kaolinite in Czech

kaolinit Entry edited by: B2

Sentence patterns related to "kaolinite"

1. Antigorite (massive serpentine), chlorite, kaolinite, Bementite, and brushite interfere

2. INTERFERENCES: Antigorite (massive serpentine), Chlorite, Kaolinite, Bementite, and Brushite interfere

3. In addition to montmorillonite and illite another common clay species that is sometimes dominant is kaolinite.

4. Samples of kaolinite, illite, and montmorillonite were consolidated from slurries containing chemical dispersant and flocculating agents.

5. Kaolinite has a low shrink–swell capacity and a low cation-exchange capacity (1–15 meq/100 g).

6. It is found that the residual soil possesses greater adsorption capacity compared to that of kaolinite.

7. By adding only 5% kaolinite in the Calcination process, the dealkalization rate could be increased to 100%.

8. The frost susceptibility of well-graded crushed aggregates increases with increasing fines content and increasing kaolinite fraction.

9. By adding only 5% kaolinite in the calcination process, the dealkalization rate could be increased to 100%.

10. The predominant clay mineral constituents in lake muds from both regions include smectite, illite-smectites and lesser kaolinite.

11. Ball clays usually contain three dominant minerals: from 20–80% kaolinite, 10–25% mica, and 6–65% quartz.

12. The region is characterized by permafrost, and smectite and kaolinite are the common authigenic clay minerals in the soils.

13. Minerals identified in the soils included smectites in the vertisol, kaolinite, quartz, hydromica, albite and biotite in the luvisols and Arenosol.

14. That absolute accumulation can occur in non-Mn-bearing weathering horizons (kaolinitic horizons) to form Mn nodules in which kaolinite is dissolved.

15. The main minerals are quartz, feldspar (andesine), clay minerals (montmorillonite, illite, Kaolinite) and the carbonate minerals (calcite, Mg-calcite, aragonite).

16. Authigenic kaolinite in sandstone occurs most commonly as fragile aggregates of crystals between sand grains, in vugs, along fractures, and as grains

17. High-reactivity metakaolin Admixture – High-reactivity metakaolin Admixture (or HRMK) is a highly processed aluminosilicate pozzolanic mineral, derived from the clay mineral kaolinite

18. Allothigenic clay minerals, particularly of the platy type (kaolinite, hy- dromica, chlorite, montmorillonite, vermiculite), are characterized by isometrical Fig.5. Allothigenic hydromica, Lower Devonian, Volga-Ural region

19. The competitive effect of equimolar Arsenate on arsenite adsorption was small and apparent only on kaolinite and illite in the pH range 6.5 to 9

20. The crystals occur in the disequilibrium assemblage calcite – phengite (2M1) – margarite – quartz – kaolinite – epidote –apatite found in Badshot marble from the almandine garnet zone of regional metamorphism.

21. Those sinters are formed of opal-A that replaced microbes, opal-A precipitated as cement, accessory minerals (e.g., kaolinite, jarosite, calcite), biological detritus (e.g., leaves, wood, pollen grains), and lithic detritus.

22. The western slope of the Queensland Plateau and the western Coral Sea Abyssal Plain very likely have received terrigenous components also from mainland Australia as indicated by admixed kaolinite.

23. In the volcanic region of Gleichenberg trachytes and trachyandesites of Miocene age are altered by postvolcanic activities, which cause the formation of kaolinite and smectite minerals as well as alunite and opal.

24. Bauxites are residually enriched rocks, mostly composed of Al-hydroxides (gibbsite, boehmite and diaspore), kaolinite, Fe-oxy-hydroxides and Ti-oxides, which form from intense lateritic weathering of aluminosilicate protoliths

25. The adsorbent may be produced by treating a suitable layered clay, e.g. a kaolinite, an attapulgite, a sepiolite or a smectite, with a strong acid under controlled conditions followed by washing to a controlled degree.

26. That absolute accumulation can occur in non-Mn-bearing weathering horizons (kaolinitic horizons) to form Mn nodules in which kaolinite is dissolved. This process provides Al which combines to Mn3+ forming Al-Mn hydroxides (lithiophorite).

27. The latitic rock mined at the Gossendorf open pit in the Gleichenberg Volcanic Area of Styria, Austria, has in places been completely altered to various associations of the secondary minerals opal-C/-CT, alunite, kaolinite and montmorillonite.

28. The weathering rate of albite was calculated to be 2.16 μmol L–1 yr–1 with the resulting formation of 3.3 μmol L–1 yr–1 of kaolinite and 0.047 μmol L–1 yr–1 of calcite.

29. They are very diverse: from rendzina soils to red soils (Rotlehm); from silt to pure clay; from siallitic (high silica content) residues to allitic (very low silica content) formations; from clays rich in kandite-minerals (kaolinite, halloysite) to bauxites containing gibbsite boehmite.

30. The clay-sized (< 2 μm) fraction of the silty and arenaceous lutites constituting CESAR cores 14 and 103 (Alpha Ridge, central Arctic Ocean) is composed predominantly of mica (40–60%), with subequal percentages (10–20%) of kaolinite and chlorite and lesser amounts (< 5%) of smectite, quartz, plagioclase, and potassium feldspar.