smectites oor Portugees
smectites
en
Plural form of smectite.
Vertalings in die woordeboek Engels - Portugees
esmectite
Bentonite: ≥ 70 % smectite (dioctahedral montmorillonite)
Bentonite: ≥ 70 % de esmectite (montemorilonite dioctaédrica)
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
voorbeelde
Advanced filtering
Voorbeelde moet herlaai word.
Bentonite: ≥ 70 % smectite (dioctahedral montmorillonite)
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Holden and Eberswalde, craters in Margaritifer Terra, are thought to have formerly held lakes because they contain deltas and iron/magnesium smectite minerals which need water to form.
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An old feature in this area, called Terra Sirenum lies in this quadrangle; Mars Reconnaissance Orbiter discovered iron/magnesium smectites there.
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A natural smectite was modified with Al-Ce solutions in the presence of Non-ionic surfactant (polyethilene oxide).
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Smectite-group minerals, products with #-amino-#-hydroxymethyl-#-propanediol
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MRO discovered iron/magnesium smectites here.
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Different variables in synthesis were evaluated in the modification of two pillared smectite clays with mixed solutions of Al-Fe-Ce.
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In general, the exchange capacity of the area’s soil is very good and provides the plants with the requisite amounts of nutrients, due to the presence of a high percentage of smectites in clay minerals, while there are high amounts of both exchange calcium and exchange magnesium.
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The results indicate that dioctahedral (aluminian) smectite is the principal component in the natural material.
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A set of nanostructured porous solids was synthesized by intercalation of TiO2 and Fe- TiO2 into the interlayer sites of a smectite clay mineral.
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To try to resolve this problem, materials type smectite have been modified with quaternary ammonium salts.
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In the present work, two experiments on adsorption of ammonia by smectite clays group, in synthetic and aquaculture wastewater, as well as for the farming of Rhamdia quelen under the influence of different temperatures have been developed.
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The main diagenetic processes in clastic sandstones and conglomerates and hybrid arenites are cementation and grain replacement by smectite, zeolites, calcite and dolomite, limited compaction and dissolution of feldspars, volcanic fragments and bioclasts.
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Unlike kaolinite, smectite has a high ion-exchange capacity and it releases potassium over time.
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The formation of kaolinite and illite from detrital smectites would have occurred under influence of subaerial exposure and pedogenesis.
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Most commercial bentonites contain more that 80% smectite, however, various other minerals can occur as impurities.
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The main processes responsible for porosity modification were the mechanical compaction, grain dissolution and eodiagenetic cementation by clayminerals (kaolinite or smectite) and carbonates (mainly dolomite/ankerite).
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Both kaolinite and smectite are essential for the fertility of floodplain soils (Junk et al., 2011).
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The smectite is responsible for the desirable properties of bentonite, but the nature of the exchangeable cations in the interlayer influences the properties too.
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The soils and suspensate had a similar composition, quartz, kaolinite, illite, and smectite, as well as anatase as an accessory mineral.
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The mineral meeting with the typical signature of Ucayali showed high percentages of smectite (~ 61%), kaolinite (~ 15%), chlorite (~ 8%) and illite (18%) and mineralogy by XRF suggests variability of most data, suggesting flood pulses during this period.
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However, very little is known about the stability of smectite (principal component of bentonite) under high-pressure and high-temperature conditions (HPHT).
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Volcaniclastic sandstones and conglomerates with intergranular porosity partially reduced by smectite rims and some grain dissolution may constitute fair hydrocarbon reservoirs.
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58 sinne gevind in 11 ms. Hulle kom uit baie bronne en word nie nagegaan nie.