Results 121 to 130 of about 14,765 (196)

Modification of Illite Structure by Differential Treatment

open access: yes
Commonly illite is described as a clay mica with a general composition of [KxAlx(Si4-xAlx)O10 (OH)2 (where 0 ...
Seglins, Valdis   +2 more
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Effect of humic acid on radiocesium sorption in illite

open access: yes, 2008
Radiocesium is one of the major contaminants released by nuclear facilities to the environment. Knowledge of the behavior of cesium (Cs) in the soil environment is important for assessing radionuclide mobility in soil and potential crop uptake.
内田 滋夫   +11 more
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Mineralogical analyses in Peştera Polovragi (Olteţului Gorges) and Peştera Muierii (Galbenului Gorges), Gorj county

open access: yesTravaux de l'Institut de Speologie Emile Racovitza, 2009
Following a series of cave mineralogy researches in Peştera Polovragi and Peştera Muierii, Gorj County, we evidence an association made up of hydroxylapatite, taranakite, calcite and secondarily of quartz and illite and respectively, of hydroxylapatite ...
GABRIEL DIACONU   +2 more
doaj  

Radiocesium sorption behavior on illite, kaolinite, and their mixtures

open access: yes, 2008
Clay minerals are one of the most important components in soil for radiocesium sorption. There are many types of clay minerals in soil, and their capacities for cesium (Cs) sorption differ.
452483   +17 more
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Mineralogical researches in "Peștera cu Lilieci din satul Peștera", Bran-Rucăr Passage

open access: yesTravaux de l'Institut de Speologie Emile Racovitza, 2008
By means of X-rays diphractometric analyses on powders, we evidence an association of minerals in “Peştera cu Lilieci din satul Peştera”, made up of hydroxylapatite(carbonate-hydroxylapatite), brushite, taranakite, calcite, quartz, illite and ...
GABRIEL DIACONU   +2 more
doaj  

A method for quantifying detrital illite from crystallite thickness measurements

open access: yes, 2005
Illite crystals in siliciclastic sediments are heterogeneous assemblages of detrital material coming from various source rocks, and, at paleotemperatures >70 °C, of superimposed diagenetic modifications of this sediment (MERRIMAN & KEMP, 1996).
ALDEGA, Luca, EBERL D. D.
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