大气CO_2增加对不同生长光强下龙须菜光合生理特性的影响

为了探讨未来大气CO2升高对不同生长光强下大型海藻的影响,选取经济红藻龙须菜为实验材料,研究了其生长速率、光合作用、呼吸作用、叶绿素荧光参数以及光合色素对CO2和光强的响应。实验设置两个CO2浓度,正常空气水平CO2浓度(390μL/L)和高CO2浓度(1000μL/L);两个光强梯度,高光(300μmol m-2s-1)和低光(100μmol m-2s-1)。结果表明,CO2和光强对龙须菜的生长和光合作用有明显的交互作用。大气CO2升高并没有显著影响龙须菜的生长速率,但在不同CO2处理下,龙须菜对光强的响应不同。在空气水平下,光强的变化对其生长速率影响不显著。而在高CO2作用下,高光处理下的藻体有更高的生长速率。CO2显著促进高光生长下龙须菜的呼吸作用速率,但是在低光下作用不明显。而对于光合作用速率来说,低光培养下的藻体CO2表现为负面效应,但对高光下生长的藻体作用不明显。CO2增加没有改变龙须菜生长状态下的电子传递速率,但在高光下,CO2表现为一定的抑制作用。CO2显著降低了龙须菜天线色素藻红蛋白和叶绿素a的含量。这些CO2与光强的结合效应表明,大气CO2的升高对龙须菜光合生理特性的影响随着光强的变化而呈现不同的效应,在未来评估CO2的增加对大型海藻的影响时,要充分考虑其他环境因子的耦合效应。     

Effects of CO2 concentration on growth of filamentous algae and Littorella uniflora in a Danish softwater lake

An experiment was conducted from May to November in Lake Hampen, Denmark, to study the effect of higher CO₂ concentration on the biomass of filamentous algae. Three enclosures (1.5 m diameter) were enriched with free CO₂ to ∼10 times atmospheric equilibrium (∼170 μM) and three enclosures were kept at atmospheric equilibrium (∼17 μM). The isoetid Littorella uniflora dominated the vegetation in the enclosures. Low concentrations of nitrate and phosphate in the water were observed, especially in the summer months. During the summer, a high biomass of filamentous algae (dominated by Zygnema sp.) developed in both types of enclosures (18–58 g dry wt. m⁻² in July and August), but the biomass of algae was significantly higher (1.9–38 times) in the CO₂ enriched enclosures than in enclosures with low CO₂ concentration. L. uniflora biomass, especially leaf biomass, also showed a significant positive response to increased CO₂ concentration (75.0 ± 10.4 and 133.3 ± 42.5 g dry wt. m⁻² at low and high CO₂ concentrations, respectively) even though the massive filamentous algal growth decreased the light intensity. Both filamentous algae (in August) and L. uniflora showed lower tissue concentrations of N and P at high CO₂ concentration.     

不同温度及二氧化碳浓度下培养的龙须菜光合生理特性对阳光紫外辐射的响应

为了研究不同温度及CO₂浓度下培养的大型海藻对紫外辐射的生理学响应,选取龙须菜(Gracilaria lemaneiformis)作为实验材料。实验设置两个温度梯度(20 ℃和24 ℃),两种CO₂浓度(390 μL/L和1000 μL/L)以及3种辐射处理,即可见光(PAR)处理(滤除紫外线A(UV-A)、紫外线B(UV-B),400-700 nm)、可见光加紫外线A(PA)处理(滤除UV-B,320-700 nm)、PAB处理(全波长辐射280-700 nm)。结果表明,酸化、升温以及紫外辐射处理都未影响大型经济红藻龙须菜的叶绿素a和类胡萝卜素的含量。然而紫外辐射处理显著降低了龙须菜的有效光化学效率,其抑制水平在酸化处理的藻体中更为显著,并且随着温度的上升而进一步加剧;酸化与温度耦合使藻体对紫外辐射的敏感性增加,导致其较低的修复速率以及较高的损伤速率。     

CO2浓度和降水协同作用对短花针茅生长的影响

关于二氧化碳(CO2)浓度和降水等单因子变化对植物生长的影响研究已很多,但多因子协同作用的影响研究仍较少,制约着植物对全球变化响应的综合理解与预测.利用开顶式生长箱(OTC)模拟研究了CO2浓度升高(450和550 μmol/mol)和降水量变化(-30％、-15％、对照、+15％和+30％)的协同作用对荒漠草原优势植物短花针茅(Stipa breviflora)生长特性的影响.结果表明:550 μmol/mol CO2浓度下短花针茅植株的生物量和叶面积较对照显著增加,但450 μmol/mol CO2浓度下的变化不明显;降水增多导致植株生物量、叶面积、叶数和株高显著增加;CO2浓度与降水协同作用显著影响短花针茅植株生物量.CO2浓度升高在一定程度上缓解了降水减少对短花针茅的胁迫效应,但降水量减少3O％则明显抑制了CO2浓度升高带来的效应.研究结果有助于增进荒漠草原植物对未来气候变化的适应性理解,可为制定荒漠草原应对气候变化的对策提供依据.     

Gas exchange of Ginkgo biloba leaves at different CO2 concentration levels

One and a half year-old Ginkgo saplings were grown for 2 years in 7 litre pots with medium fertile soil at ambient air CO₂ concentration and at 700 μmol mol⁻¹ CO₂ in temperature and humidity-controlled cabinets standing in the field. In the middle of the 2nd season of CO₂ enrichment, CO₂ exchange and transpiration in response to CO₂ concentration was measured with a mini-cuvette system. In addition, the same measurements were conducted in the crown of one 60-year-old tree in the field. Number of leaves/tree was enhanced by elevated CO₂ and specific leaf area decreased significantly.CO₂ compensation points were reached at 75–84 μmol mol⁻¹ CO₂. Gas exchange of Ginkgo saplings reacted more intensively upon CO₂ than those of the adult Ginkgo. On an average, stomatal conductance decreased by 30% as CO₂ concentration increased from 30 to 1000 μmol mol⁻¹ CO₂. Water use efficiency of net photosynthesis was positively correlated with CO₂ concentration levels. Saturation of net photosynthesis and lowest level of stomatal conductance was reached by the leaves of Ginkgo saplings at >1000 μmol mol⁻¹ CO₂. Acclimation of leaf net CO₂ assimilation to the elevated CO₂ concentration at growth occurred after 2 years of exposure. Maximum of net CO₂ assimilation was 56% higher at ambient air CO₂ concentration than at 700 μmol mol⁻¹ CO₂.     

大豆主要株型和产量指标对大气CO2和温度升高的响应

针对当前气候变暖和大气CO_2浓度升高同步发生现实,以高光效大豆品种黑农41(HN41)和3个常规对照品种周豆16号(ZD16)、中豆35号(ZD35)和桂黄豆2号(GHD2)为研究对象,通过开顶式气室模拟高CO_2浓度(650μL/L)和温度升高(±0.5—0.6℃)研究了大气CO_2和温度升高对大豆的生长发育与产量影响。结果表明,CO_2浓度升高对株高、茎粗、单株干重和单株籽粒重影响极显著;温度、CO_2与品种互作极显著地影响单株籽粒重。CO_2浓度升高有增加大豆株高、茎粗、干重和单株籽粒重的趋势,且高温下CO_2浓度升高对株高和茎粗的促进作用更大,而正常温度水平下高CO_2浓度升高更有利于干物质积累。与对照CO_2浓度比,高CO_2浓度显著促进了高温下HN41、ZD16和GHD2的株高,并显著提高了正常温度下HN41、ZD16、ZD35和GHD2的单株干重。与正常温度相比,高温仅显著提高了高CO_2处理下HN41的茎粗,并显著提高了对照CO_2处理下HN41的单株籽粒重。此外,同一CO_2浓度和温度处理下,高光效大豆HN41的茎粗、根冠比和单株籽粒重等都显著高于ZD16、ZD35和GHD2;而仅在正常温度与高CO_2浓度处理下HN41的单株干重显著高于ZD16和GHD2。CO_2浓度和温度升高显著影响了高光效大豆的生长,其中,高温下CO_2浓度升高有利于其生长势,正常温度下CO_2浓度升高有利于其光合产物积累。     

剪叶疏花条件下高浓度CO2对汕优63生长和产量的影响

利用稻田FACE(Free Air CO_2Enrichment)系统平台,以杂交稻汕优63为供试材料,二氧化碳设环境CO_2浓度(Ambient)和高CO_2浓度(Ambient+200μmol/mol),抽穗期源库改变设剪叶(剪除剑叶)和疏花处理(相间剪除1次枝梗),以不处理为对照(CK),研究大气CO_2浓度升高对不同源库处理水稻产量形成及物质生产的影响。结果表明:CK条件下,大气CO_2浓度升高使汕优63籽粒产量显著增加32%,这主要与单位面积总颖花量大幅增加(+26%)有关,结实能力亦呈增加趋势但未达显著水平。大气CO_2浓度升高使抽穗期剪叶处理水稻的籽粒产量平均增加55%,明显大于对照水稻,这主要与受精率(+28%)、饱粒率(+23%)和所有籽粒平均粒重(+19%)大幅增加有关。相反,对抽穗期疏花处理水稻而言,高CO_2浓度环境下籽粒产量的增幅(+25%,P=0.07)明显小于对照水稻,这主要与结实能力的响应略有下调有关。与产量响应类似,大气CO_2浓度升高使对照、剪叶和疏花条件下最终生物量分别增加39%、43%和28%,除疏花处理外均达显著水平。抽穗期剪叶和疏花处理本身使水稻籽粒产量分别降低40%和45%,前者主要是结实能力大幅下降所致,而后者与总颖花量减半相关。以上结果表明,大气CO_2浓度升高使杂交水稻生产力大幅增加,人为减小源库比(如剪叶)可增强CO_2肥料效应,而增加源库比(如疏花)则可使这种肥料效应减弱。     

不同CO2浓度变化下干旱对冬小麦叶面积指数的影响差异

叶面积指数是作物生长状况的一个重要表征参数,也是研究陆地生态系统的一个重要的参数.当今世界温室气体排放逐年上升,气候变暖趋势明显,对气候变化敏感的农业将受到影响.在全球变化的背景下,采用农业技术转移决策支持系统(DSSAT)系统,通过在黄淮海平原典型站点模拟3种CO2浓度条件下冬小麦在水分充足和水分亏缺2种情境下的生长过程,分析不同CO2浓度下水分亏缺对冬小麦叶面积指数的影响差异.研究发现,CO2浓度升高对叶面积指数增长有促进作用,且在干旱情况下对叶面积指数的正效应比湿润情况下更为明显,在CO2浓度倍增条件下,发生水分亏缺的作物叶面积指数数倍增长.研究结论有助于分析CO2浓度变化对农作物生长过程的影响,为农田水分管理提供依据,又为估算叶面积指数提出了一种模型的方法.     

异养微生物固定CO2的合成生物学研究进展

人类活动造成大气二氧化碳（CO₂）浓度不断升高,使当今世界面临着气候变化的重大危机。微生物CO₂固定为实现地球“碳中和”提供了一条有前景的绿色发展路线。与自养微生物相比,异养微生物具有更快的生长速度和更先进的遗传工具,但是其固定CO₂的能力还很有限。近年来,基于合成生物学技术强化异养微生物CO₂固定受到诸多关注,主要包括优化能量供给、改造羧化途径以及基于异养微生物间接固定CO₂。本综述将围绕上述3个方面重点讨论异养微生物CO₂固定的研究进展,为将来更好地利用微生物CO₂固定技术实现“碳达峰、碳中和”提供参考。     

不同温度下CO2浓度增高对坛紫菜生长和叶绿素荧光特性的影响

大气CO2浓度升高对海藻的影响已有许多的研究报道,但鲜见有关温度与CO2相互作用的研究.在4种条件下对坛紫菜进行连续通气培养:(1)15℃+ 390tmol/mol CO2,(2) 15℃+700 μmol/mol CO2,(3) 25℃+390 μmol/mol CO2,(4) 25℃+ 700 μmol/mol CO2.从而探讨这种南方海域重要栽培海藻种类的生长和叶绿素荧光特性对温度和CO2相互作用的响应.结果表明:CO2对坛紫菜的生长的影响具有温度依赖性,在低温生长条件下提高CO2浓度更有利于坛紫菜的生长.CO2对坛紫菜叶绿素a(Chlorophyll a,Chl a)和类胡萝卜素(Carotenoid,Car)的促进作用远大于温度对其产生的影响.相对于25℃的生长温度而言,15℃生长温度下的坛紫菜表现出较高的最大相对电子传递速率(rETRmax),表明坛紫菜在低温环境下有较高的光合潜力;而CO2对坛紫菜的rETRmax没有明显影响.对于在不同测定温度下的光合荧光特性而言,在10-30℃测定温度范围内,在各生长条件下的海藻的rETRmax、光能利用效率(α)和最大光化学量子产量(Fv/Fm)随温度的升高变化不明显;但在较高测定温度下(≥30℃),上述荧光参数显著下降,说明高温易引发海藻光能利用效率和光合能力的下降,这可能与光系统(PS)Ⅱ反应中心活性下调有关.同时,当测定温度大于30℃时,15℃生长条件下的坛紫菜的rETRmax、α和F/Fm值下降趋势远大于25℃生长条件下的坛紫菜的值,表明在低温生长条件下的坛紫菜对短期高温胁迫的适应能力较弱;而在高CO2浓度生长条件下的坛紫菜的rETRmax总是低于正常CO2浓度生长下的值,说明CO2浓度升高会抑制坛紫菜在短期高温条件下的光合电子传递能力.     

Aquaporins and membrane diffusion of CO2 in living organisms

Background

Determination of CO₂ diffusion rates in living cells revealed inconsistencies with existing models about the mechanisms of membrane gas transport. Mainly, these discrepancies exist in the determined CO₂ diffusion rates of bio-membranes, which were orders of magnitudes below those for pure lipid bilayers or theoretical considerations as well as in the observation that membrane insertion of specific aquaporins was rescuing high CO₂ transport rates. This effect was confirmed by functional aquaporin protein analysis in heterologous expression systems as well as in bacteria, plants and partly in mammals.

Scope of Review

This review summarizes the arguments in favor of and against aquaporin facilitated membrane diffusion of CO₂ and reports about its importance for the physiology of living organisms.

Major Conclusions

Most likely, the aquaporin tetramer forming an additional fifth pore is required for CO₂ diffusion facilitation. Aquaporin tetramer formation, membrane integration and disintegration could provide a mechanism for regulation of cellular CO₂ exchange. The physiological importance of aquaporin mediated CO₂ membrane diffusion could be shown for plants and cyanobacteria and partly for mammals.

General Significance

Taking the mentioned results into account, consequences for our current picture of cell membrane transport emerge. It appears that in some or many instances, membranes might not be as permeable as it was suggested by current bio-membrane models, opening an additional way of controlling the cellular influx or efflux of volatile substances like CO₂. This article is part of a Special Issue entitled Aquaporins.     

高CO2浓度对杂交水稻光合作用日变化的影响——FACE研究

大气二氧化碳(CO_2)浓度增高导致全球变暖,但作为光合作用底物促进绿色作物的光合作用。为了明确高CO_2浓度对杂交水稻结实期光合日变化的影响,2014年利用稻田FACE(Free Air CO_2Enrichment)平台,以生产上曾创高产纪录的两个杂交稻新组合甬优2640和Y两优2号为供试材料,设置环境CO_2和高CO_2浓度(增200μmol/mol)两个水平,测定杂交稻抽穗期和灌浆中期光合作用日变化和成熟期生物量。结果表明,高CO_2浓度环境下两组合抽穗期叶片净光合速率均大幅增加(全天平均52%),但灌浆中期的平均增幅减半,其中Y两优2号这种光合下调表现更为明显。大气CO_2浓度升高使两杂交稻组合抽穗和灌浆中期叶片气孔导度均大幅下降,导致蒸腾速率下降而水分利用效率大幅增加,Y两优2号气孔导度和蒸腾速率对CO_2的响应上午大于下午,而甬优2640表现相反。尽管大气CO_2浓度升高使杂交稻结实期不同时刻胞间CO_2浓度均大幅增加,但对气孔限制值特别是胞间CO_2与空气CO_2浓度之比多无显著影响,两品种趋势一致。大气CO_2浓度升高对甬优2640地上部生物量及其组分的影响明显大于Y两优2号,CO_2与品种间多存在互作效应。以上结果表明,与甬优2640相比,Y两优2号最终生产力从高CO_2浓度环境中获益较少可能与该品种生长后期存在明显的光合适应有关,但这种光合适应似乎不是由气孔限制造成的。     

全球CO2 水平升高对浮游植物生理和生态影响的研究进展

工业革命以来由于化石燃料的大量燃烧,大气CO₂水平不断增加,预计在21世纪末将增至现有水平的两倍,达到750 μL/L。作为全球初级生产力的重要贡献者,浮游植物应对CO₂水平升高的生理生态响应必然会对水生生态系统和碳、氮等元素的生物地球化学循环产生重要影响。全球CO₂水平的升高将显著改变水体的碳化学环境,淡水生态系统(湖泊和河流)由于容量小变化比海洋更为显著。水体碳化学环境的改变首先会影响浮游植物个体,在高CO₂水平下,浮游植物的细胞会有变小的趋势,并且细胞的光合作用强度也会有不同程度的增加,其中细胞较小或者不具有碳浓缩机制(CCM)的浮游植物增加较多,此外浮游植物细胞的化学元素计量值也将显著改变。随后浮游植物个体水平上的变化会进一步影响水生生态系统,例如水体初级生产力水平的提高,浮游植物、浮游动物群落结构组成以及水体微食物网结构的变化等。此外浮游植物对CO₂水平升高的生理生态响应程度还与水体的营养水平有关。总结了大气CO₂水平升高对浮游植物生理生态影响的研究方法,展望了未来可能的研究方向。     

改变施肥管理后不同肥力稻田土壤CO2排放特征

利用一个长达30a水稻土长期定位试验,在保证原有定位试验继续正常开展的前提下,将原化肥处理改施有机肥,原有机肥处理改施化肥或者增施有机肥。通过观测田间试验2012—2013年双季稻轮作周期内不同肥力水平稻田土壤施肥管理改变后的土体CO2排放通量(FCO2),研究不同后续施肥管理对不同肥力红壤性水稻土CO2排放的影响。结果表明:变更施肥能明显改变CO2排放动态变化,其中长期施用有机肥处理改施化肥后其FCO2明显减小,长期施用化肥或有机肥处理增施有机肥后其FCO2显著增大。有机肥和土壤有机碳均可促进土体CO2排放,有机肥处理有机物料碳添加量与CO2-C年排放量呈极显著的正相关关系(r=0.9015**,n=21),单施化肥处理土壤有机碳含量与土体CO2-C年排放量符合线性方程:y=10.962x-68.86(R2=0.7507,n=9,P0.01)。长期施用有机肥土壤改施化肥会导致其有机碳矿化损失,土壤有机碳含量越高,矿化损失量越多,最终其有机碳水平将与长期施用化肥的土壤有机碳平衡值一致;长期施用化肥或有机肥土壤改施或增施有机肥可促进土壤有机碳积累,外源添加碳越多,土壤积累碳越多;相同有机肥施用量下土壤有机碳含量越高,有机物料表观分解率越大,积累于土壤中的有机碳越少,不同有机碳水平土壤在相同有机肥管理下其有机碳最终会达到相同的平衡值。在有机碳水平较低(20.46 g/kg)红壤稻田上增施有机肥是提升已培肥水稻土有机碳含量的可持续发展措施,而在有机碳水平较高(14.45 g/kg)红壤稻田上应避免改施化肥。总之,在有机碳含量较高或者较低的中国南方红壤性水稻土上,持续的有机肥施用是保持或者提高其有机碳水平的必要措施。     

Effects of elevated atmospheric CO2 on soil enzyme activities at different nitrogen application treatments

It has been predicted that elevated atmospheric CO₂ will increase enzyme activity as a result of CO₂-induced carbon entering the soil. The objective of this study was to investigate the effects of elevated atmospheric CO₂ on soil enzyme activities under a rice/wheat rotation. This experiment was conducted in Wuxi, Jiangsu, China as part of the China FACE (Free Air Carbon Dioxide Enrichment) Project. Two atmospheric CO₂ concentrations (580±60) and (380±40) μmol·mol^-1) and three N application treatments (low-150, normal-250 and high-350 kg N·hm^-2) were included. Soil samples (0-10 cm) were collected for analysis of β-glucosidase, invertase, urease, acid phosphates and β-glucosaminidase activities. The results revealed that with elevated atmospheric CO₂ β-glucosidase activity significantly decreased (P < 0.05) at low N application rates; had no significant effect with a normal N application rate; and significantly increased (P < 0.05) with a high N application rate. For urease activity, at low and normal N application rates (but not high N application rate), elevated atmospheric CO₂ significantly increased (P < 0.05) it. With acid phosphatase elevated atmospheric CO₂ only had significant higher effects (P < 0.05) at high N application rates. Under different CO₂ concentration, effects of N fertilization are also different. Soil β-glucosidase activity at ambient CO₂ concentration decreased with N fertilization, while it increased at elevated CO₂ concentration. In addition, invertase and acid phosphatase activities at elevated CO₂ concentration, significantly increased (P < 0.05) with N treatments, but there was no effect with the ambient CO₂ concentration. For urease activity, at ambient CO₂ concentration, N fertilization increased it significantly (P < 0.05), whereas at elevated CO₂ concentration it was not significant. Additionally, with β-glucosaminidase activity, there were no significant effects from N application. In general, then, elevated atmospheric CO₂ increased soil enzyme activity, which may be attributed to the following two factors: (1) elevated atmospheric CO₂ led to more plant biomass in the soil, which in turn stimulated soil microbial biomass and activity; and (2) elevated atmospheric CO₂ increased plant photosynthesis, thereby increasing plant-derived soil enzymes.     

Effects of elevated atmospheric CO2 on soil enzyme activities at different nitrogen application treatments

It has been predicted that elevated atmospheric CO₂ will increase enzyme activity as a result of CO₂-induced carbon entering the soil. The objective of this study was to investigate the effects of elevated atmospheric CO₂ on soil enzyme activities under a rice/wheat rotation. This experiment was conducted in Wuxi, Jiangsu, China as part of the China FACE (Free Air Carbon Dioxide Enrichment) Project. Two atmospheric CO₂ concentrations (580±60) and (380±40) μmol·mol^-1) and three N application treatments (low-150, normal-250 and high-350 kg N·hm^-2) were included. Soil samples (0-10 cm) were collected for analysis of β-glucosidase, invertase, urease, acid phosphates and β-glucosaminidase activities. The results revealed that with elevated atmospheric CO₂ β-glucosidase activity significantly decreased (P < 0.05) at low N application rates; had no significant effect with a normal N application rate; and significantly increased (P < 0.05) with a high N application rate. For urease activity, at low and normal N application rates (but not high N application rate), elevated atmospheric CO₂ significantly increased (P < 0.05) it. With acid phosphatase elevated atmospheric CO₂ only had significant higher effects (P < 0.05) at high N application rates. Under different CO₂ concentration, effects of N fertilization are also different. Soil β-glucosidase activity at ambient CO₂ concentration decreased with N fertilization, while it increased at elevated CO₂ concentration. In addition, invertase and acid phosphatase activities at elevated CO₂ concentration, significantly increased (P < 0.05) with N treatments, but there was no effect with the ambient CO₂ concentration. For urease activity, at ambient CO₂ concentration, N fertilization increased it significantly (P < 0.05), whereas at elevated CO₂ concentration it was not significant. Additionally, with β-glucosaminidase activity, there were no significant effects from N application. In general, then, elevated atmospheric CO₂ increased soil enzyme activity, which may be attributed to the following two factors: (1) elevated atmospheric CO₂ led to more plant biomass in the soil, which in turn stimulated soil microbial biomass and activity; and (2) elevated atmospheric CO₂ increased plant photosynthesis, thereby increasing plant-derived soil enzymes.     

不同天气水稻光合日变化对大气CO2浓度和温度升高的响应——FACE研究

人类活动导致大气二氧化碳浓度(CO_2)升高、全球气候变暖和光合有效辐射(PAR)降低,影响着绿色作物的光合作用。为了明确高CO_2浓度、高温和低PAR对水稻光合日变化特征的影响,利用中国稻田开放空气CO_2浓度升高系统(free air CO_2enrichment,FACE),以常规粳稻南粳9108为试验材料,设置了环境CO_2和高CO_2浓度(增200μmol/mol)、环境温度和增高温度(增1—2℃)交互的4个处理,从9:00到17:00每隔1h测定了阴天和晴天水稻的光合作用,研究了不同天气对水稻光合日变化对大气CO_2浓度和温度升高的响应。观察到不同天气条件下水稻光合日变化的不同特征,晴天Pn为双峰曲线,发生了光合"午休",阴天未发生。结果表明,高CO_2浓度显著提高了水稻Pn,温度升高有降低水稻Pn趋势,CO_2浓度增加200μmol/mol对水稻光合作用的促进效应远大于增温1—2℃对其的抑制效应。高CO_2浓度显著增加了水稻胞间CO_2浓度(Ci),降低了水稻蒸腾速率(Tr),平均降幅为10.8%—22.0%。高温有降低Ci的趋势,增加了Tr,平均增幅达5.0%—13.5%。晴天比阴天增加了水稻Tr,平均增幅为9.8%—31.2%。CO_2浓度和温度同时升高显著降低了水稻气孔导度(Gs)。这些结果说明CO_2浓度、温度和PAR对水稻水分利用率(WUE)产生综合影响。阴天PAR比晴天平均低53.3%,阴天水稻Pn比晴天显著低,平均降幅达37.1%—72.0%。与对照比较,高CO_2浓度处理,较高PAR(晴天)条件下水稻Pn的增幅(38.6%—58.4%)显著大于较低PAR(阴天)条件下水稻Pn的增幅(21.6%—38.8%),这一现象值得关注和深入探讨。研究结果表明,评估气候变化对水稻生产的影响,需同时考虑未来大气CO_2浓度和温度升高以及PAR下降的因素及其相互作用。     

岩溶区不同土地利用方式下土壤CO2排放模拟研究

土地利用变化作为全球气候变化研究的重要内容之一,对土壤CO₂的排放具有重要影响。岩溶区石漠化治理过程中植被恢复伴随着土地利用方式的转变,其对土壤CO₂排放的影响有待进一步研究。基于控制性实验,以土壤、岩溶含水介质初始条件相同,仅土地利用方式不同的贵州普定沙湾模拟试验场为研究对象,通过1年的土壤CO₂浓度和通量数据,研究岩溶区不同土地利用方式下土壤CO₂的排放规律及其影响因素。结果表明：(1)土壤CO₂的浓度和通量具有明显的季节变化规律,不同季节下的土壤CO₂通量呈现昼夜变化规律,温度和降雨影响着土壤CO₂的排放,前者可促进排放量,后者可抑制排放量,且不同土地利用方式受影响的程度不同;(2)耕作活动也会影响土壤CO₂的排放,耕作使得土壤变得松散,加上岩溶区下伏基岩的溶蚀作用,增加了土壤CO₂向含水层的扩散,导致春季耕地表现为负通量;(3)不同土地利用方式下土壤CO₂的年排...     

C4作物FACE(free-air CO2 enrichment)研究进展

持续迅速上升的大气二氧化碳浓度([CO₂])是全球变暖最大的驱动因子,但其作为光合作用底物直接增加了作物的生产力。相比C₃作物,人们对未来高浓度CO₂情形下C₄作物的响应规律认识较少。与封闭或半封闭气室研究相比,FACE(free-air CO₂ enrichment)试验在空气自由流动的大田条件下对作物表现进行研究,它提供了对未来作物生长环境的真实模拟,因此提供了评估CO₂肥料效应以及揭示植物响应机制的最好机会。作为人类重要的粮食和饲料来源,高粱和玉米是最重要的C₄作物。在简介美国玉米和高粱FACE系统的基础上,综述了FACE情形下高浓度CO₂(模拟本世纪中叶大气CO₂浓度,即550 μmol/mol)对两大作物生理、生长和产量以及土壤特性等方面的影响,同时比较了与气室研究结果的异同点。(1)FACE使干旱条件下两作物光合作用显著增强,但湿润条件下没有影响;FACE条件下高粱出现光合适应现象,而玉米没有;(2)FACE使两作物气孔导度大幅下降,导致叶温升高、蒸腾速率下降、蒸发蒸腾总量减少或没有变化、叶片总水势和水分利用效率增加或没有变化;(3)FACE对两作物物候期和化学组分影响很少;(4)FACE使干旱条件下两作物生长和产量略有增加,但湿润条件下没有影响;(5)FACE使高粱田土壤丛枝状菌根真菌的长度和易提取胶状物质浓度显著增加,导致水稳性土壤团聚体增加;FACE对高粱田N₂O或含氮气体(N₂O+N₂)的排放没有影响;(6)高浓度CO₂对两作物气孔导度的影响FACE试验明显大于气室试验,而对生长和产量的影响呈相反趋势。阐明CO₂与基因型、土壤湿度和大气温度间的互作效应及其机制是下一轮C₄作物FACE研究优先考虑的方向,技术的不断进步已为利用大型FACE系统来研究这些互作效应提供了可能。     

CO2浓度升高条件下内生真菌感染对宿主植物的生理生态影响

以内蒙古草原常见伴生种、感染内生真菌的天然禾草羽茅为研究对象,通过比较不同CO₂浓度和不同养分供应条件下,带内生真菌和不带菌植物在种子发芽和幼苗生长等方面的差异,探讨带内生真菌的天然禾草对CO₂浓度增加的响应。结果表明:CO₂浓度增加对带菌种子发芽率和发芽速度均无显著影响,但CO₂浓度增加显著降低了不带菌种子的发芽率和发芽速度,即CO₂浓度升高加大了带菌和不带菌种子发芽率之间的差异;内生真菌感染显著提高了宿主植物的最大净光合速率和水分利用效率;羽茅的营养生长受CO₂浓度和养分供应的交互影响,高CO₂浓度对生长的促进作用只出现在充足养分供应条件下;CO₂浓度升高和内生真菌感染对植物根系形态有显著的交互作用,在正常CO₂浓度下,带菌植株根径>1.05 mm的根系比例显著高于不带菌植株,随着CO₂浓度的升高,带菌植株上述根径根系所占比例无显著变化而不带菌植株所占比例显著升高,CO₂浓度升高导致带菌和不带菌不同根径根系分配之间的差异缩小。