农业废弃物分解产生CO2的影响因素研究

在正交预备试验得出有机废弃物分解产生CO₂适宜条件的基础上,逐一进行单因子试验,以获得利用农业废弃物分解产生的CO₂进行棚室栽培CO₂施肥的最适发酵条件.结果表明,利用有机废弃物(稻草+猪粪)生物发酵产生CO₂的最佳条件分别为:温度50℃、含水量70%、初始pH6.0～7.0.初始C/N比因发酵目的不同有较大变化,以堆肥为目的时为30/1,而以产生CO₂为目的时,则以40/1为宜.在4个因素中,初始C/N比和含水量对CO₂释放的影响较大,其次是温度,初始pH的影响最小.     

Diurnal Oscillations in Gas Production (O2, CO2, CH4, and N2) in Soil Monoliths

Soil cores (35 cm long, 7 cm diameter) from the Macaulay Land Use Research Institute's Sourhope Research Station in the Scottish Borders were kept and monitored at constant temperature (18± 1°C) for gas production using a 1.6 mm diameter stainless steel probe fitted with a membrane inlet and connected to a quadrupole mass spectrometer. This provided a novel method for on-line, real time monitoring of soil gas dynamics. In closed-system headspace experiments, O₂ and CO₂ (measured at m/z values 32 and 44, respectively) showed anti-phase diurnal fluctuations in low-intensity simulated daylight and under a light-dark (LD, 12:12 h) regime. O₂ increased during periods of illumination and decreased in the dark. The inverse was true for CO₂ production. Ar (m/z = 40) concentration and temperature (°C) remained constant throughout the experiments. The same phase-related oscillations, in CO₂ and O₂ concentrations, were observed at 2 and 5 cm depth in soil cores. The O₂ concentration did not oscillate diurnally at 10 cm depth. In below-ground experiments, CH₄ (m/z = 15) concentration showed diurnal cycles at 2, 5 and 10 cm depth. The CH₄ production had the same diurnal phase cycle as CO₂ but with lower amplitude. Evidence of below-ground diurnal oscillations in N₂ (m/z = 28) concentration was provided at 5 cm depth. The scale of production and consumption of gases associated with soil-atmosphere interactions and below-ground processes, are shown to be a multifaceted output of several variables. These include light, circadian-controlled physiological rhythms of plants and microbes, and the interactions between these organisms.     

三江平原小叶章湿地碳排放对雪被变化的短期响应

为了解三江平原小叶章湿地碳排放对雪被变化的响应,利用黑龙江省科学院自然与生态研究所三江平原湿地生态定位研究站内试验平台,采用静态箱-气相色谱法,分别对剔除雪被处理(0 cm)和添加雪被处理(50 cm)以及对照(20 cm)小叶章湿地进行了温室气体排放通量观测,并同步观测相关环境因子。结果表明:不同处理土壤温度、含水量及碳排放量均在覆雪期较低,并随时间呈逐渐升高趋势。随着时间推移和雪被厚度增加,土壤温度不断上升,处理间差异逐渐缩小;剔除雪被处理的土壤含水量始终低于对照和添加雪被处理;在融雪期和后融雪期,对照和添加雪被处理比剔除雪被处理更能促进土壤CO₂排放;各时期土壤累积CH₄排放量在不同处理间无显著性差异。土壤温度与累积CO₂和CH₄排放量均呈显著相关关系,随土壤温度的升高,土壤累积CO₂排放量持续增加,土壤累积CH₄排放量呈先减少后迅速增加趋势;土壤含水量与累积CO₂和CH₄排放量也呈显著相关关系,随土壤含水量的增加,土壤累积CO₂排放量逐渐增多,达到一定值后趋于平缓,土壤累积CH₄排放量则持续显著增加。     

Behavioural responses of rats to gradual-fill carbon dioxide euthanasia and reduced oxygen concentrations

Carbon dioxide (CO₂) is widely used for euthanasia of laboratory rats, but little is known about the pain and distress caused by this procedure. Physiological and human self-report data suggest that CO₂ may cause pain and dyspnea, a sensation of breathlessness and increased respiratory effort, at the concentrations used for gradual-fill euthanasia. However, previous studies examining the behavioural responses of rats have reported conflicting results. In this study, detailed behavioural responses of rats were examined during gradual-fill CO₂ euthanasia and during gradual-fill with argon to produce a similar reduction in oxygen concentration. Animals were randomly allocated to the CO₂ or reduced oxygen treatment groups (n = 8 for both), and were first tested with air exposure and then with treatment gas exposure on the following day. Observations were taken for 105 s before and after gas flow began (baseline and exposure periods), as animals had ceased purposeful movement within 105 s of CO₂ flow starting. Behavioural changes from baseline during gas exposure were compared to changes during air exposure on control days. In comparison to air exposure, CO₂ resulted in increased activity, rearing, touching the nose to the chamber lid, escape behaviours and vocalizations. A small increase in touching the nose to the chamber lid was observed when oxygen concentrations were reduced with argon, but no other behavioural changes were observed. These results suggest that gradual-fill CO₂ euthanasia causes distress in rats, and that hypoxia alone is not a major cause of this distress.     

亚热带天然阔叶林转换为杉木人工林对土壤呼吸的影响

采用静态箱-气相色谱法对浙江省临安市玲珑山风景区天然阔叶林和由天然阔叶林改造的杉木人工林的土壤呼吸进行1年的定位监测.结果表明：天然阔叶林和杉木人工林土壤CO₂排放速率均呈现一致的季节性变化规律即夏秋季高、冬春季低;天然阔叶林和杉木人工林土壤CO₂排放速率分别为20.0～111.3和4.1～118.6 mg C·m^-2·h^-1;天然阔叶林土壤CO₂年累积排放通量（16.46 t CO₂·hm^-2·a^-1）显著高于杉木人工林（11.99 t CO₂·hm^-2·a^-1）.天然阔叶林和杉木人工林土壤CO₂排放速率与土壤含水量均没有显著相关性,而与5 cm处土壤温度呈显著指数相关,Q₁₀值分别为1.44和2.97;天然阔叶林土壤CO₂排放速率与土壤水溶性碳（WSOC）含量无显著相关性,杉木人工林土壤CO₂排放速率与WSOC含量呈显著相关.天然阔叶林转换为杉木人工林显著降低了土壤CO₂排放,提高了土壤呼吸对环境因子的敏感性.
     

A Compact Co2 Chilling Device for Continuous Duty in Paraffin-Type Sectioning

To obtain uniform sections cut from some of the newer embedding materials of lower melting points, particularly the polyethylene glycols, it is necessary to cool the microtome knife. A cooling device constructed for this and other paraffin-type sectioning consists of a small brass wedge attached to the knife by means of an adjustable spring clip. The wedge is small enough to mount directly on the back of the knife and does not interfere with any movement of the microtome. Three small channels are drilled in the wedge to provide one entrance and two exits for gaseous CO₂. CO₂ from an upright tank is regulated by a modified Spencer Model 930 freezing attachment, which is connected to the brass wedge by copper capillary tubing.     

开放式空气CO2浓度增高条件下旱地土壤气体CO2浓度廓线测定

设计了一套适合于FACE(free-air CO₂ enrichment)平台的旱地土壤气体CO₂浓度廓线测定方法,并将其应用于田间实验.在江苏省无锡市郊区具有太湖地区典型水稻土的稻麦轮作农田,对FACE和对照麦田以及裸土0～30cm土层的土壤气体CO₂浓度廓线进行了观测研究.结果表明,所采用的方法满足进行旱地农田土壤气体CO₂浓度廓线研究的要求;在0～30cm土层中,上层土壤气体中的CO₂向上垂直扩散要比下层土壤快;在作物旺盛生长期,大气CO₂浓度升高200±40μmol·mol^-1使0～30cm土层的土壤气体CO₂浓度显著提高14%±5%(t检验P<0.001).     

植物生长季退化草毡寒冻雏形土CO2释放特征

对中国科学院海北高寒草甸生态系统定位站地区退化草毡寒冻雏形土CO₂释放的全天候连续观测结果表明,退化草毡寒冻雏形土CO₂的释放有明显的日变化和季节动态,日最大释放速率出现于12:00～14:00,最小释放速率出现于6:00～8:00;植物生长季的最大振幅为462.49mg·m^-2·h^-1(8月18日),最小振幅为114.97mg·m^-2·h^-1(5月9日),CO₂释放速率白天大于夜晚.不同物候期CO₂释放速率亦不同,草盛期>枯黄期>返青期.最大日均值为480.76mg·m^-2·h^-1(8月18日),最小日均值为140.77mg·m^-2·h^-1(5月9日).释放速率与气温、地表温度及土壤5cm地温均呈显著或极显著相关关系,表明温度是决定CO₂释放速率季节变化的首要因素.     

Freezing by Liquid Carbon Dioxide in Making Slides Permanent

The expansion of liquid CO₂ may be employed in a quick-freeze method for making aqueous slide preparations permanent. An apparatus is described for this purpose which could be duplicated satisfactorily by cutting a 22mm square hole in the top of a standard freezing microtome specimen holder. The edges should be filed smooth to provide a flat surface for the slide to rest on, and clamps added to keep the slide in place while freezing. Once the slide is frozen, the cover slip may be readily removed, leaving practically all of the tissue on the slide. Following simultaneous thawing and dehydration of the slide in 95% alcohol, covering is done with Diaphane or Euparal and a clean, dry cover slip.     

大气CO2浓度上升和氮添加对南亚热带模拟森林生态系统土壤碳稳定性的影响

大气CO₂浓度升高和氮(N)添加对土壤碳库的影响是当前国际生态学界关注的一个热点。为阐述土壤不同形态有机碳的抗干扰能力, 运用大型开顶箱, 研究了4种处理((1)高CO₂浓度(700 µmol·mol^-1)和高氮添加(100 kg N·hm^-2·a^-1) (CN); (2)高CO₂浓度和背景氮添加(CC); (3)高氮添加和背景CO₂浓度(NN); (4)背景CO₂和背景氮添加(CK))对南亚热带模拟森林生态系统土壤有机碳库稳定性的影响。近5年的试验研究表明: (1) CN处理能明显地促进各土层中土壤总有机碳含量的增加, 其中, 下层土壤(5-60 cm土层)中的响应达到统计学水平。(2)活性有机碳库各组分对处理的响应有所差异: 不同土层中微生物生物量碳(MBC)的含量对各处理的响应趋势基本一致, 各土层中的MBC含量均为CN > CC > NN > CK, 其中0-5 cm、5-10 cm、10-20 cm 3个土层的处理间差异都达到了显著水平; 10-20 cm与20-40 cm两个土层中的易氧化有机碳处理间有显著差异; 而对于各土层中水溶性有机碳, 处理间差异均不明显。(3)各团聚体组分中的有机碳含量的响应也有所差异: 20-40 cm与40-60 cm土层中250-2000 μm组分的有机碳含量存在处理间差异; 40-60 cm土层中53-250 μm组分的有机碳对各处理响应敏感, CC处理和NN处理都有利于该组分碳的深层积累, 尤其CN处理下的效果最为明显; 在各处理10-20 cm、20-40 cm及40-60 cm土壤中, < 53 μm组分中的碳含量间差异显著。大气CO₂浓度上升和N添加促进了森林生态系统中土壤有机碳的增加, 尤其有利于深层土壤中微团聚体与粉粒、黏粒团聚体等较稳定组分中有机碳的积累, 增加了土壤有机碳库的稳定性。     

不同种源白桦根CO2释放通量地点和根径级间的差异

以草河口和帽儿山的12个种源13年生白桦(Betula platyphylla Suk.)为实验材料,在生长季分别取直径<0.5 mm、2.0~5.0 mm和> 5.0 mm三个径级根,采用红外线气体分析法离体测定根系CO2释放速率。探讨根系径级、试验地点和种源对白桦根系CO2释放通量的影响。结果表明:根直径和环境对根系CO2释放速率影响显著(P <0.01),而种源对根系CO2释放速率影响不显著(P> 0.05)。根CO2释放速率随径级的升高而显著降低(P <0.01)。草河口试验地的白桦各径级根CO2释放速率均显著高于帽儿山试验地的白桦(P <0.01)。草河口试验地和帽儿山实验地白桦直径<0.5 mm根CO2释放速率值分别为104.21和81.07 mol·g^-1·s^-1,直径2.0~5.0 mm根CO2释放速率分别为41.08和30.91 mol·g^-1·s^-1,直径> 5.0 mm根CO2释放速率分别为24.87和11.37 mol·g^-1·s^-1。白桦12个种源间的树高和胸径均差异显著(P <0.05),树高和胸径均与根系CO2释放通量呈负相关。相关研究结果将为更准确评估林木根系CO2释放通量提供重要基础。     

CO2浓度增加对半干旱区春小麦生产和水分利用效率的影响

为了解CO₂浓度升高条件下春小麦生产和水分利用效率(WUE)的响应特征,在典型半干旱区定西,利用开顶式气室(OTC)试验平台开展了CO₂浓度增加模拟试验.试验设对照(390 μmol·mol^-1)、480 μmol·mol^-1和570 μmol·mol^-1 3个CO₂浓度.结果表明: CO₂浓度升高使春小麦冠层空气温度小幅上升,10 cm深处的土壤环境温度下降;CO₂浓度增加对春小麦各器官生物量和总生物量都有明显促进作用,在480和570 μmol·mol^-1浓度下,地上干物质量平均增长20.6%和41.5%,总干物质量平均增长19.3%和39.6%.生物量增加主要是由茎叶干物质量增加所致,与生育中期物质生产能力明显增强有关;在两种CO₂浓度处理下,植株根冠比分别降低7.3%和11.8%,CO₂浓度增加对春小麦地上部分干物质积累的贡献大于地下部分;CO₂浓度升高主要通过影响穗粒数来影响最终产量,在480和570 μmol·mol^-1浓度下,小麦产量分别增加了8.9%和19.9%;大气CO₂浓度升高对春小麦光合作用影响的长期效应不明显,随CO₂浓度升高,光合速率显著提高,蒸腾速率降低,蒸发蒸腾量减小.随CO₂浓度升高,叶片、群体和产量3个水平的WUE都增加,其中群体水平的WUE增幅最大,产量水平的WUE增幅最小.     

CO2浓度增加对半干旱区春小麦生产和水分利用效率的影响

为了解CO₂浓度升高条件下春小麦生产和水分利用效率(WUE)的响应特征,在典型半干旱区定西,利用开顶式气室(OTC)试验平台开展了CO₂浓度增加模拟试验.试验设对照(390 μmol·mol^-1)、480 μmol·mol^-1和570 μmol·mol^-1 3个CO₂浓度.结果表明: CO₂浓度升高使春小麦冠层空气温度小幅上升,10 cm深处的土壤环境温度下降;CO₂浓度增加对春小麦各器官生物量和总生物量都有明显促进作用,在480和570 μmol·mol^-1浓度下,地上干物质量平均增长20.6%和41.5%,总干物质量平均增长19.3%和39.6%.生物量增加主要是由茎叶干物质量增加所致,与生育中期物质生产能力明显增强有关;在两种CO₂浓度处理下,植株根冠比分别降低7.3%和11.8%,CO₂浓度增加对春小麦地上部分干物质积累的贡献大于地下部分;CO₂浓度升高主要通过影响穗粒数来影响最终产量,在480和570 μmol·mol^-1浓度下,小麦产量分别增加了8.9%和19.9%;大气CO₂浓度升高对春小麦光合作用影响的长期效应不明显,随CO₂浓度升高,光合速率显著提高,蒸腾速率降低,蒸发蒸腾量减小.随CO₂浓度升高,叶片、群体和产量3个水平的WUE都增加,其中群体水平的WUE增幅最大,产量水平的WUE增幅最小.     

Diurnal Oscillations of Gas Production and Effluxes (CO2 and CH4) in Cores from a Peat Bog

Peat cores (15 cm diam X 30 cm deep) from Ellergower Moss, New Galloway, Scotland were kept and monitored at constant temperature (10 ± 0.1ºC) for gas production using a 1.6 mm diam stainless steel probe fitted with a membrane inlet and connected to a quadrupole mass spectrometer. In the headspace, O₂, CO₂ and CH₄ (measured at m/z values 32, 44 and 15 respectively) showed diurnal fluctuations in low-intensity natural daylight and under a light-dark (LD, 12:12) regime. Over the first few cycles O₂ and CO₂ increased together in the dark and decreased in the light, whereas CH₄ showed variations in antiphase with the other two gases. CO₂ and CH₄ also showed diurnal oscillations at 15 cm depth, but these decreased together in the light whereas argon (m/z = 40) was not varying. A highly-damped free-run of the oscillations in gas concentrations at 15cm depth was evident for only 3 cycles in complete darkness and at constant temperature. This might suggest desynchronization between individual plants with different free-running periods. A hydrocarbon signal (m/z = 26) at 15 cm depth also showed diurnal cycles but out of phase with CO 2 and CH 4 . We postulate a circadian control of microbiological activities imposed by the vascular plants (Carex, Eriophorum, Molinia, Calluna, Erica). Under natural conditions the pronounced temperature sensitivity of CO₂ and CH₄ emission results in entrainment to daily temperature cycles. The amplitudes of the rhythms are greatest when temperature and light intensity changes are most pronounced, i.e. when the fluctuations in environmental factors are most potent as synchronizers (zeitgebers) and as masking factors.     

Productivity of well-watered Panicum virgatum does not increase with CO2 enrichment

Aims Rising atmospheric CO₂ has been shown to increase aboveground net primary productivity (ANPP) in water-limited perennial grasslands, in part by reducing stomatal conductance and transpiration, thereby reducing depletion of soil moisture. However, the benefits of CO₂ enrichment for ANPP will vary with soil type and may be reduced if water limitation is low. Little is known about CO₂ effects on ANPP of Panicum virgatum, a perennial C₄ tallgrass and potential bioenergy crop. We hypothesized that if water limitation is minimized, (i) CO₂ enrichment would not increase P. virgatum ANPP because photosynthetic rates of this C₄ grass would not increase and because decreased transpiration at elevated CO₂ would provide little additional benefit in increased soil moisture and (ii) soil type will have little effect on P. virgatum CO₂ responses because of high overall soil moisture.Methods Growth and leaf physiology of P. virgatum cv. 'Alamo' were studied as plants established for 4 years on silty clay and clay soils along a 250 to 500 μl l -1 gradient in atmospheric CO₂ located in central Texas, USA. Plants were watered to replace evapotranspiration, fertilized with NO 3 NH 4 and P 2 O 5 and clipped to standard height during mid-season.Important findings ANPP increased through the third year of growth. Soil moisture (0–20 cm), ANPP, tiller numbers and leaf area index were 8–18% higher on the clay than on the silty clay soil. ANPP did not increase with CO₂ except in the planting year. However, biomass removed with clipping strongly increased with CO₂ in years 2 and 3, suggesting that CO₂ enrichment increased the early- to mid-season growth of establishing P. virgatum but not later regrowth or that of fully established plants. Furthermore, CO₂ enrichment differentially affected two components of ANPP in years 2 and 3, increasing tiller mass and reducing tiller numbers. This reallocation of resources in clipped P. virgatum suggested increased meristem limitation of productivity with CO₂ enrichment. CO₂ enrichment had little effect on photosynthesis but increasingly reduced stomatal conductance and transpiration as the plants established. As a result, water use efficiency became increasingly coupled to CO₂ as leaf area increased during establishment. These results suggest that for well-watered and clipped P. virgatum, ANPP differed between soil types, was not affected by CO₂ enrichment when fully established but interacted with clipping to alter allocation patterns during establishment. Soil type effects on ANPP-CO₂ responses will likely become more apparent when water is more limiting.     

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.     

CO2加富下水氮耦合对黄瓜叶片光合作用和超微结构的影响

以‘津优35号’黄瓜为试材,采用裂区-再裂区设计,研究了CO₂加富下水氮耦合对黄瓜叶片光合作用和超微结构的影响.主区设大气CO₂浓度(400 μmol·mol^-1,A)和加富CO₂浓度(800±20 μmol·mol^-1,E)2个CO₂浓度处理,裂区设无干旱胁迫(田间持水量的95%,W)和干旱胁迫(田间持水量的75%,D)2个水分处理,再裂区设施氮量450 kg·hm^-2(低氮,N₁)和900 kg·hm^-2(高氮,N₂)2个氮素处理.结果表明: 在干旱和高氮条件下,CO₂加富提高了黄瓜的株高,且使高氮下的叶面积显著增加.正常灌溉条件下,高氮处理的光合速率、气孔导度和蒸腾速率高于低氮处理,而干旱条件下则相反;CO₂加富提高了黄瓜叶片的水分利用效率,并且随着施氮量的增加,其水分利用效率提高.干旱胁迫下,黄瓜近轴面气孔密度增加,而CO₂加富和高氮却显著降低了气孔密度.高氮处理增加了黄瓜叶片叶绿体数量而减少了淀粉粒数量,干旱胁迫使叶绿体数量减少,但使淀粉粒数量呈上升趋势.干旱胁迫增加了叶绿体长度和宽度,显著增加了淀粉粒的大小,而高氮降低了叶绿体和淀粉粒的长度和宽度.CO₂加富和高氮均使基粒厚度和片层数增加(ADN₂除外),并且EDN₂处理的片层数显著高于ADN₂.综上所述,CO₂加富和适宜的水、氮条件能促进黄瓜叶片叶绿体类囊体膜系的发育,显著增加基粒厚度和基粒片层数,有效改善黄瓜的叶绿体结构,增强光合性能,提高黄瓜植株对CO₂和水、氮的吸收利用能力.     

CO2加富下水氮耦合对黄瓜叶片光合作用和超微结构的影响

以‘津优35号’黄瓜为试材,采用裂区-再裂区设计,研究了CO₂加富下水氮耦合对黄瓜叶片光合作用和超微结构的影响.主区设大气CO₂浓度(400 μmol·mol^-1,A)和加富CO₂浓度(800±20 μmol·mol^-1,E)2个CO₂浓度处理,裂区设无干旱胁迫(田间持水量的95%,W)和干旱胁迫(田间持水量的75%,D)2个水分处理,再裂区设施氮量450 kg·hm^-2(低氮,N₁)和900 kg·hm^-2(高氮,N₂)2个氮素处理.结果表明: 在干旱和高氮条件下,CO₂加富提高了黄瓜的株高,且使高氮下的叶面积显著增加.正常灌溉条件下,高氮处理的光合速率、气孔导度和蒸腾速率高于低氮处理,而干旱条件下则相反;CO₂加富提高了黄瓜叶片的水分利用效率,并且随着施氮量的增加,其水分利用效率提高.干旱胁迫下,黄瓜近轴面气孔密度增加,而CO₂加富和高氮却显著降低了气孔密度.高氮处理增加了黄瓜叶片叶绿体数量而减少了淀粉粒数量,干旱胁迫使叶绿体数量减少,但使淀粉粒数量呈上升趋势.干旱胁迫增加了叶绿体长度和宽度,显著增加了淀粉粒的大小,而高氮降低了叶绿体和淀粉粒的长度和宽度.CO₂加富和高氮均使基粒厚度和片层数增加(ADN₂除外),并且EDN₂处理的片层数显著高于ADN₂.综上所述,CO₂加富和适宜的水、氮条件能促进黄瓜叶片叶绿体类囊体膜系的发育,显著增加基粒厚度和基粒片层数,有效改善黄瓜的叶绿体结构,增强光合性能,提高黄瓜植株对CO₂和水、氮的吸收利用能力.     

高CO2浓度对长白山阔叶红松林主要树种的影响

组成长白山阔叶红松林的主要树种红松、云杉、落叶松、大青杨、白桦、椴树、水曲柳和色木的幼树,盆栽于模拟自然光照和人工调节CO₂浓度为700μl·L^-1、400μl·L^-1的气室内两个生长季,以生长在400μl·L^-1下的幼树为对照组,在各自生长条件下测定,高CO₂浓度下生长的红松、云杉、落叶松、大青杨、白桦、椴树、水曲柳和色木的高生长比对照组的幼树提高10%～40%.高CO₂浓度的幼树与对照CO₂下的幼树相比各树种蒸腾速率升降不一,但水分利用效率均有不同程度的提高,不同树种的可溶性糖和叶绿素含量对高CO₂浓度反应不一,反映出幼树对高CO₂浓度适应的复杂性.长期高CO₂浓度环境下生长的阔叶树对CO₂变化反应较针叶树敏感,供试树种均发生光合驯化现象.     

CO2浓度升高对水体硝化、反硝化作用的影响研究进展

大气CO₂浓度升高潜移默化地影响着水体生态系统的碳循环过程.然而,该过程如何影响与其耦合的氮循环过程仍不明确.水体硝化、反硝化过程作为水体氮循环的重要环节,必然会对大气CO₂浓度升高产生一系列的响应.本文总结了国内外关于大气CO₂浓度升高对水体理化性质、硝化作用、反硝化作用及N形态转化影响方面的研究工作,发现大气CO₂浓度升高会降低水体的pH,增加水中CO₂和HCO₃^-含量,但对富营养化与寡营养化水体中硝化、反硝化作用的影响具有明显差异.大气CO₂浓度升高抑制寡营养化水体的硝化作用和反硝化作用,降低N₂O的释放通量,抑制富营养化水体的硝化作用,但当水体pH在7~9时,可能促进反硝化作用,增加N₂O的释放通量,最终可能导致水体中NH₄⁺的积累及NO₃^-浓度的降低,影响水体中微生物的多样性.在此基础上提出目前相关研究存在的瓶颈问题及值得深入探讨的科学问题,为进一步深入理解温室效应背景下全球CO₂浓度升高对水体生态系统N循环的影响提供参考.