ライフサイエンスコーパス: mineral

1 the iron-reducing bacteria and ferrihydrite mineral.

2 tates with calcium as low-solubility apatite minerals.

3 y rover, which also identified smectite clay minerals.

4 impact-driven shock-recrystallised accessory minerals.

5 tion for wettability alteration in carbonate minerals.

6 reduces mineral bioavailability by chelating minerals.

7 are important source of nutrients including minerals.

8 and enriched with lactic acid, vitamins, and minerals.

9 generated during the first stage, onto oxide minerals.

10 s ambient, incidental iron-bearing nanoscale minerals.

11 target metabolic pathways, and vitamins and minerals.

12 c framework for the nucleation of iron oxide minerals.

13 into the solution and adsorption onto other minerals.

14 is the taxon-specific selection of skeletal minerals.

15 ar relationships between gene expression and minerals.

16 n soils rich in poorly crystalline Fe and Al minerals.

17 ed are a good source of proteins, fibres and minerals.

18 Nephropathic cystinosis CKD patients have mineral abnormalities that are distinct from those in CK

19 gher roughness and complexity than caused by mineral abrasive-free herbivorous diets.

20 we explore the effect of clay- to sand-sized mineral abrasives (quartz, volcanic ash, loess, kaolin)

21 By adding 1, 4, 5, or 8% mineral abrasives to a pelleted base diet, we test for t

22 Phaethon does not exhibit the 3-um hydrated mineral absorption (within 2sigma).

23 , an oxetane acetal persists in concentrated mineral acid (1.5 M DCl in THF-d(8)/D(2)O); its longevit

24 hrough use of partial replacement of PC with mineral admixtures.

25 little is known about how reactive Fe and Al minerals affect C cycling in restored wetlands.

26 ale, we propose a rapid Membrane Enabled Bio-Mineral Affinity Screening (MEBAS) approach supported by

27 re, reflectance, spectral slope, or hydrated minerals, although some of those characteristics correla

28 ay) were examined for proximate composition, mineral, amino acid, phenolic (free and bound) compositi

29 and pathways not yet described as underlying mineral amount.

30 s between gene expression and GEBVs for each mineral amount.

31 and miRNAs expression over the GEBVs for the mineral amounts.

32 model to map the generation of anthropogenic mineral and 23 types of the capsulated materials by targ

33 This review describes nutritional, mineral and bioactive composition of the chicory plant a

34 emical abnormalities in common causes of CKD-mineral and bone disorder have been defined, it is unkno

35 distinct from that typically observed in CKD-mineral and bone disorder.

36 ilable nitrate-N (52-57 and 225 mg kg(-1) in mineral and organic soil, respectively) was recorded wit

37 sium peroxide) to reduce N(2)O production in mineral and organic soils amended with N fertilizer in a

38 We find that insoluble forms of iron in mineral and road dust combined with sulfate from coal-fi

39 ensor for the rapid measurement of Fe(3+) in mineral and tap water samples demonstrating the real-wor

40 pril-September and the amounts of nutrients, minerals and bioactive compounds in the juices of 16 app

41 may occur in soils rich in well-crystallized minerals and exchangeable Ca(2+) regardless of the prese

42 Gluten-free (GF) breads often lack proteins, minerals and fibres and have an imbalanced energy value,

43 e carbonaceous object that contains hydrated minerals and organic molecules.

44 However, a high level of oxalic acid, minerals and soluble sugars were observed in FF infusion

45 stabilizing interactions between OM and soil minerals and this stabilization may be of increasing imp

46 the produced plants were evaluated including minerals and vitamins.

47 nefits (carbohydrates, protein, fatty acids, minerals) and health risks (heavy metals).

48 he need for protein and relates to vitamins, minerals, and numerous often-overlooked nutrients, such

49 l or osteopenic mice, the compounds increase mineral apposition rate, bone formation, bone mass, and

50 and dynamic histomorphometric analyses e.g., mineral apposition rates were comparable with similar da

51 tween WT and Col6alpha2-KO mice based on the mineral appositional rate, bone formation rate, and mine

52 uttlebone is primarily composed of a brittle mineral, aragonite, the structure is highly damage toler

53 Combustion-derived minerals are an important but understudied source of INP

54 s of these proteins while they interact with minerals are essential for understanding biomineralizati

55 of iron (Fe(aq)(2+) -> Fe(surf)(3+)) in clay minerals are fundamental for environmental geochemistry

56 Ferrous iron-bearing minerals are important reductants in the contaminated su

57 The carbonate minerals are then recollected and re-calcined.

58 vent mixture to dissolve the bulk bournonite mineral as well as inexpensive bulk CuO, PbO, and Sb(2)S

59 However, the use of iron(III)-bearing minerals as terminal electron acceptors in permafrost en

60 d with different (deeper) previously altered mineral assemblages.

61 nd separating SOM into particulate (POM) and mineral-associated (MAOM) forms, two SOM components that

62 derived C, and reducing turnover of existing mineral-associated C due to suppression of fungal growth

63 mass), and it stimulated losses of metal- or mineral-associated C.

64 Warming increased C content in the mineral-associated fraction, likely by increasing inputs

65 fungal necromass (15) N was recovered in the mineral-associated organic matter fraction through micro

66 d proteolysis suggest a large variability in mineral-associated proteins as a nitrogen source in soil

67 C was compensated by more extensive loss of mineral-associated soil C in both soils.

68 through microbial anabolism, suggesting that mineral association plays an important role in stabilizi

69 ns, we present a structural model for organo-mineral associations based on the coordination of SOC pa

70 nity Screening (MEBAS) approach supported by Mineral Binding Characterization (MBC) (TGA, ATR-FTIR an

71 Seed phytic acid reduces mineral bioavailability by chelating minerals.

72 For the first time the mineral bioavailability from the gluten and gluten-free

73 ould be used to produce breads with a higher mineral bioavailability, an important strategy for food

74 lay literature suggest soaking nuts enhances mineral bioavailability.

75 asic issue for the inception of infection or mineral biofouling.

76 Separate assessment of mineral bone disorder (MBD) parameters including calcium

77 nt of insensitive munitions formulations, by mineral-bound Fe(II) generated through ISCR of subsurfac

78 performance liquid chromatography (HPLC) and minerals by inductively coupled plasma mass spectrometry

79 rometry, focusing on biologically functional minerals (Ca, Cu, Fe, K, Mg, Mn, Na, P, Se and Zn) and t

80 The content of minerals (Ca, Fe, K, Mg, Mn, Na and Zn), dietary fiber (

81 to calibrate the model MIMICS (The MIcrobial-MIneral Carbon Stabilization model), which we compared t

82 d at 350 degrees C in TGA diagrams, as other mineral carbonates only decompose to carbon dioxide at t

83 icrobial species can selectively precipitate mineral carbonates with enhanced mechanical properties,

84 consisting of spatially discrete organic and mineral (ceramic) phases, the intrinsic mechanical prope

85 s the salivary concentrations of 5 essential minerals (cobalt, copper, manganese, molybdenum, and zin

86 Mechanisms of degradation and absorption of mineral complexes by the human digestive system are comp

87 These mineral components produced in biomass-burning aerosol s

88 n carbohydrate content, an impoverishment of mineral composition and protein content occurred.

89 rmore, they show that differences in bedrock mineral composition can influence the supplies of nutrie

90 However, studying plaque deposition and mineral composition in this spatially and temporally het

91 as well as the ascorbic acid, proximate and mineral compositions of five selected Bangladeshi wild p

92 zed in relation to color change, oxalate and mineral concentration, and protein digestibility.

93 of different soaking regimes on phytate and mineral concentrations of whole and chopped almonds, haz

94 Overall, soaking resulted in lower mineral concentrations, especially for chopped nuts, and

95 l midshaft morphometric properties, and bone mineral content (BMC) in 40 different regions of the tib

96 microhardness, smear layer removal, erosion, mineral content distribution, apatite/collagen ratio and

97 and EDTA solutions did not alter the dentin mineral content distribution.

98 Bone mineral content measured by DXA, total body water by deu

99 irs could be somewhat distinguished by their mineral content using principal component analysis (PCA)

100 Mineral contents in bovine muscle can affect meat qualit

101 The growth of mineral crystals on surfaces is a challenge across multi

102 ogenic Mt nanoparticles formed during fungal-mineral cultivation exhibit intrinsic peroxidase-like ac

103 Deproteinized bovine bone mineral (DBBM) has been extensively studied and used for

104 al approach, where deproteinized bovine bone mineral (DBBM) particles were placed contralaterally.

105 le on a gluten-free diet who often represent mineral deficiencies.

106 ut the effects of eradication of HCV on bone mineral density (BMD) and biomarkers of bone remodeling

107 The association between low bone mineral density (BMD) and periodontitis in perimenopausa

108 Background Bone mineral density (BMD) could be derived from CT localizer

109 ency virus (HIV) infection and with low bone mineral density (BMD) may be at higher risk of osteoporo

110 Bone mineral density (BMD) measurement by dual-energy x-ray a

111 Bone mineral density (BMD) was measured using DXA.

112 Plasma bone turnover markers and bone mineral density (BMD) were quantified at weeks 0, 12, 24

113 between changes in areal and volumetric bone mineral density (BMD), bone microstructure and strength,

114 The reference standard was a bone mineral density (BMD)-based Fracture Risk Assessment Too

115 fenamide had more favourable effects on bone mineral density and biomarkers of renal safety than emtr

116 ar volume, type H vessel formation, and bone mineral density and contents, as well as BV/TV, Tb.Th, T

117 We prespecified six secondary bone mineral density and renal biomarker safety endpoints to

118 Bone mineral density decreased in the first 6 months, with pa

119 erone acetate (DMPA) is associated with bone mineral density loss.

120 re after 12 weeks follow-up covered the bone mineral density, -volume, -trabecular thickness and -sep

121 The pathogenesis of declining bone mineral density, a universal feature of ageing, is not f

122 Clinical and laboratory parameters, bone mineral density, microarchitecture, and vertebral fractu

123 Notably, bone mineral density, osteoporosis and osteoporotic fracture

124 becular number, connective density, and bone mineral density.

125 Although the mineral deposition rates between groups were indifferent

126 obes to bind to active osteoblasts and their mineral deposits and highlight their potential utility a

127 duced polarization of biologically generated mineral deposits can yield a new paradigm for basin scal

128 p between cells, extracellular matrices, and mineral deposits is fundamental for an improved understa

129 Indicating earlier mineral disengagement and the subsequent onset of fibril

130 e the so-called karst morphologies formed by mineral dissolution into water.

131 forcing of greenhouse gases, ice sheets and mineral dust aerosols, this cooling translates to an equ

132 Hence, high loads of mineral dust and grit in natural diets might be identifi

133 he diatom C. meneghiniana benefits more from mineral dust particles in direct contact with cells than

134 When diatoms were physically separated from mineral dust particles, the growth responses become smal

135 The billions of tons of mineral dust released into the atmosphere each year prov

136 ith this complexity via the study of ambient mineral dust samples from diverse source regions.

137 for the first time, that radiatively active mineral dust will have a significant impact on the habit

138 Soiling consists of mineral dust, soot particles, aerosols, pollen, fungi an

139 than intrinsic silica phytoliths, extrinsic mineral dust/grit adhering to plants causes tooth wear i

140 , and sulfur (S(8)) from naturally occurring minerals (e.g., silicate, phosphate, sulfate) follows en

141 human diet, but little is known about their mineral elements composition.

142 Other mineral elements occur at moderate concentrations in all

143 Here, we demonstrate that microscopic mineral fabric and structure interact with macroscopic s

144 of insect-based foods, we analysed selected minerals (Fe-Mn-Zn-Cu-Mg) in wild-harvested and commerci

145 Here, we show that zerovalent iron (ZVI) minerals, ferrite [alpha-Fe(0)] and austenite [gamma-Fe(

146 Mineral fertiliser and manure applications have resulted

147 equent years (10%) was greater than that for mineral fertilizers.

148 ined the utility of other speleothem-forming minerals for this purpose.

149 alized dental tissues rather than inhibiting mineral formation in the ligament, which may have broade

150 The mechanisms for mineral formation include extracellular and intracellula

151 Ettringite is a naturally occurring mineral found in cementitious matrices that is known for

152 The mineral has been largely absent from global sediments si

153 We assessed and compared determinants of mineral homeostasis in patients with nephropathic cystin

154 All major aspects of mineral homeostasis were differentially effected in pati

155 lotho, which normally regulate vitamin D and mineral homeostasis, on testicular function.

156 ly through systemic changes in vitamin D and mineral homeostasis.

157 experiment in Middle Tennessee, USA, the top mineral horizon soils (0-15 cm) were collected using a s

158 marily in the transition between organic and mineral horizons in palsa underlain by intact permafrost

159 modeling and calcification in the context of mineral imbalance.

160 s showed that bone material, although mainly mineral in nature, and therefore less susceptible than o

161 t (k(=S)) for alumina, a naturally occurring mineral in soil and aquifer materials.

162 The oxidation states of manganese minerals in the geological record have been interpreted

163 ur understanding of the role of iron sulfide minerals in the stability of tetravalent uranium in the

164 the deformation mechanisms and elasticity of minerals in the transition zone and uppermost lower mant

165 In contrast, lower-mantle mineral inclusions and their host diamonds (deeper than

166 re we present oxygen isotope measurements of mineral inclusions within diamonds from Kankan, Guinea t

167 dy investigated inulin and calcium-rich milk mineral incorporation into a pork sausage in order to ex

168 SCFA formation and seemed to oppose the milk mineral-induced reduction of nitroso compound formation.

169 re sufficient to contribute to daily dietary mineral intake.

170 d (2) understand how geochemistry influences mineral intake.

171 fractures that open as rocks are exhumed and minerals interact with meteoric fluids.

172 of mineral nanoparticles produced by fungal-mineral interactions and contribute substantially to our

173 Microbe-mineral interactions are ubiquitous and can facilitate m

174 Microbe-mineral interactions have shaped the surface of the Eart

175 precipitate nucleation on bacteria, microbe-mineral interactions, and polymorph transitions.

176 At the organo-mineral interface, 88% (72-92%) and 33% (16-53%) enrichm

177 interactions of protein and nanoparticles at mineral interfaces attracting much interest in various e

178 ho influence gonadal function and testicular mineral ion homeostasis both directly and indirectly thr

179 ons, new features of the isotopic anatomy of mineral ions can now be explored with ESMS instruments t

180 In this study, we evaluated vitamin D and mineral (iron, zinc, magnesium) transfer to the bolus aq

181 Anthropogenic mineral is absorbing wide concern in the context of circ

182 catechin, rutin, vitexin and isovitexin) and minerals (K, P, Ca, Mg, Na and Fe) were predominant in W

183 ese foods have large concentrations of toxic minerals like As, Cd or Pb.

184 dietary reference intake of essential trace minerals like Cr or Mo.

185 e able to perform bioweathering of rocks and minerals, little information is available concerning the

186 n outflow-channel and a progressively-drying mineral matrix that has no running water; ecosystem cons

187 ally and microscopically isolate organic and mineral matter from alluvial sediments contaminated with

188 protein, fibrinogen, and albumin), and bone mineral metabolism (25-hydroxyvitamin D, phosphorus, cal

189 BP, physical function, and blood markers of mineral metabolism and vascular health.

190 stream end-organ complications of disordered mineral metabolism in CKD.

191 were composed of neurohormonal regulators of mineral metabolism, intermediary metabolism, and biomark

192 calcification and serum and urine markers of mineral metabolism.

193 dent DHFA, including 2 biomarkers related to mineral metabolism/calcification (fibroblast growth fact

194 Herein, the contents of health-promoting minerals, metabolites and enzymes as well as the antioxi

195 models, which represented nanoporous organic/mineral microstructure of the Marcellus Shale.

196 m for biomineralization protein control over mineral microstructure, where unstructured regions of th

197 lgal meal (Schizochytrium sp., AM) and micro-minerals (MM, either organic [OM] or inorganic [IM]) on

198 Moreover, the phytates:mineral molar ratios and the percentage of the realizati

199 or chopped nuts, and did not improve phytate:mineral molar ratios.

200 ere related to the natural occurrence of the mineral Monazite-(Ce).

201 e as the structural scaffolds for regulating mineral morphology during enamel development.

202 ts with contrasting fertilizer inputs (no N, mineral N, FYM) and regenerated woodland in the long-ter

203 ribute substantially to our understanding of mineral nanoparticles in natural ecosystems.

204 ant, but unrecognized, catalytic activity of mineral nanoparticles produced by fungal-mineral interac

205 range well-fitting the midpoint potential of minerals naturally reduced by electroactive bacteria suc

206 enic potential compared to GMSCs with strong mineral noduls, and significantly greater expression of

207 n the endodermis, which are critical for the mineral nutrient balance of plants, coordinate with the

208 permeability and, consequently, to a loss of mineral nutrient homeostasis.

209 ic activities simultaneously alter essential mineral nutrients and contaminant content in the environ

210 en groups corresponded mainly to organic OH, mineral OH and carbonyl groups.

211 ery to receive either antibiotic or placebo (mineral oil and petrolatum-based) ointment after surgery

212 ed to model OCT optical properties of water, mineral oil, and intralipid droplets and to investigate

213 pothesize that either highly reactive ferric minerals or radical S species produced by the oxidation

214 tomic structure of silicatein and the entire mineral/organic hybrid assembly with a resolution of 2.4

215 of oxygen-rich compounds in HA fractions to mineral oxides is a decisive factor for the different re

216 in response to the integrated application of mineral P and organic amendments.

217 world, with an assumed absolute shortage of mineral P fertilizer, agricultural soils worldwide will

218 In conclusion, the combination of mineral P sources with organic amendments could be succe

219 S(Ca), and S(Mg)) affected the corresponding minerals, P and Na content.

220 sponse to their interaction with the nascent mineral particles.

221 cystinosis is associated with a biochemical mineral pattern distinct from that typically observed in

222 s limited understanding of Fe and other soil mineral phase associations with OM carbon (C) moieties i

223 , the intrinsic mechanical properties of the mineral phases are poorly understood.

224 ikely supported by secondary non-crystalline mineral phases in interaction with soil organic matter a

225 response of dissolved Fe(II) (Fe(2+)) and Fe mineral phases toward mixing processes, we performed vol

226 , calcite and gypsum are formed as secondary mineral phases, which allows for oxyanion partitioning,

227 ing the mechanisms of cell encapsulation and mineral polymorphism.

228 The mineral precipitating capability of microbes is often ha

229 ing density changes, sample deformation, and mineral precipitation and dissolution.

230 ns producing CaO(3) by geologically abundant mineral precursors at various depths in Earth's mantle.

231 he mineralization process, where ions and/or mineral precursors may be transported through spaces bet

232 Here we study the mineral profile of weight loss related products, includi

233 s appear between the fibrils and, with time, mineral propagates along and within them.

234 n a condition that favors the content of all minerals, protein digestibility and reduces oxalate cont

235 ltimately, we describe a naturally occurring mineral/protein crystalline assembly at atomic resolutio

236 Here we conducted microbial iron(III) mineral reduction experiments in which anthraquinone-2,6

237 etermine the effect of in situ OM on Fe(III) mineral reduction, As mobilization, and microbial commun

238 ron-transfer rate during microbial iron(III) mineral reduction.

239 ty, whose mandates include regulation of all mineral-related activities in international waters and p

240 essential plant nutrients contained in these minerals remains unknown.

241 ios and the percentage of the realization of mineral requirements were calculated.

242 Extraterrestrial iron sulfide is a major mineral reservoir of the cosmochemically and astrobiolog

243 thquakes, formation of continental crust and mineral resources.

244 trong associations between proteins and soil minerals restrict such proteolytic reactions.

245 ions in meltwaters from an iron and silicate mineral-rich basaltic glacial catchment were an order of

246 ydrothermally active submarine volcanoes are mineral-rich biological oases contributing significantly

247 ssolved inorganic carbon (DIC) and carbonate mineral saturation state (Omega) are controlled by parti

248 esult from changes in root production and/or mineral sedimentation; (b) sea level fall events, predic

249 P-rich, mineral sediments deposited by hurricanes create legacie

250 ombined enrichment with both inulin and milk mineral showed no cumulative effect on SCFA formation an

251 d increased N(2)O production, by 74 times in mineral soil and 2 times in organic soil.

252 h N fertilizer increased N(2)O production in mineral soil but decreased in organic soil, while pine b

253 anic compounds into streams and groundwater, mineral soil samples were heated at temperatures of 150-

254 ganic soil had greater N(2)O production than mineral soil.

255 d method for evaluating SOC stock changes in mineral soils, but we further suggest that ESM may also

256 contrasted to existing allometries for OP on mineral soils.

257 ive, as it only includes the contribution of mineral soils.

258 However, mineral speciation modelling indicates that changes in s

259 inity for Co-rich mackinawite, suggestive of mineral-specific bacterial interaction.

260 7 to 87.68%), proteins (4.27 to 14.76%), and minerals, specifically Ca (2.90 to 15.65%).

261 It has been shown that reactive soil minerals, specifically iron(III) (oxyhydr)oxides, can tr

262 r Pb in both remediated natural soils and Pb-mineral spiked soils were reduced by >90% relative to Pb

263 , amino acids, phosphorylated intermediates, minerals, starch, protein, activities of enzymes in cent

264 s study urine was of no value in determining mineral status here and plasma was of limited value.

265 In all three groups, peak mineral strain coincided with maximum tissue strength (i

266 s were associated with lower peak fibril and mineral strain irrespective of treatment.

267 malized strength, with lower peak fibril and mineral strain.

268 ide, is a potential environmentally relevant mineral substrate for arsenic (As) sequestration in redu

269 osses and the concentration of residual soil minerals such as iron (Fe) and aluminum (Al).

270 Naturally occurring minerals, such as the iron sulfide mackinawite, play a k

271 e, canaliculi, small channels, collagen, and mineral suggest a concept for the mineralization process

272 alyses revealed unfolding of proteins on the mineral surface and an increase in beta sheets within th

273 that the actinide coordination chemistry of mineral surface mimics, such as silsesquioxane, is a fru

274 ing multilayers/aggregation formation on the mineral surface.

275 r iron(III) (hydr)oxide nucleation on quartz mineral surfaces by employing a flow-through, time-resol

276 activity of enzymes following adsorption on mineral surfaces requires further study.

277 water interacts with reactive components of mineral surfaces such as silicate radicals and ferrous i

278 isplacing PBAT from H-bond donating sites on mineral surfaces.

279 xchange processes may mobilize polonium from mineral surfaces.

280 742 and magnetite (Mt) as a model fungus and mineral system, we have shown for the first time that bi

281 Pyrite is a ubiquitous iron sulfide mineral that is oxidized by trace oxygen.

282 Identifying mantle minerals that can capture and stabilize xenon has been a

283 ric [Fe(III)] to ferrous [Fe(II)] state, but minerals that form during iron reduction by different me

284 ises equal carbonate to phosphate ratios and mineral to matrix ratios to that of native dentine, both

285 contribution of micronutrients (vitamins and minerals) to nutrition is often overlooked.

286 s to date including calcium hydroxide paste, mineral trioxide aggregate, and glass ionomer resin, are

287 Our findings indicate that reactive iron minerals undergo reductive dissolution inside anoxic mic

288 the molecule structure and the redox-active mineral used, and much less on the preequilibration time

289 luminescence, a light-sensitive property of minerals used for geologic dating, can be used as a long

290 tary intake of multiple nutrients, including minerals, vitamins, and carotenoids, is associated with

291 Out of 49 targeted minerals, vitamins, pigments and antioxidants, more than

292 e (37 degrees C) pretreatment with different mineral wastes (MW) was investigated.

293 ), 'non-functional' flavored, (S, n = 6) and mineral water (W, n = 6) drinks were measured under ambi

294 us real samples such as groundwater, bottled mineral water, river water and borehole water and food s

295 the importance of subglacial aluminosilicate mineral weathering and lack of retention of these specie

296 The minerals were stable and the HCl extractability decrease

297 t, including via newly formed soil carbonate minerals whose long-term fate requires assessment throug

298 igital rock physics to reticulite, a natural mineral with a strong analogy to synthetic open-cell foa

299 ecreasing concentration of essential dietary minerals with increasing plant productivity-that particu

300 ecular models of the various aluminosilicate minerals with interlayers were performed.