三峡库区消落带落羽杉人工林土壤细菌群落结构多样性及动态变化

消落带是连接陆地与水域的交错地带,具有重要的生态功能,其适生木本植物的种植对消落带土壤的生物地球化学循环起着重要的作用.为探究适生植物对三峡库区消落带环境的适应机制,采用高通量测序技术对消落带退水后适生植物落羽杉(Taxodium distichum)不同生长时期(T1:5月、 T2:7月和T3:9月)的土壤细菌群落组成及多样性进行研究,同时采用PICRUSt2对细菌功能进行预测.结果表明,土壤pH值、硝态氮、铵态氮、土壤蔗糖酶、磷酸酶和脲酶等理化指标随时间变化显著(P<0.05);土壤细菌多样性、丰富度和结构也随时间变化而变化,除Chao1以外,根际土壤细菌的α多样性均表现为：T1>T2>T3,非根际土壤细菌α多样性则表现为：T3>T1>T2. RDA分析表明,影响细菌群落的理化指标主要有土壤pH值、脲酶、铵态氮和硝态氮.所有土壤样本中共检测到细菌60门,其中以变形菌门和酸杆菌门为优势细菌门.根据PICRUSt2预测,代谢是落羽杉土壤细菌群落中普遍存在的基本功能,与C、 N和P有关的各代谢途径存在一定的时间差异.以上研究结果有助于加深对三峡消落带植被修复...     

牡蛎壳粉和石灰改良酸性水稻土对磷有效性、形态和酶活性的影响

我国南方粮食主产区土壤酸化治理是提升耕地地力促进粮食增产的重要内容,目的是探究酸化土壤改良剂牡蛎壳粉和石灰对水稻土酸度、磷有效性和形态以及酶活性和相关功能基因的影响.盆栽试验设计2种改良剂的3个施用量（0.05%、0.10%和0.15%）,以水稻为试验作物.结果表明：①牡蛎壳粉和石灰均显著提高土壤pH,降低土壤交换性酸,且改良效果随着改良剂用量增加而提高,相同用量下石灰对土壤酸性的改良效果高于牡蛎壳粉;② 4种有效磷提取剂提取的土壤有效磷测定结果表明,牡蛎壳粉和石灰显著提高H₂SO₄-P、Bray-1 P和Olsen-P含量,其中Olsen-P含量随改良剂用量的增加而提高.③土壤中不同形态无机磷含量表现为：Fe-P>Al-P>Ca-P,石灰和牡蛎壳粉显著提高Al-P和Fe-P含量,分别提高26.3%~37.4%和7.9%~23.7%;0.15%改良剂显著增加Ca-P含量;④石灰和牡蛎壳粉对土壤DHA、ALP、IPP活性和phoD基因拷贝数具有提高作用,而对土壤ACP活性、phoC和pqqC拷贝数表现为降低;⑤改良剂（0.10%和0.15%）显著提高水稻产量,0.15%用量的石灰和牡蛎壳粉分别提高水稻产量34.2%和46.8%,但对秸秆生物量无显著影响.相关分析表明,土壤无机磷和有效磷含量与pH和ALP活性呈显著正相关,改良剂通过消除土壤酸化和提高土壤磷酸酶活性来改善土壤磷营养状况,这对促进作物产量具有积极作用.     

生物炭施用对黄壤土壤养分及酶活性的影响

生物炭因其具有特殊的理化性质,作为土壤改良剂或调理剂被广泛应用于改善土壤质量;土壤养分与土壤酶活性是表征土壤质量化学性质和生物学性质的重要指标.采用大田试验,研究生物炭不同施用水平：0（CK）、5（B5）、10（B10）、20（B20）和50（B50） t·hm^-2对黄壤养分和土壤酶活性的影响,运用结构方程模型（SEM）定量分析生物炭处理对土壤养分和酶活性的直接或间接影响及其作用大小.结果表明,生物炭显著增加土壤pH值、电导率、有机碳、碱解氮、有效磷和速效钾（P<0.05）;随生物炭施用量的增加,土壤过氧化氢酶和脲酶活性先增加后降低,磷酸酶和蔗糖酶活性增加（P<0.05）;B10处理下,土壤过氧化氢酶、脲酶和磷酸酶的活性均达到最大值,蔗糖酶活性也相对较高.随生物炭作用时间增加,土壤pH值、碱解氮、有效磷和速效钾含量均增加,而电导率和有机碳与之相反;过氧化氢酶活性降低,脲酶和磷酸酶活性升高,蔗糖酶活性无明显变化规律.SEM结果显示,生物炭施用对过氧化氢酶具有直接的负效应;通过提升pH、电导率、有机碳和碱解氮含量间接影响过氧化氢酶活性,通过提升pH和电导率间接促进蔗糖酶活性,通过提高电导率以及碱解氮和有效磷含量间接增加磷酸酶活性.综上,生物炭施用量及作用时间显著影响土壤养分含量,进而间接作用于土壤酶活性;酸性黄壤施用10 t·hm^-2的生物炭较为适宜.     

纤维素降解真菌的分离鉴定及特性研究

经过实验分离到一株纤维素降解真菌CD-Q1,通过形态及分子生物学鉴定该真菌为匍匐根霉。该菌能够以滤纸、秸秆和脱酯棉为唯一碳源生长,8 d内可将26.5%的秸秆降解,可将7.5%的滤纸糖化。当以滤纸为唯一碳源时,pH=5条件下,滤纸失重及还原糖产生量最高,45 h内可将3%滤纸降解,生成0.845 mg/ml的还原糖(以葡萄糖计)。该纤维素降解真菌的分离为纤维素糖化及进一步利用提供了较好菌源,为纤维素降解性能的基因改良提供了理想的出发菌株。     

纳米零价铁在应用中存在的问题及提高反应活性的方法

纳米零价铁对多种污染物质均有较好的去除效果,在污染的水体、土壤及底泥中被广泛研究与应用。前人对纳米零价铁的制备、在污染治理各方面的应用、作用的机理等方面进行了较为详细的总结,针对纳米零价铁在应用中存在的问题虽有提及,但少有人集中进行整理。本文主要针对纳米零价铁在环境治理方面存在的问题进行论述并对提高其反应活性的常用方法进行了总结,以期为纳米零价铁实际应用领域的深入研究提供借鉴并拓展新的思路。     

An analysis of the likely success of policy actions under uncertainty: Recovery from acidification across Great Britain

In the context of wider debates about the role of uncertainty in environmental science and the development of environmental policy, we use a Generalised Likelihood Uncertainty Estimate (GLUE) approach to address the uncertainty in both acid deposition model predictions and in the sensitivity of the soils to assess the likely success of policy actions to reduce acid deposition damage across Great Britain. A subset of 11, 699 acid deposition model runs that adequately represented observed deposition data were used to provide acid deposition distributions for 2005 and 2020, following a substantial reduction in SO₂ and NO_x emissions. Uncertain critical loads data for soils were then combined with these deposition data to derive estimates of the accumulated exceedance (AE) of critical loads for 2005 and 2020. For the more sensitive soils, the differences in accumulated exceedance between 2005 and 2020 were such that we could be sure that they were significant and a meaningful environmental improvement would result. For the least sensitive soils, critical loads were largely met by 2020, hence uncertainties in the differences in accumulated exceedance were of little policy relevance. Our approach of combining estimates of uncertainty in both a pollution model and an effects model, shows that even taking these combined uncertainties into account, policy-makers can be sure that the substantial planned reduction in acidic emissions will reduce critical loads exceedances. The use of accumulated exceedance as a relative measure of environmental protection provides additional information to policy makers in tackling this ‘wicked problem’.     

Microbial biomass yield and turnover in soil biodegradation tests: carbon substrate effects

Most of the standardized biodegradation tests used to assess the ultimate biodegradation of environmentally degradable polymers are based solely on the determination of net evolved carbon dioxide. However, under aerobic conditions, it has to be considered that heterotrophic microbial consortia metabolize carbon substrates both to carbon dioxide and in the production of new cell biomass. It is generally accepted that in the relatively short term, 50% of the carbon content of most organic substrates is converted to CO₂, with the remaining carbon being assimilated as biomass or incorporated into humus. The latter is particularly important when the metabolism of the organic matter occurs in a soil environment. A straightforward relationship between the free-energy content of a carbon substrate (expressed as the standard free-energy of combustion) and its propensity for conversion to new microbial biomass rather than mineralization to CO₂ has been established. This can potentially lead to underestimation of biodegradation levels of test compounds, especially when they consist of carbon in a fairly low formal oxidation state and relatively high free-energy content. In the present work, the metabolism of different kind of carbon substrates, especially in soil, is reviewed and compared with our own experimental results from respirometric tests. The results show that conversion of highly oxidized materials, such as the commonly used reference materials, cellulose or starch, to CO₂ may be significantly overestimated. The addition of glucosidic material to soil leads to greatly increased respiration and is accompanied by a very low conversion to biomass or humic substances. In contrast, relatively less oxidized substrates metabolize more slowly to give both CO₂ and biomass to an extent which may be significantly underestimated if glucosidic materials are used as the reference. The need for an overall carbon balance taking into account both the carbon immobilized as biomass and that volatized as CO₂ must be considered in standard respirometric procedures for assessing the biodegradability of slowly degrading macromolecules.     

Bacterial colonization of the phyllosphere of nineteen plant species and antimicrobial activity of their leaf secondary metabolites against leaf associated bacteria

Summary. The scope of this work was to examine whether leaf constitutive secondary metabolites play a role in determining bacterial colonization of the phyllosphere. To this aim, we surveyed nineteen native or cultivated plant species that share a common bacterial pool in a North Mediterranean area, and estimated the size of total and ice nucleation active (INA) bacterial populations on their leaves. Large differences in the colonization of their phyllosphere were found; the population size of epiphytic bacteria ranged from 7.5 × 10² to 1 × 10⁶ CFU/g fresh weight, in eucalypt and celery, respectively. Species native in Mediterranean-type climate areas, particularly those belonging to the group of aromatic plants, are characterized by scarce presence of INA bacteria. The antibacterial activity of essential oils, surface phenolics and leaf tissue extracts was also estimated against the INA strains P. syringae and E. herbicola, isolated from two of these plant species. E. herbicola proved more sensitive than P. syringae. Of the species examined, oregano [Origanum vulgare L. subsp. hirtum (Link.) Ietswaart], an aromatic plant, had the highest antimicrobial activity, whereas six species showed no activity at all. Further experiments were performed with oregano and bean (Phaseolus vulgaris L.) that represent two extremes in their secondary metabolite content. Both plants were inoculated with P. syringae. By the end of incubation, the bacterial population on bean plants was about 100 times higher than that on oregano leaves. Scanning electron micrographs showed that bacterial growth on oregano leaves was confined to sites away from glandular hairs. Results from the bacterial colonization survey together with those from the toxicity tests showed that all species rich in antibacterial secondary metabolites harbored low leaf bacterial populations. These results provide substantial evidence that leaf secondary metabolites function as constitutive defense chemicals against microbial invasions. However, the fact that species with non- or moderately active leaf secondary metabolites are not always highly colonized suggests mediation of other unknown factors, the contribution of which requires further investigation.     

Differences in nitrous oxide fluxes from red soil under different land uses in mid-subtropical China

Red soil may play an important role in nitrous oxide (N₂O) emissions due to its recent land use change pattern. To predict the land use change effect on N₂O emissions, we examined the relationship between soil N₂O flux and environmental determinants in four different types of land uses in subtropical red soil. During two years of study (January 2005-January 2007), biweekly N₂O fluxes were measured from 09:00 to 11:00 a.m. using static closed chamber method. Objectives were to estimate the seasonal and annual N₂O flux differences from land use change and, reveal the controlling factors of soil N₂O emission by studying the relationship of dissolved organic carbon (DOC), microbial biomass carbon (MBC), water filled pore space (WFPS) and soil temperature with soil N₂O flux. Nitrous oxide fluxes were significantly higher in hot-humid season than in the cool-dry season. Significant differences in soil N₂O fluxes were observed among four land uses; 2.9, 1.9 and 1.7 times increased N₂O emissions were observed after conventional land use conversion from woodland to paddy, orchard and upland, respectively. The mean annual budgets of N₂O emission were 0.71-2.21 kg N₂O-N ha⁻¹ year⁻¹ from four land use types. The differences were partly attributed to increased fertilizer use in agriculture land uses. In all land uses, N₂O fluxes were positively related to soil temperature and DOC accounting for 22-48% and 30-46% of the seasonal N₂O flux variability, respectively. Nitrous oxide fluxes did significantly correlate with WFPS in orchard and upland only. Nitrous oxide fluxes responded positively to MBC in all land use types except orchard which had the lowest WFPS. We conclude that (1) land use conversion from woodland to agriculture land uses leads to increased soil N₂O fluxes, partly due increased fertilizer use, and (2) irrespective of land use, soil N₂O fluxes are under environmental controls, the main variables being soil temperature and DOC, both of which control the supply of nitrification and denitrification substrates.