共查询到17条相似文献,搜索用时 78 毫秒
1.
2.
3.
为了优化超临界CO2萃取槟榔碱的工艺参数,通过三元二次通用旋转组合设计实施试验,考察了萃取温度、萃取压力和萃取时间因素对槟榔碱萃取量的影响。试验结果表明:超临界萃取的温度对槟榔碱萃取量有极显著的影响,萃取时间和压力的影响较小。同时确定了槟榔碱萃取的最佳工艺参数为萃取温度72℃,压力57 MPa,时间26 min。在此条件下,槟榔碱的萃取量为6143.71 μg/g,达到理论最大萃取量的95.3%,所得萃取物中槟榔碱的百分含量为(25.85± 0.41)% 。 相似文献
4.
5.
6.
7.
超临界CO2萃取红松种仁油的工艺及其脂肪酸成分分析 总被引:1,自引:0,他引:1
为优化超临界COz萃取红松种仁油的工艺,研究了萃取压力、萃取温度和萃取时间对红松种仁油得率的影响,并对试验得到的种仁油进行了气质联用(GC—MS)分析。在单因素试验基础上进行了L9(3^4)正交试验,确定了超临界CO2萃取红松种仁油的最佳的工艺为:萃取压力40MPa,萃取温度50℃,萃取时间3h,最佳工艺条件下红松种仁油得率为45.85%。萃取压力对得率的影响最大,萃取时间次之,萃取温度对得率影响不显著。利用GC—MS鉴定出9个组分,占红松种仁油脂肪酸总量的99.98%,其中亚油酸和α亚麻酸的相对含量分别为41.79%和15.62%。 相似文献
8.
9.
10.
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。 相似文献
11.
12.
用超临界CO2脱除绿茶浓缩液中咖啡碱的工艺研究 总被引:3,自引:0,他引:3
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。 相似文献
13.
Jens-Arne Subke Ilaria Inglima Gemini Delle Vedove 《Soil biology & biochemistry》2004,36(6):1013-1015
A new principle for measuring soil CO2 efflux at constant ambient concentration is introduced. The measuring principle relies on the continuous absorption of CO2 within the system to achieve a constant CO2 concentration inside the soil chamber at ambient level, thus balancing the amount of CO2 entering the soil chamber by diffusion from the soil. We report results that show reliable soil CO2 efflux measurements with the new system. The novel measuring principle does not disturb the natural gradient of CO2 within the soil, while allowing for continuous capture of the CO2 released from the soil. It therefore holds great potential for application in simultaneous measurements of soil CO2 efflux and its δ13C, since both variables show sensitivity to a distortion of the soil CO2 profile commonly found in conventional chamber techniques. 相似文献
14.
15.
Rachhpal Jassal Andy Black Mike Novak Kai Morgenstern Zoran Nesic David Gaumont-Guay 《Agricultural and Forest Meteorology》2005,130(3-4):176-192
To better understand the biotic and abiotic factors that control soil CO2 efflux, we compared seasonal and diurnal variations in simultaneously measured forest-floor CO2 effluxes and soil CO2 concentration profiles in a 54-year-old Douglas fir forest on the east coast of Vancouver Island. We used small solid-state infrared CO2 sensors for long-term continuous real-time measurement of CO2 concentrations at different depths, and measured half-hourly soil CO2 effluxes with an automated non-steady-state chamber. We describe a simple steady-state method to measure CO2 diffusivity in undisturbed soil cores. The method accounts for the CO2 production in the soil and uses an analytical solution to the diffusion equation. The diffusivity was related to air-filled porosity by a power law function, which was independent of soil depth. CO2 concentration at all depths increased with increase in soil temperature, likely due to a rise in CO2 production, and with increase in soil water content due to decreased diffusivity or increased CO2 production or both. It also increased with soil depth reaching almost 10 mmol mol−1 at the 50-cm depth. Annually, soil CO2 efflux was best described by an exponential function of soil temperature at the 5-cm depth, with the reference efflux at 10 °C (F10) of 2.6 μmol m−2 s−1 and the Q10 of 3.7. No evidence of displacement of CO2-rich soil air with rain was observed.Effluxes calculated from soil CO2 concentration gradients near the surface closely agreed with the measured effluxes. Calculations indicated that more than 75% of the soil CO2 efflux originated in the top 20 cm soil. Calculated CO2 production varied with soil temperature, soil water content and season, and when scaled to 10 °C also showed some diurnal variation. Soil CO2 efflux and concentrations as well as soil temperature at the 5-cm depth varied in phase. Changes in CO2 storage in the 0–50 cm soil layer were an order of magnitude smaller than measured effluxes. Soil CO2 efflux was proportional to CO2 concentration at the 50-cm depth with the slope determined by soil water content, which was consistent with a simple steady-state analytical model of diffusive transport of CO2 in the soil. The latter proved successful in calculating effluxes during 2004. 相似文献
16.