Alteration of secondary minerals along a time series in young alkaline soils derived from carbonatic wastes of soda production

Grünewald, Gritta; Kaiser, Klaus; Jahn, Reinhold

doi:10.1016/j.catena.2007.03.022

Cited by 18 publications

(14 citation statements)

References 23 publications

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“…LDH is a class of ionic lamellar minerals with positively charged hydroxylated layers of divalent and trivalent metallic cations ([M II 1−x M III x (OH) 2 ] x+ ) and exchangeable hydrated gallery anions ([X q− x/q ·nH 2 O]) [26]. The neoformation of LDH may occur in alkaline soils [27][28][29][30][31] and they can be regarded as good representatives of the oxide/hydroxide soil mineral family.…”

Section: Introductionmentioning

confidence: 99%

Enhancing atrazine biodegradation by Pseudomonas sp. strain ADP adsorption to Layered Double Hydroxide bionanocomposites

Alekseeva

Prevot

Sancelme

et al. 2011

Journal of Hazardous Materials

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Section: Introductionmentioning

confidence: 99%

Enhancing atrazine biodegradation by Pseudomonas sp. strain ADP adsorption to Layered Double Hydroxide bionanocomposites

Alekseeva

Prevot

Sancelme

et al. 2011

Journal of Hazardous Materials

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“…Examples of spontaneous plant succession on soda waste sedimentation tanks can be observed in Germany near Bernburg [10,11] and in the Czech Republicnear Petrovice [13,32]. There are sedimentation tanks where the development of vegetation derived from spontaneous succession, which has lasted for over 70 years, can be seen.…”

Section: Spontaneous Successionmentioning

confidence: 92%

Selected aspects of reclamation of soda waste landfill sites.

Urbańska¹,

Urbański²

2012

geom

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“…Changes in redox conditions related to wetting/drying cycles also contribute to the formation of Fe-Mn concretions and/or coatings (e.g., Huot et al, 2014a;Sokolov et al, 2015) as well as the weathering of iron artefacts (e.g., nails: Howard et al, 2013Howard et al, , 2015. Carbonation, by reaction with atmospheric and microbial CO 2 , may occur during the early stages of weathering of alkaline materials (e.g., Grünewald et al, 2007). The weathering of glass in poorly crystalline aluminosilicates has been reported in soils formed in fly ash (e.g., Zevenbergen et al, 1999;Zikeli et al, 2002) and in iron industry by-products (e.g., Sauer and Burgardt, 2006;Huot et al, 2014a).…”

Section: Similar Processes Of Soil Formation From Technogenic and Natmentioning

confidence: 99%

Pedogenetic Trends in Soils Formed in Technogenic Parent Materials

2015

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Soils formed in technogenic parent materials are proliferating and their pedogenesis remains inadequately understood. Upon investigation of soils formed in various technogenic materials reported in the literature and of a Technosol developing on iron industry deposits, potential specificities of pedogenesis within technogenic materials are discussed. Analyses have shown that pedogenetic processes observed in these soils are similar to those occurring in natural soils. However, some particularities have been highlighted, such as the coexistence of processes rarely encountered simultaneously in natural environments or high rates of soil development during the first stages of weathering. Technogenic materials display highly diverse constituents, wide spatial variability, and temporal discontinuities as a result of human activities. These inherent features, in interaction with other soil-forming factors, may govern the pedogenesis by generating the following conditions: i) a high diversity of pedogenetic processes, including processes occurring usually in dissimilar climatic regions, ii) localized processes and distinct rates and orientations of soil development over short distance and iii) a succession and/or a superimposition of processes, constrained by the deposition of materials and human operations. This creates the potential for the simultaneity of processes coexisting rarely in natural soils developing in the same climatic region. These soils are likely to have a polycylic evolution and to evolve towards groups of soils other than Technosols, depending on the dominant processes. Further investigations of the processes and their potential interactions occurring in a larger range of soils formed in technogenic materials are required to better predict the evolution of these soils.

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Alteration of secondary minerals along a time series in young alkaline soils derived from carbonatic wastes of soda production

Cited by 18 publications

References 23 publications

Enhancing atrazine biodegradation by Pseudomonas sp. strain ADP adsorption to Layered Double Hydroxide bionanocomposites

Enhancing atrazine biodegradation by Pseudomonas sp. strain ADP adsorption to Layered Double Hydroxide bionanocomposites

Selected aspects of reclamation of soda waste landfill sites.

Pedogenetic Trends in Soils Formed in Technogenic Parent Materials

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