组培环境CO2增施监控系统的设计与试验

为改善组培苗的生长发育环境,探索CO2富集等环境因素的影响,设计制作了CO2适时增施监控系统,并以葡萄组培苗为对象,利用本控制系统与传统组培方式进行了对比试验.结果表明:系统工作稳定、正常,能够有效地将CO2浓度控制在设定的(800～1 200)μL/L范围内,满足组培苗光合作用的需要;在CO2富集环境中,组培苗生长健壮、发育良好,光合自养能力显著增强.     

无糖培养条件下大型组培箱内CO2变化规律及对组培苗的影响

该文采用中国农业大学农业部设施农业生物环境工程重点开放实验室研制的设有组培微环境实时监控系统的大型组培箱，分别对矮牵牛、菊花和番茄组培苗移栽后箱体内CO₂浓度的变化规律及不同CO₂增施浓度对无糖组培苗生长的影响进行了研究。试验表明：移栽后的当天，组培箱内的CO₂浓度便开始下降，第2 d下降速度明显加快，均降至100 μL/L以下。在移栽后的第4～5 d，箱体内CO₂浓度下降到35 μL/L左右后便不再下降，一直在30～40 μL/L之间波动。因此得出：无糖培养在组培苗移栽后的第2 d就应增施CO₂，否则会直接影响组培苗的生长。在不同CO₂增施浓度试验中，当光照度控制在80 μmol/(m²·s)时，CO₂浓度为(650±50)μL/L时培养出的组培苗生长状况最好。     

CO2气调防治储粮害虫试验研究

利用自行设计的试验装置，充入CO₂气体使储粮害虫(谷蠹与米象)窒息死亡，以达到杀灭粮食害虫的目的。试验分为两个部分，一是在实验室里进行，试验温度分别在15～18℃和23～28℃；试验的CO₂气体浓度分别控制在25%、30%、35%、40%、45%、50%、55%和60%左右；试验时间分别为24、48、72、96、120、168 h。通过多次试验，找出了实验室试验的最佳参数：温度为(25±3)℃；CO₂气体浓度为25%～35%；谷蠹杀虫保持时间为72 h以上；米象杀虫保持时间为48 h。二是在实验仓进行试验，将传感器通过管道分别布置在仓的各个部位，并每隔12～24 h，测取温、湿度等。 实验仓的试验验证了实验室的试验结果，但杀虫的持续时间为10 d以上，研究成果为实仓应用CO₂气调防治储粮害虫提供了可靠的依据。     

温室CO2气体浓度环境自动调控系统的研究

为了改善现代温室内气体环境的质量，提高温室的生产产量和产品品质，介绍一种新型温室CO₂浓度自动调控系统，并运用射流理论，分析研究了系统的设计原理和方法，对系统的工作性能也作了相应的对比实验研究，结果表明该系统具有结构简单、自动控制性能好、造价低、运行经济可靠、补充CO₂速度快、CO₂浓度和气体流速分布均匀、增产效果和经济效益明显等特点。     

几种主要CO2施肥肥源性能的比较与评价

在空闲拱棚和黄瓜日光温室内，分别研究了化学反应法(H₂SO₄+NH₄HCO₃）、煤球燃烧法和颗粒CO₂气肥3种肥源的性能，并与液体CO₂进行成本比较，结果表明：化学反应法产气迅速，设备折旧成本较低；煤球燃烧法产气速度中等，原料成本最低；颗粒CO₂气肥产气速度较慢且不易调控，原料成本最高。考虑化学反应产物的再利用因素，化学反应法、煤球燃烧法和液体CO₂ 3种肥源总成本接近，但从生态、节能、成本和效果等方面综合评价，煤球燃烧法原料丰富、成本低廉，较符合我国目前的设施、经济、资源和技术条件。     

基于C8051F005的组培CO2微环境调控系统的研制与试验

基于C8051F005芯片设计开发一种新型组培气体微环境控制系统，采用高纯度CO₂定压定量供给和自动箱内循环在线监测技术，成功解决了CO₂气体难以自动精确施放和传感器检测精度及其稳定性的问题，实现了组培微环境CO₂浓度的按需设定和自动控制。该系统能够同时记录CO₂浓度的下降量和时长，既可用于研究不同组培微环境因子对组培苗同化CO₂速率的影响，又能用于规模化组培育苗生产。以驱蚊香草、冬青、大花蕙兰组培苗为实验材料，验证系统可靠性与可行性。结果表明该系统运行可靠，控制精度高，能够满足规模化组培育苗对气体微环境调控的需求和组培微环境建模的科研要求。     

我国能源消费与CO2排放的系统动力学预测

目前我国正处在全面建设小康社会的重要发展阶段。在人口总量增加、经济持续发展、居民生活能源消费不断提高的情况下,对能源供需状况进行科学、合理的预测对保障我国能源供给、促进经济可持续发展和CO₂减排,实现社会可持续发展具有重要意义。本文在研究我国现阶段能源消费和人口、经济发展现状的基础上,运用系统动力学模型预测了我国能源需求和CO₂排放量,提出能源发展和削减CO₂排放量的设想和对策。     

典型菜地土壤剖面N2O、CH4与CO2分布特征研究

为探究菜地土壤剖面N2O、CH4与CO2时空分布特征,利用地下气体原位采集系统与气相色谱法,周年动态监测3种典型菜地,即休闲裸地、轮作地Ⅰ(芹菜?空心菜?小白菜?苋菜)以及轮作地Ⅱ(菜心?芹菜?空心菜?大青菜)7 cm、15 cm、30 cm与50 cm土层N2O、CH4与CO2浓度变化。结果表明,0~50 cm土层范围内,N2O、CH4与CO2 3种气体浓度周年变异性较大,变幅分别为0.63~1 657.0μL(N2O)?L?1、0.8~72.5μL(CH4)?L?1和0.41~36.6 m L(CO2)?L?1。轮作地Ⅰ与轮作地Ⅱ的N2O平均浓度随土壤深度增加而增加,休闲裸地则呈现先增加(0~30 cm)后降低(30~50 cm)的变化趋势。两种轮作菜地4个土层N2O平均浓度均显著高于休闲裸地,二者氮肥施用量不同并未造成相同土层间N2O平均浓度的显著差异。3种菜地CH4与CO2平均浓度均呈现50 cm30 cm15 cm7 cm的梯度特征。轮作地Ⅰ与轮作地Ⅱ0~15 cm土层CH4平均浓度均大于休闲裸地,而在15~50 cm土层则分别大于和小于休闲裸地。CO2浓度呈现明显的季节性变化,除轮作地Ⅰ50 cm土层外,两种轮作菜地其他土层CO2平均浓度均小于休闲裸地对应土层。可见,蔬菜地高氮肥施用、多频次耕作等复杂管理使得N2O、CH4与CO2表现出较大的时空变异特征,其中氮肥施用对N2O的影响大于CH4与CO2,CH4受施肥与耕作的影响均较小,CO2显著受土壤温度与耕作措施的影响,在此基础上需进一步探究N2O、CH4与CO2的其他影响因素。     

畜菜互补生态系统综合研究(Ⅱ)——CO2分布状况及传输系统试验分析

通过试验测试揭示了自然扩散状态下的畜菜互补生态系统内温室中CO₂分布不均,存在着较大的浓度梯度以及畜菜配比不当等问题。设计并试验测试了塑料风管传输装置及兼有CO₂传输功能的地下热交换系统,两者对改善系统内的CO₂分布,提高蔬菜产量起到了明显作用。     

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。     

Relationship between soil CO2 concentrations and forest-floor CO2 effluxes

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.     

A new technique to measure soil CO2 efflux at constant CO2 concentration

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.     

Elevated CO2 stimulates N2O emissions in permanent grassland

To evaluate climate forcing under increasing atmospheric CO₂ concentrations, feedback effects on greenhouse gases such as nitrous oxide (N₂O) with a high global warming potential should be taken into account. This requires long-term N₂O flux measurements because responses to elevated CO₂ may vary throughout annual courses. Here, we present an almost 9 year long continuous N₂O flux data set from a free air carbon dioxide enrichment (FACE) study on an old, N-limited temperate grassland. Prior to the FACE start, N₂O emissions were not different between plots that were later under ambient (A) and elevated (E) CO₂ treatments, respectively. However, over the entire experimental period (May 1998–December 2006), N₂O emissions more than doubled under elevated CO₂ (0.90 vs. 2.07 kg N₂O-N ha⁻¹ y⁻¹ under A and E, respectively). The strongest stimulation occurred during vegetative growth periods in the summer when soil mineral N concentrations were low. This was surprising because based on literature we had expected the highest stimulation of N₂O emissions due to elevated CO₂ when mineral N concentrations were above background values (e.g. shortly after N application in spring). N₂O emissions under elevated CO₂ were moderately stimulated during late autumn–winter, including freeze–thaw cycles which occurred in the 8th winter of the experiment. Averaged over the entire experiment, the additional N₂O emissions caused by elevated CO₂ equaled 4738 kg CO₂-equivalents ha⁻¹, corresponding to more than half a ton (546 kg) of CO₂ ha⁻¹ which has to be sequestered annually to balance the CO₂-induced N₂O emissions. Without a concomitant increase in C sequestration under rising atmospheric CO₂ concentrations, temperate grasslands may be converted into greenhouse gas sources by a positive feedback on N₂O emissions. Our results underline the need to include continuous N₂O flux measurements in ecosystem-scale CO₂ enrichment experiments.     

CO2施肥对黄瓜幼苗矿质营养吸收与分配的影响

以土培和砂培黄瓜幼苗为试材，研究CO₂施肥对植株矿质营养吸收和分配的影响。结果表明：每天上午以1100±100 μl/L CO₂浓度施肥3 h或上、下午各施肥3 h明显降低植株各部位多数矿质元素的含量，CO₂施肥时间延长，降幅增大。CO₂施肥增强了黄瓜对矿质元素的吸收能力，使单株吸收总量显著增加，且施肥时间越长，吸收数量越多。因此，在CO₂施肥的同时应增加矿质营养的供给。     

超临界CO2萃取辣椒红色素的研究初探

简介了超临界CO₂流体的基本特性及国外将该流体应用于萃取分离技术的概况。报道了作者应用超临界CO₂从红辣椒中萃取红色素的研究情况。试验表明,色素和辣味素可以全部萃取出来,并可获得基本分离。     

Impact of atmospheric CO2 and plant life forms on soil microbial activities

From the global change perspective, increase of atmospheric CO₂ and land cover transformation are among the major impacts caused by human activities. In this study, we are addressing the combined issues of the effect of CO₂ concentration increase and plant type on soil microbial activities by asking how annual and perennial plant groups affect soil microbial processes under elevated CO₂. The experimental design used a mix of species of different growth forms for both annuals and perennials. Our objective was: (1) to determine how two years of annual or perennial plant cover and CO₂ enrichment could affect Mediterranean soil microbial processes; (2) to test the resistance and the resilience of these soil functional processes after a natural perturbation. We determined the effects of 2 years atmospheric CO₂ enrichment on soil potential respiration (SIR), denitrification (DEA) and nitrification (NEA) activities. We could not find any significant effect of CO₂ increase on SIR, DEA and NEA. However, we found a strong effect of the plant cover type, i.e. annuals versus perennials, on the potential microbial activity related to N cycling. DEA and NEA were significantly higher in soil under annual plants while SIR was not significantly different. To determine whether these changes would survive a natural perturbation, we carried out a rain event experiment once the experimental treatments (i.e. different plant cover and atmospheric CO₂ concentration) were stopped. The soil potential respiration, as expressed by the SIR, was not affected and remained stable. DEA rates converged rapidly under annuals and perennials after the rain event. Under both annuals and perennials NEA increased significantly after the rain event but remained significantly higher in the soil with annual plants. The relative change of the soil microbial processes induced by annual and perennial plants was inversely related to the density and the diversity of the corresponding microbial functional groups.     

CO2浓度增加对作物影响的实验研究进展

简要综述了近10年来国内外有关CO₂增加对作物生长影响的研究方法、实验装置和实验结果。CO₂增加促进了作物光合、抑制蒸腾、提高了水分利用率,有利于作物生长发育、干物质积累和产量形成。就总体而言,C₃比C₄作物对CO₂增加的反应更为敏感。