铜镉污染土壤上CO2浓度升高对籼稻稻米品质的影响

采用盆栽试验,利用开顶式气室(Open Top Chamber,OTC)研究了5个籼稻品种在高、低铜镉复合污染土壤上,CO2浓度升高对水稻生长及吸收Cu、Cd和矿质元素Fe、Zn、Ca、Mn的影响,并对稻米中Cd的安全性进行了评价,了解Cd污染对人类健康的潜在风险。结果表明:CO2浓度升高,显著降低了低复合污染土壤上稻米的生物量,而显著增加了高复合污染土壤上的稻米生物量。CO2浓度升高降低了低污染土壤上稻米Cu含量,降低幅度为4.75%—24.49%,增加了高污染土壤上稻米Cu含量,增加幅度为6.60%—40.37%;而稻米Cu的总吸收量在低、高复合污染土壤上均是降低的。低、高复合污染土壤上,CO2浓度升高显著降低了三香优974稻米的Cd含量和吸收量;增加了其他4个品种稻米Cd含量和吸收量。CO2浓度升高对不同品种稻米中Fe、Zn、Ca、Mn含量影响存在显著差异。CO2浓度正常、升高条件下,两种污染土壤上金优463稻米中Cd含量超过食品卫生标准(Cd≤0.2mg/kg),三香优974在正常CO2浓度条件下其稻米Cd含量超过食品卫生标准。在低、高复合污染土壤上,金优463和三香优974稻米中Cd的THQ值均大于1,说明对人体暴露接触的潜在风险比较严重。CO2浓度升高显著降低了三香优974稻米中Cd对人体暴露接触的潜在风险,而对其他4个水稻品种稻米Cd的THQ值影响不明显。     

CO2浓度升高对龙血树和春羽生长及光合生理的影响

采用开顶式气室（OTC）控制模拟环境,研究了二氧化碳（CO₂）浓度升高对龙血树和春羽叶片光合生理及叶绿素荧光参数的影响。结果表明:（1）随着CO₂浓度增加,龙血树和春羽幼苗叶面积和株高均呈显著增加趋势。（2）龙血树和春羽幼苗叶片净光合速率随着CO₂浓度的升高均呈先增加后降低的趋势,而同期蒸腾速率和气孔导度显著降低。（3）随着CO₂浓度的增加,龙血树和春羽幼苗叶片最大光量子产量、实际光能转化效率均呈先升后降的趋势,而同期非光化学猝灭系数呈先降低后升高的趋势;光化学猝灭系数总体上也呈先升高后降低的趋势,但差异不显著。研究表明,一定时间的高浓度CO₂处理提高了龙血树和春羽的净光合速率,促进了植物的生长,但随着处理时间的延长,这种促进作用逐渐降低进而消失,并以春羽幼苗表现得更突出;即高浓度CO₂可能破坏了龙血树及春羽生长后期光系统Ⅱ反应中心结构,导致叶片光合能力降低。     

大气CO2和O3浓度升高对水稻根际土壤胞外酶活性的影响

大气二氧化碳(CO₂)和臭氧(O₃)浓度升高是全球气候变化的主要特征之一。土壤胞外酶作为维持土壤生态系统服务功能的重要参与者,其活性对于大气CO₂和O₃浓度升高的响应特征及驱动机制研究,以及应对并缓解未来全球气候变化具有重要意义。本研究采用开顶式气室(OTCs)分别模拟大气CO₂浓度升高(环境大气+200μmol·mol^-1,eCO₂)、大气O₃浓度升高(环境大气+0.04μmol·mol^-1,eO₃)及其交互处理(环境大气+200μmol·mol^-1 CO₂+0.04μmol·mol^-1 O₃,eCO₂+eO₃),探究水稻根际土壤胞外酶活性对大气CO₂和O₃浓度升高的响应。结果表明：与对照(环境...     

杉木人工林不同深度土壤CO2通量

土壤CO₂通量具有明显的时间和空间变异性。土壤温度和含水量是影响土壤CO₂通量的重要因素,同时,不同深度的土壤CO₂通量对温度和含水量变化的响应差异较大,因此,研究土壤CO₂通量和影响因素随土壤深度的变化,对于准确评估土壤碳排放具有重要意义。选择福建三明杉木人工林(Cunninghamia lanceolata)作为研究对象,利用非散射红外CO₂浓度探头和Li-8100开路式土壤碳通量系统,并使用Fick扩散法计算了0-60cm深度土壤CO₂的通量,结果表明:(1)5种扩散模型计算的表层(5cm)CO₂通量与Li-8100测量结果均具有显著相关性(P<0.01),Moldrup气体扩散模型计算结果较好。(2)土壤CO₂浓度随深度的增加而升高,但60cm深度以下土壤CO₂浓度开始降低;不同深度土壤CO₂浓度的日变化均呈现单峰型;0-60cm土壤CO₂通量日通量均值变化范围为0.54-2.17μmol m^-2 s^-1;(3)指数拟合分析显示,5、10cm和60cm深度处土壤CO₂通量与温度具有显著相关性,Q₁₀值分别为1.35、2.01和4.95。不同深度土壤含水量与CO₂通量的相关性不显著。     

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。     

大气CO2浓度升高对不同施氮土壤酶活性的影响

利用中国唯一的无锡FACE（Free-air CO₂ enrichment,开放式空气CO₂浓度升高）平台,研究了大气CO₂浓度升高对土壤β-葡糖苷酶、转化酶、脲酶、酸性磷酸酶、β-氨基葡糖苷酶的影响。研究发现,不同氮肥处理下大气CO₂浓度升高对某些土壤酶活性的影响不同。在低氮施肥处理中,大气CO₂浓度升高显著降低β-葡糖苷酶活性,但是在高氮施肥处理下,大气CO₂浓度升高显著增加β-葡糖苷酶活性。在低氮和常氮施肥处理中大气CO₂浓度升高显著增加了土壤脲酶活性,但在高氮水平下影响不显著。在低氮、常氮施肥处理中,大气CO₂浓度升高对土壤酸性磷酸酶活性没有影响,而在高氮施肥处理中显著增强了土壤中磷酸酶活性。大气CO₂浓度升高对土壤转化酶活性和β-氨基葡糖苷酶的活性有增加趋势,但影响不显著。研究还发现,在不同的CO₂浓度下,土壤酶活性对不同氮肥处理的响应也不同。在正常CO₂浓度下,土壤中β-葡糖苷酶活性随着氮肥施用量的增加而降低,而在大气CO₂浓度升高条件下,却随着氮肥施用量的增加而增加。在大气CO₂浓度升高条件下,高氮施肥显著增加了转化酶和酸性磷酸酶活性,而在正常CO₂浓度下,影响不显著。在大气CO₂浓度升高条件下,氮肥处理对脲酶活性的影响不大,但在正常CO₂浓度下,脲酶活性随着氮肥施用量的增加而增加。氮肥对β-氨基葡糖苷酶活性的影响不明显。     

CO2浓度升高和不同灌溉量对东北玉米光合特性及产量的影响

CO2和水分是植物光合作用的重要底物,大气CO2浓度升高或水分变化影响植物光合作用。玉米是重要的C4植物,目前已成为我国第一大作物。我国东北地区的玉米产量占全国玉米产量的1/3左右,对确保国家的粮食安全具有重要作用。但是,关于CO2浓度升高或水分变化共同作用对东北玉米的光合速率、水分利用效率和产量影响的研究甚少。基于开顶式生长箱(OTCs),模拟研究了CO2浓度变化(390、450、550μmol/mol)和降水变化(0、+15%(以试验地锦州1981—2010年6、7、8月月平均降水量88.7,153.9 mm和139.8 mm为基准))共同作用对玉米光合特性及产量的影响。以玉米品种丹玉39为材料,利用直角双曲线修正模型对6个处理(C550W+15%、C550W0、C450W+15%、C450W0、C390W+15%和C390W0)的光响应曲线进行了拟合。结果表明:在CO2浓度升高和灌溉的共同作用下,玉米叶片净光合速率(Pn)升高,且灌溉作用大于高CO2浓度作用;而蒸腾速率(Tr)则下降,使水分利用效率(WUE)升高。CO2浓度升高使气孔导度(Gs)降低,灌溉则使之升高,但灌溉的作用小于高CO2浓度作用;胞间CO2浓度(Ci)随CO2浓度增加而升高,灌溉对其影响不明显。高CO2浓度和灌溉共同作用下光响应参数差异明显。CO2浓度升高增加了最大净光合速率(Pnmax)和光饱和点(LSP),灌溉亦然;CO2浓度升高使得光补偿点(LCP)、光补偿点量子效率(φc)和暗呼吸速率(Rd)的灌溉处理和自然降水处理的差距变小。390、450、550μmol/mol CO2浓度下的灌溉处理与自然降水处理相比,叶面积分别增加了11.56%、3.31%和0.45%,干物质积累量分别增加了14.69%、8.09%和1.01%,最终使产量分别增加了10.47%、12.07%和8.96%。可见,在高CO2浓度下,适量的灌溉对玉米的整个光合作用过程起到了促进作用,最终表现为籽粒产量的增加。为研究者评估气候变化对中国东北地区作物光合能力和产量的影响及决策者调整适应气候变化措施方面提供依据。     

CO2浓度升高与硝化抑制剂对冬小麦田间N2O排放量的影响

以冬小麦中麦175为供试品种,利用农田开放式CO_2浓度增高(FACE)系统,研究未来大气高CO_2浓度对冬小麦田间N_2O排放的影响,以及施用硝化抑制剂(2-氯-6-三氯甲基吡啶)是否可以起到抑制冬小麦田间N_2O的排放量升高的潜能。试验结果表明:CO_2浓度升高显著提高冬小麦田间N2O的排放增幅达到67.6%,追肥灌溉后小麦田N_2O排放量较大,随着冬小麦生育进程的推进N_2O的排放量逐渐减少,硝化抑制剂对中麦175田间N_2O排放量的影响并不明显。因此,在未来高CO_2浓度环境条件下,可以通过采取相应的耕作制度和栽培技术措施等来降低冬小麦田N_2O的排放量。试验结果对冬小麦田间是否选择施用2-氯-6-三氯甲基吡啶来控制N_2O的排放起到一定的参考作用。     

模拟CO2浓度升高和降雨量变化对红砂生物量分配及碳氮特征的影响

以荒漠优势植物红砂2年生苗木为试材,采用盆栽试验和开顶式CO_2控制气室模拟CO_2浓度变化(350μmol/mol和700μmol/mol)研究了红砂生物量分配及碳氮特征对降水变化减少30%、减少15%、自然降水、增加15%和增加30%(-30%、-15%、0、15%、30%)的响应。结果表明:(1)CO_2浓度上升显著性的促进红砂地上茎叶和地下的根生物量,降雨量增加或减少也显著性的促进或抑制了这一作用;CO_2倍增时,红砂的地上生物量在降水增加30%时平均增加了61.28%(P0.05),而根生物量在降水增加或减少30%时均分别增加了84%(30%)和3.21%(-30%),这种响应导致红砂根冠比在降水减少时大于降雨量增加时,CO_2倍增显著地抑制了这一作用。(2)CO_2浓度上升显著性地促进了红砂根、茎、叶中的碳含量,显著性地抑制了红砂根、茎、叶中氮含量,降雨量增加或减少也显著性的促进或抑制了这一作用;这种响应导致红砂根、茎、叶的C/N在降雨减少30%时增加80.22%(根)、103.02%(茎)和199.88%(叶)(P0.05),在降雨增加30%时增加24.99%(根)、30.27%(茎0)和104.45%(叶)(P0.05),CO_2浓度倍增显著性地促进了这一作用。(3)以上结果表明,未来全球CO_2浓度升高时,在降雨量增加地区红砂因充足的碳源和水分而得以恢复;在降雨减少的地区,CO_2的升高对降雨减少造成的干旱胁迫有一定的补偿作用,红砂则以较高的根冠比来维持其在荒漠生态系统中地位。     

CO2升高对枝角类群落结构影响的原位模拟

分别于春、夏两季在太湖梅梁湾进行原位试验,设置3个CO_2浓度梯度,270、380μL/L和750μL/L,以斜生栅藻作为枝角类的食物,研究了CO_2浓度升高对枝角类群落结构的影响。结果表明高CO_2浓度能促进斜生栅藻生长,显著提高枝角类的食物数量;此外CO_2浓度的变化能显著改变枝角类的群落结构,高CO_2浓度有利于象鼻蟤属、秀体蟤属和春季蟤属的生长,而不利于网纹蟤属的生长。这可能是由于CO_2浓度变化改变了枝角类的食物质量,浮游藻类的C∶P比值随CO_2浓度的升高而增加,从而有利于体内含磷量较低,高C∶P的枝角类生长。因此枝角类的群落结构主要受食物质量的影响而与食物的数量无关。研究为预测未来气候变化对太湖浮游动物的影响提供了一些理论依据。     

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.     

土壤CO2及岩溶碳循环影响因素综述

全球碳循环已成为全球气候变化的核心问题之一,岩溶作用对大气CO2浓度的调节以及其与土壤CO2的密切关系也受到了国内外普遍关注。岩溶作用消耗土壤CO2对大气碳库起到了重要的减源作用,对土壤CO2进行研究将有利于进一步揭示岩溶碳循环过程。因此从气候条件、土壤理化性质、土地利用类型等方面综述了土壤CO2的影响因素以及其对岩溶碳循环的影响,并提出其它酸参与到岩溶碳循环中将会减弱岩溶碳汇效应。由于各个因素之间往往相互联系,共同影响土壤CO2和岩溶碳循环,在研究岩溶碳汇时,需以地球系统科学和岩溶动力系统理论为指导,综合考虑大气圈、水圈、岩石圈、生物圈中各种因素的影响。     

Effects of simulated elevated concentration of atmospheric CO2 and temperature on soil enzyme activity in the subalpine fir forest

Little is known about the responses of the activities of soil enzymes that are related to mass cycle to simulated climate change. Therefore, 72 intact soil columns from the primary fir (Abies faxoniana Rehder & E. H. Wilson) forest were parked in environment-controlled chambers with the CK (outside ambient CO₂ concentration and temperature), EC (elevated concentration CO₂ with (347.1 ± 22.1) μmol·mol^?1), ET (elevated temperature with (2.4 ± 0.4)°C), and ECT (elevated CO₂ concentration with (352.8 ± 27.6) μmol·mol^?1 and temperature with (2.2 ± 0.5)°C) treatments, and the activities of invertase, urease, nitrate reductase and acid phosphatase, which are related to the cycles of carbon, nitrogen and phosphorus in mineral soil (MS) and organic layer (OL) were measured simultaneously to understand the responses of these enzymes to climate change. Significant monthly variations on the activities of the studied enzymes were found in both OL and MS with the highest enzyme activities in summer, which were of ecological significance for soil nutrient availability and tree nutrition in the subalpine forest ecosystem. Different monthly patterns of enzyme activities were attributed to enzyme sources and soil layer. EC treatment had influenced slightly on the activities of the studied enzymes resulting from the higher CO₂ concentration in soil atmosphere and no indirect effect from the EC owing to a lack of trees planted on soils. ET treatment increased enzyme activities in comparison with the CK treatment because ET was beneficial to microbial growth and propagation. The increments of the enzyme activities in OL were higher than those in MS, implying that OL is more sensitive to climate change. ECT treatment sharply increased enzyme activities in comparison with the EC and CK, but there was no significant difference between ET and ECT, which was also attributed to no indirect effect by EC treatment owing to trees not planted on soils, implying that the increment of enzyme activities resulted from the temperature effect. However, further studies on indirect effect and complex effect on soil enzyme activity caused by EC, ET and ECT are needed to understand the soil enzyme responses to the climate change.     

高浓度CO2对树木生理生态的影响研究进展

大气CO2浓度升高已成为世界范围内的重要环境问题。CO2浓度升高势必会对植物的生理生态变化产生重要影响。综述了国内外有关高浓度CO2对树木生理生态影响研究的最新进展,具体包括高浓度CO2对树木生长发育、光合和呼吸作用、抗氧化系统、树木代谢物质、挥发性有机化合物以及树木凋落物等方面的影响。高浓度CO2一般会促进树木地上植株的生长和发育,但也因树种差异而有所不同。最新研究表明,高浓度CO2促进了树木细根周转,树木根系生长在大气CO2浓度升高条件下表现为促进作用,这种作用加快了全球森林生态系统的C循环。高浓度CO2虽然在一定程度上促进树木光合速率的增加,但长期熏蒸也往往会发生光合驯化,这种现象产生的生理学机制目前仍无定论。高浓度CO2对树木呼吸作用尤其是根系呼吸的影响将是未来研究的重点和难点。高浓度CO2一般会提高树木抗氧化酶活性与抗氧化剂含量,但不同树种响应高浓度CO2的过程和机理也有所差异。研究表明,高浓度CO2一般对树木凋落物的分解产生不利影响,但也因树种而异。需要强调的是,目前关于树木地下部分、树木对高浓度CO2的适应机理和重要过程(碳氮水耦合及基因调控等)以及多个树种包括不同类型树种及不同品种之间比较研究较少;关于某一重要生理生态机制(如根系生理代谢)尤其是多个生态因子复合条件下缺乏长期深入的研究。在此基础上给出了大气CO2浓度升高下树木生理生态学研究的未来发展方向,包括高CO2浓度条件下树木根系生理代谢及机制、树木碳氮水耦合的生理过程及机制、不同生态因子复合作用对树木生理影响机制以及树木分子作用机理等方面的研究。这些研究不仅将丰富森林树木应对未来气候变化的有关科学理论,也为全球气候变化背景下实现森林树种生态功能的优化选择及森林生态系统的可持续发展与经营提供重要的生理生态学理论依据和参考。     

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。     

大气CO2浓度及温度升高对高山灌木鬼箭锦鸡儿(Caragana jubata)生长及抗氧化系统的影响

以CO_2浓度及温度升高为主要标志的全球气候变化将对我国西北地区脆弱的生态系统产生重要影响。利用环境控制实验研究CO_2浓度倍增(eCO_2, C_1:400μmol/mol和C_2:800μmol/mol)和温度升高(eT, T_1:20℃/10℃和T_2:23℃/13℃)对高山灌木鬼箭锦鸡儿(Caragana jubata)生长及抗氧化系统的影响。结果表明:eCO_2和eT表现出相反的生长和生理效应,eT对幼苗生长的影响要大于eCO_2对其的影响。eT使幼苗的总生物量、净光合速率(NAR)和相对生长速率(RGR)降低;但可促进地上部分生长,叶生物量比及叶面积比增加。eCO_2可减缓或补偿由eT引起的总生物量、NAR和RGR的降低,并促进地下部分生长。对抗氧化系统来说,eT使得超氧化歧化酶(SOD)、过氧化物酶(POD)及抗坏血酸过氧化物酶(APX)活性降低,还原型谷胱甘肽(GSH)和抗坏血酸(ASA)含量降低;eCO_2只增加常温下SOD酶活性,并使GSH、ASA整体水平提高。结论:温度升高和CO_2浓度倍增没有协同促进鬼箭锦鸡儿幼苗的生长和光合能力。温度升高将对幼苗生长和抗氧化系统产生不利影响,eCO_2可促进生长并可能通过抗氧剂含量增加来缓解氧化胁迫。因此,未来气候变化,尤其是温度升高将会对高寒区植物产生较大影响,CO_2浓度增加可缓解增温的不利影响。     

斯洛文尼亚典型岩溶区土壤剖面CO2冬季动态变化特征

土壤CO₂是岩溶作用的重要驱动力,也是陆地生态系统碳循环与岩溶碳循环的纽带。选择斯洛文尼亚典型岩溶区草地生态系统土壤剖面,开展大气与土壤CO₂、土壤水分与土壤温度等指标高分辨率监测,分析不同指标动态变化、分层效应及相互关系。结果表明,土壤温度、水分和CO₂含量变幅分别为3.8—12.9℃、26.9%—34.7%和(682—6760)×10^-6。土壤温度变化趋势与气温变化一致,上部土壤层随气温出现昼夜变化,响应敏感,下部土壤层则表现为多日变化;土壤水分变化主要受降雨控制,对降雨过程响应及时,不同深度分层效应显著,上部与下部含量较高,暗示草地根系有利于土壤水分保持,土岩界面的存在可能是下部保持较高水分的原因。土壤CO₂含量总体上受土温控制,随着深度增加逐渐升高。降雨过程中,不同深度土壤CO₂含量均有不同程度且较快速的升降现象,暗示雨水入渗土壤层后产生的活塞效应和随后的向下迁移是导致土壤CO₂含量陡升陡降的主要原因。从降雨过程大气CO