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1.
T. Vesala T. Markkanen L. Palva E. Siivola S. Palmroth P. Hari 《Agricultural and Forest Meteorology》2000,100(4)
A set-up with 161 photosynthetically active radiation (PAR) sensors was used to investigate spatio-temporal variations of irradiance for five horizontal arrays within a Scots pine canopy. The measured PAR was converted to CO2 exchange using of a shoot-scale photosynthetic response curve and the vertical distribution of the needle area. The net ecosystem exchange was simultaneously measured by the eddy covariance technique. The effect of spatial and temporal averaging of the PAR values and the number of sensors were analysed under different conditions as regards cloudiness and the shading by the foliage. In 1/2 h CO2 exchange values for the entire canopy, a maximum overestimation of 30% resulted from a spatial averaging over horizontal arrays of 2–5 m and occurred under clear-sky conditions and significant foliage shading. Under partly cloudy conditions, the largest overestimation occurred for a case of little shading and the inaccuracy resulting from 1/2 h temporal averaging exceeded that of spatial averaging. 相似文献
2.
大气[CO2]和温度升高对农作物生理及生产的影响 总被引:3,自引:6,他引:3
全球大气[CO2]和气温升高是全球气候变化对农作物产量影响最为重要的两个因子。本文着重介绍了[CO2]和温度升高对农作物光合作用、呼吸作用、蒸腾作用、产量、品质等方面影响的研究进展。研究表明随着[CO2]升高,作物光合速率及蒸腾速率有上升趋势,呼吸作用和气孔导度下降,产量有所提高,品质将会降低,但研究仍有不确定性。随着[CO2]变化,不同光合途径(C3、C4)作物的响应不一致且存在短期和长期效应。普遍认为大气温度升高抑制作物光合作用,作物产量下降。现有的研究多采用模型或模拟试验的方法研究气候变化对作物产量的影响,但研究发现模型研究结果与模拟试验研究结果有差异,不同学者对产量的评估结果也不一致。最新研究认为温度对作物产量影响成非线性,当温度高于关键温度后产量会迅速下降。现阶段大部分模拟试验均在气室中研究,与野外实际情况差异较大,结论仍需进一步验证。目前尚缺乏对作物模型结果的实验验证。 相似文献
3.
水肥一体化对生姜生长及叶片CO2、H2O交换特性的影响 总被引:4,自引:0,他引:4
以“莱芜大姜”为试材,研究了等量施肥条件下,沟灌常规施肥(CK)、滴灌常规施肥(T1)、水肥一体化(T2)对生姜生长,叶片H2O、CO2交换参数等的影响.结果表明,不同处理生姜地上部茎叶干物质量无显著差异,但T1、T2处理的地下根茎干物质量分别较CK增加11.15%和16.95%.水肥一体化可显著提高生姜叶片色素含量和净光合速率(Pn),降低蒸腾速率(Tr),提高水分利用效率(WUE).生姜根茎膨大期(9月16日),T1、T2处理叶片叶绿素含量和Pn分别比CK高6.77%、8.99%和10.21%、16.23%;生姜发棵期(8月20日),T1、T2处理叶片的Tr分别比CK低10.19%和9.42%;T1、T2处理的WUE无显著差异,但显著高于CK,8月26日9:00达峰值时,T1、T2的WUE分别比CK高23.83%和28.74%.T1、T2处理的灌溉水生产效率分别比CK高132.06%和146.79%;肥料偏生产力分别高12.54%和17.94%. 相似文献
4.
David J.P. Moore Jia Hu William J. Sacks David S. Schimel Russell K. Monson 《Agricultural and Forest Meteorology》2008,148(10):1467-1477
Modeling how the role of forests in the carbon cycle will respond to predicted changes in water availability hinges on an understanding of the processes controlling water use in ecosystems. Recent studies in forest ecosystem modeling have employed data-assimilation techniques to generate parameter sets that conform to observations, and predict net ecosystem CO2 exchange (NEE) and its component processes. Since the carbon and water cycles are linked, there should be additional process information available from ecosystem H2O exchange. We coupled SIPNET (Simple Photosynthesis EvapoTranspiration), a simplified model of ecosystem function, with a data-assimilation system to estimate parameters leading to model predictions most closely matching the net CO2 and H2O fluxes measured by eddy covariance in a high-elevation, subalpine forest ecosystem. When optimized using measurements of CO2 exchange, the model matched observed NEE (RMSE = 0.49 g C m−2) but underestimated transpiration calculated independently from sap flow measurements by a factor of 4. Consequently, the carbon-only optimization was insensitive to imposed changes in water availability. Including eddy flux data from both CO2 and H2O exchange to the optimization reduced the model fit to the observed NEE fluxes only slightly (RME = 0.53 g C m−2), however this parameterization also reproduced transpiration calculated from independent sap flow measurements (r2 = 0.67, slope = 0.6). A significant amount of information can be extracted from simultaneous analysis of CO2 and H2O exchange, which improved the accuracy of transpiration estimates from measured evapotranspiration. Conversely, failure to include both CO2 and H2O data streams can generate results that mask the responses of ecosystem carbon cycling to variation in the precipitation. In applying the model conditioned on both CO2 and H2O fluxes to the subalpine forest at the Niwot Ridge AmeriFlux site, we observed that the onset of transpiration is coincident with warm soil temperatures. However, after snow has covered the ground in the fall, we observed significant inter-annual variability in the fraction of evapotranspiration composed of transpiration; evapotranspiration was dominated by transpiration in years when late fall air temperatures were high enough to maintain photosynthesis, but by sublimation from the surface of the snowpack in years when late fall air temperatures were colder and forest photosynthetic activity had ceased. Data-assimilation techniques and simultaneous measurements of carbon and water exchange can be used to quantify the response of net carbon uptake to changes in water availability by using an ecosystem model where the carbon and water cycles are linked. 相似文献
5.
Environmental control of net ecosystem CO2 exchange in a treed, moderately rich fen in northern Alberta 总被引:1,自引:1,他引:1
Kamran H. Syed Lawrence B. Flanagan Peter J. Carlson Aaron J. Glenn K. Eric Van Gaalen 《Agricultural and Forest Meteorology》2006,140(1-4):97
Peatlands cover about 21% of the landscape and contain about 80% of the soil carbon stock in western Canada. However, the current rates of carbon accumulation and the environmental controls on ecosystem photosynthesis and respiration in peatland ecosystems are poorly understood. As part of Fluxnet-Canada, we continuously measured net ecosystem carbon dioxide exchange (NEE) using the eddy covariance technique in a treed fen dominated by stunted Picea mariana and Larix laricina trees during August 2003–December 2004. The total carbon stock in the ecosystem was approximately 51,000 g C m−2, with only 540 g C m−2 contributed by live above ground vegetation. The NEE measurements were used to parameterize simple physiological models to assess temporal variation in maximum ecosystem photosynthesis (Amax) and ecosystem respiration rate at 10 °C (R10). During mid-summer the ecosystem had a relatively high Amax (approx. 30 μmol m−2 s−1) with relatively low R10 (approx. 4 μmol m−2 s−1). The peak mid-day NEE uptake rate during July and August was 10 μmol m−2 s−1. The ecosystem showed large seasonal variation in photosynthetic and respiratory activity that was correlated with shifts in temperature, with both spring increases and fall decreases in Amax well predicted by the mean daily air temperature averaged over the preceding 21 days. Leaf-level gas exchange and spectral reflectance measurements also suggested that seasonal changes in photosynthetic activity were primarily controlled by shifts in temperature. Ecosystem respiration was strongly correlated with changes in ecosystem photosynthesis during the growing season, suggesting important links between plant activity and mycorrhizae and microbial activity in the shallow layers of the peat. Only very low rates of respiration were observed during the winter months. During 2004, the peatland recorded a net annual gain of 144 g C m−2 year−1, the result of a difference between gross photosynthesis of 713 and total ecosystem respiration of 569 g C m−2 year−1. 相似文献
6.
利用环境生长室探讨不同CO2浓度和土壤水分亏缺处理下玉米植株生物量、气孔形态与分布特征、叶片气体交换参数、叶绿素荧光参数等生长及生理指标的变化规律。以‘郑单958’ 玉米品种为试材,利用环境生长室设置2个CO2浓度和4个土壤水分梯度对玉米进行CO2浓度和水分处理。结果表明:1)不同程度土壤水分亏缺均显著降低玉米地上生物量(P<0.05),但CO2浓度升高增加了轻度水分亏缺条件下玉米地上生物量(P<0.01)和总生物量(P<0.01)。2)大气CO2浓度升高导致轻度和中度水分亏缺条件下玉米的净光合速率(Pn)分别提高15.8%(P<0.05)和25.7%(P=0.001),而CO2浓度升高却降低了玉米叶片蒸腾速率(P<0.001)和气孔导度(P<0.001),最终导致玉米瞬时水分利用效率均显著提高(P<0.001)。3)不同水分处理对玉米叶片气孔密度和单个气孔形态特征均造成显著影响(P<0.01)。因此,大气CO2浓度升高可以增加轻度水分亏缺条件下玉米叶片氮含量、叶片非结构性碳水化合物含量和光合电子传递速率,从而提高玉米植株的生物量累积以及叶片碳同化能力和水分利用效率。研究结果将为深入理解气候变化背景下玉米对大气CO2浓度升高和土壤水分亏缺的生理生态响应机制提供科学依据。 相似文献
7.
Stephen J. Livesley Samantha GroverLindsay B. Hutley Hizbullah JamaliKlaus Butterbach-Bahl Benedikt FestJason Beringer Stefan K. Arndt 《Agricultural and Forest Meteorology》2011,151(11):1440-1452
Tropical savanna ecosystems are a major contributor to global CO2, CH4 and N2O greenhouse gas exchange. Savanna fire events represent large, discrete C emissions but the importance of ongoing soil-atmosphere gas exchange is less well understood. Seasonal rainfall and fire events are likely to impact upon savanna soil microbial processes involved in N2O and CH4 exchange. We measured soil CO2, CH4 and N2O fluxes in savanna woodland (Eucalyptus tetrodonta/Eucalyptus miniata trees above sorghum grass) at Howard Springs, Australia over a 16 month period from October 2007 to January 2009 using manual chambers and a field-based gas chromatograph connected to automated chambers. The effect of fire on soil gas exchange was investigated through two controlled burns and protected unburnt areas. Fire is a frequent natural and management action in these savanna (every 1-2 years). There was no seasonal change and no fire effect upon soil N2O exchange. Soil N2O fluxes were very low, generally between −1.0 and 1.0 μg N m−2 h−1, and often below the minimum detection limit. There was an increase in soil NH4+ in the months after the 2008 fire event, but no change in soil NO3−. There was considerable nitrification in the early wet season but minimal nitrification at all other times.Savanna soil was generally a net CH4 sink that equated to between −2.0 and −1.6 kg CH4 ha−1 y−1 with no clear seasonal pattern in response to changing soil moisture conditions. Irrigation in the dry season significantly reduced soil gas diffusion and as a consequence soil CH4 uptake. There were short periods of soil CH4 emission, up to 20 μg C m−2 h−1, likely to have been caused by termite activity in, or beneath, automated chambers. Soil CO2 fluxes showed a strong bimodal seasonal pattern, increasing fivefold from the dry into the wet season. Soil moisture showed a weak relationship with soil CH4 fluxes, but a much stronger relationship with soil CO2 fluxes, explaining up to 70% of the variation in unburnt treatments. Australian savanna soils are a small N2O source, and possibly even a sink. Annual soil CH4 flux measurements suggest that the 1.9 million km2 of Australian savanna soils may provide a C sink of between −7.7 and −9.4 Tg CO2-e per year. This sink estimate would offset potentially 10% of Australian transport related CO2-e emissions. This CH4 sink estimate does not include concurrent CH4 emissions from termite mounds or ephemeral wetlands in Australian savannas. 相似文献
8.
Aaron J. Glenn Lawrence B. Flanagan Kamran H. Syed Peter J. Carlson 《Agricultural and Forest Meteorology》2006,140(1-4):115
Net ecosystem carbon dioxide exchange was measured in two contrasting peatlands in northern Alberta, Canada using the eddy covariance technique during the growing season (May–October). Sphagnum spp. made up approximately 66% of the total LAI (1.52 m2 m−2) at the poor fen and the total N content of Sphagnum capitula was 7.8 mg g−1 at the peak of the growing season. In contrast, the dominant plant species at the extreme-rich fen site, the perennial sedge, Carex lasiocarpa, accounted for approximately 60% of the total LAI (1.09 m2 m−2), and had leaf total N content of 19.3 mg g−1 at peak biomass. In addition, the peak aboveground biomass was higher at the poor fen (230.9 g m−2) than at the extreme-rich fen (157.1 g m−2). Both sites had maximum daily rates of net CO2 uptake of approximately 5 μmol m−2 s−1, and typical nighttime rates of CO2 loss of approximately 2 μmol m−2 s−1 during the peak of the growing season. Calculations of maximum photosynthetic and respiratory capacity were consistently higher at the extreme-rich fen. The poor fen was a net sink for CO2 during 4 of the 6 months (peaking at 44 g C m−2 in July), while only slight net losses of CO2 (3 g C m−2) occurred in May and September. In contrast, the extreme-rich fen was calculated to be a significant net sink for CO2 only during 2 months of the growing season (peaking at 30 g C m−2 in August), while significant net losses of CO2 occurred in May (8 g C m−2) and in October (13 g C m−2). The plant species at the poor fen site were active earlier and later in the growing season, while it took longer for C. lasiocarpa to develop leaf tissue, and leaf senescence and reduction in photosynthetic activity occurred earlier in the fall at the extreme-rich fen. When integrated over the 6-month growing season, the poor fen was a net sink (90 g C m−2) that was three times larger than the extreme-rich fen (31 g C m−2). The ratio of cumulative total ecosystem respiration to gross primary production was 0.7 at the poor fen and 0.9 at the extreme-rich fen. 相似文献
9.
N. Morley 《Soil biology & biochemistry》2010,42(10):1864-117
Here we provide evidence that the form of carbon compound and O2 concentration exert an inter-related regulation on the production and reduction of N2O in soil. 6.7 mM d-glucose, 6.7 mM D-mannitol, 8 mM L-glutamic acid or 10 mM butyrate (all equivalent to 0.48 g C l−1) were applied to slurries of a sandy loam soil. At the start of the experiment headspace O2 concentrations were established at ∼2%, 10% and 21% O2 v/v for each C treatment, and 2 mM K15NO3 (25 atom % excess 15N) was applied, enabling quantification of 15N-N2 production, 15N-(N2O-to-N2) ratios and DNRA. The form of C compound was most important in the initially oxic (21% O2 v/v) soils, where addition of butyrate and glutamic acid resulted in greater N2O production (0.61 and 0.3 μg N2O-N g−1 soil for butyrate and glutamic acid, respectively) than the addition of carbohydrates (glucose and mannitol). Although, there was no significant effect of C compound at low initial O2 concentrations (∼2% O2 v/v), production of 15N-N2 was greatest where headspace O2 concentrations were initially, or fallen to, ∼2% O2 v/v, with greatest reduction of N2O and lowering 15N-(N2O-to-N2) ratios (∼0-0.27). This may reflect that the effect of C is indirect through stimulation of heterotrophic respiration, lowering O2 concentrations, providing sub-oxic conditions for dissimilatory nitrate reduction pathways. Addition of carbohydrates (glucose and mannitol) also resulted in greatest recovery of 15N in NH4+ from applied 15N-NO3−, indicative of the occurrence of DNRA, even in the slurries with initial 10% and 21% O2 v/v concentrations. Our 15N approach has provided the first direct evidence for enhancement of N2O reduction in the presence of carbohydrates and the dual regulation of C compound and O2 concentration on N2O production and reduction, which has implications for management of N2O emissions through changing C inputs (exudates, rhizodeposition, residues) with plant species of differing C traits, or through plant breeding. 相似文献
10.
The effects of compaction on soil porosity and soil water relations are likely to influence substrate availability and microbial activity under fluctuating soil moisture conditions. We conducted a short laboratory incubation to investigate the effects of soil compaction on substrate availability and biogenic gas (CO2 and N2O) production during the drying and rewetting of a fine-loamy soil. Prior to initiating the drying and wetting treatments, CO2 production (−10 kPa soil water content) from uncompacted soil was 2.3 times that of compacted soil and corresponded with higher concentrations of microbial biomass C (MBC) and dissolved organic C (DOC). In contrast, N2O production was 67 times higher in compacted than uncompacted soil at field capacity. Soil aeration rather than substrate availability (e.g. NO3− and DOC) appeared to be the most important factor affecting N2O production during this phase. The drying of compacted soil resulted in an initial increase in CO2 production and a nearly two-fold higher average rate of C mineralization at maximum dryness (owing to a higher water-filled pore space [WFPS]) compared to uncompacted soil. During the drying phase, N2O production was markedly reduced (by 93-96%) in both soils, though total N2O production remained slightly higher in compacted than uncompacted soil. The increase in CO2 production during the first 24 h following rewetting of dry soil was about 2.5 times higher in uncompacted soil and corresponded with a much greater release of DOC than in compacted soil. MBC appeared to be the source of the DOC released from uncompacted soil but not from compacted soil. The production of N2O during the first 24 h following rewetting of dry soil was nearly 20 times higher in compacted than uncompacted soil. Our results suggest that N2O production from compacted soil was primarily the result of denitrification, which was limited by substrates (especially NO3−) made available during drying and rewetting and occurred rapidly after the onset of anoxic conditions during the rewetting phase. In contrast, N2O production from uncompacted soil appeared to be primarily the product of nitrification that was largely associated with an accumulation of NO3− following rewetting of dry soil. Irrespective of compaction, the response to drying and rewetting was greater for N2O production than for CO2 production. 相似文献
11.
Lucy R. Hutyra J. William Munger Elizabeth Hammond-Pyle Scott R. Saleska Natalia Restrepo-Coupe Bruce C. Daube Plinio B. de Camargo Steven C. Wofsy 《Agricultural and Forest Meteorology》2008,148(8-9):1266-1279
The controls on uptake and release of CO2 by tropical rainforests, and the responses to a changing climate, are major uncertainties in global climate change models. Eddy-covariance measurements potentially provide detailed data on CO2 exchange and responses to the environment in these forests, but accurate estimates of the net ecosystem exchange of CO2 (NEE) and ecosystem respiration (Reco) require careful analysis of data representativity, treatment of data gaps, and correction for systematic errors. This study uses the comprehensive data from our study site in an old-growth tropical rainforest near Santarem, Brazil, to examine the biases in NEE and Reco potentially associated with the two most important sources of systematic error in Eddy-covariance data: lost nighttime flux and missing canopy storage measurements. We present multiple estimates for the net carbon balance and Reco at our site, including the conventional “u* filter”, a detailed bottom-up budget for respiration, estimates by similarity with 222Rn, and an independent estimate of respiration by extrapolation of daytime Eddy flux data to zero light. Eddy-covariance measurements between 2002 and 2006 showed a mean net ecosystem carbon loss of 0.25 ± 0.04 μmol m−2 s−1, with a mean respiration rate of 8.60 ± 0.11 μmol m−2 s−1 at our site. We found that lost nocturnal flux can potentially introduce significant bias into these results. We develop robust approaches to correct for these biases, showing that, where appropriate, a site-specific u* threshold can be used to avoid systematic bias in estimates of carbon exchange. Because of the presence of gaps in the data and the day–night asymmetry between storage and turbulence, inclusion of canopy storage is essential to accurate assessments of NEE. We found that short-term measurements of storage may be adequate to accurately model storage for use in obtaining ecosystem carbon balance, at sites where storage is not routinely measured. The analytical framework utilized in this study can be applied to other Eddy-covariance sites to help correct and validate measurements of the carbon cycle and its components. 相似文献
12.
Sebastian Wolf Werner EugsterCatherine Potvin Nina Buchmann 《Agricultural and Forest Meteorology》2011,151(8):1139-1151
Pasture and afforestation are land-use types of major importance in the tropics, yet, most flux tower studies have been conducted in mature tropical forests. As deforestation in the tropics is expected to continue, it is critical to improve our understanding of alternative land-use types, and the impact of interactions between land use and climate on ecosystem carbon dynamics. Thus, we measured net ecosystem CO2 fluxes of a pasture and an adjacent tropical afforestation (native tree species plantation) in Sardinilla, Panama from 2007 to 2009. The objectives of our paired site study were: (1) to assess seasonal and inter-annual variations in net ecosystem CO2 exchange (NEE) of pasture and afforestation, (2) to identify the environmental controls of net ecosystem CO2 fluxes, and (3) to constrain eddy covariance derived total ecosystem respiration (TER) with chamber-based soil respiration (RSoil) measurements. We observed distinct seasonal variations in NEE that were more pronounced in the pasture compared to the afforestation, reflecting changes in plant and microbial activities. The land conversion from pasture to afforestation increased the potential for carbon uptake by trees vs. grasses throughout most of the year. RSoil contributed about 50% to TER, with only small differences between ecosystems or seasons. Radiation and soil moisture were the main environmental controls of CO2 fluxes while temperature had no effect on NEE. The pasture ecosystem was more strongly affected by soil water limitations during the dry season, probably due to the shallower root system of grasses compared to trees. Thus, it seems likely that predicted increases in precipitation variability will impact seasonal variations of CO2 fluxes in Central Panama, in particular of pasture ecosystems. 相似文献
13.
O3与CO2浓度倍增对大豆叶片及其总生物量的影响研究 总被引:4,自引:0,他引:4
利用OTC-1型开顶式气室研究CO2和O3浓度倍增对大豆叶片及其总生物量的影响结果表明,CO2和O3浓度倍增均可致使大豆黄叶率增加,绿叶率下降;CO2浓度倍增使大豆总叶片干物质量和总叶面积、绿叶和黄叶干物质量及总生物量均明显增加;O3浓度倍增使大豆总叶干物质量和总叶面积、绿叶和黄叶干物质量及总生物量均下降;CO2与O3交互作用处理对大豆生物量的影响均表现为CO2>O3;CO2与O3持续倍增处理对大豆叶片老化的影响为O3>CO2,CO2与O3逐渐达倍增的处理在大豆鼓粒前CO2的缓解作用明显,鼓粒后CO2与O3的影响逐渐接近;大豆总生物量增长遵循自然增长曲线。 相似文献
14.
David T. Tingey Mark G. Johnson Claudia Wise David M. Olszyk Kelly K. Donegan 《Soil biology & biochemistry》2006,38(7):1764-1778
Soil respiration represents the integrated response of plant roots and soil organisms to environmental conditions and the availability of C in the soil. A multi-year study was conducted in outdoor sun-lit controlled-environment chambers containing a reconstructed ponderosa pine/soil-litter system. The study used a 2×2 factorial design with two levels of CO2 and two levels of O3 and three replicates of each treatment. The objectives of our study were to assess the effects of long-term exposure to elevated CO2 and O3, singly and in combination, on soil respiration, fine root growth and soil organisms. Fine root growth and soil organisms were included in the study as indicators of the autotrophic and heterotrophic components of soil respiration. The study evaluated three hypotheses: (1) elevated CO2 will increase C assimilation and allocation belowground increasing soil respiration; (2) elevated O3 will decrease C assimilation and allocation belowground decreasing soil respiration and (3) as elevated CO2 and O3 have opposing effects on C assimilation and allocation, elevated CO2 will eliminate or reduce the negative effects of elevated O3 on soil respiration. A mixed-model covariance analysis was used to remove the influences of soil temperature, soil moisture and days from planting when testing for the effects of CO2 and O3 on soil respiration. The covariance analysis showed that elevated CO2 significantly reduced the soil respiration while elevated O3 had no significant effect. Despite the lack of a direct CO2 stimulation of soil respiration, there were significant interactions between CO2 and soil temperature, soil moisture and days from planting indicating that elevated CO2 altered soil respiration indirectly. In elevated CO2, soil respiration was more sensitive to soil temperature changes and less sensitive to soil moisture changes than in ambient CO2. Soil respiration increased more with days from planting in elevated than in ambient CO2. Elevated CO2 had no effect on fine root biomass but increased abundance of culturable bacteria and fungi suggesting that these increases were associated with increased C allocation belowground. Elevated CO2 had no significant effect on microarthropod and nematode abundance. Elevated O3 had no significant effects on any parameter except it reduced the sensitivity of soil respiration to changes in temperature. 相似文献
15.
农田土壤主要温室气体(CO2、CH4、N2O)的源/汇强度及其温室效应研究进展 总被引:35,自引:7,他引:35
气候变化是当今全球面临的重大挑战, 人类社会生产生活引起的温室气体排放是全球气候变暖的主要原因。大气中CO2、CH4 和N2O 是最重要的温室气体, 对温室效应的贡献率占了近80%。据估计, 大气中每年有5%~20%的CO2、15%~30%的CH4、80%~90%的N2O 来源于土壤, 而农田土壤是温室气体的重要排放源。本文重点阐述了农田土壤温室气体产生、排放或吸收机理及其影响因素, 指出土地利用方式和农业生产力水平等人为控制因素通过影响土壤和作物生长条件来影响农田土壤温室气体产生与排放或吸收。所以, 我们可以从人类活动对农田生态系统的影响着手, 通过改善农业生产方式和作物生长条件来探索温室气体减排措施, 达到固碳/氮增汇的目的。对国内外关于农田温室气体排放的源/汇强度及其综合温室效应评估的最新研究进展进行了综述, 指出正确估算与评价农田土壤温室气体的源/汇强度及其对大气中主要温室气体浓度变化的贡献, 有助于为温室气体减排以及减少气候变化预测的不确定性提供理论依据。 相似文献
16.
Timothy D. Meehan Michael S. Crossley Richard L. Lindroth 《Soil biology & biochemistry》2010,42(7):1132-1137
Human alteration of atmospheric composition affects foliar chemistry and has possible implications for the structure and functioning of detrital communities. In this study, we explored the impacts of elevated carbon dioxide and ozone on aspen (Populus tremuloides) leaf litter chemistry, earthworm (Lumbricus terrestris) individual consumption and growth, and springtail (Sinella curviseta) population growth. We found that elevated carbon dioxide reduced nitrogen and increased condensed-tannin concentrations in leaf litter. These changes were associated with decreases in earthworm individual growth, earthworm growth efficiency, and springtail population growth. Elevated ozone increased fiber and lignin concentrations of leaf litter. These changes were not associated with earthworm consumption or growth, but were associated with increased springtail population growth. Our results suggest that changes in litter chemistry caused by increased carbon dioxide concentrations will have negative impacts on the productivity of diverse detritivore taxa, whereas those caused by increased ozone concentrations will have variable, taxon-specific effects. 相似文献
17.
Argyro Zerva 《Soil biology & biochemistry》2005,37(11):2025-2036
We examined the effects of forest clearfelling on the fluxes of soil CO2, CH4, and N2O in a Sitka spruce (Picea sitchensis (Bong.) Carr.) plantation on an organic-rich peaty gley soil, in Northern England. Soil CO2, CH4, N2O as well as environmental factors such as soil temperature, soil water content, and depth to the water table were recorded in two mature stands for one growing season, at the end of which one of the two stands was felled and one was left as control. Monitoring of the same parameters continued thereafter for a second growing season. For the first 10 months after clearfelling, there was a significant decrease in soil CO2 efflux, with an average efflux rate of 4.0 g m−2 d−1 in the mature stand (40-year) and 2.7 g m−2 d−1 in clearfelled site (CF). Clearfelling turned the soil from a sink (−0.37 mg m−2 d−1) for CH4 to a net source (2.01 mg m−2 d−1). For the same period, soil N2O fluxes averaged 0.57 mg m−2 d−1 in the CF and 0.23 mg m−2 d−1 in the 40-year stand. Clearfelling affected environmental factors and lead to higher daily soil temperatures during the summer period, while it caused an increase in the soil water content and a rise in the water table depth. Despite clearfelling, CO2 remained the dominant greenhouse gas in terms of its greenhouse warming potential. 相似文献
18.
To study effect of C2H2 and change of headspace gas on N2O emission,denitrification,as well as CO2 emission,slurries of an agricultural soil were anaerobically incubated for 7 days at 25℃.Both N2O reduction and CO2 emissions were inhibited by the addition of 100 mL L^-1 of C2H2.However,the inhibition to CO2 emission was alleviated by the replacement of headspace gas,and the N2O emission was enhanced by the replacement.Acetylene disappeared evidently from the soil slurries during the incubation.Consequently results obtained from the traditional C2H2 blocking technique for determination of denitrifcation rate,especially in a long-time incubation,should be explained with care because of its side effect exsting in the incubation environments without change of headspace gas.To reduce the possible side effect on the processes other than denitrification ,it is suggested that headspace gas should be replaced several times during a long-time incubation. 相似文献
19.
耕作措施对温带半干旱地区土壤温室气体(CO2、CH4、N2O)通量的影响 总被引:3,自引:1,他引:3
通过设置在甘肃省定西市李家堡镇的不同耕作措施试验, 利用CO2分析仪、静态箱-气相色谱法对双序列轮作次序下春小麦地、豌豆地生育期内CO2、CH4和N2O通量进行了测定。试验结果表明: 4种耕作措施下春小麦地和豌豆地在生育期内均表现为CO2源、N2O源和CH4汇的功能。传统耕作不覆盖、免耕不覆盖、免耕秸秆覆盖和传统耕作结合秸秆还田下, 春小麦生育期内平均土壤CO2通量(μmol·m-2·s-1)分别为0.203 6、0.221 2、0.241 8、0.224 9, CH4通量(mg·m-2·h-1)分别为-0.041 6、-0.078 0、-0.081 8、-0.053 7, N2O通量(mg·m-2·h-1)分别为0.089 1、0.069 2、0.046 1、0.065 6; 豌豆生育期内平均土壤CO2通量(μmol·m-2·s-1)分别为0.273 6、0.261 6、0.218 1、0.236 0, CH4通量(mg·m-2·h-1)分别为-0.055 0、-0.073 7、-0.066 2、-0.054 5, N2O通量(mg·m-2·h-1)分别为0.123 4、0.084 7、0.080 6、0.035 0。少免耕及小麦秸秆覆盖有利于减少土壤CO2排放通量, 免耕不覆盖、免耕秸秆覆盖及传统耕作结合秸秆还田均能不同程度地增加CH4吸收通量、减少N2O排放通量。综合来看, 免耕不覆盖、免耕秸秆覆盖和传统耕作结合秸秆还田3种保护性耕作措施有助于减少土壤温室气体的排放量。春小麦地CO2通量随着土壤温度、土壤含水量的逐渐升高而增大; CH4吸收通量随着土壤含水量的逐渐升高而增大, 而随着土壤温度的逐渐升高而减小。豌豆地CO2通量的变化与土壤含水量存在极显著正相关关系; 而春小麦地N2O通量则与平均土壤温度呈显著正相关, 豌豆地则为极显著正相关。 相似文献
20.
Mette S. Carter Per Ambus Klaus S. Larsen Anders Priemé Claus Beier 《Soil biology & biochemistry》2011,43(8):1660-1670
In temperate regions, climate change is predicted to increase annual mean temperature and intensify the duration and frequency of summer droughts, which together with elevated atmospheric carbon dioxide (CO2) concentrations, may affect the exchange of nitrous oxide (N2O) and methane (CH4) between terrestrial ecosystems and the atmosphere. We report results from the CLIMAITE experiment, where the effects of these three climate change parameters were investigated solely and in all combinations in a temperate heathland. Field measurements of N2O and CH4 fluxes took place 1-2 years after the climate change manipulations were initiated. The soil was generally a net sink for atmospheric CH4. Elevated temperature (T) increased the CH4 uptake by on average 10 μg C m−2 h−1, corresponding to a rise in the uptake rate of about 20%. However, during winter elevated CO2 (CO2) reduced the CH4 uptake, which outweighed the positive effect of warming when analyzed across the study period. Emissions of N2O were generally low (<10 μg N m−2 h−1). As single experimental factors, elevated CO2, temperature and summer drought (D) had no major effect on the N2O fluxes, but the combination of CO2 and warming (TCO2) stimulated N2O emission, whereas the N2O emission ceased when CO2 was combined with drought (DCO2). We suggest that these N2O responses are related to increased rhizodeposition under elevated CO2 combined with increased and reduced nitrogen turnover rates caused by warming and drought, respectively. The N2O flux in the multifactor treatment TDCO2 was not different from the ambient control treatment. Overall, our study suggests that in the future, CH4 uptake may increase slightly, while N2O emission will remain unchanged in temperate ecosystems on well-aerated soils. However, we propose that continued exposure to altered climate could potentially change the greenhouse gas flux pattern in the investigated heathland. 相似文献