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.     

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流体萃取杏仁油工艺研究

该研究以单因素试验和正交试验相结合的方法对苦杏仁脂肪油的超临界CO₂萃取工艺进行了研究。确定了超临界CO₂萃取杏仁油的最佳工艺为：萃取压力35 MPa、萃取温度50℃、CO₂流量24 L/ｈ、粒径60目、萃取时间2 h。各因素影响杏仁的得率的顺序为：粒径>时间>萃取压力>CO₂流量>萃取温度。最佳工艺验证试验的杏仁油的得率为52.98％。本研究的结果为下一步综合、无毒、高效地开发利用苦杏仁奠定了基础。     

超临界CO2萃取万寿菊花中叶黄素的研究

采用超临界CO₂萃取技术,研究了从万寿菊花中萃取叶黄素的工艺条件。对影响超临界CO₂萃取叶黄素的各种因素,包括分离参数、原料含水率、粉碎粒径，超临界萃取温度、压力、流速、时间等因素进行了考察,得到较佳的萃取工艺条件为:原料含水率10.92％，粒径40目，萃取温度60℃，压力30 MPa，CO₂流速15 L/h，分离釜Ⅰ温度40℃，压力6 MPa，分离釜Ⅱ温度20℃，时间为6 h。     

超临界CO2萃取大蒜精油及油树脂的研究

研究了大蒜精油及油树脂的超临界CO₂提取工艺，探讨了粒度，萃取及分离的温度、压力和时间对各萃取率的影响，建立了萃取温度、压力与各萃取率的数学模型。确定了超临界CO₂同时提取大蒜精油及油树脂的优化工艺条件。     

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。     

响应曲面法建立超临界CO2萃取结晶穿心莲内酯工艺模型

以穿心莲内酯含量为30%的穿心莲浸膏为试验原料，采用响应曲面分析法(Response Surface Methodology，RSM)建立了超临界CO₂萃取结晶穿心莲内酯结晶率的二次多项数学模型，验证了数学模型的有效性，并探讨了萃取结晶压力、温度、时间对结晶率的作用规律。根据该模型进行了工艺参数的优选，以结晶率为指标，试验所得穿心莲内酯超临界CO₂萃取结晶优化工艺条件为：压力20.88 MPa，温度50.27℃，时间97.02 min，该条件下结晶率高达74.77%。     

穿心莲内酯超临界CO2重结晶工艺初探

采用单因素实验法探讨超临界CO₂重结晶压力、温度、时间对穿心莲内酯的纯度和结晶率的影响，并借助扫描电镜进行晶体形貌考察，利用高效液相色谱仪进行纯度检测。结果表明，采用超临界CO₂重结晶技术得到的穿心莲内酯晶体形貌更加细小，并呈絮状分布在结晶板上；选择较佳纯化工艺参数为重结晶压力14 MPa，温度55℃，时间60 min，CO₂流量20 L/min时，得到的穿心莲内酯纯度达90%以上，结晶率超过45%。     

柚子花芳香油超临界CO2萃取研究

介绍了新鲜柚子花中芳香性成分超临界CO₂萃取分离工艺和分析检测方法，重点探讨了压力、温度、时间对萃取率的影响。应用正交试验优化得出：影响萃取的主次因素依次为为萃取压力、萃取温度、萃取时间；较佳工艺参数为：压力18 MPa，温度50℃，时间90 min，流量25 L/min，得到超临界柚子花芳香油的萃取率高达2.7‰。应用气相色谱-质谱联用仪共鉴定出39个组分，占总芳香油的91.281%。通过对柚子花的深度加工研究，为开发高附加值的柚子花香精提供科学依据。     

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。     

Absorption and transport of Na and Cl in rice cultivars differing in their tolerance to salinity: An examination of the effects of ammonium and potassium salts

The absorption and transport of Na and Cl from 0.1 mM and 10 mM ²²Na labelled NaCl or ³⁶Cl labelled KCl were examined in 15 days old seedlings of 3 cultivars of rice differing in their tolerance to salinity. Furthermore, the effects of 10, 100 and 1000 ppm (N)₂S on their uptake were studied. It was found that in general, the salt‐tolerant cultivars BR and PNL‐1 absorbed more Na and translocated a lesser proportion of it to the shoot, compared to the salt‐sensitive IR‐8, from 0.1 mM NaCl. The presence of (N)₂S reduced the uptake of Na in all the cultivars. It was also found that the presence of 100 ppm K, KN or NNreduced Na absorption from 0.1 mM NaCl significantly in all the cultivars, and the translocation to shoot in BR‐ Chloride transport from 0.1 mM NaCl was reduced by (N)₂S in all the cultivars. The 3 cultivars differed significantly in the rates of absorption and transport of Na and Cl. The results indicate that PNL‐1 which is a cross of IR‐8 X BR, has inherited the salt tolerance trait from BR. Lower rates of Na translocation to the shoot can be used as an index of salt tolerance in rice.     

An examination of the total analysis of major elements in soil samples

Recently conventional chemical analyses were mostly replaced by instrumental analysis. Although results from both methods were examined in details after the samples had been solubilized or extracted by appropriate techniques, the solubilization method was considerably altered so as to be convenient for the following analysis. In atomic absorption spectrophotometry (AAS), for example, fusion technique was mostly inadequate because of the higher salts concentration in the obtained solution. The use of H₂SO₄ must also be avoided in acid digestion for SO₄ ^2- precipitates with Sr²⁺ or La³⁺ which must be added to eliminate interferences in the succeeding procedure. Therefore, it is essential to consider the whole scheme including sample treatments to evaluate the suitability of instrumental analysis. In this experiment, the suitability of the methods which have been employed in our laboratory was examined by analyzing 9 rock standards.     

我国酸性硫酸盐土壤中铁锰形态转化及迁移

酸性硫酸盐土壤酸性很强，有机质含量高，造成了这种土壤所特有的铁锰淋洗、转化和迁移规律。研究结果表明：在酸性硫酸盐土壤中全铁含量较低，一般在３５－５０ｇ／ｋｇ（以Ｆｅ２Ｏ３计），全锰含量也低，一般在０．２５－０．５５ｇ／ｋｇ（以ＭｎＯ计），一般滩涂中全铁大于６０ｇ／ｋｇ，全锰大于１ｇ／ｋｇ。酸性硫酸盐土壤中，铁的游离度较小，一般在３７－７０％，铁的活化度较大，一般在８－２０％，而滩涂中铁的游离度一般     

Denitrification potential in a grassland subsoil: effect of carbon substrates

We examined the potential of a subsoil to denitrify nitrate under optimal anaerobic conditions in a laboratory-based incubation when supplied with a range of C substrates of increasing recalcitrance. Both topsoil and its associated subsoil were supplied with nitrate and either glucose, starch or cellulose. Microbial respiration and the evolution of N₂O and N₂ were measured. The subsoil supported low amounts of microbial activity and responded only to the glucose treatment; with less than one-fifth of the N₂O production measured in the top soil. Overall, our findings demonstrated that the denitrification potential of this particular subsoil is relatively low and that only simple carbohydrates could be utilised readily by the resident microorganisms.     

Availability and extractability of soil manganese in a liming experiment

Abstract

The availability of soil Mn to corn in relation to extractability of soil Mn by EDTA, Mg(NO₃)₂, CH₃COONH₄, hydroquinone, H₃PO₄, and NH₄H₂PO₄ as affected by liming was evaluated under field conditions on a single soil type. EDTA, Mg(NO₃)₂ and CH₃COONH₄‐extractable Mn were related inversely to available Mn. No useful relationships were found between hydroquinone, H₃PO₄, and NH₄H₂PO₄‐extractable soil Mn and Mn uptake by sweet corn.     

CO2, CH4 and N2O fluxes of upland black spruce (Picea mariana) forest soils after forest fires of different intensity in interior Alaska

Abstract

Forest fires can change the greenhouse gase (GHG) flux of borea forest soils. We measured carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (N₂O) fluxes with different burn histories in black spruce (Picea mariana) stands in interior Alaska. The control forest (CF) burned in 1920; partially burned (PB) in 1999; and severely burned (SB1 and SB2) in 2004. The thickness of the organic layer was 22 ± 6 cm at CF, 28 ± 10 cm at PB, 12 ± 6 cm at SB1 and 4 ± 2 cm at SB2. The mean soil temperature during CO₂ flux measurement was 8.9 ± 3.1, 6.4 ± 2.1, 5.9 ± 3.4 and 5.0 ± 2.4°C at SB2, SB1, PB and CF, respectively, and differed significantly among the sites (P < 0.01). The mean CO₂ flux was highest at PB (128 ± 85 mg CO₂-C m^?2 h^?1) and lowest at SB1 (47 ± 19 mg CO₂-C m^?2 h^?1) (P < 0.01), and within each site it was positively correlated with soil temperature (P < 0.01). The CO₂ flux at SB2 was lower than that at CF when the soil temperature was high. We attributed the low CO₂ flux at SB1 and SB2 to low root respiration and organic matter decomposition rates due to the 2004 fire. The CH₄ uptake rate was highest at SB1 [–91 ± 21 μg CH₄-C m^?2 h^?1] (P < 0.01) and positively correlated with soil temperature (P < 0.01) but not soil moisture. The CH₄ uptake rate increased with increasing soil temperature because methanotroph activity increased. The N₂O flux was highest [3.6 ± 4.7 μg N₂O-N m^?2 h^?1] at PB (P < 0.01). Our findings suggest that the soil temperature and moisture are important factors of GHG dynamics in forest soils with different fire history.     

Sulfur dioxide inhibition of photosynthesis at different CO2 and O2 concentrations in relation to photorespiration

The mechanism of SO₂ inhibition of photosynthesis in intact leaves of tomato and maze was studied to evaluate SO₂ inhibition of photorespiration. Leaf tissues were fumigated with SO₂ under photorespiratory (low CO, and/or high O, concentrations) and non-photo-respiratory conditions. When tomato leaf disks were fumigated with 10 ppm SO₂ at 2, 21 and 100° o O., SO₂ inhibited photosynthesis at 2% O₂ in the same degrees as at 21% O₂. SO₂ inhibition of photosynthesis was depressed at higher CO₂ concentrations when the disks were fumigated with SO₂ at different CO₂ concentrations. High CO₂ concentrations also reduced the photosynthesis inhibition of maize leaf disks. These results suggest that SO₂ inhibits photosynthesis through other mechanisms than photorespiration inhibition and confirm the view that SO₂ competes with CO₂ for the carboxylating enzymes in photosynthesis     

土壤有机矿质复合体研究Ⅵ.胶散复合体的化学组成及其结合特征

本文研究水热条件渐变的地带性土壤中Ｇ１、Ｇ２组胶散复合体有机、无机物的化学组成及其结合特点。结果表明：Ｇ２组中铁有积累现象，游离态铁、铝氧化物含量为Ｇ２＞Ｇ１，但均随土壤类型变化。松结态腐殖质（Ｈ１）为Ｇ１＞Ｇ２，紧结态腐殖质（Ｈ３）则为Ｇ１＜Ｇ２。可提取腐殖质中，松、稳结态腐殖质之比值Ｈ１／Ｈ２和胡敏酸、富里酸之比值ＨＡ／ＦＡ，除个别土壤之外，都相关不大。Ｇ１、Ｇ２两组复合体中都含有一定数量的络     

Acidifying emissions in The Netherlands

The emission of acidifying compounds to air in the Netherlands, expressed as acidifying equivalents, consisted in 1992 mainly of NO_X (45%), NH₃ (35%) and SO₂ (20%). Transportation, agriculture and large combustion plants each contributed about 30% to the national total emission of acidifying compounds. The emissions from transportation activities mainly consisted of NO_X, while in agriculture NH₃ emission strongly dominated. Combustion processes in large combustion plants resulted both in SO₂ emissions (especially from refineries) and NO_X emissions (especially from public power plants). The total emission of acidifying substances decreases steadily in the Netherlands. The emission in 1992 was 24% lower than in 1985. It is expected to decrease further in future. The emission levels in 1992 and 1993 still are more than twice as high as the emission objective for the year 2000, set by Dutch environmental policy.     

Factors regulating acetylene reduction assay for measuring heterotrophic nitrogen fixation in water-logged soils

In the C₂H₂-C₂H₄ assay for measurement of heterotrophic N₂ fixation in water-logged soils, the diffusion of C₂H₂ into the soil and the recovery of C₂H₄ from it are critical factors regulating the assay result. To establish an C₂H₂-C₂H₄ assay technique suitable for waterlogged soils, the C₂H₂-reducing activities (ARA), assayed by varying the method of assay gas filling, the pC₂H₂ of the assay gas, the duration of assay incubation and of soil vibration before the gas sampling, were compared.

A maximum ARA was measured when the following set of procedures were applied to the soil sample in assay flasks: 1) a 4-fold repetition of I-min evacuation under 0.01 atmospheric pressure and the subsequent I-min filling under 1 atmospheric pressure with assay gas at pC₂H₂ of 0.1 atm, 2) an assay incubation for 3 hr, and 3) a sampling of an aliquot of the headspace gas after strongly vibrating the flask for 1 min.

The ARA measured by this technique was several times larger than those measured by the techniques hitherto applied, and corresponded to an almost 80% of the V _max of the sample. This technique was, therefore, proposed for the assay of heterotrophic N₂ fixation in waterlogged soils.

A striking depression of ARA in the soil sample prepared with agitation indicated that a microbial ecosystem established in the soil should be kept as undisturbed as possible throughout the C₂H₂-C₂H₄ assay.