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Organic mineralization

Development work by Russian workers had led to interesting products formed by reaction of furfuryl alcohol with acetone and with aniline hydrochloride. The resins formed in each case have been found to be useful in the manufacture of organic-mineral non-cement concretes with good petrol, water and gas resistance. They also have the advantage of requiring only a small amount of resin to act as a binder. [Pg.813]

The products of thermal decomposition of organic-mineral fertiliser mixtures were studied by IR spectroscopy, and implications for fire and explosion hazards considered. [Pg.1680]

Ultrastructural patterns that arise when amino acids or small peptides interact with mineral surfaces have been studied in some detail99,100). A poly-L-alanine solution evaporated at 40 °C on a rhombohedral plane of R-quartz deposits the peptide principally in a-conformation. Chain-folded helices are aligned in the form of lamellae which exhibit a sharp phase boundary at the organic-mineral contact zone (Fig. 9). Frequently the lamellae are split along the direction of their fold axis ("zipper effect ). Insertion of 0-pleated sheets running perpendicular to the long axis of the lamellae act as dispersion forces and cause the formation of cross-0-... [Pg.14]

Schulten, H.-R., and Leinweber, P. (2000). New insights into organic-mineral particles composition, properties and models of molecular structure. Biol. Fertil. Soils 30, 399 432. [Pg.142]

Organic-Mineral Particle Size, Density, and Aggregate Fractions 565... [Pg.539]

Figure 14.13. Proportions of compound classes in organic-mineral particle-size fractions of long-term fertilization experiments in Germany. The gray areas indicate the largest and smallest proportions of these compound classes found by Py-FIMS of other particle-size fractions. Figure 14.13. Proportions of compound classes in organic-mineral particle-size fractions of long-term fertilization experiments in Germany. The gray areas indicate the largest and smallest proportions of these compound classes found by Py-FIMS of other particle-size fractions.
Figure 17.17. Principal component analysis map of sample (left) and color-coded spectra (right) from a sample of marine suspended particulate matter. The lower three spectra are characteristic of low organic mineral phases, while the upper three organic phases have distinctively different C-NEXAFS spectra. Background regions are shown in black (J. Brandes, unpublished data 2007). See color insert. Figure 17.17. Principal component analysis map of sample (left) and color-coded spectra (right) from a sample of marine suspended particulate matter. The lower three spectra are characteristic of low organic mineral phases, while the upper three organic phases have distinctively different C-NEXAFS spectra. Background regions are shown in black (J. Brandes, unpublished data 2007). See color insert.
Oxidizable carbon OXC Easily oxidizable OC, not stabilized in organic—mineral complexes... [Pg.226]


See other pages where Organic mineralization is mentioned: [Pg.342]    [Pg.430]    [Pg.56]    [Pg.213]    [Pg.475]    [Pg.431]    [Pg.462]    [Pg.463]    [Pg.474]    [Pg.512]    [Pg.515]    [Pg.464]    [Pg.509]    [Pg.540]    [Pg.541]    [Pg.541]    [Pg.565]    [Pg.566]    [Pg.568]    [Pg.568]    [Pg.578]    [Pg.144]    [Pg.568]    [Pg.38]   
See also in sourсe #XX -- [ Pg.296 ]




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Abiotic organic reactions at mineral

Abiotic organic reactions at mineral surfaces

Adsorption of Ionized Organic Compounds from Aqueous Solutions to Charged Mineral Surfaces

Clay minerals organic matter

Kinetics organic mineralization

Lignins organic minerals

Mediated mineralization, biogenic organisms

Mineral surfaces abiotic organic reactions

Mineral weathering organic acid role

Mineral-organic layers

Mineralization of Organic Nitrogen

Mineralization of organic phosphorus

Mineralization organic halides

Mineralization organic nitrogen

Mineralization toxic organic compounds

Mineralized organisms, nanoscale

Minerals organic complexes

Minerals soil organic matter, clay

Model Organic Species and Explosives with Clay Minerals

Nitrogen compounds organic minerals

Nuclear magnetic resonance organic minerals

Organic ammonium cation exchange, clay minerals

Organic and Inorganic Stains for Raw Feed Mineral Identification

Organic carbon mineralization rate

Organic cation exchange, clay minerals

Organic complexes with clay minerals

Organic complexes with clay minerals cations

Organic compounds minerals

Organic mater mineralization

Organic matter mineralization

Organic matter mineralization rate

Organic matter on minerals

Organic molecule-mineral surface

Organic reactions clay minerals

Organic-mineral compartment

Organic-surface interactions, oxide minerals

Regulators of Organic Nitrogen Mineralization

Regulators of Organic Phosphorus Mineralization

Silicate minerals structural organization

Soil organic carbon biomass mineralization

Soil organic carbon mineralization kinetics

Structural organization in silicate minerals

Substrate-Induced Organic Phosphorus Mineralization

Sulfate Reduction and Organic Carbon Mineralization

Surface mineral, abiotic organic

The Organic Matrix, Mineral Phase and Bone Mineralization

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