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1 multaneous co-sorption of As(V) and Sb(V) to jarosite.
2 d in Sb(V) being sequestered by newly formed jarosite.
3 ring the transformation of schwertmannite to jarosite.
4 s ferric arsenate (AFA), schwertmannite, and jarosite.
5 etic behavior for the AV(3)(OH)(6)(SO(4))(2) jarosites.
6                                              Jarosite, a common mineral in acidic sulfur-rich environ
7 rts per trillion to 100 parts per billion in jarosite, a sulfate-rich mineral associated with liquid
8                             The presences of jarosite-alunite group minerals were found in the lower
9 y diffraction, for verifying the presence of jarosite-alunite group minerals.
10 3(OH)6(SO4)2, along with the selenate-capped jarosite analogues of potassium, KFe3(OH)6(SeO4)2, and r
11  at the Tl L3-edge, partly Tl(I)-substituted jarosite and avicennite (Tl2O3) were identified as Tl-be
12 h secondary Mn (birnessite) and Fe minerals (jarosite and goethite), which together accounted for nea
13                                       Both K-jarosite and heated PLJ-treated samples were investigate
14 Cu, and Zn are associated with metal-bearing jarosite and other minerals (e.g., clays, Fe-(oxy)hydrox
15 unity identified the ferric sulphate mineral jarosite and possible relicts of gypsum at the Meridiani
16 A four-step extraction procedure to quantify jarosite and schwertmannite separately with various solu
17 ification of the fractions of Tl(III), Tl(I)-jarosite and Tl(I)-illite in bulk samples based on XAS i
18                                              Jarosites and schwertmannite can be formed in the unsatu
19 m poorly crystalline phases, hydrated salts, jarosite, and clays.
20                                              Jarosites are produced during metallurgical processing,
21                            The solubility of jarosite at near-neutral pH and biogeochemical processes
22 isms controlling As(V) and Sb(V) sorption to jarosite at pH 3 (in dual and single metalloid treatment
23 loped for the preparation of a new series of jarosites, AV(3)(OH)(6)(SO(4))(2) (A = Na(+), K(+), Rb(+
24 f K-jarosite is expected to be key to future jarosite-based soil Pb remediation method development.
25                                              Jarosite can be an important scavenger for arsenic (As)
26  that Fe(2+)-induced transformation of As/Sb-jarosite can increase Sb mobility and exert major influe
27 nt a new approach for the preparation of the jarosite class of compounds, which for the past several
28             We conclude that the presence of jarosite combined with residual basalt at Meridiani Plan
29 hetic methods to future magnetism studies of jarosite compounds.
30                          Below 1000 m depth, jarosite crystals adhering on residual silica-rich parti
31                   Well-developed pseudocubic jarosite crystals formed surface coatings, and in some i
32           Measurements on a diamagnetic host jarosite doped with magnetically dilute spin carriers, K
33 vironment and Tl is readily released from Tl-jarosite during both abiotic and biotic dissolution.
34       Despite the environmental relevance of jarosites, few studies have examined their biogeochemica
35                                              Jarosite formation is thus thought to require a wet, oxi
36 ce and supports the ice-weathering model for jarosite formation on Mars, highlighting the geologic im
37   We report a multi-analytical indication of jarosite formation within deep ice.
38 ot proceed to completion, and that following jarosite formation, arid conditions must have prevailed.
39                                              Jarosite-group minerals may incorporate multiple interla
40 perature resulted in increased conversion to jarosite-group minerals, but addition of potassium (K) j
41 hat relies on converting soil Pb and As into jarosite-group minerals, such as plumbojarosite (PLJ) an
42  examined the dissolution of synthetic Tl(I)-jarosite, (H(3)O)(0.29)Tl(0.71)Fe(2.74)(SO(4))(2)(OH)(5.
43                                    On Earth, jarosite has been found to form in acid mine drainage en
44 ter in hydrated minerals, such as gypsum and jarosite, has numerous applications in studies of recent
45                                    The V(3+) jarosites have been characterized by single-crystal X-ra
46  is needed to verify that schwertmannite and jarosite in the pit sediment do not convert to goethite,
47      We show that all magnetic properties of jarosites, including LRO, find their origin in the basic
48                    The newfound utility of K-jarosite is expected to be key to future jarosite-based
49 mately 20 to 30%)], and hematite; only minor jarosite is identified in Mini-TES spectra.
50 results indicate, for the first time, that K-jarosite may successfully convert soil Pb to PLJ without
51       When subjected to reducing conditions, jarosite may undergo reductive dissolution, thereby rele
52 ammonium sulphate yielding shwertmannite and jarosite minerals.
53 n of a new series of stoichiometrically pure jarosites of the formula, AV(3)(OH)(6)(SO(4))(2) with A
54                                          But jarosite on Earth only persists over geologically releva
55  of abiotic Fe(2+)-induced transformation of jarosite on the mobility, speciation, and partitioning o
56 Cu, with minor amounts of Cu associated with jarosite or goethite.
57 V) during the dissolution of synthetic Pb-As jarosite (PbFe(3)(SO(4),AsO(4))(2)(OH)(6)) by Shewanella
58 ound Sb(V), while highlighting the role that jarosite plays in controlling the Sb(V) mobility and fat
59                                     The iron jarosites, plumbojarosite, Pb0.5Fe3(OH)6(SO4)2, argentoj
60 ining magnetostructural correlations for the jarosites possessing various interlayer cation and cappi
61 rating conditions of the ammonium salt-based jarosite process.
62                       Samples treated with K-jarosite promoted Pb transformation to low-bioaccessibil
63                                        These jarosites represent the first instance of strong ferroma
64                                     All iron jarosites show long-range order (LRO), signified by a sh
65 ctions included Sb(V) incorporation into the jarosite structure via partial Sb(V)-for-Fe(III) substit
66 ia bidentate corner-sharing complexes on the jarosite surface when Sb(V) was absent or present at low
67 te minerals (including magnesium sulfate and jarosite) that constitute several tens of percent of the
68 tic techniques on the magnetic properties of jarosites, the V(3+) jarosites were also prepared accord
69  AFe3(OH)6(SO4)2 (A = Na+, K+, Rb+ and NH4+) jarosites, these compounds provide a framework for probi
70 entojarosite, AgFe3(OH)6(SO4)2, and thallium jarosite, TlFe3(OH)6(SO4)2, along with the selenate-capp
71 (10 and 20 mM) rapidly (<10 min) transformed jarosite to a green rust intermediary, prior to the subs
72 trigger the Fe(2+)-induced transformation of jarosite to more stable Fe(III) minerals, such as goethi
73 ions; therefore, we probed the potential for jarosite to remediate Pb via intercalation by reacting p
74                             Our methods of K-jarosite treatment yielded <10% Pb and As bioaccessibili
75 sorption mechanisms of Sb(V) versus As(V) to jarosite under acidic environmental conditions.
76 hwertmannite is metastable and transforms to jarosite under strongly acidic conditions.
77                                              Jarosite was found to sorb Sb(V) to a greater extent tha
78 roup minerals, but addition of potassium (K) jarosite was most critical to Pb and As bioaccessibility
79  magnetic properties of jarosites, the V(3+) jarosites were also prepared according to the nonredox t
80  ferric compounds, mainly schwertmannite and jarosite, which settled to the bottom of the lake.
81 ion by reacting presynthesized potassium (K)-jarosite with aqueous Pb and/or Pb-contaminated soil at
82 ave been proposed to explain the presence of jarosite within Martian surficial sediments, including t