ライフサイエンスコーパス: hematite

1 these vacancies, inclusions of alpha-Fe2O3 (hematite).

2 the secondary structure during adsorption on hematite.

3 d is lost altogether upon incorporation into hematite.

4 ity from binding to coordinated iron(III) in hematite.

5 nd 10(-6) M at pH 5 and 0.3 g/L (9.3 m(2)/L) hematite.

6 contaminant, onto the ubiquitous iron oxide, hematite.

7 10.5) and aged to induce crystallization of hematite.

8 e-like clusters, epitaxially intergrown with hematite.

9 tter deposited with a thin layer (230 nm) of hematite.

10 reoxidation with ferrihydrite, goethite, and hematite.

11 ong the (210) plane with the (0001) plane of hematite.

12 nduced by the photocatalytic activity of the hematite.

13 (-1) with goethite, and 8.8 muM day(-1) with hematite.

14 owing fungus and an iron-containing mineral, hematite.

15 goethite, and suspensions of Fe(II)-amended hematite.

16 ns as well as in the presence of goethite or hematite.

17 of Cu-, Co-, and Mn-substituted goethite and hematite.

18 All analyses identified the red material as hematite.

19 hotoelectrochemical (PEC) water splitting by hematite.

20 ce layer of the nonmagnetic iron oxide-phase hematite.

21 chanically denatured MtrC molecules bound to hematite.

22 l tens of percent of the rock by weight, and hematite.

23 ltrafast electron transfer from aluminium to hematite.

24 duction kinetics and extents of goethite and hematite.

25 g fundamental insight into the reactivity of hematite.

26 M day(-1); rates were less with goethite and hematite (0.66 and 0.71 muM day(-1), respectively).

27 oxidation reaction on the fully hydroxylated hematite (0001) surface.

28 FT calculations confirmed that Fe(II) on the hematite (001) surface, created by interfacial electron

29 iferromagnetically coupled iron dimer on the hematite (110) surface, analogous to that of the methano

30 The Pb(II)-binding mechanism on an annealed hematite (1102) surface was studied using crystal trunca

31 ose a stoichiometry of Pb(II) binding on the hematite (1102) surface which indicates proton release t

32 i NWs absorb photons that are transparent to hematite (600 nm < lambda < 1100 nm) and convert the ene

33 show that the reaction between aluminium and hematite, a common iron oxide, can be tracked with femto

34 ry changes during the treatment period using hematite, a model Fe INP, suspended in filtered field wa

35 via char gasification and the employment of hematite, a natural iron resource greatly extended the a

36 III) (oxyhydr)oxides goethite, magnetite and hematite added as potential nucleation sites.

37 ns, were involved in sulfate reduction, with hematite addition increasing the sulfate recycling or th

38 sulfate in all experiments (with and without hematite addition) suggests that oxidized forms of iron,

39 nstrated Ni(II) cycling through goethite and hematite (adsorbed Ni incorporates into the mineral stru

40 ite (alpha-Fe(2)O(3)) mixed with TiO(2) than hematite alone.

41 ngsten grown by atomic layer deposition on a hematite alpha-Fe(2)O(3)(0001) surface, we report direct

42 py (XPS) and using the Mn(II) oxygenation on hematite (alpha-Fe(2)O(3)) and anatase (TiO(2)) NPs as a

43 Here, using hematite (alpha-Fe(2)O(3)) as a model system, we show ho

44 odeling, and this study investigated natural hematite (alpha-Fe(2)O(3)) as an economical and sustaina

45 ed that RNA hydrolysis was also catalyzed by hematite (alpha-Fe(2)O(3)) but not by aluminum-containin

46 Hematite (alpha-Fe(2)O(3)) constitutes one of the most p

47 Uniform thin films of hematite (alpha-Fe(2)O(3)) deposited by atomic layer dep

48 igated the sorption of silicate to colloidal hematite (alpha-Fe(2)O(3)) in short-term (48 h) and long

49 Hematite (alpha-Fe(2)O(3)) is a promising photoanode mat

50 Hematite (alpha-Fe(2)O(3)) is the most studied artificia

51 r growth response to ilmenite (FeTiO(3)) and hematite (alpha-Fe(2)O(3)) mixed with TiO(2) than hemati

52 persion/aggregation of three morphologies of hematite (alpha-Fe(2)O(3)) nanoparticles in varied aqueo

53 ce between Burkholderia cepacia biofilms and hematite (alpha-Fe(2)O(3)) or corundum (alpha-Al(2)O(3))

54 Hematite (alpha-Fe(2)O(3)) was grown on vertically align

55 putrefaciens strain CN-32 to the surface of hematite (alpha-Fe(2)O(3)) was studied with in situ ATR-

56 Mg-doped hematite (alpha-Fe(2)O(3)) was synthesized by atomic lay

57 hest external quantum efficiency measured on hematite (alpha-Fe(2)O(3)) without intentional doping in

58 tors that include solid metal oxides such as hematite (alpha-Fe(2)O(3)).

59 a widely used water splitting material, bulk-hematite (alpha-Fe(2)O(3)).

60 ature and reduce Cr(VI) to form chromite and hematite (alpha-Fe(2)O(3)).

61 IP) in a dynamic column containing nanosized hematite (alpha-Fe(2)O(3)).

62 Hematite (alpha-Fe2 O3) is engineered to improve photoex

63 Using hematite (alpha-Fe2O3) as a model oxide, we show through

64 study investigated heteroaggregation between hematite (alpha-Fe2O3) colloids and citrate-capped gold

65 ly induced surface potential gradient across hematite (alpha-Fe2O3) crystals is sufficiently high and

66 homogeneous case, goethite (alpha-FeOOH) and hematite (alpha-Fe2O3) increased and gamma-alumina (gamm

67 Hematite (alpha-Fe2O3) is one of the most common iron ox

68 ier recombination in Si-doped nanostructured hematite (alpha-Fe2O3) photoanodes as a function of appl

69 emical performances for water splitting over hematite (alpha-Fe2O3) photoanodes.

70 ction of time and plutonium concentration in hematite (alpha-Fe2O3) suspensions containing initially

71 adsorbed to lepidocrocite (gamma-FeOOH) and hematite (alpha-Fe2O3) was assessed when exposed to aque

72 Here, growth of hematite (alpha-Fe2O3) within a silica hydrogel resulted

73 g afresh a popular and viable photocatalyst, hematite, alpha-Fe2O3 that exhibits most of the properti

74 ext, titanium dioxide (TiO2) and iron oxide (hematite, alpha-Fe2O3) are among the most investigated c

75 ction in soils enriched with goethite and/or hematite, among which in dryland soils microbial sulfate

76 the work associated with water flipping, on hematite, an earth abundant OER semiconductor associated

77 Here, we report hematite, an earth-abundant material, to be highly effec

78 tions ultimately results in the formation of hematite, analysis of the atomic pair distribution funct

79 This structural composite of hematite and angelellite-like clusters represents a new

80 understanding of uranium incorporation into hematite and define the nature of the bonding environmen

81 In the presence of both hematite and Fe(2+)((aq)), NTO was quantitatively reduce

82 goethite)(-1)) were >5-fold higher than with hematite and ferrihydrite; monophosphorylated ribonucleo

83 esses were investigated for Ni adsorption to hematite and goethite at pH 7 in the presence of oxalate

84 nning electron microscopy indicate that both hematite and goethite have been transformed into magneti

85 uring the crystallization of ferrihydrite to hematite and goethite was explored in a range of systems

86 containing two commonly studied iron oxides-hematite and goethite-and aqueous Fe2+ reached thermodyn

87 formation after band gap excitation in alpha-hematite and identify the three underlying d-d transitio

88 ond order in the density of surface holes on hematite and independent of the applied potential.

89 orption spectra indicated that U(IV) in both hematite and lepidocrocite suspensions was not in the fo

90 elta(56)Fe) and Ni (delta(60)Ni) isotopes in hematite and magnetite, alongside bulk-rock and in-situ

91 water redox potentials and the band edges of hematite and many other low-cost metal oxides, enabling

92 id conditions in the Atacama Desert, rich in hematite and mudstones containing clays such as vermicul

93 Coarse crystalline hematite and olivine-rich basaltic sands were observed a

94 with ground, dark red-to-black fragments of hematite and pyrite.

95 sorptive interactions of organic matter with hematite and reductive release of hematite-bound organic

96 position and conformation on its sorption by hematite and release during the reduction reaction were

97 solution, and its interaction with insoluble hematite and small organic ligands, demonstrate the fund

98 he multihole catalysis of water oxidation by hematite, and demonstrates the hole accumulation level r

99 or K-feldspar, magnetite, quartz, anhydrite, hematite, and ilmenite.

100 an those reported for reduction of goethite, hematite, and lepidocrocite by S. oneidensis, and the or

101 ds, nanofibers, nanowires) based on titania, hematite, and on alpha-Fe2O3/TiO2 heterostructures, for

102 ce of SRNOM at pH values where Cit-AuNPs and hematite are oppositely charged, attachment efficiencies

103 s the dominant oxidation state of uranium in hematite around Eh -0.24 to -0.28 V and pH 7.7-8.6 for a

104 cobalt-based molecular cubane cocatalysts on hematite as a model system.

105 U(V), but not U(IV), was also detected in hematite at Eh +0.21 V (pH 7.1-7.3).

106 rimental conditions predict the formation of hematite at pH < 7.50 and magnetite at pH > 7.50, explai

107 of Tc(IV)-Tc(IV) dimers onto a Fe oxide like hematite at pH 6.00 +/- 0.07, and Tc(IV) incorporation i

108 f the lowest turn-on potentials observed for hematite-based PEC water splitting systems.

109 e heavily cratered terrains and underlie the hematite-bearing plains explored by the Opportunity rove

110 osed in a valley and plateau to the north of hematite-bearing plains.

111 The strength of the OmcA-hematite bond was approximately twice that of the MtrC-h

112 ond was approximately twice that of the MtrC-hematite bond, but direct binding to hematite was twice

113 We found that hematite-bound aliphatic carbon was more resistant to re

114 ion over a 16 h period triggers oxidation of hematite-bound CIP into byproducts.

115 atter with hematite and reductive release of hematite-bound organic matter.

116 onsumption of S(-II)aq proceeded slower with hematite, but yielded maximum dissolved U concentrations

117 ndamental dependencies in lead adsorption to hematite by coupling extended X-ray absorption fine stru

118 alyst affecting the nucleation and growth of hematite by modifying the Fe(2+)(aq)/Fe(3+)(aq) ratio at

119 bsence of water on the surface of magnetite, hematite, calcite, and dolomite nanoparticles (NPs) was

120 To explore whether doped hematite can exhibit an even lower overpotential, we con

121 c iron arsenate with structural relations to hematite, can epitaxially intergrow along the (210) plan

122 e thermodynamically more stable goethite and hematite changed from complete and fast to incomplete an

123 Dating of the hematite clasts verified the occurrence of a ~2.2 to 2.0

124 Our result indicates that a 1% hematite coating on a silica surface inhibited catechol

125 colloids is similar to that of goethite and hematite colloids.

126 hat Cr is present as Cr(3+) substituted into hematite, consistent with TEM analysis.

127 The generated hematite contained 97.3% Fe(2)O(3), 0.64% ZnO and 0.58%

128 structures composed of a submicrometer cubic hematite core (alpha-Fe(2)O(3)) and nanostructured silic

129 grown on cubic, rod-like, and peanut-shaped hematite core particles, we validate the argument.

130 ite dates and therefore cannot be related to hematite crystallization and ore formation.

131 Subsequent analyses on mixed goethite and hematite crystallization products (pH 9.5 and 11) showed

132 adsorption, the incorporation of As into the hematite crystals can be of great relevance for As immob

133 e presence of As (up to 1.9 wt %) within the hematite crystals could be demonstrated.

134 The force measurements for the hematite-cytochrome pairs were compared to spectra colle

135 hosphate mineral dates overlap with obtained hematite dates and therefore cannot be related to hemati

136 ology conclusively links all major preserved hematite deposits to a far younger (1.4 to 1.1 Ga) forma

137 ion of charge carrier self-localisation in a hematite device, and demonstrate that this process affec

138 o reveal new photophysics of broadly-studied hematite devices.

139 tion and by spectroscopically monitoring the hematite dissolution front in the micromodel.

140 nerals, including hypersthene, magnetite and hematite, distributed in a light matrix of a resin.

141 We introduce a self-propelled colloidal hematite docker that can be steered to a small particle

142 The hematite dockers are simple single-component particles a

143 pproximately 3000 ppm) was incorporated into hematite during ferrihydrite aggregation and the early s

144 incorporation of Np(V) into the structure of hematite during its crystallization from ferrihydrite (p

145 -substituted goethite and Zn(II)-substituted hematite during reaction with aqueous Fe(II).

146 ase from Ni- and Zn-substituted goethite and hematite during reaction with Fe(II).

147 lect and store photogenerated holes from the hematite electrode.

148 In the present study we prepared thin film hematite electrodes by atomic layer deposition to study

149 impedance spectroscopy in investigations of hematite electrodes to provide key parameters of photoel

150 enhances the water-splitting performance of hematite electrodes.

151 recombination phase to recombination of bulk hematite electrons with long-lived holes accumulated at

152 Additional clusters of irregular hematite ellipsoids could reflect abiotic processes of s

153 copies show that the association of DOM with hematite enhances the cleavage of aromatic groups during

154 on of Fe with aluminum, and the detection of hematite (Fe(2)O(3)) by micro-X-ray diffraction.

155 f dissolved cerium increases the porosity of hematite (Fe(2)O(3)) formed via fluid-induced, redox-ind

156 Hematite (Fe(2)O(3)) is an important magnetic carrier mi

157 ynthesized using a H(2)S plasma to sulfurize hematite (Fe(2)O(3)) nanorods deposited by chemical bath

158 tect whether a specific bond forms between a hematite (Fe(2)O(3)) thin film, created with oxygen plas

159 We studied NTO reduction by the hematite-Fe(2+) redox couple to assess the importance of

160 m in the presence of a ferric oxide mineral, hematite (Fe2O3), resulted in enhanced glucose decomposi

161 e formation of magnetite (Fe3O4) rather than hematite (Fe2O3).

162 ort images of centimeter-size, autochthonous hematite filaments that are pectinate-branching, paralle

163 h and Cit-AuNPs are capable of destabilizing hematite following an "electrostatic patch" mechanism.

164 It addresses a critical challenge of using hematite for PEC water splitting, namely, the fact that

165 ltra-thin monolayer of a molecular Ir WOC to hematite for solar water splitting in acidic solutions.

166 xide precipitates was observed, resulting in hematite formation after 7 days.

167 0(+3), and 1.08 x 10(+2) L (mol min)(-1) for hematite, goethite, and gamma-alumina, respectively.

168 t minerals containing significant Fe and Mn (hematite, goethite, magnetite, and groutite) adsorbed Pu

169 ntmorillonite and a range of other minerals (hematite, goethite, magnetite, groutite, corundum, diasp

170 the destruction of magnetic ordering at the hematite --> Rh(2)O(3)-II type (RhII) transition at 70 G

171 mmobilization of U(VI) by incorporation into hematite has clear and important implications for limiti

172 ulk electrochemical properties, acid-treated hematite has significantly decreased surface electron-ho

173 Stable phases such as goethite and hematite, however, can undergo reductive recrystallizati

174 ncement that typically precedes formation of hematite in aerobic soil and weathering environments.

175 ged presence of S(-II)aq in experiments with hematite in combination with a larger release of adsorbe

176 Reductive dissolution of hematite in porous media was investigated using a microm

177 The hematite in the micromodel was reduced by injecting pH-v

178 ed evidence that uranium was incorporated in hematite in uranate, likely octahedral coordination.

179 at mineralogical changes to ferrihydrite and hematite induced by radiation may lead to an increase in

180 enic nanoparticles formed through the fungus-hematite interactions can behave as mimetic catalysts, s

181 l pH values, goethite, amorphous iron oxide, hematite, iron-coated sand, and montmorillonite that wer

182 how that Zn incorporated in the structure of hematite is associated with coupled O-Fe and protonated

183 Hematite is concentrated in spherules eroded from the st

184 Hematite is the most abundant surficial iron oxide on Ea

185 n with the incorporation of silicon into the hematite lattice and propagate through to the nanoscale

186 standing-wave atomic images relative to the hematite lattice show dramatic (but redox-reversible) ch

187 (oxyhydr)oxide minerals such as goethite and hematite leads to rapid recrystallization marked, in pri

188 for a coating on the rock Mazatzal, where a hematite-like sextet is present.

189 Here, we demonstrate that hematite links physically separated redox reactions by c

190 Comparisons between different phases (hematite, maghemite, and ferrihydrite) revealed that sho

191 natural mineral particles (basalt, granite, hematite, magnetite, mica, milky quartz, and clear quart

192 ds with high oxygen fugacities, close to the hematite-magnetite buffer, that can contain significant

193 shown that iron oxides, such as goethite and hematite, may recrystallize in the presence of aqueous F

194 e broadly studied model protein BSA onto the hematite mineral surface was characterized as a function

195 Fe(2+) and thereby raising pe, and by making hematite more negatively charged and hence impeding NTO

196 nstrate the successful production of endless hematite nanocomposite fibers which highlights this tech

197 dation efficiency for the myriad of possible hematite nanoparticle morphologies and more broadly help

198 sing two different structurally well-defined hematite nanoparticle morphologies.

199 rbon nanotubes (CNTs) and positively charged hematite nanoparticles (HemNPs) were obtained over a bro

200 Hematite nanoparticles are abundant in the photic zone o

201 Here we show that incorporation of a hematite nanorod array into a plasmonic gold nanohole ar

202 can suppress the charge recombination in the hematite nanorod photoanode in a photoelectrochemical ce

203 g single-crystal but porous alpha-Fe(2)O(3) (hematite) nanowires via topotactic transformation.

204 Hematite nodules have been reported also from the Meridi

205 had the highest adsorption (Magnetite NPs > Hematite NPs > Calcite NPs > Dolomite NPs).

206 Fe (oxyhydr)oxides (predominant goethite and hematite) on OC storage and stabilization under natural

207 Compared with hematite-only photoelectrodes, those with Si NWs exhibit

208 et silicates (approximately 20 to 30%)], and hematite; only minor jarosite is identified in Mini-TES

209 docrocite, 2-line ferrihydrite, goethite and hematite) over an environmentally relevant pH range (4-8

210 ption fine structure (EXAFS) spectroscopy on hematite particles (10 and 50 nm) with resonant anomalou

211 95% of the initial Fe content was removed as hematite particles with diameters of approximately 200 n

212 ibiotic with two sets of synthetic nanosized hematite particles, with relatively smooth (H10, 10-20 n

213 further enables the preparation of a stable hematite/perovskite solar cell tandem device, which perf

214 n as a function of surface hole density on a hematite photoanode employing photoinduced absorption sp

215 Hematite photoanodes are promising for the oxygen evolut

216 set potential for photocurrent generation in hematite photoanodes is typically ~500 mV anodic of flat

217 as required for water photoelectrolysis with hematite photoanodes, observed following surface treatme

218 uppression of electron-hole recombination in hematite photoanodes.

219 in film and high-aspect ratio nanostructured hematite photoanodes.

220 thodic shift of the appearance of long-lived hematite photoholes, due to a retardation of electron/ho

221 Here, we validate pigmentary hematite ("pigmentite") as a proxy indicator for the Lat

222 Hematite plays a decisive role in regulating the mobilit

223 and arsenite sorption was studied by use of hematite pre-equilibrated with silicate for different ti

224 ycled via an integrated acid dissolution and hematite precipitation method.

225 ore resistant to reduction release, although hematite preferred to sorb more aromatic carbon.

226 ses investigated, with the only exception of hematite, present at least two distinct reactive pools w

227 ication of the Maastricht-Belvedere finds as hematite pushes the use of red ochre by (early) Neandert

228 In situ hematite U-Pb geochronology on hematite-quartz veins, which crosscut and are cut by Tav

229 Anodic bias significantly retards hematite recombination dynamics, and causes the appearan

230 couple and 769 +/- 2 mV for the aqueous Fe2+-hematite redox couple.

231 calculation of electron transfer) suggested hematite reduction as a proton-consuming reaction effect

232 was either added (type I) or formed through hematite reduction by dithionite (type II).

233 e in the rate and extent of ferrihydrite and hematite reduction by S. oneidensis in the presence of a

234 Such maintenance of a stable pH through hematite reduction for enhanced glucose fermentation com

235 nts and rates of ferrihydrite, goethite, and hematite reduction over a range of negative reaction fre

236 xperiment was also performed to estimate the hematite reduction rate under the well-mixed condition.

237 that thermodynamics controlled goethite and hematite reduction rates.

238 Hematite remains a prominent photoanode candidate for th

239 wever, Cu release and Co and Mn release from hematite require the sum of two rates to adequately mode

240 Diagenetic features include hematite-rich concretions and crystal-mold vugs.

241 The size of hematite-rich concretions decreases up-section, document

242 water, strata with smaller and more abundant hematite-rich concretions than those seen previously, po

243 Eolian ripples, armored by well-sorted hematite-rich grains, pervade Meridiani Planum.

244 Hematite-rich spherules are embedded in the rock and ero

245 croscopic images support the hypothesis that hematite-rich spherules observed in outcrops and soils a

246 e-grained basaltic sand and a surface lag of hematite-rich spherules, spherule fragments, and other g

247 tion, with continued uptake occurring during hematite ripening.

248 Hematite's common (001) and (012) facets are frequently

249 us research groups have attempted to improve hematite's photocatalytic efficiency despite a lack of f

250 Acid-treated hematite showed a substantially enhanced photocurrent de

251 Goethite and hematite showed increased solubility at arid RH, but no

252 temperature Mossbauer spectrum of irradiated hematite shows the emergence of a paramagnetic Fe(III) p

253 Mini-TES spectra show only a hematite signature in the millimeter-sized spherules.

254 The reduced surface of a natural Hematite single crystal alpha-Fe(2)O(3)(0001) sample has

255 to dehydroxylation and leads to formation of hematite skins on serpentinite particles, slowing down s

256 tion mechanisms on a pure (1x1) hydroxylated hematite slab (corresponding to 1/3 ML of reactive sites

257 A sub-picosecond reorganisation of the hematite structure has been proposed as the mechanism wh

258 attributed to trace amounts of Fe(II) in the hematite structure.

259 where CH(4) is activated by reaction with a hematite surface oxygen first, followed by a catalytic c

260 change in protonation or in coordination to hematite surface sites as pH is modified.

261 mation of inner-sphere coordinative bonds to hematite surface sites.

262 a Ga(2)O(3) overlayer, reported to passivate hematite surface states.

263 The polymerization of silicate on the hematite surface was monitored by attenuated total refle

264 f P-based bacterial functional groups to the hematite surface.

265 eferential coordination of P-moieties at the hematite surface.

266 pecific bond between each cytochrome and the hematite surface.

267 ater structures upon U(VI) adsorption at the hematite surface.

268 enic can be immobilized by adsorption to the hematite surface; however, the incorporation of As in he

269 The condensation of silicate on hematite surfaces adsorbed from monomeric silicate solut

270 inner-sphere adsorption modes for all three hematite surfaces and additionally revealed outer-sphere

271 The reaction energetics on pure or doped hematite surfaces are described using a volcano plot.

272 Co- or Ni-doped hematite surfaces give the most thermodynamically favore

273 sphere bidentate complex formation of CIP at hematite surfaces in 0.01 M NaCl, irrespective of pH and

274 forms a well-defined monomolecular layer on hematite surfaces, where it assumes an orientation that

275 te, in ferrihydrite systems, and siderite in hematite systems.

276 activity; Zn release is more pronounced from hematite than goethite, whereas the opposite trend occur

277 rpentines, chlorite, smectite, goethite, and hematite) the isotopic exchange and metal-solid interact

278 When grown on n-type hematite, the p-type layer was found to create a built-i

279 e, whereas above the absorption band edge of hematite, the surface plasmon polariton launches a guide

280 y studied photoanode systems: nanostructured hematite thin films.

281 For unbiased hematite, this recombination exhibits a 50% decay time o

282 The addition of hematite to these microcosm experiments resulted in sign

283 Adding soil amendments (olivine, hematite) to the paddy soil had no effect on Sb and As c

284 apparent optical band gap dropped from 2.2 (hematite) to ~1 eV (pyrite), with completely converted l

285 In situ hematite U-Pb geochronology on hematite-quartz veins, wh

286 The buffering effect of hematite was further supported by a greater extent of gl

287 surface; however, the incorporation of As in hematite was never seriously considered.

288 U(VI) doped hematite was synthesized and exposed to two different or

289 he MtrC-hematite bond, but direct binding to hematite was twice as favorable for MtrC.

290 hite side with an orange mix of goethite and hematite, was abandoned after breakage at Cueva Anton, 6

291 cattering (SAXS), and its interaction at the hematite-water interface by neutron reflectometry.

292 The Np(V) reactions at the hematite-water interface were comprehensively investigat

293 phosphate (TSP), and bone meal biochar] and hematite were applied at a molar ratio of Pb:Fe/P = 1:5.

294 reactive iron minerals such as magnetite and hematite were applied.

295 anced picture of the coordination of lead to hematite while also providing fundamental insight into t

296 the particle size decreased for goethite and hematite, while for magnetite, the relative solubility w

297 The phase transformation to hematite will result in less available surface area for

298 ation of schwertmannite to a nanocrystalline hematite with greater surface area and smaller particle

299 he soil were mainly crystalline goethite and hematite, with lesser amounts of poorly crystalline ferr

300 ease the extent of reaction with goethite or hematite, with no reoxidation in this case.