稻田甲烷排放影响因素及其研究进展

CH4是大气中仅次于CO2的最重要的温室气体之一,其温室效应贡献已达15～20%。中国稻田是CH4的重要排放源,对全球大气的CH4排放起着重要的作用。本文较为详细地介绍了近几十年来国内外关于稻田CH4排放的研究进展。对稻田CH4的排放机理、CH4的排放规律及影响稻田CH4排放的各种因素作了详细分析,并相应地提出了控制稻田CH4排放的各种措施,最后提出了今后我国稻田CH4排放研究应加强的几个方面内容。     

南京郊区番茄地中氮肥的气态氮损失

采用田间试验研究了番茄地施用化学氮肥后的氨挥发、反硝化损失和N2O排放及其影响因素。氨挥发采用通气密闭室法测定，反硝化损失（N2＋N2O）采用乙炔抑制-土柱培养法测定，不加乙炔测定N2O排放。结果表明，番茄生长期间全部处理均未检测到氨挥发，其原因是土表氨分压低于检测灵敏度，较低的氨分压是由于表层土壤的铵态氮浓度和pH都不高所致。在番茄生长期间，对照区即来自有机肥和土壤本身的反硝化损失和N2O℃排放量相当高，反硝化损失总量高达N29．6kghm^-2，N2O排放量为N7．76kghm^-2。施用化学氮肥显著增加了反硝化损失和N2O排放，3个施用化学氮肥处理的反硝化损失变化在N40．8～46．1kghm^-2之间，占施入化肥氮量的5．50％～6．01％；N2O排放量为N13．6～17．6kghm^-2，占施入化肥氮量的2．62％～4．92％；与尿素相比，包衣尿素未能显著减低反硝化损失和N2O排放。施用尿素的处理在每次追肥后，耕层土壤均会出现NO3^--N高峰，继之的反硝化和N2O排放高峰。反硝化速率与土壤含水量呈极显著正相关。总的看来，番茄生长期间没有氨挥发，而硝化反硝化是氮素损失的重要途径之一。     

秸秆还田对灌溉玉米田土壤反硝化及N2O排放的影响

运用乙炔抑制技术研究了不同施氮水平下秸秆还田对灌溉玉米田土壤反硝化反应和氧化亚氮(N2O)排放的影响。结果表明,土壤反硝化速率及N2O的排放受氮肥施用、秸秆处理方式及其交互作用的显著影响。与秸秆燃烧相比,不施氮或低施氮水平时,秸秆还田可刺激培养初期反硝化反应速率及N2O排放,增加培养期间N2O平均排放通量;高施氮水平时,秸秆还田可降低反硝化反应速率及反硝化过程中的N2O排放。秸秆还田可降低反硝化中N2O/N2的比例。     

淹水土壤有机酸积累与秸秆碳氮比及氮供应的关系

有机酸积累和毒害是稻田秸杆还田中受到广泛关注的问题。本文以水稻与小麦秸杆为材料，采用淹水培养研究了甲酸、乙酸、丙酸及丁酸在士壤中的积累及其与秸秆碳氮比、氮肥添加量的关系。结果表明，在不施用氮肥的情况下。随秸秆用量的增加，秸秆处理的有机酸积累均显著增多。与稻秸处理相比，麦秸处理的有机酸（尤其足丙酸）积累量显著较高，土壤溶液中NH4^＋浓度显著较低。加入尿素明显减少有机酸积累，促进CH4排放，但对CO2的排放无显著影响；氮素的影响在麦秸处理中表现的尤为明显。上述结果说明麦秸的高碳氮比增加了无机氮的生物固定，抑制有机酸向CH4转化，从而导致麦秸处理有机酸积累量高于稻秸处理。施用氮肥是减少麦秸还田后有机酸积累的有效措施之一，但此措施将可能促进CH4的排放。     

Nitrification controls N2O production rates in a frozen boreal forest soil

The winter season has been identified as a significant contributor to N₂O emissions from boreal soils, but our understanding of the processes regulating these emissions is fragmentary. We investigated potential N-sources and pathways involved in N₂O formation in a frozen boreal forest soil by labeling soil samples with ¹⁵N-containing substrates, and measured rates of ¹⁵N₂O/¹⁵N₂ formation under both oxic and anoxic conditions. Our results showed that all N₂O produced in the frozen samples originate from denitrification, but the rate-limiting factor is NO₃⁻ availability, which is largely governed by nitrification. This suggests that N₂O formation in frozen boreal soils may be sustained for a prolonged period of time, but is governed by a delicate balance of the O₂ regime.     

Dinitrogen and N2O emissions in arable soils: Effect of tillage, N source and soil moisture

A laboratory investigation was performed to compare the fluxes of dinitrogen (N₂), N₂O and carbon dioxide (CO₂) from no-till (NT) and conventional till (CT) soils under the same water, mineral nitrogen and temperature status. Intact soil cores (0-10 cm) were incubated for 2 weeks at 25 °C at either 75% or 60% water-filled pore space (WFPS) with ¹⁵N-labeled fertilizers (100 mg N kg⁻¹ soil). Gas and soil samples were collected at 1-4 day intervals during the incubation period. The N₂O and CO₂ fluxes were measured by a gas chromatography (GC) system while total N₂ and N₂O losses and their ¹⁵N mole fractions in the soil mineral N pool were determined by a mass spectrometer. The daily accumulative fluxes of N₂ and N₂O were significantly affected by tillage, N source and soil moisture. We observed higher (P<0.05) fluxes of N₂+N₂O, N₂O and CO₂ from the NT soils than from the CT soils. Compared with the addition of nitrate (NO₃⁻), the addition of ammonium (NH₄⁺) enhanced the emissions of these N and C gases in the CT and NT soils, but the effect of NH₄⁺ on the N₂ and/or N₂O fluxes was evident only at 60% WFPS, indicating that nitrification and subsequent denitrification contributed largely to the gaseous N losses and N₂O emission under the lower moisture condition. Total and fertilizer-induced emissions of N₂ and/or N₂O were higher (P<0.05) at 75% WFPS than with 60% WFPS, while CO₂ fluxes were not influenced by the two moisture levels. These laboratory results indicate that there is greater potential for N₂O loss from NT soils than CT soils. Avoiding wet soil conditions (>60% WFPS) and applying a NO₃⁻ form of N fertilizer would reduce potential N₂O emissions from arable soils.     

纳米二氧化硅改性脲醛树脂的应用及机理研究

采用纳米SiO2 改性脲醛树脂, 当纳米SiO2 用量<1 5%时, 用量越大, 树脂的胶合强度越高, 游离甲醛含量越低, 粘度越大, 固化时间不变 用纳米SiO2 (用量1% ) /脲醛树脂(F/U摩尔比1 2)压制胶合板、刨花板、中密度纤维板, 板的各项性能指标都超过国家标准要求, 甲醛释放量达到E级水平 通过红外光谱分析, 初步探讨了纳米SiO对脲醛树脂的增强机理     

婴幼儿配方乳粉中甲醛含量测定及暴露污染评估

采用气相色谱定量及气相色谱-质谱确证,建立婴幼儿配方乳粉中甲醛含量的测定方法,并对网购45份婴幼儿配方乳粉中甲醛的污染水平进行调查分析与暴露风险评估.通过优化前处理条件,考察方法的线性关系、精密度、准确度、检出限及定量限等指标,采用外标法定量.结果表明:该方法在0～10μg范围内线性良好(r>0.999),方法检出限为...     

木质素基碳点和石墨烯量子点制备方法研究进展

碳点(CDs)和石墨烯量子点(GQDs)由于结构稳定、环境友好、水分散性和生物相容性良好、易于功能化改性和可光致发光等优点已成为备受关注的零维碳纳米材料,有望广泛应用于生化指示、生物医学、储能、显示器件和催化等前沿领域。近年来,相比于传统的化石燃料基化合物,来自可再生生物质的木质素及其衍生物不仅价廉易得、活性基团丰富,而且具有天然芳香结构,已成为CDs和GQDs的重要前驱体。但是,已有报道对木质素的解聚机制认识不足,这也逐渐成为制约木质素基CDs和GQDs性能提升的瓶颈之一。因此,必须阐明木质素在相关工艺过程中发生解聚的化学本质,并明确杂原子掺杂与木质素基CDs和GQDs的激发依赖发光行为的内在联系。笔者首先介绍了木质素基CDs和GQDs的制备方法发展历程和潜在应用,同时对其结构和性质等进行评述,重点讨论并总结了制备具有出色激发依赖发光行为的木质素基CDs和GQDs的技术难点,认为开发一类适用于普遍性木质素原料的高效环保解聚策略,以及揭示木质素基CDs和GQDs的杂原子掺杂与其激发依赖发光行为的关联机理将成为该领域今后的重点研究方向。     

漏缝地板发酵床对育肥羊养殖气体排放的影响及微生物学机理

为明确漏缝地板发酵床对育肥羊养殖过程氨(NH₃)和温室气体排放特征的影响机制,本研究设置地面和漏缝地板发酵床两个试验处理,测定分析了育肥羊养殖过程NH₃、氧化亚氮(N₂O)、二氧化碳(CO₂)和甲烷(CH₄)的排放特征,并采用宏基因组学解析了影响上述气体排放的微生物学机理。试验结果表明,与地面相比,漏缝地板发酵床能够显著降低育肥羊养殖过程的NH₃排放(P<0.05),其NH₃排放速率为21.64～58.92 mg·m^-2·h^-1,NH₃累积排放量为86.36±1.06 g·m^-2,减排率达58.60%。漏缝地板发酵床同样也能显著降低育肥羊养殖过程的CH₄排放速率(P<0.05),其CH₄累积排放量为26.66 g·m^-2,减排率可达64.42%。然而,漏缝地板发酵床会使得...