CO2浓度、氮和水分对春小麦光合、蒸散及水分利用效率的影响

研究了不同土壤氮和土壤水分条件下,大气CO₂浓度升高对春小麦光合作用、气孔导度、蒸散和水分利用效率的影响.结果表明,CO₂浓度升高,干旱处理的春小麦(Triticum aestivum L.)叶片光合作用速率幅度增加大于湿润处理,随着氮肥用量增加光合速率相应增加,而不施氮肥增加有限;干旱处理气孔导度幅度减少大于湿润处理,不施氮肥的大于氮肥充足的.CO₂浓度升高,干旱处理的蒸散量减少比湿润处理多,不施氮肥的蒸散量减少较为明显;但干旱处理单叶WUE增加大于湿润处理;随着氮肥用量增加,冠层WUE提高,而不施氮肥的冠层WUE最低.因而CO₂浓度升高、光合速率增加和蒸散量减少会减缓干旱的不利影响,增强作物对干旱胁迫的抵御能力.     

土壤干旱条件下磷素营养对春小麦水分状况和光合作用的影响

研究了土壤干旱条件下磷素营养对春小麦水分状况和光合作用的影响。结果表明：土壤干旱下,磷素营养明显改善了春小麦的水分状况,维持了较高的ψｗ和ＲＷＣ,并因而导致了较高的净光合速率和较大的气孔开度。不同干旱程度下,限制春小麦光合的因子并不相同,轻度干旱下,光合降低主要是气孔的作用,而严重干旱下则主要是非气孔因子的作用。无论何种水分水平下,施磷处理的净光合速率皆高于不施磷处理,与其较大的气孔导度和叶肉光合     

作物光合、蒸腾与水分高效利用的试验研究

通过田间试验,对作物光合、蒸腾、气孔行为及其影响因素进行了研究。结果表明,光合与蒸腾的非线性关系可以用抛物线方程表述,其中光合速率最高时的蒸腾速率为临界值,超出该值即为奢侈蒸腾,干旱处理的临界值较低,通过合适的调控措施,抑制奢侈蒸腾并不影响光合生产,综合分析光合速率、蒸腾速率与气孔导度的关系,气孑L导度大于0．12mol·m^-2·s^-1,实施提高气孔阻力并抑制蒸腾的措施,既节约水分又促进光合作用,增加产量．光合速率基本上随光合有效辐射的增加而提高,并有光饱和点存在,水分条件影响叶片光合作用达到饱和的早晚,干旱处理的光饱和点远远低于湿润处理,强光需要水分充足相耦合,才能充分发挥光能利用率,蒸腾与辐射的线性关系十分显著。从光合有效辐射入手,在光合有效辐射大于1000μmol·m^-2·s^-1时实施措施,既可大大降低蒸腾,又可改善光合,节水增产效果不言而喻。     

干旱、CO2和温度升高对春小麦光合、蒸发蒸腾及水分利用效率的影响

研究了干旱、CO2 浓度和温度升高对春小麦生育期、光合速率 (Pn)、蒸发蒸腾 (ET)及水分利用效率 (WUE)的影响 .结果表明 ,大气CO2 浓度升高 (5 5 0、70 0 μmol·mol-1)虽可延长抽穗 成熟期 ,但高温 (日平均温度高于正常日平均温度约 4 .8℃ )对生育期的影响远大于高CO2 影响 ,使得高CO2 、高温下抽穗 成熟期缩短 ,且种子提前萌发 ;CO2 浓度升高和高温共同作用使各水分处理的小麦光合增强、气孔阻力增加、叶片水平的水分利用效率 (WUEl)和群体水平的水分利用效率 (WUE)增大 ,但对蒸腾速率影响不显著 .对蒸发蒸腾的影响因不同的土壤水分而不同 ,在高 (田间持水量的 75 %～ 85 % )、中 (田间持水量的 5 5 %～6 5 % )水分条件下 ,高温和高CO2 使蒸发蒸腾增加 ,而在低水分条件 (田间持水量的 35 %～ 4 5 % )下 ,高温和高CO2 使蒸发蒸腾减少     

NaCl胁迫对菠菜叶片中水分和光合气体交换的影响(简报)

NaCl胁迫下,菠菜幼苗叶片的净光合速率（Pn）、气孔导度（Gs）和蒸腾速率（Tr）下降。短期处理的叶片中CO2浓度（Ci）降低,气孔限制值（Is）升高,水分利用效率（WUE）增大,而长期处理的叶片中Ci升高,Is下降,WUE降低。NaCl短期处理下,菠菜光合降低以气孔限制为主,而在长期处理下光合的非气孔限制因素增大。     

干旱区胡杨光合作用对高温和CO2浓度的响应

采用LI-6400便携式光合作用测定仪实测的塔里木河下游胡杨(Populus euphratica oliv)光合作用参数,探讨了不同地下水埋深下的胡杨光合作用对CO2浓度增加和温度升高的响应.结果表明:(1)CO2浓度升高减小了胡杨气孔导度,促进了光合速率、胞间CO2浓度和水分利用效率的增加,但不同地下水埋深下,胡杨光合作用参数对CO2浓度升高的响应不同,干旱环境(地下水埋深较深)下的响应程度大于水分适宜(地下水埋深浅)环境下的响应;(2) 高温引起胡杨气孔发生不完全关闭,导致了光合作用的光抑制发生,从而降低了胡杨光合速率,但降低程度受水分条件的影响,地下水埋深较深环境下的影响程度大于地下水埋深浅的;(3)地下水埋深是控制干旱区胡杨光合作用对CO2浓度和温度升高的根本因素,6m是胡杨生长正常的临界地下水埋深,地下水埋深>6m,胡杨即遭到水分胁迫,地下水埋深>7m,胡杨即受到了较严重的水分胁迫.     

CO2浓度升高和干旱对春小麦生长和水分利用的生态效应

利用开顶式气室对春小麦进行了一个生长季的CO2倍增盆栽实验,土壤水分控制为3个水平（分别为田间持水量（FWC）的80％,60％,40％）。结果显示,CO2倍增显提高小麦的光合速率。但在相同的CO2测定浓度下,生长在加倍CO2浓度下的小麦的光合速率比当前CO2浓度下小麦低22％。高CO2浓度显促进小麦生长,相对增加幅度在适宜水分下最大为14．8％。80％FWC水分条件下高CO2使植株的干重／高度比增加15．7％,高CO2条件下,小麦的蒸腾速率降低,累积耗水量减少,水分利用效率（WUE）提高,WUE的提高幅度在适宜水分下最大,为30％。干旱（40％FWC）使小麦地上干重和WUE在当前CO2条件下分别降低72％和19％,加倍CO2条件下降低幅度较大,分别为76％和23％。根据以上结果得出结论：（1）高CO2条件下,小麦的光合速率,地上生物量和水分利用效率提高;（2）植物长期生长于高CO2浓度导致光合能力降低;（3）高CO2对植物侧向生长的促进作用大于垂直生长,即高CO2下植株将相对粗壮;（4）高CO2对植物的生态效应依赖于土壤水分,在适宜水分下相对较大;（4）在未来高CO2条件下,干旱引起的减产和水分利用效率减低幅度将会更大。     

CO2浓度升高和干旱对春小麦生长和水分利用的生态效应

利用开顶式气室对春小麦进行了一个生长季的CO2倍增盆栽实验,土壤水分控制为3个水平(分别为田间持水量(FWC)的80%、60%、40%).结果显示,CO2倍增显著提高小麦的光合速率.但在相同的CO2测定浓度下, 生长在加倍CO2浓度下的小麦的光合速率比当前CO2浓度下小麦低22%.高CO2浓度显著促进小麦生长,相对增加幅度在适宜水分下最大,为14.8%.80%FWC水分条件下高CO2使植株的干重/高度比增加15.7%.高CO2条件下,小麦的蒸腾速率降低、累积耗水量减少、水分利用效率(WUE)提高,WUE的提高幅度在适宜水分下最大,为30%.干旱(40%FWC)使小麦地上干重和WUE在当前CO2条件下分别降低72%和19%,加倍CO2条件下降低幅度较大,分别为76%和23%.根据以上结果得出结论: (1) 高CO2条件下, 小麦的光合速率、地上生物量和水分利用效率提高;(2) 植物长期生长于高CO2浓度导致光合能力降低;(3) 高CO2对植物侧向生长的促进作用大于垂直生长,即高CO2下植株将相对粗壮;(4) 高CO2对植物的生态效应依赖于土壤水分,在适宜水分下相对较大;(5) 在未来高CO2条件下,干旱引起的减产和水分利用效率减低幅度将会更大.     

山西太岳山辽东栎的光合特性

对自然生长的辽东栎林木用 LI-640 0测定其光合作用 ,实验包括以下内容 :在完全接近自然生长的条件下测定辽东栎叶片光合作用的日变化规律 ;控制光合有效辐射强度 ,测定叶片在不同 CO2 浓度下光合作用的变化规律 ;控制温度比对应时间段的温度高 2～ 4℃ ,并控制 CO2 浓度在 3 75～ 70 0 ml· m- 3间变化 ,测定辽东栎光合作用的变化情况。结果如下 :1自然状态下辽东栎光合作用的日变化有两个光合速率峰 ,峰高接近 ,上午的光合速率峰持续时间较下午的长。叶片气孔导度与光合速率间有很强的正相关 ,且对胞内 CO2 浓度和蒸腾速率有较大影响。气孔导度与叶片水压亏缺呈相反的变化趋势 ,而水压亏缺受光合有效辐射、气温的影响较大。 2在控制片温度、光合有效辐射不变的情况下 ,辽东栎的叶片水压亏缺变化幅度很小 ,气孔导度变化主要受 CO2 浓度的调节 ,表现出在目前 CO2 浓度至加倍 CO2 浓度下 ,随浓度增加而增大的趋势 ,与之对应光合速率增大 ,同时光补偿点也有所提高。当 CO2 浓度超过 80 0 ml· m- 3继续上升时 ,气孔导度、光合速率均下降 ,光补偿点继续升高。3对辽东栎叶片进行升温和高 CO2 浓度处理 ,在试验进行时的温度 (2 8～ 3 7℃ )下 ,发现在 3 75～ 70 0 ml· m- 3的 CO2 浓度范围内 ,升温均导致光     

氮素减施对茶树光合作用和氮肥利用率的影响

为探讨当前茶园施肥水平下氮素减施对茶树的生长与氮肥利用率的影响,在大田条件下设置不施氮(空白对照CK),纯氮16 kg·667 m^-2(减氮55.6%,处理A)、纯氮26kg·667 m^-2(减氮27.8%,处理B)、纯氮36 kg·667 m^-2(常规施氮CF)4个施氮处理,研究氮素用量减施对茶树光合作用、产量、氮素吸收及其利用效率的影响。结果表明:与CF比较,处理B能提高茶树的叶绿素含量、净光合速率(Pn)、气孔导度(Gs)、蒸腾速率(Tr),降低胞间CO2浓度(Ci)和水分利用率(WUE);各施氮肥处理中以处理B的产量最高,氮肥农学效率最高,土壤养分剩余较少,氮素的利用效率较高;CF产量较处理B增加不显著,氮肥农学效率降低,土壤未利用养分较多。因此,减氮27.8%的施肥能保证与常规施肥的茶叶产量,氮素利用率明显提升,有利于茶业的可持续发展。     

大气CO2浓度升高对稻季土壤中麦秸降解及氮素分趋的影响

利用中国唯一的稻麦轮作FACE(free-air carbon dioxide enrichment,开放式空气CO2浓度增高)试验平台,研究大气CO2浓度升高对稻季土壤中小麦秸秆降解速率及其氮素分趋的影响.试验设置Ambient(目前空气对照)和FACE(Ambient+200 μmol·mol-1)两个CO2浓度以及低氮处理(LN,150 kg·hm-2)和高氮处理(HN,250 kg·hm-2)两个氮肥水平,在稻季之初按标记麦秸/土壤重量比0.3%添加15N标记小麦秸秆,根据水稻生长时期依次采样测定秸秆降解速率,并通过分析土壤全氮、植株全氮及其15N丰度来观察已降解秸秆的氮素分趋情况.结果发现,大气CO2浓度升高对高氮处理土壤中小麦秸秆降解速率没有显著影响,但显著促进了低氮处理土壤中小麦秸秆的降解(p < 0.05),使其提高到与高氮处理土壤相当水平;大气CO2浓度升高显著增加了已降解秸秆中氮素的流失,在高氮处理土壤中尤为严重,而对植物吸收已降解秸秆中的氮素没有显著影响.结果表明,大气CO2浓度升高在土壤氮素相对不足时会加速土壤中小麦秸秆的降解,而在土壤氮素相对充足时又会加大降解秸秆中氮素的流失.     

不同氮和水分条件下CO2浓度升高对小麦碳氮比和碳磷比的影响

 试验设两种CO2浓度水平（350 μmol·mol-1和700 μmol·mol-1）,两种土壤水分处理（湿润、干旱）和5种N肥施用水平（0、 50、 100、 150、 200 mg·kg-1土）。结果表明,CO2浓度增加,地上部氮(N)磷(P)浓度下降,根系N浓度略有下降。无论CO2浓度是升高或是当前水平,与干旱处理相比,湿润处理的地上部和根系N浓度明显降低;地上部和根系N浓度随氮肥用量增加而增加。小麦体内N浓度下降,是因为CO2浓度升高,水分利用效率增加,这将减少质流运送养分到根系为作物利用以及氮     

Elevated CO2, rhizosphere processes,and soil organic matter decomposition

The rhizosphere is one of the key fine-scale components of C cycles. This study was undertaken to improve understanding of the potential effects of atmospheric CO2 increase on rhizosphere processes. Using C isotope techniques, we found that elevated atmospheric CO2 significantly increased wheat plant growth, dry mass accumulation, rhizosphere respiration, and soluble C concentrations in the rhizosphere. When plants were grown under elevated CO2 concentration, soluble C concentration in the rhizosphere increased by approximately 60%. The degree of elevated CO2 enhancement on rhizosphere respiration was much higher than on root biomass. Averaged between the two nitrogen treatments and compared with the ambient CO2 treatment, wheat rhizosphere respiration rate increased 60% and root biomass only increased 26% under the elevated CO2 treatment. These results indicated that elevated atmospheric CO2 in a wheat-soil system significantly increased substrate input to the rhizosphere due to both increased root growth and increased root activities per unit of roots. Nitrogen treatments changed the effect of elevated CO2 on soil organic matter decomposition. Elevated CO2 increased soil organic matter decomposition (22%) in the nitrogen-added treatment but decreased soil organic matter decomposition (18%) without nitrogen addition. Soil nitrogen status was therefore found to be important in determining the directions of the effect of elevated CO2 on soil organic matter decomposition.     

Responses of soil water balance and precipitation storage efficiency to increased fertilizer application in winter wheat

Increased fertilizer use over many years may have detrimental effects on crop production due to its high soil water consumption in rainfed regions. In this study, based on a long-term fertilization experiment initiated in 1984, we report the effect of increased fertilization on soil water balance, precipitation storage efficiency (PSE), yield and water use efficiency of winter wheat from 2005 to 2009. The experimental design consisted of a control treatment (CK) and three fertilizer treatments: nitrogen, phosphorus and manure (NPM), nitrogen and phosphorus (NP), and nitrogen (N). Soil water storage in NP and NPM was significantly lower than that in CK and N at both harvest and planting time. Compared with the CK, on average, treatments N, NP and NPM increased soil water recharge during the fallow period by 11%, 22% and 17%, and they also increased soil water depletion during growing season by 17%, 23% and 23% (P?<?0.05), respectively. The average value of annual soil water balance was positive for all treatments, and was not significantly different among treatments. Increased fertilizer application significantly (P?<?0.05) increased PSE during the summer fallow periods, and the average PSE was 28%, 32%, 34% and 33% for CK, N, NP and NPM, respectively. Wheat yield and water use efficiency increased significantly after long term fertilization, especially for treatments NP and NPM. The results indicated that more of rainfall was used for evapotranspiration and less was lost during the fallow season for the high fertility treatments after long term fertilizer application. In the long run, such changes in water use pattern could help to improve the sustainability of winter wheat production.     

CO2浓度升高和施氮条件下小麦根际呼吸对土壤呼吸的贡献

依托FACE技术平台,采用稳定13C同位素技术,通过将小麦(C3作物)种植于长期单作玉米(C4作物)的土壤上,研究了大气CO2浓度升高和不同氮肥水平对土壤排放CO2的δ13C值及根际呼吸的影响.结果表明:种植小麦后土壤排放CO2的δ13C值随作物生长逐渐降低,CO2浓度升高200 μmol·mol-1显著降低了孕穗、抽穗期(施氮量为250 kg·hm-2,HN)与拔节、孕穗期(施氮量为150 kg·hm-2,LN)土壤排放CO2的δ13C值,显著提高了孕穗、抽穗期的根际呼吸比例.拔节至成熟期,根际呼吸占土壤呼吸的比例在高CO2浓度下为24％～48％ (HN)和21％ ～48％ (LN),在正常CO2浓度下为20％ ～36％ (HN)和19％～32％(LN).不同CO2浓度下土壤排放CO2的δ13C值和根际呼吸对氮肥增加的响应不同,CO2浓度与氮肥用量在拔节期对根际呼吸的交互效应显著.     

The effects of host carbon dioxide, nitrogen and water supply on the infection of wheat by powdery mildew and aphids

In two experiments, winter wheat (Triticum aestivum cv. Cerco) was grown in 350 (ambient) and 700 μmol mol^-1 (elevated) atmospheric CO₂ concentrations. In the first experiment, plants were grown at five levels of nitrogen fertilization, and in the second experiment, plants were grown at three levels of water supply. All plants were infected with powdery mildew, caused by the fungus Erysiphe graminis. Plants grown in elevated atmospheric CO₂ concentrations had significantly reduced % shoot nitrogen contents and significantly increased % shoot water contents. At elevated atmospheric CO₂ concentrations, where plant nitrogen content was significantly reduced, the severity of mildew infection was significantly reduced, and where host water content was significantly increased, the severity of mildew infection was significantly increased. In a moderate water supply treatment, the plants grown in elevated atmospheric CO₂ concentrations had significantly reduced nitrogen contents (9·9%) and significantly increased water content (4%), the amount of mildew infection was unchanged. The severity of mildew infection appeared to be more sensitive to host water content than to host nitrogen content.     

Carbon isotope discrimination and bundle sheath leakiness in three C(4) subtypes grown under variable nitrogen,water and atmospheric CO(2) supply

The changes in composition and productivity of semi-arid C(4) grassland, anticipated with rising atmospheric CO(2), will depend on soil water and nutrient availability. The interactive effects of soil resource limitation and elevated CO(2 )on these grasses, furthermore, may vary among C(4) biochemical subtypes (NADP-ME, NAD-ME, PCK) that differ in bundle sheath leakiness (Phi) responses to drought and nitrogen supply. To address C(4) subtype responses to soil resource gradients, the carbon isotope discrimination (Delta), bundle sheath leakiness (Phi), leaf gas exchange (A, g(s), c(i)/c(a)) and above-ground biomass accumulation were measured on three dominant grasses of semi-desert grassland in south-eastern Arizona. Bouteloua curtipendula (PCK), Aristida glabrata (NADP-ME) and the non-native Eragrostis lehmanniana (NAD-ME) were grown in controlled-environment chambers from seed under a complete, multi-factorial combination of present ambient (370 ppm) and elevated (690 ppm) CO(2) concentration and under high and low water and nitrogen supply. E. lehmanniana (NAD-ME) had the highest photosynthetic rate (A) and lowest Phi compared to the other two grasses when grown under low nitrogen and water availability. However, favourable water and nitrogen supply and elevated atmospheric CO(2) enhanced photosynthetic performance and above-ground biomass production of B. curtipendula (PCK) to a greater extent than in A. glabrata and E. lehmanniana. Contrary to pre vious studies, Phi and Delta in the NADP-ME subtype (A. glabrata) were most affected by changing environmental conditions compared to the other subtypes; deviations from the classic NADP-ME anatomy in Aristida could have accounted for this result. Overall, response of semi-arid grasslands to rising atmospheric CO(2) may depend more on species-specific responses to drought and nitrogen limitation than on general C(4) subtype responses.