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1 erials including gypsum, anhydrite, marl and limestone.
2 higher than that measured for the reference limestone.
3 h was more than double the value achieved by limestone.
4 60% higher than that measured for Rheinkalk limestone.
5 as seen in Archaeopteryx from the Solnhofen limestone.
6 tent of modern ground waters in contact with limestones.
7 content increased the high reactivity of the limestones.
8 ity of CaO sorbent derived from four natural limestones.
11 same fjord, reductions being largest for the limestone (50-90%) followed by clay (50-70%), and the AC
12 e used to maintain neutral pH, after initial limestone addition to achieve neutral pH, thus maintaini
13 residual trapping of supercritical CO2 in a limestone altered to a mixed-wet state with oil was sign
14 in Neoproterozoic (1.0-0.542 Ga) and younger limestones altered under the influence of ground waters,
15 s (8.5 and 12.0 MPa) for scCO2-brine, and in limestone and dolomite sands at 23 degrees C (0.1 MPa) f
16 ata indicate that slightly thicker layers of limestone and dredged clay can show as good physicochemi
17 f plant photoassimilate to weather grains of limestone and silicates each with a combined calcium and
18 uses solid CaO sorbent derived from natural limestone and takes advantage of the reversible reaction
19 orrelation between insoluble elements in the limestone and the marls, which indicates a similar compo
23 magnitude of F(-) sorption by HA-coated-fine limestone are comparable to those of pure HA, and the F(
29 errestrial chromite grains in mid-Ordovician limestone can be used to constrain in detail the tempora
30 c hominin species that occupied Liang Bua, a limestone cave on Flores in eastern Indonesia, during th
32 a vidalii, first recovered from lithographic limestone deposits in the Pyrenees of Spain more than 10
34 ar isotopic characteristics and carry mainly limestone-derived and anthropogenic Sr and Nd as well as
38 ury from the suspensions of the gypsums, the limestones enriched in iron increased Hg(0) re-emission
41 rom mid-Ordovician approximately 470 Myr-old limestone >100 fossil L-chondritic meteorites have been
42 reef builders or producers of shallow marine limestones have generally corresponded in mineral compos
43 on the multicyclic CO2 capture of a natural limestone in a fixed bed at CaL conditions as affected b
47 tforms, indicating that reworking of crustal limestone is an important source of volcanic carbon.
48 use of naturally occurring CaCO(3), that is, limestone, is the rapid decay of its CO(2) capture capac
49 e An. scanloni is restricted to 'islands' of limestone karst habitat, this suggests there is a metapo
51 A different, inorganic bone deposit on a limestone ledge in Sawmill Sink is a Late Pleistocene ow
52 ology over multiple reaction cycles, whereas limestone lost its initial nanostructured morphology rap
56 chemical (XRF) data, to evaluate whether the limestone/marl couplets reflect an original cyclic signa
57 rare cases where chitinozoans differ between limestone/marl facies are deemed insufficient for the id
60 by early diagenetic calcite, from bituminous limestone of the 551- to 542-mega-annum Dengying Formati
61 iserial arranged modular units), from marine limestone of the 551-541 Ma Dengying Formation in South
62 antiornithine bird from the Lower Cretaceous limestones of Las Hoyas, Spain, which reveals the overal
63 composition, particle size, and porosity of limestones on their reactivity and the effect of sorbent
64 influence of the effect of the properties of limestones on their reactivity and the re-emission of me
65 sisted of a passive material (coarse or fine limestone or a marine clay) and an active material (acti
66 ither tightly bound to the impurities of the limestone or was transformed into insoluble mercury spec
67 le Ordovician (480 million years ago) marine limestone over an area of approximately 250,000 square k
68 uscan amphoras (ca. 500-475 B.C.) and into a limestone pressing platform (ca. 425-400 B.C.) at the an
71 binary blends were investigated, three with limestone (reference mixes) and three with the CaL spent
72 ng (CaL) spent sorbent (i) can be a suitable limestone replacement in the production of both ordinary
73 estone whereas complete regeneration for raw limestone requires a minimum calcination temperature of
74 e HP and SHP surface coatings for increasing limestone resistance to sulfation, and thus retarding gy
75 and imbibition Pc-Sw curves were measured in limestone sands at 45 degrees C under elevated pressures
76 e have extracted fossil micrometeorites from limestone sedimentary rock that had accumulated slowly 2
77 (KT) boundary was discovered in the pelagic limestone sequence at Gubbio on the basis of 12 samples
79 s and positive delta18O excursions in marine limestones suggest that glaciation events may have punct
80 re able to excavate carbonate minerals, from limestone to biogenic carbonates, including coral reefs,
81 rometer sized HA on the surfaces of granular limestone to improve the sorption efficiency of the HA-b
82 as a function of rock type, with granite and limestone tombstones from the same cemeteries harbouring
85 rformed core flooding experiments on Indiana limestone using the porous plate method to measure the a
88 tolerance and chemotaxis, while bacteria on limestone were more likely to be lichen associated and h
89 evelopment of a fracture network in a porous limestone when cooling to -9.7 degrees C, at which an ex
90 es C in short residence times for the milled limestone whereas complete regeneration for raw limeston
91 nt marine carbonate sediments and of ancient limestones, which contain unique records of changes in o
92 to micrometer sized HA crystals on granular limestone with the maximum surface coverage at lower pH
93 y suggest that the use of highly crystalline limestones would be detrimental since excessively high c
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