Titlebook: Effect of Mineral-Organic-Microorganism Interactions on Soil and Freshwater Environments; J. Berthelin,P. M. Huang,F. Andreux Book 1999 Sp

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浮夸

Comparison Between Bacterial and Chemical Dissolution of al-Substituted Goethite. Incidence on Mobilay also form as a result of steel corrosion. While pure iron oxides may be obtained synthetically, natural iron oxides generally contain noniron metals (NIM), particularly Al. The solubility of iron oxides in pure water is generally extremely low (Schwertmann, 1991). However, Fe oxides dissolution i

腐爛

Preparation and Thermodynamic Equilibria of Green Rusts in Aqueous Solutions and their Identificatio66; Allmann, 1968) corresponds to the stacking of brucite-like layers carrying a positive charge and layers constituted of anions and water molecules. In this paper, we deal with the Fe(II)-Fe(III) compounds generally known by the generic name of Green Rusts, GRs, since the original classification b

BRAVE

An Xps and Afm Coupled Study of Air and Bio-Oxidized Pyrite Surfacesue to acid mine drainage and soil and water pollution by heavy metals. Many chemical reactions, including natural metal leaching and industrial metal recovery, involve bacteria: sulfide oxidation by . is a typical example. Frequently, bio-oxidation of sulfides is described in terms of pure biologica

猜忌

Transformation of Iron-Containing Minerals in Kaolin During Growth of a Mixed Bacterial Culture Deri as impurities. Iron in kaolins occurs in the form of goethite, hematite, hydrogoethite, magnetite, and pyrite, or as iron oxide films on the surface of the silicate minerals, or it may be included in their crystalline lattices (Avgustinik, 1975).

Mutter

Effect of Succinic Acid Produced by Microorganisms and Plant Roots on Copper Sorption by Soil 1981, 1989). Sorption behavior of metals is dependent on interaction with various components of soil solution, especially chelating agents such as fulvic acid, aminoacids, organic acids, and phenolic compounds. Organic ligands are formed in soil during the decomposition of organic matter, root exud

Mutter

Interaction of Iron and Organic Matter in Relation to its Uptake by Plantspplication or foliar spray than FeSO4 in correcting iron deficiency in these soils characterized by alkaline pH and high CaCO3 content. Due to costs and irregular supply of the synthetic chelates in the market, crop production was affected. The addition of organic residues to these soils was found t

心胸開(kāi)闊

Effects of Organic Matter, Iron and Aluminium on Soil Structural Stability organic matter (OM), iron and aluminium oxides, colloidal silica or calcium carbonate (Baver et al., 1972). The relative importance of these stabilizing agents depends on their nature and abundance in the soil. Although there is a general agreement on the fundamental role that OM, Fe and Al play in

Infant

Interactions of Mugineic Acid with Allophane, Imogolite, Montmorillonite and Gibbsite. 1) (Takemoto .., 1978; Takagi, 1993). In our previous paper (Inoue ., 1993), we studied interactions between MA and Fe oxides in relation to the chemistry of Fe nutrition of graminaceous plants grown in Fe-deficient soil conditions.

leniency

Aluminum Speciation, Toxicity and Transfer from Soils to Surface Waters in Two Contrasting Watershedparticularly in the northeast United States (Driscoll and Van Dreason, 1993; David and Lawrence, 1996) and Central and Northern Europe (Ulrich .., 1980; Nilsson .., 1983; Rosseland and Henriksen, 1990; Matzner and Prenzel, 1992; DeVries .., 1995), including the north-east of France in the Vosges mou