谷氨酸棒状杆菌尿素传感器的研究

基于腺酶催化尿素分解产生氨,以氨气敏电极为基础电极,用含脲酶丰富的谷氨酸棒状杆菌研制成测定尿素的微生物传感器.在30℃、pH8.0、0.1mol/L磷酸盐缓冲液中,该传感器的线性范围为1.1×10^-4～1.4×10^-2mol/L,斜率为51.2mV/decade,检测下限为1.0×10^-5mol/L,寿命可达45d.考察了传感器响应初速和底物浓度之间的关系,测定了微生物膜中脲酶的表观米氏常数K_m及最大响应初速v_m.     

氮添加对马尾松人工林土壤团聚体氮矿化及土壤酶活性的影响

土壤氮库是生态系统氮素重要的源和汇。以三峡库区马尾松（Pinus massoniana）人工林为研究对象,从团聚体视角出发分析土壤养分和酶活性对氮添加的响应规律,以及相应的变化对氮矿化的影响,为预测该地区在大气氮沉降持续增加的背景下土壤氮动态提供参考。设置4种量的氮添加处理（N₀：0 kg N hm^-2 a^-1;N₃₀：30 kg N hm^-2 a^-1;N₆₀：60 kg N hm^-2 a^-1;N₉₀：90 kg N hm^-2 a^-1）,将土壤按粒径分为>2000 μm （大团聚体）、250-2000 μm （小团聚体）和<250 μm （微团聚体）3个组分的团聚体,观察团聚体氮矿化特征。结果表明：（1）与对照相比,N₃₀和N₆₀处理提高了有机质（SOM）含量,但土壤SOM和全氮（TN）含量在N₉₀下开始出现下降;氮添加降低了土壤速效磷（aP）含量,在小团聚体中表现最为显著。除微团聚体中的POD和NAG以外,其余3种酶的活性均在N₃₀和N₆₀处理之下被提高。（2）土壤平均净硝化速率整体高于土壤平均净氨化速率;大团聚体和小团聚体中净氨化速率在氮添加处理后显著降低,大团聚体净硝化速率低于其他两个粒径;土壤净氮转化速率在N₉₀处理下最高。（3）土壤养分和无机氮含量与土壤酸性磷酸酶（AP）、N-乙酰-β-D-葡糖苷酶（NAG）、过氧化物酶（POD）、硝酸还原酶（NR）和脲酶（UE）的活性呈显著相关,酶活性变化是多因子综合作用的结果;RDA分析显示,UE与土壤净氨化速率存在显著正相关,NAG和POD是与净氮转化速率分别存在显著正相关和显著负相关的关键土壤酶。综上所述,硝化作用是土壤净氮转化的主要贡献者,微团聚体在土壤氮矿化中发挥主要作用,NAG和POD是改变土壤净氮转化的主要生物酶。此外,氮添加会引起土壤氮素的流失,引起土壤的磷限制,并对土壤养分循环产生显著影响。     

油菜素内酯浸种对盐胁迫番茄种子萌发的影响及其生理机制

为揭示油菜素甾醇类化合物提高作物耐盐的效应和机理,研究了10^-11、10^-10、10^-9、10^-8、10^-7、10^-6、10^-5 mol/L 2,4-表油菜素内酯（EBL）浸种处理对0、50、100、150、175 mmol/L NaCl胁迫7 d的番茄种子萌发、生长、溶质积累、抗氧化代谢的影响。结果显示：NaCl浓度越高的盐胁迫下,10^-9 mol/L EBL浸种可体现出越显著的促进番茄种子萌发的效应;在所有处理下,EBL浸种浓度过高,即10^-6、10^-5 mol/L EBL,均表现出对种子萌发的抑制效应。盐胁迫下种子萌发后,一定浓度的EBL浸种可表现出明显的增加种子胚根和下胚轴长,提高萌发种子鲜重和种子活力指数,其中10^-9 mol/L EBL浸种处理促进效果最适;EBL浸种浓度过高,则表现出抑制效应。150 mmol/L NaCl胁迫或非盐胁迫下,10^-9 mol/L EBL浸种均可降低萌发种子体内的O₂^·-、H₂O₂、丙二醛（MDA）和脯氨酸（Pro）含量;盐胁迫下,10^-9 mol/L EBL浸种可显著提高萌发种子可溶性糖（SS）和可溶性蛋白（SP）的含量。150 mmol/L NaCl胁迫或非盐胁迫下,10^-9 mol/L EBL处理可不同程度促进番茄种苗超氧化物歧化酶（SOD）和过氧化物酶（POD）活性的上升。综上所述,盐胁迫下,一定浓度范围内的EBL浸种可明显促进番茄种子萌发或成苗,其中以10^-9 mol/L EBL浸种的效果最好,主要是因为EBL施用可积极促进番茄种子萌发中物质转化,SS和SP等溶质积累增多,增强其渗透调节能力;同时SOD和POD酶活增强,缓解盐胁迫导致番茄种子萌发中的次生氧化胁迫。     

2.5次微分伏安法对生物样品中丙二醛的测定

以0.1mol/L NH₄Cl溶液为介质, 用2.5次微分伏安法测定了丙二醛, 线性范围为1.0×10^-6至1.0×10^-3 mol/L, 检测限达1.0×10^-7 mol/L. 并测定了细胞培养液介质中新生SD大鼠心室肌细胞样品中的丙二醛.     

氮肥形态对冬小麦根际土壤氮素生理群活性及无机氮含量的影响

采用大田盆栽方法研究了硝态氮肥、铵态氮肥、酰胺态氮肥3种氮肥形态对冬小麦品种豫麦50生育中后期(拔节期、开花期、花后14 d、花后28 d)根际土壤氮转化相关微生物活性、酶活性和根际土壤NH+4离子、NO-3离子含量的影响。结果表明:随着生育期的推进,除脲酶外,氨化细菌、硝化细菌、亚硝化细菌、反硝化细菌和蛋白酶活性变化的均为"倒V"型变化特征,以花后14 d活性最强;而脲酶活性在拔节期最强,并且其活性远大于其它微生物及酶。氮肥形态对根际土壤氮素生理群及无机氮的影响不同。酰胺态氮肥促进了根际氨化细菌、反硝化细菌、脲酶、蛋白酶的活性,而硝化细菌、亚硝化细菌在硝态氮肥条件下活性较强。除拔节期外,土壤中NH+4离子在铵态氮肥处理下含量较高,NO-3离子在酰氨态氮肥处理下含量较高。因此,酰胺态氮能够促进小麦根际土壤有机氮的分解,硝态氮肥可以促进土壤中氨的转化,以利于小麦根系的吸收与利用。氮肥形态主要是通过影响土壤中氮素生理类群及酶的活性,从而影响土壤中无机氮的含量。     

重茬地黄土壤酚酸的动态积累及其对地黄生长的影响

为了探究酚酸物质与地黄连作障碍之间的关系,检测了重茬地黄土壤中阿魏酸、香草酸、香草醛和对羟基苯甲酸等4种酚酸物质的积累量,并通过水培条件下添加酚酸,研究了4种酚酸对地黄生长的影响。结果表明：阿魏酸、香草酸和香草醛含量在地黄生长期表现为持续增加,而对羟基苯甲酸含量先升高后降低;外加阿魏酸（8 μg·ml^-1）、香草酸（0.8 μg·ml^-1）、香草醛（1.2 μg·ml^-1）和对羟基苯甲酸（3.0 μg·ml^-1）对水培地黄根长、根质量、全株鲜质量和株高有较强的抑制作用;酚酸处理使地黄叶片叶绿素含量降低,除对羟基苯甲酸外差异性极显著;经过酚酸处理的地黄幼苗SOD和POD活性为先升高后下降,丙二醛含量升高,其中阿魏酸的处理使根中酶活性降至最低,根部腐烂死亡。推测4种酚酸可能是造成地黄化感作用的物质。     

氮素添加对贝加尔针茅草原土壤团聚体微生物群落的影响

大气氮沉降增加作为全球气候变化的重要因素,其对土壤生态系统影响的研究受到了生态学家的广泛关注。土壤微生物是有机物分解和养分循环的主要参与者,在维持土壤的功能多样性和可持续发展方面发挥着重要的作用。氮沉降的激增会引起土壤微生物群落结构和功能的改变。土壤中营养物质在不同团聚体组分中分布的不均匀,为微生物提供了空间异质微生境。为揭示草原土壤不同粒径团聚体中微生物群落分布及其对氮素添加响应特征。自2010年起,在内蒙古贝加尔针茅草原典型地段设置N₀（0 kg hm^-2 a^-1）、N₁₅（15 kg hm^-2 a^-1）、N₃₀（30 kg hm^-2 a^-1）、N₅₀（50 kg hm^-2 a^-1）、N₁₀₀（100 kg hm^-2 a^-1）、N₁₅₀（150 kg hm^-2 a^-1）6个氮素添加处理模拟氮沉降野外控制试验。采用磷脂脂肪酸（phospholipid fatty acid,PLFA）法测定>2 mm、0.25-2 mm和<0.25 mm 3个粒径土壤团聚体中微生物PLFA含量,探讨氮素添加对土壤团聚体微生物群落结构的影响。结果表明：氮素添加提高了土壤碳、氮含量,降低了土壤pH。氮素添加显著提高了0.25-2 mm土壤团聚体微生物群落磷脂脂肪酸总量、真菌磷脂脂肪酸含量和真菌/细菌（Fungi/bacteria,F/B）、革兰氏阳性菌/革兰氏阴性菌（Gram-positive bacteria/gram-negative bacteria,G⁺/G^-）的比值（P<0.05）,降低了土壤团聚体微生物Margalef丰富度指数（P<0.05）。相关性分析表明,土壤团聚体微生物总PLFAs、真菌PLFAs含量、G⁺/G^-、F/B与土壤有机碳、全氮含量呈显著正相关关系,与C/N值负相关。综合研究表明,连续8年氮素添加显著提高了土壤有机碳和全氮含量、降低了土壤pH;提高了0.25-2 mm土壤团聚体真菌群落,土壤有机碳、全氮的固持与真菌群落的增加有关。     

川续断提取皂甙促进骨质疏松模型中骨髓基质细胞成骨分化的作用机制研究

摘要 目的：探讨川续断提取皂甙（ASA）促进骨质疏松模型中骨髓基质细胞（rBMSCs）成骨分化的作用机制。方法：选取3月龄的雌性SD大鼠60只,随机分为卵巢切除组和假手术组,每组30只。采取卵巢切除法构建骨质疏松模型。建模成功后采用微型计算机断层扫描获得其松质骨微观结构的三维图像并进行分析。采用CCK-8法测定ASA对卵巢切除组rBMSCs增殖的影响。分析碱性磷酸酶（ALP）活性;荧光定量PCR检测成骨基因ALP、骨桥蛋白（OPN）、Runt相关转录因子2（RUNX2）的表达情况;蛋白免疫印迹试验检测磷脂酰肌醇3激酶（PI3K）、磷酸化蛋白激酶B（p-AKT）蛋白表达情况。结果：与假手术组比较,卵巢切除组骨小梁数量、骨小梁厚度和骨体积分数下降,但骨小梁分离度升高,差异有统计学意义（P＜0.05）。第4天和第7天,ASA(10^-5 mol/L)组、ASA(10^-6 mol/L) 组、ASA(10^-7 mol/L) 组和ASA(10^-8 mol/L) 组rBMSC增殖均显著高于ASA(0学艺术mol/L)组,以ASA(10^-5 mol/L)最为显著;而ASA(10^-1 mol/L) 组、ASA(10^-2 mol/L) 组、ASA(10^-3 mol/L) 组和ASA(10^-4 mol/L) 组rBMSC增殖显著低于ASA(0 mol/L)组,以ASA(10^-4 mol/L)最为显著,差异均有统计学意义（P＜0.05）。第7天和第14天,ASA(10^-5 mol/L)组、ASA(10^-6 mol/L) 组、ASA(10 ^-7 mol/L) 组和ASA(10^-8 mol/L) 组ALP活性均显著高于ASA(0 mol/L)组,且第14天ALP活性高于第7天,差异均有统计学意义（P＜0.05）。与对照组比较,ASA组成骨相关基因ALP、OPN和RUNX2相对mRNA表达水平显著升高,差异有统计学意义（P＜0.05）;与ASA组比较,wortmannin组成骨相关基因ALP、OPN和RUNX2相对mRNA表达水平均显著降低,差异有统计学意义（P＜0.05）。与对照组比较,ASA组PI3K、p-AKT蛋白表达水平显著升高,差异有统计学意义（P＜0.05）;与ASA组比较,wortmannin组PI3K、p-AKT蛋白表达水平显著降低,差异均有统计学意义（P＜0.05）。结论：ASA能促进骨质疏松模型rBMSCs增殖,增强ALP活性,增强ALP、OPN和RUNX2的表达,而PI3K通路抑制剂wortmannin降低了这些成骨作用,并降低了ASA诱导的PI3K、p-AKT水平,表明ASA通过PI3K/AKT信号通路促进骨质疏松模型rBMSCs成骨分化。     

紫罗酮和麦角固醇对酵母生长及产辅酶Q10的影响

研究了β-紫罗酮和麦角固醇对酵母生长及产辅酶Q₁₀的影响。研究发现,β-紫罗酮能促进菌体积累辅酶Q₁₀,当培养基中β-紫罗酮的添加量为0.208×10^-3mol/L时,菌体中CoQ₁₀的含量提高了28.3%;少量麦角固醇能促进菌体产辅酶Q₁₀,当麦角固醇的添加量为0.15×10^-4mol/L时,菌体中CoQ₁₀的含量提高了31.8%,而增加麦角固醇的添加     

用基因克隆大肠杆菌发光体系测定长链脂肪醛

利用基因克隆大肠杆菌发光体系分别测试了五种长链脂肪醛和脂肪酸。结果表明:可在几分钟内测出癸醛,正辛醛和十二烷醛的极限浓度分别为1×10^-14mol/L、1×10^-12mol/L和1×10^-9mol/L,是一种灵敏、快速的测试方法。     

Efficient release of ferulic acid from sweet potato (<Emphasis Type="Italic">Ipomoea batatas</Emphasis>) stems by chemical hydrolysis

An efficient method for release of ferulic acid from sweet potato stems was developed. Ferulic acid along with phenolic compounds were released from stems by acid and alkaline treatments. The base hydrolysis with 0.1 N NaOH yielded the highest quantity of total extracts (471.1 mg/g). The stems released more phenolic compounds when 0.0125∼0.025 N NaOH was employed. Where as ferulic acid release was maximal with 0.05 N H₂SO₄ (0.32 mg/g). Ferulic acid was separated from phenolics by column chromatography. Among the elution solvents, ethyl acetate fractions (80%) contained ferulic acid. Ethyl acetate eluants were further fractionated with n-hexane/ethyl acetate/formic acid (100/50/0.5, v/v/v). All fractions showed ferulic acid and phenolic compounds. Fraction V among them was ascribed to ferulic acid with an yield of 5.41 mg/g of dry sweet potato tissue.     

Redox Fluctuations Frame Microbial Community Impacts on N-cycling Rates in a Humid Tropical Forest Soil

Fluctuating soil redox regimes may facilitate the co-occurrence of microbial nitrogen transformations with significantly different sensitivities to soil oxygen availability. In an upland humid tropical forest, we explored the impact of fluctuating redox regimes on gross nitrogen cycling rates and microbial community composition. Our results suggest that the rapidly fluctuating redox conditions that characterize these upland soils allow anoxic and oxic N processing to co-occur. Gross nitrogen mineralization was insensitive to soil redox fluctuations. In contrast, nitrifiers in this soil were directly affected by low redox periods, yet retained some activity even after 3–6 weeks of anoxia. Dissimilatory nitrate reduction to ammonium (DNRA) was less sensitive to oxygen exposure than expected, indicating that the organisms mediating this reductive process were also tolerant of unfavorable (oxic) conditions. Denitrification was a stronger sink for NO₃⁻ in consistently anoxic soils than in variable redox soils. Microbial biomass and community composition were maintained with redox fluctuation, but biomass decreased and composition changed under static oxic and anoxic soil regimes. Bacterial community structure was significantly correlated with rates of nitrification, denitrification and DNRA, suggesting that redox-control of soil microbial community structure was an important determinant of soil N-cycling rates. Specific nitrogen cycling functional groups in this environment (such as nitrifiers, DNRA organisms, and denitrifiers) appear to have adapted to nutrient resources that are spatially and temporally variable. In soils where oxygen is frequently depleted and re-supplied, characteristics of microbial tolerance and resilience can frame N cycling patterns.     

Treatment of domestic and agricultural wastewater by reed bed systems

The purification capacity and seasonal variability of two newly created reed bed systems was monitored over 1 year. In one of the systems treating domestic wastewater, the reduction in the concentrations of chemical oxygen demand (COD), total N, total P and fecal coliform bacteria (FC) ranged from 80 to 99%. In the second system, treating a mixture of domestic and agricultural wastewater produced by a cheese dairy, treatment efficiency ranged between 13 and 99%. The removal rates did not show any seasonal pattern for domestic wastewater, in contrast to the mixture of domestic and agricultural wastewater with increased removal rates in the summer. Bacteria which are involved in N metabolism was estimated by the most probable number-test (MPN). In both reed bed systems the MPN of proteolytic bacteria, ammonifiers, nitrifiers and denitrifiers/g DW of gravel substrate were of the orders of magnitude of 10⁴–10⁶, 10⁵–10⁷, 10¹–10⁵ and 0–10³, respectively. On the basis of the microbial assemblage there is a need to improve the conditions for both nitrification and denitrification to enhance the efficiency of N removal.     

连作障碍与根际微生态研究Ⅲ.土壤酚酸物质及其生物学效应

以黑龙江省大豆重茬 5年与正茬土壤和根系为主要研究对象 ,采用高效液相色谱法 ,研究土壤和根系浸提液中的酚酸物质的含量及其生物学效应 .结果表明 ,重茬土壤中对羟基苯甲酸和香草酸的含量 (1mol·L-1NaOH提取 )大于正茬土壤 ,且差异达到极显著水平 ,香草醛含量差异不显著 ;重茬大豆根系水提液中对羟基苯甲酸、香草酸、阿魏酸、香草醛、香豆素含量均高于正茬 .大豆连作条件下土壤多酚氧化酶活性高于正茬土壤 .重茬大豆根系水提液及在水培条件下外加对羟基苯甲酸对大豆幼苗生长发育有一定的抑制作用 ;酚酸物质加入土壤 1周后 ,对羟基苯甲酸、香草酸、香草醛、阿魏酸、苯甲酸、香豆素残留率分别为 10 .4%、15 .3 %、4.1%、2 .3 %、5 .0 %、17.5 % ;且外加酚酸浓度与土壤中真菌数量呈极显著指数相关 .     

Relative Rates of Nitric Oxide and Nitrous Oxide Production by Nitrifiers, Denitrifiers, and Nitrate Respirers

Biogenic emissions of nitric and nitrous oxides have important impacts on the photochemistry and chemistry of the atmosphere. Although biogenic production appears to be the overwhelming source of N₂O, the magnitude of the biogenic emission of NO is very uncertain. In soils, possible sources of NO and N₂O include nitrification by autotrophic and heterotrophic nitrifiers, denitrification by nitrifiers and denitrifiers, nitrate respiration by fermenters, and chemodenitrification. The availability of oxygen determines to a large extent the relative activities of these various groups of organisms. To better understand this influence, we investigated the effect of the partial pressure of oxygen (pO₂) on the production of NO and N₂O by a wide variety of common soil nitrifying, denitrifying, and nitrate-respiring bacteria under laboratory conditions. The production of NO per cell was highest by autotrophic nitrifiers and was independent of pO₂ in the range tested (0.5 to 10%), whereas N₂O production was inversely proportional to pO₂. Nitrous oxide production was highest in the denitrifier Pseudomonas fluorescens, but only under anaerobic conditions. The molar ratio of NO/N₂O produced was usually greater than unity for nitrifiers and much less than unity for denitrifiers. Chemodenitrification was the major source of both the NO and N₂O produced by the nitrate respirer Serratia marcescens. Chemodenitrification was also a possible source of NO and N₂O in nitrifier cultures but only when high concentrations of nitrite had accumulated or were added to the medium. Although most of the denitrifiers produced NO and N₂O only under anaerobic conditions, chemostat cultures of Alcaligenes faecalis continued to emit these gases even when the cultures were sparged with air. Based upon these results, we predict that aerobic soils are primary sources of NO and that N₂O is produced only when there is sufficient soil moisture to provide the anaerobic microsites necessary for denitrification by either denitrifiers or nitrifiers.     

Characterization of N<Subscript>2</Subscript>O emissions and associated microbial communities from the ant mounds in soils of a humid tropical rainforest

Tropical rainforest soils harbor a considerable diversity of soil fauna that contributes to emissions of N₂O. Despite their ecological dominance, there is limited information available about the contribution of epigeal ant mounds to N₂O emissions in these tropical soils. This study aimed to determine whether ant mounds contribute to local soil N emissions in the tropical humid rainforest. N₂O emission was determined in vitro from individual live ants, ant-processed mound soils, and surrounding reference soils for two trophically distinct and abundant ant species: the leaf-cutting Atta mexicana and omnivorous Solenopsis geminata. The abundance of total bacteria, nitrifiers (AOA and AOB), and denitrifiers (nirK, nirS, and nosZ) was estimated in these soils using quantitative PCR, and their respective mineral N contents determined. There was negligible N₂O emission detected from live ant individuals. However, the mound soils of both species emitted significantly greater (3-fold) amount of N₂O than their respective surrounding reference soils. This emission increased significantly up to 6-fold in the presence of acetylene, indicating that, in addition to N₂O, dinitrogen (N₂) is also produced from these mound soils at an equivalent rate (N₂O/N₂?=?0.57). Functional gene abundance (nitrifiers and denitrifiers) and mineral N pools (ammonium and nitrate) were significantly greater in mound soils than in their respective reference soils. Furthermore, in the light of the measured parameters and their correlation trends, nitrification and denitrification appeared to represent the major N₂O-producing microbial processes in ant mound soils. The ant mounds were estimated to contribute from 0.1 to 3.7% of the total N₂O emissions of tropical rainforest soils.     

Physicochemical and biological processes affecting the recovery of exogenously applied ferulic acid from tropical forest soils

Ferulic acid (4-hydroxy-3-methoxycinnamic acid) is found in both plants and soils, and some evidence suggests its involvement in biochemical interactions between plants (allelopathy) and other organisms living in the soil. Knowledge of the processes affecting the concentrations of such potential allelochemicals in soil is essential if we are to understand their roles in the soil environment. It was the intent of this study to address the effects that soil physicochemical and biological processes have on the recovery of exogenously applied ferulic acid from tropical forest soils. Soil extractants used in this study are thought to recover potentially bioavailable concentrations of applied ferulic acid. Water and sodium acetate extractions of soil (immediately and after one and two days) were employed in the recovery of ferulic acid (added at a rate of 5.15 mmoles kg^–1) from steam-sterilized and non-sterilized forest soil materials. Sterilization of soil was used to isolate physicochemical effects from microbial effects on ferulic acid. Results indicate some sterilization treatment effects on the immediate recovery of ferulic acid. Physicochemical and biological processes of soils decreased the recovery of ferulic acid. The immediate recovery of ferulic acid from non-sterile soils is inversely related to the % organic carbon present in the soils. Certain soils have the ability to trap ferulic acid molecules for subsequent release into the soil-solution phase. Furthermore, results suggest that microbial degradation of ferulic acid may only occur in the solution (bulk) phase; ferulic acid molecules thought to be bound to soil surfaces appear to be protected from degradation.Use of trade names in this publication does not imply endorsement by the Organization for Tropical Studies, North Carolina State University or the Savannah River Ecology Laboratory of the products named nor criticism of similar ones not mentioned.     

宏基因组技术研究泥岩母质发育的三种不同pH紫色土硝化微生物群落演变规律

【目的】揭示典型农田旱地紫色土硝化微生物的群落组成及其对pH的响应规律。【方法】针对同一母质发育但pH差异显著的3种紫色土,利用宏基因组技术深度测序研究土壤中硝化微生物丰度和群落,包括氨氧化古菌(ammonia-oxidizing archaea,AOA),氨氧化细菌(ammonia-oxidizing bacteria,AOB),亚硝酸盐氧化细菌(nitrite-oxidizingbacteria,NOB)和全程氨氧化细菌(completeammoniaoxidizer,Comammox)。【结果】土壤中硝化微生物的丰度占总微生物的2.130%–6.082%。3种紫色土中AOA、AOB和NOB的相对丰度有显著差异:酸性紫色土中AOA的相对丰度显著大于碱性紫色土,而AOB则相反;NOB的相对丰度在中性紫色土中最高。所有土样中均发现了1种全程氨氧化细菌Candidatus Nitrospira inopinata (Ca. N. inopinata),其在中性紫色土中相对丰度最高,占总微生物的0.203%。3种不同pH紫色土中AOA均以Nitrososphaera为主,NOB均以Nitrospira为主;酸性紫色土中AOB以Nitroscoccus为主,而中性和石灰性紫色土中则以Nitrosospira为主。Pearson相关性分析发现,土壤pH和铵态氮是影响硝化微生物丰度最大的两个因子。【结论】Comammox存在于3种不同pH紫色土中,且偏好中性环境;AOA、AOB和NOB群落结构和相对丰度都存在显著差异,结合相关性分析发现土壤pH和铵态氮是导致差异最重要的两个因子。     

Quantitative analysis of phenolics in selected crop species and biological activity of these compounds evaluated by sensitivity of Echinochloa crus-galli

The purpose of this study was to determine the content of selected phenolic compounds in white mustard, buckwheat, spring barley, oat and rye grown under field conditions. Moreover, the allelopathic efficiency of these compounds was evaluated by sensitivity of Echinochloa crus-galli. The aromatic acids: trans-cinnamic, salicylic, ferulic, chlorogenic, p-hydroxybenzoic, protocatechuic, p-coumaric and vanillic were separated from crop plants by TLC and determined spectrophotometrically. Differences in concentrations of analysed compounds were observed for most of the examined plant species. The highest concentration was noticed for cinnamic acid and ranged from 360 μg·g⁻¹ DW in rye to 2770 μg·g⁻¹ DW in spring barley. The relatively high concentration was noticed for ferulic acid (from 73.8 μg·g⁻¹ DW in buckwheat to 1046 μg·g⁻¹ DW in spring barley) and p-coumaric acid (from 50 μg·g⁻¹ DW in oat to 1499 μg·g⁻¹ DW in buckwheat). The observed differences in the phenolics content between two successive vegetation seasons can reflect the effect of abiotic and biotic environmental factors on the phenolics level in studied plants. In the greenhouse experiment the effect of particular compounds on the growth of Echinochloa crus-galli was also studied. It has been found that the examined phenolics, and especially trans-cinnamic acid and mixture of phenolic compounds, significantly inhibit the growth of Echinochloa crus-galli. The obtained results may contribute to the explanation of the biological activity of some phenolic compounds.     

氨基酸添加对亚热带森林红壤氮素转化的影响

为探究氨基酸氮形态对亚热带土壤氮素含量及转化的影响,选择建瓯市万木林保护区的山地红壤为对象,采用室内培养实验法,通过设计60%和90%WHC两种土壤含水量并添加不同性质氨基酸,测定了土壤中铵态氮、硝态氮、可溶性有机氮的含量和氧化亚氮的释放量,分析了可溶性有机碳、土壤p H值的大小变化及其与氮素的相互关系。结果表明:与对照处理相比,氨基酸添加显著增加了土壤NH_4~+-N含量并使土壤p H值升高,且在一定程度上解除了高含水量(90%WHC)对NH_4~+-N产生的抑制,其中甲硫氨基酸的效果最为明显。酸性、碱性、中性氨基酸对土壤NO_3~--N含量和N_2O释放影响不显著,但甲硫氨基酸可显著抑制土壤硝化从而导致NH_4~+-N的积累,并在培养前期抑制土壤N_2O产生而在培养后期促进N_2O释放,总体上促进N_2O释放。60%WHC的氨基酸添加处理较90%WHC条件下降低土壤可溶性有机氮的幅度更大。氨基酸对土壤氮素转化的影响与带电性关系较小,而可能与其分解产物密切相关。可见,不同性质氨基酸处理对森林土壤氮素含量及转化存在不同程度的影响,且甲硫氨基酸对土壤氮素转化的影响机理值得深入研究。