responsible for some of the la

138 r, an atmospherically important component of mineral dust.

139 Bone mineral elastic modulus was similar at 24 hours but redu

140 associated with a reduction in collagen and mineral elastic modulus.

141 ary excretion of various biomarkers, such as minerals, electrolytes, most polyphenols, and BPA, is re

142 dition to higher levels of FOS and CGA, some mineral elements, such as K, Ca and P, and essential ami

143 With this platform, we devise several mineral-enabled dynamic surfaces and interfaces.

144 We investigated mineral, endocrine, and renal responses during the first

145 -born infants fed an isocaloric protein- and mineral-enriched postdischarge formula (PDF) from term a

146 In addition to clay minerals, Fe(III) oxides particles have recently been sh

147 ruit pulp were evaluated when treated with a mineral fertilizer (control) (MIN) or cattle manure at a

148 C (C/N) based on short-term isotope-labelled mineral fertilizer additions should be questioned.

149 13% N w/w) and P (1.5% P w/w) can be used as mineral fertilizer.

150 The structures suggest a mechanism for iron mineral formation at the protein interface.

151 model of U(IV) speciation in the absence of mineral formation under field-relevant conditions has no

152 ange (9-30% at pH 7) and inhibited secondary mineral formation.

153 Porous mineral formations near subsea alkaline hydrothermal ven

154 Nominally anhydrous minerals formed deep in the mantle and transported to th

155 Fe(II)-rich clay minerals found in subsurface redox transition zones (RTZ

156 Aside from isolated mineral-free exception (e.g., marine polychaetes and squ

157 oxidation rates in all treatments except the mineral-free systems at 21% pO2, and SRFA decreased Fe(I

158 is fundamentally controlled by the bulk rock mineral geometry.

159 pids, protein, dietary fibre, phenolics, and minerals, greatly impacted the flour properties.

160 ining a complete atomic-level picture of how minerals grow from aqueous solution remains a challenge

161 rounding perilacunar bone matrix to maintain mineral homeostasis.

162 fa-columns, formed by the hydrated carbonate mineral ikaite, present a unique alkaline microbial habi

163 or olivine ((Mg, Fe)2SiO4) the most abundant mineral in this region.

164 ffective at concentrating As-bound Fe plaque minerals in a uniform coating onto membranes that could

165 rough the dissolution of aluminum-containing minerals in acidic sulfate solutions, such as those that

166 should consider weathering of trace sulfide minerals in addition to silicate minerals.

167 ck interaction, the dissolution of carbonate minerals in Eagle Ford shale leads to the physical detac

168 ions among litter chemistry, soil biota, and minerals in mediating soil C storage in unmanaged ecosys

169 Polyphenols, fiber, vitamins, and minerals in nuts may confer this observed protective eff

170 we report the occurrence of unidentified REE minerals in the granites from South Chinese deposits.

171 various ferrous- and ferric-iron containing minerals, including hypersthene, magnetite and hematite,

172 ough the kinetics of mineralization and cell-mineral interactions depended on the nature of minerals.

173 in distinguishing the role of plant-microbe-mineral interactions from the broader edaphic and climat

174 ost molecular scale knowledge on soil organo-mineral interactions remains qualitative due to instrume

175 ing provide mechanistic insights into organo-mineral interactions, which could potentially inform lan

176 of molecular-level understanding of As-water-mineral interactions.

177 on and chemical stabilization at the organic-mineral interface.

178 chanism by which these organisms produce the mineral is poorly understood (see review by [2]).

179 Radioisotopic dating of volcanic minerals is a powerful method for establishing absolute

180 ced from the oxidation of indigenous Cr(III) minerals is increasingly being recognized as a threat to

181 (1) As desorption/adsorption from/onto clay minerals is the major reaction controlling its mobilizat

182 testarum derives most of its carbon from the mineral it excavates, growing preferentially as an endol

183 itions of iron cycling and stability of iron minerals it does not provide a simple proxy for long-ter

184 of 0.04 mg/mL LRAP, however, densely packed mineral layers, comprising bundles of small needle-like

185 ndocrine responses but did not affect plasma mineral levels.

186 Both the trace elements and minerals levels in the 4-6months vegetarian meal were th

187 acidity through chemical interactions at the mineral-liquid interface.

188 Interactions between organic matter and mineral matrices are critical to the preservation of soi

189 Mineralization was conducted in mineral matrixes commonly found on Mars and Early-Earth,

190 f contact between organic materials and soil minerals may promote C stabilization in Oxisols.

191 result from degassing processes rather than mineral-melt partitioning.

192 Of particular interest is the Ca-phosphate mineral merrillite, the anhydrous end-member of the merr

193 thodontic tooth movement, suggesting altered mineral metabolism contributing to disrupted tooth movem

194 eatinine ratio, comorbidity, and measures of mineral metabolism.

195 of laboratory data for Earth's most abundant mineral, (Mg,Fe,Al)(Al,Fe,Si)O3 bridgmanite (also known

196 Manganese-oxide minerals (MnOx) are widely distributed over the Earth's

197 derived from litter decomposition than from mineral N additions (60% and 20%, respectively), primari

198 ined in ecosystem pools differently to added mineral N, then estimates of the effects of NDEP on the

199 gs support the role of EVs as early sites of mineral nucleation and demonstrate their value for promo

200 nstrated the rapid formation of Fe-rich clay minerals of variable crystallinity from aqueous Fe(3+) w

201 d i.p. with pristane (develop lupus) but not mineral oil (MO) (do not develop lupus).

202 a RAFT dispersion polymerization directly in mineral oil.

203 cilitate organic carbon (C) accumulation via mineral-organic C interactions but Oxisols often have lo

204 ugh reductive dissolution of arsenic-bearing mineral oxides in both sea and river water inundations,

205 Sorbed and mineral P phases determined P speciation in the high-P t

206 we explore the distribution of natural clay mineral particles in poly(ethylene glycol) (PEG)/dextran

207 Despite smaller Fe mineral particles in the coprecipitate and flocs as comp

208 and support the formation of a pre-apatitic mineral phase, which was identified using infrared spect

209 othermal conditions control the stability of mineral phases and hence frictional-mechanical processes

210 The lead white pigment, composed of two main mineral phases cerussite PbCO3 and hydrocerussite 2PbCO3

211 VII) reduction and incorporation into stable mineral phases.

212 eas the latter conferred a quasi-normal bone mineral phenotype through compensatory homeostatic mecha

213 Layered Mn oxide minerals (phyllomanganates) often control trace metal fa

214 by combining seismological observations with mineral physics elasticity measurements.

215 over various length scales creates oriented mineral platelets and chiral vaterite suprastructures.

216 Sulfide mineral precipitation occurs at mid-ocean ridge (MOR) sp

217 Aragonite is the dominant CaCO3 mineral present in the lake deposits.

218 Globally, mineral processing activities produce an estimated 680 G

219 x, and describe early stage formation of its mineral products.

220 ts on separate soil C pools (particulate and mineral-protected carbon) because they are differentiall

221 Mineral reactions during CO2 sequestration will change t

222 initial carbonation, pure diffusion sustains mineral reactions for longer time frames and generates g

223 e of the urease enzyme that hydrolyzes urea, minerals readily precipitate in nonwater urinals and pip

224 This strain was capable of electrode and mineral reduction (including magnetite) at pH 9.

225 r the foreseeable future to ensure that such minerals remain available to industry.

226 e exact nature and origin of this Cl-bearing mineral remained speculative.

227 es (synthetic antigorite-olivine aggregates, minerals representative of subduction zones lithologies)

228 r potential to promote more efficient use of mineral resources in agriculture.

229 Rates were correlated with the mineral's isoelectric point (IEP) and reactive surface a

230 The method involves precisely step-heating a mineral sample, allowing the separation of the different

231 in vulnerable systems such as those with low mineral sediment supply or where migration upwards withi

232 settings indicates that the availability of mineral sediments and terrestrial derived OC may exert a

233 along the crest of the moraine and analyzed mineral separates of pyroxene for cosmogenic (3)He.

234 These REE minerals show higher initial Nd isotope than primary REE

235 ventional harvests do not deplete SOC in the mineral soil have been a function of their short time fr

236 es nonetheless suggested that communities in mineral soil samples were statistically distinct from co

237 ume a long-term net transfer of SOC from the mineral soil to the atmosphere when primary forests are

238 iochemical composition of forest floor, bulk mineral soil, as well as free and occluded particulate o

239 In a deep warming experiment in mineral soil, we found that CO2 production from all soil

240 superficial organic layer compared with the mineral soil.

241 emperature (MAT) was similar for organic and mineral soils (0.029 degrees C(-1) ).

242 we postulate that the pore structure of many mineral soils could undergo N-dependent changes as atmos

243 oils, we analysed the xyloglucan contents of mineral soils of known age exposed upon the retreat of g

244 e may significantly accelerate C losses from mineral soils over weeks to months-a critical mechanisti

245 dominate in organic layers and others favor mineral soils.

246 ion by O2 commonly occurs in the presence of mineral sorbents and organic matter (OM) in soils and se

247 w-crystalline ferrihydrite in the absence of mineral sorbents, low-crystalline lepidocrocite in the p

248 ining nutrients from recalcitrant organic or mineral sources in the soil, besides increasing fungal c

249 sport conditions and bulk composition, exact mineral spatial distributions do not impact the amount o

250 luate the roles of transport limitations and mineral spatial distributions on mineral dissolution and

251 me of the Martian mantle may contain hydrous mineral species as a consequence of surface reactions, c

252 sis reveals total Fe quantity but misses the mineral structure of the Fe (oxyhydr)oxide.

253 lectron equivalents retained within the clay mineral structure.

254 xo Al clusters function as models for common mineral structures and reactions.

255 Our results suggest that Fe-rich clay minerals such as nontronite can form rapidly under oxidi

256 tropy is comparable to those of upper mantle minerals such as olivine and enstatite.

257 formation of jarosite to more stable Fe(III) minerals, such as goethite.

258 ozoic, while fewer occurrences of many other minerals suggest enhanced erosion of Rodinian volcanic a

259 roundwater and injected solutions can induce mineral supersaturation of constituents and drive precip

260 ure ecologically viable continuity of global mineral supply over the coming decades.

261 Three kinds of mineral-supported polyethylene glycol (PEG) as form-stab

262 ate the mechanisms of radical generation and mineral surface complexation.

263 anic matter have been attributed to reactive mineral surface sites that sorb organic species and caus

264 or through the adsorption of Fe(II) onto the mineral surface.

265 Adsorption and redox transformations on clay mineral surfaces are prevalent in surface environments.

266 provide insights into the potential role of mineral surfaces in mimicking aspects of biochemical rea

267 identified to predict lipid self-assembly at mineral surfaces.

268 ground-, and surface waters either from ore minerals that weather in near surface environments, or d

269 on Cr(VI) reduction kinetics: for both clay minerals, the rate constant of Cr(VI) reduction varies b

270 mplished via photochemistry on semiconductor minerals, the synthesis of clays was demonstrated at low

271 at evaluating the main nutrients (proximate, minerals), their contribution for Dietary Reference Valu

272 ey can influence the weathering of rocks and minerals, these communities and their contributions to m

273 y alter how metals associate with iron oxide minerals through a series of cooperative or competitive

274 nteract with calcite, a widespread carbonate mineral, through a coupled dissolution-precipitation mec

275 Trace minerals (TM) play a role in skin integrity and wound he

276 Understanding how rock-forming minerals transform under shock loading is critical for m

277 aqueous Fe(II), triggering Fe(II)-catalyzed mineral transformations and trace metal(loid) release.

278 hism of hydrated mafic crusts, and calculate mineral transition-induced bulk-density changes at condi

279 nical properties, rather than increased bone mineral turnover.

280 ed to assess the bioaccessibility of fifteen minerals, twenty-two phenolic compounds and the antioxid

281 can induce the transformation of these iron minerals, typically from less crystalline to more crysta

282 The characterization of trace elements in minerals using extended X-ray absorption fine structure

283 her initial Nd isotope than primary REE-rich minerals (varepsilonNd(t)=0.9+/-0.8 versus -11.5+/-0.5).

284 he tooth and fail to degrade and thus normal mineral volume is never completely restored.

285 The mineral was observed in Bidart (France) and Gubbio (Ital

286 tion, the highest content of tocopherols and minerals was observed in the 1st growth stage, whereas s

287 Mineral water and energy drinks were chosen for removal

288 nd recovery trials with seawater, tap water, mineral water, and alcoholic beverages and by comparing

289 Reactive mineral-water interfaces exert control on the bioavailab

290 rganic functional group chemistry with model minerals, we demonstrate that chemistry of both the orga

291 these communities and their contributions to mineral weathering remain poorly resolved.

292 Clay minerals were co-located with P only to a lesser extent.

293 Minerals were determined using ICP-OES and volatiles usi

294 equilibrium constants (Keq) for U-V bearing minerals were more than 6 orders of magnitude different

295 Schwertmannite is a ferric oxyhydroxysulfate mineral, which is common in acid sulfate systems.

296 alkali roasting of niobium-tantalum bearing minerals with sodium bicarbonate.

297 and phosphate-containing hydroxyapatite (HA) mineral within a collagenous matrix.

298 The minerals within meteorites therefore hold the key to add

299 supercontinents, relatively more Nb-bearing minerals, Y-bearing minerals, and zircons formed during

300 more occurrences of corresponding Nb-bearing minerals, Y-bearing minerals, and zircons result from si