不同参数超临界CO2处理对乳酸菌活性的影响

为了研究超临界CO2作为非水相介质在生化反应工程中的作用,有必要考察超临界CO2处理对微生物活性的影响.本文以乳酸杆菌为试验菌种,进行了该菌在不同参数超临界CO2处理对菌体生长曲线、耐渗透压能力、耐酸能力、抑菌能力、降解胆固醇能力等活性指标影响的研究.结果表明:当提高超临界CO2压强或延长超临界CO2处理时间,乳酸杆菌的活性指标会发生如下变化:生长曲线的最大菌体浓度降低,但菌体的生长速率差异不大;菌体的耐渗透能力、耐酸能力降低;所得的抑菌圈比较明显,但抑菌圈直径减小;平均胆固醇降解率降低,而且长时间处理对降解效果的影响比高压强处理的明显.因此,在工程应用中需要研究一定的弥补措施.     

超临界CO2杀灭大肠杆菌过程中菌体蛋白变化的研究

通过SDS-聚丙烯酰胺凝胶电泳,结合超临界CO₂对大肠杆菌的杀菌曲线,研究超临界压力、温度和处理时间对大肠杆菌菌体蛋白的影响。结果表明：超临界CO₂在杀灭大肠杆菌过程中,可显著降低菌体碱溶性（pH8.0）蛋白的溶解性,但对菌体总蛋白含量和种类没有影响;37 ℃下超临界CO2处理大肠杆菌30 min,压力为10MPa时,大肠杆菌存活率为2.8%,菌体碱溶性蛋白的溶解性显著降低,但当压力增加到50MPa时,大肠杆菌存活率和碱溶性蛋白溶解性变化不明显;超临界温度和处理时间对菌体碱溶性蛋白溶解性的影响与大肠杆菌在超临界CO₂中的存活趋势基本一致可,随处理时间的延长和温度的增加大肠杆菌存活率逐渐降低到0,碱溶性蛋白溶解性逐渐降低,直至部分蛋白带消失,但菌体总蛋白含量和种类并没有明显变化;升高温度比增加压力更能显著地导致菌体碱溶性蛋白变性,溶解性下降。     

用超临界CO2脱除绿茶浓缩液中咖啡碱的工艺研究

对绿茶浓缩液中咖啡碱的超临界CO₂萃取工艺进行了研究，通过4因素正交试验探讨了浓缩液的浓度、操作压强、操作温度、萃取时间对咖啡碱脱除率的影响。结果表明，超临界CO₂萃取技术可以有效地脱除绿茶浓缩液中大部分的咖啡碱，在此基础上完成了用超临界CO₂脱除绿茶浓缩液中咖啡碱的连续作业试验，从而获得了加工脱咖啡碱绿茶浓缩液或速溶绿茶的新工艺。     

乙醇溶剂与超临界CO2相结合提取高纯度卵黄磷脂的研究

采用乙醇溶剂首先提取蛋黄粉中的卵黄油，然后用超临界CO₂萃取方法脱除卵黄油中的中性脂肪，获得高纯度的卵黄磷脂。考察了工艺参数对提取效果的影响。试验表明：在乙醇溶剂提取卵黄油阶段，乙醇浓度是影响卵黄油提取率的最主要因素，温度是影响卵黄磷脂提取率的最主要因素；在超临界CO₂萃取阶段，磷脂的溶解度随萃取温度的升高而降低，中性脂质在55℃时溶解度最大。采用此工艺，卵黄磷脂得率为17.66%，纯度94.41%，且不含胆固醇。     

超声强化超临界CO2萃取人参皂苷的研究

为了探讨超声波对超临界CO₂萃取(SCE)的影响，考察了在不同萃取温度、萃取压力、萃取时间和流体流量下，有、无超声时超临界CO₂萃取人参皂苷的萃取率。试验结果发现，超声强化超临界CO₂萃取(USCE)的合适萃取温度比没加超声(SCE)时的低10℃；在各自合适的萃取压力下，USCE的皂苷萃取率是SCE的1.64倍；CO₂流体的流量大更有利于USCE。在SCE中，超声的加入能明显提高产物的萃取率和生产效率，降低生产能耗和节     

超临界CO2连续浓缩鱼油EPA和DHA的研究

为了克服鱼油有效组分超临界CO₂间歇萃取方法的缺点，设计建造了超临界CO₂在内径14 mm、填料高1.8 m的填料塔中连续萃取浓缩鱼油有效组分的流程。根据单因素试验的结果，对工艺参数进行优化。设计了4因素3水平并考虑部分交互作用的正交试验方案，以综合指标进行评价，得到了优化工艺参数为：填料塔压为12.5 MPa；CO₂流量为5L/min；鱼油进料流量为0.8 mL/min；塔的温度分布为40～85℃。经方差分析得知，温度分布的影响对综合指标高度显著，鱼油进料流量对综合指标的影响显著，试验范围内的压力、CO₂流量、压力和温度分布交互作用、温度分布和CO₂流量交互作用以及压力和CO₂流量交互作用对综合指标没有显著影响。     

环境因素对自然气调下双孢蘑菇呼吸速率影响的初步研究

研究了温度、容器内顶隙气体体积与双孢蘑菇体积比、O₂浓度、CO₂浓度及处理时间t对双孢蘑菇呼吸速率的影响，并采用多因素方差分析、重回归分析法，确定了双孢蘑菇呼吸速率的显著性影响因素，结果表明：温度对双孢蘑菇呼吸耗氧率R_O2、二氧化碳生成率R_CO2、呼吸商RQ的影响比体积比的影响更显著；25、18和4℃时，O₂浓度、CO₂浓度及时间t 3因素中，时间t对R_CO2的影响最大，而12℃时，CO₂浓度对R_CO2的影响最大；12℃时，随着体积比的增大，CO₂浓度、时间t的影响作用减弱，O₂浓度作用增强。     

空间电场对植物吸收CO2和生长速度的影响

为研究空间电场对植物吸收CO₂和生长速度的影响，首先采用同位素示踪法，分析了不同空间电场调控营养液栽培的番茄秧吸收CO₂气体和HCO^-₃阴离子的能力，证实了 ¹⁴C—HCO^-₃是一种受控于空间电场变化的阴离子，且空间电场强度的变化方向调控着 ¹⁴C—HCO^-₃阴离子流的流动方向。在此基础上以蕹菜(空心菜)为试验材料，采取空间电场与增施CO₂浓度的参数组合，做对比生长试验，通过红外线CO₂分析法揭示了空间电场的极性对植物吸收CO₂的速度有显著影响，且正向空间电场能显著促进植物对CO₂的吸收，并得到正向空间电场与足量的CO₂浓度相配合能大幅度提高温室蔬菜生长速度，使作物产量倍增的结论，为建立空间电场促进植物生长技术提供理论依据。     

缺氮培养大豆Bragg结瘤突变系对CO2倍增的反应

研究了在缺氮条件下，CO₂倍增对大豆（GtycinemaxL.）Bragg及其等基因突变体超结瘤大豆nts382和不结瘤大豆Nod49生长和固氮的影响。结果表明在缺氮条件下CO₂倍增明显提高大生物量和根系结涵量，但对固氮酶活性的影响则随幼苗的生长而异。播种后25天取样结果显示CO₂倍增条件下，Bragg和nts382的固氮比活性和单株固氮活性都显著提高，而其后3天取样的结果没有表现出增加趋势，固氮比活性在nts382反而明显降低。两种CO₂浓度条件下，nts382单株固氮活性高于Bragg，但固氮比活性低于后者。两次测定结果的差异说明植物对CO₂倍增的反应具有很强的时效性;同时表明，CO₂倍增对植物生长和固氮的促进作用不能长期维持。这可能与生物固氮过程本身的复杂性有关。根据本研究结果推测，在未来全球环境变化、CO₂倍增条件下，共生固氮植物可能在生态系统氮素平衡中起到更为重要的作用;并有可能通过育种技术改良固氮农作物，提高农作物产量。     

水培条件下CO2与NH+4/NO-3配比对番茄幼苗生育的影响

升高CO₂浓度能够促进作物的光合作用，提高作物的生物量和产量，但关于CO₂与NH⁺₄/NO^-₃比及其交互作用对作物影响的研究较少，为探索番茄幼苗生长发育对CO₂浓度升高的响应是否对NH⁺₄/NO^-₃配比有较强的依赖关系，本试验在营养液栽培条件下，以番茄(Lycopersicun esculentum Mill)为试材，研究正常大气CO₂浓度(360 μL/L)和倍增CO₂浓度(720 μL/L)与不同NH⁺₄/NO^-₃配比的交互作用对番茄幼苗生长的影响。结果表明：CO₂浓度升高提高了低NH⁺₄/NO^-₃比例处理中番茄叶片的光合速率和水分利用率，提高幅度随NH⁺₄/NO^-₃比例的降低而增强，光合速率增强最大达55%。在同一CO₂浓度处理下净光合速率与水分利用率均随NH⁺₄/NO^-₃比例的增加而显著降低。这说明CO₂浓度升高对番茄幼苗生长发育的促进作用随NH⁺₄/NO^-₃比例的降低而提高，但并没有减弱全NH⁺₄-N处理中番茄幼苗的受毒害作用。综上所述，CO₂浓度升高能提高植物生产的节水能力和水分生产力；水培条件下，NO^-₃-N是最适合番茄幼苗生长发育的氮源，其它NH⁺₄/NO^-₃比例对番茄幼苗的生长发育有一定的抑制作用，仅以NH⁺₄-N作氮源则番茄幼苗很难生长。     

Changes in the fungal-to-bacterial respiratory ratio and microbial biomass in agriculturally managed soils under free-air CO2 enrichment (FACE) - A six-year survey of a field study

In soil ecology, microbial parameters have been identified as sensitive indicators of changes in the soil environment. The Braunschweig FACE project provided the opportunity to study the effects of elevated CO₂ (550 μmol mol⁻¹) as compared to ambient CO₂ (370 μmol mol⁻¹) on total microbial biomass (C_mic), C_mic-to-C_org ratio and the fungal-to-bacterial respiratory ratio together with total C_org, N_t, C:N ratio and pH over a six-year period. Field management followed a typical crop rotation system of this region with either a crop-related full nitrogen supply (N100) or 50% reduced N supply (N50). The soil microbial parameters responded to the elevated CO₂ treatment in varying intensities and time spans. The fungal-to-bacterial respiratory ratio was the most sensitive parameter in responding to an elevated CO₂ treatment with highly significant differences to ambient CO₂-treated control plots in the third year of CO₂ fumigation. After six years bacterial respiratory activity had increased in ascending order to 34% in FACE-treated plots (N50 and N100) as compared to control plots. Soil microbial biomass (C_mic) responded more slowly to the FACE treatment with highly significant increases of >12% after the fourth year of CO₂ fumigation. The C_mic-to-C_org ratio responded very late in the last two years of the CO₂ treatment with a significant increase of >7.0% only in the N100 variant. Total C_org and N_t were slightly but significantly increased under FACE around 10.0% with ascending tendency over time starting with the second year of CO₂ treatment. No significant FACE effects could be recorded for the C:N ratio or pH.These results suggest that under FACE treatment changes in the soil microbial community will occur. In our study the fungal-to-bacterial respiratory ratio was superior to total C_mic as microbial bioindicators in reflecting changes in the soil organic matter composition.     

压力、温度对穿心莲内酯超临界CO2萃取-结晶的影响

以穿心莲浸膏为原料，进行了穿心莲内酯的超临界CO₂萃取结晶分离纯化。考察了单因素参数压力、温度对穿心莲内酯纯度、结晶量等的影响。结果表明：超临界CO₂萃取结晶穿心莲内酯的纯度在结晶板上呈梯度分布；在25 MPa以下，压力升高，结晶板上部晶体纯度升高，而结晶量先增后减；在结晶板下部穿心莲内酯的纯度和结晶量都是先升高后降低；温度在一定范围内能提高晶体纯度，且有利于缩短萃取结晶时间。     

Microbial activity and bacterial composition of H2-treated soils with net CO2 fixation

The effects of H₂ gas treatment of an agricultural soil cultivated previously with a mixture of clover (Trifolium pratense) and alfalfa (Medicago sativa) on CO₂ dynamics and microbial activity and composition were analyzed. The H₂ emission rate of 250 nmol H₂ g⁻¹ soil h⁻¹ was similar to the upper limit of estimated H₂ amounts emitted from N₂ fixing nodules into the surrounding soil ([Dong, Z., Layzell, D.B., 2001. H₂ oxidation, O₂ uptake and CO₂ fixation in hydrogen treated soil. Plant and Soil 229, 1-12.]). After 1 week of H₂ supply to soil samples simultaneously with H₂ uptake net CO₂ production declined continuously and this finally led to a net CO₂ fixation rate in the H₂-treated soil of 8 nmol CO₂ g⁻¹ soil h⁻¹. The time course of H₂ uptake and CO₂ fixation in the soils corresponded with an increase in microbial activity and biomass of the H₂-treated soil determined by microcalorimetric measurements, fluorescence in situ hybridization analysis (FISH) and DNA staining (DAPI). Shifts in the bacterial community structure caused by the supply of H₂ were recorded. While the H₂ treatment stimulated β-and γ-subclasses of Proteobacteria, it had no significant effect on α-Proteobacteria. In addition, FISH-detectable bacteria of the Cytophaga-Flavobacterium-Bacteroides phylum increased in numbers.     

Microbial biomass and activity indices after organic substrate addition to a selenium-contaminated soil

High concentrations of Se in soil might have negative effects on microorganisms. For this reason, the effect of organic substrate addition (glucose + maize straw) on Se volatilisation in relation to changes in microbial biomass and activity indices was investigated using an artificially Se-contaminated soil. Microbial biomass N was reduced on average by more than 50% after substrate addition, but adenylate energy charge (AEC) and metabolic quotient qCO₂ were both increased. The Se content decreased by nearly 30% only with the addition of the organic substrate at 25°C. No significant Se loss occurred without substrate at 25°C or with substrate at 5°C. In the two treatments with substrate addition, the substrate-derived CO₂ evolution was about 30% lower with Se addition than without. In contrast, Se had no effect on any of the other soil microbial indices analysed, i.e. microbial biomass C, microbial biomass N, adenosine triphosphate (ATP), AEC, ATP-to-microbial biomass C, and qCO₂.     

模拟干旱和盐碱胁迫对碱蓬、盐地碱蓬种子萌发的影响

为研究干旱和盐碱胁迫对碱蓬(Suaeda glauca)、盐地碱蓬(Suaeda salsa)种子萌发的影响,比较碱蓬和盐地碱蓬逆境生理特性的异同,本研究利用PEG6000、NaCl和Na_2CO_3分别模拟干旱、盐和碱胁迫,配制相同渗透势的PEG6000、NaCl、Na_2CO_3处理液,以蒸馏水处理为对照,对碱蓬、盐地碱蓬种子的萌发与胚的生长进行比较研究。结果表明:1)低渗处理(-0.46 MPa)对碱蓬、盐地碱蓬种子的萌发无显著影响;高渗处理(-1.38MPa、-1.84 MPa)抑制碱蓬、盐地碱蓬种子的萌发。2)当溶液渗透势相等时,NaCl处理下碱蓬种子的萌发率显著大于PEG、Na_2CO_3处理;而等渗PEG、NaCl、Na_2CO_3处理对盐地碱蓬种子萌发率的影响无显著差异。3)PEG、NaCl、Na_2CO_3处理组碱蓬、盐地碱蓬种子的最终萌发率与对照无显著差异。4)在幼苗形成阶段,PEG、Na_2CO_3处理对碱蓬、盐地碱蓬胚的抑制作用显著大于等渗NaCl处理。5)碱蓬、盐地碱蓬胚的生长对NaCl、Na_2CO_3胁迫的响应存在差异。-0.92 MPa NaCl处理抑制碱蓬胚的生长,却对盐地碱蓬产生促进作用;-0.46 MPa Na_2CO_3处理对碱蓬胚的抑制作用小于盐地碱蓬。综合分析表明:碱蓬、盐地碱蓬均具有很强的抗盐性。在种子萌发阶段,碱蓬种子的抗旱、抗碱能力低于盐地碱蓬;在幼苗形成阶段,碱蓬胚的抗盐性小于盐地碱蓬,但对轻度碱胁迫的抗性高于盐地碱蓬。     

Interactions of NaCl and Na2SO4 on soil organic C mineralization after addition of maize straws

NaCl and Na₂SO₄ often dominate salt compositions in saline soils. While either salt alone affects soil organic matter mineralization, their interactions on soil organic matter dynamics are unknown. This study aimed to investigate interactive effects of the two salts on organic C mineralization and microbial biomass C of the saline soils after addition of maize straws. Both NaCl and Na₂SO₄ were applied at 0, 40 and 80 mmol Na kg⁻¹ soil and the incubation was undertaken at soil water content of 15% and 20% (w/w) in dark at 28.5 °C for 70 days. The study found significant interactions of NaCl and Na₂SO₄ on CO₂-C evolution during the early incubation periods—a suppressing effect at days 1-2 but a stimulating effect at days 6-8 and 17-20, and thereafter the salt interactions were influenced by water content. The interactions of water content with NaCl or Na₂SO₄ on CO₂-C evolution were observed through the incubation periods except days 1-2, showing that the salt effects were dependent on water content. Total CO₂ evolution over the 70-day-long incubation decreased with increasing NaCl but increased with increasing Na₂SO₄ compared to the nil-salted treatment. Salt interactions on soil microbial biomass C were observed at days 7, 21, but not at day 49. Microbial biomass C increased at day 7 in the soils treated with either NaCl or Na₂SO₄ but decreased where the two salts were combined. At day 21, microbial biomass C increased with NaCl but decreased with Na₂SO₄ regardless whether the counterpart salt was added. The results suggest that soil organic C mineralization can be affected by the interactions of NaCl and Na₂SO₄, possibly through the salt-induced changes in microbial biomass community structure.     

Short and long-term effects of elevated CO2 on Lolium perenne rhizodeposition and its consequences on soil organic matter turnover and plant N yield

It is still unclear whether elevated CO₂ increases plant root exudation and consequently affects the soil microbial biomass. The effects of elevated CO₂ on the fate of the C and nitrogen (N) contained in old soil organic matter pools is also unclear. In this study the short and long-term effects of elevated CO₂ on C and N pools and fluxes were assessed by growing isolated plants of ryegrass (Lolium perenne) in glasshouses at elevated and ambient atmospheric CO₂ and using soil from the New Zealand FACE site that had >4 years exposure to CO₂ enrichment. Using ¹⁴CO₂ pulse labelling, the effects of elevated CO₂ on C allocation within the plant-soil system were studied. Under elevated CO₂ more root derived C was found in the soil and in the microbial biomass 48 h after labelling. The increased availability of substrate significantly stimulated soil microbial growth and acted as priming effect, enhancing native soil organic matter decomposition regardless of the mineral N supply. Despite indications of faster N cycling in soil under elevated CO₂, N availability to plants stayed unchanged. Soil previously exposed to elevated CO₂ exhibited a higher N cycling rate but again there was no effect on plant N uptake. With respect to the difficulties of extrapolating glasshouse experiment results to the field, we concluded that the accumulation of coarse organic matter observed in the field under elevated CO₂ was probably not created by an imbalance between C and N but was likely to be due to more complex phenomena involving soil mesofauna and/or other nutrients limitations.     

Climate change goes underground: effects of elevated atmospheric CO<Subscript>2</Subscript> on microbial community structure and activities in the rhizosphere

General concern about climate change has led to growing interest in the responses of terrestrial ecosystems to elevated concentrations of CO₂ in the atmosphere. Experimentation during the last two to three decades using a large variety of approaches has provided sufficient information to conclude that enrichment of atmospheric CO₂ may have severe impact on terrestrial ecosystems. This impact is mainly due to the changes in the organic C dynamics as a result of the effects of elevated CO₂ on the primary source of organic C in soil, i.e., plant photosynthesis. As the majority of life in soil is heterotrophic and dependent on the input of plant-derived organic C, the activity and functioning of soil organisms will greatly be influenced by changes in the atmospheric CO₂ concentration. In this review, we examine the current state of the art with respect to effects of elevated atmospheric CO₂ on soil microbial communities, with a focus on microbial community structure. On the basis of the existing information, we conclude that the main effects of elevated atmospheric CO₂ on soil microbiota occur via plant metabolism and root secretion, especially in C3 plants, thereby directly affecting the mycorrhizal, bacterial, and fungal communities in the close vicinity of the root. There is little or no direct effect on the microbial community of the bulk soil. In particular, we have explored the impact of these changes on rhizosphere interactions and ecosystem processes, including food web interactions.     

Assessment of 10 years of CO2 fumigation on soil microbial communities and function in a sweetgum plantation

Increased vegetative growth and soil carbon (C) storage under elevated carbon dioxide concentration ([CO₂]) has been demonstrated in a number of experiments. However, the ability of ecosystems, either above- or belowground, to maintain increased C storage relies on the response of soil processes, such as those that control nitrogen (N) mineralization, to climatic change. These soil processes are mediated by microbial communities whose activity and structure may also respond to increasing atmospheric [CO₂]. We took advantage of a long-term (ca 10 y) CO₂ enrichment experiment in a sweetgum plantation located in the southeastern United States to test the hypothesis that observed increases in root production in elevated relative to ambient CO₂ plots would alter microbial community structure, increase microbial activity, and increase soil nutrient cycling. We found that elevated [CO₂] had no detectable effect on microbial community structure using 16S rRNA gene clone libraries, on microbial activity measured with extracellular enzyme activity, or on potential soil N mineralization and nitrification rates. These results support findings at other forested Free Air [CO₂] Enrichment (FACE) sites.