The pozzolanic reaction between por

The pozzolanic reaction between portlandite and different types of nearly pure natural zeolites was studied.
Analcime, phillipsite, chabazite, erionite, mordenite and clinoptilolite-rich tuffs were mixed with portlandite
and water (1:1:2 by weight), and the progress of the pozzolanic reaction was quantitatively determined by
thermogravimetrical analyses from 3 to 180 days.
A thorough characterization of the raw materials was performed by quantitative XRD, XRF, SEM-EDX, BET
specific surface area measurements, grain-size analyses, FTIR and Cation Exchange Capacity measurements.
The difference in reactivity of the samples containing zeolites with varying Si/Al ratios, as well as between
clinoptilolite-rich samples exchanged with different cations or ground to different grain sizes was assessed.
The results indicate that the external surface area only influences the short-term reactivity, whereas the cation
content has an effect on both the long- and short-term reactivity. The early reactivity of the unexchanged
samples can be explained by these two parameters, but their long-term reactivity is mainly related to the Si/Al
ratio of the zeolites. Samples with zeolites rich in Si react faster then their Al-rich counterparts.
Офиолиты являются породами мантийного происхождения, которые кристаллизовались и консолидировались в подкоровых глубинах из перидотитового расплава, а впоследствии по глубинным разломам внедрились в виде протрузии в приповерхностные уровни земной коры, обходя океаническую обстановку. Термины офиолиты следует использовать в качестве названия гипербазитов, а не ассоциации пород из ультраосновного, габброидного, вулканического и базальтового комплекса подушечных лав и глубоководных пелагических глинистых и кремнистых осадков-радиоляритов океанического дна.

Результаты (английский) 1:

the pozzolanic reaction between portlandite and different types of nearly pure natural zeolites was studied.
analcime, phillipsite, chabazite, erionite, mordenite and clinoptilolite-rich tuffs were mixed with portlandite
and water (1:1:2 by weight), and the progress of the pozzolanic reaction was quantitatively determined by
thermogravimetrical analyses from 3 to 180 days.
a thorough characterization of the raw materials was performed by quantitative xrd, xrf, sem-edx, bet
specific surface area measurements, grain-size analyses, ftir and cation exchange capacity measurements.
the difference in reactivity of the samples containing zeolites with varying si / al ratios, as well as between
clinoptilolite-rich samples exchanged with different cations or ground to different grain sizes was assessed.
the results indicate that the external surface area only influences the short-term reactivity, whereas the cation
content has an effect on both the long-and short- term reactivity. the early reactivity of the unexchanged
samples can be explained by these two parameters,but their long-term reactivity is mainly related to the si / al
ratio of the zeolites. samples with zeolites rich in si react faster then their al-rich counterparts.
ophiolites are rocks of mantle origin,which crystallized and consolidated into subcrustal depths of peridotite melt and subsequently infiltrated in deep faults in the form of a protrusion in the surface levels of the crust,bypassing the oceanic environment. Terms ophiolites should be used as the title giperbazitov instead of ultramafic rock association, gabbroid,volcanic basalt complex and pillow lavas and deep-sea pelagic clay and siliceous sediments radiolarites-seafloor.

Результаты (английский) 2:

The pozzolanic reaction between portlandite and different types of nearly pure natural zeolites was studied.
Analcime, chabazite, phillipsite, mordenite, erionite and clinoptilolite-rich tuffs were mixed with portlandite
and water (1: 1: 2 by weight), and the progress of the pozzolanic reaction was quantitatively determined by
thermogravimetrical analyses from 3 to 180 days.
A thorough characterization of the raw materials was performed by quantitative XRD, XRF, SEM-EDX, BET surface area specific measurements of
, grain-size analyses, Cation Exchange Capacity and FTIR measurements.
The difference in reactivity of the samples containing zeolites with varying Si/Al ratios, as well as between
clinoptilolite-rich samples exchanged with different automotive products is responsible or ground to different grain sizes was assessed.
The results indicate that the external surface area only influences the short-term reactivity, whereas the cation
content has an effect on both the long-and short-term reactivity. The early reactivity of the unexchanged
samples can be explained by these two parameters, but their long-term reactivity is mainly related to the Si/Al
ratio of the zeolites. Samples with rich in zeolites Si react faster then their rich counterparts, Al-.
Ophiolites are the rocks of mantle origin, which got crystallized and consolidated in the podkorovyh depths of the peridotitic melt, and subsequently on the deep faults have a protrusion in near-surface layers of the Earth's crust, bypassing the oceanic environment. The term Ophiolite to use as the title of the giperbazitov, not the Association of ul′traosnovnogo rocks, gabbroidnogo, lava and basalt complex podušečnyh love and deep pelagic clay and siliceous sediments-radiolâritov of the ocean floor.

Результаты (английский) 3:

The pоzzоlаniс reaction between pоrtlаndite and different types of neаrly pure natural zeоlites was studied.
Anаlсime, phillipsite, сhаbаzite, eriоnite, mоrdenite and сlinоptilоlite-rich tuffs browsed mixed with pоrtlаndite
and water (1:1:2 by weight), and the progress of the reaction was quаntitаtively pоzzоlаniс greatly by
thermоgrаvimetriсаl analyzes from 3 to 180 days.
A is thorough сhаrасterizаtiоn of the raw materials was performed by quantitative XRD, XRF, SEM-EDX point, bet
specific surface area measurements, grain-size analyzes, FTIR and Cаtiоn exchange capacity measurements.
the difference in reасtivity of the samples соntаining zeоlites with vаrying Si/Al liquidity ratios include the following:, as well as between
Сlinоptilоlite-rich samples exсhаnged with different саtiоns or ground to different grain sizes'd аssessed.
The results indicate that the external surface area only influenсes the short-term reасtivity, whereаs the саtiоn
content has an effect on both the long- and short-term reасtivity. The early reасtivity of the unexсhаnged
samples can be explained by these two parameters,But their long-term reасtivity mаinly is related to the Si/Al ratio of the
zeоlites. Samples with zeоlites rich in Si react faster then their al-rich соunterpаrts.
Ophiolites are native species diocesan bishop origin,Which кристаллизовались and reside in the depths of the перидотитового подкоровых melt, and subsequently the underlying subduction have eaten in the form of a tentative electrophysical phenomena протрузии levels in earth's crust,Bypassing oceanic environment. Ophiolites terms should be used as the title sciences, and not association species from phoscorites was formed by juvenile solutions, габброидного,And volcanic basalt complex подушечных love and deep-sea pelagic clay and кремнистых rainfall-радиоляритов ocean-floor.