Size-related mineralogical and surface physicochemical properties of the mineral particles from the recent sediments of the Eastern Adriatic Sea

Ivanić, Maja; Durn, Goran; Škapin, Srečo D.; Sondi, Ivan

doi:10.1016/j.chemosphere.2020.126531

Cited by 16 publications

(2 citation statements)

References 59 publications

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“…For the soil we studied, the SSA determined by the methylene blue method is 30.5 cm 2 /g. This value is close to those determined for soils of similar composition, which can vary from 11.3 to 27.8 m 2 /g [34]. In general, the methylene blue method widely used by researchers when they do not have the possibility to use the BET, to have an approximate value of the SSA [35][36][37].…”

Section: Resultssupporting

confidence: 77%

Physico-chemical, mineralogical, and technological characterization of stabilized clay bricks for restoration of Kasbah Ait Benhadou- Ouarzazate (south-east of Morocco)

Lechheb¹,

Harrou²,

Boukili³

et al. 2022

Materials Today: Proceedings

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Section: Resultssupporting

confidence: 77%

Physico-chemical, mineralogical, and technological characterization of stabilized clay bricks for restoration of Kasbah Ait Benhadou- Ouarzazate (south-east of Morocco)

Lechheb¹,

Harrou²,

Boukili³

et al. 2022

Materials Today: Proceedings

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“…The higher share of MLCM in Calcocambisol/colluvium compared to marine lake sediment supports this proposal. The absence of chlorite in the sediment from Malo Jezero (IVANIĆ et al, 2020) is probably the result of local soil distribution/erosion and the fact that the marine lake sediment in this study was sampled closer to the lake shore, whereas in the case of Malo Jezero the sediment was sampled in the deeper part of the lake.…”

Section: Mineral Composition Of the Analyzed Samplesmentioning

confidence: 78%

The relationship between the geochemical and mineralogical characteristics of Calcocambisol, colluvium and recent marine lake sediment of the narrow seashore intertidal zone: a case study from the Veliko Jezero (Mljet Island, Croatia)

Ružičić¹,

Durn²,

Sondi³

et al. 2021

Geol Cro

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This study investigates the mineral composition, particle size distribution and geochemical characteristics of Calcocambisol, colluvium and recent marine lake sediment in a narrow intertidal seashore zone of the Veliko Jezero on the Island of Mljet (Croatia). The obtained results show that the fractions of Calcocambisol/colluvium less than 2 mm and 2 μm display similar particle size distribution (PSD) curves compared to marine lake sediments containing larger particles in these fractions. The smallest fractions of the investigated materials that are less than 1 μm show identical PSD curves. The bulk and clay mineral composition of the marine lake sediment show that the non-carbonate fraction is derived from weathering of the surrounding soils and colluvium containing quartz, feldspars and phyllosilicates (illitic material, kaolinites, chlorite, and a mixedlayer clay mineral, MLCM), as well as the authigenic formation of early-diagenetic pyrite, while one part is related to the yield of material by aeolian deposition (amphibole). The observed difference between the phyllosilicate mineral phases in the clay fraction of the Calcocambisol/colluvium and the carbonate-free clay fraction of the marine lake sediment is related to 1) the presence of chlorite in the marine lake sediment and 2) the higher content of MLCM in the Calcocambisol/colluvium. The chlorite in the marine lake sediment was inherited from the Calcocambisol/colluvium as a result of soil erosion prior to its complete destabilization in the soil. High Chemical Index of Alteration (CIA) values in the Calcocambisol and colluvium clearly indicate their intense weathering. Based on the Sm/Nd and Ti/Al ratios, it can be concluded that the aluminosilicates in the Calcocambisol, colluvium and marine lake sediment are of the same provenance. The distribution of each analysed element among the sequential fractions is very similar in both the Calcocambisol and colluvium. The highest concentrations for most of trace elements in the Calcocambisol, colluvium and marine lake sediment was determined in their residual fraction. Mn, Co and Pb show a different partitioning between the Calcocambisol/colluvium and marine lake sediment, respectively.

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Assessment of the physico-chemical characteristics and elemental properties of water and sediments from Owan river in Edo State, Nigeria

Akinnusotu

Justinah

Felix

et al. 2021

Int J Energ Water Res

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Size-related mineralogical and surface physicochemical properties of the mineral particles from the recent sediments of the Eastern Adriatic Sea

Cited by 16 publications

References 59 publications

Physico-chemical, mineralogical, and technological characterization of stabilized clay bricks for restoration of Kasbah Ait Benhadou- Ouarzazate (south-east of Morocco)

Physico-chemical, mineralogical, and technological characterization of stabilized clay bricks for restoration of Kasbah Ait Benhadou- Ouarzazate (south-east of Morocco)

The relationship between the geochemical and mineralogical characteristics of Calcocambisol, colluvium and recent marine lake sediment of the narrow seashore intertidal zone: a case study from the Veliko Jezero (Mljet Island, Croatia)

Assessment of the physico-chemical characteristics and elemental properties of water and sediments from Owan river in Edo State, Nigeria

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