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1.
节水灌溉水稻叶片胞间CO2浓度及气孔与非气孔限制   总被引:4,自引:3,他引:4  
为了揭示节水灌溉水稻叶片光合作用的气孔与非气孔限制特征,在研究节水控制灌溉水稻叶片胞间CO2浓度的动态变化规律基础上,进一步探讨了气孔限制与非气孔限制情况。结果表明:水稻叶片胞间CO2浓度呈现v型的日变化规律,在12:00-14:00达到最低值,非气孔限制指标Ci/C与气孔限制值Ls变化规律相反;节水灌溉条件下未出现重度水分亏缺,没有改变胞间CO2浓度与光合作用速率的关系;较低的土壤含水率情况下,控制灌溉水稻的叶片气孔限制值Ls出现增加,非气孔限制没有增加,光合速率没有出现明显降低;气孔限制值增大、光合速率增加的现象表明Ls夸大了叶片光合作用的气孔限制情况。与常规灌溉相比,节水灌溉水稻叶片胞间CO2浓度的变化及其与影响因子间的关系并未发生变化,节水灌溉水稻叶片光合作用的气孔限制有所增加,但光合速率未出现明显降低。  相似文献   

2.
Understanding the interactions between salinity and fertilizers is of significant importance for enhancing crop yield and fertilizeruse efficiency. In this study a complete block design experiment was performed in the Hetao Irrigation District of Inner Mongolia,China, to evaluate the effects of interactions between soil salinity and nitrogen(N) application rate on sunflower photosynthesis and growth and to determine the optimum N application rate for sunflower growth in the district. Four levels of soil salinity expressed as electrical conductivity(0.33–0.60, 0.60–1.22, 1.2–2.44, and 2.44–3.95 dS m-1) and three application rates of N fertilization(90, 135,and 180 kg ha-1) were applied to 36 micro-plots. Soil salinity inhibited the photosynthetic rate, stomatal conductance, transpiration rate, plant height, leaf area, and aboveground dry matter of sunflowers. The intercellular CO2 concentration first decreased and then increased with increasing soil salinity in the seedling stage, and the instantaneous leaf water-use efficiency fluctuated with soil salinity. The stomatal and non-stomatal limitations of sunflowers alternated in the seedling stage; however, in the bud, blooming,and mature stages, the stomatal limitation was prevalent when the salinity level was lower than 2.44 dS m-1, whereas the nonstomatal limitation was predominant above the salinity level. The application of N fertilizer alleviated the adverse effects of salinity on sunflower photosynthesis and growth to some extent. During some key growth periods, such as the seedling and bud stages, a moderate N application rate(135 kg ha-1) resulted in the maximum photosynthetic rate and yielded the maximum dry matter. We suggest a moderate N application rate(135 kg ha-1) for the Hetao Irrigation District and other sunflower-growing areas with similar ecological conditions.  相似文献   

3.
以CO2浓度升高为主要特征的气候变化对作物生长发育及产量形成的影响日益受到重视。冬小麦是我国主要粮食作物之一, 主要分布在干旱及半干旱地区, 且生长期内多干旱少雨。研究不同水分条件下冬小麦的生长变化及水分利用对CO2浓度升高的响应具有重要的科学和实践意义。本研究在封顶式生长室中对2个土壤水分水平[适宜水分: 70%~80%田间持水量; 干旱胁迫: 50%~60%田间持水量]的盆栽冬小麦进行了CO2熏蒸试验[背景大气浓度: (396.1±29.2) μmol·mol-1; 升高的浓度: (760.1±36.1)μmol·mol-1]。对小麦植株生理指标、生物量、产量、耗水量和水分利用效率(WUE)等的研究结果表明, 与背景大气CO2浓度相比, CO2浓度升高可促进冬小麦生长, 其地上生物量显著增加, 适宜水分和干旱胁迫条件下分别增加了28.6%和18.6%; 籽粒产量显著增加, 适宜水分和干旱胁迫条件下分别增加了32.6%和22.6%; CO2浓度升高主要通过增加穗粒数提高籽粒产量, 穗粒数在适宜水分条件下提高24.3%, 干旱胁迫条件下提高15.5%, 对千粒重没有显著影响。CO2浓度升高使群体和产量WUE显著提高, 在适宜水分条件下提高幅度较大, 分别提高17.7%和24.8%。CO2浓度升高显著提高了叶片光合速率(Pn)、降低了气孔导度(Gs)和蒸腾速率(Tr); 在适宜水分和干旱胁迫下Pn分别提高15.6%与12.9%, Gs分别降低22.7%与18.2%, Tr分别降低8.9%与7.5%。CO2浓度升高提高了叶片水势及叶绿素含量; 在适宜水分条件下叶片水势提高幅度较大, 为7.7%; 叶片叶绿素含量在2种水分条件分别提高7.5%与3.8%。由以上试验结果可得出: CO2浓度升高对冬小麦的生长、产量及水分利用效率均具有促进作用, 而且在土壤水分状况较好时, 这种作用效果更明显; CO2浓度升高主要通过增加穗粒数来促进产量提高。  相似文献   

4.
Rising levels of atmospheric CO2 have often been found to increase above and belowground biomass production of C3 plants. The additional translocation of organic matter into soils by increased root mass and exudates are supposed to possibly increase C pools in terrestrial ecosystems. Corresponding investigations were mostly conducted under more or less artificial indoor conditions with disturbed soils. To overcome these limitations, we conducted a 14CO2 pulse-labelling experiment within the German FACE project to elucidate the role of an arable crop system in carbon sequestration under elevated CO2. We cultivated spring wheat cv. “Minaret” with usual fertilisation and ample water supply in stainless steel cylinders forced into the soil of a control and a FACE plot. Between stem elongation and beginning of ripening the plants were repeatedly pulse-labelled with 14CO2 in the field. Soil born total CO2 and 14CO2 was monitored daily till harvest. Thereafter, the distribution of 14C was analysed in all plant parts, soil, soil mineral fractions and soil microbial biomass. Due to the small number of grown wheat plants (40) in each ring and the inherent low statistical power, no significant above and belowground growth effect of elevated CO2 was detected at harvest. But in comparison to ambient conditions, 28% more 14CO2 and 12% more total CO2 was evolved from soil under elevated CO2 (550 μmol CO2 mol−1). In the root-free soil 27% more residual 14C was found in the FACE soil than in the soil from the ambient ring. In soil samples from both treatments about 80% of residual 14C was found in the clay fraction and 7% in the silt fraction. Very low 14C contents in the CFE extracts of microbial biomass in the soil from both CO2 treatments did not allow assessing their influence on this parameter. Since the calculated specific radioactivity of soil born 14CO2 gave no indication of an accelerated priming effect in the FACE soil, we conclude that wheat plants grown under elevated CO2 can contribute to an additional net carbon gain in soils.  相似文献   

5.
不同水分条件下CO2浓度升高对冬小麦碳氮转运的影响   总被引:1,自引:1,他引:1  
CO2浓度升高对作物的影响日益受到重视,水分是作物生长的必要条件之一。冬小麦是我国的主要粮食作物之一,阐明高CO2浓度和水分条件互作对冬小麦碳氮转运的影响,对客观认识气候变化背景下作物的水分管理及肥料施用具有实际指导意义。本研究利用开放式CO2富集系统(FACE)平台,以冬麦品种‘中麦175’为试验材料,采用盆栽试验方法,研究了不同CO2浓度[正常浓度(391±40)μmol·mol?1和高浓度(550±60)μmol·mol?1]及水分条件(湿润条件和干旱条件,即75%和55%田间土壤最大持水量)的冬小麦花前碳氮积累及花后碳氮转运的规律特征。结果表明:湿润条件下,与正常CO2浓度相比,高CO2浓度促进冬小麦地上部干物质及碳氮积累,开花期增幅分别为18.1%、16.5%、14.9%,成熟期增幅分别为6.6%、1.3%、4.5%,并提高碳氮转运能力及对籽粒贡献率,转运量、转运率及对籽粒贡献率的增幅碳素依次为39.3%、20.0%、30.0%,氮素依次为19.1%、3.8%、10.8%。干旱条件下,与正常CO2浓度相比,高CO2浓度对地上部碳氮积累有一定的促进作用,开花期和成熟期碳积累量分别增加3.0%和10.7%,氮积累量分别增加0和15.8%;但高CO2浓度阻碍了碳氮的转运,转运量、转运率降幅碳素分别为10.2%、12.8%,氮素分别为7.2%、7.1%;碳氮对籽粒贡献率则变化不同,碳降低14.4%,而氮升高31.3%。干旱及高CO2浓度互作与湿润条件正常CO2浓度处理相比,冬小麦碳素转运对籽粒贡献率降低更明显,地上部碳素转运量、转运率及对籽粒贡献率降幅分别为36.2%、16.9%、22.3%,但提高了氮素转运对籽粒贡献率,氮素转运量及转运率分别降低35.7%、15.2%,对籽粒贡献率增加7.0%。综合而言,高CO2浓度可促进冬小麦碳氮积累及其在花后向籽粒的转运,水分不足可能成为主要的物质转运障碍因子,限制CO2促进作用发挥。  相似文献   

6.
Abstract

Vegetables are a large source of nitrate (NO3?) in our diet. As NO2? is toxic to humans, it is undesirable to consume vegetables with high NO3? content. Therefore, this study aimed to investigate the effect of supplementing of red- and blue-LED lighting to B. alboglabra grown in the tropical greenhouse in terms of moderating NO3? accumulation, improving photosynthesis, and enhancing productivity. All plants were grown hydroponically in full nutrients under prevailing greenhouse conditions for 20?days (full sunlight). Thereafter, plants were subjected to three different light treatments for 12?days: full sunlight, shade, and shade supplemented with LEDs. The average midday photosynthetic photon flux density (PPFD) during the light treatment periods were 220?μmol m?2 s?1 (full sunlight), 55?μmol m?2 s?1 (shade), and 220?μmol m?2 s?1 (shade supplemented with LEDs). Shoot nitrate (NO3?) concentration increased significantly in plants grown in the shade. However, shoot NO3? concentration was reduced when plants were supplemented with red- and blue-LED lighting. Photosynthetic CO2 assimilation, stomatal conductance, and productivity also improved in these plants. Our results suggest that supplemental red- and blue-LED lighting in a tropical greenhouse during periods of cloudy and hazy weather could improve productivity and nutrient quality of Chinese broccoli.  相似文献   

7.
翅果油树净光合速率日变化及其主要影响因子   总被引:3,自引:0,他引:3  
对翅果油树叶片净光合速率日变化进行了测定,并分析其与蒸腾速率、胞间CO2浓度等光合参数及环境因子的关系.结果表明:翅果油树叶片净光合速率日变化呈"双峰"曲线,具有明显的光合"午休"现象,最高峰分别出现在9:00和15:00,变化范围在1.25~11.35 μmol·m-2·s-1之间;11:00~12:00引起净光合速率降低的主要因素是气孔限制因素,9:00~11:00、15:00~19:00则为非气孔限制因素.净光合速率与光合参数的关系在一天中不同时段表现不同,6:00~9:00、15:00~19:00叶片净光合速率与蒸腾速率和气孔导度呈极显著正相关,与胞间CO2浓度呈极显著负相关;9:00~12:00叶片净光合速率与胞间CO2浓度、气孔导度分别呈显著和极显著正相关,与蒸腾速率呈不显著负相关;12:00~15:00叶片净光合速率与蒸腾速率和气孔导度呈显著正相关,而与胞间CO2浓度呈不显著正相关.6:00~9:00影响叶片净光合速率的主要环境因子及其作用大小为光合有效辐射>胞间CO2浓度,且前者表现为正效应,后者表现为负效应;9:00~12:00为光合有效辐射>空气CO2浓度,且前者表现为负效应,后者表现为正效应;12:00~15:00为空气相对湿度,表现为正效应;15:00~19:00为光合有效辐射>空气温度,两者均表现为正效应.  相似文献   

8.
蒸散发(ET)是陆地水循环过程的重要组成部分,同时也是区域能量平衡以及水量平衡的关键环节,精确估算ET,对于提高水分利用效率以及优化区域用水结构具有重要意义。本文利用黑河重大计划观测数据,对比了考虑CO_2浓度和不考虑CO_2浓度对玉米冠层影响的冠层阻力模型,分别将其耦合到双源的Shuttleworth-Wallace(S-W)模型中,并利用这两种模型分时段对玉米整个生育期内半小时尺度上的ET进行模拟,利用涡度相关实测数据对模型进行验证,最后分别对影响玉米冠层阻力的气象要素和影响ET的阻力参数进行敏感性分析,探寻大气CO_2浓度改变条件下黑河中游绿洲区玉米不同生长阶段的农田耗水规律。结果表明:本文所修正的考虑CO_2浓度对玉米冠层影响的冠层阻力模型耦合到S-W模型后,能够较精准地模拟玉米整个生育期不同生长阶段半小时尺度上农田耗水过程。敏感性分析表明:各生长阶段冠层阻力(r_s~c)和冠层面高度到参考面高度间的空气动力阻力(r_a~a)对ET的影响最为强烈,其他阻力参数对ET的影响不明显,ET的变化程度随着r_s~c和r_a~a的增大而减小。本文所修正的考虑CO_2浓度影响的分时段双源模型能够精准地模拟玉米整个生育期各生长阶段的ET,可为种植结构调整和土地利用方式改变以及CO_2浓度变化环境下的农田蒸散研究提供参考。  相似文献   

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