Potato and wheat plants were grown for 50 d at 400, 1000 and 10000 micromoles mol-1 carbon dioxide (CO2). and sweetpotato and soybean were grown at 1000 micromoles mol-1 CO2 in controlled environment chambers to study stomatal conductance and plant water use. Lighting was provided with fluorescent lamps as a 12 h photoperiod with 300 micromoles m-2 s-1 PAR. Mid-day stomatal conductances for potato were greatest at 400 and 10000 micromoles mol-1 and least at 1000 micromoles mol-1 CO2. Mid-day conductances for wheat were greatest at 400 micromoles mol-1 and least at 1000 and 10000 micromoles mol-1 CO2. Mid-dark period conductances for potato were significantly greater at 10000 micromoles mol-1 than at 400 or 1000 micromoles mol-1, whereas dark conductance for wheat was similar in all CO2 treatments. Temporarily changing the CO2 concentration from the native 1000 micromoles mol-1 to 400 micromoles mol-1 increased mid-day conductance for all species, while temporarily changing from 1000 to 10000 micromoles mol-1 also increased conductance for potato and sweetpotato. Temporarily changing the dark period CO2 from 1000 to 10000 micromoles mol-1 increased conductance for potato, soybean and sweetpotato. In all cases, the stomatal responses were reversible, i.e. conductances returned to original rates following temporary changes in CO2 concentration. Canopy water use for potato was greatest at 10000, intermediate at 400, and least at 1000 micromoles mol-1 CO2, whereas canopy water use for wheat was greatest at 400 and similar at 1000 and 10000 micromoles mol-1 CO2. Elevated CO2 treatments (i.e. 1000 and 10000 micromoles mol-1) resulted in increased plant biomass for both wheat and potato relative to 400 micromoles mol-1, and no injurious effects were apparent from the 10000 micromoles mol-1 treatment. Results indicate that super-elevated CO2 (i.e. 10000 micromoles mol-1) can increase stomatal conductance in some species, particularly during the dark period, resulting in increased water use and decreased water use efficiency. 相似文献
氮沉降增加和降水格局改变是全球变化的两项重要内容,但是同时考虑上述两因素对温室气体CH4和CO2通量影响的原位双因子模拟研究还相当有限.本研究以长白山温带阔叶红松林土壤为研究对象,采用静态箱法研究了外施氮源(50 kg N·hm-2·a-1)和增减30%降水对土壤CH4和CO2通量的影响.结果表明:施氮能抑制土壤CH4吸收,有时甚至能将土壤对CH4的吸收转为释放,但这种抑制效应只能维持5d左右,且能在一定程度上改变CH4通量和环境因子(温度、土壤pH、粘粒含量)的相关关系.降水改变未能显著影响土壤CH4通量.对CO2通量而言,施氮能降低土壤CO2排放,长白山阔叶红松林连续施氮第4年的平均抑制效应为27.4%.长期连续施氮的平均抑制效应随施氮时间延长而逐渐增大,一定年限后达到最大值.单次施氮的抑制效应随时间延长逐渐减弱,并在1个月的施氮周期末期基本消失.施氮的抑制效应和土壤充水孔隙度(WFPS)呈显著负相关关系,且升温能增强施氮对CO2释放的抑制效应并延长抑制时间.施氮、降水有可能改变土壤呼吸的温度敏感性.本研究表明,长白山森林土壤氮素尚未达到一定阈值,未来氮沉降增加将抑制CO2的释放和CH4的吸收,因此总体来看施氮抑制土壤碳排放. 相似文献
Wetlands are significant sources of the important greenhouse gas CH4. Here we explore the use of an experimental system developed for the determination of continuous fluxes of CO2 and CH4 in closed ecosystem monoliths including the capture of 14CO2 and 14CH4 following pulse labelling with 14CO2. We show that, in the ecosystem studied, ebullition (bubble emission) may account for 18 to 50% of the total CH4 emission, representing fluxes that have been difficult to estimate accurately in the past. Furthermore, using plant removal and 14C labelling techniques, we use the system to detail the direct influence of vascular plants on CH4 emission. This influence is observed to be dependent on the amount of vascular plants present. The results that may be produced using the presented experimental set-up have implications for an improved understanding of wetland ecosystem/atmosphere interactions, including possible feedback effects on climate change. In recent years much attention has been devoted to ascertaining and subsequently using the relationship between net ecosystem productivity and CH4 emission as a basis for extrapolation of fluxes across large areas. The experimental system presented may be used to study the complex relationship between vascular plants and CH4 emission and here we show examples of how this may vary considerably in nature between and even within ecosystems. 相似文献
Proton NMR spectroscopy has been used to obtain the equilibrium constants for the reaction in CDCl3 solvent: where B represents neutral bases with oxygen or nitrogen donors. The ΔG of reaction is well correlated with the Gutmann donor number of the bases. For the oxygen bases, ΔG correlates with Drago's EB parameter but not the CB parameter; for the nitrogen bases, the reverse was obtained (i.e., correlation with the CB but not the EB). 相似文献
We tested the hypothesis that the diurnal patterns of variationin lacunal gas concentrations and isotopic fractionationpreviously reported in a single plant genera (Typha)typified the patterns of all through-flow convective plantsby extending our observations to Phragmites australisCav. In daylight, Phragmites CH4 transport isdriven by internal pressurization which results in gas flowdown young green culms and its exit from one year old deadbrown culms. Flow rates of 10.4 ± 4.0 mL min–1 weremeasured in this study. At night, CH4 is transportedfrom the sediments to the atmosphere via the lacunal plantspaces by molecular diffusion. Within green culms, lacunalCH4 concentrations varied by a factor of 1000, from 3%(parts by volume) pre-dawn to lows of 25 ppmv during midday.Methane in brown culms varied by a factor of 10 diurnally,from 5% pre-dawn to 0.3% at midday. Lacunal CO2concentrations varied similarly.Concentrations of both gases varied inversely with lacunalpressure. In green culms, large isotopic fractionations wereobserved in CH4 and CO2 in the morning and eveningduring transitions in gas transport mode and were associatedwith slight downward flows counter to the upward diffusionof these gases. Methane 13C as depletedas –100 was observed. In daylight, lacunal CH4 wassimilar to or 13C depleted relative to sedimentary andemitted CH4 isotopic values, but at night lacunalCH4 was 13C enriched relative to sedimentarymethane. Overall, the diurnal variations of CH4concentration and 13C value inPhragmiteswere similar to those observed in Typha andindicate that these patterns should be consistent in otherconvective-flow plants. Furthermore, our results demonstratethat the large isotopic fractionations found in aquaticplants can result solely from isotopic fractionationassociated with gas transport. 相似文献
The thermophilic methanogenic bacterium, Methanobacterium thermoautotrophicum, was grown on H2CO2. In continuous culture, high CH4 productivities were obtained (288 litres litre−1 day−1) with 96% CH4 in the effluent gas, i.e. the productivity was twice as high as that obtained previously by other authors, with pure or mixed cultures; the biomass was 3·6 g dry wt litre−1. 相似文献