Changes in physical and chemical properties of pretreated wheat straw during hydrolysis with cellulase

Summary After 5 days of enzymatic hydrolysis, the average wheat straw particle size has decreased by 62% and there is a dramatic shift to particle sizes less than 25 microns in size. Before hydrolysis, all particle size fractions have the same composition. After hydrolysis, the cellulose fraction is reduced in all particles and the decrease is greater for smaller particles.     

Aspects of the chemical structure of soil organic materials as revealed by solid-state13C NMR spectroscopy

Solid-state cross-polarisation/magic-angle-spinning³C nuclear magnetic resonance (CP/MAS¹³C NMR) spectroscopy was used to characterise semi-quantitatively the organic materials contained in particle size and density fractions isolated from five different mineral soils: two Mollisols, two Oxisols and an Andosol. The acquired spectra were analysed to determine the relative proportion of carboxyl, aromatic, O-alkyl and alkyl carbon contained in each fraction. Although similar types of carbon were present in all of the fractions analysed, an influence of both soil type and particle size was evident.The chemical structure of the organic materials contained in the particle size fractions isolated from the Andosol was similar; however, for the Mollisols and Oxisols, the content of O-alkyl, aromatic and alkyl carbon was greatest in the coarse, intermediate and fine fractions, respectively. The compositional differences noted in progressing from the coarser to finer particle size fractions in the Mollisols and Oxisols were consistent with the changes noted in other studies where CP/MAS¹³C NMR was used to monitor the decomposition of natural organic materials. Changes in the C:N ratio of the particle size fractions supported the proposal that the extent of decomposition of the organic materials contained in the fine fractions was greater than that contained in the coarse fractions. The increased content of aromatic and alkyl carbon in the intermediate size fractions could be explained completely by a selective preservation mechanism; however, the further accumulation of alkyl carbon in the clay fractions appeared to result from both a selective preservation and anin situ synthesis.The largest compositional differences noted for the entire organic fraction of the five soils were observed between soil orders. The differences within orders were smaller. The Mollisols and the Andosol were both dominated by O-alkyl carbon but the Andosol had a lower alkyl carbon content. The Oxisols were dominated by both O-alkyl and alkyl carbon.A model describing the oxidative decomposition of plant materials in mineral soils is proposed and used to explain the influence of soil order and particle size on the chemical composition of soil organic matter in terms of its extent of decomposition and bioavailability.     

The cellulase system of the anaerobic rumen fungus Neocallimastix frontalis: studies on the properties of fractions rich in endo-(1→4)-β-D-glucanase activity

Seven fractions rich in endoglucanase activity were separated from the extracellular cellulase system of the anaerobic rumen fungus Neocallimastix frontalis. The fractions (ES1, ES3, ES2U1, ES2U2, ES2U4, ES2U3C1 and ES2U3C2) were separated from each other and from a fraction that could solubilize crystalline cellulose (the so-called crystalline-cellulose-solubilizing component, CCSC) by the sequential use of differential adsorption on the microcrystalline cellulose Avicel, gel filtration and affinity chromatography on concanavalin-A—Sepharose. The molecular masses of the endoglucanase fractions, when determined by gel filtration, were 64, 30, 61, 113, 17, 38 and 93 kDa respectively. Each enzyme degraded carboxymethylcellulose and was rich in activity to cellulose swollen in phosphoric acid to break the hydrogen bonding: cellobiose, cellotriose and cellotetraose were released in differing proportions. Each fraction showed a characteristic gradient when the capacity of each enzyme to increase the fluidity of a solution of carboxymethylcellulose was plotted against the increase in reducing power of the solution. Although neither endoglucanase fraction, acting in isolation, could degrade crystalline cellulose, three of the fractions (ES1, ES3 and ES2U1) could act synergistically with the CCSC fraction in this regard. Remarkably, the same three fractions also acted in synergism with the cellobiohydrolase (CBH I and CBH II) of the aerobic fungus Penicillium pinophilum in degrading crystalline cellulose, but only when both cellobiohydrolase enzymes were present in the solution along with any one of the three endoglucanases. These observations support the conclusion that the mechanism of action of the cellulase system of N. frontalis in degrading crystalline cellulose may be similar to that operating in the aerobic fungi.     

Microbial population structures in soil particle size fractions of a long-term fertilizer field experiment

Soil structure depends on the association between mineral soil particles (sand, silt, and clay) and organic matter, in which aggregates of different size and stability are formed. Although the chemistry of organic materials, total microbial biomass, and different enzyme activities in different soil particle size fractions have been well studied, little information is available on the structure of microbial populations in microhabitats. In this study, topsoil samples of different fertilizer treatments of a long-term field experiment were analyzed. Size fractions of 200 to 63 microm (fine sand fraction), 63 to 2 microm (silt fraction), and 2 to 0.1 microm (clay fraction) were obtained by a combination of low-energy sonication, wet sieving, and repeated centrifugation. Terminal restriction fragment length polymorphism analysis and cloning and sequencing of 16S rRNA genes were used to compare bacterial community structures in different particle size fractions. The microbial community structure was significantly affected by particle size, yielding higher diversity of microbes in small size fractions than in coarse size fractions. The higher biomass previously found in silt and clay fractions could be attributed to higher diversity rather than to better colonization of particular species. Low nutrient availability, protozoan grazing, and competition with fungal organisms may have been responsible for reduced diversities in larger size fractions. Furthermore, larger particle sizes were dominated by alpha-Proteobacteria, whereas high abundance and diversity of bacteria belonging to the Holophaga/Acidobacterium division were found in smaller size fractions. Although very contrasting organic amendments (green manure, animal manure, sewage sludge, and peat) were examined, our results demonstrated that the bacterial community structure was affected to a greater extent by the particle size fraction than by the kind of fertilizer applied. Therefore, our results demonstrate specific microbe-particle associations that are affected to only a small extent by external factors.     

Utilization of by-products from the tequila industry. Part 2: Potential value of Agave tequilana Weber azul leaves

The leaves of the agave plant are left in the field after harvesting the heads for tequila production. Different types of agave leaves were isolated, classified, and their content in the total plant determined. The usable fractions were collected and their properties determined. Of the total wet weight of the agave plant, 54% corresponds to the agave head, 32% corresponds to materials which could be usable for sugar and fiber production which leaves 14% of the wet plant without apparent utility. The fractions with higher total reducing sugars (TRS) content were the fresh fraction of partially dry leaves stuck to the head and the leaf bases with a TRS content of 16.1% and 13.1%, respectively. The highest TRS concentration (16-28%) is in the agave head which is used for tequila production. The leaves are 90-120 cm long and 8-12 cm wide and contain fiber bundles that are 23-52 cm long and 0.6-13 mm wide. The ultimate fiber length is approximately 1.6 mm with an average width of 25 microns. There are several types of leaf fibers that can be utilized depending on what part of the plant they come from and what product is desired. Agave leaf fibers were pulped using a soda pulping process and the pulp was hand formed into test sheets. Test sheets made from pulped agave leaf fibers had a breaking length comparable to paper made from both pine and eucalyptus fibers, but the tear index and burst index were lower than the other two papers.     

中性糖在土壤中的来源与分布特征

糖类(即碳水化合物)是土壤有机质的重要组成部分, 经生物化学降解形成不同结构的单糖。土壤中的中性单糖也叫中性糖, 主要包括木糖、核糖、阿拉伯糖、葡萄糖、半乳糖、甘露糖、岩藻糖和鼠李糖。其中, 植物来源的糖主要为五碳糖, 如木糖和阿拉伯糖; 微生物来源的糖主要包括半乳糖、甘露糖、岩藻糖、鼠李糖等六碳糖。研究中常利用六碳糖和五碳糖的比例指示微生物和植物对土壤有机碳的相对贡献。中性糖是微生物重要的碳源和能量来源, 在团聚体的形成过程中扮演着重要角色。该文整合了近30年土壤中性糖的研究进展, 对比了提取中性糖的常用方法, 分析了不同土地利用类型和不同土壤组分中中性糖的含量、来源和周转特征, 综述了影响中性糖含量和分布的主要环境因素。结果表明, 中性糖在耕地土壤中的绝对含量和相对含量均显著低于针叶林、阔叶林、草地和灌丛4种土地利用类型。(半乳糖+甘露糖)/(阿拉伯糖+木糖)(GM/AX)在不同土地利用间差异不显著, 而(鼠李糖+岩藻糖)/(阿拉伯糖+木糖)(RF/AX)则表明草地土壤中的微生物来源的中性糖含量高于针叶林和耕地。不同密度的土壤组分中, 轻质组分中中性糖的含量比重质组分高, 重质组分中微生物来源的中性糖较多; 就不同粒径(或团聚体)而言, 黏粒(或微团聚体)中微生物来源的中性糖含量更丰富。有关影响土壤中性糖含量和分布的因素的研究, 目前主要集中在人为活动(如耕种和放牧等), 而有关温度、降水等自然环境因素影响的研究较少。     

Grazing and the distribution of sediment particle sizes in artificial stream systems

Recent research has shown that grazing by the algivorous minnows of the genus Campostoma can have a significant effect on both structural and functional parameters in stream ecosystems, influencing algal height and type, primary productivity, carbon dynamics, bacterial biomass and the size fractionation of benthic organic matter. This study was undertaken to evaluate the effect of minnow grazing on benthic particulate organic matter (BPOM) under the controlled conditions available in experimental streams. For this study, four grazed and four ungrazed artificial streams were sampled for BPOM on two dates. The samples were partitioned into large, medium, fine and ultrafine fractions via wet filtration. Fish grazed systems had significantly larger percentages of the fine fraction and significantly smaller percentages of the ultrafine fraction. The ability of grazers to alter particle size distribution is important to overall stream organic matter dynamics because recent studies have shown the importance of particle size in determining bacterial numbers and activity, which in turn influence fundamental stream process like respiration and organic carbon dynamics.     

Chemical Speciation of Lead and Cadmium in Different Size Fractions of Dust Samples from Two Busy Roads in Irbid City,Jordan

Concentrations of Pb and Cd in different size fractions in road dust samples taken from areas of high traffic flows in two streets in Irbid City, Jordan, have been measured using graphite furnace atomic absorption spectrometry (GFAAS). A series of road dust particles in the following size ranges, < 90, 90–106, 106–125, 125–250, 250–1000 and 1000-2000 μ m, were investigated to evaluate the ratio between metal content in each fraction of particle size and total metal content. Results show most of the highest levels were found in the small particle sizes. Sequential extraction procedure was used for chemical speciation in road dust samples of < 90 μ m. Two standard reference materials, CRM142R and SRM 2709, were analyzed to assess the accuracy and the reliability of the proposed method, and the precision of the results was expressed by relative standard deviation (rsd < 6%).     

Sequestration and turnover of plant- and microbially derived sugars in a temperate grassland soil during 7 years exposed to elevated atmospheric pCO2

Temperate grasslands contribute about 20% to the global terrestrial carbon (C) budget with sugars contributing 10–50% to this soil C pool. Whether the observed increase of the atmospheric CO₂ concentration (pCO₂) leads to additional C sequestration into these ecosystems or enhanced mineralization of soil organic matter (SOM) is still unclear. Therefore, the aim of the presented study was to investigate the impact of elevated atmospheric pCO₂ on C sequestration and turnover of plant‐ (arabinose and xylose) and microbially derived (fucose, rhamnose, galactose, mannose) sugars in soil, representing a labile SOM pool. The study was carried out at the Swiss Free Air Carbon Dioxide Enrichment (FACE) experiment near Zurich. For 7 years, Lolium perenne swards were exposed to ambient and elevated pCO₂ (36 and 60 Pa, respectively). The additional CO₂ in the FACE plots was depleted in ¹³C compared with ambient plots, so that ‘new’ (<7 years) C inputs could be determined by means of compound‐specific stable isotope analysis (¹³C : ¹²C). Samples were fractionated into clay, silt, fine sand and coarse sand, which yielded relatively stable and labile SOM pools with different turnover rates. Total sugar sequestration into bulk soil after 7 years of exposure to elevated pCO₂ was about 28% compared with the control plots. In both ambient and elevated plots, total sugar concentrations in particle size fractions increased in the order sand2 for coarse sand, fine sand and silt (about 274%, 17% and 96%, respectively) but about 14% lower for clay compared with the control plots, corroborating that sugars belong to the labile SOM pool. The fraction of newly produced sugars gradually increased by up to 50% in bulk soil samples after 7 years under elevated pCO₂. In the ambient plots, sugars were enriched in ¹³C by up to 10‰ when compared with bulk soil samples from the same plots. The enrichment of ¹³C in plant‐derived sugars was up to 13.4‰ when compared with parent plant material. After 7 years, the δ¹³C values of individual sugars decreased under elevated (¹³C‐depleted) CO₂ in bulk soil and particle size fractions, varying between −13.7‰ and −37.8‰ under elevated pCO₂. In coarse and fine sand, silt and clay fractions newly produced sugars made up 106%, 63%, 60% and 45%, respectively, of the total sugars present after 7 years. Mean residence time (MRT) of the sugars were calculated according to two models revealing a few decades, mean values increasing in the order coarse sand2 led to a net sequestration of about 30% of labile SOM (sugars) while no increase of total organic C was observed at the same plots. The additional labile SOM is gradually incorporated into more stable SOM pools such as silt and clay fractions in the medium term (<7 years). MRT of labile (sugar) SOM under elevated pCO₂ is in the same order of magnitude when compared with studies under ambient pCO₂ though no direct comparison of elevated and ambient plots was possible.     

Microbial Population Structures in Soil Particle Size Fractions of a Long-Term Fertilizer Field Experiment

Soil structure depends on the association between mineral soil particles (sand, silt, and clay) and organic matter, in which aggregates of different size and stability are formed. Although the chemistry of organic materials, total microbial biomass, and different enzyme activities in different soil particle size fractions have been well studied, little information is available on the structure of microbial populations in microhabitats. In this study, topsoil samples of different fertilizer treatments of a long-term field experiment were analyzed. Size fractions of 200 to 63 μm (fine sand fraction), 63 to 2 μm (silt fraction), and 2 to 0.1 μm (clay fraction) were obtained by a combination of low-energy sonication, wet sieving, and repeated centrifugation. Terminal restriction fragment length polymorphism analysis and cloning and sequencing of 16S rRNA genes were used to compare bacterial community structures in different particle size fractions. The microbial community structure was significantly affected by particle size, yielding higher diversity of microbes in small size fractions than in coarse size fractions. The higher biomass previously found in silt and clay fractions could be attributed to higher diversity rather than to better colonization of particular species. Low nutrient availability, protozoan grazing, and competition with fungal organisms may have been responsible for reduced diversities in larger size fractions. Furthermore, larger particle sizes were dominated by α-Proteobacteria, whereas high abundance and diversity of bacteria belonging to the Holophaga/Acidobacterium division were found in smaller size fractions. Although very contrasting organic amendments (green manure, animal manure, sewage sludge, and peat) were examined, our results demonstrated that the bacterial community structure was affected to a greater extent by the particle size fraction than by the kind of fertilizer applied. Therefore, our results demonstrate specific microbe-particle associations that are affected to only a small extent by external factors.     

Different forms of nitrogen in particle size fractions separated from two soils

Summary The possible use of particle size separation of soils in water was tested for preparing fractions rich in ‘unknown’-N, which constitutes between 41 and 46% of the total N. Ten particle size fractions ranging from <0.2 to>1,000.0 μm were separated from the A horizon of the Bainsville soil, an Orthic Humic Gleysol, and from the Bh horizon of the Armadale soil, a poorly drained Podzol. The distribution of N (hydrolyzable-, amino acid-, protein-, amino sugar-, ammonia-, ‘unknown’-and unidentified-N) in the initial soils and in each size fraction was determined. While particle size separation did not yield fractions which contained essentially only ‘unknown’-N and few known N-components, it was possible to isolate fractions which were either rich in amino acid-or protein-N or in NH₃-N. In general, the finer size fractions tended to be enriched in amino acid-N while NH₃-N was more prominent in the coarser fractions. The amino sugar-N content of all size fractions was low.     

Bacterial biomass on fine detritus particles in a woodland stream of Hokkaido,Japan

Bacterial biomass on four different size fractions of benthic fine particulate organic matter (FPOM) was measured throughout a year in a woodland stream in Hokkaido, Japan. Bacterial biomass per ash free dry mass (AFDM) of the FPOM was significantly different among the four size fractions, while the biomass per unit surface area of FPOM was not. Annual mean of bacterial biomass per particle mass positively correlated to the surface area per mass in the four size fractions. In addition, negative correlation was found between the C:N ratio and bacterial biomass per AFDM in FPOM when all fractions were pooled. There was also negative correlation between C:N ratio and the surface area per particle mass in the four size fractions. The difference of bacterial biomass on FPOM among the size fractions could be ascribed to surface area and/or C:N ratio of FPOM, although these effects were not separately evaluated in the present study.     

Distribution of soil organic matter between fractions and aggregate size classes in grazed semiarid steppe soil profiles

Grazed steppe ecosystems are discussed as one of the big global carbon sinks that may have the potential to sequester large amounts of atmospheric CO₂ and mitigate the effects of global change if grazing is abandoned or management improved. But until today, little is known about sequestration potentials and stabilisation mechanisms in complete soil profiles of semiarid grasslands and how these systems react to grazing cessation. We applied a combined aggregate size, density and particle size fractionation procedure to sandy steppe soils under different grazing intensities (continuously grazed = Cg, winter grazing = Wg, ungrazed since 1999 = Ug99, ungrazed since 1979 = Ug79). Higher inputs of organic matter in ungrazed treatments led to higher amounts of OC in coarse aggregate size classes (ASC) and especially in particulate organic matter (POM) fractions across all depth. These processes started in the topsoil and took more than 5 years to reach deeper soil horizons (>10 cm). After 25 years of grazing cessation, subsoils showed clearly higher POM amounts. We found no grazing-induced changes of soil organic matter (SOM) quantity in fine ASC and particle size fractions. Current C-loading of fine particle size fractions was similar between differently grazed plots and decreased with depth, pointing towards free sequestration capacities in deeper horizons. Despite these free capacities, we found no increase in current C-loading on fine mineral soil fractions after 25 years of grazing exclusion. Silt and clay fractions appeared to be saturated. We suppose empirical estimations to overestimate sequestration potentials of particle size fractions or climatic conditions to delay the decomposition and incorporation of OM into these particle size fractions. POM quality was analysed using solid-state ¹³C NMR spectroscopy to clarify if grazing cessation changed chemical composition of POM in different ASC and soil depths via changing litter quality or changing decomposition dynamics. We found comparable POM compositions between different grazing intensities. POM is decomposed hierarchically from coarse to fine particles in all soil depths and grazing cessation has not affected the OM decomposition processes. The surplus of OM due to grazing cessation was predominately sequestered in readily decomposable POM fractions across all affected horizons. We question the long-term stabilisation of OM in these steppe soils during the first 25 years after grazing cessation and request more studies in the field of long-term OM stabilisation processes and assessment of carbon sequestration capacities to consider deeper soil horizons.     

Distribution and location of polycyclic aromatic hydrocarbons (PAHs) and PAH-degrading bacteria within polluted soil aggregates

A study was conducted to determine the location and distribution of PAH and PAH-degrading bacteria in different aggregate size fractions of an industrially polluted soil. The estimation of PAH-degrading bacteria using an MPN microplate technique indicated that these bacteria are most numerous in the aggregate size fractions corresponding to fine silt (2–20m) and clay(<2m) compared to larger fractions or unfractionated soil.PAH concentrations were also highest in the aggregate size fraction corresponding to fine silt. Similar results were found in a spiked soil (incubated for 6 months) with similar carbonated minerals. Transmission electron microscopy observations showed that the autochtonous PAH-degrading bacteria were embedded in the aggregates where PAHs were abundant. In spite of this extensive co-localisation PAH degradation was limited during 6 months incubation. This indicates that factors other than spatial distribution and PAH degrading ability control degradation rates. The fine silt fraction of the industrial soil had an elevated C/N ratio (35) compared to the clay fraction (C/N: 16). Thus the fraction which assumably had the highest specific surface area contained less PAH but similar numbers of PAH-degraders. N thus seem to play an important role in the long term, but as PAH degradation was low in fine size fractions, other sources/factors were probably limiting (easily degradable C, P org, O₂ etc.). Based on these findings, soil particle organization and structure of soil aggregates appear to be important for the characterization of a polluted soil (localization and sequestration). Manipulations that modify aggregation in polluted soils could thus potentially influence the accessibility and biodegradability of PAHs.     

Selective ingestion of detritus by a north temperate omnivorous fish, the juvenile white sucker, Catostomus commersoni

Synopsis The capacity of the juvenile white sucker, Catostomus commersoni, to feed selectively on detritus was examined by analyzing gut contents of fish feeding in a northern Michigan pond and in laboratory aquaria. Suckers selected fine particle detritus. The median length of detritus particles consumed by pond suckers ranged from 26–38 m for all seasons sampled. Although suckers in the pond ingested invertebrates > 215 m they never ingested detritus particles > 215 m. Suckers fed pond detritus in laboratory aquaria selectively ingested the fine particle fraction (Kolmogorov-Smirnov test, p < 0.0001). Suckers excluded particles > 220 m and ingested a median particle size of 54 m. Amorphous detritus particles comprised 100% of the detritus particles in 93% of the foreguts analyzed. Suckers fed fine particle (< 45 ) pond detritus in laboratory aquaria rejected the inorganic fraction and selectively ingested organicmaterial with the highest protein and energy content. Ash free dry mass (AFDM) as a percent of dry-mass was 2.6 times greater in the foregut contents than in the detritus (p < 0.001). The amino acid concentration and energy density of the ingested organic matter were 1.9 times higher (p < 0.044) and 1.3 times higher (p < 0.025) than the respective amino acid and energy content of the organic fraction of the detritus. These results indicate that suckers have the capacity to consume selectively fine particle detritus with the highest nutritional value.     

Physical properties and compact analysis of commonly used direct compression binders

This study investigated the basic physico-chemical property and binding functionality of commonly used commercial direct compression binders/fillers. The compressibility of these materials was also analyzed using compression parameters derived from the Heckel, Kawakita, and Cooper-Eaton equations. Five classes of excipients were evaluated, including microcrystalline cellulose (MCC), starch, lactose, dicalcium phosphate (DCP), and sugar. In general, the starch category exhibited the highest moisture content followed by MCC, DCP, lactose, and finally sugars; DCP displayed the highest density, followed by sugar, lactose, starch, and MCC; the material particle size is highly processing dependent. The data also demonstrated that MCC had moderate flowability, excellent compressibility, and extremely good compact hardness; with some exceptions, starch, lactose, and sugar generally exhibited moderate flowability, compressibility, and hardness; DCP had excellent flowability, but poor compressibility and hardness. This research additionally confirmed the binding mechanism that had been well documented: MCC performs as binder because of its plastic deformation under pressure; fragmentation is the predominant mechanism in the case of lactose and DCP; starch and sugar perform by both mechanism.     

Changes in the origin and quality of soil organic matter after pasture introduction in Rondônia (Brazil)

We examined the effects of the conversion of tropical forest to pasture on soil organic matter (SOM) origin and quality along a chronosequence of sites, including a primary forest and six pastures. Bulk soil samples received a physical size-fractionation treatment to assess the contribution of each compartment to total SOM pool. Besides a general increase in total C and N stocks along the chronosequence, we observed a reduction of the relative contribution of the coarser fractions to total soil C content, and an increased concentration in the finer fractions. The origin of the C in each size fraction was established from measurements of¹³C abundance. After 80 years about 93% of the C in the least humified fraction of the top 10 cm of soil was of pasture origin, while in the most humified it was 82%. Chemical analyses indicated that the fine silt and coarse clay fractions contained the most refractory carbon.     

Determination of birch pollen allergens in different aerosol sizes

Allergens in fine particles may cause symptoms inallergic asthmatics. In order to assess the exposureof susceptible persons, a method to measure theallergen load in fine and coarse particles wasdeveloped.Aerosols are collected with a high-volume air samplerby multistage impaction. They are separated into fivesize classes, ranging from >10 m to <1 mand sampled on glass fibre filters. After sampling,filters are crushed into a fine powder using ahydraulic press. Allergens are then eluted on a shakerinto Tween-20-containing phosphate buffered saline.After microfiltration, the eluate is ready foranalysis with ELISA-techniques (Enzyme Linked ImmunoSorbens Assay).Two different methods are used for the analysis ofallergens: One is a sandwich-ELISA using monoclonalIgG-antibodies, the other is a competitive ELISA basedon polyclonal IgE-antibodies obtained from patientsallergic to birch pollen. Using the monoclonalantibodies information on the amount of one particularallergen (the major allergen Bet v1) is obtained. Onthe other hand the competitive ELISA using thepolyclonal IgE is much more sensitive and indicatesthe total birch pollen allergens. Data obtained duringspring 1998 show good correlation of pollen counts andallergen content in the coarse particle fractioncontaining intact pollen (>10 m). In smallersized fractions, the allergen load is often close tothe detection limit. When clearly detectable amountsof allergen are present, in the fine size fraction theallergen load shows only a weak correlation to thepollen counts and the allergen concentrations in thecoarse particle fraction.     

Effects of Particle Size and Redox Potential on Arsenic Fractionation in Soils Irrigated with Arsenate-rich Water

Aging affects arsenic (As) bioaccessibility in soils. This study focuses on the influences of particle size and redox potential on As(V) aging in irrigated soils. The results showed that variation of As fractions in fine particles, except the loosely adsorbed fraction, was larger than that in coarse particles over time. Anoxic conditions decreased the change in As fractions, with the exception of the exchangeable fraction in soils over time, in comparison to the aerobic condition. The aging processes of As(V) in different particle sizes and soils at different redox potentials exhibited several stages. The only significant difference in the aging process of As(V) in different particle sizes was the longer transformation period of the water-soluble fraction into the Fe/Mn/Al oxides-bound fraction in fine particles than in coarse particles. The redox potential had a significant influence on the aging process of As(V) in soils after 10 days of incubation. In terms of As bioaccessibility, anoxic conditions shortened the aging process of As(V) in soils. During the aging process, fine particles and aerobic conditions intensified the decrease in As(V) bioaccessibility in soils in comparison to the coarse particles and anoxic condition.     

Synergism between components of the cellulase system of the anaerobic rumen fungus Neocallimastix frontalis and those of the aerobic fungi Penicillium pinophilum and Trichoderma koningii in degrading crystalline cellulose

The cellulase system of Neocallimastix frontalis was separated by differential affinity on cellulose into an adsorbed fraction that could solubilize crystalline cellulose (crystalline-cellulose-solubilizing fraction, CCSF), and a non-adsorbed fraction that contained endoglucanase and -glucosidase activities (non-adsorbed endoglucanase/ -glucosidas, NAE/-G) but which showed no activity to crystalline cellulose. Both fractions were tested for their capacity to act synergistically with the cellobiohydrolase (CBH) components of aerobic fungi in degrading crystalline cellulose. The CCSF acted synergistically with CBH I components of both Penicillium pinophilum and Trichoderma koningii but not with CBH II. The NAE/-G fraction also acted synergistically with the CBH components of P. pinophilum but, remarkably, only when both CBH I and CBH II were present in the reaction mixture. By comparison with previously published studies on the mechanism of action of P. pinophilum cellulase it is speculated that the CCSF of N. frontalis may contain CBH I- and CBH II-type enzymes.