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Clay-Humus Complex _ clay-humus complex — Deutsch Übersetzung

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Übersetzungen für clays im Englisch » Deutsch-Wörterbuch (Springe zu Deutsch » Englisch) Ergebnis-Übersicht clay I. Nomen II. Nomen ˈboul·der clay Nomen clay ˈpi·geon Nomen ˈclay shoot Nomen clay mineral Nomen clay mud clay soil Nomen clay ˈpi·geon shoot Nomen clay ˈpi·geon shoot·ing Nomen clay-humus complex Nomen Zur In soil systems, C is stored in the recalcitrant pool as clay-humus complexes resulting in the development of stable soil aggregates. Moreover, it is also physically protected within the aggregate, making it less available to microbes for further degradation. Therefore, soil C stabilization is prerequisite for SOC sequestration.

Humification of leaf litter and formation of clay-humus complexes Compost which is readily capable of further decomposition is sometimes referred to as effective or active humus, though again scientists would say that if it is not stable, it’s not humus at all. clay-humus complex Die Bodengare, optimale Bodenstruktur, wird durch das Bodenleben mit der Bildung von Ton – Humus – Komplexen extrem nachhaltig gefördert!

Clay, Humus, Loam, Mulch, Sand, Silt, Soil

22. Clay – Humus Complex There are two types of linkages take place in formation of clay-humus formation 1. Stable linkage: Being held together by

clay-humus complex — Deutsch Übersetzung

The complex chemical and biochemical interactions of HSs in soils are also responsible for improving soil quality and maintaining soil fertility. The dissociation of H + ions mostly from carboxyl and phenolic groups creates negative sites Soil management systems that encourage the formation and stabilization of recalcitrant clay–humic complexes will have the greatest long-term impact on C sequestration and soil quality. The objective

Ton-Humus Komplex ist die Übersetzung von „clay-humus complex” aus dem Englisch ins Deutsch. Beispiel eines übersetzten Satzes: This is about the Clay-Humus-Complex and the almost natural raw materials. ↔ Toolisan enthält viele Spurenelemente in ausgewogenem Verhältnis, ist reich an organischer Substanz und besitzt den vielfachen Humuswert gegenüber

Cations at the particle surface of the clay–humus complex are strongly polarized. Cationic polarization has a critical role in humus‐increased

Similarly, chemical phenomena like adsorption and desorption of heavy metals (e.g. Zn, Cd, Pd etc.), and fixation of P and K depend on a great extent on soil mineralogy, especially clay mineralogy. Clay minerals form bonds of varying strengths with soil humus resulting in clay-humus complexes of varying stability.

  • Studies on decomposition of humus in clay-humus complexes
  • clay-humus complex — Deutsch Übersetzung
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  • What is Humus in Soil? Formation, Importance and Much More!

Many translated example sentences containing „clay-humus complex“ – French-English dictionary and search engine for French translations. The clay-humus complex as described in soil study refers to the formation of aggregates of organic fragments such as humic substances with inorganic particles such as clay minerals.

Übersetzung im Kontext von „clay-humus complex“ in Englisch-Deutsch von Reverso Context: The formation of a continuous clay-humus complex is thereby supported, increasing soil fertility. Some aspects of clay-humus complex-ation Effect of exchangeable cations and lattice charge. Soil Sci. 151,220-227. [Pg.144] Jung (1943) was one of the earlier workers on clay-humus complex formation. His results indicated that sesquioxides of Fe and A1 play an important part in binding the humus to clays.

Clay-humus complexation: Effect of pH and the nature of bonding

Clay soil: everything you need to know | Green Renewables

In humus, different nutrients are bound together with clay minerals through adsorption processes. This association of organic fragments such as humic substances with inorganic particles such as clay minerals is usually called the “clay-humus complex.” Without minerals, a true humus formation would not be possible. PDF | The effects of the pH variation on the complexation of humic substances by dried clay-humus systems were investigated. The amounts of FA (fulvic | Find, read and cite all the research you

While the clay minerals and the humic acid residues (organic dipoles) of the humus particles are negatively charged, the Ca2+ ion or other polyvalent cations, for example Mg2+, form a neutralising bridge. The resulting organo-mineral compounds are known as clay-humus complexes (CHC) or lime-clay-humus complexes. Summary Decomposition studies with humic acids (HAs) present in HA-clay complexes revealed that such decomposition decreases at higher clay concentrations. At high clay concentration, moreover, it Formation of clay–humus complex is also important for aggregation. Chemical transformations include solution, hydration, hydrolysis, oxidation, reduction, carbonation, and other acid reactions.

The results indicate that the biochemistry of the clay-humic complexes differs substantially from that of whole soils and that soil clay mineralogy strongly influences humification.

Carbon content of humus complex, C t, at a time t, after desorption of humus from clay humus complex was fitted to a simple first order equation. Ct=C0 exp-kt C t = Carbon content of humus complex at a time t. C 0 is the initial C content and k

Chapter 9 The Interaction of Organic Matter with Clays

Alexandrova (1958, 1960 suggested that three groups of these compounds be distinguished: i) humates and fluvates of strong bases, ii) complex aluminium ± and iron-humus compounds, and iii) products of their interaction with soil containing fractions with different particle sizes, Kononova (1963) cites the last classification proposed by A major fraction of HA (in clay-humus complexes) shows thermal destabilisation due to multiple attachments on the clay surface; a small fraction is also thermally stabilised by ionic bonding with Ca 2+ /Mg 2+ and absence of ring strain in the complex. Only the Alfisol HA does not show thermal stabilisation in the complex. A semi-stable, intimate mixture of silicate clay minerals and humus having colloidal properties that largely determine the nature and fertility of soils. In temperate environments, the clay-humus complex results largely from the passage of soil and organic matter through the gut of earthworms. The resulting worm cast is slightly calcareous and has an intimate association of

Clay-humus complexes from 5 different soils (Entisol, Alfisol, Vertisol, and 2 Mollisols) were isolated by aqueous dispersion. Humic acid (HA) extractable from the complexes by alkali solutions ranging from pH 8 to 14, before and after acid pretreatment, were studied. Extraction by alkali solutions alone was not very effective except with the Alfisol sample. 2002.40, 691-703 Soil clay—humus complexes. l. Alkali dissolution, T EM, and XRD studies Nayan .4hmeaAC, Chandrika VaradachariHD Kuna/ Gho.s/rA ADepartment Of Chemistry Soil Science, University

Toolisan developed a clay-humus-complex in the soil and thus prevents a soil depletion, promotes the soil fertility and the optimum soil composition sustained! Zahlreiche Übersetzungsbeispiele nach Fachgebieten geordnet für clay-humus complex – Englisch-Deutsch Wörterbuch und smarter Übersetzungsassistent.

[Biological stability and physical behaviour of a clay-humus complex in different calcium and potassium saturations]. [French] 来自 AGRIS 喜欢 0 阅读量: 37

Investigate the influence of soil microorganisms and enzymes on cation bridging in clay-humus complexes, enhancing our understanding of microbial contributions to soil structure and organic matter stability. A chemical method based on batch desorption of adsorbed humus on clay-humus complex by sodium hydroxide-sodium pyrophosphate solution was used to assess the stability of humus C through the desorption rate constant using simple first order exponential equation in a toposequence of Western Himalaya region of India. The rate constant values were significantly A cation, which is usually Ca +2 or Fe +2, forms a bridge between clay minerals and organic polymers to hold them together. Ca +2 gives very strong bonds that are very stable, which impede very rapid mineralisation of humic SOM and oppose dispersion of the clays (Figs. 7.3 and 7.4). 2. The humus-Ca 2+ clay complex gives the soil its dark colour, which is often