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1.
The change of humic acids in alkaline solution Five natural humic acids were fragmented under the conditions of the conventional method of extraction of humic substances with sodium hydroxide. Fulvic acid, hymatomelanic acid and a water soluble fraction (at pH 2) could be isolated as fragmentation products. The three fractions were formed directly after the treatment with sodium hydroxide, their quantities depend on the concentration and time of treatment with sodium hydroxide and from the function of the system. The deviating, differentiating and reproducing formation of fragments is explained by partial reversible reactions. Therefore fulvic acid and hymatomelanic acid must be regarded as artefacts. existing during the procedure of isolation of humic substances at high pH-values. Therefore the conventional isolation of humic substances from soils should always be accompanied by experiments, which inform about the arteficial production of ‘fulvic acids’ and ‘hymatomelanic acids’ during the procedure of isolation. 相似文献
2.
Three soil humic acids were degraded by a new mild chemical oxidation method using potassium persulfate at pH 2.0. The method degraded 30–40% of the starting material. The type and relative quantities of the products or fragments released as determined by GC/MS varied with the source of the polymers. Humic acid extracted from an Inceptisol yielded fatty, benzenecarboxylic and phenolic acids; humic acid from a Typic Chromoxerert produced largely dialkyl phthalates, and humic acid from an Humic Haplorthod gave only branched and straight-chain fatty acids. It is suggested that the method may be used to advantage as a first oxidant in a sequential degradation. 相似文献
3.
T. M. Hayes M. H. B. Hayes J. O. Skjemstad & R. S. Swift 《European Journal of Soil Science》2008,59(4):603-616
We present a novel study of the compositional relationships between soil organic components extractable in aqueous extractants and those in sub-soil drainage and surface runoff waters from the soil. The surface soil (0–20 cm) of a stagnogley in long-term grassland was sequentially and exhaustively extracted in aqueous media at pH values of 7, 10.6 and 12.6. Extracts from the soils and their runoff and drainage waters were processed by the procedures of the International Humic Substances Society (IHSS), and fractionated into humic, fulvic, and XAD-4 acids. Elemental, δ13 C, δ15 N, sugar, amino acids, and solid state CPMAS 13 C NMR analyses were used to identify similarities and differences between the fractions from the different extracts. There were few differences between the compositions of drainage water samples taken 1 year apart, and these had compositional features similar to those from the more highly oxidized fractions isolated from the soil at pH 7. There were significant differences between the humic components from the drainage waters and isolated from the soil at pH 7 and those of the humic fractions isolated at the higher pH values whose compositions are more clearly related to origins in plants. The compositions of the surface runoff waters indicate origins in transformed plant and animal manures on the soil surface, whereas those of the deep drainage waters originate in more extensively transformed materials, including products of microbial metabolism. The resin technique used in the fractionation allowed the isolation of novel humic acid fractions from the soil extracts, in particular at pH 7 and 12.6. These fractions clearly originated in microbial sources, were rich in saccharides and amino acids (peptides), and low in lignin-derived components. 相似文献
4.
The qualitative and quantitative distribution of N-compounds in 10 tropical soils, and in a number of humic materials extracted from representative samples thereof, was determined after 6 N HCl hydrolysis.Eighty to 98% of the total N in the soils and humic materials was hydrolysable by 6n HCl. Slightly less than one half the hydrolysable N in the soils and humic fractions consisted of amino acids. Well-drained soils and fulvic acids extracted from them contained unusually high concentrations of the acidic amino acids, aspartic and glutamic acids. Between 80 and 95% of the amino acids in the soils was accounted for in the humic materials + NaOH-insoluble organic residues. NH+4-N released by acid hydrolysis was generally higher for the soil samples than for the humic materials. Amino sugar-N constituted relatively small proportions of the total N in the soils and humic fractions.Our data suggest that large quantities of amorphous allophanic materials coupled with relatively high enzymic activity are responsible for the observed accumulation of acidic amino acids in the well-drained tropical volcanic soils. 相似文献
5.
6.
Alexander JokiĆ Radivoje Srejić Petar A. Pfendt Joanna Zakrzewska 《Water, air, and soil pollution》1995,84(1-2):159-173
Humic acids were extracted from the bottom sediment of the three lakes (Zlatari, Vasici and Vodozahvat) that together comprise Lake ?elije a regional drinking water reservoir. The humic acids were examined by high resolution 13C and 1H solution NMR and 13C CPMAS. The aromaticity expressed as the number of benzene rings per 1000 g of humic acid is 1.8 for Zlatari, 2.3 for Vasici and 1.9 for Vodozahvat. Oxygen-substituted aromatic carbon structures in humic acids from the first two lakes (Zlatari and Vasici) are similar and resemble p-coumaryl units in lignin while those in Lake Vodozahvat more closely resemble coniferyl or sinapyl units in lignin. The aromatic rings of all three humic acids are highly substituted. Humic acids from the first two lakes have very similar carbohydrate carbon contents (19.9 and 19.5% respectively) compared to 23.3% for Vodozahvat humic acid. Zlatari and Vodozahvat humic acids have a higher alkyl chain content which indicates a greater potential for forming hydrophobic cavities. The carboxyl and aromatic OH group content of each humic acid influences their capacity for forming complexes with metal ions. 相似文献
7.
Soil organic matter components of classical humic acid and humic fractions were extracted from two paleosols using 0.1 M Na4 P3 O2:0.1 M NaOH. These fractions were subjected to chemical treatment with 6 M HC1 or 70 per cent HNO, before radiocarbon assay, and their radiocarbon dates were compared with those of similar but untreated fractions, untreated buried soils, and previously published charcoal dates. Hydrolysis of humic acid and humin fractions with mineral acids, particularly 70 per cent HNO3 led to older radiocarbon dates, comparable to, though slightly older than, those of charcoal derived from the same buried layers. In contrast, the dates of soils and their humic acid and humin fractions before acid hydrolysis were younger and therefore less reliable. The application of this procedure to studies of paleosols in New Zealand is discussed. 相似文献
8.
《Communications in Soil Science and Plant Analysis》2012,43(9-10):787-796
Abstract Different molecular weight fractions obtained by ultrafiltration of a humic acid (HA) extracted from a Mollisol were analyzed by chemical, infrared, electron microscopy, and isotachophoresis methods. The results showed that the different HA fractions did not differ substantially in characteristics from each other, although each fraction was composed of subfractions exhibiting different electromobilities. It appeared that fractionation of HA would yield molecular weight fractions as imposed by any exclusion limits used in the procedure. However, the elemental composition, infrared spectra, and electron micrographs showed that the fractions, separated by molecular weight limits, contained similar compounds. These results do not support the concept of humic acids as a heterogeneous mixture of compounds, but show instead that humic acids may possess a composition more homogeneous in nature than previously postulated. 相似文献
9.
Chemical heterogeneity of humic substances: characterization of size fractions obtained by hollow-fibre ultrafiltration 总被引：7，自引：0，他引：7
I. Christl H. Knicker I. Kögel-Knabner & R. Kretzschmar 《European Journal of Soil Science》2000,51(4):617-625
To investigate the chemical heterogeneity of humic substances in relation to molecular size, fulvic and humic acids were extracted and purified from the surface horizon of a Humic Gleysol in northern Switzerland. A fractionation scheme using hollow‐fibre ultrafiltration cartridges was developed and used to obtain four size fractions of the humic acid with nominal molecular weight ranges > 300 kDa, 100–300 kDa, 30–100 kDa, and 10–30 kDa. The fulvic acid and all humic acid fractions were characterized by size exclusion chromatography, elemental analysis (C, H, N, S), as well as spectroscopic techniques including UV‐VIS, CP‐MAS 13C‐NMR, FT‐IR, and fluorescence spectroscopy. Clear chemical differences between the humic acid size fractions were observed. Smaller size fractions of the soil humic acid contained more chargeable functional groups and a larger percentage of aromatic carbon than the larger size fractions. Conversely, the percentage of aliphatic carbon increased with increasing apparent molecular weight. The chemical composition of the smallest humic acid fraction differed clearly from the fulvic acid fraction, despite similar apparent molecular size and carboxyl carbon content. Small humic acids contained much more aromatic carbon and less aliphatic carbon than the fulvic acid fraction. Apparently, humic size fractions differ in their chemical composition, which can have important implications for their environmental behaviour. 相似文献
10.
The interactions between earthworms and microorganisms can produce significant quantities of plant growth hormones and humic acids which act as plant regulators. Experiments were designed to evaluate the effects of humic acids extracted from vermicompost and compare them with the action of commercial humic acid in combination with a commercial plant growth hormone, indole acetic acid (IAA) which is a commonly found in vermicomposts. In the first experiments, humic acids were extracted from cattle, food and paper waste vermicomposts. They were applied to a plant growth medium, Metro-Mix360 (MM360), at rates of 0, 250 or 500 mg humates kg−1 dry wt. of MM360, to marigold, pepper, and strawberry plants in the greenhouse. Substitution of humates ranging from 250 to 1000 mg kg−1 MM360 increased the growth of marigold and pepper roots, and increased the growth of roots and numbers of fruits of strawberries significantly. In other experiments, humic acids extracted from food waste vermicomposts were applied at a rate of 500 mg kg−1 dry wt. of MM360, singly or in combination with IAA at a rate of 10−5 μM, to pepper seedlings. This experiment was designed to compare the differences in effects between the most effective dosage rate of humic acid from food waste, a phytohormone (IAA), and a commercial source of humic acid. The numbers of pepper flowers and fruits increased significantly in response to treatment with humic acid, IAA and a combination of humic acid and IAA. Peppers treated with humic acids extracted from food waste vermicomposts produced significantly more fruits and flowers than those treated with commercially-produced humic acids. 相似文献
11.
Methylated fulvic and humic acids were oxidized by permanganate in chloroform in the presence of a cyclic polyether, 18-crown-6. The total amount of oxidation products identified was 6.5% for fulvic acid and 6.7% for humic acid. About 46% of the oxidation products found from both fractions were dicarboxylic acids (15 compounds), the rest were benzenecarboxylic acids and their methoxyl derivatives (15 compounds). Alkanes and fatty acids were also found.Nonandioic acid and 3,4-dimethoxy-benzenecarboxylic acid are found in almost equal amounts. Each accounts for 1.3% of the starting material, and together they represent 40% of the oxidation products. 3,4-Dimethoxy-benzoic acid and 4-methoxy-benzoic acid are believed to result from the oxidation of terminal groups in the humic polymer.Proton resonance spectra show that about 25% of the aliphatic protons are part of methylene chains. The most prominent chain lengths consist of 6–8 methylene groups as shown by the dicarboxylic acids formed by oxidation. 相似文献
12.
Humic acids extracted from the Bh horizon of a kauri (Agathis australis) podzol and the A horizon of a yellow-brown earth under hard beech (Nothofagus truncata), both New Zealand soils, were fractionated by a ‘salt boundary’ technique using a dextran gel, and the fractions hydrolysed with 6 M hydrochloric acid. Lignin-derived phenolic acids were analysed by gas chromatography of the ether-soluble hydrolysis products of the humic acids. The lignin derivatives from the kauri podzol humic acid are probably modern products derived from the present-day scrub vegetation, whereas those from the yellow-brown earth humic acid are derived from the deciduous vegetation. 相似文献
13.
Abstract Charred plant fragments were isolated from 5 Ando soil samples, containing Type A humic acids, by the specific gravity (s.g.) method using a sodium polytungstate solution as heavy solution. Microscopic observation indicated that the charred plant fragments, which are black or blackish brown, were the main components in both fractions of less than s.g. 1.6 Mg m?3 that had been isolated before and after HCl-HF treatment of the soil samples. Furthermore, it was suggested that most of the fragments in the < 1.6 fractions isolated before the treatment originated from woody plants. On the other hand, the fragments in the < 1.6 fractions isolated after the treatment were mainly amorphous, although the shape of several fragments was similar to that of vascular tissues of woody and herbaceous plants. The sum of the organic-C contents of both < 1.6 fractions ranged from 4.08 to 47.8 g kg? whole soil, and 3.8–32.7% of total organic-C of the whole soil originated from these fractions. No constant relationship was observed between the organic-C contents of both fractions and the morphological characteristics of the charred plant fragments. 相似文献
14.
Two humic acids, extracted from widely different soils, have been fractionated with respect to molecular weight by means of gel chromatography. The resulting fractions were assayed for total nitrogen, amino acid nitrogen, phosphorus and sulphur. Nitrogen and phosphorus contents were greatest in the high molecular weight fractions and decreased considerably with decreasing humic acid molecular weight. The change in nitrogen content was accounted for mainly by the loss of amino acid nitrogen. By contrast, sulphur contents remained constant throughout the molecular weight range. These changes may reflect part of the process whereby nutrient elements, combined organically within humic acid, are made available for plant growth. 相似文献
15.
With the aid of in-source pyrolysis-field ionization mass spectrometry (Py-FIMS) and Curie-point pyrolysis-gas chromatography/mass spectrometry (cPy-GC/MS) in the conventional electron impact mode, characteristic signals of 23 amino acid standards were described. Thermal and mass spectrometric fragmentation pathways of these amino acids differed with each method and complemented each other. Pyrolysis products assigned by Py-FIMS extended the range of signals for N-containing compounds in humic substances and soil organic matter and gave marker signals for free amino acids and their subunits in proteinaceous materials. These characteristic signals were correlated with the amino acid content in N-rich humic fractions consisting of seven fulvic acids and eight humic acids. The selected marker signals reflected 25–84% of the variances of the molar distribution of acidic, neutral, neutral aromatic, and basic amino acids in the humic fractions. In addition, a well described agricultural soil (0.08% amino acid N) was spiked with a standard amino acid mixture (0.08 mg amino acid N 100 mg-1 dry soil) and produced enhancements of the relative abundances of the corresponding amino acid signals. Moreover, for 27 samples of whole agricultural soils of widely different origins, soil types, and vegetations, 15 selected amino acid indicators were correlated significantly with -amino N (r=0.76***) and total N (r=0.65***). 相似文献
16.
《Communications in Soil Science and Plant Analysis》2012,43(5-6):621-634
Abstract Comparisons were made between the chemical compositions of humic substances extracted from three soils covered by different vegetation and their biological activities assayed using 15‐ and 30‐day‐old seedlings of Pinus sylvestris and Picea abies. The growth, “α‐amylase and invertase activity were affected by humic fractions and by gibberellic acid (GA), indicating that humic matter had a gibberellin‐like activity. The isoenzymatic polymorphism in the electrophoretic patterns of esterase was influenced in a similar way by all humic fractions and by indoleacetic acid (IAA), which also suggested that the humic fractions exhibited an auxin‐like activity. The humic fractions extracted from the grassland, exhibiting higher amounts of phenolic and a considerable amount of carboxyl carbon, showed the best metabolic effect. The forest humic fractions, characterized by lower phenolic carbon content, appeared less effective in influencing plant metabolism, whereas the grassland‐forest humic substances proved to be even more less effective. The auxin‐ and the gibberellin‐like activities were related to a high content of phenolic and carboxylic groups. These results presented evidence that the biological activity of the humic substances was attributed to their chemical structure and to their functional groups, which could interact with hormone‐binding proteins in the membrane systems, evoking a hormone‐like response. 相似文献
17.
Humus composition of soils under forest, coffee and arable cultivation in hilly areas of south Sumatra, Indonesia 总被引：4，自引：0，他引：4
A. Watanabe Sarno J. Rumbanraja K. Tsutsuki & M. Kimura 《European Journal of Soil Science》2001,52(4):599-606
To understand the effect of land use changes on the composition of humus in tropical soils, samples from land under primary forest, secondary forest, coffee plantation, and arable crops were investigated at three sites in south Sumatra, Indonesia. Total carbon and total nitrogen contents were 1.7 to 4.3 times and 1.1 to 2.8 times greater in the topsoil under primary forest than under the other types of land use. Following change from primary forest to other uses, the proportion of humic acids in the organic matter of the topsoils decreased while that of the fulvic acid fraction increased. Within the range of land uses, differences in the yields of humic acids and fulvic acid fractions were, respectively, larger and smaller than those in total carbon content. The humic acids were classified into the low and middle classes in the degree of humification. Absorption due to the green fraction of humic acids, Pg, was detected in the UV‐visible spectra of almost all the humic acids. No relation was observed between the degree of humification of humic acids or the strength of Pg absorption in their spectra and land use change. The fulvic acid fractions were fractionated on insoluble polyvinylpyrrolidone (PVP) into the adsorbed fractions consisting of humic substances and the non‐adsorbed fractions consisting of non‐humic substances. A positive correlation between the amount of the fulvic acid fraction and the percentage of the PVP‐adsorbed fraction within it indicated that the variation in the amount of the fulvic acid fraction was attributable to acid‐soluble humic substances. The ionization difference spectra of solutions between pH 12 and pH 7 suggested that the chemical structures of the PVP‐adsorbed fulvic acids have been altered by land use change. 相似文献
18.
本文研究了采自泰安、南京、昆明3地在相近植被类型下的石灰性土壤和非石灰性土壤的腐殖质组成和胡敏酸的结构特征。结果表明,和同一地区的非石灰性土壤相比,石灰性土壤不但胡敏酸/富里酸比值恒较高,活性胡敏酸的相对含量显著较低,且其胡敏酸的芳化度和羧基含量较高,全氮及酰胺态氮的含量较低。看来,土壤呈微碱性反应不仅有利于有机物质腐解过程的进行,而且有利于游离基的形成,从而有利于酚类物质相互之间以及酚类物质与含氮化合物之间的缩聚反应和腐殖酸的脱胺作用的进行。 相似文献
19.
The acidic properties of lignins from the native vegetation of a virgin Ella loamy sand and the humic acids, the 1, 4-dioxane extractable humic fraction and residual humic acids from the virgin and cultivated soils were investigated by determining solid-state cation exchange capacities for Cu and Ca and by non-aqueous potentiometric titration, using potassium methoxide in a benzene-methanol mixture as titrant. The lignins and soil dioxane extracts were titrated in pyridine; the humic acids in dimethylformamide. Platinized Pt and CH3OH modified calomel electrodes formed the electrode combination. The CEC of the humic acids were much higher than the CEC of lignins with both cations but the Cu: Ca absorption ratios were less for humic acids than for lignins. Titration curves of lignins showed two potential breaks with total acidities of 960 to 1,190 me/100 g. Titration curves of the humic acids showed three to six potential breaks while curves of the soil dioxane extracts showed three and four. The total acidities of the two types of humic isolates were 1,100-1,200 me/100 g. The equivalent weights of most lignins and humic materials were very similar although the acid groups might be different with respect to types and acid strength. Lignins from other plant materials and humic isolates from other soils were also investigated by non-aqueous titration to determine the general applicability of the results obtained with isolates from the Ella soils. 相似文献
20.
Potential antioxidant capacity of sulfated polysaccharides from the edible marine brown seaweed Fucus vesiculosus 总被引：12，自引：0，他引：12
Fucus vesiculosus was sequentially extracted with water at 22 degrees C (fraction 1 (F1)) and 60 degrees C (F2), and with 0.1 M HCl (F3) and 2 M KOH (F4) at 37 degrees C. Soluble fractions (42.3% yield) were composed of neutral sugars (18.9-48 g/100 g), uronic acids (8.8-52.8 g/100 g), sulfate (2.4-11.5 g/100 g), small amounts of protein (< 1-6.1 g/100 g), and nondialyzable polyphenols (0.1-2.7 g/100 g). The main neutral sugars were fucose, glucose, galactose, and xylose. Infrared (IR) spectra of the fractions showed absorption bands at 820-850 and 1225-1250 cm(-1) for sulfate. F1, F2, and F4 also exhibited an absorption band at 1425 cm(-1), due to uronic acids, and their IR spectra resembled that of alginate. F3 had an IR spectrum similar to that of fucoidan with an average molecular weight of 1.6 x 10(6) Da, calculated by molecular exclusion high-performance liquid chromatography. The presence of fucose in this polysaccharide was confirmed by (1)H NMR spectroscopy. This fraction showed the highest potential to be antioxidant by the ferric reducing antioxidant power (FRAP) assay, followed by the alkali- and water-soluble fractions. Sulfated polysaccharides from edible seaweeds potentially could be used as natural antioxidants by the food industry. 相似文献