干/湿法烘焙预处理对稻壳燃烧反应特性的影响

烘焙是提高生物质燃料性质的重要技术手段,探究干/湿法烘焙对稻壳热解燃烧反应特性的影响具有重要意义。该研究利用固定床与高压反应釜对稻壳进行了不同温度下的干法烘焙和湿法烘焙（水热碳化）预处理,并利用热重分析仪对稻壳、稻壳烘焙炭和稻壳水热炭开展了非等温燃烧反应特性分析,并且利用Coats?Redfern法与三种常见的气-固反应机理模型对样品的燃烧反应特性进行了动力学分析。最后,该研究对干法与湿法烘焙两种预处理方式对稻壳的热解燃烧反应特性的影响进行了比较。结果表明两种预处理方式对稻壳的热解与燃烧反应参数存在影响：均导致热解反应性降低,干烘焙提高稻壳燃烧反应性,且反应性随着干烘焙温度的提高而升高。但湿烘焙使稻壳燃烧反应性略有降低。在相同的预处理温度条件下,稻壳烘焙炭较稻壳水热炭具有更高的热解起始失重温度、更低的热解最大失重速率及其对应温度和热解反应性。对于稻壳、稻壳烘焙炭及稻壳水热炭的热解燃烧反应性,模型O1较其他两个模型的线性回归指数更高。干/湿法烘焙使稻壳热解活化能升高,而湿烘焙使燃烧活化能降低。此外,两个阶段样品的指前因子（A）均随活化能的增大而增大,二者间存在明显的线性关系（R2均大于0.95）,表明反应过程具有动力学补偿效应。     

白灵菇木质素降解酶系的检测及其染料脱色能力的研究

[目的]明确白灵菇(Pleurotus ferulae)分泌木质素过氧化物酶(LiP)、锰过氧化物酶(MnP)和漆酶(Laccase)的规律,以及白灵菇染料脱色的能力。[方法]利用紫外可见分光光度计,检测4种培养方式下白灵菇木质素降解酶活性,并在此基础上进行了白灵菇对5种染料的脱色研究。[结果]4种培养方式下,可以检测到MnP和Laccase的活性,但并未检测到LiP。添加Mn2+和2,6-二甲氧基苯酚(2,6-DMP)对MnP和Laccase的产生有抑制作用,而添加青杨木屑可以将MnP的活性提高1.28倍,将Laccase的活性提高3.75倍;白灵菇对中性红和活性黑2种染料的最大脱色率分别为87.12%和86.13%,对活性红和刚果红的最大脱色率分别为45.91%和32.28%,而对结晶紫几乎无脱色能力。[结论]白灵菇产Laccace活性要高于MnP;与脱色活性红、刚果红、结晶紫相比,白灵菇对中性红和活性黑2种染料的脱色更为彻底。     

脲醛树脂及三聚氰胺改性脲醛树脂对桉木热解液组分的影响

为了有效利用热解技术处理废弃人造板,采用气质联用技术对比分析桉木、添加质量分数10% 脲醛(UF)树 脂的桉木、添加质量分数10%三聚氰胺改性脲醛(MUF)树脂的桉木、UF 树脂、MUF 树脂的热解液组分。结果表 明:桉木热解液成分复杂,其中2,5-二甲基呋喃的相对含量达到27.56%,3-甲基-2-羟基-2-环戊烯-1-酮和4-(2-氧 代)-2-环己烯-1-酮的相对含量分别为7.04%和7.02%,2,6-二甲氧基苯酚的相对含量为9.48%。添加UF 树脂的 桉木热解液检测到含氮物质的相对含量比桉木热解液增加22.93%,该热解液有望用于肥料生产和土壤改良;添加 MUF 树脂的桉木热解液出现了木糖、丁内酯等桉木热解液中未检测到的产物。      

玉米芯和桉木的低温热解特性

为实现生物质资源的分级综合利用,该文采用热重分析仪和裂解气质联用仪进行了对玉米芯和桉木低温热解特性的研究。试验结果表明不同生物质原料低温快速热解产物有明显差异,玉米芯的低温快速热解产物主要有乙酸、2,3-二氢-苯并呋喃和2-甲氧基-4-乙烯基苯酚,而桉木的产物主要是乙酸、糠醛和5,6-二氢-4-羟基-吡喃-2-酮。生物质低温快速热解产物种类较少,分布较为集中,玉米芯和桉木的酸类、呋喃类,桉木的吡喃类热解产物相对含量随温度上升而降低。生物质低温热解能有效分解其半纤维素,这为降低中温热解油的酸性和水分提供了理论指导。     

Impact of long-term N fertilization on the structural composition of spruce litter and mor humus

The aims of this study were to determine the degree of lignin degradation and to investigate changes in the chemical composition of the organic matter in the forest floor in an N fertilized Norway spruce forest soil. Needle litter and mor humus were collected from the field experiment at Skogaby in southern Sweden (56°33′N; 13°13′E). The spruce stand had been fertilized for 11 years with 100 kg N ha⁻¹ yr⁻¹ as (NH₄)₂SO₄. The degree of lignin degradation was determined with alkaline CuO oxidation followed by HPLC analysis. The chemical composition of the organic matter was characterized by CPMAS ¹³C NMR. Tannin was specifically analyzed using dipolar dephasing CPMAS ¹³C NMR and the N distribution was studied by CPMAS ¹⁵N NMR.The C-to-N ratios in the fertilized Oi and Oe layers were significantly lower than in the unfertilized layers (24 compared to 34 and 23 compared to 27, respectively). Neither the sum of the CuO oxidation products (Vanillyls+Syringyls+Cinnamyls expressed as VSC) nor the acid-to-aldehyde ratio ((Ac/Al)_V) showed any significant treatment effects. The content of aromatic C (including phenolic C) was significantly lower in the unfertilized than in the fertilized Oi layer (18 versus 21%). In the unfertilized soil, VSC was positively correlated (r=+0.63, p<0.05) with the C-to-N ratio, whereas the phenolic C content was negatively correlated (r=−0.61, p<0.05). The tannin index showed a tendency of increasing from Oi to Oe layers in both treatments. Most of the organic N was found as amide-N, whereas no heterocyclic N was detected. We have not been able to show any major C structural changes due to N fertilization. We suggest that the significantly higher content of aromatic and phenolic C in the fertilized Oi layer is due to an initial stimulation of the microbial community.     

脲醛树脂的纳米级改性研究

介绍了蒙脱土、有机蒙脱土、木质素三种物质对脲醛树脂的改性过程并对改性后脲醛树脂的各项性能进行了测试。结果表明:蒙脱土通过插层处理变为有机蒙脱土后,能显著改善脲醛树脂的性能指标。木质素和未改性的蒙脱土对改善脲醛树脂胶黏剂游离甲醛释放量几乎无影响。     

Analysis of leaf and needle litter decomposition by differential scanning calorimetry and differential thermogravimetry

Summary Changes in the physicochemical properties of three kinds of litter (Prunus serotina leaves, Carpinus betulus leaves, and Pinus sylvestris needles) were analyzed by differential scanning calorimetry and differential thermogravimetry after decomposition for 12 to 27 months under field conditions. As expected, holocellulose was always decomposed to a larger extent than the corresponding lignin components, leading to an enrichment of lignin in the residue. These lignins were more or less modified depending on the plant species. Moreover, the results suggest that energy-rich crystalline cellulose accumulates during decomposition at the expense of easier degradable amorphous cellulose and hemicelluloses. The quotient Q, from the corresponding calorimetry and thermogravimetry values, was introduced to estimate the specific energy content as a measure for the decomposition of litter components.Dedicated to the late Prof. Dr. W. Kühnelt     

Organic C and N stabilization in a forest soil: Evidence from sequential density fractionation

In mineral soil, organic matter (OM) accumulates mainly on and around surfaces of silt- and clay-size particles. When fractionated according to particle density, C and N concentration (per g fraction) and C/N of these soil organo-mineral particles decrease with increasing particle density across soils of widely divergent texture, mineralogy, location, and management. The variation in particle density is explained potentially by two factors: (1) a decrease in the mass ratio of organic to mineral phase of these particles, and (2) variations in density of the mineral phase. The first explanation implies that the thickness of the organic accumulations decreases with increasing particle density. The decrease in C/N can be explained at least partially by especially stable sorption of nitrogenous N-containing compounds (amine, amide, and pyrrole) directly to mineral surfaces, a phenomenon well documented both empirically and theoretically. These peptidic compounds, along with ligand-exchanged carboxylic compounds, could then form a stable inner organic layer onto which other organics could sorb more readily than onto the unconditioned mineral surfaces (“onion” layering model).To explore mechanisms underlying this trend in C concentration and C/N with particle density, we sequentially density fractionated an Oregon andic soil at 1.65, 1.85, 2.00, 2.28, and 2.55 g cm⁻³ and analyzed the six fractions for measures of organic matter and mineral phase properties.All measures of OM composition showed either: (1) a monotonic change with density, or (2) a monotonic change across the lightest fractions, then little change over the heaviest fractions. Total C, N, and lignin phenol concentration all decreased monotonically with increasing density, and ¹⁴C mean residence time (MRT) increased with particle density from ca. 150 years to >980 years in the four organo-mineral fractions. In contrast, C/N, ¹³C and ¹⁵N concentration all showed the second pattern. All these data are consistent with a general pattern of an increase in extent of microbial processing with increasing organo-mineral particle density, and also with an “onion” layering model.X-ray diffraction before and after separation of magnetic materials showed that the sequential density fractionation (SDF) isolated pools of differing mineralogy, with layer-silicate clays dominating in two of the intermediate fractions and primary minerals in the heaviest two fractions. There was no indication that these differences in mineralogy controlled the differences in density of the organo-mineral particles in this soil. Thus, our data are consistent with the hypothesis that variation in particle density reflects variation in thickness of the organic accumulations and with an “onion” layering model for organic matter accumulation on mineral surfaces. However, the mineralogy differences among fractions made it difficult to test either the layer-thickness or “onion” layering models with this soil. Although SDF isolated pools of distinct mineralogy and organic-matter composition, more work will be needed to understand mechanisms relating the two factors.     

Constraints on development of fungal biomass and decomposition processes during restoration of arable sandy soils

In an earlier study we reported the apparent stabilization of a low fungal biomass in ex-arable lands during the first decades after abandonment. It was hypothesized that the lack of increase in fungal biomass was due to constraints on development of fungi with persistent hyphae such as lignocellulolytic basidiomycetes and ericoid mycorrhizal fungi. With respect to the former group, the slow increase of the pool of lignocellulose-rich organic matter was expected to be the major constraint for their development. To study this, we enriched soil samples of one arable land, of two recently abandoned arable lands, of one older abandoned arable land and of heathland with carbon substrates that differed in composition (glucose, cellulose and sawdust). In addition, we combined the effect of carbon addition on fungal biomass development in arable and recently abandoned lands with inoculation of 1% of soil from the older abandoned site and the heathland. All treatments induced a fast increase and a subsequent rapid decline in fungal biomass in the arable and ex-arable fields. Denaturing Gradient Gel Electrophoresis (DGGE) band patterns and enzyme activities did show differences between the carbon treatments but not between the recent and older abandoned field sites, indicating a similarly responding fungal community even after three decades of land abandonment and irrespective of soil inoculation. Identification of fungi by sequencing and culturing confirmed that decomposition processes were mostly dominated by opportunistic fungi in arable and ex-arable fields. In the heathland, only a very slow increase of microbial activity was observed after addition of carbon and sequencing of DGGE bands showed that ericoid mycorrhiza (ERM) fungi were responsible for carbon decomposition. We conclude that an increase of enduringly present fungal hyphae in ex-arable land may only be possible when a separate litter layer develops and/or when suitable host plants for ERM fungi become established.