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Cretaceous-paleogene boundary clays from Spain and New Zealand: arsenic anomaly and the Deccan Traps

100%

Premovic P. I.

tom 55

High arsenic (As) contents have been reported in numerous Cretaceous-Paleogene boundary (KPB) clays worldwide including those from Spain (at Caravaca and Agost) and N. Zealand (at Woodside Creek). The Deccan Traps (India) enormous volcanism is one of the interpretations which have been offered to explain this anomaly. This report shows that the estimated surface densities of As in the boundary clays in Spain and New Zealand strongly contradict that anomalous As was sourced by this volcanic event.

The influence of the mineral composition of the clay fraction on zinc sorption in rendzina soils

100%

Zagorski Z.

nr 1

Zinc sorption was tested through four mineralogically diverse clay fractions of rendzina soils. The value and mechanisms of Zn sorption are strictly linked to the mineralogical composition of the clay fraction. Analysis of the variation of the buffer coefficient da/dCe, calculated according to the Freundlich isotherm, indicates that the fractions containing prevailing quantities of smectite, illite or kaolinite sorb Zn exchangeably (not specifically). Zn bonding in the smectite fraction is feeblest. The fraction containing opal CT adsorbs Zn permanently (specifically).

Porównanie właściwości ekspansywnych iłów neogeńskich z Mazowsza

84%

Gawriuczenkow I. , Wójcik E.

Przegląd Geologiczny

2013

tom Vol. 61, nr 4

243--247

Development of building projects in the Mazovia region causes the risk of their location on the soils of specific expansive properties. These properties, expressed as swelling or shrinkage, are a serious engineering problem. Many methods are used for the evaluation ofexpansiveness; both direct and indirect test methods are used. Tests were performed on clays from the areas of Warsaw, Dobre near Mińsk Mazowiecki and Mszczonów. Comparative analysis of expansive properties of Neogene clays is based on the results of laboratory tests of mineral composition, grain size distribution, moisture content, free swelling and swelling pressure. The tests have shown that the expansive properties ofclays from the Mazowsze region can have extremely high values, which causes the needfor individual determination of potential expan-siveness for different types of clays, depending on moisture content, swelling pressure and chemistry of the environment.

The effect of removal of organic matter, iron oxides and aluminum oxides on the micropore characteristics of the soil clay fraction

67%

Jozefaciuk G. , Sokolowska Z.

nr 2

111-119

Surface-micropore properties of the clay fractions of several soils before and after removal of a particular clay fraction components: organic matter, iron oxides and aluminum oxides were studied with an application of the water vapor adsorption-desorption method. Changes in micropore radii, volumes and fractal dimensions were observed after the removal of each component.