Evaluation of the stabilization level of pig organic waste: Influence of humic‐like compounds

Abstract

The evolution of the organic matter during the maturation of solid samples of pig sludges and pig manure composted with straw was followed. A sample of pig sludge about 15 years old also was characterized for comparison. The organic matter of the composts and sludges was extracted and the humic (HA) and fulvic acids (FA) were separated. The organic carbon in the total extract (TEC) in the fulvic fraction and in the humic fraction was determined in order to evaluate the stabilization level of the organic matter using some humification parameters. The nature of the organic extract also was evaluated by characterization with analytical isoelectric focusing (IEF). The results confirm that the degree of humification (DH) decreases during the first period of maturation of the organic matter, because of the degradation of humic and fulvic‐like compounds contained into the raw organic materials, while then it increases progressively for all the maturation period. The data collected in this study confirm that the FA fraction could be the main cause of the lack of regularity in the trend of increasing DH as maturation progresses. The FA/TEC ratio infact decreases progressively for all the maturation period, while the HA/TEC ratio increases. The results obtained in the IEF characterization confirm the validity of this analytical technique. Moreover, the results do not appear to be affected by the presence of the humic‐like compounds. The presence of the bands focused at the higher pH values appear to be directly related to the stabilization of the organic material.     

Carbon and nitrogen transformation during composting of sweet sorghum bagasse

Two types of compost, consisting of sweet sorghum bagasse with either sewage sludge or a mixture of pig slurry and poultry manure, were studied in a pilot plant using the Rutgers system. The total degradation of the piles as determined by the weight loss of organic matter during the bio-oxidative and maturation phases accounted for 64% of the organic matter applied and followed a first-order kinetic function. Concentrations of total and organic N increased during the composting process as the degradation of organic C compounds reduced the compost weight. Losses of N through NH₃ volatilization were low, particularly in the compost with sewage sludge due to pH values of <7.0 and the low temperatures reached in the compost during the first 2 weeks. The C:N ratio in the two composts decreased from 24.0 and 15.4 to values between 12 and 10. Increases in cation exchange capacity and in fulvic and humic acid-like C revealed that the organic matter had been humified during composting. The humification index, the C:N ratio, fulvic:humic acid-like C, and cation exchange capacity proved to be the most suitable parameters for assessing the maturity of these composts.     

Dynamics of Organic C Mineralization and the Mobile Fraction of Heavy Metals in a Calcareous Soil Incubated with Organic Wastes

Organic wastes such as sewage sludge and compost increase the input of carbon and nutrients to the soil. However, sewage sludge-applied heavy metals, and organic pollutants adversely affect soil biochemical properties. Therefore, an incubation experiment lasting 90 days was carried out to evaluate the effect of the addition of two sources of organic C: sewage sludge or composted turf and plant residues to a calcareous soil at three rates (15, 45, and 90 t of dry matter ha^–1) on pH, EC, dissolved organic C, humic substances C, organic matter mineralization, microbial biomass C, and metabolic quotient. The mobile fraction of heavy metals (Zn, Cd, Cu, Ni, and Pb) extracted by NH₄NO₃ was also investigated.The addition of sewage sludge decreased soil pH and increased soil salinity to a greater extent than the addition of compost. Both sewage sludge and compost increased significantly the values of the cumulative C mineralized, dissolved organic C, humic and fulvic acid C, microbial biomass C, and metabolic quotient (qCO₂), especially with increasing application rate. Compared to compost, the addition of sewage sludge caused higher increases in the values of these parameters. The values of dissolved organic C, fulvic acid C, microbial biomass C, metabolic quotient, and C/N ratio tended to decrease with time. The soil treated with sewage sludge showed a significant increase in the mobile fractions of Zn, Cd, Cu, and Ni and a significant decrease in the mobile fraction of Pb compared to control. The high application rate of compost resulted in the lowest mobility of Cu, Ni, and Pb. The results suggest that biochemical properties of calcareous soil can be enhanced by both organic wastes. But, the high salinity and extractability of heavy metals, due to the addition of sewage sludge, may limit the application of sewage sludge.     

Study of Organic Matter Evolution in Citrus Compost by Isoelectrofocusing Technique

Three composts from citrus-processing industry wastes, sampled at prefixed times during the composting process, were studied with the aim to follow the organic matter evolution by using the isoelectrofocusing (IEF) technique. Results indicated that IEF qualitative analyses allowed evaluation of the organic matter transformation during composting process, showing a decrease of IEF peaks focused at lower values of pH (less stabilized organic matter) and a corresponding increase of peaks focused at higher value of pH (more humified material). The parameter A %, defined as the areas sum of IEF peaks focused at pH>4.7, could be considered particularly effective as a “threshold value” to evaluate the level of organic matter evolution for the considered composts.     

Differences in the chemical composition of dissolved organic matter from waste material of different sources

The chemical composition of waste-material-derived dissolved organic matter (DOM) was characterized by chemolytic analyses and ¹H, ¹³C and ³¹P nuclear magnetic resonance (NMR) spectroscopy. Dissolved organic matter was extracted by water from an aerobic fermented urban waste compost, a sewage sludge and a pig slurry and then fractionated using the XAD-8 method. The amount of water-extractable dissolved organic carbon (DOC) ranged from 3% in the sewage sludge to 22% in the pig slurry. Dissolved organic matter isolated from pig slurry was equally distributed between hydrophilic and hydrophobic DOC, whereas in the sewage-sludge-derived material the hydrophobic fraction was predominant. Dissolved organic C from the urban waste compost was mainly within the hydrophilic fraction. Wet-chemical analysis and ¹H- and ¹³C-NMR spectra showed that both DOM fractions from the urban waste compost were low in neutral, acidic and amino sugars as well as in lignin-derived compounds. In turn, the materials were rich in low-molecular-weight aliphatic compounds. The chemical structure of both fractions is probably the result of the intensive transformation of urban waste compost during its fermentation. The hydrophilic fractions of DOM from sewage sludge and pig slurry contained considerable amounts of carbohydrates but were also rich in low-molecular-weight aliphatics. The respective hydrophobic fractions had the largest contents of CuO-extractable phenols which may in part derive from sources other than lignin. By contrast with the other materials, the hydrophobic fraction from the pig slurry seemed to contain polymeric rather than low-molecular-weight material. The ³¹P-NMR spectrum of the hydrophilic DOM fraction from urban waste compost did not show signals of inorganic or organic P compounds while the spectrum of the hydrophobic fraction revealed traces of monoester P, diester P, and orthophosphate. ³¹P-NMR spectroscopy suggested that both the hydrophobic and hydrophilic fractions from pig slurry did not contain organic P. The hydrophilic DOM fraction from sewage sludge contained orthophosphate, organic monoester P and a little pyrophosphate. The hydrophobic fraction contained mainly organic diester P and smaller amounts of teichoic acids and organic monoester P. Considering that water-soluble fractions of urban waste compost contained no easily plant-available P and a low content of labile organics, we conclude that this material contains less labile nutrients and is more refractory than the soluble constituents of pig slurry and sewage sludge.     

Long-term effects of metal-containing farmyard manure and sewage sludge on soil organic matter in a fluvisol

Our aim was to establish the long-term effects of repeated applications after 20 y of organic amendments (farmyard manure at 10 t ha⁻¹ y⁻¹, and urban sewage sludge at two different rates, 10 t ha⁻¹ y⁻¹ and 100 t ha⁻¹ every 2 y) on the quality of a sandy and poorly buffered soil (Fluvisol, pH 6). Chemical characteristics and biodegradability of the labile organic matter, which is mainly derived from microbial biomass and biodegradation products of organic residues, were chosen as indicators for soil quality. The organic C content had reached a maximal value (30.6 g C kg⁻¹ in the 100 t sludge-treated soil), i.e. about 2.5 times that in the control. Six years after the last application, the organic C content and the microbial biomass content remained higher in sludge-treated soils than in the control. In contrast, the proportion of labile organic matter was significantly lower in sludge-treated soils than in manure-treated and control soils. The labile organic matter of sludge extracts appeared less humified than that of manure-treated and control soils.     

剩余污泥厌氧消化过程重金属形态转化及生物有效性分析

为研究污泥厌氧消化过程中物理化学性质的变化对典型重金属形态转化的影响,对其农用的可行性及生物有效性进行评估,对取自某城市污水处理厂的剩余污泥进行了序批式厌氧消化实验,在试验过程中测定了污泥理化学性质,采用Tessier分步提取法提取了污泥样品中的典型重金属,并采用电感耦合等离子发射光谱仪（ICP-OES）测定各形态重金属含量及总量。结果表明,厌氧消化过程中重金属的形态发生了显著变化,由不稳定态向比较稳定的残渣态和有机结合态转变,某些重金属形态与污泥理化性质如pH、碱度、VS/TS及氨氮显著相关。厌氧消化可以有效地降低污泥中重金属的潜在迁移能力和生物有效性,经厌氧消化后污泥可以更好地进行土地利用。     

Determining competitive nitrate and chloride adsorption in an andisol by the unsaturated transient flow method

Abstract

Activated sludge from a sewage disposal plant was labeled with ¹⁵N in the laboratory. The labeled sludge (dewatered cake) was then incubated under aerobic conditions for 30 days with four kinds of cultivated soils: volcanic ash soil, red-yellow soil, paddy soil, and sandy dune soil. The nitrogen mineralization of the soil organic matter was remarkable only in the case of the paddy soil. In this soil, a priming effect caused by the addition of the sludge was observed. After 30 days of incubation, the ¹⁵N organic fractions remaining in the red-yellow soil were determined. It was found that the amino acid and the unidentified fractions in the hydrolyzable nitrogen forms of the sludge contributed mainly to the amount of nitrogen mineralized. Finally, using sludges which originated from the same organic matter source, the lnftuence of a generally-used inorganic coagulator Oime and ferric chloride) of sludge on the nitrogen cycle was clarified. This coagulator caused a reduction in the amount of inorpnic nitrogen mineralized in the soil and also accelerated the nitrification process.     

Chemical fractions of copper and zinc in organic‐rich particles from aqueous extracts of a metal‐contaminated granite soil

Abstract

Chemical fractions of copper (Cu) and zinc (Zn) in the organic‐rich particles collected from filtered aqueous extracts (<20 μm) of an acid soil were determined. A sequential extraction procedure was used to partition the particulate Cu and Zn into four operationally defined chemical fractions: adsorbed (ADS), iron (Fe) and manganese (Mn) oxides bound (FeMnOX), organic matter bound (OM) and residual (RESD). Total extractable concentrations of Cu and Zn in the fine particles were higher than their total concentrations in the original bulk soil. The concentration of particulate Cu was usually much higher than that of particulate Zn. Addition of lime stabilized sewage sludge cake and/or inorganic metal salts markedly increased the concentrations of particulate Cu and Zn in aqueous extracts, especially from limed soil. The proportional distributions of particulate Cu and Zn were quite similar. The two particulate metals were present predominantly in the ADS and FeMnOX fractions, with less (about 20%) in the OM and RESD fractions. Some of the ADS metal fraction was associated with dissolved organic substances. The concentrations of particulate Cu and Zn in the various extractable fractions were significantly affected by the application of lime, lime stabilized sewage sludge cake, or inorganic metal salts.     

Characterization of Organic Matter in Compost Produced with Municipal Solid Wastes: An Italian Approach

Stabilization of the organic matter of a static pile of compost from municipal solid wastes (MSW) under a forced-pressure ventilation composting system was followed for 55 days during winter season. The materials were analyzed according to the official methodologies required by Italian regulations regarding the quality of composts from MSW. The stabilization process of the organic matter was monitored using both the degree of humification (DH), i.e. the ratio between the humified fractions (HA + FA) and the total extractable carbon (TEC), and the electrofocusing technique (EF). The DH increased steadily in compost during stabilization process and converged asymptotically at the end of the period of composting. The EF analyses of the organic extracts of compost from MSW showed a definite trend in the humification process and confirmed the actual evolution of the organic matter composted.     

Characterization of the organic fraction of an uncomposted and composted sewage sludge by isoelectric focusing and gel filtration

Summary Isoelectric focusing was used to characterize the organic matter of composted and uncomposted sewage sludge. The technique was applied to organic matter extracts and to three fractions, obtained by ultrafiltration, with different molecular weights (<10³, 10³–10⁴, >10⁴). The elution curves of the extracts through Sephadex G-50 revealed a loss in the proportion of organic matter of low molecular weight as composting progressed, together with an enrichment of the high-molecular-weight proportion. Separation into fractions by controlled ultrafiltration proved to be valid, as deduced from the chromatograms obtained by Sephadex G-50 filtration. The extracts of uncomposted sludge showed a greater number of bands with a low isoelectric point than the composted extract, because there were more acidic molecules in the samples that had not undergone humification. The spectrum corresponding to the extract of the 210-day compost showed greater homogeneity with a lower number of bands. A great part of the organic matter extracted with 0.1 M Na₄P₂O₇ at pH 7.1 corresponded to an intermediate molecular weight. The ampholytes at pH 4–6 gave better resolution than those at pH 3.5–10, in the focusing of fractions with the lowest and the greatest molecular weight. A more homogeneous spectrum was observed for the high-molecular-weight fractions from extracts of the 210-day composted sample; in addition, the bands were displaced towards higher isoelectric points, which indicated that the molecules were more condensed, with a minor content of negatively charged groups and a spectrum similar to that of relative fractions of true humic acids.     

Characterization by isoelectric focusing of the organic matter of a regenerated soil

Abstract

Regeneration of a soil with a high degree of desertification was conducted by the addition of different doses of municipal solid waste organic matter (MSW). Five years after this treatment, humic substances were extracted from these soils and characterized by spectroscopy and isoelectric focusing. No significant differences between E4/E6 ratio and ?log K (Log A400 nm‐log A600 nm) were observed for humic substances extracted from treated and untreated soils. However, the isoelectric focusing (IEF) technique established differences between the humic substances from control and treated soils. The focusing pattern of the former showed a well defined band at pH 9.1 which nearly disappeared in the soils with high doses of MSW (1–2 %). However the organic matter which focused at pH 5.8 was present in all soils.     

Effects of sewage sludge stabilization on organic‐N mineralization in two soils

Sewage sludge is a valuable source of organic matter, N, P and certain micronutrients that have beneficial effects on plant growth and biomass production. However, sanitary regulations often require the stabilization of sewage materials prior to applying them to soils as biosolids. Environmental regulations also demand appropriate management of biosolid‐N to avoid groundwater contamination. Because stabilization processes usually make sewage sludge less putrescible, we hypothesized that the mineralization rates of organic‐N from stabilized biosolids would be affected. Therefore, this study aimed to evaluate the mineralization of five biosolids in two soils – a sandy Spodosol and a clayey Oxisol. Digested sludge, composted sludge, limed sludge, heat‐dried sludge and solar‐irradiated sludge were mixed with soil samples at a concentration of 32.6 mg N/kg soil (1.0 dry t/ha of digested sludge) and incubated at 25 °C in a humidity chamber for 23 weeks. Results showed that the stabilization processes generally slowed the release of mineral‐N in soils relative to the digested sludge from which the biosolids originated. However, increments in the levels of mineral‐N were more influenced by soil type than by the type of stabilization process applied to the sewage sludge. Mineralization rates were up to 5‐fold higher in the Oxisol than in the Spodosol soil, and as a result, organic‐N in biosolids mineralized 10–24% in Spodosol and 23–52% in Oxisol. Any appropriate plan for the management of biosolid‐N for plant use should consider the interaction between soil type and biosolid type.     

Organic matter in volcanic soils in Chile: Chemical and biochemical characterization

Abstract

Determinations were made of total soil organic matter (SOM), stable and labile organic fractions, biomass carbon (C), and chemical composition of several humus‐soil‐fractions in Chilean volcanic soils, Andosols and Ultisols. Their physico‐chemical properties and humification degree at different stages in edaphic evolution were also assessed. In addition, organic matter models were obtained by chemical and biological syntheses and the structures and properties of natural and synthetic humic materials were compared with SOM. Results indicate that Andosols have higher SOM levels than Ultisols, but the fraction distribution in the latter suggests a shift of the more stable fractions to the more labile ones. Moreover, contents of humines, and humic and fulvic acids suggest that Chilean volcanic soil SOM is highly humified. On the other hand, among the SOM labile fractions, carbohydrate and biomass are about 15% of the SOM which are one of the most important fractions in soil fertility.     

Effects of thermally dried and composted sewage sludges on the fertility of residual soils from limestone quarries

Limestone quarrying reduces the land's capacity to support a complete functional ecosystem. Adding sewage sludge to mining residues facilitates the establishment of a vegetation cover and can stimulate C and N cycling.We aimed to evaluate the effects of three composted and three thermally dried sewage sludges, on some biological properties of two types of debris (extraction soil and trituration soil) from a limestone quarry. Lysimeters filled with debris-sludge mixtures and control soils were sampled immediately after preparation and after being left in the open for 13 months. Total carbohydrates (TCH), 0.5 M K₂SO₄ extractable (ECH) carbohydrates, 0.5 M K₂SO₄ extractable organic C (EOC), microbial biomass carbon (MBC), microbial respiration (MR), β-glucosidase activity and β-galactosidase activity were determined immediately after sampling. The treated soils were also analyzed for their more general physicochemical characteristics. Adding sewage sludge clearly improved the physicochemical and biological properties of the residual soil and the effect of the type of sludge was greater than that of the type of soil. The sludge effect was generally more durable over the trituration soil. The sludge effect decreased the most in MR and EOC followed by MBC and ECH. Total carbohydrates showed the least enhancement but the sludge effect on this endpoint had the smaller decrease with time. Root exudates and plant debris contributed to β-glucosidase and β-galactosidase activities in the treated soils. Activities present in mixtures partly corresponded to enzymes free in the soil aqueous face. β-Glucosidase was also partly associated with humified organic matter. Thirteen months after sludge addition a fraction of the organic matter present in soils was still moderately labile. Results observed in BMC and MR suggests the sludge did not cause major toxic effects on residual soils. The sludge effect differed with the pre and post treatments of the sludges; thermal drying made the sludge organic matter more easily decomposable.     

Sludge-derived organic carbon in an agricultural soil estimated by 13C abundance measurements

The objective of this study is to develop a method to follow the dynamics of sludge‐derived organic carbon, which will allow us to understand the behaviour of trace metals in the sludge‐treated soils. We studied, in a sandy agricultural soil of southwest France, cultivated with maize and amended with sewage‐sludge over 20 years, the dynamics of different sources of organic matter and compared this with a control, which had never received any treatment. For the first time, a method is proposed that will distinguish and quantify sludge‐derived organic carbon, maize‐derived organic carbon, and native organic carbon. This method is based on the mean differences in δ¹³C abundances between native (−26.5‰), maize (−12.5‰) and sludge (−25.4‰) organic carbon. Three hypotheses on the dynamics of soil organic matter sources are proposed: (i) isotopic differences observed between control and sludge‐treated soils are due only to the incorporation of sludge C, whereas in the others, the control was used to model the incorporation of (ii) maize C or (iii) native C in the sludge‐treated soils. The comparison of the stocks of each source (native C, maize C and sludge C) found in the bulk soil with the sum of corresponding stocks found in particle‐size fractions allowed us to reject the two first hypotheses and to validate the last one. Repeated applications of sewage‐sludge induced accumulation of sludge‐derived organic carbon in the topsoil, and simultaneously contributed to the preservation of maize‐derived organic carbon. When sludge applications ceased, the rapid decrease in soil organic matter stocks was mostly caused by the degradation of the sludge‐derived organic carbon sources. At the same time, the maize‐derived organic carbon shifted from the coarsest fraction (200–2000 μm) to the finest fraction (0–50 μm). Therefore, this study has shown that repeated applications of sewage‐sludge induced changes in soil organic matter dynamics over time.     

Microdetermination of protease activity in humic bands of different sizes after analytical isoelectric focusing

Summary Extracellular benzoyl-l,-argininamide (BAA)-hydrolysing protease was extracted with neutral pyrophosphate from an arable soil and fractionated by membrane ultrafiltration. There were three fractions: A₁ (molecular weight > 10⁵), A_II (molecular weight 10⁴–10⁵), and R (molecular weight < 10⁴). Analytical isoelectric focusing (IEF) of the fractions was carried out on polyacrylamide gels with a restricted pH gradient of 4.0 to 5.0. Two extracellular proteases characterized soil extract E, with one peak (Ip 4.44) bound to a large amount of humic matter and the other (Ip 4.06) bound to a small amount of humus. Following ultrafiltration, the humus-enzyme complex of extract E (Ip 4.44) split into the fractions A_I, A_II, and R, and was displaced at Ip values that depended on the electrophysical properties of bound organic matter, whereas that at Ip 4.06 was completely removed from the extract E and accumulated only into the low-molecular-weight fraction R. High recoveries of absolute activity were obtained after IEF of the whole extract E, and fractions A_II and R, but only about 50% was recovered from fraction A_I.It appears that humic substances have reversible inhibitory effects on extracellular proteases, since the maximum recoveries of activity were obtained from fractions where high amounts of protease non-active organic matter had been removed by IER IEF was able to fractionate humic molecules and purify humic-protease complexes on the basis of smaller differences in Ip, and even smaller differences of 0.05 pH units. The present results show that BAA hydrolysing proteases were preferentially linked with a specific class of humic molecules with an Ip of close to 4.44.Joint program CNR (Italy) — C.S.I.C. (Spain), no. 7, 1985–1986. This paper is part of the doctoral thesis of Prof. M. Bonmati     

Rhizosphere effects on Cu availability and fractionation in sewage sludge‐amended calcareous soils

Rhizosphere processes have a major impact on copper (Cu) availability and its fractions in soils. A greenhouse experiment with wheat was performed to investigate availability (using seven chemical procedures) and fractionation of Cu in the rhizosphere of ten agricultural soils (Typic Calcixerepts) amended with sewage sludge (1% w/w) using rhizoboxes. The results show that available Cu concentrations in rhizosphere soils were significantly (P < 1%) lower than in bulk soils. In comparison with the bulk soils, in the rhizosphere soils the concentration of Cu associated with organic matter and residual Cu increased by 24 and 4%, respectively, whereas exchangeable Cu, Cu associated with iron‐manganese oxides, and Cu associated with carbonate decreased by 20, 14, and 12%, respectively. Dissolved organic carbon (DOC) and Cu associated with iron‐manganese oxides and Cu associated with organic matter in the rhizosphere and bulk soils were significantly correlated (P < 5%). The results show that the differences between rhizosphere and bulk soils in chemical conditions such as DOC concentrations can change the proportion of soil Cu fractions and, therefore, Cu availability for wheat in calcareous soils amended with sewage sludge. The results show that the wheat root‐induced modifications of chemical and biological soil conditions do not only lead to Cu depletion in mobile soil Cu fractions, but also to modification in soil Cu fractions which are commonly considered as more stable.     

Changes of metal forms by organic amendments to Hawaii soils

Abstract

Forms of metals in soils control their availability to plants and animals and affect the environment differently. To evaluate shifts of metal forms as affected by organic amendments, a sequential extraction procedure was used to fractionate calcium (Ca), iron (Fe), magnesium (Mg), manganese (Mn), and zinc (Zn) in two Hawaii soils amended with three organic wastes. The designated forms are water‐soluble, exchangeable, sorbed, organically bound, carbonate, and residual fractions. The soils, a Mollisol (Waimanalo series) and an Ultisol (Paaloa series), were incubated at 25°C±2°C at field capacity with either chicken manure, sewage sludge, or green manure (cowpea leaves) at 0, 5, and 20 Mg#lbha^‐1 for one or five months. Organically bound metals decreased with time because of organic matter decomposition. Iron was mostly residual, but water‐soluble Fe also increased in the acid Paaloa soil. Unlike Fe, most forms of Ca and Mg were transformed to the exchangeable form in 5 months. There was no significant change of Mn forms during the 5‐month incubation. Virtually all organically bound Zn shifted to carbonate and residual forms in the neutral Mollisol (pH 6.2), but shifted to carbonate and exchangeable forms in the acid Ultisol (pH 4.5). The solubilities and exchangeabilities of the five metals in the two soils treated with sewage sludge were not significantly different from those treated with cowpea green manure or chicken manure during the 5‐month incubation. The results suggest that the additions of sewage sludge, chicken manure, or cowpea green manure to Hawaii soils at 20 Mg#lbha^‐1 do not have environmentally significant impacts in terms of Ca, Mg, Fe, Mn, and Zn. On the other hand, the amendments may decrease Ca and Mg deficiencies in highly weathered, nutrient‐poor soils such as Ultisols and Oxisols of the tropics.