Biological decomposition of fulvic acid preparations

Decomposition of preparations of various fractions of fulvio acids in pure cultures of bacteria and in the soil was investigated. In the soils enriched with fulvic acids the amount of bacteria increased, oxygen consumption and formation of carbon dioxide followed a typical sigmoid curve. The above measurements indicated that mineralization occurred after a very short or negligible lag phase. During the decomposition of fulvic acids the ability of microorganisms to oxidize aromatic compounds,e.g. vanillio andphydroxybenzoic acid, increased. The presence of aromatic structures in the used preparations of fulvic acids was demonstrated on the basis of their IR spectra and according to the results of Chromatographic analyses of their hydrolysates. The results indicated a relationship between metabolism offulvio acids and aromatic oompounds. In samples of the soil preincubated with glucose the fulvic acids decomposed more rapidly than in untreated samples.     

Hyphal growth and mycorrhiza formation by the arbuscular mycorrhizal fungus Glomus claroideum BEG 23 is stimulated by humic substances

Effects of humic substances (humic acid or fulvic soil extract) or saprophytic microorganisms (Paecilomyces lilacinus and an unidentified actinomycete) on growth of mycelium and mycorrhiza formation by Glomus claroideum BEG23 were studied in a hydroponic system. Humic substances stimulated root colonization and production of extraradical mycelium by the mycorrhizal fungus. Both humic and fulvic acids tended to decrease populations of culturable bacteria and fungi in the cultivation system, indicating a moderately antibiotic activity. The addition of saprophytic microorganisms able to use humic substances to the cultivation system further stimulated the development of the mycorrhizal fungus. However, stimulation of G. claroideum was also observed when the saprophytic microorganisms were heat-killed, suggesting that their effect was not linked to a specific action on humic substances. The results indicate that humic substances may represent a stimulatory component of the soil environment with respect to arbuscular mycorrhizal fungi.     

Photo-oxidation of dissolved organic matter for trace metal analysis

Abstract

Photo-oxidation of dissolved organic matter in saline and non- saline samples is monitored by measurement of residual fluorescence intensity. For fulvic acids, the method has a detection limit of 0.005 mg C L^?1, and maximum photo-oxidation is achieved with H₂O₂ oxidant and a low-intensity UV source.     

Effects of humic and fulvic acids on growth of tobacco

Summary Organic matter was extracted with a mixture of 0.1M Na₄P₂O₇ and 0.1M NaOH from soil and a commercial organic matter product, Aqua Humus, and separated into humic and fulvic acids according to their solubility in acid and alkaline solutions. They were purified by passage through a cation exchange resin, freeze-dried, and used for characterization and seedling growth studies. The CEC increased with pH for both humic and fulvic acids. Data from tobacco seedling studies show that humic and fulvic acids from both sources increased root number and length at low concentrations while at high concentrations, humic acids inhibited length and number of roots but fulvic acids had no effect. The results support the proposition that fractions of organic matter referred to as humic and fulvic acids affect root development by means other than as a source of nutrients.     

Is the computed speciation of copper in a wide range of Chinese soils reliable?

Free Cu species in soils is a key issue to its bioavailability. However, predictive models for Cu speciation across a wide range of soils were still unavailable. In this study, Cu speciation in 34 contaminated soil samples were investigated via analytical technique and predictive models. The results showed that most of free Cu²⁺ was underestimated when using default log K_CuFA and 65% active fulvic acid as inputs in models of WHAM VI and NICA-Donnan. The best prediction was found when using either adjusted active fulvic acid from 10% to 125% for WHAM VI or from 15% to 65% for NICA-Donnan model with the RMSE < 0.32 and r² > 0.96. In contrast, NICA-Donnan demonstrated a slightly stronger binding for Cu than WHAM VI due to extra 26% of samples was underestimated. This work presents a comprehensive database of Cu speciation and an effective attempt of free Cu²⁺ prediction in a wide range of Chinese soils.     

Contribution of bacterial cell nitrogen to soil humic fractions

Summary Living cells ofSerratia marcescens, uniformly labelled with¹⁵N, were added to samples of maple (Acer saccharum) and black spruce (Picea mariana) forest soils. After different periods of incubation from zero time to 100 days, the soils were subjected to alkali-acid and phenol extraction to provide humic acid, fulvic acid, humin and humoprotein fractions. Significant amounts of the cell nitrogen were recovered in the humic and fulvic acids immediately after addition. After incubation, less cell, nitrogen appeared in the humic acid and more in the fulvic acid. The amount of cell nitrogen recovered in the humin fraction increased with incubation. Roughly 5 to 10 per cent of the added cell nitrogen was found as amino acid nitrogen from humoprotein in a phenol extract of the humic acid. The data are consistent with the occurrence of co-precipitation of biologically labile biomass nitrogen compounds with humic polymers during the alkaline extraction procedure involved in the humic-fulvic fractionation.     

Evidence for the induction of catechol-1,2-oxygenase by fulvic acid

Summary The effect of fulvic acid on the growth of a benzoate-metabolizing Arthrobacter sp. has been studied. The Arthrobacter grew exponentially with benzoate and fulvic acid but if fulvic acid was omitted then growth was progressively slower and catechol accumulated. These results indicated that fulvic acid enhanced the synthesis of catechol-1,2-oxygenase. Catechol-1,2-oxygenase activity measurements support this suggestion. re]19750822     

Effect of a fulvic acid fraction on the growth of a Pseudomonas from Tjeukemeer (The Netherlands)

In this paper the effect of a fulvic acid fraction on the growth of a Pseudomonas sp. from fresh water is reported. The presence of fulvic acid in the culture medium caused an increase in the cell yield and in the cell yield per μl O₂ taken up by the Pseudomonas. The observed stimulating effect has been explained in terms of co-metabolism of fulvic acid by the Pseudomonas.     

Saponine als pflanzliche Pilzabwehrstoffe

Zusammenfassung 19 verschiedene Saponine und Saponingemische wurden gegen 15 Arten hauptsächlich pflanzenpathogener Pilze getestet. Dabei zeigten die Pilze unterschiedliche Empfindlichkeit, doch war keiner generell saponinresistent. Die fungistatische Wirkung auf eine Reihe von Pilzen tritt schon in einem Konzentrationsbereich ein, der oft noch unter dem tatsächlichen Saponingehalt zahlreicher Pflanzen liegt.

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Saponins as plant fungistatic compoundsOn the antibiotic action of saponins. III

Summary The action of 19 saponins and saponin fractions on 15 species of fungi, mostly plant pathogenes, was tested. The fungi showed different sensitivity, but no fungus was generally resistant to saponins. The fungistatic action on several species was observed at concentrations often below the real saponin content of many plants.

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Meinem verehrten Lehrer, Herrn Professor Dr. Dr. h. c. Dr. h. c. Richard Harder, zum 80. Geburtstag gewidmet.     

Spectroscopic properties of dissolved humic substances - a reflection of land use history in a fen area

The elemental composition and spectroscopic properties of dissolved fulvic acids isolated from different sampling media (topsoil, ground and surface water) of a natural fen area (high portion of organic soils) were examined to reveal the effects of land use history. These effects need to be known if dissolved humic substances are to be a major factor in identifying the impact of present and future changes in land use. Dissolved fulvic acids (topsoil, groundwater) from highly degraded peatlands (due to a long-term agricultural use) exhibit lower C/N ratios, higher absorption in the UV spectra, and higher absorption at 1,620 cm^–1 in the FTIR spectra compared with fulvic acids from relatively intact peatlands. These properties illustrate that long-term agricultural use with high inputs results in increased aromatic structures and a further humification of dissolved fulvic acids due to very strong peat decomposition compared with relatively intact peatlands. Synchronous fluorescence spectra also indicate the higher level of aromatic structures within fulvic acids isolated from sites with long-term agricultural use (high peat decomposition) compared with a land use history resulting in a lower peat decomposition. The different sources of fulvic acids in surface water (precipitation, runoff, interflow, groundwater) are the main reason for these effects not being detected in fulvic acids isolated from surface water. Short-term changes in land use characterized by a transition from crop farming to an unimproved grassland were found not to affect the spectroscopic properties of dissolved fulvic acids. A humification index deduced from the synchronous fluorescence spectra is proposed. We have strong evidence that dissolved humic substances indicate changes in the environmental conditions (both anthropogenic and natural) of wetlands with a high proportion of organic soils.     

Roles of Soil Organic Matter and Humic Substance Structure in Cu and Pb Adsorption in Histosols

ABSTRACT

Histosols have a high organic matter content and therefore a high variability of structures and chemical functional groups with adsorptive capacity. This study aimed to select the most appropriate models to describe the sorption phenomena of Cu and Pb in Histosols, identify the types of bonds between these metals and soil samples, and assess the influence of soil attributes and soil humic substance structures on these bonds. The Freundlich and Langmuir models were selected based on the values of the corrected Akaike information criterion and variation of Akaike information criterion as the best models for describing Cu and Pb sorption in Histosols. The values of the adsorption coefficients provided by the models indicated that Pb has higher affinity with the studied soil relative to Cu. However, Cu adsorption to soil occurs specifically and Pb is adsorbed nonspecifically. In general, the contents of N and fulvic acids were the factors that most influenced Pb sorption. Pb has a higher association with more aliphatic fulvic character structures, while Cu has a higher association with soil humic character structures. Therefore, compared to Cu, Pb in the studied Histosol has greater bioavailability potential and, consequently, greater risks of contamination and entering the food chain.     

Molecular characterization of Cladium peat from the Florida Everglades: biomarker associations with humic fractions

The accumulation and preservation of peat soils in Everglades freshwater marshes and mangrove swamps is an essential process in the ecological functioning of these ecosystems. Human intervention and climate change have modified nutrient dynamics and hydroperiod in the Everglades and peat loss due to such anthropogenic activities is evident. However, not much is known on the molecular level regarding the biogeochemical characteristics, which allow peat to be preserved in the Everglades. Lipid biomarkers trapped within or bound to humic-type structures can provide important geochemical information regarding the origin and microbial transformation of OM in peat. Four lipid fractions obtained from a Cladium peat, namely the freely extractable fraction and those associated with humin, humic acid, and fulvic acid fractions, showed clear differences in their molecular distribution suggesting different OM sources and structural and diagenetic states of the source material. Both, higher plant derived and microbial lipids were found in association with these humic-type substances. Most biomarker distributions suggest an increment in the microbial/terrestrial lipid ratio from the free to humin to humic to fulvic fractions. Microbial reworking of lipids, and the incorporation of microbial biomarkers into the humic-type fractions was evident, as well as the preservation of diagenetic byproducts. The lipid distribution associated with the fulvic acids suggests a high degree of microbial reworking for this fraction. Evidence for this 3D structure was obtained through the presence of the relatively high abundance of α,ω-dicarboxylic acids and phenolic and benzenecarboxylic compounds. The increment in structural complexity of the phenolic and benzencarboxylic compounds in combination with the reduction in the carbon chain length of the dicarboxylic acids from the free to fulvic fraction suggests the latter to be structurally the most stable, compacted and diagenetically altered substrate. This analytical approach can now be applied to peat samples from other areas within the Everglades ecosystem, affected differently by human intervention with the aim to assess changes in organic matter preservation.     

Zum Mechanismus der stoffwechselbedingten Vakuolenfluorochromierung mit Uranin

Zusammenfassung Es wird chromatographisch und spektrometrisch gezeigt, daß der Farbstoff Fluoreszein bei der Umlagerung vom Protoplasma zur Vakuole eine chemische Änderung erfährt. Diese dürfte mit großer Wahrscheinlichkeit eine Veresterung mit Essigsäure sein. Es wird vermutet, daß dieser Ester durch Reaktion von Fluoreszein mit Acetyl-Coenzym A entsteht.

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On the mechanism of the metabolically dependant uraninfluorochroming of vacuoles

Summary It is proofed by chromatographic and spectrometric observations, that the dyestuff fluorescein is chemically changed during the translocation from protoplasma to the vacuole. One may assume, that an esterification with acetic acid takes place. The fluorescein is supposed to be esterfied by the action of acetyl-coenzyme A.

     

Characterization of Nanming River (southwestern China) sewerage-impacted pollution using an excitation-emission matrix and PARAFAC

Nanming River, the largest urban river in Guizhou Province, southwestern China plateau, has been severely polluted for decades. This study characterizes the organic materials and their sources in the upstream and downstream waters by dissolved organic carbon (DOC), excitation emission matrix (EEM) spectroscopy, parallel factor (PARAFAC) analysis and photo-microbial experiments. DOC concentrations were low (47–120 μM C) upstream and relatively high (146–462 μM C) downstream. The PARAFAC studies on the sample EEM spectra demonstrated that the upstream dissolved organic matter (DOM) was mostly composed of one component that had a fulvic acid-like substance; downstream DOM was composed of two components with mixtures of tryptophan-like and fulvic acid-like substances. From the results of the sewerage drainage samples collected along the bank of the river, it is evident that both household detergent-like and protein-like or tryptophan-like substances are predominantly present, indicating that untreated sewerage effluents are the major sources of organic matter pollution in Nanming River. The degradation experiments conducted on river, sewerage drainage and commercial detergent samples demonstrated that the detergent-like and tryptophan-like substances are both photochemically and microbiologically more decomposable than fulvic acid-like materials under sunlight and dark incubations. These results suggest that the input of the untreated sewerage effluents along the streams is the major pollution source in Nanming River, and the fluorescent DOM was efficiently affected by both photochemical and microbial processes.     

De l'effet de l'Hexachlorcyclohexane sur le plankton

Summary In running water the plankton is not influenced in a nocious way by adding 3 mgr gamma isomere of hexachlorcyclohexane.In stagnant water his influence is only perceptible parting from a concentration of 30 mgr isomere gamma.

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Resumé En eau courante le plankton ne subit pas d'action nocive par l'adjonction de 3 mgr d'isomère gamma d'hexachlorcyclohexane par litre d'eau.En eau stagnante il ne faut pas moins de 30 mgr par litre d'eau pour observer une telle action.

     

Spectroscopic and elemental investigation of microbial decomposition of aquatic fulvic acid in biological process of drinking water treatment

As humic substances left in treated water tend to form trihalomethans during chlorination, their removal in water treatment processes is a significant concern for drinking water supplies. One of the removal technologies, the biofilm reactor is studied for the microbial decomposition of aquatic fulvic acid (AFA). The AFA is characterized by elemental analysis, UV-Vis, ¹³C-NMR, and IR spectroscopic methods. The spectroscopic and elemental investigation was capable of characterizing the microbial decomposition of AFA. Biologically treated fulvic acid was in a more oxidized state; its spectra displayed a higher degree of condensation of aromatic constituents than influent fulvic acid. Microbial degradation of AFA was more active in the low molecular weight fractions and intensively occurred in the aliphatic fraction.Abbreviations A the absorbance at wavelength - specific absorptivities - AFAs aquatic fulvic acids - AHS aquatic humic substances - COD chemical oxygen demand - Da dalton - DO dissolved oxygen - E₄/E₆ratio a ratio between absorbance at 465 and 665 nm - FA fulvic acid - IR infrared - NMR nuclear magnetic resonance - TOC total organic carbon - UV-Vis ultraviolet-visible     

Effect of a soil fulvic acid on stem elongation in peas

Summary Previously observed marked stimulating effects on root initiation produced by a naturally occurring fulvic acid, prompted a further study of the growth reactions of plants exposed for short durations to high concentrations of this acid. Fulvic acid concentrations up to 4000 ppm were found to inhibit stem elongation in dark grown Alaska pea stems in the presence and absence of added IAA by 46% and 33% respectively. Concentrations higher than 4000 ppm produced toxic reactions which increased sharply at pH 4.0 and lower and at pH 7.0 and higher. The fulvic acid appeared to block the uptake of GA₃ in Laxton's Progress No 9 peas when the two substances were applied simultaneously to the leaves, but when these substances were applied separately the fulvic acid had no effect on GA₃-stimulated growth. Contribution No.114 of the Food Research Institute; No.291 Soil Research Institute, Canada Department of Agriculture, Ottawa, Ontario.     

Survival and Reproduction of Some Nematodes as Affected by Muck and Organic Acids

Fulvic, humic, acetic, N-bulyric, formic, lactic, and propionic acids were inhibitory to the survival or reproduction of Aphelenchus avenae, Aphelenchoides goodeyi, Helicotylenchus pseudorobustus, Meloidogyne hapla or Xiphinema americanum. Reproduction of H. pseudorobustus and M. hapla significantly increased with increasing amounts of muck added to sand, and with the initial amount of nematode inoculum. All acids except humic and fulvic were lethal, in vitro, to all nematode species tested. When A. goodeyi was treated with fulvic acid, reproduction was reduced significantly when compared with sodium humate or water treatments. Treatment of H. pseudorobustus with fulvic acid (pH 3.5) resulted in a greater reduction in reproduction in soil than did treatment with humic acid (pH 3.5).     

Observations sur la spécificité de la coloration aux acides phosphotungstique et phosphomolybdique

Résumé Les Auteurs ont démontré que, en conditions histochimiques sur du matériel fixé au formol, les acides phosphotungstique et phosphomolybdique ont une double action: 1. une action oxydative à la charge des radicaux PAS-positifs (vic-glycols et éthyleniques) en milieu aqueux, et à la charge des radicaux aminiques en milieu anhydre; cette action entraine la transformation de ces radicaux en aldéhydes; 2. la formation d'une liaison chimique entre les aldéhydes et les molécules des acides phosphomolybdique et phosphotungstique. — La coloration du collagène, au contraire, n'est pas due ni aux radicaux aminiques ni vic-glycols et implique un mécanisme encore inconnu.

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Observations about the specificity of staining of phosphotungstic and phosphomolybdic acid

Summary The authors demonstrated that phosphotungstic and phosphomolybdic acid applied to formol-fixed tissues explete two following actions: 1. An oxidative action on the PAS-positive radicals (double bonds, vic-glycols groups) if in water solution and on aminogroups if in anhydrous solution. This oxidation results in a production of aldehydic radicals 2. The formation of chemical bonds between the aldehydic new-formed groups and the molecules of phosphotungstic or phosphomolybdicacid.— However, the above mentioned mechanism of action is not applicable to the collagen staining for which a different explanation has to be supposed.

     

Potentiometric measurement of stability constants of complexes between fulvic acid carboxylate and Fe3+

The stability constants of complexes formed between iron (III) and fulvic acid extracted from organic manures and wastes such as urban domestic sewage sludge, farmyard manure, poultry manure and sulfitation pressmud were investigated by the potentiometric titration method in an ionic medium of 0.1 M KNO₃ at 25±1 °C. A modification of the Katchalsky's model was employed for the estimation of stability constants. The displacement of the titration curves due to presence of Fe³⁺ in FA solutions formed the basis of calculations. The weak acidic property of fulvic acids due to carboxyl groups resulted in buffering over a wide range of pH; fulvic acids were completely neutralized in the pH range of 7.00–8.85. Apparent dissociation constants (pK_APP) of weakly acidic carboxyl groups were a direct function of degree of dissociation (α_L) in the mid-range of titration curves but were non-linear at high and low α_L values. The stability constants for formation of Fe–FA complexes (log β_Fe) calculated from the titration data were in the range of 5.64–7.55, depending upon α_L and electrostatic properties of fulvic acids. The relatively high stability constants of Fe–FA complexes in comparison to those with other competing cations suggest that the Fe–FA complexes are relatively stable in a soil environment. This revised version was published online in June 2006 with corrections to the Cover Date.