亚适宜温光环境下不同硝铵比营养液对黄瓜幼苗生长、氮吸收和代谢的影响

以‘中农26’黄瓜为试材,研究亚适宜温光(18 ℃/10 ℃,180±20 μmol·m^-2·s^-1)下不同硝铵比(26:2、21:7和14:14)营养液对黄瓜幼苗生长和生理特性的影响.结果表明:硝铵比为21:7处理的黄瓜总根长最长、根体积和根表面积最大、根尖数最多;根中H⁺-ATPase活性最高;硝态氮转运蛋白(NRT)和铵转运蛋白(AMT)基因表达量也升高,提高了根系的氮吸收能力;叶中硝酸还原酶(NR)、谷氨酰胺合成酶(GS)和谷氨酸合酶(GOGAT)活性较高,提高了体内氮代谢能力,使黄瓜氮含量和干物质积累显著增加.亚适宜温光下,营养液中硝铵比为21:7时,黄瓜幼苗干质量分别比26:2和14:14处理增加14.0%和19.3%.亚适宜温光下,可通过调整营养液中硝铵比,提高黄瓜氮吸收与代谢能力,缓解亚适宜温光对黄瓜幼苗的不利影响,促进黄瓜生长.     

Root length/leaf area ratios of chalk grassland perennials and their importance for competitive interactions

Abstract. The use of root / shoot ratios to describe allocation of dry weight to structures for capturing soil resources and light is limited due to other functions of the root and shoot such as support and storage. The ratio of fine-root length to leaf area (RLA) provides a better expression of the relative sizes of above-and below-ground exchange surfaces. Dry matter partitioning, leaf area and root lengths were determined for five species of chalk grassland perennial (Carex flacca, Cirsium acaule, Festuca ovina, Leontodon hispidus and Scabiosa columbaria) by extraction of soil cores from an intact sward. The forb species had a greater proportion of their dry matter below-ground. Interspecific variation in values of RLA was considerable, mean values ranging from 137 m/m² in Cirsium acaule to ca. 27 000 m/m² for Festuca ovina. The implications of this interspecific variation in RLA for the competitive interactions in infertile calcareous grasslands are discussed in relation to phenology and internal nutrient cycling.     

应用15N示踪研究欧美杨对PM2.5无机成分NH4+和NO3-的吸收与分配

通过气溶胶发生系统模拟PM2.5颗粒的发生,运用15N示踪技术研究了欧美杨107(Populus euramericana Neva.)对PM2.5中水溶性无机成分NH+4和NO-3的吸收与分配规律。结果表明,欧美杨能够有效吸收PM2.5中的NH+4和NO-3。轻度和重度污染下,欧美杨叶片对NH+4和NO-3的吸收速率均于处理后第1天达到峰值,之后,轻度污染下对NH+4和NO-3的吸收速率迅速降低以后趋于稳定,而重度污染下对NH+4和NO-3的吸收速率缓慢下降至趋于稳定。轻度污染下的欧美杨叶片的15N含量在处理后第1天达到峰值,15N(NH+4)的含量为0.11 mg/g,干重,15N(NO-3)的为0.14 mg/g,干重,之后15N含量迅速下降至趋于稳定。重度污染下的叶片15N含量在处理第1天迅速增长,之后缓慢增长至处理后第7天达到最高值,15N(NH+4)的含量为0.11 mg/g,干重,15N(NO-3)的为0.13 mg/g,干重。处理7 d后,欧美杨不同组织器官吸收或通过再分配获取的15N含量存在差异。轻度污染下,细根对NH+4和NO-3的吸收量最高,树皮、叶柄、叶片次之,髓最低。而重度污染下,叶片对NH+4和NO-3的吸收量最高,细根、叶柄、树皮次之,髓最低。欧美杨各组织器官中NH+4和NO-3的含量均表现为重度污染大于轻度污染,且两种污染程度下的欧美杨各组织器官对NO-3的吸收均大于对NH+4的吸收。重度污染下,欧美杨茎木质部对15N(NH+4和NO-3)的吸收征调能力(Ndff,Nitrogen derived from fertilizer)最大,其次为髓,叶片最小;欧美杨各组织器官中的15N分配率表现为叶片细根叶柄树皮粗根茎木质部髓。研究结果对进一步揭示植物吸收PM2.5的机制及有效利用植物降低颗粒物污染、净化环境提供了重要的科学理论依据。     

Effects of limiting nutrients and N:P ratios on the phytoplankton growth in a shallow hypertrophic reservoir

The purpose of this study was to evaluate the effects of limiting nutrients and the N:P ratios on the growth of phytoplankton (mainly cyanobacteria) in a shallow hypertrophic reservoir between November 2002 and December 2003. Nutrient enrichment bioassays (NEBs) were conducted, along with analyses of seasonal ambient nutrients and phytoplankton taxa, in the reservoir. The average DIN:TDP and TN:TP mass ratios in the ambient water were 90 (range: 17–187) and 34 (13–60), respectively, during the study period. The dissolved inorganic phosphorus showed seasonal variation, but less than that of inorganic nitrogen. The TN:TP ratios ranged from 13 to 46 (mean: 27 ± 6) during June–December when the cyanobacteria, Microcystis, dominated the phytoplankton composition. The NEBs showed that phytoplankton growth was mainly stimulated by the phosphorus (all of total 17 cases), rather than the nitrogen concentration (8 of 17 cases). The rapid growth rate of cyanobacteria was evident with TN:TP ratios less than 30. According to the results of the NEBs with different N concentrations (0.07, 0.7 and 3.5 mg l⁻¹), but the same N:P ratios and when the nitrogen concentration was highest, the cyanobacterial growth reached a maximum at N:P ratios <1. Overall, the response of cyanobacterial growth was a direct function of added phosphorus in the NEBs, and was greater with increased N concentrations. Thus, cyanobacterial blooms favored relatively low N:P ratios in this hypertrophic reservoir system. An erratum to this article is available at .     

Growth responses of the perennial legume Sesbania sesban to NH4 and NO3 nutrition and effects on root nodulation

Preference for NH₄⁺ or NO₃⁻ nutrition by the perennial legume Sesbania sesban (L.) Merr. was assessed by supplying plants with NH₄⁺ and NO₃⁻ alone or mixed at equal concentrations (0.5 mM) in hydroponic culture. In addition, growth responses of S. sesban to NH₄⁺ and NO₃⁻ nutrition and the effects on root nodulation and nutrient and mineral composition of the plant tissues were evaluated in a hydroponic setup at a range of external concentration of NH₄⁺ and NO₃⁻ (0, 0.1, 0.2, 0.5, 2 and 5 mM). Seedlings of S. sesban grew equally well when supplied with either NH₄⁺ or NO₃⁻ alone or mixed and had high relative growth rates (RGRs) ranging between 0.19 and 0.21 d⁻¹. When larger plants of S. sesban were supplied with NH₄⁺ or NO₃⁻ alone, the RGRs and shoot elongation rates were not affected by the external concentration of inorganic N. At external N concentrations up to 0.5 mM nodulation occurred and contributed to the N nutrition through fixation of gaseous N₂ from the atmosphere. For both NH₄⁺ and NO₃⁻-fed plants the N concentration in the plant tissues, particularly water-extractable NO₃⁻, increased at high supply concentrations, and concentrations of mineral cations generally decreased. It is concluded that S. sesban can grow without an external inorganic N supply by fixing atmospheric N₂ gas via root nodules. Also, S. sesban grows well on both NH₄⁺ and NO₃⁻ as the external N source and the plant can tolerate relatively high concentrations of NH₄⁺. This wide ecological amplitude concerning N nutrition makes S. sesban very useful as a N₂-fixing fallow crop in N deficient areas and also a candidate species for use in constructed wetland systems for the treatment of NH₄⁺ rich waters.     

Structure and thermal behavior of the layered zincophosphate [NH3-CH2-CH(NH3)-CH3](ZnPO4)2

A zinc phosphate with the composition [NH₃-CH₂-CH(NH₃)-CH₃](ZnPO₄)₂, containing the doubly protonated 1,2-diaminopropane (abbr. HDAP), was synthesized by hydrothermal crystallization of zinc nitrate, phosphoric acid, 1,2-diaminopropane and trimethylenedipiperidine. The single crystal analysis shows a layered inorganic-organic structure built up of a sandwich-like motif of alternating inorganic layers and HDAP cations (trimethylenedipiperidine not being a constituent of the structure). The HDAP species are found to be disordered and serve as bridges between two adjacent inorganic layers which are separated by 3.95 Å. The bridging interaction occurs via a hydrogen-bonding network. The inorganic layer features a pattern of four-membered rings involving two ZnO₄ and two PO₄ tetrahedra connected by sharing O atoms. Thermal analysis shows that the compound is stable up to 370 °C and that the thermal decomposition of HDAP occurs in two steps between 370 and 460 °C, causing the collapse of the structure. The first decomposition step corresponds to ammonia removal which proceeds with a high activation energy (E_a = 282 kJ mol⁻¹). The high E_a value is mainly attributed to strong electrostatic interactions between organic cations and anionic inorganic layers, the disruption of the interactions being the main reason for structural collapse after the HDAP removal.     

Pressure-tuning infrared spectra of the three Magnus’ Green salts, [Pt(NH3)4][PtCl4], [Pt(ND3)4][PtCl4] and [Pt(NH3)4][PtBr4]

Pressure-tuning infrared spectra (up to ca. 40 kbar) are reported for Magnus’ Green salt, [Pt(NH₃)₄][PtCl₄] and two of its derivatives, [Pt(ND₃)₄][PtCl₄] and [Pt(NH₃)₄][PtBr₄]. The spectroscopic data indicate that there is restricted rotation of the coordinated ammonia groups about the Pt-N bonds in the complexes. It is possible that this restricted rotation is due to the presence of weak hydrogen bonding to the halogens, i.e., N-H?X (X = Cl, Br) interactions.     

Fungal and bacterial growth in soil with plant materials of different C/N ratios

Fungal (acetate-in-ergosterol incorporation) and bacterial (leucine/thymidine incorporation) growth resulting from alfalfa (C/N=15) and barley straw (C/N=75) addition was studied in soil microcosms for 64 days. Nitrogen amendments were used to compensate for the C/N difference between the substrates. Fungal growth increased to a maximum after 3–7 days, at five to eight times the controls, following the addition of straw, and three to four times the controls following the addition of alfalfa. After 20–30 days, the fungal growth rate converged with the controls, resulting in a cumulative fungal growth two to three times the controls following straw addition and about 20% higher than the controls following alfalfa addition. The bacterial growth rate reached rates five times the controls following alfalfa addition and twice that of the controls following straw addition after 3–7 days. It remained elevated after 64 days. The cumulative bacterial growth was two and four times the controls following straw and alfalfa addition, respectively. A negative correlation was found between N addition and bacterial growth, while N stimulated fungal growth. Thus, the C/N ratio of the additions (substrate and extra N) could not entirely explain the different results regarding fungal and bacterial growths. Respiration was not always related to the combined growth of the microorganisms, emphasizing the requirement for a better understanding of growth efficiencies of fungi and bacteria.     

The crystal and molecular structure of [Co(NH3)5PO4]·3H2O,a Na+-K+ ATPase probe

The title compound, Co(NH₃)₅PO₄, prepared by a modified literature procedure, was used to study the inhibition of Na⁺-K⁺ ATPase and to serve as a structural model for ML₄(nucleotide) complexes. The structure was determined by single crystal X-ray diffraction techniques. The crystals are monoclinic, space group P2₁/n, a = 8.638(3), b = 14.517(2), c = 9.145(2) Å, and β = 112.71(2)°. The structure, solved by the heavy atom method to an R value of 3.3% for 1924 reflections, consists of a slightly distorted octahedron with the cobalt bound to the five amines and a monodentate phosphate. Solution structural data is taken from ³¹P NMR measurements. From comparison with other metal phosphate complexes it is concluded that multiple monodentate coordination of a di- or triphosphate closely resembles the coordination of a monophosphate This is based on the similarity of the MO bond angle which is 129.6° in the present example.     

Interactive effects of growth‐limiting N supply and elevated atmospheric CO2 concentration on growth and carbon balance of Plantago major

To assess the interactions between concentration of atmospheric CO₂ and N supply, the response of Plantago major ssp. pleiosperma Pilger to a doubling of the ambient CO₂ concentration of 350 µl l^?1 was investigated in a range of exponential rates of N addition. The relative growth rate (RGR) as a function of the internal plant nitrogen concentration (N_i), was increased by elevated CO₂ at optimal and intermediate N_i. The rate of photosynthesis, expressed per unit leaf area and plotted versus N_i. was increased by 20-30% at elevated CO₂ for N_i above 30 mg N g^?1 dry weight. However, the rate of photosynthesis, expressed on a leaf dry matter basis and plotted versus N_i, was not affected by the CO₂ concentration. The allocation of dry matter between shoot and root was not affected by the CO₂ concentration at any of the N addition rates. This is in good agreement with theoretical models. based on a balance between the rate of photosynthesis of the shoot and the acquisition of N by the roots. The concentration of total nonstructural carbohydrates (TNC) was increased at elevated CO₂ and at N limitation, resulting in a shift in the partitioning of photosynthates from structural to nonstructural and, in terms of carbon balance, unproductive dry matter. The increase in concentration of TNC led to a decrease in both specific leaf area (SLA) and N_i at all levels of nutrient supply, and was the cause of the increased rate of photosynthesis per unit leaf area. Correction of the relationship between RGR and Ni for the accumulation of TNC made the effect of elevated CO₂ on the relationship between RGR and N_i disappear. We conclude that the shift in the relationship between RGR and N_i was due to the accumulation of TNC and not due to differences in physiological variables such as photosynthesis and shoot and root respiration, changes in leaf morphology or allocation of dry matter.     

重要理化因子对小球藻生长和油脂产量的影响

本文采用通气培养的方法研究了N、P、Fe3 、盐度、光照强度、温度对小球藻(Chlorella sp. XQ-200419)生长速率、生物量和油脂产量的影响。主要结果如下：N浓度对小球藻的生长和油脂产量均有显著的影响,在KNO3浓度0.05—0.3g/L范围内,小球藻生长速率随N浓度的增加而提高,并积累更多的生物量,而油脂含量随之递减,KNO3浓度为0.3g/L时,油脂产量最高。小球藻对P浓度变化的适应范围很大,K2HPO4浓度在10—160mg/L范围内,对小球藻的生长和油脂产量都没有显著影响。在小球藻培养后期补加不同浓度Fe3 对其生长速率没有显著影响,总脂含量随着Fe3 浓度升高呈现上升的趋势,均比对照有极显著提高,Fe3 浓度为0.75mmol/L时油脂产量最高。盐度对小球藻的生长有一定的抑制作用;油脂含量先随着盐度的增大而提高,当NaCl浓度达到0.6mol/L, 油脂含量又显著降低;油脂含量和油脂产量均在盐度为0.2mol/L时最高。光照强度对处于生长后期的小球藻的生长影响不大,但影响其油脂积累,小球藻的油脂含量和产量随光照强度的增大而显著提高,当光照强度增至280μmolm-2s-1时,油脂含量和油脂产量最高。温度对小球藻的生长速率、生物量、油脂含量和油脂产量都有显著的影响,在15-40℃范围内,随着培养温度的升高,生长速率、生物量、油脂含量和油脂产量都经历了一个先上升然后下降的过程,适合小球藻生长、积累油脂的温度范围是20-35℃,30-35℃时油脂产量最高,40℃时生物量、油脂含量和产量都最低。理化因子对生长和油脂含量的影响分为两种情况：1. 温度、光强、铁浓度和盐度的影响表现为在适宜生长的条件下提高油脂含量,这种模式可以称为“适宜模式”;2. 氮浓度的影响表现为在不利于生长的条件下提高油脂含量,这种模式可以称为“胁迫模式”。两种模式都可以提高油脂含量,但是,只有适宜模式才可以提高油脂产量。在筛选小球藻优良产油藻种时要注意,只有在适宜的培养条件下油脂含量高的藻种才具有高产油潜力。     

FT-IR and 1H NMR spectroscopic evidence of sugar ring conformational change in NH4GpG on complexation to form cis-[Pt(NH3)2(GpG)]+

The conformational change of the ribose ring in NH₄GpG and cis-[Pt(NH₃)₂(GpG)]⁺ was confirmed by FT-IR spectroscopic evidence as being C2′-endo, C3′-endo, anti, gg sugar ring pucker in the solid state. These results were compared with ¹H NMR spectral data in aqueous solution. The FT-IR spectrum of NH₄GpG shows marker bands at 802 cm^?1 and 797 cm^?1 which are assigned to the C3′-endo, anti, gg sugar-phosphate vibrations of ribose (?pG) and ribose (Gp?), respectively. The FT-IR spectrum of cis-[Pt(NH₃)₂(GpG)]⁺ (with N7N7 chelation in the GpG sequence) shows a marker band at 800 cm^?1 which is assigned to the C3′-endo, and a new shoulder band at 820 cm^?1 related to a C2′-endo ring pucker. The ribose conformation of (?pG) moiety in NH₄-GpG, C3′-endo, anti, gg changes into C2′-endo, anti, gg when a platinum atom is chelated to N7N7 in the GpG sequence.     

Studies of the reaction products of adenosine with [Pt(NH3)3Cl]Cl and cis-Pt(NH3)2Cl2 by high performance liquid chromatography

The reaction products of adenosine with [Pt(NH₃)₃Cl]Cl or cis-Pt(NH₃)₂Cl₂ have been studied using high performance liquid chromatography and uv spectroscopy. The reaction of [Pt(NH₃)₃Cl]Cl with adenosine (pH = 7.0, Pt/base = 0.5) gives four products. Two of them, mononuclear complexes in which platinum is bound to adenosine through N(7) or N(1), comprise more than 90% of all the products. The N(1) and N(7) sites on adenosine indicate almost equal binding affinity for [Pt(NH₃)₃Cl]Cl. The reaction of cis-Pt(NH₃)₂Cl₂ with adenosine has been studied in the presence of a large excess of adenosine (Pt/base ? 0.05). The reaction gives four products. One is the monomeric 2:1 complex with cis-Pt(NH₃)₂²⁺ bound to two adenosine molecules through the N(7) site and the N(1) site, and another is the monomeric 2:1 complex with cis-Pt(NH₃)₂²⁺ bound to two adenosine molecules through the N(7) sites. cis-Pt(NH₃)₂Cl₂ is stronger affinity to the N(7) site than of adenosine to the N(1) site.     

The effect of root temperature on the uptake of nitrogen and the relative size of the root system in Lolium perenne. I. Solutions containing both NH+4 and NO3−

Abstract Lolium perenne L. cv. S23 was grown in flowing culture solution, pH 5, in which the concentrations of NH₄⁺, NO₃^? and K⁺ were frequently monitored and adjusted to set values. In a pre-experimental period, plants were acclimatized to a regime in which roots were treated at 5°C with shoots at 25°C. The root temperature was then changed to one of the following, 3, 7, 9, 11, 13, 17 or 25°C, while air temperature remained at 25°C. When root temperature was increased from 5X, the relative growth rate of roots increased immediately while that of shoots changed much less for a period of approximately 9 d (phase 1). Thus, the root: shoot ratio increased, but eventually approached a new, temperature-dependent, steady value (phase 2). The fresh: freeze-dried weight ratio (i.e. water content) in shoots (and roots) increased during the first phase of morphological adjustment (phase 1). In both growth phases and at all temperatures, plants absorbed more NH₄⁺ than NO₄⁺, the tendency being extreme at temperatures below 9° where more than 85% of the N absorbed was NH₄⁺. Plants at different root temperatures, growing at markedly different rates, had very similar concentrations of total N in their tissues (cells) on a fresh weight basis, despite the fact that they derived their N with differing preference for NH₄⁺. Specific absorption rates for NH₄⁺, NO_x^?, K⁺ and H₂PO₄^? showed very marked dependence on root temperature in phase 1, but ceased to show this dependence once a steady state root: shoot ratio had been established in phase 2. The results indicate the importance of relative root size in determining ion fluxes at the root surface. At higher temperatures where the root system was relatively large, ‘demand’ per unit root was low, whereas at low temperatures roots were small relative to shoots and ‘demand’ was high enough to offset the inhibitory effects of low temperature on transport processes.     

黄花倒水莲生长与内源激素水平动态变化关系研究北大核心CSCD

为探索黄花倒水莲春梢生理生化特性的差异以及不同内源激素的变化规律,该文对黄花倒水莲春梢的生长动态进行监测,采用间接酶联免疫吸附法(ELISA)测定脱落酸(ABA)、生长素(IAA)、赤霉素(GA)、乙烯(ETH)和玉米素核苷(ZR)五种内源激素含量的动态变化,并对两者间的相关性进行分析。结果表明:(1)黄花倒水莲春梢生长发育过程可分为快速增长期(0~12 d)、生长转折期(16~20 d)和缓慢增长期(24~32 d)三个阶段。(2)内源激素ABA、GA、ETH和ZR含量在缓慢增长期显著高于快速增长期和生长转折期,IAA含量各时期差异较小。(3)春梢长、底部叶长和叶宽在快速增长期与ABA、GA、ETH和ZR含量呈负相关,且与ZR含量具有一定显著性,与IAA含量呈正相关;生长转折期,各指标与GA、ETH和ZR含量呈正相关,与GA含量具有一定显著性,与ABA含量呈负相关;缓慢增长期,各指标与五种内源激素含量均呈正相关,与IAA和ZR含量具有一定显著性。该研究结果为生产上利用外源激素调控黄花倒水莲春梢抽出以及生长提供了理论基础。     

原始森林土壤NH4+/NO3-生境特征与某些针叶树种的适应性

在陆地生态系统中,生存地段的土壤养分环境构成了植物的“营养生境”。植物在长期进化过程中往往产生对原生营养生境的生态适应,其中对NH4 和NO3-两种无机氮源的吸收、利用特性便可能是这种适应的一个重要方面。由于硝化抑制(限制)或微生物对NO3-的强烈吸收、固持作用,酸性、弱酸性的原始森林土壤中NH4 含量大都远高于NO3-,从而形成了以NH4 占绝对优势的“氮营养生境”。很多针叶树种(尤其是演替晚期阶段占优势者)对其长期所处的NH4 优势生境产生了充分适应,以致对非还原态氮(NO3-)的吸收、利用能力严重下降。这些针叶树往往表现出典型的“喜铵性”,而在NO3-优势环境中则会引起氮代谢失调和生长下降。从氮同化酶、高耐铵性、根对NH4 和NO3-的相对吸收能力及NO3-吸收的反馈控制、养分关系与养分平衡、根部碳流失、光合作用及耐荫性等多方面阐述了喜铵针叶树适应的生理生化机制。这种生态适应可能是顶极森林群落维持长期稳定的重要机制之一,而采伐干扰后NO3-明显增加的立地条件则可能会导致喜铵的“原优势针叶树种”更新困难。在温带退化森林生态系统恢复与重建过程中,顶极针叶树种对NH4 营养生境的固有适应性是必须充分考虑的问题。     

A moderate increase in the annual CH4 efflux by raised CO2 or NH4NO3 supply in a boreal oligotrophic mire

Natural wetlands release about 20% of global emissions of CH₄, an effective greenhouse gas contributing to the total radiative forcing. Thus, changes in the carbon cycle in wetlands could have significant impacts on climate. The effect of raised supply of CO₂ or NH₄NO₃ on the annual CH₄ efflux from the lawn of a boreal oligotrophic mire was investigated over two years. Ten study plots were enclosed with mini‐FACE rings, five vented with CO₂‐enriched air and the other five with ambient air. In addition, five plots were sprayed with NH₄NO₃ so that the cumulative addition of N was 3 g m^?2 y^?1; and five plots were controls. The CO₂ enrichment (target concentration 560 ppm_v) increased CH₄ efflux about 30–40%, but half of this increase seemed to be caused by the air‐blowing system. The increasing atmospheric concentration of CO₂ would promote CH₄ release in boreal mires, but the increase in CH₄ efflux would be clearly smaller than that reported in studies made in temperate or subtropical temperature conditions. Addition of N enhanced the annual release of CH₄ only slightly. At least over the short‐term, the increase in N deposition would have little effect on CH₄ effluxes. The increase in CH₄ release would probably increase radiative forcing and thus accelerate climate change. However, CH₄ effluxes are only a small part in the whole matter balance in mires and thus further studies are needed to define the net effects of raised supply of CO₂ or N for carbon accumulation, trace gas fluxes and radiative forcing.     

The effects of CO2, temperature and their interaction on the growth and yield of carrot (Daucus carota L.)

Stands of carrot (Daucus carota L.) were grown in the field within polyethylene-covered tunnels at a range of soil temperatures (from a mean of 7·5°C to 10·9°C) at either 348 (SE = 4·7) or 551 (SE = 7·7) μmol mol⁻¹ CO₂. The effect of increased atmospheric CO₂ concentration on root yield was greater than that on total biomass. At the last harvest (137d from sowing), total biomass was 16% (95% CI = 6%, 27%) greater at 551 than at 348 μmol mol⁻¹ CO₂, and 37% (95% CI = 30%, 44%) greater as a result of a 1°C rise in soil temperature. Enrichment with CO₂ or a 1°C rise in soil temperature increased root yield by 31% (95% CI = 19%, 45%) and 34% (95% CI = 27%, 42%), respectively, at this harvest. No effect on total biomass or root yield of an interaction between temperature and atmospheric CO₂ concentration at 137 DAS was detected. When compared at a given leaf number (seven leaves), CO₂ enrichment increased total biomass by 25% and root yields by 80%, but no effect of differences in temperature on plant weights was found. Thus, increases in total biomass and root yield observed in the warmer crops were a result of the effects of temperature on the timing of crop growth and development. Partitioning to the storage roots during early root expansion was greater at 551 than at 348 μmol mol⁻¹ CO₂. The root to total weight ratio was unaffected by differences in temperature at 551 μmol mol⁻¹CO₂, but was reduced by cooler temperatures at 348 μmol mol⁻¹ CO₂. At a given thermal time from sowing, CO₂ enrichment increased the leaf area per plant, particularly during early root growth, primarily as a result of an increase in the rate of leaf area expansion, and not an increase in leaf number.     

等渗NaCl和Ca(NO_3)_2胁迫对黄瓜幼苗生长和生理特性的影响

以盐敏感型的黄瓜品种‘津春2号’为材料,采用营养液栽培方法,研究了等渗NaCl和Ca(NO3)2胁迫对黄瓜幼苗生长和生理特性的影响。结果表明,NaCl胁迫不仅抑制黄瓜幼苗地上部生长,而且对根系生长也具有抑制作用;而Ca(NO3)2胁迫主要抑制黄瓜幼苗地上部生长,对根系生长没有明显影响。NaCl胁迫下,黄瓜幼苗净光合速率(Pn)降低不仅由非气孔因素引起,而且碳同化能力也降低;而Ca(NO3)2胁迫下Pn降低主要由非气孔因素引起,对植株的碳同化能力没有明显影响。等渗NaCl和Ca(NO3)2胁迫导致黄瓜幼苗叶片光系统Ⅱ(PSⅡ)反应中心过剩光能(Ex)显著升高,致使叶片超氧阴离子自由基(O-·2)产生速率加快,过氧化氢(H2O2)含量显著升高,但NaCl胁迫的升高幅度均大于Ca(NO3)2胁迫。NaCl胁迫在提高过氧化物酶(POD)和过氧化氢酶(CAT)活性的同时,降低了超氧化物歧化酶(SOD)活性,对活性氧(ROS)的清除能力有限,致使叶片ROS大量积累,膜质过氧化伤害严重;而Ca(NO3)2胁迫显著提高了SOD、POD和CAT活性,有效清除了ROS,对叶片未造成严重的膜质过氧化伤害。NaCl和Ca(NO3)2胁迫分别导致黄瓜幼苗体内Na+和Ca2+大量积累,致使离子平衡被打破,但过多Na+要比过多的Ca2+对植物体的伤害作用大。上述结果说明,黄瓜幼苗对等渗NaCl和Ca(NO3)2胁迫的生理响应存在差异。NaCl胁迫下黄瓜幼苗体内Na+大量积累,不仅限制了环境中CO2进入叶肉细胞,而且使碳同化能力降低,加之ROS清除能力有限,不能有效清除PSⅡ反应中心过剩能量所导致的ROS,因而产生了严重的膜质过氧化,影响了植株生长和光合速率;而Ca(NO3)2胁迫下,黄瓜幼苗碳同化能力没有受到影响,ROS也能够被抗氧化系统有效清除,植株没有产生严重的膜质过氧化,因而对生长和光合速率的影响没有NaCl胁迫大。     

Influences of soil volume and an elevated CO2 level on growth and CO2 exchange for the Crassulacean acid metabolism plant Opuntia ficus-indica

Effects of the current (38 Pa) and an elevated (74 Pa) CO₂ partial pressure on root and shoot areas, biomass accumulation and daily net CO₂ exchange were determined for Opuntia ficus-indica (L.) Miller, a highly productive Crassulacean acid metabolism species cultivated worldwide. Plants were grown in environmentally controlled rooms for 18 weeks in pots of three soil volumes (2 600, 6 500 and 26 000 cm³), the smallest of which was intended to restrict root growth. For plants in the medium-sized soil volume, basal cladodes tended to be thicker and areas of main and lateral roots tended to be greater as the CO₂ level was doubled. Daughter cladodes tended to be initiated sooner at the current compared with the elevated CO₂ level but total areas were similar by 10 weeks. At 10 weeks, daily net CO₂ uptake for the three soil volumes averaged 24% higher for plants growing under elevated compared with current CO₂ levels, but at 18 weeks only 3% enhancement in uptake occurred. Dry weight gain was enhanced 24% by elevated CO₂ during the first 10 weeks but only 8% over 18 weeks. Increasing the soil volume 10-fold led to a greater stimulation of daily net CO₂ uptake and biomass production than did doubling the CO₂ level. At 18 weeks, root biomass doubled and shoot biomass nearly doubled as the soil volume was increased 10-fold; the effects of soil volume tended to be greater for elevated CO₂. The amount of cladode nitrogen per unit dry weight decreased as the CO₂ level was raised and increased as soil volume increased, the latter suggesting that the effects of soil volume could be due to nitrogen limitations.