Organic matter and carbohydrate distribution in an orthic humic gleysol

Wet sieving was used to separate an Orthic Humic Gleysol into fractions of seven different particle sizes ranging from < 105 μm to 420. All fractions, including the coarse plant residue and water soluble material, were hydrolysed with H₂SO₄ and analysed for total C and neutral sugar content. Their carbohydrate composition was determined by gas-liquid chromatography of the alditol acetates. The major fraction which consisted of particles < 105 μm was enriched by 30% in both organic matter and carbohydrate content. Although the ratio of carbohydrate to organic matter in the major fraction was the same as in the original soil, it varied considerably in the other fractions. The distribution of monomers among the individual fractions varied in a regular pattern. The relative amount of monomers (hexoses, pentoses and deoxyhexoses) in the major fraction ( < 105 μm, and the water soluble material, were essentially the same as in the original soil. It is concluded that the results of this study support the view that the polysaccharides in soil are of bacterial origin.     

Electrofocusing: A new method for characterization of soil humic matter

Electrofocusing in polyacrylamide gel was carried out on humic substances extracted by 0.1 n NaOH, 0.1m Na₄P₂O₇, and by the method of Burns, El Sayed and McLaren (1972) from the upper and lower organic horizons of an alpine podsol. The electrophoretic patterns were characteristic of both humus origin and extractions procedure. The best resolution of the isoelectric bands for the humus were obtained by the Burns-McLaren procedure. The ionic component does not have much influence on the distribution of humus constituents within the electrophoretic pattern, but the presence of phosphate appears to be essential to obtain good separations.     

Effects of land-use and management practices on soil ergosterol content in andosols

Ergosterol is a fungus-specific chemical component which has been extensively used to assess the fungal biomass and activity in soils. In the present study, we investigated the soil ergosterol content in a group of Japanese soils differing in management. In addition, the relationships among the soil ergosterol content (SEC), microbial biomass C (MBC), and microbial biomass N (MBN) were also tested in different seasons. Our results showed that the SEC was lower in intensively cropped soils than in pasture and forest soils. In general, no consistent trend was observed for SEC of pasture soils within the same sampling period. However, SEC tended to decrease in most of the soils in autumn, which may be ascribed to the effect of seasonal changes on fungal biomass. No strong evidence could be obtained for the effect of different fertilizers on SEC, which can be due to different management variables and interspecific variations between fungal communities at different soil sites. Our results did not suggest the presence of a noticeable correlation between SEC and MBC or MBN. The ratio of SEC in total biomass C was lower (0.20 and 0.11% in spring and autumn, respectively) compared with the values reported.     

Interpretation of humic acid coagulation and soluble soil organic matter using a calculated electrostatic potential

The coagulation of humic substances and its role in controlling the solubility of organic matter in soils are not well understood. We therefore studied the physico‐chemical behaviour of purified humic acid from forest soil coagulated with Na, Ca, Cu, Al at pH 4 and 6, and then modelled the behaviour with the Non‐Ideal Consistent Competitive Adsorption Donnan (NICA‐Donnan) model. We found that the coagulation of humic acid occurs when the Donnan potential is less negative than ?0.08 V. Based on this result, an empirical relation between the Donnan potential of humic acid and its concentration in solution was derived. In addition, the Donnan potential of the dissolved organic matter in the soil solution of six soil profiles from forests was calculated using the NICA‐Donnan model under the assumption that all the dissolved organic matter behaves as humic acid. The measured concentration of dissolved organic matter also decreases in a soil profile, as the calculated potential becomes less negative. The results are in many cases in semi‐quantitative agreement with the predicted concentration based on the humic acid coagulation experiment. Acid soils contain more dissolved organic matter, which may result from the presence of a fairly large fraction of more soluble organic molecules, such as fulvic acid.     

Studies on the properties of organic matter in buried humic horizon derived from volcanic ash

Abstract

Humic acids were extracted from the surface horizon Yu 1 and buried humic horizons (Yu 2, 800-864 AD; Yu 4, ca. 4,000 years B.P.; Yu 6, 7,000 years B.P.; Yu 7, ca. 10,000 years B.P.). The humic acids were filtered with ultramembranes with 20, 10, 5, 1 or 0.1 × 10' M.W. in this order and separated into five fractions; (>20), (20-10), (10-5), (5-1) and (1-0.1) × 10⁴ M.W. fractions. The elementary composition, functional groups, optical properties, and hydrolyzable total- and sugar-carbon contents of each humic acid fraction were determined, and the changes in properties of the humic acid with age after burial were discussed.

In horizons Yu 1 to Yu 6, the patterns of M.W. distribution of the >20 × 10⁴ to (1- 0.1) × 10⁴ fractions were rather similar. In contrast, Yu 7 was characterized by the predominance of (1-0.1) x 10' M.W. fraction and the presence of a small amount of <0.1 × 10⁴ M.W. fraction.

The chemical properties of humic acid (HA) fractions of each humic horizon and their changes with age after burial were as folIows:

1) Elementary composition of HA fractions of each humic horizon was rather similar to each other. The C% and C/N ratio increased, and the H%, N% and H/C ratio decreased in all HA fractions with age.

2) Total acidity and carboxyl contents of HA fractions of Yu 1 were higher in the lower M.W. fractions. These values increased with age up to Yu 4 or Yu 6 horizons, then decreased in the Yu 6 or Yu 7 horizon. The contents of carbonyl groups in all the HA fractions which were very low in Yu 1, showed a wide range of variations in Yu 2, intermediate values from Yu 4 to Yu 6 horizons then decreased in the HA fractions of Yu 7, except for the (>20) fraction.

3) The degree of humification of the HA fractions of Yu 1 judging from the RF and \sDlogK values, tended to be higher in higher M.W. fractions, and increased in all the HA fractions with age after burial.

4) Hydrolyzable total- and sugar-carbon contents were high in the HA fractions of Yu 1 and decreased with age.

5) Changes of elementary composition, degree of humification and hydrolyzable total- and sugar-carbon contents were conspicuous from the Yu 1 to Yu 2 horizons, and less significant afterwards.

6) The 0%, C/O ratio and phenolic OH content did not show any consistent change with age after burial.     

Contribution of denitrification and autotrophic and heterotrophic nitrification to nitrous oxide production in andosols

To quantify the contribution of denitrification and autotrophic and heterotrophic nitrification to N₂O production in Andosols with a relatively high organic matter content, we first examined the effect of C₂H₂ concentrations on N₂O production and on changes in mineral N contents. The optimum C₂H₂ concentration for inhibiting autotrophic nitrification was 10 Pa. Secondly, and Andosol taken from an arable field was incubated for 32 days at 30°C at 60, 80, and 100% water-holding capacity with or without the addition of NH ₄ ⁺ or NO _inf3 ^sup- (200 mg N kg^-1), and subsamples collected every 4–8 days were further incubated for 24 h with or without C₂H₂ (10 Pa). At 60 and 80% water-holding capacity with NH ₄ ⁺ added, 87–92% of N₂O produced (200–250 g N₂O–N kg^-1) was derived from autotrophic nitrification. In contrast, at 100% water-holding capacity with or without added NO _inf3 ^sup- , enormous amounts of N₂O (29–90 mg N₂O–N kg^-1) were produced rapidly, mostly by denitrification (96–98% of total production). Thirdly, to examine N₂O production by heterotrophic nitrification, the Andosol was amended with peptone or NH ₄ ⁺ (both 1000 mg N kg^-1)+citric acid (20 g C kg^-1) and with or without dicyandiamide (200 mg N kg^-1). Treatment with citric acid alone or with citric acid+dicyandiamide suppressed N₂O production. In contrast, peptone increased N₂O production (5.66 mg N₂O–N kg^-1) mainly by denitrification (80% of total production). However, dicyandiamide reduced N₂O production to 1.1 mg N₂O–N kg^-1. These results indicate that autotrophic nitrification was the main process for N₂O production except at 100% water-holding capacity where denitrification became dominant and that heterotrophic nitrification had a lesser importance in the soils examine.Dedicated to Professor J. C. G. Ottow on the occasion of his 60th birthday     

Relationships between the primary mineral and the clay mineral compositions of some recent andosols

Relationships between the clay mineralogy and the primary mineral association were studied on seventeen Andosol samples (<3,000 years old) collected from Aomori, Hokkaido, and Iwate. Opaline silica, allophane, and imogolite were predominant in the soils derived from volcanic ashes which contained practically no quartz, while opaline silica, crystalline layer silicates, alumina-rich gel-like materials, and allophanelike constituents were abundant in the soils which contained abundant quartz. There was no positive indication of the presence of allophane in any quartz andesitic Andosols. High contents of finely comminuted amphibole and mica in the quartz andesitic volcanic ashes suggested that the crystalline layer silicates are inherited and are not formed pedochemically from amorphous materials.     

Mechanism of reduction of exchangeable aluminum by gypsum application in acid andosols

Mechanism of reduction of exchangeable aluminum in acid Andosols treated with gypsum was studied by using cation exchange resin methods to determine the amount of polymerized aluminum. Two types of acid Andosols were used as test soils: Kitakami light colored Andosol (fine, mixed, mesic, Andic Dystrochrept) and Kawatabi thick high humic Andosol (medial, mesic mixed Alic Pachic Melanudand). Polymerization of aluminum in the soil solution of both Kitakami and Kawatabi Andosols treated with gypsum was suggested based on an analysis using cation exchange resin methods, whereas that in monomer aluminum solution was not detected. Accumulation of polymerized aluminum in both Kitakami and Kawatabi Andosols was determined by using cation exchange resin, and the amounts of polymer aluminum trapped by the resin and the ratio of polymer aluminum to monomer aluminum were increased with the incubation time. The values of CEC which decreased in the Kitakami Andosol after gypsum treatment were almost equivalent to the amounts of cation exchange sites occupied by polymer aluminum ions which were calculated based on the decrease of the values of Y _l. We conclude that the mechanism of reduction of exchangeable aluminum in strongly acid Andosols treated with gypsum is as follows: firstly, exchangeable aluminum adsorbed on the cation exchange sites of soils may be released into the soil solution due to the increase in the ion strength caused by gypsum application, and then monomer aluminum in soil solution may be polymerized in the presence of soil colloidal materials. Consequently, the polymer aluminum formed in the soil solution may be selectively and irreversibly fixed on the cation exchange sites of 2 : 1 clay minerals.     

Combined effects of technical grade fenitrothion, humic acids and particulate matter on cholinesterase activity in freshwater invertebrates

Purpose

The relative sensitivity of two freshwater invertebrate organisms to the organophosphorus insecticide fenitrothion was assessed by measuring cholinesterase (ChE) activity, a well-known biomarker of both exposure and effect to organophosphorus pesticides. The influence of different concentrations of humic acids (HAs) and particulate matter on fenitrothion bioavailability was assessed in the more sensitive species.

Materials and methods

The selected invertebrates were the dwelling feeding oligochaete Lumbriculus variegatus and the pulmonate gastropod Biomphalaria glabrata. Acute 48-h bioassays were performed exposing organisms to different fenitrothion concentrations. The concentrations that induced 50 % inhibition of enzyme activity (EC₅₀) were calculated. Fenitrothion bioavailability was investigated using different concentrations of commercial HA or particulate matter. Sand and a diverse selection of chromatographic resins that have been proposed as analogues of natural sediments were selected. For these experiments, animals were exposed to a fenitrothion value similar to the EC₅₀.

Results and discussion

The 48-h EC₅₀ values were 12?±?2 and 23?±?3 μg?l^?1 for L. variegatus and B. glabrata, respectively. Depending on HA concentration and the characteristics of particles, ChE activity was similar or higher than the value recorded for animals exposed only to the pesticide in aqueous solution.

Conclusion

The results indicated that L. variegatus was the more sensitive species of the two. In this species, fenitrothion bioavailability did not increase due to the presence of either different HA concentrations or particulate matter. The experimental approach may constitute a useful tool to predict the influence of dissolved organic matter and sediment particles on fenitrothion bioavailability and toxicity to non-target aquatic invertebrates.     

Effects of pH, ionic strength, and solutes on DNA adsorption by andosols

The adsorption of DNA by two andosols was investigated as function of solution pH, ionic strength in solution and some solutes, so as to understand the behavior of extracellular DNA molecules in two andosols. DNA adsorptions greatly decreased by increasing pH of suspensions in a pH range of 3.0–9.0. The adsorption of DNA molecules by both andosols was not affected by ionic strength from 0.1 to 0.5 mol L⁻¹ NaCl. However, the DNA adsorption increased proportionally by increasing Mg²⁺ concentration in the suspension. Addition of phosphate decreased DNA adsorption, indicating competition between DNA molecules and phosphate ion in the adsorption by andosols. These results suggest that there are several DNA adsorption mechanisms in soil.     

Effects of liming on organic matter decomposition and phosphorus extractability in an acid humic Ranker soil from northwest Spain

Summary A laboratory incubation experiment was carried out over 17 weeks to determine the effect of liming on soil organic matter. The amount of lime as calcium hydroxide [Ca(OH)₂] required to completely neutralise exchangeable Al was found to be five times the standard lime requirement. This large amount of lime had a limited overall effect on the short-term stability of soil organic matter, causing the release of 1300 g g^-1 of C (1.7% total soil C) above the control during the incubation. Liming may have altered the potential availability of soil organic matter and organic P, as shown by a marked reduction in the extractability of soil organic P with sodium bicarbonate and sodium hydroxide. The latter was unlikely to be due to the formation of calclium-P artefacts, and may be attributed to the combined chemical effects of added calcium hydroxide and precipitation of exchangeable Al on the nature and solubility of soil organic constituents and organomineral complexes. The addition of lime increased the degradation of added oak leaf litter by 50%, from 3.2 to 4.7 mg g^-1, as determined by CO₂ evolution. The enhanced litter degradation indicated increased microbial activity in limed soil, but this improvement had only minor effects on the stability of native organic matter. This study highlights the need for further research into the relationships between the chemical nature of organic P in soil and the physical, chemical, temporal, and agronomic factors that control its turnover and availability.     

An appreciation of the contribution of Frank Stevenson to the advancement of studies of soil organic matter and humic substances

Purpose

The aims of this paper are to outline the state of knowledge with regard to the chemistry of soil organic matter (SOM) prior to 1950; then, to review and evaluate the contributions made by Frank Stevenson during Stevenson’s research period (1950–1994); and subsequently to outline advances that are being made in the modern era.

Progress in the Stevenson period

Frank Stevenson’s research career began in the middle of the twentieth century when a number of techniques of colloid chemistry were available to him, but relatively few of the recently developed instrumental techniques and other procedures of analytical organic chemistry that have enabled significant advances to be made in the chemistry and properties of SOM components.The contributions that Frank Stevenson has made to the chemistry of SOM and of humic substances (HSs) are an integral part of his book (first and second editions) Humus Chemistry: Genesis, Composition, Reactions. The validity of the terms humus and HSs are being questioned as legitimate terms that describe definable components, and SOM is being viewed as a ‘continuum of progressively decomposing organic compounds’. The legitimacy of isolating the organic matter components from their native soil environment is questioned. Those who pose such questions would do well to consider how progress could have been made in the vital life sciences areas of, for example, proteomics and genomics, without the isolation of the relevant cellular components. We recognise the importance of clear and rigorous definitions of HS components and stress the need to isolate these components from the SOM matrix as a prerequisite to the study of the composition, structure and reactivity of these components. We disagree with proposals or suggestions that do not recognise HSs as a scientific entity, and we feel sure that Frank Stevenson would have supported this stance. Various studies of SOM and of HSs have taken place over the centuries, but progress was slow because the tools required to study such complex systems were not available. Frank Stevenson’s research involved many areas of humic chemistry, and his major advances were in aspects of functionality and in the interactions of humic functional groups with metals and to a lesser extent with anthropogenic organic chemicals. His studies of nitrogen and of ammonia in relation to organic matter also had a very great impact.

Progress in the modern era

Frank Stevenson can be said to have provided the stimulation that enabled beginners and established scientists to obtain a good grasp of the fundamentals of SOM and the humic sciences. His scientific contributions have catalysed many of the significant advances that have been made in the field since he retired. In the final section, some of the advances that have been made using modern analytical techniques are addressed and some of the controversial topics that have recently arisen are discussed.

     

Nitrogen fertilization increases rhizodeposit incorporation into microbial biomass and reduces soil organic matter losses

Agricultural soils receive large amounts of anthropogenic nitrogen (N), which directly and indirectly affect soil organic matter (SOM) stocks and CO₂ fluxes. However, our current understanding of mechanisms on how N fertilization affects SOM pools of various ages and turnover remains poor. The δ¹³C values of SOM after wheat (C₃)-maize (C₄) vegetation change were used to calculate the contribution of C₄-derived rhizodeposited C (rhizo-C) and C₃-derived SOM pools, i.e., rhizo-C and SOM. Soil (Ap from Haplic Luvisol) sampled from maize rhizosphere was incubated over 56 days with increasing N fertilization (four levels up to 300 kg N ha^?1), and CO₂ efflux and its δ¹³C were measured. Nitrogen fertilization decreased CO₂ efflux by 27–42% as compared to unfertilized soil. This CO₂ decrease was mainly caused by the retardation of SOM (C₃) mineralization. Microbial availability of rhizo-C (released by maize roots within 4 weeks) was about 10 times higher than that of SOM (older than 4 weeks). Microbial biomass and dissolved organic C remained at the same level with increasing N. However, N fertilization increased the relative contribution of rhizo-C to microbial biomass by two to five times and to CO₂ for about two times. This increased contribution of rhizo-C reflects strongly accelerated microbial biomass turnover by N addition. The decomposition rate of rhizo-C was 3.7 times faster than that of SOM, and it increased additionally by 6.5 times under 300 kg N ha^?1 N fertilization. This is the first report estimating the turnover and incorporation of very recent rhizo-C (4 weeks old) into soil C pools and shows that the turnover of rhizo-C was much faster than that of SOM. We conclude that the contribution of rhizo-C to CO₂ and to microbial biomass is highly dependent on N fertilization. Despite acceleration of rhizo-C turnover, the increased N fertilization facilitates C sequestration by decreasing SOM decomposition.     

Dry matter and primary nutrient accumulation in soybeans as affected by combined Nitrogen levels

Nodulating and non‐nodulating soybeans were grown on a Alfic Udipsamment and a Typic Hapludoll amended with 10 or 100 kg N/ha. Tissue and grain samples were analyzed to determine N₂‐fixation, dry matter, and N, P, and K accumulation. Highest grain yields were associated with the highest levels of N₂‐fixation and N and K accumulation in grain. The largest dry matter production was by nodulating plants grown on a high soil N regime. Nodulating plants accumulated more grain and tissue N, P, and K than non‐nodulating plants. Nitrogen stress increased P concentrations in both grain and tissue and decreased harvest indices.     

The chemical composition of soil organic matter in classical humic compound fractions and in bulk samples — a review

In the present paper new findings in soil organic matter (SOM) research were reviewed with regard to non-aromatic species in order to make evident the recent conception about the chemical nature of humic matter structure. The main purpose of this paper was to unravel the manifold information of SOM investigations in order to characterize the classical humic matter fractions (fulvic acids, humic acids, humins) and bulk soil samples. Such common state-of-the-art information is missing in current SOM literature. In addition we focus on improvements in SOM research due to the application of the new instrumental methods such as NMR and pyrolysis-MS and its problems of analysis.     

Nitrogen mineralization in marsh meadows in relation to soil organic matter content and watertable level

The objective of the present study was to asses the effect of watertable level on N mineralization in a Histosol and a Humic Gleysol profile under natural meadows in Ljubljana marsh, Slovenia. The two soils differ significantly in organic matter content (27—40 % in Histosol and 14—20 % in Humic Gleysol) but not in C : N ratio (13—20) and pH (6.5—7.0). For each soil, the watertable was maintained at two levels (above or below 50 cm from the soil surface) for approximately one year. The four main plots, according to soil carbon content and watertable level were divided into 4 subplots, according to 4 fertilization treatments (unfertilized control, PK, PK + 50 kg N ha^—1, PK + 3 × 50 kg N ha^—1). Net N mineralization in unfertilized subplots was estimated from indices of N mineralization obtained by incubation of soil samples in the laboratory and by seasonal dynamics of mineral N content in the field. Annual uptake of N in herbage under the 4 fertilization treatments was also measured. Total mineral N content in topsoil was 20—80 % higher in Histosol than in Humic Gleysol. Similarly, aerobic N mineralization potentials along the entire soil profile (0—90 cm) were 20—130 % higher in Histosol than in Humic Gleysol. By contrast, anaerobic N mineralization potentials in subsoil were 10—60 % lower in Histosol than in Humic Gleysol. Both, aerobic and anaerobic N mineralization potentials strongly depended on watertable levels at sampling time. Seasonal dynamics of soil mineral N content as well as N mineralization potentials indicated that the N mineralization in the Histosol could be 10—40 % higher at low than at high watertable level. In the Humic Gleysol the N mineralization could be 10—100 % higher at high watertable level. Higher N availability in Histosol at low watertable and in Humic Gleysol at high watertable was also reflected in higher N uptake in herbage. These results indicate that N mineralization in Histosol and Humic Gleysol, was proportional to soil organic matter content, whereas in both soils, higher N mineralization rates can be expected at watertable levels between 40 and 60 cm below the soil surface, than at higher/lower watertable levels.     

Properties and composition of soil organic matter in forest and arable soils of schleswig-holstein. 2. litter and humic compounds in mineral horizons

Organic matter composition is an important soil constituent with regard to function in soil ecosystems. In the recent paper litter and humic compound contents from about 100 mineral soil investigations are presented. The soil horizons are divided into four groups (Ah, Ap, M. Bh) in order to compare the SOM quality. Ap and Ah horizons showed a similar litter and humic compound distribution. Structural differences in the humic compound fractions were only visible with CPMAS ¹³C-NMR. SOM-containing non-spodic subsoil horizons had a similar SOM quality as the A horizons. In the Bh horizons the humic compounds dominated with about 75% in the SOM. Alkylic and O-alkylic carbon units are the main fractions. The combination of the solid-state ¹³C-NMR spectroscopy of whole soil samples and the wet chemical analysis of litter compounds allowed the estimation of the liner and chemically defined humic compound distribution in soil samples.     

Nitrogen fertilization of strawberries: Nmin,leaf dry matter,and leaf sap analyses as control methods

In a three‐year survey several control methods of nitrogen (N) supply in strawberry were investigated. It was found that N_min analysis could be used as a measurement of control from the beginning of the season, indicating the need of additional N supply. Leaf dry matter analysis, taken during flowering, could be used as an indicator thus making it possible to make corrections within the season, if needed. When leaf dry matter analysis was compared to leaf sap analysis, correlations were evident for the majority of nutrients, N being an important exception. It was concluded that the use of N_min‐ and leaf dry matter analyses combined might make corrections in N fertilization within the same year possible.     

Nitrogen and cation mobilization by soil fauna feeding on leaf litter and soil organic matter from deciduous woodlands

Decomposing oak litter was incubated in laboratory microcosms and the effects of adding a variety of soil animals upon nitrogen and cation release were monitored. Various groups of macrofauna caused a marked increase in ammonium release with smaller increases in calcium, potassium and sodium leaching. Microfauna also had significant but much less marked effects upon nitrogen and cation release.The effects of different grazing intensities of the millipede Glomeris marginata on a variety of forest organic substrates show that the animals amplified existing patterns of nutrient release.