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.     

Survival of bacterial DNA and culturable bacteria in archived soils from the Rothamsted Broadbalk experiment

Dried soil samples from many sources have been stored in archives world-wide over the years, but there has been little research on their value for studying microbial populations. Samples collected since 1843 from the Broadbalk field experiment on crop nutrition at Rothamsted have been used to document changes in the structure and composition of soils as agricultural practices evolve, also offering an invaluable record of environmental changes from the pre- to post-industrial era in the UK. To date, the microbial communities of these soils have not been studied, in part due to the well-documented drop in bacterial culturability in dried soils. However, modern molecular methods based on PCR amplification of DNA extracted directly from soil do not require bacterial cells to be viable or intact and may allow investigations into the legacy of bacteria that were present at the time of sample collection.

In a preliminary study, to establish if dried soils can provide a historical record of bacterial communities, samples from the Broadbalk soil archive dating back to 1868 were investigated and plots treated with either farmyard manure (FYM) or inorganic fertilizer (NPK) were compared. As anticipated, the processes of air-drying and milling greatly reduced bacterial viability whilst DNA yields declined less and may be preserved by desiccation. A higher proportion of culturable bacteria survived the archiving process in the FYM soil, possibly protected by the increased soil organic matter. The majority of surviving bacteria were firmicutes, whether collected in 2003 or in 1914, but a wide range of genera was detected in DNA extracted from the samples using PCR and DGGE of 16S rRNA genes. Analysis of DGGE band profiles indicated that the two plots maintained divergent populations. Sequence analysis of bands excised from DGGE gels, from a sample collected in 1914, revealed DNA from - and β-proteobacteria as well as firmicutes. PCR using primers specific for ammonia oxidizing bacteria showed similar band profiles across the two treatments in recently collected samples, however older samples from the NPK plot showed greater divergence. Primers specific for the genus Pseudomonas were designed and used in real-time quantitative PCR to indicate that archived soil collected in 1868 contained 10-fold less pseudomonad DNA than fresh soil, representing around 10⁵ genomes g⁻¹ soil. Prior to milling, dramatically less pseudomonad DNA was extracted from recently collected air-dried soil from the NPK compared to the FYM plot; otherwise, the two plots followed similar trends. Overall bacterial abundance, diversity and survival during the archiving process differed in the two soils, possibly due to differences in clay and soil organic matter content. Nevertheless, the results demonstrate that air-dried soils can protect microbial DNA for more than 150 years and offer an invaluable resource for future research.     

典型旱作农田土壤氧化亚氮排放的氨氧化微生物相对贡献

氨氧化过程对氧化亚氮（N2O）排放具有重要贡献。在不同土壤类型和农田管理下,氨氧化微生物类群对N2O排放的相对贡献组成规律还缺乏系统的研究。本研究选取典型农田耕层土壤（潮土、黑土、砖红壤）,以及有机肥改良的砖红壤剖面土壤,采用选择性抑制法（乙炔和辛炔）研究氨氧化细菌（AOB）、氨氧化古菌和全程硝化菌（AOA+comammox）以及异养硝化菌对土壤硝化潜势、净硝化速率及N2O排放的相对贡献。结果表明,在耕层土壤中,潮土、黑土和砖红壤的pH分别是8.0、6.7和5.7,硝化潜势分别是N 32.5、6.6和4.8 mg?kg-1?d-1,净硝化速率分别是N 7.1、3.0和0.5 mg?kg-1?d-1,7天N2O累积排放量分别是N 38.0、35.4和8.7 μg?kg-1。AOB主导耕层土壤的硝化潜势,对硝化潜势的贡献分别是82%、58%和100%。对于净硝化速率,在潮土和砖红壤中,AOB和AOA+comammox贡献相当（均在30%~40%）,而黑土中由AOB主导（72%）。AOB主导耕层土壤的N2O排放,对N2O排放的贡献分别是72%、92%和58%。在改良的砖红壤剖面土壤中,在0~20 cm、20~40 cm和40~60 cm,pH分别是7.0、5.5和4.9,硝化潜势分别是N 6.6、2.0和1.1 mg?kg-1?d-1,净硝化速率分别是N 4.1、0.9和0.2 mg?kg-1?d-1,N2O排放分别是N 16.3、6.5和2.8 mg?kg-1?d-1。随土壤由深层至表层,硝化潜势、净硝化速率及N2O排放显著提高。AOA+comammox主导表层硝化潜势及净硝化速率的提高（分别贡献63%和54%）,AOB主导N2O排放的增加（贡献54%）。本研究为制定与土壤氨氧化特性及土壤性质相匹配的N2O减排措施提供了新的科学依据。     

辽河平原玉米田不同施肥下的土壤氨挥发特征

【目的】通过不同施肥措施对氨气排放贡献的研究,获得辽河平原化肥施用本地化的氨排放因子,为大气环境和生态等领域的相关研究提供参考借鉴。【方法】于2018年5—10月在沈阳农业大学试验基地开展不同施肥措施下的氨气排放的大田试验,以基肥施树脂包衣缓释化肥、拔节期追施尿素为常规施肥方式,设置无氮处理（T0）、常规施肥减半（T1）、常规施肥+生物炭（T2）、常规施肥一次性施入（T3）、常规施肥（T4）5个处理。采用通气法在玉米全生育期内定时收集氨气,利用流动分析仪检测计算氨排放通量,同时测定土壤铵态氮含量。【结果】施基肥后氨挥发速率呈现双峰趋势,各处理分别于施基肥后第1—2天或第5—7天达到氨挥发速率最大值,施基肥后各处理氨挥发速率最大值表现为：常规施肥减半（T1）>常规施肥+生物炭（T2）>常规施肥一次性施入（T3）>常规施肥（T4）>无氮处理（T0）;施追肥后各处理均于第1—2天达到氨挥发速率最大值,追肥后各处理氨挥发速率最大值表现为：常规施肥（T4）>常规施肥+生物炭（T2）>常规施肥减半（T1）>常规施肥一次性施入（T3）>无氮处理（T0）。氨挥发损失累积量表现为常规施肥+生物炭（T2)>常规施肥（T4）>常规施肥一次性施入（T3）>常规施肥减半（T1）>无氮处理（T0）。各时期各处理间的土壤铵态氮含量差异并不显著,但土壤铵态氮含量和同时期土壤氨挥发速率呈现出相似的变化趋势,施追肥后两者的变化趋势比施基肥后更加相似。由于T1、T2、T4追肥期施尿素,尿素释放铵态氮比缓释化肥更加迅速,同时氨挥发也相对较快。整体来看,减少50%施氮量,氨挥发损失累积量只减少20%。各处理间生长季内氨挥发损失累积量差异显著,常规施肥+生物炭（T2）的氨挥发损失累积量最多,在施氮量相同的情况下,加施生物炭氨挥发损失累积量增加22%。全生长季施氮量相同的情况下,一次性施入缓释化肥而不采取尿素追肥的措施比以尿素作为追肥的措施的氨挥发累积量减少12%。【结论】氨挥发随着施氮量增加呈现边际递减效应。生物炭促进了农田氨挥发,玉米秸秆生物炭呈碱性,导致了氨挥发累积量的增加,但其具有孔隙度和比表面积大、吸附效果强的特点,可改良土壤和减少其他温室气体。一次性施入缓释化肥而不采取尿素追肥显著降低了氨挥发。     

生物炭连续施用对农田土壤氮转化微生物及N2O排放的影响

【目的】研究连续添加生物炭6年后对农田土壤氮转化相关微生物功能基因的影响,揭示生物炭影响作物产量和N₂O排放的微生物学机制,并为生物炭的推广使用提供理论依据。【方法】通过在潮土农田设置0（BC0,对照)、2.25（BCL,低量）、6.75（BCM,中量）和11.25 t·hm^-2（BCH,高量）4个秸秆生物炭量处理的田间定位试验,采用田间观测、化学分析、荧光定量PCR（qPCR）技术,系统研究施用生物炭对氧化亚氮（N₂O）排放、氨单加氧酶（amoA）、亚硝酸还原酶（nirK、nirS）、氧化亚氮还原酶（nosZ）基因丰度及夏玉米产量的影响。【结果】与对照BC0处理相比,施用生物炭可显著提高夏玉米籽粒产量,且BCM处理籽粒产量达到最大值10 811 kg·hm^-2,显著降低夏玉米生育期N₂O累积排放量,并以BCM处理减少N₂O排放效果最优。研究还发现,在夏玉米多个生育时期,与对照比较,生物炭施用可以显著提高耕层土壤无机氮储量和土壤含水量。此外,随着生物炭施用量增加,土壤氨氧化古菌（AOA）基因拷贝数在夏玉米大喇叭口期和成熟期均表现为先上升后下降趋势,且两个时期均以BCM处理最高,而氨氧化细菌（AOB）基因拷贝数在夏玉米大喇叭口期和成熟期分别为BCH处理和BCM处理最高。与对照相比,中、高量生物炭施用（BCM、BCH处理）可显著提高夏玉米大喇叭口期和成熟期土壤反硝化作用功能相关基因（nirK、nirS、nosZ）拷贝数。相关性分析表明,夏玉米成熟期土壤N₂O排放通量与土壤硝态氮、土壤含水量、AOA、AOB、nirK、nirS、nosZ呈显著负相关关系。【结论】施用生物炭通过增加土壤微生物氮转化功能基因丰度进而降低土壤N₂O排放,通过增加土壤耕层无机氮储量和土壤水分含量进而提高作物产量,并以中等用量（6.75 t·hm^-2）施用效果最优。     

不同灌水下限设施番茄土壤CO2排放特征及其影响因素研究

【目的】探讨不同灌水下限设施土壤CO2排放特征及其影响因素,为调控设施土壤水分和碳排放提供理论依据。【方法】在番茄生育期内采用LI-8100A土壤碳通量自动测定仪观测不同灌水下限[20 kPa(D20)、30 kPa(D30)、40 kPa(D40)]下的土壤CO2排放速率,并分析其影响因素。【结果】在番茄生育期内,不同灌水下限设施土壤CO2排放速率变化趋势基本一致,D20处理最高,平均速率为2.759μmol/(m2·s),其次是D30处理,为2.601μmol/(m2·s),D40处理最低,为2.559μmol/(m2·s)。在土壤CO2累积排放量方面,D20处理显著高于其他2个处理,而D30和D40处理之间无显著差异。就单因素模型而言,不同灌水下限处理的土壤CO2排放速率与15 cm土壤温度呈指数回归关系,且均达显著水平(P<0.05);不同灌水下限处理的土壤CO2排放速率与15 cm土壤含水率均呈显著二次回归关系(P<0.05);与单因素模型相比,土壤温度和土壤含水率的双因素复合模型(68.5%~83.8%)可以更好地解释土壤CO2排放的变化。土壤温度敏感系数Q10值在1.442~1.498之间,其中D20处理最敏感,D40处理最不敏感。相关分析结果表明,土壤CO2累积排放量与0~20 cm土层土壤有机质量、pH值、全氮量、速效磷量、速效钾量、碱解氮量和微生物量碳呈显著相关关系。采用PCA分析提取出的2个主成分累积贡献率为85.79%。【结论】灌水下限影响设施土壤CO2的排放,其中D20处理促进了设施土壤CO2的排放。     

反刍家畜胃肠道甲烷排放与减排策略

反刍家畜胃肠道甲烷排放是重要的温室气体排放源,减少反刍家畜胃肠道甲烷排放有助于缓解全球温室效应和提高家畜饲养效率。本论文从中国反刍家畜胃肠道甲烷排放现状、瘤胃甲烷生成机制、甲烷生成的日粮营养影响因子和甲烷减排策略与潜力4个方面系统综述反刍家畜胃肠道甲烷排放的研究进展。目前,中国反刍家畜甲烷总排放量超过10 Tg,占全球胃肠道甲烷排放的比例超过15%。反刍家畜胃肠道甲烷排放主要来自瘤胃和后肠道,其中瘤胃甲烷占胃肠道甲烷生成总量的80%以上。二氧化碳还原路径利用瘤胃内的氢和二氧化碳合成甲烷,是瘤胃内生成甲烷的主要路径。瘤胃内的氢还可被相关微生物利用,合成挥发性脂肪酸和微生物蛋白等代谢产物,进而被机体利用。减少反刍家畜胃肠道甲烷排放的关键在于促进瘤胃内氢的利用,以及阻断瘤胃内的氢被甲烷菌利用合成甲烷。甲烷减排的日粮营养调控策略包括优化日粮组成、改善饲料品质、提高瘤胃流通速率、添加氢池和甲烷抑制剂等。大多数营养调控策略的甲烷减排效果小于40%,最新研制的3-NOP抑制剂的甲烷减排效果最高可达80%。但是,一些减排策略的产业化应用还受添加剂残留、抗生素禁用、食品安全、产品价格和消费者喜好等因素影响。牧场管理和遗传选育也是降低甲烷排放量的重要手段,过去100年来已实现每千克标准乳的甲烷排放量减排效果为57%。未来反刍家畜胃肠道甲烷研究将主要集中在低排放品种的遗传选育、不同营养调控策略间的组合效果、甲烷减排的经济效益和可持续性、家畜生长性能与健康、食品安全、消费者喜好等方面。     

丛枝菌根真菌调控土壤氧化亚氮排放的机制

氮素是陆地生态系统初级生产力的主要限制因子,自Haber-Bosch反应以来,氮肥的生产和施用极大地提高了粮食产量.然而过量施用氮肥导致氮肥利用率低,并造成了严重的环境污染,包括氮沉降、硝态氮淋洗以及N2O排放等.微生物直接参与土壤氮素循环,固氮微生物、氨氧化和反硝化微生物分别在土壤固氮、铵态氮转化和硝态氮转化过程中起...